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Rose Quartz: The Pink Gemstone

Rose Quartz: The Pink Gemstone
Rose Quartz: The Pink Gemstone

Introduction to Rose Quartz

Rose Quartz is one of the most popular varieties of quartz, recognized for its soft pink hue that ranges from pale blush to a deeper rosy shade. As a member of the quartz family, Rose Quartz stands out for its aesthetic appeal and widespread availability, often used in decorative and industrial applications. This pink gemstone has captivated geologists, gemologists, and collectors for centuries due to its beauty and unique properties.

In this article, we will examine the geological aspects of Rose Quartz, from its formation and mineral composition to its key properties and modern uses.

Geological Formation of Rose Quartz

Rose Quartz, like other forms of quartz, is a silicon dioxide (SiO2) mineral that forms through a variety of geological processes. It typically forms in pegmatites, which are coarse-grained igneous rocks that form during the final stages of magma crystallization. Pegmatites often contain large crystals of quartz, feldspar, and mica, and provide the perfect environment for Rose Quartz to develop.

The Role of Trace Elements in Rose Quartz Color

The distinct pink coloration of Rose Quartz is attributed to trace amounts of titanium, iron, or manganese within the crystal structure. These elements become incorporated into the quartz during its formation, influencing the final hue of the gemstone. Recent studies also suggest that microscopic inclusions of fibrous minerals, such as dumortierite, may contribute to the cloudiness and unique pink color of some Rose Quartz specimens.

Physical and Chemical Properties of Rose Quartz

Rose Quartz shares the same fundamental properties as all members of the quartz family, which is composed of silicon and oxygen in a continuous framework of SiO4 silicon-oxygen tetrahedra.

Chemical Composition and Crystal Structure

  • Chemical Formula: SiO₂ (Silicon Dioxide)
  • Crystal System: Trigonal
  • Hardness: 7 on the Mohs scale
  • Density: 2.65 g/cm³
  • Luster: Vitreous to greasy
  • Cleavage: None (Quartz has conchoidal fracture)

Rose Quartz does not typically form in well-defined crystals like other quartz varieties (e.g., amethyst). Instead, it often occurs in massive form, with the pink coloration being distributed evenly throughout the mineral. Its transparency can range from transparent to translucent, with some specimens appearing more milky due to internal fractures and inclusions.

Durability and Weather Resistance

Quartz, including Rose Quartz, is highly durable, with a hardness of 7 on the Mohs scale, which makes it resistant to scratching and abrasion. This durability makes it suitable for various industrial applications, from construction materials to electronics. Additionally, Rose Quartz, like all quartz, is chemically stable, resisting weathering and most forms of chemical erosion.

Where Rose Quartz Is Found

Rose Quartz is found in a number of regions worldwide, particularly in large pegmatite deposits. Some of the most significant sources include:

  • Brazil: Brazil is one of the largest producers of Rose Quartz, with major deposits located in the states of Minas Gerais and Bahia. Brazilian Rose Quartz is known for its transparency and uniform color.
  • Madagascar: Another important source, Madagascar produces high-quality Rose Quartz with a more intense pink hue.
  • South Dakota, USA: The Black Hills region of South Dakota is renowned for its Rose Quartz deposits, where the stone is often found in pegmatite veins.
  • India: India is also home to significant Rose Quartz deposits, particularly in the states of Karnataka and Tamil Nadu.
  • South Africa: South Africa contributes to the global supply of Rose Quartz, often producing lighter-colored varieties.

Uses of Rose Quartz in Industry and Manufacturing

While Rose Quartz is primarily admired for its aesthetic qualities, it also serves important roles in various industries due to its physical properties.

Jewelry and Ornamental Uses

Rose Quartz is most commonly used in jewelry and as ornamental stones due to its appealing color and ability to be cut and polished into cabochons, beads, and other decorative pieces. Its relatively low cost, compared to other gemstones like diamonds or sapphires, makes it a popular choice for both fine and costume jewelry. Sculptors and artisans also use large masses of Rose Quartz to create carvings, statues, and decorative objects.

Construction and Architectural Uses

Quartz, including Rose Quartz, is often used in the construction industry for its durability and resistance to weathering. Crushed quartz is used in concrete, road construction, and as aggregate in various building materials. Additionally, quartz sand, which may include traces of Rose Quartz, is essential for producing glass, ceramics, and silicon-based materials used in electronics.

The Role of Quartz in Electronics

Quartz crystals have unique piezoelectric properties, meaning they generate an electrical charge when mechanical pressure is applied. This makes quartz essential for use in electronic components, particularly in oscillators, watches, and communication devices. While pure quartz crystals are typically preferred for these applications, the widespread use of quartz highlights the importance of the mineral in modern technology.

Rose Quartz in Geology and Gemology

In both geology and gemology, Rose Quartz holds significance for its formation process and its distinct color, which offers insight into the geological environments where it forms. Rose Quartz’s common association with pegmatites and hydrothermal veins points to the importance of these geological structures in mineral formation.

Gemological Classification

From a gemological perspective, Rose Quartz is classified as a semi-precious stone due to its abundance and affordability compared to other gemstones like emeralds or rubies. While its pink hue makes it highly desirable for decorative purposes, Rose Quartz’s massive form and lack of crystal points mean that it is often shaped into cabochons or beads rather than faceted gems. The rarity of faceted Rose Quartz pieces makes them particularly prized by collectors.

Varieties of Rose Quartz

There are a few notable variations within Rose Quartz that are of interest to collectors and gemologists.

  • Star Rose Quartz: A rare variety of Rose Quartz that exhibits asterism, or a star-like pattern, when light hits it. This phenomenon occurs due to needle-like inclusions of minerals such as rutile, which reflect light in a specific pattern.
  • Transparent Rose Quartz: Though most Rose Quartz is cloudy, transparent specimens are occasionally found. These pieces are often considered more valuable due to their rarity.
  • Milky Rose Quartz: A more opaque variety of Rose Quartz with a softer, milky appearance, which results from a higher density of internal fractures and inclusions.

Synthetic and Imitation Rose Quartz

As demand for gemstones increases, synthetic quartz, including Rose Quartz, is produced in laboratories for industrial use. These synthetic versions are chemically identical to natural quartz but are often purer and free of the inclusions that give natural Rose Quartz its cloudy or milky appearance.

Imitation Rose Quartz is also found in the market, typically made from dyed glass or other artificial materials designed to mimic the appearance of the natural gemstone. Buyers should be aware of these imitations, particularly when purchasing jewelry or high-quality decorative items.

Conclusion: Rose Quartz in Geology and Beyond

Rose Quartz is much more than just a beautiful pink stone; it is a geological marvel with a rich history and a wide range of applications. Its formation process, driven by the presence of trace elements and unique geological conditions, makes it a fascinating subject for geologists and gemologists alike. Whether adorning jewelry, decorating spaces, or serving practical roles in construction and technology, Rose Quartz continues to captivate for both its beauty and its versatility.

As science continues to explore the depths of Earth’s geological formations, Rose Quartz remains a symbol of the complexity and beauty found in nature.


FAQs: Frequently Asked Questions About Rose Quartz

What gives Rose Quartz its pink color?

The pink color of Rose Quartz is typically caused by trace amounts of titanium, iron, or manganese within the mineral’s structure. Recent studies suggest that inclusions of microscopic fibrous minerals like dumortierite may also play a role.

Where is Rose Quartz commonly found?

Rose Quartz is commonly found in pegmatite deposits across Brazil, Madagascar, the USA (South Dakota), India, and South Africa.

How is Rose Quartz used in industry?

Apart from its use in jewelry, Rose Quartz is used in the construction industry for concrete and road materials. Quartz is also vital in electronics due to its piezoelectric properties.

What is Star Rose Quartz?

Star Rose Quartz is a rare variety of Rose Quartz that exhibits asterism, a star-like effect on the surface of the stone caused by mineral inclusions reflecting light.

Can Rose Quartz form in crystal points?

While most Rose Quartz forms in massive shapes, it rarely forms in crystal points, making those rare specimens highly prized by collectors.

Is there synthetic Rose Quartz?

Yes, synthetic Rose Quartz is produced in laboratories for industrial applications. These synthetics are chemically identical to natural quartz but often have fewer inclusions.

Rhodium: The Most Expensive Metal

Rhodium: The Most Expensive Metal
Rhodium: The Most Expensive Metal

Table of Contents

Introduction to Precious Metals

Precious metals have been a cornerstone of human civilization for thousands of years. From ancient times to the present day, they have been used as currency, in the creation of jewelry, and for various industrial applications. But beyond their beauty and history, certain metals stand out for their immense value. Today, the conversation around precious metals extends beyond gold and silver to include lesser-known but significantly more expensive metals like rhodium and palladium.

What Are Precious Metals?

Precious metals are rare, naturally occurring metallic chemical elements of high economic value. Historically, gold and silver have been the most prominent, but metals like platinum, palladium, and rhodium have become increasingly valuable due to their rarity and industrial applications. These metals are often called “noble metals” because of their resistance to corrosion and oxidation, which increases their longevity and appeal.

The Role of Metals in Industry, Jewelry, and Technology

While precious metals are widely known for their use in luxury goods like jewelry, their role in modern industry is even more critical. Metals like rhodium and palladium are indispensable in the automotive industry, where they are used in catalytic converters to reduce vehicle emissions. Platinum and gold are heavily used in electronics and medical equipment, where their excellent conductivity and non-reactive properties are essential.

What Determines the Value of a Metal?

The value of metals is determined by a range of factors, including their rarity, demand, and the costs associated with extracting and refining them. The global supply of a metal and its applications across industries also play significant roles in setting its price. Understanding these factors can provide insight into why certain metals command higher prices than others.

Rarity and Availability

Rhodium, for example, is an extremely rare metal, with its annual global production barely exceeding a few tons. This rarity drives up its price significantly. Mining conditions and geopolitical factors also impact availability. Many of the world’s precious metals are mined in politically unstable regions, which can disrupt supply chains and cause prices to fluctuate.

Industrial Demand

The demand for metals in industries such as automotive manufacturing, electronics, and healthcare plays a crucial role in their market value. For instance, the use of palladium in catalytic converters for cars has surged due to stricter emission regulations, leading to a sharp increase in its price. Rhodium’s value similarly hinges on its crucial role in the auto industry.

Applications in Technology and Jewelry

Jewelry remains a significant driver of demand for metals like gold and platinum. However, the tech industry’s need for these metals, particularly for use in electronic components, is growing rapidly. Gold, known for its conductivity and resistance to corrosion, is widely used in computer processors and other electronics, adding to its demand beyond aesthetic purposes.

Overview of the World’s Most Expensive Metals

Many people are familiar with gold and platinum as valuable metals, but few know about the much higher prices of rhodium or palladium. Let’s compare some of the most expensive metals and understand what sets them apart from the rest.

A Comparison of Gold, Platinum, Rhodium, and Others

  • Gold: Always a classic, gold has been used as a store of value for centuries. Its price has historically been a barometer of economic health and is often considered a safe-haven asset during times of economic instability.
  • Platinum: With its stunning white luster and rarity, platinum has long been more expensive than gold, though it is also heavily used in industrial applications, particularly in catalytic converters.
  • Rhodium: The reigning champion in terms of price, rhodium is primarily used in the automotive industry, with very little availability from mining operations, making it the world’s most expensive metal today.
  • Palladium: This lesser-known metal has seen its value skyrocket due to its use in catalytic converters. Its price has risen faster than gold in recent years due to supply shortages and increased demand.

How Prices Are Determined and Tracked

The prices of these metals are determined by several factors, including supply and demand dynamics, geopolitical stability, mining output, and industrial usage. Commodities exchanges like the London Metal Exchange (LME) and New York Mercantile Exchange (NYMEX) track prices and facilitate the trading of metals, allowing investors to buy and sell these commodities in real-time.

The Rise of Rhodium: The Most Expensive Metal

Rhodium’s Journey to the Top

Rhodium, a member of the platinum group metals, has been a critical player in the automotive industry due to its effectiveness in reducing harmful emissions. In the 21st century, environmental regulations across the world have tightened, increasing demand for rhodium in catalytic converters. This surge in demand, combined with the metal’s rarity, has sent its price skyrocketing, surpassing that of both gold and platinum.

Why Rhodium Is So Valuable

The extreme rarity of rhodium is a primary factor in its high price. With only about 30 tons mined globally each year, rhodium is much scarcer than other precious metals like gold and silver. Its industrial utility in emission control systems for vehicles makes it indispensable, especially as global regulations continue to push for greener technologies.

Industrial and Commercial Applications of Rhodium

Rhodium’s primary application is in the automotive industry, where it is used in catalytic converters to reduce nitrogen oxide emissions from vehicles. It is also used in the production of glass and as an alloying agent in platinum and palladium to improve their corrosion resistance. Rhodium is highly reflective and resists tarnishing, which is why it is often used to plate jewelry, giving white gold its bright finish.

Rhodium’s Price Surge: A Historical Perspective

The Price Fluctuations of Rhodium Over Time

Rhodium prices have been historically volatile. After reaching record highs in the 2000s, its price crashed during the 2008 financial crisis, only to surge again in the 2020s as environmental regulations in Europe and China increased demand. Prices can rise or fall by thousands of dollars per ounce within short periods, reflecting its sensitivity to shifts in supply and demand.

The Supply and Demand Impact on Its Value

Rhodium’s price is driven largely by the supply from a small number of mines in South Africa, which produce around 80% of the global supply. Any disruption to these mines, whether due to labor strikes or geopolitical issues, can severely impact the global supply, leading to price spikes. Demand, on the other hand, is linked to the automotive industry’s need for emission-reducing technology.

Other Highly Valuable Metals

While rhodium takes the top spot, several other metals are close contenders in terms of price and rarity.

Platinum: A Close Contender

Platinum is another member of the platinum group metals (PGMs), known for its use in both jewelry and industry. While historically more expensive than gold, platinum’s price has fluctuated in recent years due to varying demand from the automotive and jewelry sectors. Platinum remains a key component in fuel cells and catalytic converters, ensuring its continued value.

Palladium: The Underrated Heavyweight

Palladium has recently surged in price, outperforming gold due to its critical role in catalytic converters for gasoline engines. The metal has become increasingly scarce as mining output struggles to meet the high demand, particularly as automakers pivot toward producing cleaner vehicles.

Gold: The Timeless Benchmark

While gold may not be the most expensive metal, it remains a benchmark for wealth and stability. Its cultural significance, combined with its use in electronics, jewelry, and finance, ensures that gold continues to hold immense value across the globe.

Industrial Applications of Expensive Metals

The utility of precious and expensive metals extends far beyond jewelry and coinage. Their unique physical and chemical properties make them indispensable in several industrial sectors. As technology advances, the demand for these metals in industries such as automotive, electronics, and aerospace has grown significantly.

How These Metals Are Used in Automotive, Electronics, and Aerospace Industries

  • Automotive Industry: The primary use of metals like rhodium, palladium, and platinum is in catalytic converters, which help reduce harmful emissions from internal combustion engines. These metals act as catalysts to convert toxic gases, such as nitrogen oxides, carbon monoxide, and hydrocarbons, into less harmful substances like carbon dioxide and water vapor. As global regulations on vehicle emissions have tightened, demand for these metals has surged, driving up their prices.
  • Electronics: Gold, platinum, and palladium are extensively used in the electronics industry due to their excellent conductivity and resistance to corrosion. Gold is commonly used in circuit boards, connectors, and memory chips, ensuring reliability and longevity in devices. Palladium’s ability to absorb hydrogen makes it useful in fuel cell technology, which is being explored as a potential energy source for the future.
  • Aerospace Industry: In the aerospace sector, where materials must withstand extreme temperatures and stress, platinum group metals (PGMs) play a crucial role. These metals are used in high-performance turbine engines and fuel cells. Their resistance to high temperatures and corrosion ensures that aerospace components function reliably over long periods, even in the harshest conditions.

