Category: Paleontology


Fossil described in June 6 edition of prestigious journal, Nature

An artist’s conception of what the newly discovered primate, Archicebus achilles, might have looked like. Credit: Mat Severson, Northern Illinois University

An artist’s conception of what the newly discovered primate, Archicebus achilles, might have looked like.
Credit: Mat Severson, Northern Illinois University

An international team of paleontologists that includes Northern Illinois University anthropologist Dan Gebo is announcing the discovery of a nearly complete, articulated skeleton of a new tiny, tree-dwelling primate dating back 55 million years.

The Eocene Epoch fossil was recovered from Hubei Province in central China.

“This is the oldest primate skeleton of this quality and completeness ever discovered and one of the most primitive primate fossils ever documented,” Gebo said. “The origin of primates sets the first milestone for all primate lineages, including that of humanity.

“Although scientists have found primate teeth, jaws, occasionally skulls or a few limb bones from this time period, none of this evidence is as complete as this new skeleton from China,” Gebo added. “With completeness comes more information and better evidence for the adaptive and evolutionary themes concerning primate evolution. It takes guessing out of the game.”

The research team, led by Xijun Ni of the Institute of Vertebrate Paleontology and Paleoanthropology (IVPP) at the Chinese Academy of Sciences in Beijing, describes the fossil in the June 6 edition of the prestigious science journal, Nature.

Other authors on the article include Marian Dagosto of the Feinberg School of Medicine at Northwestern University in Chicago; K. Christopher Beard of the Carnegie Museum of Natural History in Pittsburgh; Paul Tafforeau of the European Synchrotron Radiation Facility in Grenoble, France; and Jin Meng and John Flynn of the American Museum of Natural History in New York.

This fossil primate was encased within a rock and discovered after the rock was split open, yielding a skeleton and impressions of primate bones on each side of the two rock halves. One half is shown here. Photo Credit: Dr. Xijun Ni, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences in Beijing (China)

This fossil primate was encased within a rock and discovered after the rock was split open, yielding a skeleton and impressions of primate bones on each side of the two rock halves. One half is shown here.
Photo Credit: Dr. Xijun Ni, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences in Beijing (China)

Ni said that while doing fieldwork years ago in Hubei Province, he first came across the fossil, which had been found by a local farmer and was later donated to the IVPP. The fossil was encased within a rock and discovered after the rock was split open, yielding fossils and impressions of the primate on each side of the two halves.

It was discovered in a quarry that had once been a lake and is known for producing ancient fish and bird fossils from the Eocene Epoch. The quarry is near Jingzhou City, south of the Yangtze River, and about 270 kilometers southwest of Wuhan City, the province capital.

“This region would have been a large series of lakes, surrounded by lush tropical forests during the early Eocene,” Ni said. “Our analysis shows this new primate was very small and would have weighed less than an ounce. It had slender limbs and a long tail, would have been an excellent arboreal leaper, active during the daytime, and mainly fed on insects.”

The fossil has been named, Archicebus achilles.

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The graph shows the percentage of marine animals becoming extinct. The five major events are:

Ordovician-Silurian, Late Devonian, Permo-Triassic, Triassic-Jurassic and Cretaceous-Paleogene.

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March 23, 2013

Is Earth Undergoing a 6th Mass Extinction? –”99.9% of all Past Species Extinct”

 

 

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Of all species that have existed on Earth, 99.9 percent are now extinct. Many of them perished in five cataclysmic events. The classical “Big Five” mass extinctions identified by Raup and Sepkoski are widely agreed upon as some of the most significant: End Ordovician, Late Devonian, End Permian, End Triassic, and End Cretaceous. According to a recent poll, seven out of ten biologists think we are currently in the throes of a sixth mass extinction. Some say it could wipe out as many as 90 percent of all species living today. Other scientists dispute such dire projections.

“If you look at the fossil record, it is just littered with dead bodies from past catastrophes,” observes University of Washington paleontologist Peter Ward. Ward says that only one extinction in Earth’s past was caused by an asteroid impact – the event 65 million years ago that ended the age of the dinosaurs. All the rest, he claims, were caused by global warming.

