WFS News: New Dinosaur Elaphrosaur Unearthed in Australia

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Life reconstruction of the first Australian elaphrosaur. Image credit: Ruairidh Duncan.

Life reconstruction of the first Australian elaphrosaur. Image credit: Ruairidh Duncan.

The newly-discovered dinosaur belongs to Elaphrosaurinae, an enigmatic group of gracile ceratosaurian dinosaurs known from the Late Jurassic period of Africa and Asia, and the early Late Cretaceous period of Argentina.

“Elaphrosaurs were strange looking dinosaurs — they ran low to the ground on two legs, with a slender body, long neck, stubby arms, and a delicate toothless skull,” said Dr. Tim Ziegler, collection manager of vertebrate palaeontology at Museums Victoria.

“They started life eating a wide range of foods, but shed their teeth as they aged. Elaphrosaurs are unusual among theropods because adults had a plant-based diet, rather than hunting prey.”

“Young elaphrosaurs might have hunted the tiny monotremes along with snapping up insects and fruits.”

The 110-million-year-old neck vertebra of the Australian elaphrosaur. Scale bars – 10 mm.Image credit: Stephen Poropat, Museums Victoria.

The 110-million-year-old neck vertebra of the Australian elaphrosaur. Scale bars – 10 mm.Image credit: Stephen Poropat, Museums Victoria.

The nearly complete neck vertebra of the new elaphrosaur was found at the Eric the Red West site — which is part of the Eumeralla Formation — near Cape Otway, Victoria, by Dinosaur Dreaming volunteer Jessica Parker in 2015.

This is the first record of Elaphrosaurinae from Australia and is only the second Cretaceous record of the group worldwide.

In tandem with the recently-described dinosaur Huinculsaurus montesi, the new elaphrosaur extends the record of Elaphrosaurinae by more than 40 million years.

“New discoveries like this elaphrosaur fossil overturn past ideas, and help to interpret discoveries yet to come,” Dr. Ziegler said.

The discovery is reported in a paper in the journal Gondwana Research.

Source: Sci news

journal ref: Stephen F. Poropat et al. First elaphrosaurine theropod dinosaur (Ceratosauria: Noasauridae) from Australia – A cervical vertebra from the Early Cretaceous of Victoria. Gondwana Research, published online May 6, 2020; doi: 10.1016/j.gr.2020.03.009

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Cassowary gloss and a novel form of structural color in birds

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Cassowaries are big flightless birds with blue heads and dinosaur-looking feet; they look like emus that time forgot, and they’re objectively terrifying. They’re also, along with their ostrich and kiwi cousins, part of the bird family that split off from chickens, ducks, and songbirds 100 million years ago. In songbirds and their relatives, scientists have found that the physical make-up of feathers produce iridescent colors, but they’d never seen that mechanism in the group that cassowaries are part of — until now. In a double-whammy of a paper in Science Advances, researchers have discovered both what gives cassowary feathers their glossy black shine and what the feathers of birds that lived 52 million years ago looked like.

Structural gloss in cassowary feathers. (A) Cassowary contour feather sampled from the upper left breast region. (B) Image of a southern cassowary (C. casuarius; photo credit: Albert Straub, CC license). (C) Close-up of feather from (A) showing microstructure. (D) AFM image of the surface of the rachis. (E) TEM image of the rachis. Scale bars, 5 mm (A), 500 μm (C), and 500 nm (E).

Structural gloss in cassowary feathers.(A) Cassowary contour feather sampled from the upper left breast region. (B) Image of a southern cassowary (C. casuarius; photo credit: Albert Straub, CC license). (C) Close-up of feather from (A) showing microstructure. (D) AFM image of the surface of the rachis. (E) TEM image of the rachis. Scale bars, 5 mm (A), 500 μm (C), and 500 nm (E).

“A lot of times we overlook these weird flightless birds. When we’re thinking about what early birds looked like, it’s important to study both of these two sister lineages that would have branched from a common ancestor 80 million or so years ago,” says Chad Eliason, a staff scientist at the Field Museum and the paper’s first author.

“Understanding basic attributes — like how colors are generated — is something we often take for granted in living animals. Surely, we think, we must know everything there is to know? But here, we started with simple curiosity. What makes cassowaries so shiny? Chad found an underlying mechanism behind this shine that was undescribed in birds. These kinds of observations are key to understanding how color evolves and also inform how we think about extinct species,” says Julia Clarke, a paleontologist at the Jackson School of Geosciences at the University of Texas at Austin and the paper’s senior author. Eliason began conducting research for this paper while working with Clarke at the University of Texas as part of a larger project funded by the National Science Foundation (NSF EAR 1355292) to study how flightless birds like cassowaries have evolved their characteristic features.

Sampling map of two Lithornithid fossils from the Green River Formation in Wyoming. Lithornithid specimens AMNH FARB 30578 (A) and AMNH FARB 30560 (B) used with permission from Nesbitt and Clarke (15). Circle color indicates samples predicted as black (black), iridescent (purple), or unknown due to a lack of melanosomes in the sample (unfilled circles). All feather identities are tentative given the disarticulated nature of the specimen, with the exception of some wing and tail remiges. Panels on the right show fossil melanosomes similar to black (sample 5) (C) and iridescent melanosome morphologies in extant birds (samples 7 and 8) (D and E). Scale bars, 500 nm (C to E).

Sampling map of two Lithornithid fossils from the Green River Formation in Wyoming.
Lithornithid specimens AMNH FARB 30578 (A) and AMNH FARB 30560 (B) used with permission from Nesbitt and Clarke (15). Circle color indicates samples predicted as black (black), iridescent (purple), or unknown due to a lack of melanosomes in the sample (unfilled circles). All feather identities are tentative given the disarticulated nature of the specimen, with the exception of some wing and tail remiges. Panels on the right show fossil melanosomes similar to black (sample 5) (C) and iridescent melanosome morphologies in extant birds (samples 7 and 8) (D and E). Scale bars, 500 nm (C to E).

