WFS News: Tanis: Fossil found of dinosaur killed in asteroid strike

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Scientists have presented a stunningly preserved leg of a dinosaur.

The limb, complete with skin, is just one of a series of remarkable finds emerging from the Tanis fossil site in the US State of North Dakota.

But it’s not just their exquisite condition that’s turning heads – it’s what these ancient specimens are purported to represent.

The claim is the Tanis creatures were killed and entombed on the actual day a giant asteroid struck Earth.

The day 66 million years ago when the reign of the dinosaurs ended and the rise of mammals began.

Very few dinosaur remains have been found in the rocks that record even the final few thousand years before the impact. To have a specimen from the cataclysm itself would be extraordinary.

Sir David will review the discoveries, many that will be getting their first public viewing.

Along with that leg, there are fish that breathed in impact debris as it rained down from the sky.

We see a fossil turtle that was skewered by a wooden stake; the remains of small mammals and the burrows they made; skin from a horned triceratops; the embryo of a flying pterosaur inside its egg; and what appears to be a fragment from the asteroid impactor itself.

“We’ve got so many details with this site that tell us what happened moment by moment, it’s almost like watching it play out in the movies. You look at the rock column, you look at the fossils there, and it brings you back to that day,” says Robert DePalma, the University of Manchester, UK, graduate student who leads the Tanis dig.

It’s now widely accepted that a roughly 12km-wide space rock hit our planet to cause the last mass extinction.

The impact site has been identified in the Gulf of Mexico, off the Yucatan Peninsula. That’s some 3,000km away from Tanis, but such was the energy imparted in the event, its devastation was felt far and wide.

The North Dakota fossil site is a chaotic jumble.

The remains of animals and plants seem to have been rolled together into a sediment dump by waves of river water set in train by unimaginable earth tremors. Aquatic organisms are mixed in with the land-based creatures.

The sturgeon and paddlefish in this fossil tangle are key. They have small particles stuck in their gills. These are the spherules of molten rock kicked out from the impact that then fell back across the planet. The fish would have breathed in the particles as they entered the river.

The spherules have been linked chemically and by radiometric dating to the Mexican impact location, and in two of the particles recovered from preserved tree resin there are also tiny inclusions that imply an extra-terrestrial origin.

“When we noticed there were inclusions within these little glass spherules, we chemically analysed them at the Diamond X-ray synchrotron near Oxford,” explains Prof Phil Manning, who is Mr DePalma’s PhD supervisor at Manchester.

“We were able to pull apart the chemistry and identify the composition of that material. All the evidence, all of the chemical data, from that study suggests strongly that we’re looking at a piece of the impactor; of the asteroid that ended it for the dinosaurs.”
Sir David examines the remains of a triceratops dinosaur

Sir David examines the remains of a triceratops dinosaur

The existence of Tanis, and the claims made for it, first emerged in the public sphere in the New Yorker Magazine in 2019. This caused a furore at the time.

Science usually demands the initial presentation of new discoveries is made in the pages of a scholarly journal. A few peer-reviewed papers have now been published, and the dig team promises many more as it works through the meticulous process of extracting, preparing and describing the fossils.

To make its TV programme, the BBC called in outside consultants to examine a number of the finds.

Prof Paul Barrett from London’s Natural History Museum looked at the leg. He’s an expert in ornithischian (mostly plant-eating) dinosaurs.

“It’s a Thescelosaurus. It’s from a group that we didn’t have any previous record of what its skin looked like, and it shows very conclusively that these animals were very scaly like lizards. They weren’t feathered like their meat-eating contemporaries.

“This looks like an animal whose leg has simply been ripped off really quickly. There’s no evidence on the leg of disease, there are no obvious pathologies, there’s no trace of the leg being scavenged, such as bite marks or bits of it that are missing,” he tells me.

“So, the best idea that we have is that this is an animal that died more or less instantaneously.”

The big question is whether this dinosaur did actually die on the day the asteroid struck, as a direct result of the ensuing cataclysm. The Tanis team thinks it very likely did, given the limb’s position in the dig sediments.

If that is the case, it would be quite the discovery.

But Prof Steve Brusatte from University of Edinburgh says he’s sceptical – for the time being.

He’s acted as another of the BBC’s outside consultants. He wants to see the arguments presented in more peer-reviewed articles, and for some palaeo-scientists with very specific specialisms to go into the site to give their independent assessment.

Prof Brusatte says it’s possible, for example, that animals that had died before the impact were exhumed by the violence on the day and then re-interred in a way that made their deaths appear concurrent.

“Those fish with the spherules in their gills, they’re an absolute calling card for the asteroid. But for some of the other claims – I’d say they have a lot circumstantial evidence that hasn’t yet been presented to the jury,” he says.

“For some of these discoveries, though, does it even matter if they died on the day or years before? The pterosaur egg with a pterosaur baby inside is super-rare; there’s nothing else like it from North America. It doesn’t all have to be about the asteroid.”

A pterosaur embryo inside an egg, found at the Tanis site...

A pterosaur embryo inside an egg, found at the Tanis site…

There’s no doubting the pterosaur egg is special.

With modern X-ray technology it’s possible to determine the chemistry and properties of the egg shell. It was likely leathery rather than hard, which may indicate the pterosaur mother buried the egg in sand or sediment like a turtle.

It’s also possible with X-ray tomography to extract virtually the bones of the pterosaur chick inside, to print them and reconstruct what the animal would have looked like. Mr DePalma has done this.

The baby pterosaur was probably a type of azhdarchid, a group of flying reptiles whose adult wings could reach more than 10m from tip to tip.

Mr DePalma gave a special lecture on the Tanis discoveries to an audience at the US space agency Nasa’s Goddard Space Flight Center on Wednesday. He and Prof Manning will also present their latest data to the European Geosciences Union General Assembly in May.

Dinosaurs: The Final Day with Sir David Attenborough will be broadcast on BBC One on 15 April at 18:30 BST. A version has been made for the US science series Nova on the PBS network to be broadcast later in the year.