Ward’s study, Under a Green Sky, explores extinctions in Earth’s past and predicts extinctions to come in the future. Ward demonstrates that the ancient past is not just of academic concern. Everyone has heard about how an asteroid did in the dinosaurs, and NASA and other agencies now track Near Earth objects.

Unfortunately, we may not be protecting ourselves against the likeliest cause of our species’ demise. Ward explains how those extinctions happened, and then applies those chilling lessons to the modern day: expect drought, superstorms, poison–belching oceans, mass extinction of much life, and sickly green skies.

The significant points Ward stresses are geologically rapid climate change has been the underlying cause of most great “extinction” events. Those events have been, observed Harvard evolutionary biologist Stephen Gould, major drivers of evolution.

Drastic climate change has not always been gradual; there is solid empirical evidence of catastrophic warming events taking place in centuries, perhaps even decades. The impact of atmospheric warming is most potent in its modification of ocean chemistry and of circulating currents; warming inevitably leads to non-mixing anoxic dead seas.

We are already in the middle, not the beginning, of an anthropogenic global warming, caused by agriculture and deforestation, which began some 10,000 years ago but which is now accelerating exponentially; though the earliest wave of anthropogenic warming has been stabilizing and beneficial to human development, it appears to have the potential for catastrophic effects within a lifetime or two.

Looking at the ancient evidence, Ward notes that ice caps began to shrink. “Melting all the ice caps causes a 75-meter increase in sea level will remove every coastal city on our planet.” It will also cover earth’s most productive farmland, the author warns, adding, “It will happen if we do not somehow control CO2 rise in the atmosphere.”

An analysis of the geological record of the Earth’s sea level, carried out by scientists at Princeton and Harvard universities supports Ward using a novel statistical approach that reveals the planet’s polar ice sheets are vulnerable to large-scale melting even under moderate global warming scenarios. Such melting would lead to a large and relatively rapid rise in global sea level.

According to the analysis, an additional 2 degrees of global warming could commit the planet to 6 to 9 meters (20 to 30 feet) of long-term sea level rise. This rise would inundate low-lying coastal areas where hundreds of millions of people now reside. It would permanently submerge New Orleans and other parts of southern Louisiana, much of southern Florida and other parts of the U.S. East Coast, much of Bangladesh, and most of the Netherlands, unless unprecedented and expensive coastal protection were undertaken. And while the researchers’ findings indicate that such a rise would likely take centuries to complete, if emissions of greenhouse gases are not abated, the planet could be committed during this century to a level of warming sufficient to trigger this outcome.

 

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By
Adonai

Posted on March 7, 2013

Canadian research team, helped by scientists at The University of Manchester, discovered the first evidence of an extinct giant camel in the High Arctic. The 3,5 million year old fossil was identified using new collagen fingerprinting from bone fragments unearthed on Canada’s High Arctic Ellesmere Island. It’s the furthest North a camel has ever been found. The fossils were collected during summers of 2006, 2008 and 2010 by Dr. Natalia Rybczynski, a vertebrate paleontologist with the Canadian Museum of Nature.   The camel bone fragments were collected from a steep slope at the Fyles Leaf Bed site, a sandy deposit near...
  • The Watchers

Canadian research team, helped by scientists at The University of Manchester, discovered the first evidence of an extinct giant camel in the High Arctic. The 3,5 million year old fossil was identified using new collagen fingerprinting from bone fragments unearthed on Canada’s High Arctic Ellesmere Island. It’s the furthest North a camel has ever been found.

The fossils were collected during summers of 2006, 2008 and 2010 by Dr. Natalia Rybczynski, a vertebrate paleontologist with the Canadian Museum of Nature.

Dr. Natalia Rybczynski, paleobiologist at the Canadian Museum of Nature collects a fossil bone at the Fyles Leaf Bed site on Ellesmere Island in 2008. The fossil in situ looks very similar to wood. She uses toilet paper to wrap the fossil for transport to the base camp. CREDIT: Martin Lipman, Canadian Museum of Nature.

