Fossil Discovery May Be Of Earliest Dinosaur Known

Some of the earliest known dinosaurs to have walked the planet were considered to be small dinosaurs like the swift-footed Eoraptor. But researchers have discovered a new dinosaur-like fossil that may be even older. Called Nyasasaurus parringtoni, the specimen is thought to have existed 10 to 15 million years earlier than dinosaur fossils have previously shown, originating in the Middle rather than the Late Triassic Period.

Study lead author Sterling Nesbitt, a University of Washington postdoctoral researcher in biology, said if this “newly named Nyasasaurus parringtoni is not the earliest dinosaur, then it is the closest relative found so far.” His paper is published online today in the Royal Society’s Biology Letters journal.

Paul Barrett, with the Natural History Museum in London, told BBC News that this specimen “fills a gap between what we previously knew to be the oldest dinosaurs and their other closest relatives… There was this big gap in the fossil record where dinosaurs should’ve been present and this fossil neatly fills that gap.”

Nesbitt said scientists have long suggested that dinosaurs should have existed in the Middle Triassic, but there hasn’t been any conclusive proof of that to date. “Some scientists used fossilized footprints, but we now know that other animals from that time have a very similar foot. Other scientists pointed to a single dinosaur-like characteristic in a single bone, but that can be misleading because some characteristics evolved in a number of reptile groups and are not a result of a shared ancestry.”

If the newly named species proves not to be a dinosaur, yet only a close relative, then the Middle Triassic dinosaur theory would still prove inconclusive.

With that being said, the team said they cannot definitively say their new specimen is the earliest known dinosaur due to insufficient material: one upper arm bone and six vertebrae.

The team said it is difficult to sort out the early evolution of dinosaurs because they were so closely related to a variety of reptiles that proliferated at the time. However, the research team, which also included Sarah Werning from the University of California at Berkeley, noticed a few features in the fossil that were distinctive of dinosaurs, notably the “elongated deltopectoral crest” that served as an anchor for strong pectoral muscles.

Nesbitt, who also led a 2010 study that described an animal group—Silesaurs—calling it the dinosaurs’ oldest relative, said based on the fossil fragments described, the team estimates the animal stood upright, was 7 to 10 feet in length, 3 feet tall at the hip, and weighed in the neighborhood of 135 pounds.

The fossil fragments were collected in Tanzania in the 1930s, although it is difficult to say if dinosaurs actually originated in that region. When N. parringtoni was alive, the world’s continents were joined together as one supercontinent called Pangaea. Tanzania would have been part of Southern Pangaea, which included Africa, South America, Antarctica and Australia.

It is safe to say, based on the new fossil description, that dinosaurs’ lineage derived from the southern continents, a region where Archosaurs, one of the earliest animal groups linked to dinosaur evolution, derive, according to the researchers.

This finding “takes dinosaurs back to the right kind of time when those two groups would have split apart from each other,” added Barrett

He explained that during this time, dinosaurs would not have been as dominant as they later became. This would have been an early point in the evolutionary scale for dinosaurs, a time “when lots of reptile groups are evolving,” noted Barrett.

“Dinosaurs start out as a very insignificant group of reptiles – all relatively small animals, relatively rare in comparison with other reptile groups – and it’s only a bit later in their history that they suddenly explode and take over as the dominant forms of life for nearly 100 million years,” he added.

Werning, who conducted the bone analysis for the research, said the bone tissues of N. parringtoni “had a lot of bone cells and blood vessels… In living animals, we only see this many bone cells and blood vessels in animals that grow quickly, like some mammals or birds.”

“The bone tissue of Nyasasaurus is exactly what we would expect for an animal at this position on the dinosaur family tree,” she added. “It’s a very good example of a transitional fossil; the bone tissue shows that Nyasasaurus grew about as fast as other primitive dinosaurs, but not as fast as later ones.”

“Nyasasaurus and its age have important implications regardless of whether this taxon is a dinosaur or the closest relatives of dinosaurs,” Nesbitt said. “It establishes that dinosaurs likely evolved earlier than previously expected and refutes the idea that dinosaur diversity burst onto the scene in the Late Triassic, a burst of diversification unseen in any other groups at that time.”

“Dinosaurs are just part of this archosaur diversification, an explosion of new forms soon after the Permian extinction,” Nesbitt said.

The specimen researchers described came from a collection at the Natural History Museum in London. Four vertebrae from a second specimen, also used in the research, are housed in a museum in Cape Town, South Africa. Funding for the research came from the National Science Foundation (NSF) and the Natural History Museum in London.

While the species name parringtoni is new, the genus name Nyasasaurus is not. The name is derived from Nyasa, a lake in Africa located between Malawi and Tanzania, and saurus, meaning lizard. The genus was named by late paleontologist Alan Charig. The species name parringtoni is in honor of University of Cambridge’s Rex Parrington, who discovered the fossils in the 1930s.