Rock layers before and after asteroid impact

Rock layers before and after asteroid impact

Source : https://www.bbc.com/news/science-environment-61013740 article by Jonathan Amos
Science correspondent,@BBCAmoson Twitter

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WFS News: Earliest geochemical evidence of plate tectonics found in 3.8-billion-year-old crystal

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A handful of ancient zircon crystals found in South Africa hold the oldest evidence of subduction, a key element of plate tectonics, according to a new study published today in AGU Advances, AGU’s journal for high-impact, open-access research and commentary across the Earth and space sciences.

These rare time capsules from Earth’s youth point to a transition around 3.8 billion years ago from a long-lived, stable rock surface to the active processes that shape our planet today, providing a new clue in a hot debate about when plate tectonics was set in motion.

Earth’s crust and the top layer of mantle just under it are broken up into rigid plates that move slowly on top of viscous but mobile lower layers of mantle rock. Heat from Earth’s core drives this slow but inexorable motion, responsible for volcanoes, earthquakes, and the uplift of mountain ranges.

Estimates for when this process revved up and modern crust formed range from over 4 billion years ago to just 800 million years ago. Uncertainty arises because the geologic record from Earth’s youth is sparse, due to the surface recycling effect of plate tectonics itself. Almost nothing remains from the Hadean Eon, Earth’s first 500 million years.

“The Hadean Earth is this big mystery box,” said Nadja Drabon, a geologist at Harvard University and the lead author of the new study.

Tiny time capsules

In an exciting step forward in solving this mystery, in 2018 Drabon and her colleagues unearthed a chronological series of 33 microscopic zircon crystals from a rare, ancient block of crust in the Barberton Greenstone Belt in South Africa, that formed at different times over a critical 800-million-year span from 4.15 to 3.3 billion years ago.

Zircon is a relatively common accessory mineral in Earth’s crust, but ancient representatives from the Hadean Eon, 4 to 4.56 billion years ago, are exceedingly rare, found in only 12 places on Earth, and usually in numbers fewer than three at each location.

Map of the Barberton greenstone belt and detrital zircon geochronology of the Green Sandstones Bed (GSB). (a) Generalized map of the Barberton Greenstone Belt and (b) a detailed geological map of the study area modified from Lowe et al. (2012) with sample locations. Sample NAD-106 was taken from the GSB type locality and corresponds to sample numbers SA 22 and SA 51 of Byerly et al. (2018) Sample NAD-180 was taken from a second locality which corresponds to SA 811 of Byerly et al. (2018). (c) Probability density plots (PDPs) of 207Pb/206Pb detrital zircon geochronology from different stratigraphic intervals of the GSB. Insets represent detailed age spectra of zircons >3600 Ma. MDA = maximum depositional age. Colors of PDPs highlight different age clusters.

Map of the Barberton greenstone belt and detrital zircon geochronology of the Green Sandstones Bed (GSB). (a) Generalized map of the Barberton Greenstone Belt and (b) a detailed geological map of the study area modified from Lowe et al. (2012) with sample locations. Sample NAD-106 was taken from the GSB type locality and corresponds to sample numbers SA 22 and SA 51 of Byerly et al. (2018) Sample NAD-180 was taken from a second locality which corresponds to SA 811 of Byerly et al. (2018). (c) Probability density plots (PDPs) of 207Pb/206Pb detrital zircon geochronology from different stratigraphic intervals of the GSB. Insets represent detailed age spectra of zircons >3600 Ma. MDA = maximum depositional age. Colors of PDPs highlight different age clusters.

Hafnium isotopes and trace elements preserved in the Greenstone Belt zircons told a story about the conditions on Earth at the time they crystalized. Zircons 3.8-billion-years-old and younger appeared to have formed in rock experiencing pressures and melting similar to modern subduction zones, suggesting the crust may have started moving.

“When I say plate tectonics, I’m specifically referring to an arc setting, when one plate goes under another and you have all that volcanism — think of the Andes, for example, and the Ring of Fire,” Drabon said, describing a classic example of subduction.

“At 3.8 billion years there is a dramatic shift where the crust is destabilized, we have new rocks forming and we see geochemical signatures becoming more and more similar to what we see in modern plate tectonics,” Drabon said.

In contrast, the older zircons preserved evidence of a global cap of “protocrust” derived from remelting mantle rock that had remained stable for 600 million years, the study found.

Signs of global change

The new study found a similar transition to conditions resembling modern subduction in zircons from other locations around the world, dating to within about 200 million years of the South African zircons.

“We see evidence for a significant change on the Earth around 3.8 to 3.6 billion years ago and evolution toward plate tectonics is one clear possibility.” Drabon said.

While not conclusive, the results suggest a global change may have begun, Drabon said, possibly starting and stopping in scattered locations before settling into the efficient global engine of constantly moving plates we see today.

Plate tectonics shapes Earth’s atmosphere as well as its surface. Release of volcanic gasses and production of new silicate rock, which consumes large amounts carbon dioxide from the atmosphere, temper large temperature swings from too much or too little greenhouse gas.

“Without all of the recycling and new crust forming, we might be going back and forth between boiling hot and freezing cold,” Drabon said. “It’s kind of like a thermostat for the climate.”

Plate tectonics has, so far, only been observed on Earth, and may be essential to making a planet livable, Drabon said, which makes the origins of plate motions of interest in research into the early development of life.

“The record we have for the earliest Earth is really limited, but just seeing a similar transition in so many different places makes it really feasible that it might have been a global change in crustal processes,” Drabon said. “Some kind of kind of reorganization was happening on Earth.”

