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‘Cold bone’: Researchers discover first dinosaur species that lived on Greenland 214 million years ago

Living reconstruction of Issi saaneq / Photo: Victor Beccari
Living reconstruction of Issi saaneq / Photo: Victor Beccari

The two-legged dinosaur Issi saaneq lived about 214 million years ago in what is now Greenland. It was a medium-sized, long-necked herbivore and a predecessor of the sauropods, the largest land animals ever to live. It was discovered by an international team of researchers from Portugal, Denmark and Germany, including the Martin Luther University Halle-Wittenberg (MLU). The name of the new dinosaur pays tribute to Greenland’s Inuit language and means “cold bone.” The team reports on its discovery in the journal Diversity.

The initial remains of the dinosaur — two well-preserved skulls — were first unearthed in 1994 during an excavation in East Greenland by palaeontologists from Harvard University. One of the specimens was originally thought to be from a Plateosaurus, a well-known long-necked dinosaur that lived in Germany, France and Switzerland during the Triassic Period. Only a few finds from East Greenland have been prepared and thoroughly documented. “It is exciting to discover a close relative of the well-known Plateosaurus, hundreds of which have already been found here in Germany,” says co-author Dr Oliver Wings from MLU.

The team performed a micro-CT scan of the bones, which enabled them to create digital 3D models of the internal structures and the bones still covered by sediment. “The anatomy of the two skulls is unique in many respects, for example in the shape and proportions of the bones. These specimens certainly belong to a new species,” says lead author Victor Beccari, who carried out the analyses at NOVA University Lisbon.

The plant-eating dinosaur Issi saaneq lived around 214 million years ago during the Late Triassic Period. It was at this time that the supercontinent Pangaea broke apart and the Atlantic Ocean began forming. “At the time, the Earth was experiencing climate changes that enabled the first plant-eating dinosaurs to reach Europe and beyond,” explains Professor Lars Clemmensen from the University of Copenhagen.

The two skulls of the new species come from a juvenile and an almost adult individual. Apart from the size, the differences in bone structure are minor and only relate to proportions. The new Greenlandic dinosaur differs from all other sauropodomorphs discovered so far, however it does have similarities with dinosaurs found in Brazil, such as the Macrocollum and Unaysaurus, which are almost 15 million years older. Together with the Plateosaurus from Germany, they form the group of plateosaurids: relatively graceful bipeds that reached lengths of 3 to 10 metres.

The new findings are the first evidence of a distinct Greenlandic dinosaur species, which not only adds to the diverse range of dinosaurs from the Late Triassic (235-201 million years ago) but also allows us to better understand the evolutionary pathways and timeline of the iconic group of sauropods that inhabited the Earth for nearly 150 million years.

Once the scientific work is completed, the fossils will be transferred to the Natural History Museum of Denmark.

Reference:
Victor Beccari, Octávio Mateus, Oliver Wings, Jesper Milàn, Lars B. Clemmensen. Issi saaneq gen. et sp. nov.—A New Sauropodomorph Dinosaur from the Late Triassic (Norian) of Jameson Land, Central East Greenland. Diversity, 2021; 13 (11): 561 DOI: 10.3390/d13110561

Note: The above post is reprinted from materials provided by Martin-Luther-Universität Halle-Wittenberg.

Humans hastened the extinction of the woolly mammoth

Woolly mammoth illustration Mauricio Antón © 2008 Public Library of Science
Woolly mammoth illustration Mauricio Antón © 2008 Public Library of Science

New research shows that humans had a significant role in the extinction of woolly mammoths in Eurasia, occurring thousands of years later than previously thought.

An international team of scientists led by researchers from the University of Adelaide and University of Copenhagen, has revealed a 20,000-year pathway to extinction for the woolly mammoth.

“Our research shows that humans were a crucial and chronic driver of population declines of woolly mammoths, having an essential role in the timing and location of their extinction,” said lead author Associate Professor Damien Fordham from the University of Adelaide’s Environment Institute.

“Using computer models, fossils and ancient DNA we have identified the very mechanisms and threats that were integral in the initial decline and later extinction of the woolly mammoth.”

Signatures of past changes in the distribution and demography of woolly mammoths identified from fossils and ancient DNA show that people hastened the extinction of woolly mammoths by up to 4,000 years in some regions.

“We know that humans exploited woolly mammoths for meat, skins, bones and ivory. However, until now it has been difficult to disentangle the exact roles that climate warming and human hunting had on its extinction,” said Associate Professor Fordham.

The study also shows that woolly mammoths are likely to have survived in the Arctic for thousands of years longer than previously thought, existing in small areas of habitat with suitable climatic conditions and low densities of humans.

“Our finding of long-term persistence in Eurasia independently confirms recently published environmental DNA evidence that shows that woolly mammoths were roaming around Siberia 5,000 years ago,” said Associate Professor Jeremey Austin from the University of Adelaide’s Australian Centre for Ancient DNA.

Associate Professor David Nogues-Bravo from the University of Copenhagen was a co-author of the study which is published in the journal Ecology Letters.

“Our analyses strengthens and better resolves the case for human impacts as a driver of population declines and range collapses of megafauna in Eurasia during the late Pleistocene,” he said.

“It also refutes a prevalent theory that climate change alone decimated woolly mammoth populations and that the role of humans was limited to hunters delivering the coup de grâce”.

“And shows that species extinctions are usually the result of complex interactions between threatening processes.”

The researchers emphasise that the pathway to extinction for the woolly mammoth was long and lasting, starting many millennia before the final extinction event.

Reference:
Damien A. Fordham, Stuart C. Brown, H. Reşit Akçakaya, Barry W. Brook, Sean Haythorne, Andrea Manica, Kevin T. Shoemaker, Jeremy J. Austin, Benjamin Blonder, Julia Pilowsky, Carsten Rahbek, David Nogues‐Bravo. Process‐explicit models reveal pathway to extinction for woolly mammoth using pattern‐oriented validation. Ecology Letters, 2021; DOI: 10.1111/ele.13911

Note: The above post is reprinted from materials provided by University of Adelaide. Original written by Crispin Savage.

Tooth Fast, Tooth Curious?

 Long neck, long tail, tiny head, tiny teeth. These iconic, gargantuan dinosaurs developed a wholly unique dining strategy to support their massive size. Image by Stephanie Abramowicz, courtesy of the Natural History Museum of Los Angeles County (NHM).
Long neck, long tail, tiny head, tiny teeth. These iconic, gargantuan dinosaurs developed a wholly unique dining strategy to support their massive size. Image by Stephanie Abramowicz, courtesy of the Natural History Museum of Los Angeles County (NHM).

How did the largest animals to ever walk the Earth dominate their environments? By doing something totally revolutionary: keeping it simple. Published in BMC Ecology and Evolution, a new study led by Postdoctoral Research Scientist and periodic dinosaur dentist Dr. Keegan Melstrom at the Natural History Museum of Los Angeles County’s Dinosaur Institute ??reveals that colossal sauropod dinosaurs, the largest animals to ever walk the Earth, had a strategy for dining on plants unique to long-necked dinosaurs: linking tooth complexity to how fast teeth were replaced.

“In nearly every other animal we look at, the complexity of a tooth relates to the animal’s diet,” says Dr. Melstrom. “Carnivores have simple teeth, herbivores have complex teeth, often with distinct ridges, crests, and cusps for processing plant material. But sauropods break this incredibly consistent pattern. Instead, these dinosaurs link complexity to tooth replacement rate, with simple teeth being replaced every few weeks!”

The shapes of an animal’s teeth are thought to reveal a lot about its diet and by extension its lifestyle. The banana-sized knives ringing the mouths of T. Rex are perfect for ripping flesh, and deadly simple sharp teeth abound in living and extinct carnivores. Typically, herbivores have extremely complex teeth: perfect for grinding down fibrous leaves or grasses. When it comes to the largest animals to ever walk the Earth, sauropods chewed their own path. Unlike any other plant-eating animals living or extinct, sauropods rely on quickly replacing their teeth to keep the salad flowing.

Keep It Simple, Sauropods

“The diet of extinct dinosaurs was incredibly varied, spanning tiny meat-eaters to massive plant-eaters,” says Dr. Melstrom. “Our research sheds light on the range of adaptations that allowed so many plant-eaters to live alongside one another.”

Using computerized tomography (CT) and microCT scanning, Dr. Melstrom and his colleagues made 3D models of specimens from around the globe, capturing the great diversity of tooth complexity in Late Jurassic dinosaurs.

“This whole project was conducted during the pandemic. Instead of traveling the world to gather data, we relied on researchers who had made their data available to other scientists, as well as the incredible collections here at NHM. I think this project really demonstrates the importance of sharing information, it can lead to new discoveries even during a pandemic,” says Dr. Melstrom.

They converted the toothy hills and valleys of dinosaur teeth into numbers, quantifying tooth complexity between the three groups of dinosaurs: meat-eating theropods, plant-eating ornithischians, and similarly herbivorous sauropods.

What they found was an entirely new evolutionary strategy to handle a plant-based diet 150 million years ago. While meat-eating dinosaurs had sharp simple teeth expected for carnivores, and ornithischians had the more complex teeth similar to herbivores living today, sauropods had very simple teeth, unlike any other known herbivores extinct or living.

In sauropods, they found that the more complex the tooth, the more slowly teeth were replaced, a correlation that demonstrates that tooth replacement rate is related to tooth complexity, unlike any other known animals. More specifically, diplodocoids like Apatosaurus and Diplodocus exhibited incredibly fast replacement rates and simple teeth, possibly allowing them to eat different foods from the other group of sauropods, macronarians like ??Brachiosaurus, which had more complex teeth.

Simple teeth would have made sense for sauropods’ long necks. Smaller teeth built to be lost weigh less than the tougher teeth of all other herbivores, which helps lighten the skull at the end of those long necks. The peculiar tooth replacement pattern meant these sauropods could focus on plant food other dinosaurs and non-dinosaur plant-eaters passed by.

“Time and time again, the fossil record shows us that there isn’t one solution to evolutionary problems. For sauropods, when it comes to eating tough plants, the simplest solution was the best,” says Dr. Melstrom.

Reference:
Keegan M. Melstrom, Luis M. Chiappe, Nathan D. Smith. Exceptionally simple, rapidly replaced teeth in sauropod dinosaurs demonstrate a novel evolutionary strategy for herbivory in Late Jurassic ecosystems. BMC Ecology and Evolution, 2021; 21 (1) DOI: 10.1186/s12862-021-01932-4

Note: The above post is reprinted from materials provided by Natural History Museum of Los Angeles County.

New species of iguanodontian dinosaur discovered from Isle of Wight

Brighstoneus simmondsi reconstruction. Credit: John Sibbick
Brighstoneus simmondsi reconstruction. Credit: John Sibbick

Scientists from the Natural History Museum and University of Portsmouth have described a new genus and species of dinosaur from a specimen found on the Isle of Wight.