In humans and other mammals, color mostly comes from pigments like melanin that are in our skin and hair. Birds’ colors don’t just come from pigment — some of their coloration, like the rainbow flecks on hummingbirds and the shiny, glossy black on crows, is due to the physical makeup of their feathers. The parts of their cells that produce pigment, called melanosomes, affect the feathers’ color based on how light bounces off those melanosomes. Different shapes or arrays of melanosomes can create different structural colors, and so can the layers of keratin making up the birds’ feathers. They can reflect a rainbow of light, and they can make the difference between dull, matte feathers and feathers with a glossy shine.

Scientists had never found structural colors in the feathers of paleognaths like cassowaries and ostriches — only in the neognath group of birds like songbirds. But paleognaths can make structural colors: the blue skin on cassowaries’ heads is due to structural color, and so is the shiny sheen on eggs laid by their cousins, the tinamous. Eliason and Clarke, who study structural colors in birds and dinosaurs, wanted to see if structural color was also present in paleognath feathers.

A bird’s feather is structured a little like a tree. The long trunk running through the middle is called the rachis, and it has branches called barbs. The barbs are covered with tiny structures called barbules, akin to the leaves on tree branches. In other shiny birds, glossiness is produced by the shape of the barbs and layers of melanosomes in barbules. Eliason and Clarke didn’t find that in cassowary feathers, though. Instead, they discovered that the shiny black color came from the rachis running down the middle of the feathers. Since the fluffy barbules on cassowary feathers are pretty sparse, the rachis gets more exposure to light than in “thick-feathered” birds, giving it a chance to literally shine.

In addition to finding structural color in cassowary feathers, Eliason and Clarke also explored the feathers of a cousin of the cassowary that lived 52 million years ago. The extinct bird Calxavis grandei lived in what’s now Wyoming, and its incredibly well-preserved fossils include imprints of its feathers.

“You can look at a fossil slab and see an outline of where their feathers were, because you kind of see the black stain of melanin that’s left over, even after you 50 million years or so,” explains Eliason. “We peeled off little flakes of the fossil from the dark spots of melanin, and then we used scanning electron microscopes to look for remnants of preserved melanosomes.”

By examining these feather imprints on a microscopic level, the researchers were able to see the shape of the pigment-producing melanosomes in the leaf-like barbules of the feathers. The melanosomes were long, skinny, and green bean-shaped, which in modern birds is associated with iridescence.

Before this study, scientists had never found evidence of structural color in paleognath feathers — now, they’ve got two different examples. The researchers aren’t sure why cassowaries and the fossil birds evolved two different ways to build shiny feathers — why reinvent the wheel? Eliason suspects that flightlessness might have given cassowaries more room to experiment with their feathers. In flighted birds, including the fossil birds in this study, the number one priority for feather structure is being aerodynamic. Since cassowaries don’t need to worry about flying, they had more evolutionary leeway to develop their oddly-shaped, thick-spined feathers. “Needing to be able to fly is a very strong stabilizing force on wing shape,” says Eliason. “Losing that constraint, that need to fly, might result in new feather morphologies that produce gloss in a way that a flying bird might not.”

In addition to the questions this study poses about why these birds’ feathers evolved so differently, Eliason and Clarke note that it gives us a better overall understanding of life on Earth. “It gives us a glimpse into the time when dinosaurs were going extinct and the birds were rising,” says Eliason. “Studying these paleognaths gives us a better understanding of what was happening there, because you can’t just study neognaths; you need to study both sister clades to understand their ancestors.”

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Source: Chad M. Eliason, Julia A. Clarke. Cassowary gloss and a novel form of structural color in birdsScience Advances, 2020; 6 (20): eaba0187 DOI: 10.1126/sciadv.aba0187

WFS News: Skeleton of a Cretaceous mammal from Madagascar reflects long-term insularity

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

In evolutionary terms, islands are the stuff of weirdness. It is on islands where animals evolve in isolation, often for millions of years, with different food sources, competitors, predators, and parasites…indeed, different everything compared to mainland species. As a result, they develop into different shapes and sizes and evolve into new species that, given enough time, spawn yet more new species.

Such is the case with the discovery of a new, bizarre 66-million-old mammal in Madagascar by a team of international researchers led by Dr. David Krause, senior curator of vertebrate paleontology at the Denver Museum of Nature & Science and professor emeritus at Stony Brook University, where part of the research was done. The discovery of this opossum-sized mammal that lived among dinosaurs and massive crocodiles on the fourth largest island on Earth was announced today in the journal Nature. Dr. James B. Rossie of Stony Brook University is one of the study’s co-authors. The late Yaoming Hu of Stony Brook University was also a co-author.

The finding of the new mammal, called Adalatherium, which is translated from the Malagasy and Greek languages and means “crazy beast,” is based on a nearly complete skeleton that is astoundingly well preserved. The skeleton is the most complete for any Mesozoic mammal yet discovered in the southern hemisphere.

Krause said that, “knowing what we know about the skeletal anatomy of all living and extinct mammals, it is difficult to imagine that a mammal like Adalatherium could have evolved; it bends and even breaks a lot of rules.”

In fact, although a life-like reconstruction might lead one to think that Adalatherium was a run-of-the-mill badger, its “normality” is literally only skin deep. Below the surface, its skeleton is nothing short of “outlandish.” It has primitive features in its snout region (like a septomaxilla bone) that hadn’t been seen for a hundred million years in the lineage leading to modern mammals.

“Its nasal cavity exhibits an amazing mosaic of features, some of which are very standard for a mammal, but some that I’ve never seen in anything before,” Rossie declared.

Adalatherium had more holes (foramina) on its face than any known mammal, holes that served as passageways for nerves and blood vessels supplying a very sensitive snout that was covered with whiskers. And there is one very large hole on the top of its snout for which there is just no parallel in any known mammal, living or extinct.