  1. Nadja Drabon, Benjamin L. Byerly, Gary R. Byerly, Joseph L. Wooden, Michael Wiedenbeck, John W. Valley, Kouki Kitajima, Ann M. Bauer, Donald R. Lowe. Destabilization of Long‐Lived Hadean Protocrust and the Onset of Pervasive Hydrous Melting at 3.8 GaAGU Advances, 2022; 3 (2) DOI: 10.1029/2021AV000520
American Geophysical Union. “Earliest geochemical evidence of plate tectonics found in 3.8-billion-year-old crystal: Tiny zircons found in South Africa point to an early start for the active global process that shapes Earth’s surface and climate.” ScienceDaily. ScienceDaily, 21 April 2022.www.sciencedaily.com/releases/2022/04/220421131008.htm>.
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WFS News: Scientists claim they’ve found a perfectly preserved dinosaur fossil killed when the mass extinction asteroid hit the earth 66 million years ago

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Scientists say that the perfectly preserved leg of a Thescelosaurus dinosaur, complete with scaly skin, can be dated back to the mass extinction event because of the presence of debris from the impact, the BBC said.

It is widely believed that when the 7.5 mile-wide asteroid, approximately the size of Mount Everest, hit the Gulf of Mexico, all non-avian dinosaurs on earth were wiped out.

The skin of a triceratops, perfectly preserved in this fossil found at the Tanis site, is being filmed by the BBC documentary crew.BBC Studios/Eric Burge

The skin of a triceratops, perfectly preserved in this fossil found at the Tanis site, is being filmed by the BBC documentary crew.BBC Studios/Eric Burge

An upcoming BBC documentary looks at a slew of fossils found at the Tanis site in North Dakota. It includes the Thescelosaurus leg,  and the skin of a triceratops, pictured above.

The site is rich in well-preserved fossils, including fish, a turtle, and even the embryo of a flying pterosaur encased in an egg.

Scientists believe that tiny glass-like particles of molten rock lodged in the gills of fish fossils found at the site were kicked up by the asteroid’s explosive impact, the BBC said.

“We’ve got so many details with this site that tells us what happened moment by moment. It’s almost like watching it play out in the movies,” Robert DePalma, a graduate student from the University of Manchester, UK, who leads the Tanis dig, told the BBC.

Prof Phil Manning, DePalma’s Ph.D. supervisor at Manchester, told BBC Radio 4’s Today program that the discovery was “absolutely bonkers” and something he “never dreamt in all my career.”

“The time resolution we can achieve at this site is beyond our wildest dreams. This really should not exist, and it’s absolutely gobsmackingly beautiful,” Manning said.

The documentary, which David Attenborough presents, was filmed over three years and will be released on April 15.

In the BBC documentary, Robert DePalma, a relative of film director Brian De Palma, can be seen sporting an Indiana Jones-style fedora and tan shirt.

He christened the paleontological site “Tanis,” the last resting place of the Ark of the Covenant in the 1981 film “Raiders of the Lost Ark,” per The New Yorker.

The findings from Tanis, and the work of DePalma, have attracted controversy over the years.

The New Yorker first wrote about the Tanis site in 2019 before presenting the findings in an academic journal.

While paleontologists usually cede their rights and curation of the fossils to institutions, DePalma, who had collected few academic laurels until the discovery of the site, insists on contractual clauses that give him oversight over the specimens. He has controlled how the fossils are presented, per The New Yorker.

In response to the article, Kate Wong, science editor of Scientific American, said in a 2019 tweet that the findings from the site “have met with a good deal of skepticism from the paleontology community.”

A few peer-reviewed papers have since been published, and the BBC said that the dig team promises more.

The BBC also said that it has called outside consultants to verify the specimens.

Spherules are seen in sediment.BBC Studios/Ali Pares

Spherules are seen in sediment.BBC Studios/Ali Pares

Prof Paul Barrett from London’s Natural History Museum looked at the leg and said it was a Thescelosaurus that likely died “more or less instantaneously.”

“It’s from a group that we didn’t have any previous record of what its skin looked like, and it shows very conclusively that these animals were very scaly like lizards. They weren’t feathered like their meat-eating contemporaries,” Barrett told the BBC.

However, Prof Steve Brusatte, an outside consultant on the documentary from the University of Edinburgh, told the BBC he was skeptical about the dinosaurs’ findings for now and would like to see the hypotheses being subjected to the scrutiny of peer review.

“Those fish with the spherules in their gills, they’re an absolute calling card for the asteroid. But for some of the other claims — I’d say they have a lot of circumstantial evidence that hasn’t yet been presented to the jury,” he said.

Prof Brusatte said that it is possible that some of the animals died before the asteroid strike but could have been exhumed and then buried again by the impact.

But ultimately, Brussate said the quality of the fossils trumps the controversy about the event’s timing.

“For some of these discoveries, though, does it even matter if they died on the day or years before? The pterosaur egg with a pterosaur baby inside is super-rare; there’s nothing else like it from North America. It doesn’t all have to be about the asteroid.”

Source: https://www.businessinsider.in/science/news/scientists-claim-theyve-found-a-perfectly-preserved-dinosaur-fossil-killed-when-the-mass-extinction-asteroid-hit-the-earth-66-million-years-ago/articleshow/90760067.cms

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WFS News: Well-preserved new dinosaur fossil found in Alberta

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six years after miners had discovered it by accident, the best preserved dinosaur fossil was was unveiled at Canada’s Royal Tyrrell Museum of Paleontology.

Dinosaur fossils are not more than a rock for the casual observers, before they are put into the museum.

However, the observers this time were in for a surprise. The remains of the dinosaur were so well-preserved that it looked more like a statue than a fossil, as per a report by the National Geographic.

The remnants of skin which are fossilized, cover the armor plates on the dinosaur’s remains, which are petrified from the head to the hips. “We don’t just have a skeleton. We have a dinosaur as it would have been,” Caleb Brown said, National Geographic reported.

The accidental discovery of the fossil has an interesting story. As per Science Alert, on March 21, 2011, Shawn Funk was digging in Alberta’s Millennium Mine with a mechanical backhoe, when he hit “something much harder than the surrounding rock.”