Rhodium in Catalytic Converters

The Role of Rhodium in Emission Control

Rhodium is irreplaceable in the fight against air pollution due to its effectiveness in reducing nitrogen oxide (NOx) emissions, which are some of the most harmful pollutants from vehicle exhaust. NOx gases contribute to the formation of smog and acid rain, posing serious environmental and health risks. Rhodium, when used in catalytic converters, helps convert NOx into nitrogen and oxygen, which are harmless to the atmosphere.

Why the Auto Industry Drives Rhodium Demand

The automotive sector is the primary driver of rhodium demand, with over 80% of the global supply being used in catalytic converters. As governments around the world implement stricter environmental regulations, such as the Euro 6 standard in Europe and tighter fuel efficiency standards in the U.S. and China, automakers are increasingly reliant on rhodium to meet these requirements. This demand, combined with the metal’s rarity, has made rhodium the most expensive metal on the planet.

Rhodium in Jewelry and Investment

While rhodium’s primary use is industrial, it has also found a niche in the luxury goods market, particularly in jewelry.

Rhodium Plating and Its Role in Fine Jewelry

Rhodium is often used to plate white gold, giving it a bright, reflective finish and making the metal more durable and resistant to tarnishing. This practice is particularly common in engagement rings and other fine jewelry, where the rhodium layer enhances the appearance of the underlying gold or platinum. Despite its thin application, the rhodium plating is highly valued for its visual appeal and the prestige associated with the metal.

Investment Trends for Rhodium

Rhodium is also attracting attention from investors due to its extraordinary price increases in recent years. Unlike gold, silver, or platinum, rhodium has a smaller, more specialized market, which makes it both an attractive but highly volatile investment. Rhodium’s price can be influenced by shifts in industrial demand, geopolitical issues affecting supply, or changes in environmental regulations.

However, the rhodium market is not as liquid as gold or silver, meaning that buying and selling can be more challenging. Investors who choose rhodium should be aware of its price volatility and the potential for dramatic swings in value.

Environmental and Ethical Concerns

The Environmental Impact of Mining Expensive Metals

Mining for precious metals, especially rare ones like rhodium, platinum, and palladium, has significant environmental consequences. The extraction of these metals often involves deep mining operations that can lead to deforestation, water pollution, and habitat destruction. Mining for platinum group metals (PGMs) in South Africa, where most of the world’s supply is sourced, has raised concerns about land degradation and the health impacts on local communities.

Additionally, refining these metals is an energy-intensive process that contributes to greenhouse gas emissions. The environmental toll of mining and refining must be considered alongside the industrial benefits these metals provide.

Ethical Issues in Sourcing and Trading

Ethical concerns also arise in the sourcing of expensive metals, particularly when mining occurs in politically unstable regions. “Conflict minerals” is a term used to describe metals that are mined in conditions where profits from the trade support armed conflict or human rights abuses. While platinum and palladium are less frequently associated with conflict minerals compared to others like coltan or tungsten, the mining of these metals can still involve poor working conditions, child labor, and exploitation.

Consumers and investors are increasingly demanding that the metals they purchase be sourced ethically, prompting industries to adopt certification schemes and more transparent supply chains.

The Future of Metal Prices

Trends in Precious Metal Prices

The prices of precious metals are notoriously difficult to predict, but some trends are emerging based on shifts in technology, industry, and environmental policy. Metals like rhodium and palladium, which are essential for reducing vehicle emissions, are expected to remain in high demand as the world moves toward cleaner energy solutions.

  • Rhodium: Given the ongoing global efforts to reduce carbon emissions and air pollution, demand for rhodium in catalytic converters is likely to stay high, especially with the growing automotive markets in Asia.
  • Palladium: As a key metal in catalytic converters for gasoline engines, palladium’s price trajectory is closely linked to the global automotive industry. While electric vehicles (EVs) are on the rise, internal combustion engines still dominate the market, ensuring that palladium will remain valuable in the near future.
  • Platinum: Platinum’s price, long trailing behind rhodium and palladium, may see a resurgence due to its potential role in hydrogen fuel cell technology, which could be critical in the future of renewable energy.

Predictions for Rhodium and Other Expensive Metals

Experts predict that rhodium’s price will continue to fluctuate based on market demand and supply challenges. As more countries adopt stringent environmental regulations, the need for rhodium in catalytic converters could grow. However, advancements in electric vehicle technology, which doesn’t rely on catalytic converters, could dampen demand for rhodium over time, leading to price corrections.

Investing in Expensive Metals: Risks and Rewards

Why Investors Are Drawn to Expensive Metals

Precious and rare metals offer a unique investment opportunity due to their intrinsic value and use across industries. Metals like gold and platinum have long been considered safe-haven assets during times of economic uncertainty, while others, like rhodium, offer the potential for significant returns due to their rarity and industrial demand. Investors are drawn to these metals not just for their monetary value but for their tangibility and ability to retain worth even in volatile markets.

The Volatility of Metal Markets

The metal markets are notoriously volatile, and investing in expensive metals comes with risks. Rhodium, for instance, has experienced massive price swings in the past, sometimes doubling or halving in value over the course of a single year. This volatility is driven by supply chain disruptions, shifts in industrial demand, and global economic conditions. Investors must be prepared for the unpredictable nature of these markets and should diversify their portfolios to mitigate risks.

How to Buy and Store Precious Metals

Popular Platforms for Purchasing Metals

Investors looking to purchase expensive metals can do so through several platforms:

  • Commodities Markets: Precious metals like gold, silver, platinum, and rhodium can be traded on commodities exchanges such as the London Metal Exchange (LME) or New York Mercantile Exchange (NYMEX). These platforms allow for futures trading, which enables investors to speculate on the future price of metals.
  • Bullion Dealers: Many investors prefer to buy physical metals in the form of bullion or coins. Trusted bullion dealers, such as JM Bullion or APMEX, offer gold, silver, platinum, and rhodium bars and coins. Physical ownership can provide a sense of security, though it requires safe storage.

Secure Storage Solutions

Storing precious metals requires careful consideration. Physical metals should be stored in a secure location, such as a bank safety deposit box or a home safe. Some investors also use third-party vaulting services, which offer high-security storage and insurance for a fee. For those who trade in large quantities, professional storage options like the vaults provided by the Royal Canadian Mint or Brinks are essential.

The Role of Metals in Global Economies

How Expensive Metals Influence Global Markets

Precious metals are not just commodities; they are strategic assets that influence global markets. Central banks around the world hold large reserves of gold as part of their monetary policy, using it as a hedge against inflation and currency devaluation. Similarly, the supply and demand for metals like rhodium and palladium can affect national economies, especially in countries that rely on mining as a major part of their GDP.

For example, South Africa’s economy is closely tied to the mining of platinum group metals (PGMs), including rhodium and palladium. Disruptions in the mining industry due to strikes or political instability can ripple through the global supply chain, affecting prices and availability.

The Strategic Importance of Precious Metals

Beyond their economic value, precious metals play a strategic role in national security and technological innovation. Metals like platinum and palladium are used in military and aerospace applications, while others, like rhodium, are critical for maintaining environmental standards. As global industries evolve and the demand for cleaner technologies grows, the strategic importance of these metals will only increase.

Conclusion: Why Expensive Metals Will Always Fascinate Us

The allure of expensive metals is undeniable. From their role in shaping civilizations to their modern applications in technology and industry, these metals captivate us with their rarity, beauty, and utility. Rhodium, with its staggering price tag, highlights how essential these metals are in today’s world, particularly as we strive for a cleaner, more sustainable future. As technology evolves, the demand for precious metals will continue to grow, ensuring their place as valuable commodities in the global economy.

While investing in these metals comes with risks, their appeal as both luxury items and strategic assets will always attract those who seek to own a piece of the world’s most prized elements.


FAQs: Frequently Asked Questions About Expensive Metals

Why is rhodium more expensive than gold?

Rhodium is much rarer than gold and has specific industrial applications, particularly in catalytic converters for cars. Its limited supply and high demand from the automotive sector have driven its price above that of gold.

Can rhodium prices fall?

Yes, rhodium prices are highly volatile and can experience significant fluctuations due to changes in demand, supply disruptions, or shifts in environmental regulations affecting the automotive industry.

What is palladium used for?

Palladium is primarily used in catalytic converters for gasoline engines, helping reduce harmful emissions. It is also used in electronics, dentistry, and as a component in fuel cells.

Is investing in metals risky?

Investing in metals can be risky due to price volatility, supply chain disruptions, and changing industrial demand. However, many investors consider metals a hedge against inflation and currency devaluation.

What is the rarest metal on Earth?

The rarest metal on Earth is likely rhodium, given its extremely limited supply and high demand in industrial applications. Other rare metals include platinum group metals (PGMs) like palladium and osmium.

Why are some metals so expensive?

The price of metals is driven by a combination of factors, including rarity, difficulty in mining and refining, industrial demand, and geopolitical influences. Metals like rhodium and palladium are expensive because they are both rare and essential to key industries like automotive manufacturing.

Fukang Meteorite: The Most Expensive Meteorite

Fukang Meteorite
Fukang Meteorite

Table of Contents

Introduction to Meteorites

Meteorites, fragments of celestial bodies that survive their journey through Earth’s atmosphere and land on the planet, offer a unique glimpse into the cosmos. These extraterrestrial rocks often date back to the formation of the solar system, making them invaluable to both scientists and collectors. But what exactly are meteorites, and what makes them so valuable? To appreciate the most expensive meteorite in history, one must first understand the basics of these fascinating space travelers.

What Are Meteorites?

Meteorites are solid pieces of debris from objects such as comets, asteroids, or meteoroids that originate in outer space and survive their passage through the atmosphere to reach Earth’s surface. When these objects enter Earth’s atmosphere, they become meteors or “shooting stars,” but only a fraction of them make it through the atmosphere to land on Earth.

Types of Meteorites: Stony, Iron, and Stony-Iron

Meteorites fall into three primary categories based on their composition:

  1. Stony Meteorites – Composed mainly of silicate minerals, these are the most common type.
  2. Iron Meteorites – Comprising mostly metallic iron and nickel, they are denser and much rarer.
  3. Stony-Iron Meteorites – A mix of silicate minerals and metal, these are the rarest and most valuable, both scientifically and financially.

Understanding the classification of meteorites is essential to grasp why certain types are prized by collectors and scientists alike.

The Meteorite Market: Understanding the Value

While meteorites are scientifically priceless, they also carry significant monetary value. The price of a meteorite can vary dramatically, depending on several factors that collectors and dealers consider when determining its worth.

What Determines the Value of a Meteorite?

Several factors influence the market value of a meteorite:

  • Rarity – The rarer a meteorite, the more valuable it is. Stony-iron meteorites, for instance, are highly sought after due to their scarcity.
  • Size – Larger meteorites typically command higher prices due to their rarity and the logistical challenges of finding and recovering them.
  • Composition – Meteorites rich in metals like nickel and iron are often more valuable due to their durability and visual appeal.
  • Provenance – Meteorites with a documented history, especially those tied to significant scientific discoveries, are valued higher.

Rarity, Size, and Composition

Among all these factors, rarity plays the most crucial role in determining a meteorite’s price. A meteorite that is either unique in its composition or comes from an event with historical significance can fetch millions of dollars at auctions.

Notable Meteorite Sales in History

The meteorite market has seen some astonishing sales over the past few decades, with collectors and institutions vying for a piece of cosmic history. While most meteorites are sold for tens of thousands of dollars, a few have broken the million-dollar mark.

Famous Meteorite Auctions

Some of the most famous meteorites have fetched prices that rival fine art. In 2012, an auction held by Christie’s showcased meteorites as collectibles, with the most expensive item, a part of the Gibeon meteorite, selling for nearly $100,000.

Record-breaking Meteorites: A Detailed Look

One meteorite sale stands out above the rest — the sale of the Fukang meteorite, a stunning pallasite with translucent olivine crystals embedded in its iron-nickel matrix. The value and beauty of this meteorite shattered auction records, solidifying its place as the most expensive meteorite ever sold.

The Most Expensive Meteorite Ever Sold

The Sale of the Fukang Meteorite

The Fukang meteorite is a pallasite meteorite discovered in the mountains near Fukang, China, in 2000. With an estimated weight of around 1,003 kilograms, it is one of the most beautiful and scientifically significant meteorites ever found. In a 2008 auction, part of the Fukang meteorite was priced at an astronomical $2 million.

Price and Ownership

While the entire meteorite has not been sold as a single unit, fragments of the Fukang meteorite have been sold for as much as $1,000 per gram, placing the total value of the meteorite well into the millions.

What Makes Fukang Special?

The Fukang meteorite is particularly prized for its beauty and its rarity. Pallasites, which make up less than 1% of all known meteorites, contain large crystals of the mineral olivine embedded in an iron-nickel matrix. When polished, the olivine crystals become translucent, creating a striking appearance that resembles a stained-glass window. The aesthetic appeal, combined with its rarity, makes the Fukang meteorite a coveted piece among collectors.

Rarity and Uniqueness of the Fukang Meteorite

Origins and Discovery of the Fukang Meteorite

The Fukang meteorite was discovered by a hiker in the Gobi Desert, near Fukang, China, in 2000. This initial discovery led to further excavations, revealing a massive specimen weighing over a ton. Its origins trace back billions of years, offering scientists insights into the early solar system.

Its Size, Weight, and Composition

Weighing over 1,003 kilograms, the Fukang meteorite is enormous compared to most meteorites found on Earth. Its stunning olivine crystals are set within a metallic structure, making it both scientifically significant and aesthetically beautiful.

Other High-Value Meteorites in the World

While the Fukang meteorite holds the crown for the most expensive, other high-value meteorites have also made headlines for their unique characteristics and auction prices.

The Gibeon Meteorite

Discovered in Namibia in the 19th century, the Gibeon meteorite is an iron meteorite that fragmented over a vast area. Known for its beautiful Widmanstätten patterns, it has fetched high prices at auctions.

The Brenham Meteorite

The Brenham meteorite, a pallasite found in Kansas, USA, in 1882, is another example of a high-value meteorite due to its rarity and the beauty of its olivine crystals.

The Willamette Meteorite

The largest meteorite ever found in the United States, the Willamette meteorite weighs over 15 tons. Though not for sale, its cultural significance has made it a priceless artifact.

What Makes Meteorites So Valuable?

Scientific Importance of Meteorites

Meteorites serve as windows into the early solar system, offering clues about the formation of planets and the presence of water and organic compounds. For researchers, owning a piece of this cosmic history is invaluable for advancing scientific knowledge.

The Appeal to Private Collectors

For private collectors, meteorites represent not only a piece of history but also a unique work of art. Their rarity and beauty make them attractive to wealthy individuals looking for unique investments or showpieces.

Legal and Ethical Considerations in Meteorite Sales

Ownership Rights and Legal Frameworks

The sale and ownership of meteorites fall into a complex legal framework that varies significantly across different countries. In the United States, private ownership of meteorites found on privately owned land is allowed, provided permission from the landowner is granted. However, some countries, like Argentina and Australia, have strict regulations prohibiting the sale of meteorites, classifying them as national treasures. The United Nations’ Outer Space Treaty also influences the legal status of extraterrestrial objects, ensuring that no country can claim ownership of celestial bodies, but does not explicitly cover meteorites.

Collectors and dealers must navigate these legal frameworks, especially when purchasing meteorites from foreign countries or indigenous lands. Meteorites found on public land in many countries, including the U.S., may belong to the government, making unauthorized sales illegal. International treaties, national laws, and ethical concerns all intersect to create a sometimes murky marketplace for these cosmic treasures.

Ethical Issues in the Meteorite Trade

Beyond the legal issues, ethical concerns also arise when dealing with meteorites. For example, some meteorites are discovered on culturally or historically significant land, such as the Willamette Meteorite, found on land sacred to Native American tribes. Selling such artifacts can lead to tensions between collectors and indigenous communities.

Another issue is the growing practice of “meteorite hunting,” where individuals or corporations comb remote areas, particularly deserts, for meteorites to sell on the open market. While this may sound harmless, overzealous hunting can disrupt local ecosystems, and the commercialization of such activities raises concerns about the loss of scientifically valuable materials to private ownership.