 

Source: Lawrence LeBlond for redOrbit.com – Your Universe Online

Flying fish fossil recovered

Chinese researchers have tracked the “exceptionally well-preserved fossils” to the Middle Triassic of China (235-242 million years ago).

The Triassic period saw the re-establishment of ecosystems after the Permian mass extinction.

The fossils represent new evidence that marine ecosystems re-established more quickly than previously thought.

The Permian mass extinction had a bigger impact on the earth’s ecological systems than any other mass extinction, wiping out 90-95% of marine species.

Previous studies have suggested that Triassic marine life developed more quickly than was once thought and that marine ecosystems were re-established more rapidly than terrestrial ecosystems.

The new research, published in Proceedings of the Royal Society B journal, was carried out by scientists from Peking University, the Chinese Academy of Sciences and the Zhejiang Museum of Natural History.

The study shows that the new flying fish, named Potanichthys xingyiensis, was 153mm long and had the “unusual combination of morphological features” associated with gliding strategy in fishes.

The fossils show an asymmetrical, forked caudal (tail) fin and a “four-winged” body formation: a pair of enlarged pectoral fins forming “primary wings”, and a smaller pair of pelvic fins acting as “auxiliary wings”, according to the study.

The fossils were discovered in Guizhou Province in south-west China. They represent the first record of the extinct Thoracopteridae family of fishes to be found in Asia.

A reconstruction of what Potanichthys xingyiensis would have looked like

Previous Thoracopteridae fossils have been confined to the Upper Triassic of Austria and Italy, but the new discovery extends the group’s geographical distribution from the western to the eastern rim of the Paleo-Tethys Ocean (an ocean that closed during the Jurassic period).

The Triassic Thoracopteridae family belongs in the same Neopterygii group of animals as today’s flying fishes, of which there are around 50 species belonging to the Exocoetidae family.

Gliding has evolved many times in animals, such as in frogs, lizards and mammals but has “evolved only twice among fishes”, according to the study: once in the Triassic Thoracopteridae fishes and again in the modern-day Exocoetidae family.

Scientists suggest both families of flying fishes evolved so that they could escape marine predators by “gliding” over-water to safety.

Inoceramus : Stock Photo, World Fossil Society

This Inoceramus specimen on limestone clump is from Cretaceous Trichy, India.

Name: Inoceramus (Strong pot).
Phonetic: In-o-cer-a-mus.
Named By: James Sowerby – 1814.
Classification: Mollusca, Bivalvia, Pteriomorphia, Praecardioida, Inoceramidae.
Species: I. bellvuensis, I. biformis, I. comancheanus, I. dakotensis, I. perplexus, I. pictus, I. proximus, I. triangularis.
Type: Filter feeder.
Size: Largest specimen measures 1.87 meters.
Known locations: Worldwide.
Time period: Cretaceous.
Fossil representation: Lots of specimens recovered.

Inoceramus

Inoceramus

Inoceramus is the largest known bivalve clam in the fossil record. It is thought that it grew so large so that it could have a larger gill area to cope with oxygen deficient waters. Like smaller versions, Inoceramus would have opened its shell to expose its soft tissue and filter food from the water. When threatened it would then close up to protect the fleshy parts within.

Isotope Patterns in Ancient Volcanic Sulfur Tell Which Global Cooling Episodes Were Caused by Volcanic Eruptions

Volcanoes are well known for cooling the climate. But just how much and when has been a bone of contention among historians, glaciologists and archeologists. Now a team of atmosphere chemists, from the Tokyo Institute of Technology and the University of Copenhagen, has come up with a way to say for sure which historic episodes of global cooling were caused by volcanic eruptions.

The answer lies in patterns of isotopes found in ancient volcanic sulfur trapped in ice core, patterns due to stratospheric photochemistry. Their mechanism is published in the Proceedings of the National Academy of Sciences.

Better history through atmospheric chemistry

Matthew Johnson is an associate professor at the Department of Chemistry, University of Copenhagen where he studies chemical mechanisms in the atmosphere. He is thrilled at the prospect of giving a more precise tool to historians studying cold spells.

“Historical records are not always so accurate. Some may have been written down long after the fact, or when a different calendar was in use by a different culture. But the chemistry does not lie,” says Johnson.

Method reads height by analyzing effect of sunshine

Powerful volcanoes can shoot gases through the atmosphere and high into the stratosphere where it can affect climate globally for a year or more. Less powerful eruptions can also have powerful impacts, but only locally, and for shorter times. And here’s the trick. High plumes spend longer in the harsh sunlight of the stratosphere, and that changes the chemical signature of the sulfur in the plume. The balance of various isotopes is changed according to very precise rules, explains Mathew Johnson.