A closer look revealed something that looked like no rock Funk had ever seen, just “row after row of sandy brown disks, each ringed in gunmetal gray stone”.

What he had found was a 2,500-pound (1,130 kg) dinosaur fossil, which was soon shipped to the museum in Alberta, where technicians scraped extraneous rock from the fossilised bone and experts examined the specimen.

“I couldn’t believe my eyes – it was a dinosaur,” Donald Henderson, the curator of dinosaurs at the museum, told Alberta Oil.

“When we first saw the pictures we were convinced we were going to see another plesiosaur (a more commonly discovered marine reptile).”

More specifically, it was the snout-to-hips portion of a nodosaur, a “member of the heavily-armored ankylosaur subgroup,” that roamed during the Cretaceous Period, according to Smithsonian.

Usually, only the bones and teeth are preserved. Some other dinosaur fossils have been found in flat “mummified” form. These fossils maintain a shape that is so near to life that it “might have been walking around a couple of weeks ago,” Jakob Vinther, a paleobiologist, told National Geographic.

According to The TeCake, around 110-million-year-old fossil revealed a new species of nodosaur having thorny armor which is used to protect them against the predators. It also had two, 20-inch-long spikes which protruded from its shoulders.

They were a group of heavy herbivores, which used to walk on four legs, and somewhat resembled a cross between a lizard and a lion having the only difference of being covered in scales. “These guys were like four-footed tanks,” dinosaur tracker Ray Stanford said in The Washington Post in the year 2012.

This particular species of them was 18 feet (5.4 meters) long and weighed around 3,000 pounds (1,360 kilograms).

“The more I look at it, the more mind-boggling it becomes. Fossilized remnants of skin still cover the bumpy armor plates dotting the animal’s skull. Its right forefoot lies by its side, its five digits splayed upward. I can count the scales on its sole.”

Caleb Brown, a postdoctoral researcher at the museum, says “We don’t just have a skeleton”. “We have a dinosaur as it would have been.”

Eventually, this creature of land floated out to the sea to where it was once found and sank to the bottom. According to the researchers, it was on a river’s edge, probably drinking water, when a flood swept it away.

The minerals present there quickly “infiltrated the skin and armor and cradled its back, ensuring that the dead nodosaur would keep its true-to-life form as eons’ worth of rock piled atop it.”

However, if one needs to reach out to the bones of the dinosaur’s it would require destroying its outer layers.

CT scans done by the National Geographic Society has revealed a little, as the rocks are very opaque.

“Even partially complete skeletons remain elusive,” Smithsonian said in a report.

Source: Zeenews.com

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WFS News:Forget mammoths: These researchers are exploring bringing back the extinct Christmas Island rat.

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Dinosaurs went extinct 65 million years ago, mammoths 4,000 years ago, and the Christmas Island Rat 119 years ago. Since becoming a popular concept in the 1990s, de-extinction efforts have focused on grand animals with mythical stature, but in a paper published March 9 in the journal Current Biology, a team of paleogeneticists turn their attention to Rattus macleari,and their findings provide insights into the limitations of de-extinction across all species.

De-extinction work is defined by what is unknown. When sequencing the genome of an extinct species, scientists face the challenge of working with degraded DNA, which doesn’t yield all the genetic information required to reconstruct a full genome of the extinct animal. With the Christmas Island rat, which is believed to have gone extinct because of diseases brought over on European ships, evolutionary geneticist Tom Gilbert (@Evohologen) at University of Copenhagen and his colleagues lucked out.

Not only was the team able to obtain almost all of the rodent’s genome, but since it diverged from other Rattus species relatively recently, it shares about 95% of its genome with a living rat, the Norway brown rat. “It was a quite a nice test model,” says Gilbert. “It’s the perfect case because when you sequence the genome, you have to compare it to a really good modern reference.”

After the DNA has been sequenced as well as possible and the genome is matched up against the reference genome of the living species, the scientists identify the parts of the genomes that don’t match up and, in theory, would then use CRISPR technology to gene edit the DNA of the living species to match that of the extinct one. The brown-rat-to-Christmas-Island-rat scenario is a particularly good test case because the evolutionary divergence is similar to that of the elephant and the mammoth.

Though the sequencing of the Christmas Island rat was mostly successful, a few key genes were missing. These genes were related to olfaction, meaning that a resurrected Christmas Island Rat would likely be unable to process smells in the way as it would have originally. “With current technology, it may be completely impossible to ever recover the full sequence, and therefore it is impossible to ever generate a perfect replica of the Christmas Island rat,” says Gilbert.

“It is very, very clear that we are never going to be able to get all the information to create a perfect recovered form of an extinct species,” he says. “There will always be some kind of hybrid.” Though a replica will never be perfect, the key is that scientists are able to edit for the DNA that makes the extinct animal functionally different from the living one.

Gilbert says that in order to make an ecologically functional mammoth, for example, it might be enough to edit elephant DNA to make the animal hairy and able to live in the cold. “If you’re making a weird fuzzy elephant to live in a zoo, it probably doesn’t matter if it is missing some behavioral genes,” he says. “But that brings up a whole lot of ethical questions.”

Gilbert plans to try doing the actual gene editing on rats but would like to start with species that are still living. He intends to begin by doing CRISPR edits on a black rat genome to change it to a Norway brown rat before attempting to resurrect the Christmas Island rat. Though he is excited about his future research, the whole process still gives him pause. “I think it’s a fascinating idea in technology, but one has to wonder if that’s the best use of money as opposed to keeping the things alive that are still here,” he says.