The Role of Meteorites in Science and Research

Contributions to Space Science

Meteorites are more than just collectibles or symbols of wealth; they play a crucial role in advancing our understanding of the universe. These space rocks are the remnants of the early solar system, offering valuable clues about its formation, evolution, and the processes that shaped planets and moons. Many meteorites contain high concentrations of metal, rare isotopes, or even organic compounds like amino acids, which are the building blocks of life.

For instance, the Murchison meteorite, which fell in Australia in 1969, contains over 90 amino acids, many of which are not found on Earth. This discovery spurred significant research into the possibility that meteorites brought the necessary ingredients for life to Earth, supporting theories about panspermia.

Meteorites as Windows into the Early Solar System

Meteorites often contain chondrules, tiny, round grains that formed in the early solar nebula. Studying these chondrules helps scientists understand conditions that existed over 4.5 billion years ago, long before planets like Earth formed. Iron meteorites, which come from the cores of ancient, shattered asteroids, offer insight into the processes of planetary differentiation, where molten planets separated into layers of core, mantle, and crust.

In essence, meteorites act as time capsules, providing scientists with direct samples of celestial bodies and the material that formed our solar system.

Meteorites in Art and Culture

Artistic and Cultural Significance

Throughout history, meteorites have captured the human imagination, inspiring myths, legends, and artistic creations. Many ancient cultures viewed meteorites as gifts from the gods. In Egypt, meteoritic iron was used in the creation of ceremonial objects, such as King Tutankhamun’s famous iron dagger, which was crafted from iron believed to have come from a meteorite.

In modern times, artists have incorporated meteorites into their work, attracted by their otherworldly origins and striking appearances. Sculptors have used iron meteorites for both their physical beauty and their symbolic connection to space and time. Jewelry designers have also embraced meteorites, crafting rings, necklaces, and other accessories from pieces of cosmic debris.

Meteorites as Symbols of Power and Mystery

Meteorites have often been seen as symbols of power, mystery, and transcendence. Their origins in outer space make them inherently exotic, and their rarity only adds to their allure. Some collectors view owning a meteorite as a way to possess a piece of the universe, something that connects them directly to the cosmos.

The Future of the Meteorite Market

Trends in Meteorite Pricing

Meteorite prices have been steadily rising over the past few decades, driven by increased demand from collectors, institutions, and investors. As meteorites become more scarce and their scientific importance becomes better understood, their value is expected to continue climbing. Rare types, such as lunar and Martian meteorites, command especially high prices due to their rarity and the difficulty of obtaining samples from these celestial bodies.

Additionally, as space exploration continues to advance, more meteorites may be brought back from other planets and moons. These space-exploration-driven meteorites could lead to new market dynamics, though natural meteorites will always hold a special place due to their historical significance.

Predictions for Future Meteorite Sales

Experts predict that the meteorite market will continue to grow, especially as more people become interested in space and astronomy. High-profile auctions, like those held by Christie’s or Bonhams, bring attention to the investment potential of meteorites, encouraging more individuals to enter the market. However, with this growth comes the risk of market volatility. Like any collectible, the value of meteorites is subject to fluctuations based on demand, rarity, and global economic conditions.

Investing in Meteorites: Risks and Rewards

Understanding Market Volatility

Investing in meteorites can be lucrative, but it comes with its own set of risks. The value of a meteorite can vary greatly depending on market trends, scientific discoveries, and even public interest in space exploration. While some investors have made substantial profits, others have seen the value of their collections drop as new discoveries or market shifts impact demand.

Pros and Cons of Meteorite Investment

Investing in meteorites offers unique advantages, such as the potential for high returns and the thrill of owning a piece of cosmic history. However, it also comes with significant challenges, including the need for specialized knowledge to identify, authenticate, and properly care for meteorites. Fraud is a concern in the meteorite market, as fakes can be difficult for the untrained eye to spot.

How to Identify and Authenticate Meteorites

Common Techniques for Meteorite Identification

Identifying a genuine meteorite requires a keen understanding of its physical characteristics, including its weight, magnetic properties, and fusion crust (the outer layer formed as the meteorite burns through the atmosphere). Many meteorites also display a metallic luster or have a distinct Widmanstätten pattern, a crisscrossed design found in iron meteorites that forms over millions of years as the iron cools.

Experts often use more advanced techniques, such as isotopic analysis or scanning electron microscopy, to confirm a meteorite’s authenticity. These methods help determine the meteorite’s chemical composition, providing definitive proof of its extraterrestrial origin.

How to Avoid Fraud in Meteorite Purchases

With the rising value of meteorites, the market has seen a corresponding rise in forgeries. Unscrupulous sellers may attempt to pass off Earth rocks as meteorites or sell fragments of genuine meteorites at inflated prices. To avoid fraud, buyers should only purchase meteorites from reputable dealers or auctions and, if possible, obtain a certificate of authenticity from a qualified meteorite expert.

Where to Buy and Sell Meteorites

Popular Auction Houses and Online Platforms

For those looking to buy or sell meteorites, several reputable auction houses and online platforms specialize in meteorite transactions. Christie’s and Bonhams regularly feature meteorites in their natural history auctions, while online platforms like Heritage Auctions and specialized dealers such as Aerolite Meteorites offer a wide selection of meteorites for sale.

A Guide to Meteorite Dealers

It’s essential to work with experienced meteorite dealers who have a deep understanding of the market and offer guarantees of authenticity. Many dealers are also members of professional organizations like the International Meteorite Collectors Association (IMCA), which ensures a level of credibility and expertise in the field.

Conclusion: Why Meteorites Continue to Fascinate

Meteorites hold a unique position at the intersection of science, art, and investment. Their ability to unlock the secrets of the universe makes them scientifically priceless, while their rarity and beauty give them significant financial value. For private collectors, owning a meteorite is more than just an investment—it’s an opportunity to connect with the cosmos in a tangible way. As the world continues to look toward the stars, meteorites will undoubtedly remain a symbol of our enduring fascination with space and our place within it.


FAQs: Frequently Asked Questions About Meteorites

What is the rarest type of meteorite?

The rarest type of meteorite is the stony-iron pallasite, which makes up less than 1% of all known meteorites. Pallasites contain olivine crystals set in a nickel-iron matrix, making them highly prized for their beauty and rarity.

Can you legally own a meteorite?

Yes, in most countries, individuals can legally own meteorites, especially if they are found on private property. However, some countries have strict regulations, and it’s important to be aware of local laws before purchasing or collecting meteorites.

What is the largest meteorite ever found?

The largest meteorite ever found is the Hoba meteorite in Namibia, which weighs around 60 tons. It is so large that it has never been moved from its discovery site and remains a popular tourist attraction.

How are meteorites priced?

Meteorites are priced based on several factors, including their rarity, size, composition, and provenance. Rare types of meteorites, such as Martian or lunar samples, can fetch extremely high prices, while common stony meteorites are much less expensive.

Can meteorites be faked?

Yes, meteorites can be faked, and the market has seen an increase in fraudulent sales. Buyers should always work with reputable dealers and seek certificates of authenticity to ensure they are purchasing genuine meteorites.

Why are meteorites important for science?

Meteorites provide valuable insights into the formation of the solar system, planetary differentiation, and the presence of organic compounds in space. They are essential tools for researchers studying the history and composition of celestial bodies.

Mountain of God: The Weirdest Volcano in the World

 Ol Doinyo Lengai volcano spews extremely runny lava that turns bone white when it dries. (Image credit: Jean-Denis JOUBERT via Getty Images)
Ol Doinyo Lengai volcano spews extremely runny lava that turns bone white when it dries. (Image credit: Jean-Denis JOUBERT via Getty Images)

Introduction

Tucked away in the heart of Tanzania lies one of the most fascinating and unusual volcanoes on Earth—Ol Doinyo Lengai, often referred to as the “Mountain of God” by the local Maasai people. Unlike most volcanoes, this enigmatic mountain possesses characteristics that set it apart from the rest of the world’s volcanoes. Known for its rare carbonatite lava, which is cooler and flows faster than the usual silica-rich lava, Ol Doinyo Lengai offers a unique geological wonder that has baffled and intrigued scientists for decades.

In this article, we will explore what makes the Mountain of God so weird, from its unusual lava composition to its remarkable geological history. Let’s dive deep into the bizarre and awe-inspiring nature of this one-of-a-kind volcanic marvel.


Table of Contents

  1. Location and Cultural Significance
    • Geography of Ol Doinyo Lengai
    • The Maasai and the “Mountain of God”
  2. Unique Features of Ol Doinyo Lengai
    • Carbonatite Lava: The Key to Its Uniqueness
    • Cooling Temperatures and Fast Flowing Lava
  3. Eruptions and Activity
    • Recent Eruptions
    • The Lava Fountain Phenomenon
  4. Why Is Ol Doinyo Lengai Considered the Weirdest Volcano?
    • Uncommon Lava Composition
    • Unpredictable Eruptions
    • Formation of Unique Landscapes
  5. FAQ Section

1. Location and Cultural Significance

Geography of Ol Doinyo Lengai

Ol Doinyo Lengai is located in northern Tanzania, near the eastern branch of the East African Rift Valley. It sits about 120 kilometers northwest of Arusha and is relatively close to the iconic Serengeti and Ngorongoro Crater. Towering at about 2,962 meters (9,718 feet), this active volcano overlooks the stunning landscape of the surrounding region, including the Lake Natron basin, known for its extreme alkalinity and flamingo populations.

The Maasai and the “Mountain of God”

The local Maasai people have revered Ol Doinyo Lengai for centuries, referring to it as the “Mountain of God” due to its mystical presence and the raw power of its eruptions. The Maasai hold the belief that the volcano is a sacred place where their deity resides, and as such, the mountain has immense spiritual significance. The unpredictable eruptions, rare lava, and its towering presence in the East African landscape have only added to its mythic status in the region.


2. Unique Features of Ol Doinyo Lengai

Carbonatite Lava: The Key to Its Uniqueness

The most striking feature that makes Ol Doinyo Lengai stand out is its carbonatite lava. Unlike typical lava, which is rich in silicate minerals and is extremely hot (about 1,000°C or more), the lava that flows from this volcano is unusually cool, with temperatures between 500°C and 600°C. It is the only active volcano in the world known to produce natrocarbonatite lava, a rare type of lava that contains sodium and potassium carbonate minerals.

Cooling Temperatures and Fast Flowing Lava

Because of its relatively low temperatures, carbonatite lava is much more fluid than silicate lava. It moves quickly, often resembling flowing mud rather than the sluggish movement of typical lava flows. Its dark, blackish-brown appearance when it emerges soon turns white as it cools due to the rapid weathering of its unique chemical composition. This rapid transition is caused by its reaction with moisture and CO2 in the atmosphere, resulting in the formation of white sodium carbonate crusts.


3. Eruptions and Activity

Recent Eruptions

Ol Doinyo Lengai has had a long history of volcanic activity, with eruptions recorded as far back as 1883. While many of its eruptions have been relatively small, larger and more violent eruptions have occurred as well, the most notable being in 2007-2008, when it released an explosive amount of carbonatite lava, along with ash plumes that rose as high as 15 kilometers into the atmosphere.

Its eruptions often alternate between effusive eruptions—where lava flows smoothly out of the crater—and explosive eruptions, where ash and rock are ejected. However, these transitions are highly unpredictable, adding to its mystique and reputation as one of the weirdest volcanoes in the world.

The Lava Fountain Phenomenon

Another bizarre feature of the Mountain of God is its lava fountains. Unlike the usual fiery displays seen in silicate-based volcanoes, the lava fountains at Ol Doinyo Lengai are much less violent, spewing black carbonatite lava that cools rapidly into fragile, needle-like formations. These formations are so delicate that they can disintegrate into fine powder with just a light touch.


4. Why Is Ol Doinyo Lengai Considered the Weirdest Volcano?

Uncommon Lava Composition

What truly sets Ol Doinyo Lengai apart is its natrocarbonatite lava, a geological oddity not found in any other active volcano on Earth. This rare type of lava is rich in sodium and potassium carbonates, which is a stark contrast to the silicate-rich lava produced by most volcanoes. Its chemical composition also causes it to react unusually fast with the atmosphere, creating the striking white crust on the cooled lava.

Unpredictable Eruptions

Ol Doinyo Lengai’s unpredictability further fuels its reputation as one of the weirdest volcanoes. While most volcanoes have eruption patterns that can be studied and forecasted, Ol Doinyo Lengai remains somewhat enigmatic in its behavior. It alternates between calm lava flows and sudden explosive eruptions, often without warning.

Formation of Unique Landscapes

The interaction between the alkaline lava and the surrounding environment leads to the formation of striking landscapes. Over time, the carbonatite lava creates otherworldly volcanic cones, lava plateaus, and caverns. The rapid weathering of the lava also contributes to the fertility of the surrounding soil, making the region home to unique plant species that thrive in the area’s rich volcanic ash.


5. FAQ Section

1. Why is Ol Doinyo Lengai called the “Mountain of God”?

The name comes from the local Maasai people, who have long believed that the mountain is the dwelling place of their deity. It holds spiritual significance due to its awe-inspiring eruptions and towering presence over the Tanzanian landscape.

2. What makes carbonatite lava so unique?

Carbonatite lava is rich in sodium and potassium carbonates, unlike typical silicate lava. It is much cooler, flows faster, and reacts quickly with the atmosphere to form a white crust as it cools, a process that makes it visually striking and geologically rare.

3. How often does Ol Doinyo Lengai erupt?

Ol Doinyo Lengai erupts frequently, with minor eruptions occurring regularly. Larger, more explosive eruptions are less frequent but have been recorded throughout its history. Its most recent significant eruption was in 2007-2008.

4. Can you visit the Mountain of God?

Yes, adventurous travelers and geologists often visit the region, and it has become a popular site for hikers and volcano enthusiasts. However, the climb is challenging, and safety precautions must be taken, especially considering the volcano’s unpredictable nature.

5. Is Ol Doinyo Lengai dangerous?

While Ol Doinyo Lengai’s eruptions are typically less violent than other volcanoes, it can still pose a threat due to its unpredictable eruptions. The volcanic gases and ash plumes can also affect air quality and visibility in the surrounding areas.


Conclusion

Ol Doinyo Lengai, the “Mountain of God,” is a geological marvel unlike any other. Its carbonatite lava, unpredictable eruptions, and spiritual significance make it one of the most mysterious and fascinating volcanoes in the world. Whether viewed from a scientific perspective or revered for its cultural importance, Ol Doinyo Lengai remains a symbol of the Earth’s powerful and unpredictable forces. As the only active volcano producing natrocarbonatite lava, it holds a unique place in the world of volcanology and continues to captivate the imagination of all who encounter it.

The Differences Between Sedimentary, Igneous, and Metamorphic Rocks: A Comprehensive Guide

Representative image: Hand holding a rock
Representative image: Hand holding a rock

Introduction

The Earth’s crust is a dynamic system that has evolved over millions of years, giving rise to different types of rocks. These rocks—sedimentary, igneous, and metamorphic—form the foundation of Earth’s geology and hold clues to its past. Each rock type is defined by its formation process, composition, and texture, which are directly related to the environments in which they form.

Understanding the differences between these three rock types is essential for geologists, students, and anyone interested in the Earth sciences. This article delves deep into each type, explaining how they form, what distinguishes them, and their key characteristics. By the end of this guide, you’ll have a comprehensive understanding of sedimentary, igneous, and metamorphic rocks, and the role they play in shaping our planet.


Table of Contents

  1. What Are Sedimentary Rocks?
    • How Sedimentary Rocks Form
    • Types of Sedimentary Rocks
    • Characteristics of Sedimentary Rocks
    • Examples of Sedimentary Rocks
  2. What Are Igneous Rocks?
    • How Igneous Rocks Form
    • Types of Igneous Rocks
    • Characteristics of Igneous Rocks
    • Examples of Igneous Rocks
  3. What Are Metamorphic Rocks?
    • How Metamorphic Rocks Form
    • Types of Metamorphic Rocks
    • Characteristics of Metamorphic Rocks
    • Examples of Metamorphic Rocks
  4. Key Differences Between Sedimentary, Igneous, and Metamorphic Rocks
    • Formation Process Comparison
    • Textural Differences
    • Composition and Mineralogy
    • Distribution and Occurrence
    • Economic and Environmental Importance
  5. FAQ Section

1. What Are Sedimentary Rocks?

Sedimentary rocks are formed from the accumulation and cementation of mineral and organic particles, often referred to as sediments. These particles are typically transported by water, wind, or ice, and deposited in layers over time. This process of deposition is commonly associated with environments like rivers, lakes, and oceans, but it also occurs in deserts and other terrestrial landscapes.