The teeth of Adalatherium are vastly different in construction than any known mammal. Its backbone had more vertebrae than any Mesozoic mammal and one of its leg bones was strangely curved.

About the size of a Virginia opossum, Adalatherium was also unusual in that it was very large for its day; most mammals that lived alongside dinosaurs were much smaller, mouse-sized on average.

Adalatherium belongs to an extinct group of mammals called gondwanatherians because they are only known from the ancient southern supercontinent of Gondwana. Gondwanatherian fossils were first found in Argentina in the 1980s but have since also been found in Africa, India, the Antarctic Peninsula, and Madagascar. Gondwanatherians were first thought to be related to modern-day sloths, anteaters, and armadillos but “now are known to have been part of a grand evolutionary experiment, doing their own thing, an experiment that failed and was snuffed out in the Eocene, about 45 million years ago,” Krause explained.

Prior to the discovery of the nearly complete skeleton of Adalatherium, gondwanatherians were only known from isolated teeth and jaw fragments, with the exception of a cranium from Madagascar described by Krause and his team in 2014.

The completeness and excellent preservation of the skeleton of Adalatherium potentially opens up new windows into what gondwanatherians looked like and how they lived, but the bizarre features still have the scientific team guessing.

As Krause’s primary collaborator Simone Hoffmann of the New York Institute of Technology put it, “Adalatherium is the oddest of oddballs. Trying to figure out how it moved is nearly impossible because, for instance, its front end is telling us a different story than its back end.” The research team is still uncovering clues but thinks that, although Adalatherium might have been a powerful digging animal, it was also capable of running and potentially even had other forms of locomotion.

The plate tectonic history of Gondwana provides independent evidence for why Adalatherium is so bizarre. Adalatherium was found in rocks dated to near the end of the Cretaceous, at 66 million years ago. Madagascar, with the Indian subcontinent attached to the east, separated from Africa over a hundred million years before and finally became isolated as an island in the Indian Ocean when the Indian subcontinent detached at approximately 88 million years ago and drifted northward. That left the lineage that ultimately resulted in Adalatherium to evolve, isolated from mainland populations, for over 20 million years — “ample time to develop its many ludicrous features,” said Krause.

The fossil record of early mammals from the northern hemisphere is roughly an order of magnitude better than from the south.

Adalatherium is just one piece, but an important piece, in a very large puzzle on early mammalian evolution in the southern hemisphere,” Krause noted. “Unfortunately, most of the pieces are still missing.”

More than anything, this discovery underscores to the researchers how much more remains to be learned by making new discoveries of early mammals in Madagascar and other parts of the former Gondwana.

In addition to Krause, Hoffmann, and Rossie, other researchers involved in the new discovery — which was funded by the National Science Foundation and National Geographic Society — were: the late Yaoming Hu of Stony Brook University; John R. Wible of Carnegie Museum of Natural History; Guillermo W. Rougier of University of Louisville; E. Christopher Kirk of University of Texas at Austin; Joseph R. Groenke of Stony Brook University and Ohio University; Raymond R. Rogers of Macalester College; Julia A. Schultz of Institut für Geowissenschaften der Universität Bonn, Alistair R. Evans of Monash University and Museums Victoria; Wighart von Koenigswald of Institut für Geowissenschaften der Universität Bonn; and Lydia J. Rahantarisoa of Université d’Antananarivo.

The new Adalatherium mammal is just the latest of a series of bizarre back-boned animals discovered by Krause and his research team on Madagascar over the past 25 years. Earlier discoveries have included a giant, armored, predatory frog (Beelzebufo), a pug-nosed, vegetarian crocodile (Simosuchus), and a small, buck-toothed dinosaur (Masiakasaurus).

The island itself is filled with animals (and plants) found nowhere else on the planet, including hissing cockroaches, giraffe weevils, tomato frogs, Satanic leaf-tailed geckos, panther chameleons, and streaked tenrecs to name a few. And, of course, there is the signature group of mammals — lemurs — made famous in the animated “Madagascar” movies. Only a few thousand years ago, the Madagascar fauna also included 1400-pound elephant birds, gorilla-sized lemurs, and pygmy hippopotamuses.

David W. Krause, Simone Hoffmann, Yaoming Hu, John R. Wible, Guillermo W. Rougier, E. Christopher Kirk, Joseph R. Groenke, Raymond R. Rogers, James B. Rossie, Julia A. Schultz, Alistair R. Evans, Wighart von Koenigswald, Lydia J. Rahantarisoa. Skeleton of a Cretaceous mammal from Madagascar reflects long-term insularityNature, 2020; DOI: 10.1038/s41586-020-2234-8

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: 200-million-year-old ‘squid’ attack revealed

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Scientists have discovered the world’s oldest known example of a squid-like creature attacking its prey, in a fossil dating back almost 200 million years.

The fossil was found on the Jurassic coast of southern England in the 19th century and is currently housed within the collections of the British Geological Survey in Nottingham.

In a new analysis, researchers say it appears to show a creature — which they have identified as Clarkeiteuthis montefiorei — with a herring-like fish (Dorsetichthys bechei) in its jaws.

They say the position of the arms, alongside the body of the fish, suggests this is not a fortuitous quirk of fossilization but that it is recording an actual palaeobiological event.

They also believe it dates from the Sinemurian period (between 190 and 199 million years ago), which would predate any previously recorded similar sample by more than 10 million years.

The research was led by the University of Plymouth, in conjunction with the University of Kansas and Dorset-based company, The Forge Fossils.

It has been accepted for publication in Proceedings of the Geologists’ Association and will also be presented as part of Sharing Geoscience Online, a virtual alternative to the traditional General Assembly held annually by the European Geosciences Union (EGU).

Professor Malcolm Hart, Emeritus Professor in Plymouth and the study’s lead author, said: “Since the 19th century, the Blue Lias and Charmouth Mudstone formations of the Dorset coast have provided large numbers of important body fossils that inform our knowledge of coleoid palaeontology. In many of these mudstones, specimens of palaeobiological significance have been found, especially those with the arms and hooks with which the living animals caught their prey.