“Using our method we can determine whether a given eruption was powerful enough for the plume to enter the stratosphere affecting global climate. If we can find material from ancient eruptions it can now be used to give an accurate record of global volcanic events extending many hundreds of thousands of years back in time.,” says Johnson.

Clue to fires found in ice

Strangely, the best place to look for traces of the fiery events is in ice. Tracking climate history is performed on cores drilled from the ice shields of Greenland and Antarctica. Much like tree rings, the snows of each year is compacted into a layer representing that year. As you go further down in the borehole, you descend into deeper history.

If volcanic material shows up in a layer, you know there was an eruption in that year. Using the method developed by Johnson and his colleagues it is now possible to analyze exactly how powerful a given eruption was.

“With the sulfur isotope method, we now have a way to prove whether a given eruption was so explosive that it entered the stratosphere, affecting global climate and civilizations, or, whether a given eruption was confined to the troposphere and local in its effects” says Johnson and goes on: “There are many controversial eruptions. The Mediterranean island of Santorini blew apart and caused the end of the Minoan culture. But there is a huge debate about when exactly this occurred. 1601 was the ‘year without a summer’ — but nobody knows where the volcano was that erupted. There’s debate over whether there was an eruption on Iceland in 527, or 535, or 541. The sulfur isotope trick is a definite method to solve debates like this and get the most information out of the ice core records” Says Matthew Johnson.

Global collaboration crucial to get results

Denmark has absolutely no volcanoes. So revealing the mechanism required the very different talents of two groups practically on opposite sides of the globe, explains Johnson.

“The Tokyo Institute of Technology specializes in analysis of the patterns of sulfur isotopes found in samples in nature, and was able to synthesize the isotopically labelled samples. The University of Copenhagen has a strong group in atmospheric chemistry and spectroscopy; the laboratory measurements were carried out in Copenhagen. Together we were able to do the experiments and build the atmospheric chemical model that demonstrated the stratospheric photoexcitation mechanism,” concludes Johnson.

New NASA Mission to Help Us Better Estimate Asteroid Impact Hazard

Every year, sensors designed to detect nuclear explosions see harmless bursts in Earth’s upper atmosphere from the breakup of an asteroid a few yards across. Tiny asteroids are much more numerous than big ones, so destructive hits to Earth are very rare. However, because of their potential for devastation, NASA’s Near-Earth Object (NEO) observations program supports surveys which are undertaking sustained searches to find the largest objects and predict their impact threat to Earth.

According to NASA’s NEO program, there are more than 1,300 “Potentially Hazardous Asteroids” (PHAs) — objects at least 150 yards (about 140 meters) across with a very small chance of impacting us someday because their orbital paths take them close to Earth’s orbit.

This is an artist's concept of the OSIRIS-REx spacecraft near asteroid 1999 RQ36. (Credit: NASA Goddard Space Flight Center)

This is an artist’s concept of the OSIRIS-REx spacecraft near asteroid 1999 RQ36. (Credit: NASA Goddard Space Flight Center)

“Asteroids move at an average of 12 to 15 kilometers per second (about 27,000 to 33,000 miles per hour) relative to Earth, so fast that they carry enormous energy by virtue of their velocity,” says Edward Beshore of the University of Arizona, Tucson, deputy principal investigator for NASA’s OSIRIS-REx asteroid sample return mission. “Anything over a few hundred yards across that appears to be on a collision course with Earth is very worrisome.”

The main difficulty is obtaining sufficient observations to be able to predict their orbits with enough certainty to find out if they could hit us at some point.

“When an asteroid makes a close pass to Earth, the gravitational pull from our planet changes the asteroid’s orbit,” says Beshore. “However, how this change will affect the evolution of the asteroid’s orbit is difficult for us to predict because there are also other small forces continuously acting on the asteroid to change its orbit. The most significant of these smaller forces is the Yarkovsky effect — a minute push on an asteroid that happens when it is warmed up by the sun and then later re-radiates this heat in a different direction as infrared radiation.”

The Yarkovsky effect happens simply because it takes time for things to heat up and cool down. Objects tend to be coldest just before dawn and warmest at mid-afternoon, after hours of illumination by the high sun. “A brick building can feel warm even in the early evening hours, because it is radiating away the heat accumulated from an entire day of sunshine,” says Beshore. In the same way, an asteroid radiates most of its heat from its late “afternoon side,” giving it the small Yarkovsky push which is variable depending mostly on the asteroid’s size, shape and composition.

NASA’s OSIRIS-REx mission (Origins, Spectral Interpretation, Resource Identification, Security, and Regolith Explorer) will make the most precise measurements of the Yarkovsky effect to date by visiting a PHA called “1999 RQ36” or just “RQ36.”