How Sedimentary Rocks Form

The formation of sedimentary rocks involves a multi-step process:

  1. Weathering: Rocks at the Earth’s surface are broken down into smaller particles through processes like mechanical weathering (physical breaking apart) and chemical weathering (dissolution of minerals).
  2. Erosion and Transport: Once weathered, the particles are carried away by natural forces such as water, wind, and glaciers. These particles are often transported over long distances before being deposited.
  3. Deposition: Sediments are deposited in layers in bodies of water or on land. As more layers accumulate over time, the weight of the upper layers compresses the lower layers, compacting the material.
  4. Compaction and Cementation: With time, the buried sediments are compacted due to the weight of overlying layers. Minerals in groundwater precipitate and act as a cement, binding the particles together to form solid rock.

Types of Sedimentary Rocks

Sedimentary rocks can be classified into three main types:

  • Clastic Sedimentary Rocks: Formed from fragments of other rocks (clasts). Examples include sandstone, shale, and conglomerate.
  • Chemical Sedimentary Rocks: Formed by precipitation of minerals from water. Examples include limestone and evaporites like rock salt.
  • Organic Sedimentary Rocks: Composed of the remains of plants and animals. Examples include coal and certain forms of limestone formed from shells or coral.

Characteristics of Sedimentary Rocks

  • Layering: One of the most recognizable features is the presence of distinct layers, or strata, which result from the sequential deposition of sediments.
  • Fossils: Sedimentary rocks are the primary hosts of fossils, the preserved remains of ancient organisms, because the low-pressure environments where they form allow for fossilization.
  • Porosity: Sedimentary rocks often have high porosity due to the spaces between the particles, making them excellent reservoirs for water, oil, and gas.

Examples of Sedimentary Rocks

  • Sandstone: Composed primarily of sand-sized particles, often quartz.
  • Shale: Fine-grained rock made from silt and clay, often found in ancient marine environments.
  • Limestone: Formed from calcium carbonate, typically precipitated from water or from marine organisms’ remains.

2. What Are Igneous Rocks?

Igneous rocks form from the cooling and solidification of magma or lava. These rocks are the primary constituents of the Earth’s crust and represent the original form of solid rock on Earth. The word “igneous” comes from the Latin word for fire, reflecting their fiery origins deep within the Earth or at its surface through volcanic activity.

How Igneous Rocks Form

The process of igneous rock formation involves two major stages:

  1. Melting: The rock material deep within the Earth melts due to intense heat and pressure, forming magma. This can occur in the mantle or lower crust.
  2. Cooling and Solidification: Magma that reaches the Earth’s surface as lava cools and crystallizes to form extrusive igneous rocks. Magma that remains below the surface cools slowly and forms intrusive igneous rocks.

Types of Igneous Rocks

Igneous rocks are divided into two major categories:

  • Intrusive (Plutonic) Igneous Rocks: Formed when magma cools slowly beneath the Earth’s surface. The slow cooling allows large crystals to form. Examples include granite and diorite.
  • Extrusive (Volcanic) Igneous Rocks: Formed when magma erupts onto the surface as lava and cools rapidly. This quick cooling leads to smaller crystals. Examples include basalt, rhyolite, and andesite.

Characteristics of Igneous Rocks

  • Crystal Size: One of the key distinguishing features of igneous rocks is their crystal size. Intrusive igneous rocks have large, visible crystals, while extrusive rocks have small, fine-grained textures.
  • Mineral Composition: Igneous rocks are classified based on their mineral content. For example, rocks rich in silica are called felsic, while rocks with less silica and more iron and magnesium are termed mafic.
  • Texture: Igneous rocks can exhibit a range of textures, from glassy (such as obsidian) to porphyritic (where larger crystals are embedded in a finer-grained matrix).

Examples of Igneous Rocks

  • Granite: A coarse-grained intrusive rock, commonly used in construction.
  • Basalt: A fine-grained extrusive rock that makes up much of the ocean floor.
  • Obsidian: A naturally occurring volcanic glass, known for its smooth, glassy texture.

3. What Are Metamorphic Rocks?

Metamorphic rocks are formed from the transformation of existing rock types (whether igneous, sedimentary, or other metamorphic rocks) through high heat, pressure, and chemical processes. This transformation occurs without the rock melting; instead, it changes its mineral composition and texture in response to its new environmental conditions.

How Metamorphic Rocks Form

Metamorphism occurs in two primary settings:

  1. Regional Metamorphism: Occurs over large areas due to tectonic forces. This is typical in mountain-building regions where rocks are buried deep underground and subjected to intense pressure and heat.
  2. Contact Metamorphism: Occurs when rocks are heated by nearby magma or lava, leading to changes in the mineral structure of the rock.

Types of Metamorphic Rocks

Metamorphic rocks are broadly categorized into two types:

  • Foliated Metamorphic Rocks: These rocks have a layered or banded appearance due to the re-alignment of minerals under pressure. Examples include schist and gneiss.
  • Non-foliated Metamorphic Rocks: These rocks do not have a layered texture. Examples include marble and quartzite.

Characteristics of Metamorphic Rocks

  • Foliation: The development of a banded texture due to the alignment of minerals, which is common in rocks like schist and gneiss.
  • Recrystallization: The minerals within the rock may grow and change in response to heat and pressure without the rock melting.
  • Hardness and Density: Metamorphic rocks are generally harder and more dense than their original forms due to the intense conditions they endure.

Examples of Metamorphic Rocks

  • Marble: Formed from limestone under high pressure and temperature, marble is prized for its use in sculptures and building materials.
  • Slate: A fine-grained rock that originates from shale and is commonly used in roofing and flooring.
  • Schist: Known for its foliated texture, schist contains visible grains of mica and other minerals.

4. Key Differences Between Sedimentary, Igneous, and Metamorphic Rocks

While each type of rock forms under different conditions, they are interconnected through the rock cycle—the continuous process of transformation from one type of rock to another. Here’s a detailed comparison of the major differences:

1. Formation Process Comparison

  • Sedimentary Rocks: Formed from the accumulation and cementation of sediments.
  • Igneous Rocks: Formed from the cooling and solidification of molten rock (magma or lava).
  • Metamorphic Rocks: Formed from the transformation of existing rocks under heat and pressure.

2. Textural Differences

  • Sedimentary Rocks: Typically display layering and may have fossils.
  • Igneous Rocks: Characterized by crystal size—large in intrusive rocks, small or glassy in extrusive rocks.
  • Metamorphic Rocks: Often foliated (banded) but can also be non-foliated.

3. Composition and Mineralogy

  • Sedimentary Rocks: Composed of particles like sand, silt, clay, or organic material.
  • Igneous Rocks: Contain minerals like quartz, feldspar, and mica, with varying silica content.
  • Metamorphic Rocks: Contain re-crystallized minerals, often with banding or foliation.

4. Distribution and Occurrence

  • Sedimentary Rocks: Found in layers near the Earth’s surface, covering about 75% of the Earth’s continental surface.
  • Igneous Rocks: Make up the bulk of the Earth’s crust, especially beneath the ocean floors.
  • Metamorphic Rocks: Commonly found in regions of tectonic activity, like mountain ranges.

5. Economic and Environmental Importance

  • Sedimentary Rocks: Serve as reservoirs for fossil fuels like oil, gas, and coal.
  • Igneous Rocks: Provide valuable minerals and metals, such as granite for construction.
  • Metamorphic Rocks: Used in building materials (marble, slate) and as indicators of geological processes.

5. FAQ Section

1. Can one rock type transform into another?

Yes, through the rock cycle. Sedimentary rocks can become metamorphic rocks under heat and pressure. Metamorphic rocks can melt and become igneous rocks. Igneous rocks can weather and erode to form sedimentary rocks.

2. Why are fossils found mostly in sedimentary rocks?

Sedimentary rocks form in low-temperature environments, which are conducive to the preservation of fossils. The layers of deposited sediments often trap and preserve biological material.

3. What are common uses of these rock types?

  • Sedimentary rocks: Used in construction and as sources of fossil fuels.
  • Igneous rocks: Commonly used in construction, jewelry (e.g., diamonds), and industrial processes.
  • Metamorphic rocks: Used in sculpture, architecture, and construction due to their strength and beauty.

4. How can you tell the difference between rock types?

Look at their texture, crystal size, and mineral composition. Sedimentary rocks often have layers or fossils, igneous rocks have interlocking crystals, and metamorphic rocks show banding or foliation.


Conclusion

Sedimentary, igneous, and metamorphic rocks are integral to the structure of the Earth, each playing a unique role in its geological history. While their formation processes and characteristics differ significantly, these rocks are interconnected through the rock cycle, continuously transforming over millions of years. By understanding the distinctions between these three rock types, we gain insights into Earth’s dynamic processes and the history of our planet. Whether for academic study, industry, or pure curiosity, a solid grasp of these rock types is essential for appreciating the Earth’s geology.

Florida Tornadoes Exposed: Your Complete Guide to Understanding and Surviving

Florida tornado
Florida tornado

1. Introduction: The Reality of Tornadoes in Florida

When people think of Florida’s natural disasters, hurricanes and tropical storms are usually the first events that come to mind. However, tornadoes are a significant threat in the Sunshine State, with more tornadoes per 10,000 square miles annually than any other state. While Florida’s tornadoes are typically weaker compared to those in the Midwest, they can still be highly destructive and dangerous. This article aims to provide a deep understanding of tornado formation, the factors contributing to tornadoes in Florida, and safety measures to protect yourself from these violent windstorms.

Key Statistics:

  • Florida averages 66 tornadoes per year.
  • Tornadoes in Florida are often smaller, but their frequency makes them a serious threat.
  • Tornadoes can occur year-round in Florida, with peak activity during spring and hurricane season.

2. Understanding Tornado Formation

What is a Tornado?

A tornado is a rapidly rotating column of air that extends from a thunderstorm to the ground. This violently spinning air mass, often visible as a funnel-shaped cloud, can produce winds in excess of 300 miles per hour, making tornadoes one of nature’s most destructive forces. The intense low pressure within a tornado can cause buildings to explode due to the rapid reduction in external pressure.

Key Characteristics:

  • Funnel Cloud: Tornadoes often manifest as funnel clouds before reaching the ground.
  • Rotation: The defining feature of a tornado is its intense, spiraling rotation.
  • Wind Speeds: Ranging from 65 to over 300 mph depending on the tornado’s intensity.

The Role of Thunderstorms in Tornado Development

Most tornadoes form during severe thunderstorms, specifically those known as supercells. Supercells are a special type of thunderstorm that possess a rotating updraft known as a mesocyclone. It is this rotating column of air within the storm that can eventually tighten and stretch into a tornado.

Key Elements of Thunderstorms that Contribute to Tornadoes:

  • Moisture: High levels of moisture in the lower atmosphere fuel thunderstorms.
  • Instability: Warm, moist air near the surface rising into cooler, dry air in the upper atmosphere creates instability.
  • Wind Shear: Differences in wind speed or direction at different altitudes help storms rotate and potentially form tornadoes.

Tornado Formation Stages

  1. Mesocyclone Formation: A rotating storm forms due to wind shear.
  2. Funnel Cloud: The mesocyclone strengthens, lowering the air pressure and stretching downward to form a funnel cloud.
  3. Tornado Touchdown: Once the funnel cloud reaches the ground, it officially becomes a tornado.

3. Why Tornadoes Form in Florida

Geographic and Meteorological Factors

Florida’s unique geographic position between the Atlantic Ocean and the Gulf of Mexico makes it particularly vulnerable to tornadoes. The state lies in a region where cold air masses from the north collide with warm, moist air from the tropics, creating the perfect environment for thunderstorms and tornadoes.

Key Factors Leading to Tornado Formation:

  • Peninsular Geography: Surrounded by water on three sides, Florida’s weather is influenced by oceanic winds that create strong thunderstorms.
  • Sea Breezes: Converging sea breezes from the Gulf of Mexico and the Atlantic can enhance thunderstorm development and, by extension, tornado potential.

The Influence of Hurricanes on Tornado Development

Hurricanes are significant tornado producers, particularly in Florida. As these massive tropical cyclones move over land, they often spawn tornadoes in their outer rainbands. Tornadoes formed during hurricanes tend to be short-lived and weaker, but they still cause significant damage.

Key Insights:

  • Tornadoes often form in the northeast quadrant of a hurricane, where wind shear is greatest.
  • Florida’s frequent exposure to hurricanes and tropical storms increases the likelihood of tornado formation.

The Role of Jet Streams

Jet streams, fast-moving air currents high in the atmosphere, play a critical role in tornado formation. Florida, especially during the winter and early spring months, experiences interactions between the subtropical jet and the polar jet, enhancing the wind shear necessary for tornado development.

4. Tornadoes in Florida: A Historical Overview

Tornado Patterns and Seasons

Unlike the traditional “tornado alley” in the Midwest, tornadoes in Florida can occur at any time of the year. However, there are specific seasons where tornado activity is heightened:

  • Winter Tornadoes: December to February sees a peak in tornado activity due to cold fronts moving in from the north.
  • Spring Tornadoes: March to May is another active period, as warm moist air from the Gulf meets cold air from the north.
  • Hurricane Season: Tornadoes are most frequent during the Atlantic hurricane season, from June to November.

Notable Florida Tornadoes

Florida has experienced several devastating tornadoes throughout its history. Notable events include:

  • The Kissimmee Tornado Outbreak (1998): A series of deadly tornadoes swept across Central Florida, killing 42 people and causing millions in damage.
  • Hurricane Ivan Tornadoes (2004): As Hurricane Ivan made landfall, it spawned over 100 tornadoes across the southeastern U.S., with several hitting Florida.

5. Tornado Classifications: Understanding the EF Scale

The Enhanced Fujita Scale (EF Scale) is used to rate the intensity of tornadoes based on the damage they cause to structures and vegetation. The EF scale ranges from EF0 to EF5, with EF5 being the most destructive.

  • EF0: 65–85 mph winds; light damage such as broken branches.
  • EF1: 86–110 mph winds; moderate damage, including roof damage.
  • EF2: 111–135 mph winds; significant damage, such as destroyed roofs and overturned cars.
  • EF3: 136–165 mph winds; severe damage, with houses destroyed and trees uprooted.
  • EF4: 166–200 mph winds; devastating damage, with well-constructed homes leveled.
  • EF5: 200+ mph winds; incredible damage, where buildings are swept off foundations.

6. Precautions and Safety Tips During Tornadoes

Before a Tornado

Preparation is key when it comes to tornado safety. Knowing what to do before a tornado hits can save lives.

Key Precautions:

  • Create an Emergency Kit: Include essentials like water, non-perishable food, flashlights, and first-aid supplies.
  • Identify Safe Spaces: Safe rooms should be on the lowest floor, away from windows, and preferably in an interior room like a bathroom or closet.
  • Stay Informed: Pay attention to weather alerts, especially Tornado Watches (when conditions are favorable for tornadoes) and Tornado Warnings (when a tornado has been sighted).

During a Tornado

When a tornado is imminent, taking immediate action can be the difference between life and death.

Key Actions:

  • Take Shelter Immediately: Move to a pre-identified safe room, such as a basement or an interior room on the lowest floor.
  • Protect Your Head: Use a mattress, helmet, or heavy blankets to shield your head and neck from flying debris.
  • Avoid Windows: Windows are prone to shattering and can cause severe injuries.

After a Tornado

Once the storm has passed, it’s crucial to remain cautious and assess the situation.