  1. Jianqing Lin, David Duchêne, Christian Carøe, Oliver Smith, Marta Maria Ciucani, Jonas Niemann, Douglas Richmond, Alex D. Greenwood, Ross MacPhee, Guojie Zhang, Shyam Gopalakrishnan, M. Thomas P. Gilbert. Probing the genomic limits of de-extinction in the Christmas Island ratCurrent Biology, 2022; DOI: 10.1016/j.cub.2022.02.027
Cell Press. “Forget mammoths: These researchers are exploring bringing back the extinct Christmas Island rat.” ScienceDaily. ScienceDaily, 9 March 2022. <www.sciencedaily.com/releases/2022/03/220309111050.htm>.
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WFS News:Large new titanosaurian dinosaur from the Pyrenees

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Researchers from the Institut Català de Paleontologia Miquel Crusafont (ICP), the Conca Dellà Museum (MCD), the Universitat Autònoma de Barcelona (UAB), the University of Zaragoza (UNIZAR) and the NOVA University of Lisbon (UNL) have described the new species of titanosaur dinosaur Abditosaurus kuehnei from the remains excavated at the Orcau-1 site, in the southern Pyrenees (Catalonia, Spain). The semiarticulated 70.5-million-year-old skeleton is the most complete specimen of this herbivorous group of dinosaurs discovered so far in Europe. Moreover, Abditosaurus is the largest titanosaur species found in the Ibero-Armorican island — an ancient region nowadays comprising Iberia and the south of France — representing a senescent individual estimated to be 17,5 meters in length with body mass of 14,000 kg.

The size of this giant is one of the most surprising facts to researchers. “Titanosaurs from the Upper Cretaceous of Europe tend to be small or medium-sized due to their evolution in insular conditions,” explained Bernat Vila, paleontologist at the ICP leading the research. During the Upper Cretaceous (between 83 and 66 million years ago), Europe was a large archipelago made up of dozens of islands. The species that evolved there tend to be relatively small, or even dwarves compared to their relatives living in large landmasses, due primarily to the limitation of food resources in islands. “It is a recurring phenomenon in the history of life on Earth, we have several examples worldwide in the fossil record of this evolutionary trend. That’s why we were astonished by the large dimensions of this specimen,” said Vila.

The fieldwork conducted over several decades unearthed 53 skeletal elements of the specimen. These include several teeth, vertebrae, ribs, and limb, scapular and pelvic bones, as well as a semiarticulated fragment of the neck formed by 12 cervical vertebrae. “We were really lucky, it is unusual to find such complete specimens in the Pyrenees due to its troubled geologic history,” explains Àngel Galobart, ICP researcher and director of the Conca Dellà Museum (Isona, Catalonia).

The excavation of the neck in 2014 was a technical challenge. Once prepared for extraction, the neck was encased in a large block of polyurethane foam, becoming one of the largest jackets ever excavated in Europe.

The history of the research that has led to the description of the new species dates back to 1954, when German paleontologist Walter Kühne collected the first remains and sent them to Madrid. The site fell into oblivion until 1986, when some more remains began to be extracted until a great storm forced the cancellation of the excavation. Subsequently, fieldwork on the site fell again into oblivion until a paleontologist from the ICP resumed systematic excavations in Orcau-1. The story of this finding was featured in the 2017 documentary “Europe’s last giant.” The generic name Abditosaurus means ‘forgotten reptile’ and the specific epithet kuehnei is a tribute to its discoverer.

A migrating dinosaur

In their article published in Nature Ecology & Evolution, researchers conclude that Abditosaurus belongs to a group of saltasaurine titanosaurs from South America and Africa, different from the rest of European titanosaurs that are characterized by a smaller size. These authors hypothesize that the Abditosaurus lineage reached the Ibero-Armorican island taking advantage of a global drop in sea level that reactivated ancient migration routes between Africa and Europe.

“Other evidence support the migration hypothesis,” explains Albert Sellés, paleontologist at the ICP and co-author of the article. “In the same site we have found eggshells of dinosaur species known to have inhabited Gondwana, the southernmost continent.”

The new finding is a major advance in the understanding of the evolution of sauropod dinosaurs at the end of the Cretaceous and brings a new perspective to the phylogenetic and paleobiogeographic puzzle of sauropods in the last 15 million years before their extinction.

In addition to Vila, Sellés and Galobart, Novella Razzolini (Institut Català de Paleontologia Miquel Crusafont and Conca Dellà Museum), Miguel Moreno (Museu de Lurinhã and NOVA University of Lisbon), Iñaki Canudo (Aragosaurus-IUCA Group, University of Zaragoza) and Alejandro Gil (Universitat Autònoma de Barcelona) participated in this study.

“During the Jurassic and Cretaceous, Iberia was the point of connection between Eurasia, Africa and North America. Studying how Abditosaurus relates to the fauna of these continents helps us to understand when there were connections between them, and when they became isolated,” says Miguel Moreno, researcher at the Museu de Lurinhã and NOVA University of Lisbon that has performed the paleobiogeographic study.

The large Cretaceous herbivores

Titanosaurs are a group of sauropod dinosaurs that become very diverse and abundant in the terrestrial ecosystems of the Cretaceous. All of them were quadrupeds and phytophagous. Titanosaurs had a small and pointed skull, with small nail-shaped teeth used to uproot vegetation. Their body was robust, with forelimbs shorter than the hindlimbs and a long necks and tails. Some species sported a skin covered with bony plates named osteoderms that may have served as a protective shield or as a reserve of calcium.

The paleontological sites within the Catalan Pyrenees have provided exceptional dinosaur fossils over the last century. Research is especially significant as its fossil record includes the last vertebrate faunas, including non-avian dinosaurs, that lived in Europe right before the global extinction event that took place 66 million years ago.

On the ICP: The Institut Català de Paleontologia Miquel Crusafont (ICP) is a CERCA center (Centres de Recerca de Catalunya, Generalitat de Catalunya) ascribed to to the Universitat Autònoma de Barcelona (UAB) and devoted to research in vertebrate and human paleontology at the highest international level, as well as the conservation and dissemination of the Catalan paleontological heritage. It is constituted as a public foundation with a board of trustees made up of the Government of Catalonia and the UAB.