“This, however, is a most unusual if not extraordinary fossil as predation events are only very occasionally found in the geological record. It points to a particularly violent attack which ultimately appears to have caused the death, and subsequent preservation, of both animals.”

In their analysis, the researchers say the fossilised remains indicate a brutal incident in which the head bones of the fish were apparently crushed by its attacker.

They also suggest two potential hypotheses for how the two animals ultimately came to be preserved together for eternity.

Firstly, they suggest that the fish was too large for its attacker or became stuck in its jaws so that the pair — already dead — settled to the seafloor where they were preserved.

Alternatively, the Clarkeiteuthis took its prey to the seafloor in a display of ‘distraction sinking’ to avoid the possibility of being attacked by another predator. However, in doing so it entered waters low in oxygen and suffocated.

Source: University of Plymouth. “Fossil reveals evidence of 200-million-year-old ‘squid’ attack.” ScienceDaily. ScienceDaily, 6 May 2020. <www.sciencedaily.com/releases/2020/05/200506133625.htm>.
@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Scientists have reconstructed the skulls of some of the world’s oldest known dinosaur embryos in 3D, using synchrotron techniques.

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Dinosaur egg concept (stock image). Credit: © Esa Riutta / Adobe Stock

Dinosaur egg concept (stock image).Credit: © Esa Riutta / Adobe Stock

An international team of scientists led by the University of the Witwatersrand in South Africa, has been able to reconstruct, in the smallest details, the skulls of some of the world’s oldest known dinosaur embryos in 3D, using powerful and non-destructive synchrotron techniques at the ESRF, the European Synchrotron in France. They found that the skulls develop in the same order as those of today’s crocodiles, chickens, turtles and lizards. The findings are published today in Scientific Reports.

University of the Witwatersrand scientists publish 3D reconstructions of the ~2cm-long skulls of some of the world’s oldest dinosaur embryos in an article in Scientific Reports. The embryos, found in 1976 in Golden Gate Highlands National Park (Free State Province, South Africa) belong to South Africa’s iconic dinosaur Massospondylus carinatus, a 5-meter long herbivore that nested in the Free State region 200 million years ago.

The scientific usefulness of the embryos was previously limited by their extremely fragile nature and tiny size. In 2015, scientists Kimi Chapelle and Jonah Choiniere, from the University of Witwatersrand, brought them to the European Synchrotron (ESRF) in Grenoble, France for scanning. At the ESRF, an 844 metre-ring of electrons travelling at the speed of light emits high-powered X-ray beams that can be used to non-destructively scan matter, including fossils. The embryos were scanned at an unprecedented level of detail — at the resolution of an individual bone cell. With these data in hand, and after nearly 3 years of data processing at Wits’ laboratory, the team was able to reconstruct a 3D model of the baby dinosaur skull. “No lab CT scanner in the world can generate these kinds of data,” said Vincent Fernandez, one of the co-authors and scientist at the Natural History Museum in London (UK). “Only with a huge facility like the ESRF can we unlock the hidden potential of our most exciting fossils. This research is a great example of a global collaboration between Europe and the South African National Research Foundation,” he adds.

Up until now, it was believed that the embryos in those eggs had died just before hatching. However, during the study, lead author Chapelle noticed similarities with the developing embryos of living dinosaur relatives (crocodiles, chickens, turtles, and lizards). By comparing which bones of the skull were present at different stages of their embryonic development, Chapelle and co-authors can now show that the Massospondylus embryos were actually much younger than previously thought and were only at 60% through their incubation period.

The team also found that each embryo had two types of teeth preserved in its developing jaws. One set was made up of very simple triangular teeth that would have been resorbed or shed before hatching, just like geckos and crocodiles today. The second set were very similar to those of adults, and would be the ones that the embryos hatched with. “I was really surprised to find that these embryos not only had teeth, but had two types of teeth. The teeth are so tiny; they range from 0.4 to 0.7mm wide. That’s smaller than the tip of a toothpick!,” explains Chapelle.

The conclusion of this research is that dinosaurs developed in the egg just like their reptilian relatives, whose embryonic developmental pattern hasn’t changed in 200 million years. “It’s incredible that in more than 250 million years of reptile evolution, the way the skull develops in the egg remains more or less the same. Goes to show — you don’t mess with a good thing!,” concludes Jonah Choiniere, professor at the University of Witwatersrand and also co-author of the study.

The team hopes to apply their method to other dinosaur embryos to estimate their level of development. They will be looking at the rest of the skeleton of the Massospondylus embryos to see if it also shares similarities in development with today’s dinosaur relatives. The arms and legs of the Massospondylus embryos have already been used to show that hatchlings likely walked on two legs.

Main findings:

  1. High powered X-rays were used to reconstruct the skulls of some of the world’s oldest known dinosaur embryos.
  2. The skull could be seen in 3D at an unprecedented level of detail.
  3. Dinosaur embryo skulls appear to develop in the same order as those of today’s crocodiles, chickens, turtles and lizards.
  4. These dinosaur embryos appear to have been fossilised at approximately 60% through their incubation period. This is much earlier than previously thought.
  5. The dinosaur embryos have two types of teeth that range in size from 0.4 to 0.7mm wide. One of these sets would have been shed or resorbed before hatching.