Key Post-Tornado Safety Tips:

  • Check for Injuries: Administer first aid if needed, and seek medical help for serious injuries.
  • Stay Away from Damaged Buildings: Structures may be unstable and could collapse.
  • Watch for Hazards: Downed power lines, broken glass, and sharp debris are common hazards after tornadoes.

7. Tornado Preparedness for Florida Residents

Florida residents must be proactive in tornado preparedness due to the state’s vulnerability. Having a clear action plan is essential.

Tornado Warning Systems

  • NOAA Weather Radios: These devices provide up-to-date warnings from the National Weather Service.
  • Mobile Alerts: Download weather apps that provide real-time notifications of tornado activity.
  • Community Sirens: Many Florida counties have outdoor warning sirens to alert residents.

Home Safety Measures

  • Storm Shelters: Consider investing in a storm shelter or a reinforced safe room.
  • Strengthening Homes: Retrofit homes with hurricane straps or additional bracing to withstand strong winds.

Evacuation Plans

While most tornado safety advice emphasizes staying indoors, in certain cases (like mobile homes), evacuation may be the best option. Plan multiple evacuation routes and designate meeting points for your family.

A river is pushing up Mount Everest’s peak

Himalaya
Mountains Annapurna South and Hiunchuli from near Ghandruk in the Himalaya of central Nepal. Credit: David Whipp

Mount Everest is about 15 to 50 metres taller than it would otherwise be because of uplift caused by a nearby eroding river gorge, and continues to grow because of it, finds a new study by UCL researchers.

The study, published in Nature Geoscience, found that erosion from a river network about 75 kilometres from Mount Everest is carving away a substantial gorge. The loss of this landmass is causing the mountain to spring upwards by as much as 2 millimetres a year and has already increased its height by between 15 and 50 metres over the past 89,000 years.

At 8,849 metres high, Mount Everest, also known as Chomolungma in Tibetan or Sagarmāthā in Nepali, is the tallest mountain on Earth, and rises about 250 metres above the next tallest peak in the Himalayas. Everest is considered anomalously high for the mountain range, as the next three tallest peaks — K2, Kangchenjunga and Lhotse — all only differ by about 120 metres from each other.

A significant portion of this anomaly can be explained by an uplifting force caused by pressure from below Earth’s crust after a nearby river eroded away a sizeable amount of rocks and soils. It’s an effect called isostatic rebound, where a section of the Earth’s crust that loses mass flexes and “floats” upwards because the intense pressure of the liquid mantle below is greater than the downward force of gravity after the loss of mass. It’s a gradual process, usually only a few millimetres a year, but over geological timeframes can make a significant difference to the Earth’s surface.

The researchers found that because of this process Mount Everest grew by about 15 to 50 metres over the last 89,000 years, since the nearby Arun river merged with the adjacent Kosi river network.

Co-author, PhD student Adam Smith (UCL Earth Sciences) said: “Mount Everest is a remarkable mountain of myth and legend and it’s still growing. Our research shows that as the nearby river system cuts deeper, the loss of material is causing the mountain to spring further upwards.”

Today, the Arun river runs to the east of Mount Everest and merges downstream with the larger Kosi river system. Over millennia, the Arun has carved out a substantial gorge along its banks, washing away billions of tonnes of earth and sediment.

Co-author Dr Jin-Gen Dai of the China University of Geosciences, said: “An interesting river system exists in the Everest region. The upstream Arun river flows east at high altitude with a flat valley. It then abruptly turns south as the Kosi river, dropping in elevation and becoming steeper. This unique topography, indicative of an unsteady state, likely relates to Everest’s extreme height.”

The uplift is not limited to Mount Everest, and affects neighbouring peaks including Lhotse and Makalu, the world’s fourth and fifth highest peaks respectively. The isostatic rebound boosts the heights of these peaks by a similar amount as it does Everest, though Makalu, located closest to the Arun river, would experience a slightly higher rate of uplift.

Co-author Dr Matthew Fox (UCL Earth Sciences) said: “Mount Everest and its neighbouring peaks are growing because the isostatic rebound is raising them up faster than erosion is wearing them down. We can see them growing by about two millimetres a year using GPS instruments and now we have a better understanding of what’s driving it.”

By looking at the erosion rates of the Arun, the Kosi and other rivers in the region, the researchers were able to determine that about 89,000 years ago the Arun river joined and merged with the Kosi river network, a process called drainage piracy. In doing so, more water was funnelled through the Kosi river, increasing its erosive power and taking more of the landscape’s soils and sediments with it. With more of the land washed away, it triggered an increased rate of uplift, pushing the mountains’ peaks higher and higher.

Lead author Dr Xu Han of China University of Geosciences, who carried out the work while on a China Scholarship Council research visit to UCL, said: “The changing height of Mount Everest really highlights the dynamic nature of the Earth’s surface. The interaction between the erosion of the Arun river and the upward pressure of the Earth’s mantle gives Mount Everest a boost, pushing it up higher than it would otherwise be.”

Reference:
Xu Han, Jin-Gen Dai, Adam G. G. Smith, Shi-Ying Xu, Bo-Rong Liu, Cheng-Shan Wang, Matthew Fox. Recent uplift of Chomolungma enhanced by river drainage piracy. Nature Geoscience, 2024; DOI: 10.1038/s41561-024-01535-w

Note: The above post is reprinted from materials provided by University College London.

Ancient sunken seafloor reveals earth’s deep secrets

A map of the East Pacific Rise region where the discovery of an ancient seafloor was made. Credit: Jingchuan Wang.
A map of the East Pacific Rise region where the discovery of an ancient seafloor was made. Credit: Jingchuan Wang.

University of Maryland scientists uncovered evidence of an ancient seafloor that sank deep into Earth during the age of dinosaurs, challenging existing theories about Earth’s interior structure. Located in the East Pacific Rise (a tectonic plate boundary on the floor of the southeastern Pacific Ocean), this previously unstudied patch of seafloor sheds new light on the inner workings of our planet and how its surface has changed over millions of years. The team’s findings were published in the journal Science Advances on September 27, 2024.

Led by geology postdoctoral researcher Jingchuan Wang, the team used innovative seismic imaging techniques to peer deep into Earth’s mantle, the layer between our planet’s crust and core. They found an unusually thick area in the mantle transition zone, a region located between about 410 and 660 kilometers below the Earth’s surface. The zone separates the upper and lower mantles, expanding or contracting based on temperature. The team believes that the newly discovered seafloor may also explain the anomalous structure of the Pacific Large Low Shear Velocity Province (LLSVP) — a massive region in Earth’s lower mantle — as the LLSVP appears to be split by the slab.

“This thickened area is like a fossilized fingerprint of an ancient piece of seafloor that subducted into the Earth approximately 250 million years ago,” Wang said. “It’s giving us a glimpse into Earth’s past that we’ve never had before.”

Subduction occurs when one tectonic plate slides beneath another, recycling surface material back into Earth’s mantle. The process often leaves visible evidence of movement, including volcanoes, earthquakes and deep marine trenches. While geologists typically study subduction by examining rock samples and sediments found on Earth’s surface, Wang worked with Geology Professor Vedran Lekic and Associate Professor Nicholas Schmerr to use seismic waves to probe through the ocean floor. By examining how seismic waves traveled through different layers of Earth, the scientists were able to create detailed mappings of the structures hiding deep within the mantle.

“You can think of seismic imaging as something similar to a CT scan. It’s basically allowed us to have a cross-sectional view of our planet’s insides,” Wang said. “Usually, oceanic slabs of material are consumed by the Earth completely, leaving no discernible traces on the surface. But seeing the ancient subduction slab through this perspective gave us new insights into the relationship between very deep Earth structures and surface geology, which were not obvious before.”

What the team found surprised them — material was moving through Earth’s interior much more slowly than previously thought. Wang believes that the unusual thickness of the area the team discovered suggests the presence of colder material in this part of the mantle transition zone, hinting that some oceanic slabs get stuck halfway down as they sink through the mantle.

“We found that in this region, the material was sinking at about half the speed we expected, which suggests that the mantle transition zone can act like a barrier and slow down the movement of material through the Earth,” Wang explained. “Our discovery opens up new questions about how the deep Earth influences what we see on the surface across vast distances and timescales.”

Looking ahead, the team plans to extend their research into other areas of the Pacific Ocean and beyond. Wang hopes to create a more comprehensive map of ancient subduction and upwelling (the geological process that occurs when subducted material heats up and rises to the surface again) zones, as well as their effects on both deep and surface Earth structures. With the seismic data acquired from this research, Wang and other scientists are improving their models of how tectonic plates have moved throughout Earth’s history.

“This is just the beginning,” Wang said. “We believe that there are many more ancient structures waiting to be discovered in Earth’s deep interior. Each one has the potential to reveal many new insights about our planet’s complex past — and even lead to a better understanding of other planets beyond ours.”

Reference:
Jingchuan Wang, Vedran Lekić, Nicholas C. Schmerr, Yu J. Gu, Yi Guo, Rongzhi Lin. Mesozoic intraoceanic subduction shaped the lower mantle beneath the East Pacific Rise. Science Advances, 2024; 10 (39) DOI: 10.1126/sciadv.ado1219

Note: The above post is reprinted from materials provided by University of Maryland.

Reconstructing the evolutionary history of the grape family

Nekemias mucronata fossil lateral leaflets from the collection of the Natural Science Museum of Barcelona.
Nekemias mucronata fossil lateral leaflets from the collection of the Natural Science Museum of Barcelona.

Until now, it was believed that plants of the grape family arrived at the European continent less than 23 million years ago. A study on fossil plants draws a new scenario on the dispersal of the ancestors of grape plants and reveals that these species were already on the territory of Europe some 41 million years ago. The paper describes a new fossil species of the same family, Nekemias mucronata, which allows us to better understand the evolutionary history of this plant group, which inhabited Europe between 40 and 23 million years ago.

This study, published in the Journal of Systematics and Evolution (JSE), is led by researcher Aixa Tosal, from the Faculty of Earth Sciences and the Biodiversity Research Institute (IRBio) of the University of Barcelona. The article is also signed by Alba Vicente, from the Biodiversity Research Institute (IRBio) and the Catalan Institute of Palaeontology Miquel Crusafont (ICP), and Thomas Denk, from the Swedish Museum of Natural History (Stockholm).

A new ancestor of the grape family

The grape family (Vitaceae) is made up of some 950 species, and is divided into five tribes (in botany, this is an intermediate taxonomic classification between the family and the genus). One of these tribes is the Viteae, made up of 200 species, including the grape vine plant (Vitis vinifera), which is of great global economic interest. The new paper published in the JSE focuses on studying the tribe Ampelopsideae, made up of 47 species.

“Our study changes the paradigms accepted until now and shows that the Ampelopsis and Nekemias lineages of the Ampelopsideae tribe were already present in Europe and Central Asia during the middle Eocene (between 47 and 37 million years ago). This indicates that this dispersal was approximately 20 million years earlier than previously estimated,” says Aixa Tosal, first author of the study and member of the UB’s Department of Earth and Ocean Dynamics.

“In particular, we show that a lineage now restricted to North America already existed in Europe and Central Asia, thanks to the discovery of the fossil species Nekemias mucronata, which is very similar to the present-day North American Nekemias arborea. Nekemias mucronata cohabited with Ampelopsis hibschii, the closest relative of today’s Ampelopsis orientalis,” explains Tosal. In contrast, the latter has had a different dispersal from N. mucronata, as this lineage is now endemic to the eastern Mediterranean. “This study helps us to better understand the evolution of the Ampelopsideae tribe during the second dispersal pulse, especially in Europe and Central Asia, which took place during the Palaeogene,” says Tosal.

Nekemias mucronata lived from the late Eocene to the late Oligocene (37-23 million years ago). It seems that it was able to grow in a broad range of climates, from regions with low winter temperatures (-4.6 °C in cold periods) — such as those found in Kazakhstan during the Oligocene (33-23) million years ago — to regions with warm mean annual temperatures — such as those of the Oligocene in the Iberian Peninsula — or even in climates with intermediate temperatures such as those recorded in the centre of the European continent.

“N. mucronata was also not overly demanding in terms of rainfall. It could grow in areas with abundant rainfall and low rainfall seasonality; for example, in Central Europe during the Oligocene, or the Iberian Peninsula or Greece during the same time,” says ICP researcher Alba Vicente. “This fossil species had a compound leaf, a peculiarity shared with some species of the vine family. Although it is difficult to confirm the number of leaflets of the compound leaf, it would have consisted of at least three. We have been able to recognize common patterns between the apical and lateral leaflets, which allows us to distinguish them from other fossil species of the vine family in Eurasia,” he adds. “What makes Nekemias mucronata unique is the presence of a mucro at the tip of the leaflet teeth, which gives the species its name. The straight shape of the base of the apical leaflet is also quite distinctive, as all other Eurasian fossil species are buckled (with an invagination near the petiole),” says Vicente.

Dispersal of Ampelopsideae across the Atlantic bridge or the Bering Strait

To date, the oldest record of the grape family has been found in the Upper Cretaceous deposits of India (75-65 Ma). The earliest record of the plant lineage in the Americas is from the Upper Eocene, around 39.4 million years ago, and at about the same time in Europe and Central Asia the Ampelopsis and Nekemias lineages are already found.

How did these species disperse in the past? These tribes diverged between the Upper Cretaceous and the Upper Eocene and, although there are still many unknowns, it seems that they dispersed and evolved quite rapidly. According to current data, which are consistent with the molecular clock technique, “the Ampelopsideae could have followed two cluster routes or a mixture of both. The first proposed route follows the North Atlantic isthmus. That is, the family appeared in India, then moved on to central Asia and Europe during the middle Eocene (between 47 and 37 million years ago), and finally moved on to the Americas via Greenland,” says Thomas Denk. “Another possible route suggests that, once the Vitaceae family appeared in India, the Ampelopsideae tribe dispersed eastward from Asia during the middle Eocene (47-37 million years ago) and quickly moved to the Americas via the Bering Strait, and from there to Europe along the North Atlantic isthmus,” Denk says.

Although the dispersal of these two species does not seem to be linked to climate, it is possible that the increase in aridity during the Oligocene in the Iberian Peninsula and southern Europe explains the extinction (27-23 million years ago) of the last population of N. mucronata found in the Iberian Peninsula. In parallel, Ampelopsis hibschii was restricted to the Balkan area and finally became extinct about 15 million years ago.

“However, there are still many unanswered questions about the early dispersal phases (from the Late Cretaceous to the Palaeogene). For this reason, we would like to continue studying this family, and perhaps we will be able to unravel what happened during their early cluster phases, which occurred between 66 and 41 million years ago,” the team concludes.

Reference:
Aixa Tosal, Alba Vicente, Thomas Denk. Cenozoic Ampelopsis and Nekemias leaves (Vitaceae, Ampelopsideae) from Eurasia: Paleobiogeographic and paleoclimatic implications. Journal of Systematics and Evolution, 2024; DOI: 10.1111/jse.13126

Note: The above post is reprinted from materials provided by University of Barcelona.

Brazilian fossils reveal jaw-dropping discovery in mammal evolution

Riograndia and BrasilodonCredit: Jorge Blanco
Riograndia and Brasilodon
Credit: Jorge Blanco

These fossils, belonging to the mammal-precursor species Brasilodon quadrangularis and Riograndia guaibensis, offer critical insights into the development of the mammalian jaw and middle ear, revealing evolutionary experiments that occurred millions of years earlier than previously thought.

Mammals stand out among vertebrates for their distinct jaw structure and the presence of three middle ear bones. This transition from earlier vertebrates, which had a single middle ear bone, has long fascinated scientists. The new study explores how mammal ancestors, known as cynodonts, evolved these features over time.

Using CT scanning, researchers were able to digitally reconstruct the jaw joint of these cynodonts for the first time. The researchers uncovered a ‘mammalian-style’ contact between the skull and the lower jaw in Riograndia guaibensis, a cynodont species that lived 17 million years before the previously oldest known example of this structure, but did not find one in Brasilodon quadrangularis, a species more closely related to mammals. This indicates that the defining mammalian jaw feature evolved multiple times in different groups of cynodonts, earlier than expected.