Journal Reference:

  1. Bernat Vila, Albert Sellés, Miguel Moreno-Azanza, Novella L. Razzolini, Alejandro Gil-Delgado, José Ignacio Canudo, Àngel Galobart. A titanosaurian sauropod with Gondwanan affinities in the latest Cretaceous of EuropeNature Ecology & Evolution, 2022; DOI: 10.1038/s41559-021-01651-5

Citation: Universitat Autonoma de Barcelona. “Large new titanosaurian dinosaur from the Pyrenees: The skeleton of Abditosaurus kuehnei is the most complete titanosaur fossil discovered so far in Europe.” ScienceDaily. ScienceDaily, 7 February 2022. <www.sciencedaily.com/releases/2022/02/220207124822.htm>.

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WFS News: Fruits of Euphorbiaceae from the Late Cretaceous Deccan Intertrappean Beds of India.

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Just before the closing scenes of the Cretaceous Period, India was a rogue subcontinent on a collision course with Asia. Before the two landmasses merged, however, India rafted over a “hot spot” within the Earth’s crust, triggering one of the largest volcanic eruptions in Earth’s history, which likely contributed to the extinction of the dinosaurs.

In a recent study, scientists excavating the fossilized remains of plant material wedged between layers of volcanic rock describe a new plant species based on the presence of distinctive fruit capsules that likely exploded to disperse their seeds. The fossils may be the oldest fruit discovered to date of the spurge family (Euphorbiaceae), a group of plants with more than 7,000 species, with well-known representatives that include poinsettia, castor oil plant, rubber trees and crotons.

The fossilized fruits were discovered near the village of Mohgaon Kalan in central India, where the remains of the once-widespread volcanic rock lie just beneath the surface in a complex mosaic.

“You can walk around these hills and find chunks of chert that have just weathered up through the topsoil,” said senior author Steven Manchester, curator of paleobotany at the Florida Museum of Natural History. “Some of the best collecting is where farmers have plowed the fields and moved the chunks to the side. For a paleobotanist, it’s like finding little Christmas presents all along the edge of the fields.”

Although there is some uncertainty in the timing, the volcanic eruptions are thought to have lasted for up to 1 million years, occurring in prolonged pulses that blanketed the surrounding landscape in thick lava layers up to 1 mile deep. Today, the basalt rocks leftover from the eruptions, known as the Deccan Traps, cover an area larger than the state of California.

The most violent of the volcanic events, which occurred at the tail end of the Cretaceous, may have been triggered by the asteroid impact half a world away.

“The impact in the Yucatan may have caused seismic perturbations that actually disturbed the regime on the other side of the planet, causing lava to erupt,” Manchester said.

New species grew in stunted forests

Sandwiched between the basalt, paleontologists have found shales, chert, limestone and clays stacked in a giant layer cake of alternating bands, most of which are rich in the fossilized remains of plants and animals. These fossils provide a glimpse into what seem to have been relatively calm periods of stability between massive lava flows.

The newly described species were likely shrubs or small trees that grew near hot springs created by the interaction of groundwater with naturally heated rock beneath the surface, similar to present-day environments in Yellowstone National Park. At the time of their preservation, India was inching its way through the Earth’s equatorial zone, creating warm, humid conditions that supported a number of tropical species, including bananas, aquatic ferns, mallows and relatives of modern crepe myrtles.

Petrified wood is a common find in the Deccan traps, but most of them have small diameters, suggesting a lack of large trees whose conspicuous absence has stumped scientists trying to stitch together the ecological history of the region.

“India was positioned at a low latitude, so we’d expect to find big forest giants. But that’s not what we’re seeing,” Manchester said.

It’s unclear why the trees were unable to obtain greater stature, but Manchester suspects the underlying basalt may have restricted the growth of roots. Alternatively, he said, the plants may have been part of young forests that grew in volcanically active regions, which would have wiped out the surrounding vegetation before it had a chance to mature. “You’re most likely to get fossils preserved when there’s been recent eruptions, which creates a lot of volcanic ash that can bury and preserve plants,” he said.

Scientists peel back the layers of mystery fruit

Fruits from the new species were found pristinely preserved in a matrix of chert by co-author Dashrath Kapgate. But with only the fruits to go on, determining which plants they belonged to required a significant amount of investigative research.

“It didn’t really fit well into any known plant group,” said lead author Rachel Reback, who studied the fossils while working as an undergraduate researcher at the Florida Museum. “We ended up having to take a large number of CT scans not only of the fossils we had but of the fruit of living species as well so that we could directly compare them.”

The researchers ultimately determined the fossils belonged to the spurge family by studying similar fruit specimens provided by the Smithsonian Institution. However, one of the fossils was so unlike anything they’d seen, they determined it represented an entirely new species belonging to the fossil genus Euphorbiotheca.

The orientation of fibers inside the fruit indicated they were likely explosive, a common means of seed dispersal in other euphorbs, including cassava, rubber trees, crown of thorns and castor oil plant. Once the fruit in these species has ripened, they begin to dry out, losing as much as 64% of their original weight, which builds up tension in the rigid outer layers. Once enough water has evaporated, “You hear this loud pop, and the seeds and pieces of the fruit go flying everywhere,” Manchester said, describing the process in rubber trees. “We think this is the case for these two fossil species as well, because we see the same anatomy, where the fibers in the inner and outer layers of the fruit wall are oriented in opposing directions, which helps build torque.”

India an incubation chamber for new groups and species

Fossils like these offer paleontologists tantalizing clues regarding the origin and movement of species. About 140 million years ago, a conjoined India and Madagascar began drifting away from the supercontinent Gondwana in the Southern Hemisphere, carrying with them plants and animals that evolved in isolation throughout the Cretaceous.

By the time India finally slammed into Eurasia, 10 million years after the extinction of the dinosaurs, it had given rise to an incredible diversity of life found nowhere else. It’s likely the first grapes evolved in India, as did the ancestors of whales. As the Himalayas took shape above the sutured landmasses, new groups of insect-eating pitcher plants, flightless birds, lizards, freshwater crabs, scorpions and praying mantises all made their way out of India and into new environments in Europe and Asia.