Following on from a new species of ankylosaur, new species of therapodand two new speciesof spinosaur dinosaurs, Brighstoneus simmondsi is the latest in a host of new dinosaur species described by Museum scientists in recent weeks.

The new dinosaur is an iguanodontian, a group that also includes the iconic Iguanodon and Mantellisaurus. Until now, iguanodontian material found from the Wealden Group (representing part of the Early Cretaceous period) on the Isle of Wight has usually been referred to as one of these two dinosaurs — with more gracile fossil bones assigned to Mantellisaurus and the larger and more robust material assigned to Iguanodon.

However, when Dr Jeremy Lockwood — a PhD student at the Museum and University of Portsmouth — was examining the specimen, he came across several unique traits that distinguished it from either of these other dinosaurs.

‘For me, the number of teeth was a sign’ Dr Lockwood says. ‘Mantellisaurus has 23 or 24, but this has 28. It also had a bulbous nose, whereas the other species have very straight noses. Altogether, these and other small differences made it very obviously a new species.’

The herbivorous dinosaur was about eight metres in length and weighed about 900kg. Published in the peer-reviewed Journal of Systematic Palaeontology, Dr Lockwood describes the species and names it Brighstoneus simmondsi: Brighstoneus after the village of Brighstone, near to the excavation site, and simmondsi honouring Mr Keith Simmonds, who made the discovery of the specimen in 1978.

The discovery of this new species suggests that there were far more iguanodontian dinosaurs in the Early Cretaceous of the UK than previously thought, and that simply assigning specimens from this period to either Iguanodon or Mantellisaurus must change.

‘We’re looking at six, maybe seven million years of deposits, and I think the genus lengths have been overestimated in the past, ‘says Dr Lockwood. ‘If that’s the case on the island, we could be seeing many more new species. It seems so unlikely to just have two animals being exactly the same for millions of years without change.’

Museum scientist Dr Susannah Maidment, a co-author of the paper, says: ‘The describing of this new species shows that there is clearly a greater diversity of iguanodontian dinosaurs in the Early Cretaceous of the UK than previously realised. It’s also showing that the century-old paradigm that gracile iguanodontian bones found on the island belong to Mantellisaurus and large elements belong to Iguanodon can no longer be substantiated’.

The Isle of Wight has long been associated with dinosaur discovery, and even yielded the crucial specimens that led to Sir Richard Owen to coin the term Dinosauria. The authors conclude that the describing of Brighstoneus simmondsi as a new species calls for a reassessment of Isle of Wight material:

‘British dinosaurs are certainly not something that’s done and dusted at all,’ says Dr Lockwood. ‘I think we could be on to a bit of a renaissance.’

Reference:
Jeremy A. F. Lockwood, David M. Martill, Susannah C. R. Maidment. A new hadrosauriform dinosaur from the Wessex Formation, Wealden Group (Early Cretaceous), of the Isle of Wight, southern England. Journal of Systematic Palaeontology, 2021; 1 DOI: 10.1080/14772019.2021.1978005

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

Rapidly evolving species more likely to go extinct, study suggests

Pleurosaurus from the Late Jurassic, some 150 million years ago, of southern Germany, a remarkable, long-bodied swimming rhynchocephalian.
Pleurosaurus from the Late Jurassic, some 150 million years ago, of southern Germany, a remarkable, long-bodied swimming rhynchocephalian.

In a new study of lizards and their relatives, Dr Jorge Herrera-Flores of Bristol’s School of Earth Sciences and colleagues have discovered that ‘slow and steady wins the race’.

The team studied lizards, snakes and their relatives, a group called the Lepidosauria. Today there are more than 10,000 species of lepidosaurs, and much of their recent success is a result of fast evolution in favourable circumstances. But this was not always the case.

Mr Herrera-Flores explained: “Lepidosaurs originated 250 million years ago in the early Mesozoic Era, and they split into two major groups, the squamates on the one hand, leading to modern lizards and snakes, and the rhynchocephalians on the other, represented today by a single species, the tuatara of New Zealand. We expected to find slow evolution in rhynchocephalians, and fast evolution in squamates. But we found the opposite.”

“We looked at the rate of change in body size among these early reptiles,” said Dr Tom Stubbs, a collaborator. “We found that some groups of squamates evolved fast in the Mesozoic, especially those with specialised lifestyles like the marine mosasaurs. But rhynchocephalians were much more consistently fast-evolving.”

“In fact, their average rates of evolution were significantly faster than those for squamates, about twice the background rate of evolution, and we really did not expect this,” said Dr Armin Elsler, another collaborator. “In the later part of the Mesozoic all the modern groups of lizards and snakes originated and began to diversify, living side-by-side with the dinosaurs, but probably not engaging with them ecologically. These early lizards were feeding on bugs, worms, and plants, but they were mainly quite small.”

Prof Mike Benton added: “‘After the extinction of the dinosaurs, 66 million years ago, at the end of the Mesozoic, the rhynchocephalians and squamates suffered a lot, but the squamates bounced back. But for most of the Mesozoic, the rhynchocephalians were the innovators and the fast evolvers. They tailed off quite severely well before the end of the Mesozoic, and the whole dynamic changed after that.”

This work confirms a challenging proposal made by the famous palaeontologist George Gaylord Simpson in his 1944 book Tempo and Mode in Evolution. He looked at the fundamental patterns of evolution in a framework of Darwinian evolution and observed that many fast-evolving species belonged to unstable groups, which were potentially adapting to rapidly changing environments.

Prof Benton continued: “Slow and steady wins the race. In the classic Aesop’s fable, the speedy hare loses the race, whereas the slow-moving tortoise crosses the finishing line first. Since the days of Darwin, biologists have debated whether evolution is more like the hare or the tortoise. Is it the case that big groups of many species are the result of fast evolution over a short time or slow evolution over a long time?

“In some cases, they can stabilise and survive well, but in many cases the species go extinct as fast as new ones emerge, and they can go extinct, just like the napping hare. On the other hand, Simpson predicted that slowly evolving species might also be slow to go extinct, and could in the end be successful in the longer term, just like the slow-moving but persistent tortoise in the fable.”

Reference:
Jorge A. Herrera-Flores, Armin Elsler, Thomas L. Stubbs, Michael J. Benton. Slow and fast evolutionary rates in the history of lepidosaurs. Paleontology, 10 November 2021 DOI: 10.1111/pala.12579

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

Muscular wing-body junction improved Pterosaur flight performance

Laser-stimulated fluorescence imaging of a pterosaur fossil reveals flight-related soft tissues. The imaging revealed a muscular wing root fairing that smooths airflow around the wing-body junction and reduces drag, as in the wing root fairings of modern aeroplanes. (Image credit: Michael Pittman)
Laser-stimulated fluorescence imaging of a pterosaur fossil reveals flight-related soft tissues. The imaging revealed a muscular wing root fairing that smooths airflow around the wing-body junction and reduces drag, as in the wing root fairings of modern aeroplanes. (Image credit: Michael Pittman)

The flying reptiles known as pterosaurs are the closest relatives of dinosaurs and were the first vertebrates to evolve powered flight. However, many details of pterosaur flight anatomy and performance are still unclear. According to a new study led by Dr Michael Pittman — Research Assistant Professor of the Department of Earth Sciences & Vertebrate Palaeontology Laboratory, The University of Hong Kong (HKU); Assistant Dean (e-learning) of HKU Faculty of Science — pterosaurs evolved a muscular wing-body junction to reduce drag and improve flight performance. The findings were recently published in the Proceedings of the National Academy of Sciences (PNAS).

Dr Pittman and colleagues used laser-stimulated fluorescence to image the bones and reveal soft tissues of a Late Jurassic pterodactyloid pterosaur fossil to analyse its flight performance. This involved scanning the fossil with a violet laser and taking long-exposure photographs of the fluorescence produced by the pterosaur’s bones and revealed soft tissues. Their results suggest that the pterosaur possessed a wing root fairing, a feature that smooths the airflow around the wing-body junction and reduces drag, as in the wing root fairings of most modern aeroplanes. “In birds, the wing root fairing is made of feathers. In bats, the wing root fairing is made of fur. In contrast, pterosaurs had a wing root fairing primarily made of skeletal muscle,” notes Mr Luke A. Barlow, a Research Assistant in Dr Pittman’s lab that studied the specimen.

Dr Pittman said, “This muscular wing root fairing appears to have provided pterosaurs with additional flight benefits, such as improved force generation during the flight stroke and sophisticated control of the wing’s shape, including minimising unwanted vibrations or ‘flutter’.” Speaking of the significance of the study, Mr Thomas G Kaye, a study co-author and Director of the Foundation of Scientific Advancement in the United States added, “Our work shows that pterosaurs were more advanced flyers than we thought, even in the Late Jurassic when birds had just evolved flight. Our study also highlights the potential contributions of new technologies to our understanding of pterosaur flight anatomy and evolution. We are excited to see where our work takes us next.”

Reference:
Michael Pittman, Luke A. Barlow, Thomas G. Kaye, Michael B. Habib. Pterosaurs evolved a muscular wing–body junction providing multifaceted flight performance benefits: Advanced aerodynamic smoothing, sophisticated wing root control, and wing force generation. Proceedings of the National Academy of Sciences, 2021; 118 (44): e2107631118 DOI: 10.1073/pnas.2107631118

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

Crushed resistance: Tectonic plate sinking into a subduction zone

The model offers new insights into how the plate subducted under Japan breaks into segments by bending and thereby crushing olivine grains on its underside. (Graphic: Taras Gerya / ETH Zurich)
The model offers new insights into how the plate subducted under Japan breaks into segments by bending and thereby crushing olivine grains on its underside. (Graphic: Taras Gerya / ETH Zurich)

The Earth’s surface consists of a few large plates and numerous smaller ones that are continuously moving either away from or towards each other at an extremely slow pace. At the boundaries of two plates, the heavier oceanic plate sinks below the lighter continental plate in a process that experts call subduction. For a long time, though, those experts have been puzzling over what happens to the plate margin that dives into the Earth’s mantle, known as the subducting slab. Some scientists assumed that the slab remains as rigid and strong as the plate itself and simply bends due to the gravity force and mechanical interaction with the Earth’s mantle.

Heavily deformed plate margin

However, models of the Earth’s interior constructed by scientists using seismic tomography revealed contradictory results: in the western United States, for example, the researchers observed anomalies at different depths on their tomographic images. These indicated that the slabs submerged beneath the Americas may be segmented. The scientists therefore concluded that the slabs in the mantle must be strongly deformed and are by no means rigid and immobile.

With the aid of computer models, other researchers, including ETH Professor Paul Tackley, confirmed that subducted slabs are indeed weak and deformable. And they formulated the subduction dichotomy hypothesis that can be expressed in simple terms: plates on the surface are rigid and strong (read: non-deformable), while the slabs in the mantle are soft and weak.