Ref: Kimberley E. J. Chapelle, Vincent Fernandez, Jonah N. Choiniere. Conserved in-ovo cranial ossification sequences of extant saurians allow estimation of embryonic dinosaur developmental stagesScientific Reports, 2020; 10 (1) DOI: 10.1038/s41598-020-60292-z

  1. Kimberley E. J. Chapelle, Roger B. J. Benson, Josef Stiegler, Alejandro Otero, Qi Zhao, Jonah N. Choiniere. A quantitative method for inferring locomotory shifts in amniotes during ontogeny, its application to dinosaurs and its bearing on the evolution of posturePalaeontology, 2020; 63 (2): 229 DOI: 10.1111/pala.12451 
Source: European Synchrotron Radiation Facility. “Synchrotron X-ray sheds light on some of the world’s oldest dinosaur eggs: Dinosaur ‘Easter eggs’ reveal their secrets in 3D thanks to X-rays and high-powered computers.” ScienceDaily. ScienceDaily, 9 April 2020. <www.sciencedaily.com/releases/2020/04/200409085641.htm>.
@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: ‘Dineobellator notohesperus’ ,dinosaur with nasty gouge mark on claw

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

An illustration showing the newfound raptor dinosaur Dineobellator notohesperus, which lived at the end of the Cretaceous Period in what is now New Mexico. The ceratopsid (horned dinosaur) Ojoceratops and sauropod Alamosaurus are in the background. (Image: © Sergey Krasovskiy)

An illustration showing the newfound raptor dinosaur Dineobellator notohesperus, which lived at the end of the Cretaceous Period in what is now New Mexico. The ceratopsid (horned dinosaur) Ojoceratops and sauropod Alamosaurus are in the background.
(Image: © Sergey Krasovskiy)

About 70 million years ago, a cousin of Velociraptor got in a brawl with a larger predator that left it with a nasty rib injury. But this dinosaur, a feathered hypercarnivore, lived to tell the tale, as its rib showed signs of healing, a new study finds.

The newfound species, dubbed Dineobellator notohesperus, had another injury; a gash on its sickle-shaped claw that “we hypothesize may have been made by another Dineobellator,” said study lead researcher Steven Jasinski, a paleontologist and head of the Paleontology and Geology Section at The State Museum of Pennsylvania.

The dinosaur’s fossils were discovered in the San Juan Basin of northwestern New Mexico during the summer of 2008. Given the dinosaur’s impressive injuries, the scientists named it Dineobellator notohesperus (pronounced “dih NAY oh – BELL a tor” “Noh toh – hes per us”), by combining the Navajo word “Diné” (Navajo people) with the Latin word “bellator” (warrior). Its species name comes from “noto” and “hesper,”  the Greek words for “south” and “west,” respectively, in reference to the American Southwest.

An illustration of Dineobellator notohesperus showing its feathers. (Image credit: Steven Jasinski)

An illustration of Dineobellator notohesperus showing its feathers. (Image credit: Steven Jasinski)

D. notohesperus belongs to the dromaeosaurid family, a group of small to medium-size feathered carnivores, including Velociraptor, that lived during the Cretaceous period (145 million to 65 million years ago). After analyzing the bones, paleontologists determined that D. notohesperus would have measured about 6.5 feet (2 meters) long, about 3 feet (1 m) tall at the hip and weighed about 40-50 lbs. (18-22 kilograms), making it about as heavy as a female poodle. Remarkably, features on its forearm revealed that D. notohesperus is “one of the rare dinosaurs from North America that shows evidence of feathers,” Jasinski said.

D. notohesperus was hypercarnivorous, meaning that it almost exclusively ate meat. If these dinosaurs lived in packs, as evidence of other raptors suggests, it’s possible that a pack of these warrior dinosaurs “would have been able to attack and take down prey several times larger than them,” Jasinski said.

The fossils also revealed that D. notohesperus was strong for its size. It had strong muscles on its humerus, or upper arm, and the nearly 4-inch-long (10 centimeters) claws on its hands and feet could have closed strongly around prey, Jasinski said. Its hands would have had “a very strong grip for grasping things,” he added.

A skeletal reconstruction of the newly discovered raptor Dineobellator notohesperus. (Image credit: Steven Jasinski)

A skeletal reconstruction of the newly discovered raptor Dineobellator notohesperus. (Image credit: Steven Jasinski)

Cheetah-like hunter?

The vertebrae near the base of its tail curved inward, suggesting that D. notohesperus had increased agility, which would have helped it hunt prey.

“Other members of this group of dinosaurs tend to have straight, stiff tails that are reinforced with rod-like features made of bones and tendons,” Jasinski said. But the newfound dinosaur appears to have had a highly mobile tail. “If you think of videos of cheetahs pursuing prey like gazelles, their tail tends to stay relatively straight but whip around as the cheetah quickly changes direction. Dineobellator would have had a similar ability to quickly change directions during pursuit,” he said.

However, the assessments of this creature’s strength and tail may be premature, said David Evans, chair of vertebrate paleontology and deputy head of the Department of Natural History at Royal Ontario Museum in Canada, who was not involved in the study.

“Ultimately, the specimen is still very fragmentary and leaves a lot of questions, including the strength of the functional inferences in the study,” Evans told Live Science in an email. “Although the bones suggest Dineobellator may have had a suite of special adaptations that could be related to predation for instance, the scrappy nature of the fossils makes it difficult to evaluate the significance of the seemingly unique shapes of its bones.”

“More complete fossils and comparative functional analyses are needed to more reliably infer the behavior of Dineobellator,” Evans said.

However, the bones do reveal D. notohesperus‘ roots. Based on the dinosaur’s anatomy, “we have determined that Dineobellator is closely related to dromaeosaurids from Asia,” meaning that D. notohesperus is a descendant of migrants from Asia, Jasinski said.

The study was published online March 26 in the journal Scientific Reports.

Source: Article By Laura Geggel,  Associated Editor, live Science.com

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Iridescent Bones of a Lost Dinosaur Herd Discovered in an Opal Mine

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

A fossil vertebrae of the newly discovered dinosaur species Fostoria dhimbangunmal discovered in opal. (Image: © Robert A. Smith/Australian Opal Centre)

A fossil vertebrae of the newly discovered dinosaur species Fostoria dhimbangunmal discovered in opal.
(Image: © Robert A. Smith/Australian Opal Centre)

Gemstones are precious, especially when they come filled with dinosaur bones.