Manchester hopes these fossils and others like them coming out of the Deccan Traps will help illuminate the distribution of species at a critical time in Earth’s history. “What were the environments in India like at a time when it had not yet connected to Eurasia and how do they compare with other regions at that time?” he said. “It’s like filling in the pieces of a puzzle.”

The team published its results in the International Journal of Plant Sciences.

  1. Rachel G. Reback, Dashrath K. Kapgate, Ken Wurdack, Steven R. Manchester. Fruits of Euphorbiaceae from the Late Cretaceous Deccan Intertrappean Beds of IndiaInternational Journal of Plant Sciences, 2022; 183 (2): 128 DOI: 10.1086/717691
  2. Source: www.sciencedaily.com/releases/2022/02/220217102028.htm

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WFS News: Ankylosaur was sluggish and deaf?

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Ankylosaurs could grow up to eight meters in body length and represent a group of herbivorous dinosaurs, also called ‘living fortresses’: Their body was cluttered with bony plates and spikes. Some of their representatives, the ankylosaurids sometimes possessed a club tail, while nodosaurids had elongated spikes on their necks and shoulders. However, some aspects of their lifestyle are still puzzling.

(A) Outline drawing of Austria with a star marking Muthmannsdorf, the type locality of Struthiosaurus austriacus. (B) Silhouette of Struthiosaurus austriacus (measuring 2.7 m in length here; copyright: Fabrizio De Rossi) and a human for comparison. Photographs (C,D,G,J) and ambient occlusion photogrammetric models (E,F,H,I,K) of the holotype specimen of Struthiosaurus austriacus, IPUW 2349/6, in (C,E) right lateral, (D,F) left lateral, (I) anterior, (J,K) ventral and (G,H) posterior views. a, armour; bo, basioccipital; bs, basisphenoid; bt, basal tuber; ct, crista tuberalis; d, damage; fm, foramen magnum; fo/cr, fenestra ovalis/columellar recess; met, metotic foramen; pbp, posterior branching plexus; sg, stapedial groove; st/pit, sella turcica/pituitary; tov, transverso-occipital vein; uvd, uncertain vascular duct; V3/icg, groove for the mandibular branch of the trigeminal nerve or for the internal carotid; VI, abducens nerve; VII, facial nerve; vcm, dorsal middle cerebral vein; XII, hypoglossal nerve

(A) Outline drawing of Austria with a star marking Muthmannsdorf, the type locality of Struthiosaurus austriacus. (B) Silhouette of Struthiosaurus austriacus (measuring 2.7 m in length here; copyright: Fabrizio De Rossi) and a human for comparison. Photographs (C,D,G,J) and ambient occlusion photogrammetric models (E,F,H,I,K) of the holotype specimen of Struthiosaurus austriacus, IPUW 2349/6, in (C,E) right lateral, (D,F) left lateral, (I) anterior, (J,K) ventral and (G,H) posterior views. a, armour; bo, basioccipital; bs, basisphenoid; bt, basal tuber; ct, crista tuberalis; d, damage; fm, foramen magnum; fo/cr, fenestra ovalis/columellar recess; met, metotic foramen; pbp, posterior branching plexus; sg, stapedial groove; st/pit, sella turcica/pituitary; tov, transverso-occipital vein; uvd, uncertain vascular duct; V3/icg, groove for the mandibular branch of the trigeminal nerve or for the internal carotid; VI, abducens nerve; VII, facial nerve; vcm, dorsal middle cerebral vein; XII, hypoglossal nerve

While many dinosaurs likely lived in groups, at least some ankylosaurs seemed to prefer a lonesome life because of an inferior sense of hearing. That’s what the scientists from the universities of Greifswald and Vienna concluded when they examined the braincase of the Austrian dinosaur with a high-resolution computer tomograph to produce a digital three-dimensional cast.

Fossil braincases, which once housed the brain and other neurosensory tissues, are rare but important for science because these structures can provide insights into the lifestyle of a given animal. For example, the inner ears can hint to auditory capacities and skull orientation.

Struthiosaurus austriacus is a comparably small nodosaurid from the Late Cretaceous (80 Ma) of Austria and comes from a locality near Muthmannsdorf, south of Vienna. The fossil remains of this dinosaur already belonged to the collection of the Institute for Paleontology in Vienna in the 19th century. For their study, Marco Schade (University of Greifswald), Cathrin Pfaff (University of Vienna) and their colleagues examined the tiny (50 mm) braincase to reveal new details of the anatomy and lifestyle of Struthiosaurus austriacus. With these data, it was possible to learn more about its sense of equilibrium and audition.

The results of this study show that Struthiosaurus’ brain was very similar to the brains of its close relatives. For example, the flocculus, an evolutionary old part of the brain, was very small. The flocculus is important for the fixation of the eyes during motions of the head, neck and whole body, which can be very useful if such an animal was trying to target potential competitors or aggressors. “In contrast to its Northamerican relative Euoplocephalus, which had a tail club and a clear flocculus on the brain cast, Struthiosaurus austriacus may rather relied on its body armor for protection,” says Marco Schade. Together with the form of the semicircular canals in the inner ear, this hints towards an exceptionally sluggish lifestyle of this Austrian plant eater. Furthermore, the scientists found the — so far — shortest lagena of a dinosaur. The lagena is the part of the inner ear where audition takes place and its size can help to infer auditory capacities. This study delivers new insights into the evolutionary history of dinosaurs and their world, in which Europe was largely submerged in the ocean.