Seeking a plausible mechanism

“Until now, however, research has lacked a plausible mechanism to explain how this bending occurs and why sinking plate margins (slabs) become soft and weak,” says Taras Gerya, Professor of Geophysics at ETH Zurich.

Observations revealed that numerous faults are found on the upper surface of a sinking plate where it meets the other plate. Seawater penetrates the plate through these faults and is in fact literally sucked in by suction forces. This weakens the plate on its upper side.

Yet this alone is not sufficient to explain the segmentation of the slab — the anomalies observed on tomographic images. Another mechanism must also be at work to weaken the underside of the margin enough for segmentation to occur.

Gerya and his American colleagues David Bercovici and Thorsten Becker therefore suspected that compression of the underside of the plate at the point where it bends downward was “crushing” large and strong, millimetres size olivine crystals in the plate by forcing them to recrystallise into much weaker, micrometres size granular aggregate — thereby reducing the plate’s resistance and allowing it to bend.

Sinking plate margin divided into segments

Using a new two-dimensional computer model that integrated this grain reduction as a central mechanism, the three researchers then studied the process in silico. Their study was recently published in the journal Nature.

And indeed, the simulations revealed that sinking plates deform due to the massive reduction of olivine grains on their undersides, splitting into individual segments over time. These segments are rigid and stiff, but remain connected to each other by weak hinges made of ground grains.

In the simulations, parallel cracks appear at the segment boundaries on the plate’s upper surface. Below these cracks are the zones with “crushed” mineral grains.

“Just imagine you’re breaking a bar of chocolate,” Gerya says with a grin. A bar of chocolate, too, can be divided into segments only along the specified weak points. The squares of chocolate are rigid, but the connecting pieces between them are weak. “That’s why a sinking plate isn’t uniformly bent or deformed, but segmented.”

And here’s how it might play out in reality: The heavier plate sinks under the lighter one. A weak spot with smaller mineral grains within the sinking plate allows it to bend. The bending stress causes the minerals to crumble in more places on the underside. The resulting weakness leads to a fracture, and a segment forms. As the plate margin sinks deeper and deeper into the mantle, it causes further segments to form at the bend. As a result, the slab eventually resembles a chain with rigid links and bendable connectors. At a depth of about 600 kilometres, the segmented plate margin slides onto what is known as the 670 km discontinuity in the Earth’s mantle, from which point it moves horizontally.

Clues from nature support simulation

“The results of our simulations are consistent with observations in nature,” Gerya explains. A great deal of research has been done on the natural situation along the Japan Trench, where the Pacific plate sinks below the Okhotsk plate. The pattern of faults found here is an exact match for the pattern produced in the simulations.

Researchers have also studied the seismic velocity structure of subducting Japan slab thoroughly using its recently produced high-resolution seismic tomography model. They found that the velocity of the seismic waves sent out by earthquakes was reduced at some nodes inside the slab. The pattern with which these nodes occur in reality coincides with that of the segment boundaries from the simulations. And both in nature and in the computer model, it is zones with very small crystals only micrometres across that are responsible for reducing the velocity of the seismic waves.

These tiny crystal grains also make the underside plate material less viscous; in other words, it becomes runnier. Researchers at the Japan Trench were able to demonstrate this, too.

“That means our model is very plausible and provides solid physical background for the hypothesis of rigid plates with weak slabs,” Gerya says. But the research is far from over: one of his Bachelor’s students, Simon Niggli, has modelled and described plate fractures in three dimensions for the first time. Next the researchers want to investigate whether the segmentation of plate margins can also be responsible for strong earthquakes.

Reference:
T. V. Gerya, D. Bercovici, T. W. Becker. Dynamic slab segmentation due to brittle–ductile damage in the outer rise. Nature, 2021; 599 (7884): 245 DOI: 10.1038/s41586-021-03937-x

Note: The above post is reprinted from materials provided by ETH Zurich. Original written by Peter Rueegg.

Researchers recreate deep-Earth conditions to see how iron copes with extreme stress

Despite ESA’s GOCE mission ending over seven years ago, scientists continue to use this remarkable satellite’s gravity data to delve deep and unearth secrets about our planet. Recent research shows how scientists have combined GOCE data with measurements taken at the surface to generate a new model of Earth’s crust and upper mantle. This is the first time such a model has been created this way – and it is shedding new light on the processes of plate tectonics. The new model produced in ESA’s 3D Earth study shows for the first time how dissimilar the sub-lithospheric mantle is beneath different oceans, and provides insight as to how the morphology and spreading rates of mid-oceanic ridges may be connected with the deep chemical and thermal structure. Credit: ESA/Planetary Visions)
Representative image:  Credit: ESA/Planetary Visions)

Far below you lies a sphere of solid iron and nickel about as wide as the broadest part of Texas: the Earth’s inner core. The metal at the inner core is under pressure about 360 million times higher than we experience in our everyday lives and temperatures approximately as hot as the Sun’s surface.

Earth’s planetary core is thankfully intact. But in space, similar cores can collide with other objects, causing the crystalline materials of the core to deform rapidly. Some asteroids in our solar system are massive iron objects that scientists suspect are the remnants of planetary cores after catastrophic impacts.

Measuring what happens during the collision of celestial bodies or at the Earth’s core is obviously not very practical. As such, much of our understanding of planetary cores is based on experimental studies of metals at less extreme temperatures and pressures. But researchers at the Department of Energy’s SLAC National Accelerator Laboratory have now observed for the first time how iron’s atomic structure deforms to accommodate the stress from the pressures and temperatures that occur just outside of the inner core.

The results appear in Physical Review Letters, where they have been highlighted as an Editor’s Suggestion.

Coping with stress

Most of the iron you encounter in your everyday life has its atoms arranged in nanoscopic cubes, with an iron atom at each corner and one in the center. If you squeeze these cubes by applying extremely high pressures, they rearrange into hexagonal prisms, which allow the atoms to pack in more tightly.

The group at SLAC wanted to see what would happen if you kept applying pressure to that hexagonal arrangement to mimic what happens to iron at the Earth’s core or during atmospheric reentry from space. “We didn’t quite make inner core conditions,” says co-author Arianna Gleason, a scientist in the High-Energy Density Science (HEDS) Division at SLAC. “But we achieved the conditions of the outer core of the planet, which is really remarkable.”

No one had ever directly observed iron’s response to stress under such high temperatures and pressures before, so the researchers didn’t know how it would respond. “As we continue to push it, the iron doesn’t know what to do with this extra stress,” says Gleason. “And it needs to relieve that stress, so it tries to find the most efficient mechanism to do that.”

The coping mechanism iron uses to deal with that extra stress is called “twinning.” The arrangement of atoms shunts to the side, rotating all the hexagonal prisms by nearly 90 degrees. Twinning is a common pressure response in metals and minerals — quartz, calcite, titanium and zirconium all undergo twinning.

“Twinning allows iron to be incredibly strong — stronger than we first thought — before it starts to flow plastically on much longer time scales,” Gleason said.

A tale of two lasers

Reaching these extreme conditions required two types of lasers. The first was an optical laser, which generated a shock wave that subjected the iron sample to extremely high temperatures and pressures. The second was SLAC’s Linac Coherent Light Source (LCLS) X-ray free-electron laser, which allowed the researchers to observe the iron on an atomic level. “At the time, LCLS was the only facility in the world where you could do that,” says lead author Sébastien Merkel of the University of Lille in France. “It’s been a door opener for other similar facilities in the world.”

The team fired both lasers at a tiny sample of iron about the width of a human hair, hitting the iron with a shock wave of heat and pressure. “The control room is just above the experimental room,” Merkel says. “When you trigger the discharge, you hear a loud pop.”

As the shock wave hit the iron, researchers used the X-ray laser to observe how the shock changed the arrangement of the iron atoms. “We were able to make a measurement in a billionth of a second,” Gleason says. “Freezing the atoms where they are in that nanosecond is really exciting.”

The researchers collected these images and assembled them into a flipbook that showed iron deforming. Before the experiment was complete, they didn’t know if iron would respond too fast for them to measure or too slow for them to ever see. “The fact that the twinning happens on the time scale that we can measure it as an important result in itself,” Merkel says.

The future is bright

This experiment serves as a bookend for understanding the behavior of iron. Scientists had gathered experimental data on the structure of iron at lower temperatures and pressures and used it to model how iron would behave at extremely high temperatures and pressures, but no one had ever experimentally tested those models.

“Now we can give a thumbs up, thumbs down on some of the physics models for really fundamental deformation mechanisms,” Gleason says. “That helps to build up some of the predictive capability we’re lacking for modeling how materials respond at extreme conditions.”

The study provides exciting insights into the structural properties of iron at extremely high temperatures and pressures. But the results are also a promising indicator that these methods could help scientists understand how other materials behave at extreme conditions, too.

“The future is bright now that we’ve developed a way to make these measurements,” Gleason says. “The recent X-ray undulator upgrade as part of the LCLS-II project allows higher X-ray energies — enabling studies on thicker alloys and materials that have lower symmetry and more complex X-ray fingerprints.”

The upgrade will also enable researchers to observe larger samples, which will give them a more comprehensive view of iron’s atomic behavior and improve their statistics. Plus, “we’re going to get more powerful optical lasers with the approval to proceed with a new flagship petawatt laser facility, known as MEC-U,” says Gleason. “That’ll make future work even more exciting because we’ll be able to get to the Earth’s inner core conditions without any problem.”

Researchers at Los Alamos National Laboratory (LANL) contributed to this study. Funding was provided by the University of Lille, an LANL Reines Laboratory Directed Research and Development grant, and the DOE Office of Science, including Gleason’s DOE Early Career Award in Fusion Energy Sciences. LCLS is a DOE Office of Science user facility.

Reference:
Sébastien Merkel, Sovanndara Hok, Cynthia Bolme, Dylan Rittman, Kyle James Ramos, Benjamin Morrow, Hae Ja Lee, Bob Nagler, Eric Galtier, Eduardo Granados, Akel Hashim, Wendy L Mao, Arianna E Gleason. Femtosecond Visualization of hcp-Iron Strength and Plasticity under Shock Compression. Physical Review Letters, 2021; 127 (20) DOI: 10.1103/PhysRevLett.127.205501

Note: The above post is reprinted from materials provided by DOE/SLAC National Accelerator Laboratory. Original written by Graycen Wheeler.

Fate of sinking tectonic plates is revealed

Boudins of amphibolite layers (metamorphosed basalts) that were stretched within quartz schists (Norway). Photo credits © Haakon Fossen.
Boudins of amphibolite layers (metamorphosed basalts) that were stretched within quartz schists (Norway). Photo credits © Haakon Fossen.

Our world’s surface is a jumble of jostling tectonic plates, with new ones emerging as others are pulled under. The ongoing cycle keeps our continents in motion and drives life on Earth. But what happens when a plate disappears into the planet’s interior?

The question has long puzzled scientists because conventional wisdom said that sinking tectonic plates must remain intact to keep pulling on the portion behind it, but according to geophysical evidence, they are destroyed.