Dr. Natalia Rybczynski  collects a fossil bone at the Fyles Leaf Bed site on Ellesmere Island in 2008. The fossil in situ looks very similar to wood. She uses toilet paper to wrap the fossil for transport to the base camp. CREDIT: Martin Lipman, Canadian Museum of Nature.

 

The camel bone fragments were collected from a steep slope at the Fyles Leaf Bed site, a sandy deposit near Strathcona Fiord on Ellesmere Island. Other fossil finds at the site suggest the High Arctic camel was living in a boreal-type of forest environment, during a global warm phase on the planet.

Dr Buckley carrying out the process of collagen fingerprinting to determine which species the bone fragments belong to.Credit: The University of Manchester

Dr Buckley carrying out the process of collagen fingerprinting to determine which species the bone fragments belong to.
Credit: The University of Manchester

At first, it was unclear which species the bones they found came from so they asked the help of Dr. Mike Buckley from Manchester Institute of Biotechnology. He used the pioneering technique called “collagen fingerprinting” to identify the animal. Dr. Buckley compared the profile he found with the 37 mondern mammal species as well as that of a fossil camel found in Yukon.

He found that the collagen profile for the High Arctic camel was almost an identical match to the modern day Dromedary as well as the Ice-Age Yukon giant camel. The collagen information, combined with the anatomical data, demonstrated that the bone fragments belonged to a giant camel as the bone is roughly 30% larger than the same bone in a living camel species.

Dr. Rybczynski said: “These bones represent the first evidence of camels living in the High Arctic region. It extends the previous range of camels in North America northward by about 1,200 km, and suggests that the lineage that gave rise to modern camels may have been originally adapted to living in an Arctic forest environment.”

“This is the first time that collagen has been extracted and used to identify a species from such ancient bone fragments. The fact the protein was able to survive for three and a half million years is due to the frozen nature of the Arctic. This has been an exciting project to work on and unlocks the huge potential collagen fingerprinting has to better identify extinct species from our preciously finite supply of fossil material.” – Dr. Buckley

The specimen found are spectacular, said Dr. Roy Wogelius from The University of Manchester’s School of Earth, Atmospheric & Environmental Sciences after he analysed the mineral content of the bones. His findings suggest that mineralization worked along with cold temperatures to help preserve the proteins in the bones. “This specimen is spectacular, and provides important clues about how such exceptional preservation may occur”, he said.

 

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Tia Ghose
LiveScience
Wed, 06 Feb 2013 16:00 CST
Jawbone

© Mirjana Roksandic
An ancient hominin jawbone unearthed in a Serbian cave may be more than half a million years old.

Scientists have unearthed a jawbone from an ancient human ancestor in a cave in Serbia.

The jawbone, which may have come from an ancient Homo erectus or a primitive-looking Neanderthal precursor, is more than 397,000 years old, and possibly more than 525,000 years old. The fossil, described today (Feb. 6) in the journal PLOS ONE, is the oldest hominin fossil found in this region of Europe, and may change the view that Neanderthals, our closest extinct human relatives, evolved throughout Europe around that time.

“It comes from an area where we basically don’t have anything that is known and well- published,” said study co-author Mirjana Roksandic, a bioarchaeologist from the University of Winnipeg in Canada. “Now we have something to start constructing a picture of what’s happening in this part of Europe at that time.”

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EARLY EARTH

New dinosaur fossil challenges bird evolution theory

by Staff Writers
Southampton UK (SPX) Feb 04, 2013


Eosinopteryx. Credit: Royal Belgian Institute of Natural Sciences.

 

Co-authored by Dr Gareth Dyke, Senior Lecturer in Vertebrate Palaeontology at the University of Southampton, the paper describes a new feathered dinosaur about 30 cm in length which pre-dates bird-like dinosaurs that birds were long thought to have evolved from.