Citation : Marco Schade, Sebastian Stumpf, Jürgen Kriwet, Christoph Kettler, Cathrin Pfaff. Neuroanatomy of the nodosaurid Struthiosaurus austriacus (Dinosauria: Thyreophora) supports potential ecological differentiations within AnkylosauriaScientific Reports, 2022; 12 (1) DOI: 10.1038/s41598-021-03599-9

Source:  www.sciencedaily.com

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WFS News: A giant millipede 326 million years old found

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Scientists say they have discovered the largest-ever fossil of a giant millipede on a beach in Northumberland, totally by chance.

The millipede, known as Arthropleura, is thought to have been more than 2.5m (8ft) long. It would have weighed about 50kg (eight stone).

The fossil segment was first spotted in 2018 when a large block of sandstone fell on to a beach at Howick Bay.

It will be displayed in Cambridge’s Sedgwick Museum next year.

“It was a complete fluke of a discovery,” said Dr Neil Davies, from Cambridge’s Department of Earth Sciences, who has been analysing the 75cm-long fossil.

“The way the boulder had fallen, it had cracked open and perfectly exposed the fossil, which one of our former PhD students happened to spot when walking by,” Dr Davies said.

When the giant millipede lived, 326 million years ago, the north-east of England had a much more tropical climate than today.

Largest ever Millipede Fossil

This specimen was found in what researchers believe was an old river channel. It may well not actually be the fossil of a dead creature, but an exoskeleton that was shed as the massive millipede grew.

“Finding these giant millipede fossils is rare, because once they died, their bodies tend to disarticulate, so it’s likely that the fossil is a moulted carapace that the animal shed as it grew,” said Mr Davies. “We have not yet found a fossilised head, so it’s difficult to know everything about them.”

One thing that can be said with certainty is, that in common with almost all millipedes, it did not have 1,000 legs – the researchers believe it had at least 32, but it may have been up to 64.

This fossil is just the third Arthropleura to be discovered, and is far older and larger than the two previous specimens which were both found in Germany.

The researchers believe that to get to such a large size, Arthropleura must have had a high-nutrient diet. That could have meant it supplementing a diet of nuts and seeds with small creatures and amphibians.

The fossil is due to go on public display in Cambridge in the new year.

A paper analysing the discovery has been published in the Journal of the Geological Society.

Source: Article by By Jonah Fisher,Environment Correspondent,BBC News

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WFS News: New fossils of Australopithecus sediba reveal a nearly complete lower back

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The lower back of Malapa Hominin 2 in ventral (left) and dorsal (right) views. New second and third lumbar vertebrae (U.W.88–232, U.W.88–233) are positioned at the top, and U.W.88–234 contributes to the upper portion of the fourth lumbar vertebra (U.W.88–127/153/234). The fifth lumbar vertebra (U.W.88–126/138) sits atop the sacrum (U.W.88–137/125). The lower back elements are preserved together in four blocks, each containing multiple elements held together in matrix and/or in partial articulation: (1) The vertebral body fragment of L1 (U.W.88–280) is preserved within the matrix of a block containing the lower thoracic vertebrae (U.W.88–43/114 and U.W.88–44) (Figure 2—figure supplement 1, Figure 3—figure supplement 1); (2) L1 inferior neural arch (U.W.88–281; concealed in matrix), L2 (U.W.88–232), L3 (U.W.88–233), and upper neural arch of L4 (U.W.88–234); (3) the L4 (U.W.88–127) and L5 (U.W.88–126) vertebral bodies, and partial S1 body (U.W.88–125); (4) most of the sacrum (U.W.88–137), the neural arch of L5 (U.W.88–153), the inferior portion of the neural arch of L4 (U.W.88–138).

The lower back of Malapa Hominin 2 in ventral (left) and dorsal (right) views.
New second and third lumbar vertebrae (U.W.88–232, U.W.88–233) are positioned at the top, and U.W.88–234 contributes to the upper portion of the fourth lumbar vertebra (U.W.88–127/153/234). The fifth lumbar vertebra (U.W.88–126/138) sits atop the sacrum (U.W.88–137/125). The lower back elements are preserved together in four blocks, each containing multiple elements held together in matrix and/or in partial articulation: (1) The vertebral body fragment of L1 (U.W.88–280) is preserved within the matrix of a block containing the lower thoracic vertebrae (U.W.88–43/114 and U.W.88–44) (Figure 2—figure supplement 1, Figure 3—figure supplement 1); (2) L1 inferior neural arch (U.W.88–281; concealed in matrix), L2 (U.W.88–232), L3 (U.W.88–233), and upper neural arch of L4 (U.W.88–234); (3) the L4 (U.W.88–127) and L5 (U.W.88–126) vertebral bodies, and partial S1 body (U.W.88–125); (4) most of the sacrum (U.W.88–137), the neural arch of L5 (U.W.88–153), the inferior portion of the neural arch of L4 (U.W.88–138).

Adaptations of the lower back to bipedalism are frequently discussed but infrequently demonstrated in early fossil hominins. Newly discovered lumbar vertebrae contribute to a near-complete lower back of Malapa Hominin 2 (MH2), offering additional insights into posture and locomotion in Australopithecus sediba. We show that MH2 possessed a lower back consistent with lumbar lordosis and other adaptations to bipedalism, including an increase in the width of intervertebral articular facets from the upper to lower lumbar column (‘pyramidal configuration’). These results contrast with some recent work on lordosis in fossil hominins, where MH2 was argued to demonstrate no appreciable lordosis (‘hypolordosis’) similar to Neandertals. Our three-dimensional geometric morphometric (3D GM) analyses show that MH2’s nearly complete middle lumbar vertebra is human-like in overall shape but its vertebral body is somewhat intermediate in shape between modern humans and great apes. Additionally, it bears long, cranially and ventrally oriented costal (transverse) processes, implying powerful trunk musculature. We interpret this combination of features to indicate that A. sediba used its lower back in both bipedal and arboreal positional behaviors, as previously suggested based on multiple lines of evidence from other parts of the skeleton and reconstructed paleobiology of A. sediba.

Cite this articleas: eLife 2021;10:e70447 DOI: 10.7554/eLife.70447

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