These findings suggest that mammalian ancestors experimented with different jaw functions, leading to the evolution of ‘mammalian’ traits independently in various lineages. The early evolution of mammals, it turns out, was far more complex and varied than previously understood.

Lead author James Rawson based in Bristol’s School of Earth Sciences explained: “The acquisition of the mammalian jaw contact was a key moment in mammal evolution.

“What these new Brazilian fossils have shown is that different cynodont groups were experimenting with various jaw joint types, and that some features once considered uniquely mammalian evolved numerous times in other lineages as well.”

This discovery has broad implications for the understanding of the early stages of mammal evolution, illustrating that features such as the mammalian jaw joint and middle ear bones evolved in a patchwork, or mosaic, fashion across different cynodont groups.

Dr. Agustín Martinelli, from the Museo Argentino de Ciencias Natural of Buenos Aires, stated: “Over the last years, these tiny fossil species from Brazil have brought marvellous information that enrich our knowledge about the origin and evolution of mammalian features. We are just in the beginning and our multi-national collaborations will bring more news soon.”

The research team is eager to further investigate the South American fossil record, which has proven to be a rich source of new information on mammalian evolution.

Professor Marina Soares of the Museu Nacional, Brazil, stated: “Nowhere else in the world has such a diverse array of cynodont forms, closely related to the earliest mammals.”

By integrating these findings with existing data, the scientists hope to deepen their understanding of how early jaw joints functioned and contributed to the development of the mammalian form.

James added: “The study opens new doors for paleontological research, as these fossils provide invaluable evidence of the complex and varied evolutionary experiments that ultimately gave rise to modern mammals.”

Reference:
Rawson, J.R.G., Martinelli, A.G., Gill, P.G. et al. Brazilian fossils reveal homoplasy in the oldest mammalian jaw joint. Nature, 2024 DOI: 10.1038/s41586-024-07971-3

Note: The above post is reprinted from materials provided by University of Bristol.

Unveiling ancient life: New method sheds light on early cellular and metabolic evolution

Results of the multimodal analysis conducted on microfossils mounted on ITO glass. Optical observation, electron microscopy, and secondary ion mass spectrometry were performed on the same sample. The analysis successfully detected phosphorus and molybdenum aligned with the microfossil's membrane structure for the first time. ©Tohoku University
Results of the multimodal analysis conducted on microfossils mounted on ITO glass. Optical observation, electron microscopy, and secondary ion mass spectrometry were performed on the same sample. The analysis successfully detected phosphorus and molybdenum aligned with the microfossil’s membrane structure for the first time. ©Tohoku University

Fossils don’t always come in large, dinosaur-sized packages. Microfossils refer to a type of fossil that is so small, it can only be perceived with a microscope. These microfossils can help us understand when and how early life forms developed essential features — ultimately allowing us to study the evolution of life. In order to analyze these microfossils, a pioneering method of analysis has been developed by a research team led by Akizumi Ishida from Tohoku University, in collaboration with experts from the University of Tokyo and Kochi University.

“To analyze microfossils, scientists must detect minute quantities of critical elements like phosphorus and molybdenum,” explains Ishida, “However, so far this has proven challenging.”

Their work focuses on 1.9-billion-year-old Gunflint microfossils, which are known as the “standard” of microfossil study.

The team employed a novel approach by fixing these microfossils onto a specially coated glass slide (ITO-glass), allowing for integrated observations using both optical and electron microscopy.

ITO-glass is a glass plate coated with a thin layer of indium tin oxide (ITO). This conductive coating of metal oxide is not only suitable for electron microscopy and secondary ion mass spectrometry (SIMS), but also allows for optical observation.

Due to its transparency, the internal structure of microfossils can be examined.

This method also enabled the precise detection of trace elements within the microfossils.

In other words, it was able to clearly detect the true amount contrasted against a base level of background “noise.” Phosphorus also occurs naturally in sedimentary rocks, for example, so it’s important to be able to tell the difference.

By overcoming the interference from rock-derived elements and materials used to mount the fossils, the researchers successfully identified extremely low levels of phosphorus and molybdenum by using NanoSIMS (High Spatial Resolution Secondary Ion Mass Spectrometer). This device allows for the imaging of almost all elements except noble gases with ultra-high spatial resolution of less than one micron.

Their analysis of phosphorus seen along the contours of microfossils revealed that these ancient microorganisms already had phospholipid cell membranes similar to those found in modern organisms.

Additionally, the presence of molybdenum within microfossil bodies suggested the existence of possible nitrogen-fixing metabolic enzymes, consistent with previous reports identifying these microfossils as cyanobacteria.

This innovative protocol is unique in its ability to provide consistent observations and analyses on the same sample.

It offers significant advancements in understanding how life evolved on Earth’s, providing direct evidence of cell membranes and metabolic processes in ancient microorganisms.

This technique is applicable not only to microfossils but also to early Earth’s geological samples with minimal organic material. It opens avenues for analyzing even older geological periods. Additionally, it extends to trace elements such as copper, nickel, and cobalt, which can reveal metabolic patterns. The findings are expected to set new standards in early life evolution research and ultimately contribute to answering the profound questions about when and where life originated and how it evolved on Earth.

Reference:
Kohei Sasaki, Akizumi Ishida, Takeshi Kakegawa, Naoto Takahata, Yuji Sano. Ultrahigh-resolution imaging of biogenic phosphorus and molybdenum in palaeoproterozoic gunflint microfossils. Scientific Reports, 2024; 14 (1) DOI: 10.1038/s41598-024-72191-8

Note: The above post is reprinted from materials provided by Tohoku University.

Over nearly half a billion years, Earth’s global temperature has changed drastically, driven by carbon dioxide

Earth has been warmer than today over the past 485 million years, but humans and animals cannot adapt fast enough to keep up with human-caused climate change at the rate it is happening today and in the future.Shutterstock
Earth has been warmer than today over the past 485 million years, but humans and animals cannot adapt fast enough to keep up with human-caused climate change at the rate it is happening today and in the future.
Shutterstock

Published in the journal Science, the study presents a curve of global mean surface temperature that reveals Earth’s temperature has varied more than previously thought over much of the Phanerozoic Eon a period of geologic time when life diversified, populated land and endured multiple mass extinctions. The curve also confirms Earth’s temperature is strongly correlated to the amount of carbon dioxide in the atmosphere.

The start of the Phanerozoic Eon 540 million years ago is marked by the Cambrian Explosion, a point in time when complex, hard-shelled organisms first appeared in the fossil record. Although researchers can create simulations all the way back to 540 million years ago, the temperature curve in the study focuses on the last 485 million years since there is limited geological data of temperature before then.

“It’s hard to find rocks that are that old and have temperature indicators preserved in them — even at 485 million years ago we don’t have that many. We were limited with how far back we could go,” said study co-author Jessica Tierney, a paleoclimatologist at the University of Arizona.

The researchers created the temperature curve using an approach called data assimilation. This allowed them to combine data from the geologic record and climate models to create a more cohesive understanding of ancient climates.

“This method was originally developed for weather forecasting,” said Emily Judd, lead author of the paper and a former postdoctoral researcher at the Smithsonian National Museum of Natural History and the U of A. “Instead of using it to forecast future weather, here we’re using it to hindcast ancient climates.”

Refining scientists’ understanding of how Earth’s temperature has fluctuated over time provides crucial context for understanding modern climate change.

“If you’re studying the last couple of million years, you won’t find anything that looks like what we expect in 2100 or 2500,” said Scott Wing, a co-author on the paper and a curator of paleobotany at the Smithsonian National Museum of Natural History. “You need to go back even further to periods when the Earth was really warm, because that’s the only way we’re going to get a better understanding of how the climate might change in the future.”

The new curve reveals that temperature varied more greatly during the past 485 million years than previously thought. Over the eon, the global temperature spanned 52 to 97 degrees Fahrenheit. Periods of extreme heat were most often linked to elevated levels of the greenhouse gas carbon dioxide in the atmosphere.

“This research illustrates clearly that carbon dioxide is the dominant control on global temperatures across geological time,” said Tierney. “When CO2 is low, the temperature is cold; when CO2 is high, the temperature is warm.”

The findings also reveal that the Earth’s current global temperature of 59 degrees Fahrenheit is cooler than Earth has been over much of the Phanerozoic. But greenhouse gas emissions from human-caused climate change are currently warming the planet at a much faster rate than even the fastest warming events of the Phanerozoic, the reseaerchers say. The speed of warming puts species and ecosystems around the world at risk and is causing a rapid rise in sea level. Some other episodes of rapid climate change during the Phanerozoic have sparked mass extinctions.

Rapidly moving toward a warmer climate could spell danger for humans who have mostly lived in a 10 degree Fahrenheit range for the global temperatures, compared to the 45 degree span of temperatures over the last 485 million years, the researchers say.

“Our entire species evolved to an ‘ice house’ climate, which doesn’t reflect most of geological history,” Tierney said. “We are changing the climate into a place that is really out of context for humans. The planet has been and can be warmer — but humans and animals can’t adapt that fast.”

The collaboration between Tierney and researchers at the Smithsonian began in 2018. The team wanted to provide museum visitors with a curve that charted Earth’s global temperature across the Phanerozoic, which began around 540 million years ago and continues into the present day.

The team collected more than 150,000 estimates of ancient temperature calculated from five different chemical indicators for temperature that are preserved in fossilized shells and other types of ancient organic matter. Their colleagues at the University of Bristol created more than 850 model simulations of what Earth’s climate could have looked like at different periods of the distant past based on continental position and atmospheric composition. The researchers then combined these two lines of evidence to create the most accurate curve of how Earth’s temperature has varied over the past 485 million years.

Another finding from the study pertains to climate sensitivity, a metric of how much the climate warms for the doubling of carbon dioxide.

“We found that carbon dioxide and temperature are not only really closely related, but related in the same way across 485 million years. We don’t see that the climate is more sensitive when it’s hot or cold,” Tierney said.

In addition to Judd, Tierney, Huber and Wing, Daniel Lunt and Paul Valdes of the University of Bristol and Isabel Montañez of the University of California, Davis are coauthors on the study.

The research was supported by Roland and Debra Sauermann through the Smithsonian; the Heising-Simons Foundation and the University of Arizona’s Thomas R. Brown Distinguished Chair in Integrative Science through Tierney; and the United Kingdom’s Natural Environment Research Council.

Reference:
Emily J. Judd, Jessica E. Tierney, Daniel J. Lunt, Isabel P. Montañez, Brian T. Huber, Scott L. Wing, Paul J. Valdes. A 485-million-year history of Earth’s surface temperature. Science, 2024; 385 (6715) DOI: 10.1126/science.adk3705

Note: The above post is reprinted from materials provided by University of Arizona.

Extinct volcanoes a ‘rich’ source of rare earth elements

volcano
volcano

A mysterious type of iron-rich magma entombed within extinct volcanoes is likely abundant with rare earth elements and could offer a new way to source these in-demand metals, according to new research from The Australian National University (ANU) and the University of the Chinese Academy of Sciences.

Rare earth elements are found in smartphones, flat screen TVs, magnets, and even trains and missiles.

They are also vital to the development of electric vehicles and renewable energy technologies such as wind turbines.

Dr Michael Anenburg from ANU said the iron-rich magma that solidified to form some extinct volcanoes is up to a hundred times more efficient at concentrating rare earth metals than the magmas that commonly erupt from active volcanoes.

“We have never seen an iron-rich magma erupt from an active volcano, but we know some extinct volcanoes, which are millions of years old, had this enigmatic type of eruption,” Dr Anenburg said.

“Our findings suggest that these iron-rich extinct volcanoes across the globe, such as El Laco in Chile, could be studied for the presence of rare earth elements.”

The researchers simulated volcanic eruptions in the lab by sourcing rocks similar to those from iron-rich extinct volcanoes.

They put these rocks into a pressurised furnace and heated them to extremely high temperatures to melt them and learn more about the minerals inside the rocks.

This is how they discovered the abundance of rare earth elements contained in iron-rich volcanic rocks.

With more countries investing heavily in renewable energy technologies, the demand for rare earth elements continues to skyrocket.

In fact, demand for these elements is expected to increase fivefold by 2030.

“Rare earth elements aren’t that rare. They are similar in abundance to lead and copper. But breaking down and extracting these metals from the minerals they reside in is challenging and expensive,” Dr Anenburg said.

China has the biggest deposit of rare earth elements on the planet, while Europe’s largest deposit of rare earths is in Sweden.

Australia has a world-class deposit at Mount Weld in Western Australia and others near Dubbo and Alice Springs.

According to Dr Anenburg, Australia has an opportunity to become a major player in the clean energy space by capitalising on its abundance of rare earth resources.

The research is published in Geochemical Perspectives Letters. This work was led by Shengchao Yan from the University of the Chinese Academy of Sciences.

Reference:
S.C. Yan, B. Wan, M. Anenburg, J.A. Mavrogenes. Silicate and iron phosphate melt immiscibility promotes REE enrichment. Geochemical Perspectives Letters, 2024; 32: 14 DOI: 10.7185/geochemlet.2436

Note: The above post is reprinted from materials provided by Australian National University.

New research reenvisions Earth’s mantle as a relatively uniform reservoir

"Lava" Earth's mantle
Credit: Massachusetts Institute of Technology

Lavas from hotspots — whether erupting in Hawaii, Samoa or Iceland — likely originate from a worldwide, uniform reservoir in Earth’s mantle, according to an evaluation of volcanic hotspots published today in Nature Geoscience.

The findings indicate Earth’s mantle is far more chemically homogenous than scientists previously thought — and that lavas only acquire their unique chemical “flavours” enroute to the surface.

“The discovery literally turns our view of hotspot lavas and the mantle upside down,” said Dr. Matthijs Smit, associate professor and Canada Research Chair at the University of British Columbia’s Department of Earth, Ocean and Atmospheric Sciences. “In a way, Earth’s lavas are much like humankind itself — a beautifully diverse population with a common ancestor, which developed differently wherever it went.”

Research of Earth’s mantle has been complicated by the fact that it can’t be sampled directly. Scientists instead have to engage in a bit of geoscientific detective work; they study this important part of our planet through trace-element and isotope analysis of lava that comes from the mantle and is erupted at oceanic volcanoes around the world. The vast differences in composition of these lavas, along with the assumption that the isotope composition of magma doesn’t change between its source and the surface, has led to the general view that the mantle contains distinct reservoirs of different age, located in different regions, and formed by different processes. The observations made by Dr. Smit and co-author Dr. Kooijman of the Swedish Museum of Natural History’s Department of Geosciences indicate that the reality may be quite different.

“By looking at a specific set of elements, we were able discern the chemical effects of various processes that act on magma melts on their way to the surface to discover that all hotspot lavas actually share the same starting composition,” said Dr. Smit. “The lavas only come out differently because the magmas interact with different types of rocks as they ascend.”

Earth’s mantle is a seething layer of molten and semi-molten material comprising about 84 per cent of the planet’s volume, which lies between the iron core and the surface crust. When magma derived from the mantle penetrates the crust and erupts onto the surface it is called lava.

Knowing what the mantle is made of is central to our understanding of how our planet formed and how the mantle has developed over time. It may also provide clues as to why the mantle behaves the way it does, how it drives plate tectonics, and what its role is in the global cycle of elements.

Besides shedding entirely new light on hotspot lavas in oceanic parts of the world, the analysis also revealed an exciting new link to basaltic lavas on the continents. These melts, which contain diamond-bearing kimberlites, are fundamentally different from magmas found at oceanic hotspots. They nevertheless prove to have the same magma “ancestor.”

“The discovery is a game-changer when it comes to models for Earth’s chemical evolution and how we look at global element cycles,” said Dr. Smit. “Not only is the mantle much more homogeneous than previously thought, it likely also no longer contains “primordial reservoirs” — entities that were once needed to explain the data, but could never really be reconciled with the concept of mantle convection.”

“This model explains the observations in a simple way and permits a myriad of new hypotheses for global geochemical research going forward,” said Dr. Kooijman.

Financial support for this research was provided by the National Science and Engineering Research Council of Canada.