Now, in a study published Nov. 11 in Nature, scientists say they’ve found an answer that reconciles the two stories: Plates are significantly weakened as they sink but not so much that they break apart entirely.

The finding came after scientists put tectonic plates through a computer-generated gauntlet of destructive geologic forces. The model showed that as the plate enters the mantle, it bends abruptly downward, cracking its cold, brittle back. At the same time, the bending changes the fine grain structure of the rock along its underbelly, leaving it weakened. Combined, the stresses pinch the plate along its weak points, leaving it mostly intact but segmented like a slinky snake.

This means the plate continues to be pulled under despite becoming folded and distorted.

According to the researchers, the model predicted a scenario that matches observations from Japan. Studies of the region where the Pacific tectonic plate dives — or subducts — under Japan have turned up large cracks where the plate bends downward, and they have shown signs of weaker material underneath. Deep seismic imaging conducted by The University of Texas at Austin’s Steve Grand has also revealed tectonic shapes in the Earth’s mantle under Japan that appear a close match for the slinky snake in the model.

Co-author Thorsten Becker, a professor in UT’s Jackson School of Geosciences, said that the study does not necessarily close the book on what happens to subducting plates, but it certainly gives a compelling case to explain several important geologic processes.

“It’s an example of the power of computational geosciences,” said Becker who assisted in developing the model and is a faculty associate at UT’s Oden Institute for Computational Engineering & Sciences. “We combined these two processes that geology and rock mechanics are telling us are happening, and we learned something about the general physics of how the Earth works that we wouldn’t have expected. As a physicist, I find that exciting.”

The study’s lead author, Taras Gerya, a professor of geophysics at ETH Zurich, added that until now, geophysicists had lacked a comprehensive explanation for how tectonic plates bend without breaking.

Things got interesting when the researchers ran their simulations with a hotter interior, similar to the early Earth. In these simulations, the tectonic snake segments made it only a few miles into the mantle before breaking off. That means that subduction would have occurred intermittently, raising the possibility that modern plate tectonics began only within the past billion years.

“Personally, I think there are a lot of good arguments for plate tectonics being much older,” Becker said, “but the mechanism revealed by our model suggests things might be more sensitive to the temperature of the mantle than we thought, and that, I think, could lead to interesting new avenues of discussion.”

Becker and Gerya were joined by David Bercovici, a geophysicist at Yale University whose investigation into how rock grains are altered in the deep mantle helped motivate the research. The study is based on a two-dimensional computer model of plate tectonics incorporating Bercovici’s rock deformation research and other plate-weakening mechanics. The researchers are now studying the phenomena using 3D models and plan to investigate what those models can tell them about the occurrence of earthquakes.

The research was supported by grants from the Swiss National Science Foundation, ETH Zurich, and the U.S. National Science Foundation. The simulations were run on high-performance computing clusters at ETH Zurich.

Reference:
T. V. Gerya, D. Bercovici, T. W. Becker. Dynamic slab segmentation due to brittle–ductile damage in the outer rise. Nature, 2021; 599 (7884): 245 DOI: 10.1038/s41586-021-03937-x

Note: The above post is reprinted from materials provided by University of Texas at Austin.

Radiocarbon is key to understanding Earth’s past

The rising Earth from the perspective of the moon.
The rising Earth from the perspective of the moon. Credit: NASA Goddard

Radiocarbon records are critical to understanding the history of Earth’s climate, magnetic field, and the Sun’s activity, say researchers.

In an article published today (November 5 2021) in the journal Science, scientists have highlighted how recent advances in our knowledge of past radiocarbon levels are improving our understanding of climate processes, solar activity, geophysics and the carbon cycle.

Understanding the past is essential to understanding our present and to projecting Earth’s potential changes in the future. Developing an accurate record of atmospheric radiocarbon extending back 55,000 years helps researchers understand Earth’s processes and consequently improve projections of climate change.

Radiocarbon also tells us about the possibility of past extreme solar storms, orders of magnitude greater than any instrumentally observed. Similar storms today would have the potential to catastrophically damage our communications networks and electricity grids.

Dr Tim Heaton, Lead Author and Senior Lecturer from the University of Sheffield’s School of Mathematics and Statistics, said: “Radiocarbon is best known as the tool by which we date and synchronise many of the various archaeological and climate records from the last 55,000 years. However, past levels of radiocarbon are also critical to understand the Sun, the geodynamo, past climate, and changes in the carbon cycle.

“Recent years have seen a revolution in our ability to construct detailed records of past radiocarbon levels, leading to new insights in the chronology of past climate events, changes in the Sun’s activity, carbon cycle and fluxes in Carbon Dioxide (CO2) levels.”

Developments in radiocarbon dating have allowed the IntCal Working Group to estimate radiocarbon levels with unprecedented accuracy back to the limits of the technique ~55,000 years ago.

Last year the IntCal Working Group recalculated the internationally-agreed radiocarbon calibration curves for the first time in seven years, making them more detailed than ever before.

They used measurements from almost 15,000 samples from objects dating back as far as 60,000 years ago to create the new radiocarbon calibration curves, which are fundamental across the scientific spectrum for accurately dating artefacts, and understanding the Earth and climate systems.

Radiocarbon is vital to geoscience and archaeology. Scientists on the Intergovernmental Panel on Climate Change (IPCC) rely upon radiocarbon to improve their models — as a proxy for the Sun, and as a target to improve their understanding of the Earth system — and as a clock to date most paleoclimatic records over the past 55,000 years. This is essential to better understand and prepare for future changes in climate. Archaeologists use radiocarbon dating to understand pivotal changes in our societal systems that help to explain our present and answer the grand challenges we face today.

Reference:
T. J. Heaton, E. Bard, C. Bronk Ramsey, M. Butzin, P. Köhler, R. Muscheler, P. J. Reimer, L. Wacker. Radiocarbon: A key tracer for studying Earth’s dynamo, climate system, carbon cycle, and Sun. Science, 2021; 374 (6568) DOI: 10.1126/science.abd7096

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

Let’s talk about the 1,800-plus ‘young’ volcanoes in the US Southwest

A view of the crater of Dotsero volcano, a monogenetic volcano that erupted in Colorado about 4,000 years ago. Credit: Greg Valentine
A view of the crater of Dotsero volcano, a monogenetic volcano that erupted in Colorado about 4,000 years ago. Credit: Greg Valentine

They’re born. They live once, erupting for a period that might last for days, years or decades. Then, they go dark and die.

This narrative describes the life of a monogenetic volcano, a type of volcanic hazard that can pose important dangers despite an ephemeral existence.

The landscape of the southwestern U.S. is heavily scarred by past eruptions of such volcanoes, and a new study marks a step toward understanding future risks for the region.

The research, which will be published on Nov. 2 in the journal Geosphere, provides a broad overview of what we know — and don’t know — about this type of volcanism in the U.S. Southwest over the past 2.58 million years, a geologic period known as the Quaternary.

During this time, more than 1,800 monogenetic volcanoes erupted in the region, according to a count covering Nevada, Utah, Arizona, Colorado, New Mexico and parts of California’s eastern edge. Add in the Pinacate volcanic field, located mostly in the Mexican state of Sonora, bordering Arizona, and the number goes up to over 2,200, scientists say. (The volcanoes included are ones whose ages are estimated to be in the range of the Quaternary, but many have not been precisely dated.)

“Monogenetic means ‘one life,'” says lead author Greg Valentine, a University at Buffalo volcanologist. “So a monogenetic volcano will erupt once, and that eruption may last for several days to several decades, but after that, the volcano is basically dead.

“In the United States, most volcanic hazards-related attention has rightly gone to places like Hawaii, and to the Pacific Northwest and Alaska, where we have big stratovolcanoes like Mount Rainier and Mount St. Helens, which will have many eruptive episodes over a long life, with widespread hazardous effects. In the past, these smaller monogenetic volcanoes really haven’t been looked at from a focus on hazards; they have been instead studied mainly for what they tell us about the deep earth. Recently, however, there has been more buzz in the research community about how we need to take a look at the kinds of hazards these volcanoes might pose.

“My experience with the general public is that most people are surprised to know that there are so many young volcanoes in the Southwest.”

The paper’s authors are Valentine, PhD, professor of geology in the UB College of Arts and Sciences; Michael H. Ort, PhD, professor emeritus of geology at Northern Arizona University; and Joaquín A. Cortés, PhD, senior lecturer of geology at Edge Hill University in England.

These volcanoes won’t erupt again. So why study them?

The 2,000-plus volcanoes noted in the paper are done erupting, so they no longer pose a threat. But studying them is important because of the potential for new ones to bloom.

“Monogenetic volcanoes tend to occur in areas that we call volcanic fields, and the American Southwest is just dotted with these,” says Valentine, who grew up in New Mexico. “These are areas of high volcanic activity where future eruptions could happen, but we don’t know when, and we don’t know exactly where.”

The city of Flagstaff, Arizona, is located in a volcanic field where multiple monogenetic volcanoes have erupted in the past, so a better understanding of possible hazards is important for people who live there.

“Two of the most recent eruptions in the Southwest occurred near Flagstaff about 1,000 years ago, one just outside of town and the other on the north rim of the Grand Canyon,” Ort says. Northern Arizona University is in Flagstaff. “People living there at the time adapted to the effects of the eruptions, changing agricultural and cultural practices as well as where they lived. We will need to do the same when the next one erupts. Albuquerque also has young volcanoes along its western margin.”

Mercifully, most volcanoes in the southwestern U.S. are in remote locations, away from large population centers. In isolated areas, threats from eruptions could include ash plumes that disrupt travel (including air) or power distribution infrastructure, researchers say.

“One of the younger eruptions in the Southwest occurred south of Grants, New Mexico a few thousand years ago, and flowed for many miles parallel to what is now Interstate 40 and part of the Burlington Northern Santa Fe railroad,” Ort says. “A similar eruption today would take out one of the most important east-west transportation routes in the country. Several volcanic fields lie along these routes, from the Mojave Desert of California to eastern New Mexico, including the one around Flagstaff.”

“The fundamental pieces of information that you need to have in order to start understanding the hazards and the chances of a future eruption are the number of volcanoes, their ages and the types of eruptions they have,” Valentine says. “What we set out to do in the study is find every bit of information that we could about these monogenetic volcanoes in the southwestern U.S. and compile it all in one place. How many of these are there? What are their characteristics? We got information from state geological surveys, published papers and other sources.”

What are the chances of a new eruption within a century?

Based solely on the total count of volcanoes that have erupted in the study region during the Quaternary Period, the chances of a new volcano emerging in the area within 100 years would be about 8%, Valentine says.

But he notes that this figure embodies lots of uncertainty. It doesn’t account for buried volcanoes, or the fact that a single eruption can create multiple vents. More research will be needed to refine this estimate and to forecast likely locations for a new eruption.