Back in the 1980s, a miner unearthed a slew of fossils preserved in opals in an opal mine near Lightning Ridge in Australia. A recent analysis of those opalized fossils revealed that they held the remains of a herd of dinosaurs — including the world’s most complete opalized dinosaur.

The fossils included parts of a previously undiscovered dinosaur species that is now named Fostoria dhimbangunmal after the opal miner Robert Foster who discovered the fossils back in the 1980s, according to a statement. The species name translates to “sheep yard” in local languages, which was given as a tribute to the opal field known as “Sheepyard,” under which is the opal mine where thebones were discovered.

Though the fossils were discovered a couple decades ago, they weren’t studied until recently when Foster’s children donated them to the Australian Opal Center.

A fossilized toe bone of Fostoria dhimbangunmal found in opal. (Image credit: Robert A. Smith/Australian Opal Centre)

A fossilized toe bone of Fostoria dhimbangunmal found in opal. (Image credit: Robert A. Smith/Australian Opal Centre)

After the donation, a team of scientists at the University of New England at Armidale in Australia began to analyze them. They found bits and pieces of four Fostoria skeletons, some juveniles and some larger, likely adults that could have been 16.4 feet (5 meters) long when alive.

“We all assumed initially that this pile of bones was from a single individual, but it wasn’t until I started piecing together the skeleton and examining each of the bones one by one that I realized something didn’t quite fit,” said lead author Phil Bell, a senior lecturer of paleontology at the University of New England. He realized the bones came from a herd or family when he identified parts of four different shoulder blades, from various-size animals.

“As a gentle herbivore, these dinosaurs didn’t have much in the way of defence,” Bell told Live Science. They didn’t have sharp claws or horns, “so safety in numbers was probably their best bet.”

This newfound two-legged species was related to Muttaburrasaurus, a plant-eating ornithopod dinosaur which was discovered decades ago in Queensland. “Most of the features that make Fostoria unique are quite subtle,” Bell said. Indeed, it took many years to demonstrate that this was a new species of dinosaur, he said. But the team had in their hands a good part of a Fostoria skull, which is the “holy grail” for understanding what dinosaurs looked like, how they were related to other groups and what they ate, he added. (They can even look into the space where the brain would have been to figure out how the dinosaur perceived and smelled its world.)

Last year, the same group discovered another dinosaur preserved in opal in Lightning Ridge. They named that plant-eater, which also walked on two legs, the Weewarrasaurus pobeni. Lightning Ridge is the only place where opalized dinosaurs are found, Bell told Live Science previously.

These dinosaurs lived during the Cretaceous period when Lightning Ridge was a floodplain. Though most of the opalized fossils found in the area were from marine creatures that lived in the nearby sea, once in a while a bone from a land animal such as a dinosaur would wash out to sea and interact with silica minerals, according to the previous Live Science report. Silica minerals, the foundations of opal, would then build up in the cavities of fossilized bones or sometimes even seep into organic bones and form a replica of them.

“Without a doubt,” Lightning Ridge still holds dinosaur fossils in its precious opals, Bell said. “The opal industry still thrives in Lightning Ridge, and where you find opals, you’re just as likely to find fossils, too.”

But these deeply buried fossil-holding opals aren’t easy to get to, he added. So “it’s really important to acknowledge the work of the miners, because without them we’d know nothing about this mysterious prehistoric world.”

The study was published online June 3 in the Journal of Vertebrate Paleontology.

Source: Article By Yasemin Saplakoglu, Livescience.com

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Discovery of the oldest bilaterian from the Ediacaran of South Australia

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Discovery of the oldest bilaterian from the Ediacaran of South Australia

 

A team led by UC Riverside geologists has discovered the first ancestor on the family tree that contains most familiar animals today, including humans.

The tiny, wormlike creature, named Ikaria wariootia, is the earliest bilaterian, or organism with a front and back, two symmetrical sides, and openings at either end connected by a gut. The paper is published today in Proceedings of the National Academy of Sciences.

The earliest multicellular organisms, such as sponges and algal mats, had variable shapes. Collectively known as the Ediacaran Biota, this group contains the oldest fossils of complex, multicellular organisms. However, most of these are not directly related to animals around today, including lily pad-shaped creatures known as Dickinsonia that lack basic features of most animals, such as a mouth or gut.

The development of bilateral symmetry was a critical step in the evolution of animal life, giving organisms the ability to move purposefully and a common, yet successful way to organize their bodies. A multitude of animals, from worms to insects to dinosaurs to humans, are organized around this same basic bilaterian body plan.

Evolutionary biologists studying the genetics of modern animals predicted the oldest ancestor of all bilaterians would have been simple and small, with rudimentary sensory organs. Preserving and identifying the fossilized remains of such an animal was thought to be difficult, if not impossible.

For 15 years, scientists agreed that fossilized burrows found in 555 million-year-old Ediacaran Period deposits in Nilpena, South Australia, were made by bilaterians. But there was no sign of the creature that made the burrows, leaving scientists with nothing but speculation.

Scott Evans, a recent doctoral graduate from UC Riverside; and Mary Droser, a professor of geology, noticed miniscule, oval impressions near some of these burrows. With funding from a NASA exobiology grant, they used a three-dimensional laser scanner that revealed the regular, consistent shape of a cylindrical body with a distinct head and tail and faintly grooved musculature. The animal ranged between 2-7 millimeters long and about 1-2.5 millimeters wide, with the largest the size and shape of a grain of rice — just the right size to have made the burrows.

“We thought these animals should have existed during this interval, but always understood they would be difficult to recognize,” Evans said. “Once we had the 3D scans, we knew that we had made an important discovery.”

The researchers, who include Ian Hughes of UC San Diego and James Gehling of the South Australia Museum, describe Ikaria wariootia, named to acknowledge the original custodians of the land. The genus name comes from Ikara, which means “meeting place” in the Adnyamathanha language. It’s the Adnyamathanha name for a grouping of mountains known in English as Wilpena Pound. The species name comes from Warioota Creek, which runs from the Flinders Ranges to Nilpena Station.