“For such a large object, it has one of the highest known probabilities of impacting Earth, a 1 in 2,400 chance late in the 22nd century, according to calculations by Steve Chesley, an astronomer at NASA’s Jet Propulsion Laboratory,” said Beshore. RQ36 is about 457 meters (500 yards) across.

The best measurements of the Yarkovsky effect are made when an asteroid’s position is precisely known. “If an asteroid comes very close, we can get radar observations on it,” says Beshore. “With radar measurements, we get very good data on its range and therefore can constrain one aspect of its orbit very well. If we can get that measurement a couple of times (or more) over a few years, it helps us understand its orbital behavior and we can start to make an estimate of the Yarkovsky effect. We estimate the position of the asteroid and what its orbit must be like by using Newtonian and Relativistic physics. If we see a deviation from the estimated position, then it must be due to the sum of all these other small forces, and the greatest of these we believe to be the Yarkovsky effect.”

Measurements like these enabled the team to estimate the very small force of the Yarkovsky effect on RQ36 — about equal to the weight felt when holding three grapes, according to Beshore. “Although very small, this force is constant and adds up over time to significantly change the asteroid’s orbit,” adds Beshore.

Scheduled for launch in 2016, OSIRIS-REx will arrive at RQ36 in 2018 and orbit the asteroid until 2021. By communicating continuously with a spacecraft in orbit around RQ36, the team will get a much better idea of the asteroid’s orbit.

“We expect OSIRIS-REx will enable us to make an estimate of the Yarkovsky force on RQ36 at least twice as precise as what’s available now,” says Jason Dworkin, OSIRIS-REx project scientist at NASA’s Goddard Space Flight Center in Greenbelt, Md.

The team will use what it learns about the Yarkovsky effect on RQ36 to help estimate the effects on other asteroids. “What we want to be able to do is create a model that says okay if you give me an asteroid of this size, made of this composition, with this kind of topography, I can estimate for you what the Yarkovsky effect will be,” says Beshore. “So now I can probably come up with a better notion of what to expect from other asteroids that I don’t have the good fortune to have a spacecraft around.”

Given that OSIRIS-REx lets us better model the Yarkovsky effect, and we discover an asteroid that might hit us someday, what if anything can be done about it?

“There are several mitigation strategies,” says Beshore. “We could explode a small nuclear device close above the surface on one side of the asteroid. This could be very effective — it would vaporize the surface layer, which would then fly off at very high speed, causing a rocket thrust that would shove everything over by a few centimeters per second. This might be plenty to deflect the asteroid. Other strategies include kinetic impactors, where you strike an asteroid very hard with a heavy projectile moving at high speed. In 2005, NASA’s Deep Impact mission hit comet Tempel 1 with a 370-kilogram (over 815-pound) copper slug at about five kilometers per second (over 11,000 miles per hour), not nearly enough to significantly alter the orbit of the five-kilometer-sized body, but a proof of the technology for this kind of mission. Another idea is to use a gravity tractor — station a spacecraft precisely enough near the asteroid which would gradually deflect it with only its gravitational pull.”

The key to all these strategies is to discover the asteroid well in advance of its impact date and attempt to deflect it early, according to Beshore. “If you’re trying to deflect an arrow, you wouldn’t need to apply much force to the arrow to make it widely miss the target if you could deflect it as it left the bow,” says Beshore. “On the other hand, if you had to deflect it right before it hit the target, you’d need to push on it a whole lot more to get it out of the way.”

One of the first things that would be done if an asteroid appeared to be on a collision course with Earth is to send a probe to the asteroid that might look very much like OSIRIS-REx, according to Beshore. “You want to characterize it first to choose the correct deflection strategy,” says Beshore. “For example, we know the density of RQ36 is about 1 gram per cubic centimeter, over two times less than solid rock. This means it is probably a rubble pile — a collection of boulders, rocks, and dust loosely held together by gravity. Some deflection strategies might be ineffective with this kind of asteroid.”

OSIRIS-REx will determine if RQ36 is actually a rubble pile by orbiting it and revealing the subtle effects on the orbit from the gravity of any large and dense lumps within the asteroid. A probe like OSIRIS-REx could map the internal structure of an asteroid this way, providing valuable information on where to target the deflection mechanism.

OSIRIS-REx will also determine the composition of RQ36 using remote measurements from both visible light and infrared spectrometers, and by collecting a sample of material from the asteroid’s surface and returning it to Earth for study. Since the Yarkovsky effect may vary depending on the type of material and its distribution, a probe with OSIRIS-REx’s capability to map the surface composition will enable a more precise estimate of the Yarkovsky effect on the asteroid’s orbit.