“There’s so much uncertainty here, and this is part of the problem,” he says. “It’s kind of a wide-open research field. When you look at the region from the perspective of volcanic hazards, we really have very little information. Most of the volcanoes have not been dated, so we don’t know how old they are, except that they likely formed sometime within the Quaternary Period. Very few have been studied in detail.”

That said, the study’s findings indicate that the frequency of eruptions across the study region may approach that of individual volcanoes in the Pacific Northwest, Valentine and Ort say. The new paper highlights gaps in knowledge, and the scientists hope that it can act as a launchpad for future, more detailed research. As Ort and Valentine point out, a new Southwest volcano could appear anywhere in any active volcanic field.

“We don’t have infinite resources, so we have to prioritize the efforts we put into forecasting and planning for hazards,” Valentine says. “But how do you set priorities? If you’re monitoring volcanic fields in the Southwest, where do you put the instruments? Being able to better answer questions like these is what we’re moving toward.”

Reference:
Greg A. Valentine, Michael H. Ort, Joaquín A. Cortés. Quaternary basaltic volcanic fields of the American Southwest. Geosphere, 2021; DOI: 10.1130/GES02405.1

Note: The above post is reprinted from materials provided by University at Buffalo. Original written by Charlotte Hsu.

Uncovering the secrets behind Earth’s first major mass extinction

Brachiopod fossils from the Ordovician Period outcrop on Anticosti Island, Quebec, Canada. (Credit: André Desrochers, University of Ottawa)
Brachiopod fossils from the Ordovician Period outcrop on Anticosti Island, Quebec, Canada. (Credit: André Desrochers, University of Ottawa)

We all know that the dinosaurs died in a mass extinction. But did you know that there were other mass extinctions? There are five most significant mass extinctions, known as the “big five,” where at least three-quarters of all species in existence across the entire Earth faced extinction during a particular geological period of time. With current trends of global warming and climate change, many researchers now believe we may be in a sixth.

Discovering the root cause of Earth’s mass extinctions has long been a hot topic for scientists, as understanding the environmental conditions that led to the elimination of the majority of species in the past could potentially help prevent a similar event from occurring in the future.

A team of scientists from Syracuse University’s Department of Earth and Environmental Sciences, the University of California, Berkeley and the University of California, Riverside, Université Bourgogne Franche-Comté, the University of New Mexico, the University of Ottawa, the University of Science and Technology of China and Stanford University recently co-authored a paper exploring the Late Ordovician mass extinction (LOME), which is the first, or oldest of the “big five (~445 million years ago).” Around 85% of marine species, most of which lived in shallow oceans near continents, disappeared during that time.

Lead author Alexandre Pohl, from UC Riverside (now a postdoctoral research fellow at Université Bourgogne Franche-Comté in Dijon, France) and his co-authors investigated the ocean environment before, during, and after the extinction in order to determine how the event was brewed and triggered. The results from their study will be published in the journal Nature Geoscience on Nov. 1.

To paint a picture of the oceanic ecosystem during the Ordovician Period, mass extinction expert Seth Finnegan, associate professor at UC Berkeley, says that seas were full of biodiversity. Oceans contained some of the first reefs made by animals, but lacked an abundance of vertebrates.

“If you had gone snorkeling in an Ordovician sea you would have seen some familiar groups like clams and snails and sponges, but also many other groups that are now very reduced in diversity or entirely extinct like trilobites, brachiopods and crinoids” says Finnegan.

Unlike with rapid mass extinctions, like the Cretaceous-Tertiary extinction event where dinosaurs and other species died off suddenly some 65.5 million years ago, Finnegan says LOME played out over a substantial period of time, with estimates between less than half a million to almost two million years.

One of the major debates surrounding LOME is whether lack of oxygen in seawater caused that period’s mass extinction. To investigate this question, the team integrated geochemical testing with numerical simulations and computer modeling.

Zunli Lu, professor of Earth and environmental sciences at Syracuse University, and his students took measurements of iodine concentration in carbonate rocks from that period, contributing important findings about oxygen levels at various ocean depths. The concentration of the element iodine in carbonate rocks serves as an indicator for changes in oceanic oxygen level in Earth’s history.

Their data, combined with computer modeling simulations, suggested that there was no evidence of anoxia – or lack of oxygen – strengthening during the extinction event in the shallow ocean animal habitat where most organisms lived, meaning that climate cooling that occurred during the Late Ordovician period combined with additional factors likely was responsible for LOME.

On the other hand, there is evidence that anoxia in deep oceans expanded during that same time, a mystery that cannot be explained by the classic model of ocean oxygen, climate modeling expert Alexandre Pohl says.

“Upper-ocean oxygenation in response to cooling was anticipated, because atmospheric oxygen preferentially dissolves in cold waters,” Pohl says. “However, we were surprised to see expanded anoxia in the lower ocean since anoxia in Earth’s history is generally associated with volcanism-induced global warming.”

They attribute the deep-sea anoxia to the circulation of seawater through global oceans. Pohl says that a key point to keep in mind is that ocean circulation is a very important component of the climatic system.

He was part of a team led by senior modeler Andy Ridgwell, professor at UC Riverside, whose computer modeling results show that climate cooling likely altered ocean circulation pattern, halting the flow of oxygen-rich water in shallow seas to the deeper ocean.

According to Lu, recognizing that climate cooling can also lead to lower oxygen levels in some parts of the ocean is a key takeaway from their study.

“For decades, the prevailing school of thoughts in our field is that global warming causes the oceans to lose oxygen and thus impact marine habitability, potentially destabilizing the entire ecosystem,” Lu says. “In recent years, mounting evidence point to several episodes in Earth’s history when oxygen levels also dropped in cooling climates.”

While the causes of Late Ordovician extinction have not been fully agreed upon, nor will they for some time, the team’s study rules out changes in oxygenation as a single explanation for this extinction and adds new data favoring temperature change being the killing mechanism for LOME.

Pohl is hopeful that as better climate data and more sophisticated numerical models become available, they will be able to offer a more robust representation of the factors that may have led to the Late Ordovician mass extinction.

Reference:
Alexandre Pohl, Zunli Lu, Wanyi Lu, Richard G. Stockey, Maya Elrick, Menghan Li, André Desrochers, Yanan Shen, Ruliang He, Seth Finnegan, Andy Ridgwell. Vertical decoupling in Late Ordovician anoxia due to reorganization of ocean circulation. Nature Geoscience, 2021; DOI: 10.1038/s41561-021-00843-9

Note: The above post is reprinted from materials provided by Syracuse University. Original written by Dan Bernardi.

Some of the world’s oldest rubies linked to early life

Photo of the ruby that this study looks at. Credit: University of Waterloo
Photo of the ruby that this study looks at. Credit: University of Waterloo

While analyzing some of the world’s oldest coloured gemstones, researchers from the University of Waterloo discovered carbon residue that was once ancient life, encased in a 2.5 billion-year-old ruby.

The research team, led by Chris Yakymchuk, professor of Earth and Environmental Sciences at Waterloo, set out to study the geology of rubies to better understand the conditions necessary for ruby formation. During this research in Greenland, which contains the oldest known deposits of rubies in the world, the team found a ruby sample that contained graphite, a mineral made of pure carbon. Analysis of this carbon indicates that it is a remnant of early life.

“The graphite inside this ruby is really unique. It’s the first time we’ve seen evidence of ancient life in ruby-bearing rocks,” says Yakymchuk. “The presence of graphite also gives us more clues to determine how rubies formed at this location, something that is impossible to do directly based on a ruby’s colour and chemical composition.”

The presence of the graphite allowed the researchers to analyze a property called isotopic composition of the carbon atoms, which measures the relative amounts of different carbon atoms. More than 98 per cent of all carbon atoms have a mass of 12 atomic mass units, but a few carbon atoms are heavier, with a mass of 13 or 14 atomic mass units.

“Living matter preferentially consists of the lighter carbon atoms because they take less energy to incorporate into cells,” said Yakymchuk. “Based on the increased amount of carbon-12 in this graphite, we concluded that the carbon atoms were once ancient life, most likely dead microorganisms such as cyanobacteria.”

The graphite is found in rocks older than 2.5 billion years ago, a time on the planet when oxygen was not abundant in the atmosphere, and life existed only in microorganisms and algae films.

During this study, Yakymchuk’s team discovered that this graphite not only links the gemstone to ancient life but was also likely necessary for this ruby to exist at all. The graphite changed the chemistry of the surrounding rocks to create favourable conditions for ruby growth. Without it, the team’s models showed that it would not have been possible to form rubies in this location.

References:

  • Chris Yakymchuk, Vincent van Hinsberg, Christopher L. Kirkland, Kristoffer Szilas, Carson Kinney, Jillian Kendrick, Julie A. Hollis. Corundum (ruby) growth during the final assembly of the Archean North Atlantic Craton, southern West Greenland. Ore Geology Reviews, 2021; 138: 104417 DOI: 10.1016/j.oregeorev.2021.104417
  • Vincent van Hinsberg, Chris Yakymchuk, Angunguak Thomas Kleist Jepsen, Christopher L. Kirkland, Kristoffer Szilas. The corundum conundrum: Constraining the compositions of fluids involved in ruby formation in metamorphic melanges of ultramafic and aluminous rocks. Chemical Geology, 2021; 571: 120180 DOI: 10.1016/j.chemgeo.2021.120180

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

Four dinosaurs discovered in Montana

A closeup view of the Flyby Trike’s occipital condyle bone — nicknamed the “trailer hitch” — the ball on the back of the skull that connects to neck vertebrae.Rachel Ormiston/Burke Museum/University of Washington
A closeup view of the Flyby Trike’s occipital condyle bone — nicknamed the “trailer hitch” — the ball on the back of the skull that connects to neck vertebrae.Rachel Ormiston/Burke Museum/University of Washington

A team of paleontologists from the University of Washington and its Burke Museum of Natural History and Culture excavated four dinosaurs in northeastern Montana this summer. All fossils will be brought back to the Burke Museum where the public can watch paleontologists remove the surrounding rock in the fossil preparation laboratory.

The four dinosaur fossils are: the ilium — or hip bones — of an ostrich-sized theropod, the group of meat-eating, two-legged dinosaurs that includes Tyrannosaurus rex and raptors; the hips and legs of a duck-billed dinosaur; a pelvis, toe claw and limbs from another theropod that could be a rare ostrich-mimic Anzu, or possibly a new species; and a Triceratops specimen consisting of its skull and other fossilized bones. Three of the four dinosaurs were all found in close proximity on Bureau of Land Management land that is currently leased to a rancher.

In July 2021, a team of volunteers, paleontology staff, K-12 educators who were part of the DIG Field School program and students from UW and other universities worked together to excavate these dinosaurs. The fossils were found in the Hell Creek Formation, a geologic formation that dates from the latest portion of Cretaceous Period, 66 to 68 million years ago. Typical paleontological digs involve excavating one known fossil. However, the Hell Creek Project is an ongoing research collaboration of paleontologists from around the world studying life right before, during and after the K-Pg mass extinction event that killed off all dinosaurs except birds. The Hell Creek Project is unique in that it is sampling all plant and animal life found throughout the rock formation in an unbiased manner.