Over many years, it has become accepted among palaeontologists that birds evolved from a group of dinosaurs called theropods from the Early Cretaceous period of Earth’s history, around 120-130 million years ago. Recent discoveries of feathered dinosaurs from the older Middle-Late Jurassic period have reinforced this theory.

The new ‘bird-dinosaur’ Eosinopteryx described in Nature Communications this week provides additional evidence to this effect.

 

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EARLY EARTH

by Staff Writers
Grenoble, France (SPX)


This is an artist’s impression of an Ichthyostega tetrapod, with the cut-out showing the 3-D reconstruction of two vetrebrae from the study. Credit: Julia Molnar.

Scientists have been able to reconstruct, for the first time, the intricate three-dimensional structure of the backbone of early tetrapods, the earliest four-legged animals. High-energy X-rays and a new data extraction protocol allowed the researchers to reconstruct the backbones of the 360 million year old fossils in exceptional detail and shed new light on how the first vertebrates moved from water onto land. The results are published 13 January 2013 in Nature.

The international team of scientists was led by Stephanie E. Pierce from The Royal Veterinary College in London and Jennifer A. Clack from the University of Cambridge. It also comprised scientists from Uppsala University (Sweden) and the European Synchrotron Radiation Facility ESRF in Grenoble (France).

The tetrapods are four-limbed vertebrates, which are today represented by amphibians, reptiles, birds and mammals. Around 400 million years ago, early tetrapods were the first vertebrates to make short excursions into shallower waters where they used their four limbs for moving around. How this happened and how they then transferred to land is a subject of intense debate among palaeontologists and evolution biologists.

 

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Palaeontology

 

EARLY EARTH

Ancient flying reptile needed a runway

by Staff Writers
Lubbock, Texas (UPI)

 


disclaimer: image is for illustration purposes only

The giant pterosaur Quetzalcoatlus may have sported a 34-foot wingspan, but it needed to taxi down a slope to take off, U.S. researchers say.

With that huge wingspan and a weight of 155 pounds the ancient flying reptile is the largest flying animal ever discovered — any larger, and it would have had to walk, scientists at Texas Tech University say.

Researcher Sankar Chatterjee used computer simulations to find out how such a heavy animal with relatively flimsy wings could become airborne, TG daily reported Thursday.

“This animal probably flew like an albatross or a frigate bird in that it could soar and glide very well. It spent most of its time in the air. But when it comes to takeoff and landing, they’re so awkward that they had to run,” he said.

“If it were taking off from a cliff, then it was OK. But if Quetzalcoatlus were on the ground, it probably had to find a sloping area like a riverbank, and then run quickly on four feet, then two to pick up enough power to get into the air. It needed an area to taxi.

“With a slight headwind and as little as a 10-degree downhill slope, an adult would be able to take off in a bipedal running start to pick up flying speed, just like a hang glider pilot,” Chatterjee said.

Like today’s condors and other large birds, Quetzalcoatlus probably relied on updraft to remain in the air, he said.

 

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Crossroads News : Changes In The World Around Us And Our Place In It

Palaeontology  :  Evolution

Cambrian fossil pushes back evolution of complex brains

by Staff Writers
Tucson AZ (SPX)


This picture shows a nearly intact fossil of Fuxianhuia protensa. The inset shows the fossilized brain in the head of another specimen. The brain structures are visible as dark outlines. Credit: Specimen photo: Xiaoya Ma; inset: Nicholas Strausfeld.

The remarkably well-preserved fossil of an extinct arthropod shows that anatomically complex brains evolved earlier than previously thought and have changed little over the course of evolution. According to University of Arizona neurobiologist Nicholas Strausfeld, who co-authored the study describing the specimen, the fossil is the earliest known to show a brain.

Embedded in mudstones deposited during the Cambrian period 520 million years ago in what today is the Yunnan Province in China, the approximately 3-inch-long fossil, which belongs to the species Fuxianhuia protensa, represents an extinct lineage of arthropods combining an advanced brain anatomy with a primitive body plan.