Reference:
Matthijs A. Smit, Ellen Kooijman. A common precursor for global hotspot lavas. Nature Geoscience, 2024; DOI: 10.1038/s41561-024-01538-7

Note: The above post is reprinted from materials provided by University of British Columbia.

Climate-change-triggered 2023 mega-landslide caused Earth to vibrate for nine days

From left to right: before (August 2023) and after (September 2023) photos of the mountain peak and glacier, taken from the fjord. Credit: Søren Rysgaard / Danish Army.
From left to right: before (August 2023) and after (September 2023) photos of the mountain peak and glacier, taken from the fjord. Credit: Søren Rysgaard / Danish Army.

A landslide in a remote part of Greenland caused a mega-tsunami that sloshed back and forth across a fjord for nine days, generating vibrations throughout Earth, according to a new study involving UCL researchers.

The study, published in the journal Science, concluded that this movement of water was the cause of a mysterious, global seismic signal that lasted for nine days and puzzled seismologists in September 2023.

The initial event, not observed by human eye, was the collapse of a 1.2km-high mountain peak into the remote Dickson Fjord beneath, causing a backsplash of water 200 metres in the air, with a wave up to 110 metres high. This wave, extending across 10km of fjord, reduced to seven metres within a few minutes, the researchers calculated, and would have fallen to a few centimetres in the days after.

The team used a detailed mathematical model, recreating the angle of the landslide and the uniquely narrow and bendy fjord, to demonstrate how the sloshing of water would have continued for nine days, with little energy able to escape.

The model predicted that the mass of water would have moved back and forth every 90 seconds, matching the recordings of vibrations travelling in the Earth’s crust all around the globe.

The landslide, the researchers wrote, was a result of the glacier at the foot of the mountain thinning, becoming unable to hold up the rock-face above it. This was ultimately due to climate change. The landslide and tsunami were the first observed in eastern Greenland.

Co-author Dr Stephen Hicks, of UCL Earth Sciences, said: “When I first saw the seismic signal, I was completely baffled. Even though we know seismometers can record a variety of sources happening on Earth’s surface, never before has such a long-lasting, globally travelling seismic wave, containing only a single frequency of oscillation, been recorded. This inspired me to co-lead a large team of scientists to figure out the puzzle.

“Our study of this event amazingly highlights the intricate interconnections between climate change in the atmosphere, destabilisation of glacier ice in the cryosphere, movements of water bodies in the hydrosphere, and Earth’s solid crust in the lithosphere.

“This is the first time that water sloshing has been recorded as vibrations through the Earth’s crust, travelling the world over and lasting several days.”

The mysterious seismic signal — coming from a vibration through the Earth’s crust — was detected by seismometers all over the globe, from the Arctic to Antarctica. It looked completely different to frequency-rich ‘rumbles’ and ‘pings’ from earthquake recordings, as it contained only a single vibration frequency, like a monotonous-sounding hum.

When the study’s authors first discovered the signal, they made a note of it as a “USO”: unidentified seismic object.

At the same time, news of a large tsunami in a remote northeast Greenland fjord reached authorities and researchers working in the area.

The researchers joined forces in a unique multidisciplinary group involving 68 scientists from 40 institutions in 15 countries, combining seismometer and infrasound data, field measurements, on-the-ground and satellite imagery, and simulations of tsunami waves.

The team also used imagery captured by the Danish military who sailed into the fjord just days after the event to inspect the collapsed mountain-face and glacier front along with the dramatic scars left by the tsunami.

It was this combination of local field data and remote, global-scale observations that allowed the team to solve the puzzle and reconstruct the extraordinary cascading sequence of events.

Lead author Dr Kristian Svennevig, from the Geological Survey of Denmark and Greenland (GEUS), said: “When we set out on this scientific adventure, everybody was puzzled and no one had the faintest idea what caused this signal. All we knew was that it was somehow associated with the landslide. We only managed to solve this enigma through a huge interdisciplinary and international effort.”

He added: “As a landslide scientist, an additional interesting aspect of this study is that this is the first-ever landslide and tsunami observed from eastern Greenland, showing how climate change already has major impacts there.”

The team estimated that 25 million cubic metres of rock and ice crashed into the fjord (enough to fill 10,000 Olympic-sized swimming pools).

They confirmed the size of the tsunami, one of the largest seen in recent history, using numerical simulations as well as local data and imagery.

Seventy kilometres away from the landslide, four-metre-high tsunami waves damaged a research base at Ella Ø (island) and destroyed cultural and archaeological heritage sites across the fjord system.

The fjord is on a route commonly used by tourist cruise ships visiting the Greenland fjords. Fortunately, no cruise ships were close to Dickson Fjord on the day of the landslide and tsunami, but if they had been, the consequences of a tsunami wave of that magnitude could have been devastating.

Mathematical models recreating the width and depth of the fjord at very high resolution demonstrated how the distinct rhythm of a mass of water moving back and forth matched the seismic signal.

The study concluded that with rapidly accelerating climate change, it will become more important than ever to characterise and monitor regions previously considered stable and provide early warning of these massive landslide and tsunami events.

Co-author Thomas Forbriger, from Karlsruhe Institute of Technology, said: “We wouldn’t have discovered or been able to analyse this amazing event without networks of high-fidelity broadband seismic stations around the world, which are the only sensors that can truly capture such a unique signal.”

Co-author Anne Mangeney, from Université Paris Cité, Institut de Physique du Globe de Paris, said: “This unique tsunami challenged the classical numerical models that we previously used to simulate just a few hours of tsunami propagation. We had to go to an unprecedentedly high numerical resolution to capture this long-duration event in Greenland. This opens up new avenues in the development of numerical methods for tsunami modelling.”

Reference:
Kristian Svennevig, Stephen P. Hicks, Thomas Forbriger, Thomas Lecocq, Rudolf Widmer-Schnidrig, Anne Mangeney, Clément Hibert, Niels J. Korsgaard, Antoine Lucas, Claudio Satriano, Robert E. Anthony, Aurélien Mordret, Sven Schippkus, Søren Rysgaard, Wieter Boone, Steven J. Gibbons, Kristen L. Cook, Sylfest Glimsdal, Finn Løvholt, Koen Van Noten, Jelle D. Assink, Alexis Marboeuf, Anthony Lomax, Kris Vanneste, Taka’aki Taira, Matteo Spagnolo, Raphael De Plaen, Paula Koelemeijer, Carl Ebeling, Andrea Cannata, William D. Harcourt, David G. Cornwell, Corentin Caudron, Piero Poli, Pascal Bernard, Eric Larose, Eleonore Stutzmann, Peter H. Voss, Bjorn Lund, Flavio Cannavo, Manuel J. Castro-Díaz, Esteban Chaves, Trine Dahl-Jensen, Nicolas De Pinho Dias, Aline Déprez, Roeland Develter, Douglas Dreger, Läslo G. Evers, Enrique D. Fernández-Nieto, Ana M. G. Ferreira, Gareth Funning, Alice-Agnes Gabriel, Marc Hendrickx, Alan L. Kafka, Marie Keiding, Jeffrey Kerby, Shfaqat A. Khan, Andreas Kjær Dideriksen, Oliver D. Lamb, Tine B. Larsen, Bradley Lipovsky, Ikha Magdalena, Jean-Philippe Malet, Mikkel Myrup, Luis Rivera, Eugenio Ruiz-Castillo, Selina Wetter, Bastien Wirtz. A rockslide-generated tsunami in a Greenland fjord rang Earth for 9 days. Science, 2024; 385 (6714): 1196 DOI: 10.1126/science.adm9247

Note: The above post is reprinted from materials provided by University College London.

Doughnut-shaped region found inside Earth’s core deepens understanding of planet’s magnetic field

A diagram showing seismic waves traveling through Earth where the newly discovered doughnut-shaped region was detected. Image: Xiaolong Ma and Hrvoje Tkalčić/ANU
A diagram showing seismic waves traveling through Earth where the newly discovered doughnut-shaped region was detected. Image: Xiaolong Ma and Hrvoje Tkalčić/ANU

A doughnut-shaped region thousands of kilometres beneath our feet within Earth’s liquid core has been discovered by scientists from The Australian National University (ANU), providing new clues about the dynamics of our planet’s magnetic field.

The structure within Earth’s liquid core is found only at low latitudes and sits parallel to the equator. According to ANU seismologists, it has remained undetected until now.

The Earth has two core layers: the inner core, a solid layer, and the outer core, a liquid layer. Surrounding the Earth’s core is the mantle. The newly discovered doughnut-shaped region is at the top of Earth’s outer core, where the liquid core meets the mantle.

Study co-author and ANU geophysicist, Professor Hrvoje Tkalčić, said the seismic waves detected are slower in the newly discovered region than in the rest of the liquid outer core.

“The region sits parallel to the equatorial plane, is confined to the low latitudes and has a doughnut shape,” he said.

“We don’t know the exact thickness of the doughnut, but we inferred that it reaches a few hundred kilometres beneath the core-mantle boundary.”

Rather than using traditional seismic wave observation techniques and observing signals generated by earthquakes within the first hour, the ANU scientists analysed the similarities between waveforms many hours after the earthquake origin times, leading them to make the unique discovery.

“By understanding the geometry of the paths of the waves and how they traverse the outer core’s volume, we reconstructed their travel times through the Earth, demonstrating that the newly discovered region has low seismic speeds,” Professor Tkal?i? said.

“The peculiar structure remained hidden until now as previous studies collected data with less volumetric coverage of the outer core by observing waves that were typically confined within one hour after the origin times of large earthquakes.

“We were able to achieve much better volumetric coverage because we studied the reverberating waves for many hours after large earthquakes.”

Study co-author, Dr Xiaolong Ma, said that the discovery uncovers some mysteries of the dynamics of Earth’s magnetic field.

“There are still mysteries about the Earth’s outer core that are yet to be solved, which requires multidisciplinary efforts from seismology, mineral physics, geomagnetism and geodynamics,” Dr Ma said.

The outer core is predominantly made of liquid iron and nickel, and the vigorous movement of the electrically conductive liquid creates Earth’s magnetic field, which shields around Earth and helps to sustain all life, protecting it from damaging solar winds and harmful radiation.

The scientists believe that knowing more about the Earth’s outer core’s composition, including light chemical elements, is fundamental to understanding the magnetic field and predicting when it could potentially cease or weaken.

“Our findings are interesting because this low velocity within the liquid core implies that we have a high concentration of light chemical elements in these regions that would cause the seismic waves to slow down. These light elements, alongside temperature differences, help stir liquid in the outer core,” Professor Tkalčić said.

“The magnetic field is a fundamental ingredient that we need for life to be sustained on the surface of our planet.

“The dynamics of Earth’s magnetic field is an area of strong interest in the scientific community, so our results could promote more research about the magnetic field on both Earth and other planets.”

The research is published in Science Advances.

Reference:
Xiaolong Ma, Hrvoje Tkalčić. Seismic low-velocity equatorial torus in the Earth’s outer core: Evidence from the late–coda correlation wavefield. Science Advances, 2024; 10 (35) DOI: 10.1126/sciadv.adn5562

Note: The above post is reprinted from materials provided by Australian National University

New sauropod dinosaur from the Cretaceous discovered in the Iberian Peninsula

General view of the Lo Hueco site during the excavation of Qunkasaura in 2007. Credit: GBE-UNED
General view of the Lo Hueco site during the excavation of Qunkasaura in 2007. Credit: GBE-UNED

A new study led by Portuguese paleontologist Pedro Mocho, from the Instituto Dom Luiz of the Faculty of Sciences of the University of Lisbon (CIÊNCIAS), has just been published in Communications Biology. It announces a new species of sauropod dinosaur that lived in Cuenca, Spain, 75 million years ago: Qunkasaura pintiquiniestra.

The more than 12,000 fossils collected from 2007 onward during works to install the Madrid-Levante high-speed train (AVE) tracks revealed this deposit, giving rise to one of the most relevant collections of fossil vertebrates from the Upper Cretaceous of Europe.

The collection has been studied continuously thanks to national projects and the Junta de Comunidades de Castilla-La Mancha, which has made it possible to significantly increase our understanding of the ecosystems of southwestern Europe during the Late Cretaceous and also identify several new species for science.

“The study of this specimen allowed us to identify for the first time the presence of two distinct lineages of saltasauroids in the same fossil locality. One of these groups, called Lirainosaurinae, is relatively known in the Iberian region and is characterized by small and medium-sized species, which evolved in an island ecosystem.

“In other words, Europe was a huge archipelago made up of several islands during the Late Cretaceous. However, Qunkasaura belongs to another group of sauropods, represented in the Iberian Peninsula by medium-large species 73 million years ago.

“This suggests to us that this lineage arrived in the Iberian Peninsula much later than other groups of dinosaurs,” explains Mocho.

One of the most relevant features of the Lo Hueco fossil record is the abundance of large partial skeletons of sauropod dinosaurs, which are rare in the rest of Europe.

Qunkasaura pintiquiniestra stands out for being one of the most complete sauropod skeletons found in Europe, including cervical, dorsal and caudal vertebrae, part of the pelvic girdle and elements of the limbs. Their unique morphology, especially in the tail vertebrae, offers new insights into the non-avian dinosaurs of the Iberian Peninsula, a historically poorly understood group.

The study identifies Qunkasaura as a representative of the opisthocoelicaudine saltasaurids, a group present in the northern hemisphere (Laurasia). On the other hand, most Late Cretaceous sauropods from southwestern Europe, including Lohuecotitan pandafilandi, previously described from Lo Hueco, belong to the group Lirainosaurinae, a group of sauropods apparently exclusive to the European continent.

This study suggests that Lo Hueco is the only place where the coexistence of both groups is known and proposes a new group of titanosaurs called Lohuecosauria, which includes representatives of both lineages. Lohuecosaurs may have originated on the southern continents (Gondwana) before dispersing globally.

The name Qunkasaura pintiquiniestra is made up of several geographic and cultural references close to the Lo Hueco site. “Qunka” refers to the oldest etymology of the toponym from the Cuenca and Fuentes area, “Saura” alludes to the feminine of the Latin saurus (lizard), but also pays homage to the painter Antonio Saura, and “pintiquiniestra” refers to the giant “Queen Pintiquiniestra,” character from a novel mentioned in “Don Quijote de la Mancha’ by Cervantes.

“Fortunately, the Lo Hueco deposit also preserves several skeletons of sauropod dinosaurs to be determined, which may correspond to new species and which will help us understand how these animals evolved,” concludes Mocho.

The study is part of the research conducted by the Evolutionary Biology Group at UNED on ecosystems with dinosaurs in central Iberian Peninsula. Part of the skeleton of Qunkasaura is already on display in the Paleontological Museum of Castilla-La Mancha in Cuenca (Spain).

Reference:
Mocho, P, A Spanish saltasauroid titanosaur reveals Europe as a melting pot of endemic and immigrant sauropods in the Late Cretaceous, Communications Biology (2024). DOI: 10.1038/s42003-024-06653-0

Note: The above post is reprinted from materials provided by University of Lisbon.

Fungus gnat entombed in a 40-million-year-old piece of amber is a rare gem

Robsonomyia baltica sp. nov. (NHMD-300551): (A) male (holotype No NHMD-300551a); (B) amber piece with position of male; (C) female (paratype No NHMD-300551b); (D) female (paratype No NHMD-300551c); (E) amber piece with position of females. Credit: Scientific Reports (2024). DOI: 10.1038/s41598-024-59448-y
Robsonomyia baltica sp. nov. (NHMD-300551): (A) male (holotype No NHMD-300551a); (B) amber piece with position of male; (C) female (paratype No NHMD-300551b); (D) female (paratype No NHMD-300551c); (E) amber piece with position of females. Credit: Scientific Reports (2024). DOI: 10.1038/s41598-024-59448-y

A Danish amber collector’s find upon a wild North Sea shore in the 1960’s has proved to be of great and surprising significance. After having thoroughly examined the roughly 40-million-year-old piece of amber, University of Copenhagen researchers have discovered it to contain the first fossil of a predatory fungus gnat belonging to a rare genus. The research contributes new knowledge about the distribution of the gnat species and about biodiversity across space and time.