“Each fossil that we collect helps us sharpen our views of the last dinosaur-dominated ecosystems and the first mammal-dominated ecosystems,” said Gregory Wilson Mantilla, a UW professor of biology and curator of vertebrate paleontology at the Burke Museum. “With these, we can better understand the processes involved in the loss and origination of biodiversity and the fragility, collapse and assembly of ecosystems.”

All of the dinosaurs except the Triceratops will be prepared in the Burke Museum’s fossil preparation laboratory this fall and winter. The Triceratops fossil remains on the site because the dig team continued to find more and more bones while excavating and needs an additional field season to excavate any further bones that may be connected to the surrounding rock. The team plans to finish excavation in the summer of 2022.

Called the “Flyby Trike” in honor of the rancher who first identified the dinosaur while he was flying his airplane over his ranch, the team has uncovered this dinosaur’s frill, horn bones, individual rib bones, lower jaw, teeth and the occipital condyle bone — nicknamed the “trailer hitch,” which is the ball on the back of the skull that connects to the neck vertebrae. The team estimates approximately 30% of this individual’s skull bones have been found to date, with more potential bones to be excavated next year.

The Flyby Trike was found in hardened mud, with the bones scattered on top of each other in ways that are different from the way the bones would be laid out in a living animal. These clues indicate the dinosaur likely died on a flood plain and then got mixed together after its death by being moved around by a flood or river system, or possibly moved around by a scavenger like a T. rex, before fossilizing. In addition, the Flyby Trike is one of the last Triceratops living before the K-Pg mass extinction. Burke paleontologists estimate it lived less than 300,000 years before the event.

“Previous to this year’s excavations, a portion of the Flyby Trike frill and a brow horn were collected and subsequently prepared by volunteer preparators in the fossil preparation lab. The frill was collected in many pieces and puzzled together fantastically by volunteers. Upon puzzling the frill portion together, it was discovered that the specimen is likely an older ‘grandparent’ Triceratops,” said Kelsie Abrams, the Burke Museum’s paleontology preparation laboratory manager who also participated in this summer’s field work. “The triangular bones along the frill, called ‘epi occipitals,’ are completely fused and almost unrecognizable on the specimen, as compared to the sharp, noticeable triangular shape seen in younger individuals. In addition, the brow horn curves downwards as opposed to upwards, and this feature has been reported to be seen in older animals as well.”

Amber and seed pods were also found with the Flyby Trike. These finds allow paleobotanists to determine what plants were living alongside Triceratops, what the dinosaurs may have eaten, and what the overall ecosystem was like in Hell Creek leading up to the mass extinction event.

“Plant fossil remains from this time period are crucial for our understanding of the wider ecosystem. Not only can plant material tell us what these dinosaurs were perhaps eating, but plants can more broadly tell us what their environment looked like,” said Paige Wilson, a UW graduate student in Earth and space sciences. “Plants are the base of the food chain and a crucial part of the fossil record. It’s exciting to see this new material found so close to vertebrate fossils!”

Museum visitors can now see paleontologists remove rock from the first of the four dinosaurs — the theropod hips — in the Burke’s paleontology preparation laboratory. Additional fossils will be prepared in the upcoming weeks. All four dinosaurs will be held in trust for the public on behalf of the Bureau of Land Management and become a part of the Burke Museum’s collections.

Note: The above post is reprinted from materials provided by University of Washington. Original written by Andrea Godinez.

First dinosaur era crab fully preserved in amber discovered

Fig. 1. Cretapsara athanata Luque gen. et sp. nov., a modern-looking eubrachyuran crab in Burmese amber. (A to D) Holotype LYAM-9. (A) Whole amber sample with crab inclusion in ventral view. (B) Close-up of ventral carapace. (C) Whole amber sample with crab inclusion in dorsal view. (D) Close-up of dorsal carapace. White arrows in (B) and (D) indicate the detached left fifth leg or pereopod. Photos by L.X. Figure by J.L.
Fig. 1. Cretapsara athanata Luque gen. et sp. nov., a modern-looking eubrachyuran crab in Burmese amber.
(A to D) Holotype LYAM-9. (A) Whole amber sample with crab inclusion in ventral view. (B) Close-up of ventral carapace. (C) Whole amber sample with crab inclusion in dorsal view. (D) Close-up of dorsal carapace. White arrows in (B) and (D) indicate the detached left fifth leg or pereopod. Photos by L.X. Figure by J.L.

Fossils trapped in amber provide a unique snapshot of the anatomy, biology, and ecology of extinct organisms. The most common fossils found in amber, which is formed from resin exuded from tree bark, are land-dwelling animals, mainly insects. But on very rare occasions scientists discover amber housing an aquatic organism.

In a study published October 20 in Science Advances an international team of researchers describe the first crab from the Cretaceous dinosaur era preserved in amber. The study used micro CT to examine and describe Cretapsara athanata, the oldest modern-looking crab (approximately 100 million years old) and the most complete fossil crab ever discovered. It is rivalled in completeness by the mysterious Callichimaera perplexa, a very distant relative nicknamed the platypus of the crab world. Callichimaera’s stunning preservation included soft tissues and delicate parts that rarely fossilize. Both Cretapsara and Callichimaera are new branches in the crab tree of life that lived during the Cretaceous Crab Revolution, a period when crabs diversified worldwide and the first modern groups originated while many others disappeared.

True crabs, or Brachyura, are an iconic group of crustaceans whose remarkable diversity of forms, species richness, and economic importance have inspired celebrations and festivals worldwide. They’ve even earned a special role in the pantheon of social media. True crabs are found all around the world, from the depths of the oceans, to coral reefs, beaches, rivers, caves, and even in trees as true crabs are among the few animal groups that have conquered land and freshwater multiple times.

The crab fossil record extends back into the early Jurassic, more than 200 million years ago. Unfortunately, fossils of nonmarine crabs are sparse and largely restricted to bits and pieces of the animals carapace — claws and legs found in sedimentary rocks. That is until now with the discovery of Cretapsara athanata. “The specimen is spectacular, it is one of a kind. It’s absolutely complete and is not missing a single hair on the body, which is remarkable,” said lead author Javier Luque, postdoctoral researcher in the Department of Organismic and Evolutionary Biology, Harvard University.

A group of scientists led by co-lead author Lida Xing, China University of Geosciences, Beijing, made micro CT scans of the fossil, which is housed in the Longyin Amber Museum in Yunnan, China. The scans created a full three-dimensional reconstruction of the exquisite preservation of the animal allowing Luque, Xing, and their team to see the complete body of the animal including delicate tissues, like the antennae and mouthparts lined with fine hairs. Shockingly they discovered the animal also had gills.

“The more we studied the fossil, the more we realized that this animal was very special in many ways,” said Luque. Cretapsara is remarkably modern-looking — superficially resembling some shore crabs found today — unlike most crabs during the mid-Cretaceous era which looked quite different from modern crabs. Yet, the animal was entombed in Cretaceous amber and the presence of well-developed gills indicated an aquatic to semi-aquatic animal. Aquatic animals are rarely preserved in tree resins that become amber. Crabs previously found in amber are by the handful and belong to a living group of tropical land and tree-dwelling crabs known as Sesarmidae from the Miocene (15 million years ago). How then, the researchers asked, did a 100 million year old aquatic animal become preserved in tree amber, which normally houses land-dwelling specimens?

Gills allow aquatic animals to breathe in water. But crabs have successfully and independently conquered land, brackish water, and fresh water at least twelve times since the dinosaur era. In doing so their gills evolved to include lung-like tissue allowing them to breathe both in and out of the water. Cretapsara however, had no lung tissue, only well-developed gills indicating the animal was not completely land dwelling. “Now we were dealing with an animal that is likely not marine, but also not fully terrestrial,” Luque said. “In the fossil record, nonmarine crabs evolved 50 million years ago, but this animal is twice that age.”

The team’s phylogenetic studies show that carcinization (the evolution of true crab-looking forms) had actually already occurred in the most recent common ancestor shared by all modern crabs more than 100 million years ago. Cretapsara bridges the gap in the fossil record and confirms that crabs actually invaded land and fresh water during the dinosaur era, not during the mammal era, pushing the evolution of nonmarine crabs much further back in time.

The researchers hypothesize that Cretapsara, measuring at five millimeters in leg span, was a juvenile crab of a freshwater to amphibious species. Or, that the animal is perhaps a semi-terrestrial juvenile crab migrating onto land from water as occurs to the iconic Christmas Island red crabs where land dwelling mother crabs release their babies into the ocean, which later swarm out of the water back onto land. They further hypothesize that like the crabs found in amber from the Miocene, Cretapsara could have been a tree climber. “These Miocene crabs are truly modern looking crabs and, as their extant relatives, they live in trees in little ponds of water,” said Luque, “these arboreal crabs can get trapped in tree resin today, but would it explain why Cretapsara is preserved in amber?”

Luque’s research is centered on understanding why things evolve into crabs, and their evolution and diversification over time leading to the modern forms seen today. “This study is pushing the timing of origin of many of these groups back in time. Every fossil we discover challenges our preconceptions about the time and place of origin of several organisms, often making us look further back in time,” Luque said.

The study is part of a National Science Foundation funded project with Luque, Professor Javier Ortega-Hernández and postdoctoral researcher Joanna Wolfe, both in the Department of Organismic and Evolutionary Biology, Harvard University, and Professor Heather Bracken-Grissom, Florida International University.

The researchers chose the name Cretapsara athanata, which means the immortal Cretaceous spirit of the clouds and waters, to honor the Cretaceous, during which this crab lived, and Apsara, a spirit of the clouds and waters in South and Southeast Asian mythology. The species name is based on “athanatos,” immortal, referring to its lifelike preservation as if ‘frozen in time’ in the time capsule that is amber.

Author’s Statement: The studied fossil, deposited in the Longyin Amber Museum (LYAM), Yunnan Province, China, comes from a batch of commercial “raw” (dull, unpolished) amber pieces collected by local miners and sold to a vendor at an amber jewelry market in Myitkyina on May 12, 2015. The polished piece containing the fossil studied was acquired by LYAM from the vendor’s mineral store in Tengchong, China, on 10 August 2015. We acknowledge the existence of a sociopolitical conflict in northern Myanmar and have limited our research to material predating the 2017 resumption of hostilities in the region. We hope that conducting research on specimens collected before the conflict and acknowledging the situation in the Kachin State will serve to raise awareness of the current conflict in Myanmar and the human cost behind it.

Reference:
Javier Luque, Lida Xing, Derek E. G. Briggs, Elizabeth G. Clark, Alex Duque, Junbo Hui, Huijuan Mai and Ryan C. McKellar. Crab in amber reveals an early colonization of nonmarine environments during the Cretaceous. Science Advances, 2021 DOI: 10.1126/sciadv.abj5689

Note: The above post is reprinted from materials provided by Harvard University, Department of Organismic and Evolutionary Biology.