The fossil provides a “missing link” that sheds light on the evolutionary history of arthropods, the taxonomic group that comprises crustaceans, arachnids and insects.

The researchers call their find “a transformative discovery” that could resolve a long-standing debate about how and when complex brains evolved.

“No one expected such an advanced brain would have evolved so early in the history of multicellular animals,” said Strausfeld, a Regents Professor in the UA department of neuroscience.

According to Strausfeld, paleontologists and evolutionary biologists have yet to agree on exactly how arthropods evolved, especially on what the common ancestor looked like that gave rise to insects.

“There has been a very long debate about the origin of insects,” Strausfeld said, adding that until now, scientists have favored one of two scenarios.

Some believe that insects evolved from the an ancestor that gave rise to the malacostracans, a group of crustaceans that include crabs and shrimp, while others point to a lineage of less commonly known crustaceans called branchiopods, which include, for example, brine shrimp.

Because the brain anatomy of branchiopods is much simpler than that of malacostracans, they have been regarded as the more likely ancestors of the arthropod lineage that would give rise to insects.

However, the discovery of a complex brain anatomy in an otherwise primitive organism such as Fuxianhuia makes this scenario unlikely. “The shape [of the fossilized brain] matches that of a comparable sized modern malacostracan,” the authors write in Nature. They argue the fossil supports the hypothesis that branchiopod brains evolved from a previously complex to a more simple architecture instead of the other way around.

This hypothesis arose from neurocladistics, a field pioneered by Strausfeld that attempts to reconstruct the evolutionary relationships among organisms based on the anatomy of their nervous system. Conventional cladistics, on the other hand, usually look to an organism’s overall morphology or molecular data such as DNA sequences.

Strausfeld, who holds appointments in other UA departments including evolutionary biology and entomology, has catalogued about 140 character traits detailing the neural anatomies of almost 40 arthropod groups.

“There have been all sorts of implications why branchiopods shouldn’t be the ancestors of insects,” he said. “Many of us thought the proof in the pudding would be a fossil that would show a malacostracan-like brain in a creature that lived long before the origin of the branchiopods; and bingo! – this is what this is.”

Strausfeld traveled to the Yunnan Key Laboratory for Palaeobiology at Yunnan University in Kunming, China, to join his collaborator, Xiaoya Ma, a postdoctoral fellow at London’s Natural History Museum, in studying the brain anatomies of various fossil specimens. In the institute’s collection, they came across the fossil of Fuxianhuia protensa described in the paper.

“I spent a frenetic five hours at the dissecting microscope, the last hours of my visit there, photographing, photographing, photographing,” he said. “And I realized that this brain actually comprises three successive neuropils in the optic regions, which is a trait of malacostracans, not branchiopods.”

Neuropils are portions of the arthropod brain that serve particular functions, such as collecting and processing input from sensory organs. For example, scent receptors in the antennae are wired to the olfactory neuropils, while the eyes connect to neuropils in the optic lobes.

When Strausfeld traced the fossilized outlines of Fuxianhuia’s brain, he realized it had three optic neuropils on each side that once were probably connected by nerve fibers in crosswise pattern as occurs in insects and malacostracans. The brain was also composed of three fused segments, whereas in branchiopods only two segments are fused.

“In branchiopods, there are always only two visual neuropils and they are not linked by crossing fibers,” Strausfeld said. “In principle, Fuxianhuia’s is a very modern brain in an ancient animal.”

The fossil supports the idea that once a basic brain design had evolved, it changed little over time, he explained. Instead, peripheral components such as the eyes, the antennae and other appendages, sensory organs, etc., underwent great diversification and specialized in different tasks but all plugged into the same basic circuitry.

“It is remarkable how constant the ground pattern of the nervous system has remained for probably more than 550 million years,” Strausfeld added. “The basic organization of the computational circuitry that deals, say, with smelling, appears to be the same as the one that deals with vision, or mechanical sensation.”

The discovery will be published in the the journal Nature.