The research is published in the journal Scientific Reports.

Are you fed up with the summertime onslaught of fruit flies, gnats, mosquitoes and other tiny winged insects? If so, be happy that you weren’t around 40 million years ago. Back then, Europe’s climate was warmer and more humid, which provided favorable conditions for gnats, among other things.

One of these gnats, which met its end after being trapped in a lump of pine resin, has given researchers from the Natural History Museum of Denmark the opportunity to add a new prehistoric gnat species to its family of insects. This first fossil of a rare and never before studied species of gnat, Robsonomyia henningseni, was found in a piece of Baltic amber along Denmark’s North Sea coast in the 1960’s.

For decades, the piece had been tucked away in the museum’s 70,000-piece amber collection. Recently, it was retrieved from the drawers and subjected to a thorough examination by a team of Polish entomologists. The insect specialists were able to identify the gnat as an extinct species from a rare genus of predatory gnats. Today, living species of the genus are only found in Hokkaido, Japan and California.

“This is the first time that anyone has found a fossil gnat of this genus, which were only thought to live in Japan and North America. The finding demonstrates that this type of gnat was also widespread in Europe during past climates and gives us new knowledge about the gnat’s distribution on Earth,” explains Alicja Pełczyńska, a Ph.D. student at the University of Łódź and University of Copenhagen, who conducted the description of the gnat.

The researchers believe that the ancient gnat is a kind of “missing link” that connects its two rare and still living relatives in Japan and the United States. The overland distance between the living species has puzzled researchers, but the new fossil demonstrates that the species’ path may have traversed the European continent.

“Until now, the distribution of this genus of gnat has been strange, with many thousands of kilometers between species. Therefore, it makes sense to have found it in Europe, which is approximately halfway between Japan and North America,” says Pełczyńska.

C.V. Henningsen—Danish amber collector and gnat namesake

To learn more about the amber-entombed gnat, the researchers began by polishing the ocean and sun-matted amber piece until it was glossy and transparent.

Once transparent, they used an advanced camera and spectrometer to take a chemical fingerprint of the amber. This confirmed that the piece is from Baltic amber. Thereafter, they examined the fossil and determined the species of insect. This part of the process took place by closely studying the males’ genitalia, where identifying characteristics often vary.

“Insects mate end to end, which places certain demands on their genitalia. The male has appendages, or forceps, next to the actual penis, which it uses to grasp the female gnat with while mating. We used the shape of these forceps to identify it,” explains Lars Vilhelmsen, an associate professor and curator at the Natural History Museum of Denmark.

Based on the analysis, the researchers estimate that the gnat buzzed about in the enormous pine forests of what we now know as Scandinavia some 35–40 million years ago. Here, the gnat became trapped in a lump of resin upon a tree, which rivers, ocean currents and glaciers of the last ice age carried to the North Sea.

“An amber collector by the name of C.V. Henningsen found the piece of amber on the western coast of Jutland back in the 1960’s. Henningsen sold the piece, along with the rest of his collection, to the Natural History Museum of Denmark. Since the gnat species had never been described before, we named it after him, and it is now known as Robsonomyia henningseni,” says Vilhelmsen.

Unlike in Jurassic Park, there’s no DNA

Amber is an outstanding natural time capsule for scientists. With its protective lamination, it preserves ancient insects and plant remains and lets us learn about what Earth looked like up to 230 million years ago. But if released from its amber encasing, the insect will disappear.

According to Vilhelmsen, there is no blood or DNA to suck out of the gnats so as to reanimate them in any way, as is done in the Jurassic Park films.

“Virtually all of the organic material in the gnat has long since decomposed, making it a hollow shell. If one tries to remove it from the amber, it crumbles. As such, the best thing we can do is to study it inside the amber. Insects trapped in amber can be studied almost as precisely as their living relatives using microCT scans,” explains Vilhelmsen.

The new discovery of the gnat fossil equips researchers with new knowledge about the general migrations of gnats across Earth and contributes to the larger picture of biodiversity through time.

Reference:
Alicja Pełczyńska et al, Eocene amber provides the first fossil record and bridges distributional gap in the rare genus Robsonomyia (Diptera: Keroplatidae), Scientific Reports (2024). DOI: 10.1038/s41598-024-59448-y

Note: The above post is reprinted from materials provided by University of Copenhagen.

Plant-eating dinosaurs evolved backup teeth to eat tough food, research reveals

The teeth of Iguanodon weren't as adapted for chewing, and formed much more slowly, than those of their later relatives. Credit: The Trustees of the Natural History Museum, London
The teeth of Iguanodon weren’t as adapted for chewing, and formed much more slowly, than those of their later relatives. Credit: The Trustees of the Natural History Museum, London

At the end of the Cretaceous, the duck-billed hadrosaurs were the most advanced herbivores on Earth. New research has revealed just how voracious these dinosaurs were, with their average tooth worn away in less than two months as they consumed enormous amounts of plants. Some of Earth’s most successful herbivores may have had hundreds of thousands of teeth in their lifetime.

The ornithopods are a group of dinosaurs that include Iguanodon, Hypsilophodon and their relatives, including the rare rhabdodontids. Ornithopods first appeared in the Middle Jurassic but were most prominent in the Cretaceous, when they became the dominant herbivores across large parts of the world.

This journey took them from small generalists to becoming large and specialized “plant-eating machines” which rival modern cows and sheep. The research, led by Dr. Attila Ősi from Eötvös Loránd University in Hungary, shows that the dinosaurs achieved this following the evolution of vast numbers of replacement teeth, which allowed them to eat even the toughest of plants in large quantities.

“The teeth and jaws of the ornithopods changed drastically during their evolution,” Attila says. “Earlier members of the group, like Iguanodon, took more than 200 days to form their teeth and at least that long to wear them down by chewing. But by the end of the Cretaceous, hadrosaurs would wear through their teeth in as little as 50 days.”

“We think this is because the later ornithopods must have been feeding on tough plants that rapidly eroded their teeth. As they wore away at a huge rate, these dinosaurs would have needed to build up banks of teeth in their skulls to stop themselves from starving.”

The findings of the study are published in the journal Nature Communications.

Becoming the top dinosaur herbivores

While herbivory is one of the most common ways of life for animals, it’s surprisingly difficult to eat plants. Unlike meat, which is easily broken down in the gut, plants are generally made up of tough fibers and complex carbohydrates which are hard to digest.

Teeth are on the front line of this dietary battle, breaking open plants and cutting them into smaller pieces so that gut bacteria can break them down more efficiently. However, as co-author Professor Paul Barrett explains, this takes its toll on the teeth.

“Across a herbivore’s life, its teeth gradually wear down,” Paul says. “This puts an upper limit on the life of some mammals, like elephants or cows. Once their teeth are gone, the animal can no longer feed, and so it dies.”

“This isn’t a problem for reptiles. They are able to continually make new teeth, with a replacement ready to surface from beneath as soon as its predecessor wears out. As a result, dinosaur teeth are common fossils, making them a valuable way to investigate how these animals evolved.”

The team were particularly interested in investigating the teeth and jaws of the ornithopods, which eventually became some of the most advanced herbivores to have ever lived on our planet. By examining well-preserved skulls, they were able to track how the dinosaurs’ skulls developed into increasingly complex forms that were better suited to eating plants.

“We can see a sequential increase in the complexity of their adaptations for herbivory as they evolve,” Paul explains. “At the start, they had single rows of fairly simple teeth with limited wear, probably because these dinosaurs focused on fruits and softer plants.”

“By the time the hadrosaurs evolved, they had vastly more teeth which developed a large blade-like edge on one side and a series of ridges behind it. This structure is unique to these dinosaurs, and kept the upper and lower teeth sharp as they ground against each other.”

Later ornithopods also moved their jaws in new ways, being able to slide them back and forth and side to side, allowing them to grind plants down even further. Their bodies also grew much bigger, allowing them to accommodate larger guts that can more effectively release the nutrients inside plants.

Different dinosaurs took different approaches to herbivory. But the team noticed that a few groups of ornithopods, like the tenontosaurids and their more advanced iguanodontian relatives, all follow a strikingly similar evolutionary path. They believe this is an example of convergent evolution.

“About 110 million years ago, these ornithopods rapidly evolved a series of similar characteristics,” Paul explains. “Their teeth increase in number, their jaws interlock more tightly and they build up more replacement teeth, making them more effective herbivores.”

“We also see this happen in the horned dinosaurs, which include species like Triceratops. It’s tempting to speculate that these changes happened for similar reasons.”

Could flowers be responsible?

While the evidence that the environment changed in the Early Cretaceous is strong, finding out exactly what happened is challenging. To try and reveal potential causes, the team examined worn areas of dinosaur teeth, known as wear facets, for signs of microscopic changes.

“Before the Early Cretaceous, ornithopod teeth had a lot of large pits,” Attila says. “This suggests that they were eating a large amount of plant seeds, as well as potentially consuming a lot of dust and soil by feeding close to the ground.”

“Later forms have fewer pits, with many more scratches instead. This suggests that they were now eating harder plants, or feeding in a different way.”

Rather than the dinosaurs actively changing what they ate, one possible explanation could be that certain plants became more common. It’s possible that the rise of flowers could be responsible, but it doesn’t quite fit the available evidence.

“While it is suspicious that the flowering plants start to diversify around this time, they were still pretty uncommon at the time,” Paul says. “In fact, until the Late Cretaceous, horsetails, ferns and conifers would be much more common for dinosaurs looking for something to eat.”

“As it’s very difficult to disentangle the plant and dinosaur fossil records, it’s unlikely we’ll ever have enough detailed evidence to prove there is a link, even if it is a very interesting idea.”

Having finished their work on the ornithopods, the team hope to gradually widen their research to other herbivorous dinosaurs, like the ankylosaurs or the horned dinosaurs. This could give us a better idea of why these reptiles were so successful, and how evolution shaped the diet of the different groups.

“We’d like to be able to sample other dinosaurs to see if the trend of increasing body size, tooth number and the change in teeth wear we found in the ornithopods is more widespread,” Attila says. “If we can find out what changes herbivores were going through at the time, it will give us a much better chance of understanding the place of these dinosaurs in the ecosystems of the Mesozoic Era.”

Reference:
Attila Ősi et al, Trophic evolution in ornithopod dinosaurs revealed by dental wear, Nature Communications (2024). DOI: 10.1038/s41467-024-51697-9

Note: The above post is reprinted from materials provided by Natural History Museum.

Some Pterosaurs Would Flap, Others Would Soar

Inabtanin alarabia, left, and Arambourgiania philadelphiae, right. With flying styles also demonstrated. ©Terryl Whitlatch
Inabtanin alarabia, left, and Arambourgiania philadelphiae, right. With flying styles also demonstrated. ©Terryl Whitlatch

Some species of pterosaurs flew by flapping their wings while others soared like vultures, demonstrates a new study published in the peer-reviewed Journal of Vertebrate Paleontology.

It has long been debated whether the largest pterosaurs could fly at all.

However, “remarkable” and “rare” three-dimensional fossils of two different large-bodied azhdarchoid pterosaur species — including one new-to-science — have enabled scientists to hypothesize that not only could the largest pterosaurs take to the air, but their flight styles could differ too.

The new findings are led by experts from the University of Michigan, in the US, the Natural Resources Authority and Yarmouk University, in Jordan, and the Saudi Geological Survey, in Saudi Arabia.

Their paper details how these fossils — which date back to the latest Cretaceous period (approximately 72 to 66 million years ago) — were remarkably three-dimensionally preserved within the two different sites that preserve a nearshore environment on the margin of Afro-Arabia, an ancient landmass that included both Africa and the Arabian Peninsula. The research team used high-resolution computed tomography (CT) scans to then analyze the internal structure of the wing bones.

“The dig team was extremely surprised to find three-dimensionally preserved pterosaur bones, this is a very rare occurrence,” explains lead author Dr Kierstin Rosenbach, from the Department of Earth and Environmental Sciences of the University of Michigan.

“Since pterosaur bones are hollow, they are very fragile and are more likely to be found flattened like a pancake, if they are preserved at all.

“With 3D preservation being so rare, we do not have a lot of information about what pterosaur bones look like on the inside, so I wanted to CT scan them.

“It was entirely possible that nothing was preserved inside, or that CT scanners were not sensitive enough to differentiate fossil bone tissue from the surrounding matrix.”

Luckily, though, what the team uncovered was “remarkable,” via “exciting internal structures not only preserved, but visible in the CT scanner.”

CT scans reveal one soars; one flaps!

Newly collected specimens of the already-known giant pterosaur, Arambourgiania philadelphiae, confirm its 10-meter wingspan and provide the first details of its bone structure. CT images revealed that the interior of its humerus, which is hollow, contains a series of ridges that spiral up and down the bone.

This resembles structures in the interior of wing bones of vultures. The spiral ridges are hypothesized to resist the torsional loadings associated with soaring (sustained powered flight that requires launch and maintenance flapping).

The other specimen analyzed was the new-to-science Inabtanin alarabia, which had a five-meter wingspan. The team named it after the place where it was excavated — near a large grape-colored hill, called Tal Inab. The generic name combines the Arabic words “inab,” for grape, and “tanin” for dragon. ‘Alarabia’ refers to the Arabian Peninsula.

Inabtanin is one of the most complete pterosaurs ever recovered from Afro-Arabia, and the CT scans revealed the structure of its flight bones was completely different from that of Arambourgiania.

The interior of the flight bones were crisscrossed by arrangement with struts that match those found in the wing bones of modern flapping birds.

This indicates it was adapted to resist bending loads associated with flapping flight, and so it is likely that Inabtanin flew this way — although this does not preclude occasional use of other flight styles too.

“The struts found in Inabtanin were cool to see, though not unusual,” says Dr Rosenbach.

“The ridges in Arambourgiania were completely unexpected, we weren’t sure what we were seeing at first!

“Being able to see the full 3D model of Arambourgiania’s humerus lined with helical ridges was just so exciting.”

What explains this difference?

The discovery of diverse flight styles in differently-sized pterosaurs is “exciting,” the experts state, because it opens a window into how these animals lived. It also poses interesting questions, like to what extent flight style is correlated with body size and which flight style is more common among pterosaurs.

“There is such limited information on the internal bone structure of pterosaurs across time, it is difficult to say with certainty which flight style came first,” Dr Rosenbach adds.

“If we look to other flying vertebrate groups, birds and bats, we can see that flapping is by far the most common flight behavior.

“Even birds that soar or glide require some flapping to get in the air and maintain flight.

“This leads me to believe that flapping flight is the default condition, and that the behavior of soaring would perhaps evolve later if it were advantageous for the pterosaur population in a specific environment; in this case the open ocean.”

Co-author Professor Jeff Wilson Mantilla, Curator at Michigan’s Museum of Paleontology, and Dr Iyad Zalmout, from the Saudi Geological Survey, found these specimens in 2007 at sites in the north and south of Jordan.

Professor Jeff Wilson Mantilla says the “variations likely reflect responses to mechanical forces applied on the pterosaurs’ wings during flight.”

Enabling further study of vertebrate flight

Concluding, Dr Rosenbach states: “Pterosaurs were the earliest and largest vertebrates to evolve powered flight, but they are the only major volant group that has gone extinct.

“Attempts to-date to understand their flight mechanics have relied on aerodynamic principles and analogy with extant birds and bats.

“This study provides a framework for further investigation of the correlation between internal bone structure and flight capacity and behavior, and will hopefully lead to broader sampling of flight bone structure in pterosaur specimens.”

Journal Reference:
Kierstin L. Rosenbach, Danielle M. Goodvin, Mohammed G. Albshysh, Hassan A. Azzam, Ahmad A. Smadi, Hakam A. Mustafa, Iyad S. A. Zalmout, Jeffrey A. Wilson Mantilla. New pterosaur remains from the Late Cretaceous of Afro-Arabia provide insight into flight capacity of large pterosaurs. Journal of Vertebrate Paleontology, 2024; DOI: 10.1080/02724634.2024.2385068

Note: The above post is reprinted from materials provided by Taylor & Francis Group.

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