The mission will also provide critical experience navigating around asteroids. “We don’t have a lot of experience doing precise maneuvers near one of these objects with very small gravity,” says Beshore. “It’s not easy to stay in orbit around it — this asteroid’s gravitational pull is so weak, the push from sunlight on our spacecraft’s solar panels will be roughly similar to the amount of force from the gravity of RQ36 itself. We have to factor in a lot of these forces to navigate and operate around an asteroid. With OSIRIS-REx, we’ll generate a set of techniques and technologies for any mission that would go to an asteroid to characterize it in advance of a mitigation mission.”

The OSIRIS-REx mission is led by Principal Investigator Dante Lauretta of the University of Arizona, supported by a science team of Co-Investigators from multiple institutions, with project management at NASA’s Goddard Space Flight Center, Greenbelt, Md., and development partnership with Lockheed Martin Space Systems, Littleton, Colo. International contributions are provided by the Canadian Space Agency. The OSIRIS-REx mission was selected under the NASA New Frontiers program, managed by NASA’s Marshall Space Flight Center, Huntsville, Ala., and funded by NASA’s Science Mission Directorate, NASA Headquarters, Washington.

More information about OSIRIS-REx can be found at: http://osiris-rex.lpl.arizona.edu/

Excavation Set to Shed New Light On London’s Victorian Past

From a clay smoking pipe to Neolithic flint, a 19th Century garden has been revealing some of its secrets to an archaeological team from London’s Kingston University.

Dr Helen Wickstead spotted an opportunity to delve below the surface of an area of land at the University’s Seething Wells hall of residence after looking at historic maps and images of the area alongside the River Thames. The former industrial site had not been excavated before and she was intrigued to see whether she could find traces of a garden marked out on early maps.

Pottery fragment from Seething Wells excavation. (Credit: Image courtesy of Kingston University)

Pottery fragment from Seething Wells excavation. (Credit: Image courtesy of Kingston University)

“The Seething Wells site in Surbiton is of historic significance because the waterworks built there and opened in 1852 were pivotal in improving the health of Londoners. They provided clean, filtered water when cholera had been ravaging the capital,” Dr Wickstead explained. “A garden on a site like this might tell us more about the people who lived and worked nearby — did they use it for leisure, was it just decorative and reserved for the privileged, or was it used for food production? It was a time of great social change so we were keen to roll back the turf to see what we could find.”

The team studied 19th Century maps from English Heritage archives, comparing them with aerial photographs taken during World War II by the Royal Air Force as well as more modern day Google Earth images. “We could see that a path existed across the site and the parched grass visible on modern satellite images also suggested its presence,” Dr Wickstead said.

After digging a 10 metre square trench, the team discovered signs of a path made from cinder and gravel. “That showed us it was a functional feature rather than decorative,” Dr Wickstead, who lectures in heritage, said. “Now we’d like to explore beneath it and sample the soil as it will have captured pollen from plants growing at the time.”

Shells in the gravel section suggest the path was probably made from waste material from the water filter gravel beds that still exist opposite the hall of residence. But one fragment spotted by chance in the waste took the team right back to the Neolithic period. “We were very excited to find a fragment of flint that we believe is a chipping from the making of Neolithic tools,” Dr Wickstead, who is also a pre-historian, said. “It could be as much as 6,000 years old. I expect it came from the river at some point and was caught up in the gravel used in the filter beds. It’s an intriguing find and took us all by surprise.”

The team also unearthed a fragment of red and white pottery with illustrations of two Victorian gentlemen. “I like to imagine one of those people could even be the engineer James Simpson who invented the capital’s water filtration system,” Dr Wickstead said.

Some more recent objects have connections to the war years. The team expected several small metal garden tags they discovered to bear the names of plants. “On closer inspection, two had names of people on them,” Dr Wickstead said. “We’d love to find out more about Derek Ellis and Mabel Gower — perhaps they worked the allotments that were on the site during World War II.”

Students studying historic building conservation joined Dr Wickstead on the dig. Third year Crispin Thomas, who is particularly interested in Medieval carpentry, helped survey the ground with an auger — a drilling device that tests resistance to see how deep top soil is. “I’d never been on an archaeological dig before and I was fascinated to see how much information could be gleaned from such a small space,” he said. “So much evidence for how we got where we are today as a society, in so many aspects of life, is right there under our feet.”

Dr Wickstead said that small green patches of land like that at Seething Wells were scattered all over London and were windows into the past just waiting to be explored. “These little open spaces are like pieces of jigsaw puzzle and no-one has ever put them all together. A comprehensive study would tell us more about the story of the capital and, importantly too, the suburbs that helped the city flourish,” she said.