Two new species of large predatory dinosaur discovered on Isle of Wight, UK

Image: Artists impression of newly identified species Credit: Anthony Hutchings
Image: Artists impression of newly identified species
Credit: Anthony Hutchings

A new study led by palaeontologists at the University of Southampton suggests that bones found on the Isle of Wight belong to two new species of spinosaurid, a group of predatory theropod dinosaurs closely related to the giant Spinosaurus. Their unusual, crocodile-like skulls helped the group expand their diets, allowing them hunt prey on both land and in the water.

The haul of bones was discovered on the beach near Brighstone over a period of several years. Keen-eyed fossil collectors initially found parts of two skulls, and a crew from Dinosaur Isle Museum recovered a large portion of a tail. In all, over 50 bones from the site have been uncovered from rocks that form part of the Wessex Formation, laid down over 125 million years ago during the Early Cretaceous.

The only spinosaurid skeleton previously unearthed in the UK belonged to Baryonyx, which was initially discovered in 1983 in a quarry in Surrey. Most other finds since have been restricted to isolated teeth and single bones.

Analysis of the bones carried out at the University of Southampton and published in Scientific Reports suggested they belonged to species of dinosaurs previously unknown to science.

Chris Barker, a PhD student at the University of Southampton and lead author of the study, said: “We found the skulls to differ not only from Baryonyx, but also one another, suggesting the UK housed a greater diversity of spinosaurids than previously thought.”

The discovery of spinosaurid dinosaurs on the Isle of Wight was a long time coming. “We’ve known for a couple of decades now that Baryonyx-like dinosaurs awaited discovered on the Isle of Wight, but finding the remains of two such animals in close succession was a huge surprise” remarked co-author Darren Naish, expert in British theropod dinosaurs.

The first specimen has been named Ceratosuchops inferodios, which translates as the “horned crocodile-faced hell heron.” With a series of low horns and bumps ornamenting the brow region the name also refers to the predator’s likely hunting style, which would be similar to that of a (terrifying) heron. Herons famously catch aquatic prey around the margins of waterways but their diet is far more flexible than is generally appreciated, and can include terrestrial prey too.

The second was named Riparovenator milnerae. This translates as “Milner’s riverbank hunter,” in honour of esteemed British palaeontologist Angela Milner, who recently passed away. Dr Milner had previously studied and named Baryonyx — a major palaeontological event whose discovery substantially improved our understanding of these distinctive predators.

Dr David Hone, co-author from Queen Mary University of London: “It might sound odd to have two similar and closely related carnivores in an ecosystem, but this is actually very common for both dinosaurs and numerous living ecosystems.”

Although the skeletons are incomplete, the researchers estimate that both Ceratosuchops and Riparovenator measured around nine metres in length, snapping up prey with their metre-long skulls. The study also suggested how spinosaurids might have first evolved in Europe, before dispersing into Asia, Africa and South America.

Dr Neil J. Gostling of the University of Southampton, who supervised the project, said: “This work has brought together universities, Dinosaur Isle museum and the public to reveal these amazing dinosaurs and the incredibly diverse ecology of the south coast of England 125 million years ago.”

The Early Cretaceous rocks on the Isle of Wight describe an ancient floodplain environment bathed in a Mediterranean-like climate. Whilst generally balmy, forest fires occasionally ravaged the landscape, and the remains of burnt wood can be seen throughout the cliffs today. With a large river and other bodies of water attracting dinosaurs and housing various fish, sharks and crocodiles, the habitat provided the newly discovered spinosaurids with plenty of hunting opportunities.

Fossil collector Brian Foster from Yorkshire, who made an important contribution to the finds and publication, said: “This is the rarest and most exciting find I’ve made in over 30 years of fossil collecting.” Fellow collector Jeremy Lockwood, who lives on the Isle of Wight and discovered several bones added, “we realised after the two snouts were found that this would be something rare and unusual. Then it just got more and more amazing as several collectors found and donated other parts of this enormous jigsaw to the museum.”

Dr Martin Munt, Curator of Dinosaur Isle Museum, noted how these new finds cement the Isle of Wight’s status as one of the top locations for dinosaur remains in Europe. The project also solidified how collectors, museums and universities can work together to bring fossil specimens to light.

Dr Munt added: “On behalf of the museum I wish to express our gratitude to the collectors, including colleagues at the museum, who have made these amazing finds, and made them available for scientific research. We also congratulate the team who have worked on these exciting finds and brought them to publication.”

Video illustrating newly discovered dinosaurs: https://www.youtube.com/watch?v=x3gUECD7axs&t=7s

The new fossils will go on display at Dinosaur Isle Museum at Sandown.

Reference:
Chris T. Barker, David W. E. Hone, Darren Naish, Andrea Cau, Jeremy A. F. Lockwood, Brian Foster, Claire E. Clarkin, Philipp Schneider, Neil J. Gostling. New spinosaurids from the Wessex Formation (Early Cretaceous, UK) and the European origins of Spinosauridae. Scientific Reports, 2021; 11 (1) DOI: 10.1038/s41598-021-97870-8

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

‘Raptor-like’ dinosaur discovered in Australian mine, actually uncovered as a timid vegetarian

Life reconstruction of herbivorous dinosaurs based on 220-million-year-old fossil footprints from Ipswich, Queensland, Australia. (Image credit: Anthony Romilio)
Life reconstruction of herbivorous dinosaurs based on 220-million-year-old fossil footprints from Ipswich, Queensland, Australia. (Image credit: Anthony Romilio)

Fossil footprints found in an Australian coal mine around 50 years ago have long been thought to be that of a large ‘raptor-like’ predatory dinosaur, but scientists have in fact discovered they were instead left by a timid long-necked herbivore.

University of Queensland palaeontologist Dr Anthony Romilio recently led an international team to re-analyse the footprints, dated to the latter part of the Triassic Period, around 220 million-year-ago.

“For years it’s been believed that these tracks were made by a massive theropod predator that was part of the dinosaur family Eubrontes, with legs over two metres tall,” Dr Romilio said.

“This idea caused a sensation decades ago because no other meat-eating dinosaur in the world approached that size during the Triassic period.”

However, findings made by a team of international researchers, published today in the peer-reviewed journal Historical Biology, in fact shows the tracks were instead made by a dinosaur known as a Prosauropod – a vegetarian dinosaur that were smaller, with legs about 1.4 metres tall and a body length of six metres.

The research team suspected there was something not-quite-right with the original size estimates and there was a good reason for their doubts.

“Unfortunately, most earlier researchers could not directly access the footprint specimen for their study, instead relying on old drawings and photographs that lacked detail,” Dr Romilio said.

The dinosaur fossils were discovered more than half a century ago around 200 metres deep underground at an Ipswich coal mine, just west of Brisbane.

“It must have been quite a sight for the first miners in the 1960s to see big bird-like footprints jutting down from the ceiling,” Dr Romilio said.

Hendrik Klein, co-author and fossil expert from Saurierwelt Paläontologisches Museum in Germany, said the footprints — referred to as ‘Evazoum’, scientifically, the footprint type made by prosauropod dinosaurs — were made on the water-sodden layers of ancient plant debris with the tracks later in-filled by silt and sand.

“This explains why today they occur in an upside-down position right above our heads,” Mr Klein said.

“After millions of years, the plant material turned into coal which was extracted by the miners to reveal a ceiling of siltstone and sandstone, complete with the natural casts of dinosaur footprints.”

The mine has long since closed, but fortunately, in 1964, geologists and the Queensland Museum mapped the trackway and made plaster casts, now used in current research.

“We made a virtual 3D model of the dinosaur footprint that was emailed to team members across the world to study,” Mr Klein said.

“The more we looked at the footprint and toe impression shapes and proportions, the less they resembled tracks made by predatory dinosaurs — this monster dinosaur was definitely a much friendlier plant-eater.

“This is still a significant discovery even if it isn’t a scary Triassic carnivore.

“This is the earliest evidence we have for this type of dinosaur in Australia, marking a 50-million-year gap before the first quadrupedal sauropod fossils known.”

The dinosaur footprint is on display at the Queensland Museum, Brisbane.

Reference:
Anthony Romilio, Hendrik Klein, Andréas Jannel, Steven W. Salisbury. Saurischian dinosaur tracks from the Upper Triassic of southern Queensland: possible evidence for Australia’s earliest sauropodomorph trackmaker. Historical Biology, 2021; 1 DOI: 10.1080/08912963.2021.1984447

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

Early dinosaurs may have lived in social herds as early as 193 million years ago

Artist’s impression of Spinosaurus. Credit: Davide Bonadonna
Artist’s impression of Spinosaurus. Credit: Davide Bonadonna

To borrow a line from the movie “Jurassic Park:” Dinosaurs do move in herds. And a new study shows that the prehistoric creatures lived in herds much earlier than previously thought.

In a paper appearing in Scientific Reports, researchers from MIT, Argentina, and South Africa detail their discovery of an exceptionally preserved group of early dinosaurs that shows signs of complex herd behavior as early as 193 million years ago — 40 million years earlier than other records of dinosaur herding.

Since 2013, members of the team have excavated more than 100 dinosaur eggs (about the size of chicken eggs) and the partial skeletons of 80 juvenile and adult dinosaurs from a rich fossil bed in southern Patagonia.

Using X-ray imaging, they were able to examine the eggs’ contents without breaking them apart, and discovered preserved embryos within, which they used to confirm that the fossils were all members of Mussaurus patagonicus — a plant-eating dinosaur that lived in the early Jurassic period and is classified as a sauropodomorph, a predecessor of the massive, long-necked sauropods that later roamed the Earth.

Surprisingly, the researchers observed that the fossils were grouped by age: Dinosaur eggs and hatchlings were found in one area, while skeletons of juveniles were grouped in a nearby location. Meanwhile, remains of adult dinosaurs were found alone or in pairs throughout the field site.

This “age segregation,” the researchers believe, is a strong sign of a complex, herd-like social structure. The dinosaurs likely worked as a community, laying their eggs in a common nesting ground. Juveniles congregated in “schools,” while adults roamed and foraged for the herd.

“This may mean that the young were not following their parents in a small family structure,” says team member Jahandar Ramezani, a research scientist in MIT’s Department of Earth, Atmospheric and Planetary Sciences. “There’s a larger community structure, where adults shared and took part in raising the whole community.”

Ramezani dated ancient sediments among the fossils and determined that the dinosaur herd dates back to around 193 million years ago, during the early Jurassic period. The team’s results represent the earliest evidence of social herding among dinosaurs.

Living in herds may have given Mussaurus and other social sauropodomorphs an evolutionary advantage. These early dinosaurs originated in the late Triassic, shortly before an extinction event wiped out many other animals. For whatever reason, sauropodomorphs held on and eventually dominated the terrestrial ecosystem in the early Jurassic.