“Burrows of Ikaria occur lower than anything else. It’s the oldest fossil we get with this type of complexity,” Droser said. “Dickinsonia and other big things were probably evolutionary dead ends. We knew that we also had lots of little things and thought these might have been the early bilaterians that we were looking for.”

In spite of its relatively simple shape, Ikaria was complex compared to other fossils from this period. It burrowed in thin layers of well-oxygenated sand on the ocean floor in search of organic matter, indicating rudimentary sensory abilities. The depth and curvature of Ikaria represent clearly distinct front and rear ends, supporting the directed movement found in the burrows.

The burrows also preserve crosswise, “V”-shaped ridges, suggesting Ikaria moved by contracting muscles across its body like a worm, known as peristaltic locomotion. Evidence of sediment displacement in the burrows and signs the organism fed on buried organic matter reveal Ikaria probably had a mouth, anus, and gut.

“This is what evolutionary biologists predicted,” Droser said. “It’s really exciting that what we have found lines up so neatly with their prediction.”

Scott D. EvansIan V. HughesJames G. Gehling, and Mary L. Droser
  1. Edited by Neil H. Shubin, University of Chicago, Chicago, IL, and approved February 17, 2020 (received for review January 21, 2020)

  2. University of California – Riverside. “Ancestor of all animals identified in Australian fossils: A wormlike creature that lived more than 555 million years ago is the earliest bilaterian.” ScienceDaily. ScienceDaily, 23 March 2020. <www.sciencedaily.com/releases/2020/03/200323152108.htm>.

WFS News: Fine-tuning radiocarbon dating could ‘rewrite’ ancient events

 

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

 

Tree rings (stock image). Credit: © CrispyMedia / Adobe Stock

                  Tree rings (stock image).Credit: © CrispyMedia / Adobe Stock

Radiocarbon dating, invented in the late 1940s and improved ever since to provide more precise measurements, is the standard method for determining the dates of artifacts in archaeology and other disciplines.

“If it’s organic and old — up to 50,000 years — you date it by radiocarbon,” said Sturt Manning, the Goldwin Smith Professor of Classical Archaeology in the College of Arts and Sciences.

Manning is lead author of a new paper that points out the need for an important new refinement to the technique. The outcomes of his study, published March 18 in Science Advances, have relevance for understanding key dates in Mediterranean history and prehistory, including the tomb of Tutankhamen and a controversial but important volcanic eruption on the Greek island of Santorini.

Radiocarbon dating measures the decomposition of carbon-14, an unstable isotope of carbon created by cosmic radiation and found in all organic matter. Cosmic radiation, however, is not constant at all times. To account for fluctuations of cosmic radiation in the Earth’s atmosphere, the radiocarbon content of known-age tree rings was measured backward in time from the 20th century, for thousands of years.

Tree-ring calibrated radiocarbon started to be widely used 50 years ago. A standard calibration curve was introduced in 1986 and is updated every few years as more data are added.

“A single Northern Hemisphere calibration curve has formed the basis of radiocarbon dating in Europe and the Mediterranean for five decades, setting the time frame for prehistory,” Manning and co-authors write. “However, as measurement precision increases, there is mounting evidence for some small but substantive regional (partly growing season) offsets in the same-year radiocarbon levels.”

In their study, Manning and co-authors question the accuracy of a single calibration curve for all of the Northern Hemisphere. Using data collected by only one lab to control for interlaboratory variation, they compared radiocarbon data from northern Europe (Germany) and from the Mediterranean (central Turkey) in the 2nd and 1st millennia B.C. They found that some small but critical periods of variation for Mediterranean radiocarbon levels exist. Data from two other radiocarbon labs on samples from central Italy and northern Turkey then provided consistency.

Growing seasons play a role, the paper says. The radiocarbon level on Earth varies according to the season; there’s a winter low and a summer high, Manning said. The carbon in a tree ring reflects when the tree was photosynthesizing and, therefore, taking carbon out of the atmosphere.

“In northern Europe or in North America, a tree is going to be doing this in April through September. But a tree in Jordan or Israel does that October through April — almost the opposite time of the year,” he said.

These variations, although small, potentially affect calendar dates for prehistory by up to a few decades, the paper concludes.

Even small date offsets — 50 years or less — are important for building the timeline of the Mediterranean region, which, in the last two millennia B.C., was a hotbed of interrelated cultures.

The adjusted dates confirm previously awkward timelines, where radiocarbon and history did not seem to agree for some historical landmarks, including the death and burial of Egyptian pharaoh Tutankhamen, which is dated around the 1320s to 1310s B.C., according to recent Egyptology.

The study also addresses a debate over the date of a massive volcanic eruption on Santorini. This much-studied event is dated around 1500 B.C. by archaeologists but earlier — 1630 to 1600 B.C. — by scientists. Manning said the new findings rule out the date of 1500 B.C., but may also modify the science. A 1630-1600 B.C. date remains possible, but a later date in the range 1600-1550 B.C. now becomes plausible, and even works better with existing archaeological and historical records, including writings from Egypt.

The study also has ramifications for understanding which culture influenced the Minoans and Mycenaeans, which led to ancient Greece.

“Getting the date right will rewrite and get our history correct in terms of what groups were significant in shaping what then became classical civilization,” Manning said. “An accurate timeline is key to our history.”

He predicts follow-up on this study and a future with more specific regional calibration curves within the Northern Hemisphere — as well as subsequent adjustment to historical dates.

This research was funded in part by grants from the National Science Foundation and the Social Science and Humanities Research Council, Canada.

Story Source:

Materials provided by Cornell University. Original written by Kate Blackwood. Note: Content may be edited for style and length.

Journal Reference:

  1. Sturt W. Manning, Bernd Kromer, Mauro Cremaschi, Michael W. Dee, Ronny Friedrich, Carol Griggs, Carla S. Hadden. Mediterranean radiocarbon offsets and calendar dates for prehistoryScience Advances, 2020; 6 (12): eaaz1096 DOI: 10.1126/sciadv.aaz1096.