Most Comprehensive Tree of Life Shows Placental Mammal Diversity Exploded After Age of Dinosaurs

An international team of scientists including University of Florida researchers has generated the most comprehensive tree of life to date on placental mammals, which are those bearing live young, including bats, rodents, whales and humans.

Appearing  February 7 in the journal Science, the study details how researchers used both genetic and physical traits to reconstruct the common ancestor of placental mammals, the creature that gave rise to many mammals alive today. The data show that contrary to a commonly held theory, the group diversified after the extinction of dinosaurs 65 million years ago. The research may help scientists better understand how mammals survived past climate change and how they may be impacted by future environmental conditions.

This is an artist’s rendering of the hypothetical placental ancestor, a small insect-eating animal. The research team reconstructed the anatomy of the animal by mapping traits onto the evolutionary tree most strongly supported by the combined phenomic and genomic data and comparing the features in placental mammals with those seen in their closest relatives. (Credit: Carl Buell)

This is an artist’s rendering of the hypothetical placental ancestor, a small insect-eating animal. The research team reconstructed the anatomy of the animal by mapping traits onto the evolutionary tree most strongly supported by the combined phenomic and genomic data and comparing the features in placental mammals with those seen in their closest relatives. (Credit: Carl Buell)

UF researchers led the team that analyzed the anatomy of living and fossil primates, including lemurs, monkeys and humans, as well as their closest living relatives, flying lemurs and tree shrews. The multi-year collaborative project was funded by the National Science Foundation Assembling the Tree of Life Program.

“With regards to evolution, it’s critical to understand the relationships of living and fossil mammals before asking questions about ‘how’ and ‘why,’ ” said co-author Jonathan Bloch, associate curator of vertebrate paleontology at the Florida Museum of Natural History on the UF campus. “This gives us a new perspective of how major change can influence the history of life, like the extinction of the dinosaurs — this was a major event in Earth’s history that potentially then results in setting the framework for the entire ordinal diversification of mammals, including our own very distant ancestors.”

Visual reconstruction of the placental ancestor — a small, insect-eating animal — was made possible with the help of a powerful cloud-based and publicly accessible database called MorphoBank. Unlike other reconstructions, the new study creates a clearer picture of the tree of life by combining two data types: Phenomic data includes observational traits such as anatomy and behavior, while genomic data is encoded by DNA.

“Discovering the tree of life is like piecing together a crime scene — it is a story that happened in the past that you can’t repeat,” said lead author Maureen O’Leary, an associate professor in the department of anatomical sciences in the School of Medicine at Stony Brook University and research associate at the American Museum of Natural History. “Just like with a crime scene, the new tools of DNA add important information, but so do other physical clues like a body or, in the scientific realm, fossils and anatomy. Combining all the evidence produces the most informed reconstruction of a past event.”

Researchers recorded observational traits for 86 placental mammal species, including 40 fossil species. The resulting database contains more than 12,000 images that correspond to more than 4,500 traits detailing characteristics like the presence or absence of wings, teeth and certain bones, type of hair cover and brain structures. The dataset is about 10 times larger than information used in previous studies of mammal relationships.

“It was a great way to learn anatomy, in a nutshell,” said co-author Zachary Randall, a UF biology graduate student and research associate at the Florida Museum. “While coding for humans, I could clearly see which anatomical features are unique, shared or not shared with other groups of mammals. This study is a great backbone for future work.”

Bloch and Randall collaborated with study co-authors Mary Silcox of the University of Toronto Scarborough and Eric Sargis of Yale University to characterize humans, plus seven other living and one fossil species from the clade Euarchonta, which includes primates, tree shrews and flying lemurs.

“I think this database is amazing because it’s being presented in such a way that it will be reproducible for the future generations,” Bloch said. “It illustrates exactly what we did and leaves nothing to the imagination — you can actually go to the pictures and see it.”

The evolutionary history of placental mammals has been interpreted in very different ways depending on the data analyzed. One leading analysis based on genomic data alone predicted that a number of placental mammal lineages existed in the Late Cretaceous and survived the Cretaceous-Paleogene extinction.

“It has been suggested that primates diverged from other mammals well before the extinction of the dinosaurs, but our work using direct evidence from the fossil record tells a different story,” Bloch said.

The team reconstructed the anatomy of the placental common ancestor by mapping traits most strongly supported by the data to determine it had a two-horned uterus, a brain with a convoluted cerebral cortex, and a placenta in which maternal blood came in close contact with membranes surrounding the fetus, as in humans.

Sense of Smell of Tyrannosaurus

Although we know quite a bit about the lifestyle of dinosaur; where they lived, what they ate, how they walked, not much was known about their sense of smell, until now.