 

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Palaeontology  :  Research -  Beauty Of Nature

A mysterious seed fern, Lepidopteris, discovered from the Upper Permian of China
A mysterious seed fern, Lepidopteris, discovered from the Upper Permian of China Enlarge The cover of Chinese Science Bulletin (English Edition) 2012, 57(27) (left) and the reconstruction of Lepidopteris baodensis (right), showing the upper surface (a) and the lower surface (b) of an ultimate pinna. Credit: ©Science China Press

Recently, a mysterious seed fern, Lepidopteris baodensis sp. nov., dating to more than 251 million years ago (Ma), was discovered at the Baijiagou of Baode, Shanxi, China, from the Upper Permian Sunjiagou Formation. This discovery completely changed the understanding of the stratigraphic distribution of the genus Lepidopteris in China and promoted the taxonomic study of late Paleozoic plants.

Since Schimper erected the genus Lepidopteris in 1869, its epidermal structure of subepidermal swellings (formerly called “blisters”) had long been an unsolved mystery. Excitingly, we found subepidermal swellings not only on the lower surfaces of the ultimate rachis and midrib, but also on the lower surfaces of secondary veins. In addition, the unique epidermal structures of subepidermal swellings on the ultimate rachis, midrib and secondary veins were revealed. The epidermis of a subepidermal swelling on an ultimate rachis was composed of ordinary epidermal cells and stomatal apparatuses forming longitudinal rows and numerous groups. The epidermal cells and stomatal apparatuses in each group were set in a concentric pattern. The epidermis of a subepidermal swelling on the midrib was also composed of ordinary epidermal cells and stomatal apparatuses that formed only 3 groups, and were set in a concentric pattern. The epidermis of a subepidermal swelling on a secondary vein was composed of ordinary epidermal cells and stomatal apparatuses, forming a concentric pattern. Because, unlike the lower surface, the upper surface lacked subepidermal swellings, the difference in epidermal structures between the upper and lower surfaces is remarkable. This situation is very rare in plants. This research was carried out by Dr. Zhang Yi, Associate Professor at the College of Paleontology, Shenyang Normal University, Mr. Zheng Shaolin, Adjunct Professor at the College of Paleontology, Shenyang Normal University, and Dr. Naugolnykh, Professor at the Geological Institute, Russian Academy of Sciences. This article was published as a cover article on Chinese Science Bulletin (Chinese Edition) 2012, 57(24) and Chinese Science Bulletin (English Edition) 2012, 57(27). In 2004, the noted paleontologists and biostratigraphers Rong Jiayu (Academician Professor of NIGPAS) and Fang Zongjie (Professor of NIGPAS) pointed out in the book “Mass Extinction and Recovery” that the Earth experienced a mass extinction and recovery between the Late Permian and the Triassic, traced back to 260 Ma. The climate became extremely hot and arid at the end of the Permian. The mass extinction, which was the largest in Earth’s history, destroyed most terrestrial and marine ecosystems. On land, coal-forming floras, represented by Lepidodendron and Cordaites, went extinct. The Euramerican, Cathaysian, Gondwanan and Angaran floras disappeared, and a new flora, represented by Pleuromeia, flourished after the disaster. The recovery of coal-forming floras on a large scale did not begin until the Late Triassic.