“We’ve now observed and documented this earliest social behavior in dinosaurs,” Ramezani says. “This raises the question now of whether living in a herd may have had a major role in dinosaurs’ early evolutionary success. This gives us some clues to how dinosaurs evolved.”

A fossil flood

Since 2013, paleontologists on the team have worked in the Laguna Colorada Formation, a site in southern Patagonia that is known for bearing fossils of early sauropodomorphs. When scientists first discovered fossils within this formation in the 1970s, they named them Mussaurus for “mouse lizard,” as they assumed the skeletons were of miniature dinosaurs.

Only much later did scientists, including members of the Argentinian team, discover bigger skeletons, indicating Mussaurus adults were much larger than their rodent namesakes. The name stuck, however, and the team has continued to unearth a rich collection of Mussaurus fossils from a small, square kilometer of the formation.

The fossils they have identified so far were found in three sedimentary layers spaced close together, indicating that the region may have been a common breeding ground where the dinosaurs returned regularly, perhaps to take advantage of favorable seasonal conditions.

Among the fossils they uncovered, the team discovered a group of 11 articulated juvenile skeletons, intertwined and overlapping each other, as if they had been suddenly thrown together. In fact, judging from the remarkably preserved nature of the entire collection, the team believes this particular herd of Mussaurus died “synchronously,” perhaps quickly buried by sediments.

Based on evidence of ancient flora in the nearby outcrops, the Laguna Colorada Formation has long been assumed to be relatively old on the dinosaur timescale. The team wondered: Could these dinosaurs have been herding from early on?

“People already knew that in the late Jurassic and Cretaceous, the large herbivore dinosaurs exhibited social behavior — they lived in herds and had nesting spots,” Ramezani says. “But the question has always been, when was the earliest time for such herding behavior?”

A gregarious line

To find out, Diego Pol, a paleontologist at the Egidio Feruglio Paleontological Museum in Argentina who led the study, looked for samples of volcanic ash among the fossils to send to Ramezani’s lab at MIT. Volcanic ash can contain zircon — mineral grains contaning uranium and lead, the isotopic ratios of which Ramezani can precisely measure. Based on uranium’s half-life, or the time it takes for half of the element to decay into lead, he can calculate the age of the zircon and the ash in which it was found. Ramezani successfully identified zircons in two ash samples, all of which he dated to around 193 million years old.

Since the volcanic ash was found in the same sediment layers as the fossils, Ramezani’s analyses strongly suggest that the dinosaurs were buried at the same time the ash was deposited. A likely scenario may have involved a flash flood or windblown dust that buried the herd, while ash from a distant eruption happened to drift over and, luckily for science, deposit zircons in the sediments.

Taken together, the team’s results show that Mussaurus and possibly other dinosaurs evolved to live in complex social herds as early as 193 million years ago, around the dawn of the Jurassic period.

Scientists suspect that two other types of early dinosaurs — Massospondylus from South Africa and Lufengosaurus from China — also lived in herds around the same time, although the dating for these dinosaurs has been less precise. If multiple separate lines of dinosaurs lived in herds, the researchers believe the social behavior may have evolved earlier, perhaps as far back as their common ancestor, in the late Triassic.

“Now we know herding was going on 193 million years ago,” Ramezani says. “This is the earliest confirmed evidence of gregarious behavior in dinosaurs. But paleontological understanding says, if you find social behavior in this type of dinosaur at this time, it must have originated earlier.”

This research was supported, in part, by National Science Foundation in the U.S. and the National Scientific and Technical Research Council of Argentina.

Reference:
Pol, D., Mancuso, A.C., Smith, R.M.H. et al. Earliest evidence of herd-living and age segregation amongst dinosaurs. Sci Rep, 2021 DOI: 10.1038/s41598-021-99176-1

Note: The above post is reprinted from materials provided by Massachusetts Institute of Technology. Original written by Jennifer Chu.

What to do if you find fossils or artifacts

A trilobite fossil, Redlichia rex found at Emu Bay, Kangaroo Island – a marine creature that lived over 500 million years ago during the Cambrian period. Credit: Macquarie University
A trilobite fossil, Redlichia rex found at Emu Bay, Kangaroo Island – a marine creature that lived over 500 million years ago during the Cambrian period. Credit: Macquarie University

Six years ago, grazier Robert Hacon was driving around his cattle property in outback Queensland when he drove over what he thought was a cow skull.

When he turned his ute around, on the ground in front of him lay the 1.6 meter jaw bone of a Kronosaurus queenslandicus—an 11-meter-long marine creature with a crocodile-like head that lived about 100 million years ago. It turned out to be the most intact Kronosaurus jawbone ever found.

A year later, construction workers building Sydney’s light rail in Randwick uncovered tens of thousands of spearheads and tools used by Bidjigal or Gadigal peoples of the Eora nation, including evidence they traded with people from what is now the Hunter Valley.

So what should you do if you stumble on a fossil or an Indigenous artifact in your backyard, at the beach, in a local park, on a bushwalk or on a rural property?

Macquarie University Biological Sciences Masters student Sally Hurst is trying to answer these questions. She’s created a website Found a Fossil to inform people what steps to take, who to contact and what your rights are over ownership of the fossil or artifact.

Honorary Professor in the Department of Biological Sciences, Glenn Brock, says the site will potentially engage thousands of people around Australia online who might have found an important fossil or an artifact and are not sure what to do next.

“It greatly improves our chances that more finds will end up in the hands of scientists who’ll recognize their significance,” says Brock who supervised Hurst during the project.

The website is part of Hurst’s research which includes surveying people’s attitudes to fossils and artifacts Australia-wide.

“There’s a huge gap in knowledge and information and so I saw it as an opportunity to do something,” Hurst says. “I’m passionate about paleontology, archaeology and also an enthusiastic science communicator and this project has combined all my interests.”

What most intrigues Hurst is that through her website she’s engaging members of the public to become citizen scientists. She encourages them to photograph, record the GPS location, determine if there’s other similar objects nearby and then report their find.

“Fossils are really important,” Hurst says. “They give us information about the evolution and extinction of plant and animal species. They also tell us about our changing environment. We need to understand this to adapt to future changes.” Similarly, learning about artifacts deepens our understanding of our shared culture and our history.

Own the land, own the fossil

The good news is that if you find a fossil on your private property in NSW, then you own it and you can decide what to do with it, says Hurst. “But you still should inform your local council or museum, because if it’s a rare find, then it will contribute to our scientific knowledge.”

Also, it’s important to report it for preservation purposes. “If it’s been in the ground for a long time and then a storm or some kind of digging disturbs it, and it’s suddenly exposed to the air, it could rapidly deteriorate. A museum will know how best to take care of it,” she says.

If you discover the fossil in a national park, on a beach or someone else’s private property then you’ll have to get the landowner’s permission for what to do next.

Spread the knowledge

Finding a cultural artifact involves similar steps, Hurst says. After growing up on a property in central NSW, Hurst knew of many farmers who had a box full of Aborignial stone tools at the back of a cupboard, unsure of who to talk to about it.

“If you find an Aboriginal or Torres Strait Islander artifact on your property it does not affect your land ownership at all—you’re just encouraged not to disturb it as it’s part of the oldest living culture and people want to interpret it. So the best thing is to inform your local council or Indigenous community.”

On her website, Hurst also includes contact details to report or donate your discovery to the Australian Museum and different state museums, as well state cultural heritage guidelines and sites. It also links you to Fossils Australia to identify your fossil.

To further inform her website content, Hurst is conducting a survey of Macquarie University students to find out what they would do if they found a fossil or artifact. Early next year, she’ll launch an Australia-wide survey as part of her Masters project to gather information about what people would do if they did find something.

“My hope is that this project, and the website resources, will contribute towards the protection of Australia’s natural and cultural heritage for the future,” she says.

Visit Found a Fossil if you have found a fossil or artifact and would like more information on what to do next.

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

Grass found in Baltic amber

Eograminis balticus
Eograminis balticus

Amber research by the Oregon State University College of Science has produced the first definite identification of grass in fossilized tree resin from the Baltic region, home to the world’s most well-known amber deposits.

The specimen studied by George Poinar Jr., named Eograminis balticus, also represents the first fossil member of Arundinoideae, a subfamily of the widespread Poaceae family that includes cereal grasses, bamboos and many species found in lawns and natural grasslands.

Findings, now in preprint, will be published in the International Journal of Plant Sciences.

Blown or shoved against a resin-producing tree, the fossil grass lost one of its spikelets some 40 or 50 million years ago, along with an accompanying insect that had been feeding on it.

A spikelet is one unit of inflorescence, or flower arrangement, and consists of two glumes and one or more florets. A glume is a leaflike structure below the flower cluster, and a floret is one of the small flowers in the cluster.

The fossil spikelet is the first definite evidence that grasses were among the various plants in the Baltic amber forest.

“The discovery not only adds a new plant group to the extensive flora that have been described from Baltic amber but provides new insights into the forest habitat the amber came from, a controversial topic in this field of study,” said Poinar, an international expert in using plant and animal life forms preserved in amber to learn more about the biology and ecology of the distant past.

Poinar says some scientists have proposed that fossiliferous amber from the Baltic region was formed in tropical and subtropical woods, and others say it came from a humid, marshy, warm-temperate forest.

“Our new grass suggests that for at least a time the habitat was warm-temperate, like you see today in mixed deciduous and conifer forests,” said Poinar, who collaborated on the study with Roberg Soreng of the Smithsonian Institution. “Present on the spikelet is an immature grasshopper-like insect and a leaf-spot fungal spore that provide information on the microhabitat of the fossil grass. The spikelet has structural and developmental features that existed in early Cenozoic grasses and establishes an important calibration point for future studies on the origin and splitting of genera in its subtribe.”

Because of the excellent preservation of the spikelet, observations could be made under direct light with both stereoscopic and compound microscopes, Poinar said.

“The spikelet has some features of members of the extant wetland genus Molinia in the tribe Molinieae, subtribe Moliniinae,” Poinar said. “Molinia species are concentrated around the Baltic Sea, but some of those species’ characteristics are different from what we see in this fossil.”

Informally known as moor grass, Molinia is a wetland genus. In addition to the Baltic region, Molinia is found in sand in habitats ranging from coastal to subalpine, and in fens and sphagnum bogs in forests. A fen is a peat-accumulating wetland that is fed by surface or ground water rich in minerals.

The Eograminis balticus spikelet specimen originated from the Samland Peninsula in the Kalinin District of the Russian Federation, Poinar said.

The name of the genus derives from the Latin words for age (aeon) and grass (graminis).

Reference:
George Poinar, Robert J. Soreng. A New Genus and Species of Grass, Eograminis balticus (Poaceae: Arundinoideae), in Baltic Amber. International Journal of Plant Sciences, 2021; 000 DOI: 10.1086/716781

Note: The above post is reprinted from materials provided by Oregon State University. Original written by Steve Lundeberg.

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