Scientists at the University of Calgary and the Royal Tyrrell Museum are providing new insight into the sense of smell of carnivorous dinosaurs and primitive birds in a research paper published in the British journal Proceedings of the Royal Society B. The study, by U of C paleontologist Darla Zelenitsky and Royal Tyrrell Museum curator of dinosaur palaeoecology François Therrien, is the first time that the sense of smell has been evaluated in prehistoric meat-eating dinosaurs. They found that Tyrannosaurus rex had the best nose of all meat-eating dinosaurs, and their results tone down the reputation of T. rex as a scavenger.

UCMP's T. rex skeleton

The researchers looked at the importance of the sense of smell among various meat-eating dinosaurs, also called theropods, based on the size of their olfactory bulbs, the part of the brain associated with the sense of smell. Although the brains of dinosaurs are not preserved, the impressions they left on skull bones or the space they occupied in the skull reveals the size and shape of the different parts of the brain. Zelenitsky and Therrien CT-scanned and measured the skulls of a wide variety of theropod dinosaurs, including raptors and ostrich-like dinosaurs, as well as the primitive bird Archaeopteryx.

“T. rex has previously been accused of being a scavenger due to its keen sniffer, although its nose may point to alternative lifestyles based on what we see in living animals” says Zelenitsky, the lead investigator on the study. “Large olfactory bulbs are found in living birds and mammals that rely heavily on smell to find meat, in animals that are active at night, and in those animals that patrol large areas. Although the king of carnivorous dinosaurs wouldn’t have passed on scavenging a free dead meal, it may have used its sense of smell to strike at night or to navigate through large territories to find its next victim.”

In addition to providing clues about the biology and behavior of the ancient predators, the study also reveals some surprising information about the sense of smell in the ancestors of modern birds.

Therrien and Zelenitsky found that the extinct bird Archaeopteryx, known to have evolved from small meat-eating dinosaurs, had an olfactory bulb size comparable to most theropod dinosaurs. Although sight is very good in most birds today, their sense of smell is usually poor, a pattern that does not hold true in the ancestry of living birds.

“Our results tell us that the sense of smell in early birds was not inferior to that of meat-eating dinosaurs,” says Therrien. “Although it had been previously suggested that smell had become less important than eye sight in the ancestors of birds, we have shown that this wasn’t so. The primitive bird Archaeopteryx had a sense of smell comparable to meat-eating dinosaurs, while at the same time it had very good eye sight. The sense of smell must have become less important at some point during the evolution of those birds more advanced than Archaeopteryx.”

Note: This story has been adapted from an earlier news release issued by University of Calgary

Museum of Somerset marine insect fossil study starts

Most of the fossils from Strawberry Bank were found in this package found in the Taunton collection

A collection of 3,000 marine fossils “rediscovered” at the Museum of Somerset two years ago has now been curated by fossil experts.

The fossils were excavated by the geologist Charles Moore during the 1800s at Strawberry Bank near Ilminster and other sites around the South West.

Satchel where most of the Strawberry Bank fossils were found

Since these items were catalogued, it has been discovered they are the remaining 15% of the larger Strawberry Bank fossil collection which had been “missing” for several decades.

This now means the collection Moore wrote about in his diaries is fully restored and accounted for.

Jurassic insect diversity

The Strawberry Bank fossil collection is considered to be rare and unusual by experts because of the detail in the muscles, guts, and traces of skin of the insects and fish.

Taunton collection of fossils wrapped in newspapers of the day Some Taunton fossils were found wrapped in newspapers which are also being preserved

There is also the possibility there could be new species among the collection although it will take time before this is established.

The Bath Royal Literary and Scientific Institution has been overseeing the project to restore the Strawberry Bank fossils.

Matt Williams, the collection manager for the project, said: “If there are new species among the insects, it’s important as palaeontologists are always interested in the diversity of prehistoric ecosystems.

“Often new fossil [extinct] species also help us to understand the evolutionary history of groups of living [extant] animals.”

‘Big flashy stuff’

Now the fossils in Taunton have been fully catalogued, research work can begin.

Mr Williams said: “About 15% of the collection I looked at was from Strawberry Bank and there were over 500 specimens of insects that could be identified at order level.

“There were nine different orders – dragonflies and damsel flies, cockroaches, earwigs, grasshoppers, crickets and locusts, true bugs, beetles, flies, scorpion flies and lacewings.”

All of the fossils date back to 183 million years ago during the Jurassic period.

The collection also offers an insight into Moore’s approach to fossil collecting.

“He didn’t have a collecting bias towards larger fossils,” explained Mr Williams.

“Some collectors in the past have only collected the big flashy stuff and have ignored the tiny little things.

“But here we’ve got the entire fauna so we can look at the ecological interrelations of the animals and start to produce a really interesting narrative both in terms of science and communication about the history of that area.”

Mr Williams has worked with Dennis Parsons at the Somerset Heritage Centre, Somerset Archaeological Natural History Society, which owns the collection, and leading insect fossil expert Andrew Ross, from the Museum of Scotland, to get the Taunton collection curated.

‘Perfect detail’

However, the quality of the collection has been variable.

“They’re not as well preserved as the fish and the reptiles from that locality [Strawberry Bank],” he said.

“Obviously they are fairly well preserved that they can be identified to that level – some of those fossils that I was looking at I couldn’t see at all but Andrew [Ross] who’s a real expert could tell me what it was.

“That said, you could see some of the wings in perfect detail – so it is quite variable but enough to be quite informative about the animals that were living there.”

He said the variation was due to the type of limestone the fossils were excavated from, which can reduce the level of detail – or resolution – of the specimens.

The hope now is to learn more about the fauna during this period and attract further research.

“We’ll try to get some more researchers to work on specific elements of it now we understand what the different things are – say for people who are particularly interested in scorpion flies from that age, or insects from that age, we’ll do something on that,” Mr Williams said.

“We’ll see if we can look at broader relations, such as the trophic relationships, what was eating what from that locality.”

Source: article by Tammy McAllister BBC News, Somerset

 

New Kind of Extinct Flying Reptile Discovered

A new kind of pterosaur, a flying reptile from the time of the dinosaurs, has been identified by scientists from the Transylvanian Museum Society in Romania, the University of Southampton in the UK and the Museau Nacional in Rio de Janiero, Brazil.

Full body reconstruction of Eurazhdarcho langendorfensis. Preserved skeletal elements are in white. Scale bar is 500 mm. (Credit: Image courtesy of Mark Witton / Citation: Mátyás Vremir, Alexander W. A. Kellner, Darren Naish, Gareth J. Dyke. A New Azhdarchid Pterosaur from the Late Cretaceous of the Transylvanian Basin, Romania: Implications for Azhdarchid Diversity and Distribution. PLoS ONE, 2013; 8 (1): e54268 DOI: 10.1371/journal.pone.0054268)

Full body reconstruction of Eurazhdarcho langendorfensis. Preserved skeletal elements are in white. Scale bar is 500 mm. (Credit: Image courtesy of Mark Witton / Citation: Mátyás Vremir, Alexander W. A. Kellner, Darren Naish, Gareth J. Dyke. A New Azhdarchid Pterosaur from the Late Cretaceous of the Transylvanian Basin, Romania: Implications for Azhdarchid Diversity and Distribution. PLoS ONE, 2013; 8 (1): e54268 DOI: 10.1371/journal.pone.0054268)

The fossilised bones come from the Late Cretaceous rocks of Sebeş-Glod in the Transylvanian Basin, Romania, which are approximately 68 million years old. The Transylvanian Basin is world-famous for its many Late Cretaceous fossils, including dinosaurs of many kinds, as well as fossilised mammals, turtles, lizards and ancient relatives of crocodiles.

A paper on the new species, named Eurazhdarcho langendorfensis has been published in the online journal PLoS ONE. Dr Darren Naish, from the University of Southampton’s Vertebrate Palaeontology Research Group, who helped identify the new species, says: “Eurazhdarcho belong to a group of pterosaurs called the azhdarchids. These were long-necked, long-beaked pterosaurs whose wings were strongly adapted for a soaring lifestyle. Several features of their wing and hind limb bones show that they could fold their wings up and walk on all fours when needed.

“With a three-metre wingspan, Eurazhdarcho would have been large, but not gigantic. This is true of many of the animals so far discovered in Romania; they were often unusually small compared to their relatives elsewhere.”

The discovery is the most complete example of an azhdarchid found in Europe so far and its discovery supports a long-argued theory about the behaviour of these types of creatures.

Dr Gareth Dyke, Senior Lecturer in Vertebrate Palaeontology, based at the National Oceanography Centre Southampton says: “Experts have argued for years over the lifestyle and behaviour of azhdarchids. It has been suggested that they grabbed prey from the water while in flight, that they patrolled wetlands and hunted in a heron or stork-like fashion, or that they were like gigantic sandpipers, hunting by pushing their long bills into mud.

“One of the newest ideas is that azhdarchids walked through forests, plains and other places in search of small animal prey. Eurazhdarcho supports this view of azhdarchids, since these fossils come from an inland, continental environment where there were forests and plains as well as large, meandering rivers and swampy regions.”

Fossils from the region show that there were several places where both giant azhdarchids and small azhdarchids lived side by side. Eurazhdarcho‘s discovery indicates that there were many different animals hunting different prey in the region at the same time, demonstrating a much more complicated picture of the Late Cretaceous world than first thought.