Although the terrestrial and marine ecosystems of the Earth experienced their largest mass extinction in the Late Permian, the seed fern Lepidopteris became an important element of remnant vegetation and persisted through the Triassic. Thus, the study of Lepidopteris plays a very important role in understanding this mass extinction and recovery. Which adaptations allowed Lepidopteris to survive the harsh environment? The authors believe its persistence was probably related to the subepidermal swellings, which were special tissues unique to Lepidopteris. Based on analysis of the cuticle, the lower surfaces of the ultimate rachis, midrib and secondary veins, which are related to conducting tissues, were covered with subepidermal swellings. These subepidermal swellings were probably small water storage features that absorbed water during high flows in conducting tissues and released it during low flows, like an irrigation system. In this way, Lepidopteris, a seed fern that originally needed much water to live, probably survived the hot and arid environment. Of course, subepidermal swellings are likely to have had other functions as well. Although Lepidopteris was a typical element of the Late Permian Euramerican flora, the species L. ottonis was considered to be an index fossil for the Upper Triassic in China. As a result, the stratigraphic distribution of this very important genus in the Upper Permian of China was long neglected. The new species L. baodensis not only expands our knowledge of the biology and taxonomy of Lepidopteris and the stratigraphy of the Upper Permian of China, but also provides an opportunity to understand the relationship between Euramerican and Cathaysian floras in a paleoclimatic, paleoenvironmental and paleogeographic context. The experimental works were accomplished in the newly established laboratory of the College of Paleontology, Shenyang Normal University, Liaoning Province, China. Specimens are housed at the College of Paleontology, Shenyang Normal University. The Baijiagou of Baode, Shanxi, China, the locality where Lepidopteris baodensis was discovered, has become an area of intense research for Chinese and foreign geologists.

Crossroads News : Changes In The World Around Us And Our Place In It

Paleontology  :  Research

Fossil skeleton of strange, ancient digging mammal clears up 30-year evolutionary debate

FLORA AND FAUNA

by Staff Writers
Washington DC (SPX)

 

 

File:Ernanodon antelios.JPG

Image from Wikimedia Commons

Attribution: Apokryltaros at en.wikipedia

 


These are elements of the skeleton of Ernanodon from the Naran Bulak locality in Mongolia. Credit: Peter Kondrashov.

Shortly after dinosaurs like Tyrannosaurus and Triceratops went extinct 65 million years ago, Earth’s ancient landscapes were filled with unusual mammals only distantly related to those alive today. Until recently, one of these creatures, Ernanodon antelios, was only known from a single, highly distorted specimen that raised many questions about its habits and evolutionary relationships.

In the most recent issue of the Journal of Vertebrate Paleontology, scientists describe a second specimen of Ernanodon that sheds new light on this curious beast from the dawn of the “Age of Mammals.”

The remarkable new skeleton comes from rocks in Mongolia that were deposited 57 million years ago during a period known as the Paleocene Epoch.

“Ernanodon is a unique find and represents one of the most complete skeletons ever collected from the Paleocene of the Naran Bulak locality,” said Alexander Agadjanian of the Borissiak Paleontological Institute of the Russian Academy of Sciences, co-author of the study.

The first specimen was discovered by a team of Soviet paleontologists in 1979 but remained unstudied for more than thirty years. The new specimen preserves most of the arms, legs, and backbone of the badger-sized animal, including many bones that were not preserved in the first specimen.

The authors of the new study made detailed comparisons among the bones of Ernanodon and those of modern mammals and concluded that Ernanodon was highly specialized for digging. It may have dug for food, for shelter, or both.

“Only a handful of Asian Paleocene mammals are known by their postcranial skeleton, which makes Ernanodon a unique source of very important information about its habits, lifestyle, and affinities,” said Peter Kondrashov of A.T. Still University of Health Sciences, lead author of the study.

The strong limbs and large claws of Ernanodon, combined with its unusual, simplified teeth, have caused much confusion about its evolutionary relationships.

Some scientists thought Ernanodon was an ancient relative of modern armadillos and anteaters, whereas other scientists thought Ernanodon was more closely related to a group of African and Asian ant-eating mammals known as pangolins or “scaly anteaters.”

The new study concludes that Ernanodon was a closer relative of pangolins than armadillos and anteaters, but that it represents a very early side branch of the pangolin family tree.

“Few other fossil mammals presented as many controversies in the scientific world as Ernanodon did and we are glad the new skeleton helped us resolve them,” Kondrashov added.

The article appears in the Journal of Vertebrate Paleontology 32(5) published by Taylor and Francis. The full citation is: Kondrashov, P. and A.K. Agadjanian. 2012. A nearly complete skeleton of Ernanodon (Mammalia, Palaeanodonta) from Mongolia: morphofunctional analysis. Journal of Vertebrate Paleontology (32)5:983-1001.

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