WFS News: Microbes were living on land as early as 3.22 billion years ago?

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

The earliest signs of life on a young Earth, around 3.5 billion years ago, have generally come from the ocean in the form of fossilized microbes within ancient rock. Now, scientists working in the Barberton Greenstone Belt in South Africa—where some of the oldest rocks on Earth are preserved—find evidence of terrestrial microbial life that they estimate is about 3.22 billion years old. The results, published today (July 23) in Nature Geosciencesrepresent the oldest signs of land-based life on our planet yet discovered

“This work represents the oldest and least ambiguous work that we have so far that life existed on land already 3.2 billion years ago,” Kurt Konhauser, a professor of earth and atmospheric sciences at the University of Alberta in Canada who was also not involved in the work, writes in an email to The Scientist.

Researchers have found more fossil evidence of the earliest microbial life in shallow, marine deposits, which supports the dominant theory that before 3 billion years ago, most of the Earth consisted of oceans interspersed with volcanic islands. Evidence for life on land has so far been harder to come by. Part of the reason is that ancient marine rocks appear to be better preserved than terrestrial sediments. Another issue, according to Martin Homann, a postdoc at the European Institute for Marine Studies (IUEM) in Brest, France, is that very old terrestrial sediments are also difficult to distinguish from marine sediments because so-called index fossils—which help to determine the environment and to date rocks—do not exist from this early period of Earth’s history.

According to the study authors, the previously oldest visible fossilized remains of microbes on land were about 2.7 billion years old, found in a different location from the Barberton Greenstone Belt in South Africa and also in Australia. In a study published last year, researchers analyzed rocks from what they interpreted as hot springs in the Pilbara region of Western Australia. Although that paper, according to Konhauser, suggests that some 3.5-billion-year-old volcanoes may have been on land, the current study is definitive in showing there was extensive exposure of continental crust on the Earth’s surface 3.2 billion years ago.

Christoph Heubeck of the Freie Universität in Berlin, Germany, (left) and Martin Homann (right) in an abandoned gold mine near Sheba Mine sampling the lava at the Barberton Greenstone Belt NADJA DRABON, STANFORD UNIVERSITY

Christoph Heubeck of the Freie Universität in Berlin, Germany, (left) and Martin Homann (right) in an abandoned gold mine near Sheba Mine sampling the lava at the Barberton Greenstone Belt
NADJA DRABON, STANFORD UNIVERSITY

For the current study, Homann and his colleagues focused on ancient sedimentary rocks, known as the Moodies Group, in the Barberton Greenstone Belt that were shown by geologists earlier to be approximately 3.22 billion years old. There, the team uncovered what are known as fossilized microbial mats—composed mainly of the imprints of bacteria and archaea and are among the earliest preserved forms of life. While living on the early Earth, these microbial community mats became interlayered and packed together with sedimentary rock made of rounded stones of different sizes that geologists call a conglomerate.

The team first analyzed and described the rocks’ positions in detail and compared these to current rock formations to understand how they moved, formed, and were preserved. The investigators concluded that the mat-forming microbes were indigenous to the host rock and part of what was once an ancient river delta.

“These are good data that show indeed that these fossilized, microbial mats [in Barberton Greenstone Belt] come from a terrestrial environment,” says Dominic Papineau, who studies the origin and evolution of life at the London Centre for Nanotechnology at University College London and who was not involved in the study.

The researchers then analyzed both the organic carbon and nitrogen isotopes within these fossilized terrestrial microbial mats and compared the profiles to isotopes extracted from nearby fossilized marine microbial mats. Both the carbon and nitrogen isotope values from the terrestrial and marine samples were unique from one another, suggesting that there were differences in the metabolism of microbes in the ocean compared to those on land.

“Already at 3.2 billion years ago, we see evidence of differences in mat-forming microbial communities suggesting that some were likely better adapted for life in the ocean versus on land,” says Homann.

A 15-centimenter-thick interval of fossilized microbial mats (arrow) embedded with sedimentary rock and sandstones in the Barberton Greenstone Belt, South Africa
MARTIN HOMANN, EUROPEAN INSTITUTE FOR MARINE STUDIES, FRANCE

A major question for scientists is whether the early Earth might have already had localized pockets of free oxygen in an atmosphere generally lacking it. Most modern microbial mats are composed of cyanobacteria, which create oxygen as a byproduct of their metabolism (oxygenic photosynthesis), and are thought to have been responsible for the accumulation of oxygen in Earth’s atmosphere. “The data here cannot distinguish whether these microorganisms produced oxygen through their photosynthesis or did anoxygenic photosynthesis,” says Papineau.

The nitrogen isotope values, which reflect the ratio of the most abundant nitrogen-14 and the more rare and heavier nitrogen-15, of the land microbial mats were more positive compared to the marine samples. This suggested to Homann and his colleagues that the land 3.2 billion years ago contained atmospheric nitrate. Another way that these positive nitrogen values could have come about would be if there were atmospheric oxygen 3.22 billion years ago, which is less likely, according to the study authors, as it would imply that there already existed oxygen-producing cyanobacteria, for which there is currently not enough evidence.

For Konhauser, it would be interesting to dig deeper into the source of the nitrate in the samples and whether it might have indeed come from the atmosphere or via generation of oxygen from the ancient photosynthetic bacteria. “The structures and isotopic composition of the microbial mats certainly seem to suggest the presence of photosynthetic microbes already existing on land,” writes Konhauser. If the nitrate were indeed formed by the microbes in the mats, he adds, then perhaps oxygen-producing cyanobacteria were around at this early stage of the Earth’s history.

M. Homann et al., “Microbial life and biogeochemical cycling on land 3,220 million years ago,” Nature Geosciencesdoi.org/10.1038/s41561-018-0190-9, 2018.

Source: Article by Anna Azvolinsky,The Scientist.com

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev