Dinosaur Diary : Utahraptor

Name: Utahraptor ostrommaysorum
(Pronunciation: YOU-tah-WRAP-tore ah-STROM-ay-SORE-um)

Age: Early Cretaceous (~125 million years ago)

Where It’s Found in Utah: Dalton Wells Quarry and Gaston Quarry, near Moab, Grand County, Utah.
Geologic Formation: Cedar Mountain Formation (Yellow Cat Member)

Classification: Saurischia – Theropoda – Coelurosauria – Dromaeosauridae

Utahraptor

Utahraptor

Description: Utahraptor ostrommaysorum is one of the geologically oldest and largest known dromaeosaurids. This group of carnivorous dinosaurs had a large retractable sickle claw on its foot, specialized for cutting.  With a name meaning “Utah’s predator,” Utahraptor was a ferocious hunter that used its sickle-shaped claws to attack and rip apart its prey. The claw itself was 9.5 inches (24 cm) long! The species name ‘ostrommaysorumhonors Dr. John Ostrom of Yale University for his pioneering research linking carnivorous dinosaurs to the ancestry of birds. Utahraptor was the inspiration for the Velociraptors in the film Jurassic Park! Utahraptor, however, was quite a bit bigger than Velociraptor; adults were around 23 feet (7 meters) long and around 6 feet (1.8 meters) tall at the hip.

Why It’s a Top NHMU Dinosaur:  Prior to the discovery of Utahraptor, paleontologists believed sickle-clawed dromaeosaurids were small carnivores that only lived in the Late Cretaceous. Utahraptor required paleontologists to revise their understanding of this family of dinosaurs as it was much larger and lived the Early Cretaceous. In addition, Utahraptor is closely related to birds.  Dromaeosaurids, troodontids (small bipedal theropod feathered dinosaurs that also had a sickle claw on the foot), and the ancestors of modern birds all reside on the same branch of the dinosaur family tree.  It may be hard to think of something so large and ferocious as being related to birds. A decrease in body size had to occur for these animals to evolve flight and to resemble more closely the birds we see today. Although dromaeosaurids died out some 65.5 million years ago, their close relatives survived and became remarkably successful. Remember, not all dinosaurs went extinct!

CT and 3-D Printers Used to Recreate Dinosaur Fossils

Data from computed tomography (CT) scans can be used with three-dimensional (3-D) printers to make accurate copies of fossilized bones, according to new research published online in the journal Radiology.

Fossils are often stored in plaster casts, or jackets, to protect them from damage. Getting information about a fossil typically requires the removal of the plaster and all the sediment surrounding it, which can lead to loss of material or even destruction of the fossil itself.

3-D print of vertebral body. (Credit: Image courtesy of Radiological Society of North America)

3-D print of vertebral body. (Credit: Image courtesy of Radiological Society of North America)

German researchers studied the feasibility of using CT and 3-D printers to nondestructively separate fossilized bone from its surrounding sediment matrix and produce a 3-D print of the fossilized bone itself.

“The most important benefit of this method is that it is non-destructive, and the risk of harming the fossil is minimal,” said study author Ahi Sema Issever, M.D., from the Department of Radiology at Charité Campus Mitte in Berlin. “Also, it is not as time-consuming as conventional preparation.”

Dr. Issever and colleagues applied the method to an unidentified fossil from the Museum für Naturkunde, a major natural history museum in Berlin. The fossil and others like it were buried under rubble in the basement of the museum after a World War II bombing raid. Since then, museum staff members have had difficulty sorting and identifying some of the plaster jackets.

Researchers performed CT on the unidentified fossil with a 320-slice multi-detector system. The different attenuation, or absorption of radiation, through the bone compared with the surrounding matrix enabled clear depiction of a fossilized vertebral body.

After studying the CT scan and comparing it to old excavation drawings, the researchers were able to trace the fossil’s origin to the Halberstadt excavation, a major dig from 1910 to 1927 in a clay pit south of Halberstadt, Germany. In addition, the CT study provided valuable information about the condition and integrity of the fossil, showing multiple fractures and destruction of the front rim of the vertebral body.

Furthermore, the CT dataset helped the researchers build an accurate reconstruction of the fossil with selective laser sintering, a technology that uses a high-powered laser to fuse together materials to make a 3-D object.

Dr. Issever noted that the findings come at a time when advances in technology and cheaper availability of 3-D printers are making them more common as a tool for research. Digital models of the objects can be transferred rapidly among researchers, and endless numbers of exact copies may be produced and distributed, greatly advancing scientific exchange, Dr. Issever said. The technology also potentially enables a global interchange of unique fossils with museums, schools and other settings.

“The digital dataset and, ultimately, reproductions of the 3-D print may easily be shared, and other research facilities could thus gain valuable informational access to rare fossils, which otherwise would have been restricted,” Dr. Issever said. “Just like Gutenberg’s printing press opened the world of books to the public, digital datasets and 3-D prints of fossils may now be distributed more broadly, while protecting the original intact fossil.”

Newly Discovered Protist Suggests Evolutionary Answers, Questions

From Massachusetts to Mississippi, a unicellular protist is hinting at answers about the evolution of multicellularity while raising a whole new set of questions.

Matthew Brown, assistant professor of biological sciences at Mississippi State University, recently led a research team that identified the protist as a new organism and classified its genomics. Obazoa is the name of the new group.

Jeffrey Silberman collected sediment specimens in Marstons Mills, a village in Barnstable, Mass., and the University of Arkansas associate professor isolated an organism he found. Since Brown had begun post-doctoral work in genomics at Dalhousie University in Nova Scotia, Silberman offered his former UA doctoral student the opportunity to name and classify it on the evolutionary tree of life.

Mississippi State University's Matthew Brown, associate professor of biological sciences, led a team that recently classified this newly discovered protist, Pygsuia biforma.

Mississippi State University’s Matthew Brown, associate professor of biological sciences, led a team that recently classified this newly discovered protist, Pygsuia biforma.

Brown headed the investigation that discovered the unicellular organism’s proteins and genes are similar to those found in multicellular life-forms.

“We then looked for specific multicellular toolkit genes, and we found genes that scientists had believed to be animal-specific,” Brown said. “Integrins and the whole suite of proteins that work with integrins were thought to be something innate to multicellularity and used only for cell-to-cell communication.

“This discovery shows that these genes have been co-opted for a different use. We don’t know what it does in unicellular organisms, but we can now place the origin of genes that are associated with multicellularity in unicellular organisms.”

Additionally, the anaerobic protist has mitochondria, energy factories that produce adenosine triphosphate, or ATP. Brown said ATP production typically requires oxygen, but the protist lives in oxygen depleted environments. As a result, Pygsuia biforma raises questions related to the presence and function of mitochondria in anaerobic unicellular organisms.

These discoveries and new research questions they raise are important because they offer new insights into the science of evolution, Brown explained.

“By tracking the evolutionary history of these particular organisms, we’re able to look at ancestral states of certain gene suites, and that’s the really important thing — we need a better understanding of protist diversity and protist genome evolution to understand how organisms like animals evolved,” Brown said.

Amber Provides New Insights Into the Evolution of Earth’s Atmosphere: Low Oxygen Levels for Dinosaurs

An international team of researchers led by Ralf Tappert, University of Innsbruck, reconstructed the composition of Earth’s atmosphere of the last 220 million years by analyzing modern and fossil plant resins. The results suggest that atmospheric oxygen was considerably lower in Earth’s geological past than previously assumed. This new study questions some of the current theories about the evolution of climate and life, including the causes for the gigantism of dinosaurs.

Scientists encounter big challenges when reconstructing atmospheric compositions in Earth’s geological past because of the lack of useable sample material. One of the few organic materials that may preserve reliable data of Earth’s geological history over millions of years are fossil resins (e.g. amber). “Compared to other organic matter, amber has the advantage that it remains chemically and isotopically almost unchanged over long periods of geological time,” explains Ralf Tappert from the Institute of Mineralogy and Petrography at the University of Innsbruck. The mineralogist and his colleagues from the University of Alberta in Canada and universities in the USA and Spain have produced a comprehensive study of the chemical composition of Earth’s atmosphere since the Triassic period.

The team analyzed amber samples from almost all well-known amber deposits worldwide. This amber originates from the Cretaceous period, an inclusion of foliage of the extinct conifer tree Parataxodium sp. from the Foremost Formation at Grassy Lake, Alberta, Canada. It is approximately 77 million years old. (Credit: Ryan C. McKellar)

The team analyzed amber samples from almost all well-known amber deposits worldwide. This amber originates from the Cretaceous period, an inclusion of foliage of the extinct conifer tree Parataxodium sp. from the Foremost Formation at Grassy Lake, Alberta, Canada. It is approximately 77 million years old. (Credit: Ryan C. McKellar)

The study has been published in the journal Geochimica et Cosmochimica Acta. The interdisciplinary team, consisting of mineralogists, paleontologists and geochemists, use the preserving properties of plant resins, caused by polymerization, for their study. “During photosynthesis plants bind atmospheric carbon, whose isotopic composition is preserved in resins over millions of years, and from this, we can infer atmospheric oxygen concentrations,” explains Ralf Tappert. The information about oxygen concentration comes from the isotopic composition of carbon or rather from the ratio between the stable carbon isotopes 12C and 13C.

Atmospheric oxygen between 10 and 15 percent

The research team analyzed a total of 538 amber samples from from well-known amber deposits worldwide, with the oldest samples being approximately 220 million years old and recovered from the Dolomites in Italy. The team also compared fossil amber with modern resins to test the validity of the data. The results of this comprehensive study suggest that atmospheric oxygen during most of the past 220 million years was considerably lower than today’s 21 percent. “We suggest numbers between 10 and 15 percent,” says Tappert. These oxygen concentrations are not only lower than today but also considerably lower than the majority of previous investigations propose for the same time period. For the Cretaceous period (65 — 145 million years ago), for example, up to 30 percent atmospheric oxygen has been suggested previously.

Effects on climate and environment

The researchers also relate this low atmospheric oxygen to climatic developments in Earth’s history. “We found that particularly low oxygen levels coincided with intervals of elevated global temperatures and high carbon dioxide concentrations,” explains Tappert. The mineralogist suggests that oxygen may influence carbon dioxide levels and, under certain circumstances, might even accelerate the influx of carbon dioxide into the atmosphere. “Basically, we are dealing here with simple oxidation reactions that are amplified particularly during intervals of high temperatures such as during the Cretaceous period.” The researchers, thus, conclude that an increase in carbon dioxide levels caused by extremely strong vulcanism was accompanied by a decrease of atmospheric oxygen. This becomes particularly apparent when looking at the last 50 million years of geological history. Following the results of this study, the comparably low temperatures of the more recent past (i.e. the Ice Ages) may be attributed to the absence of large scale vulcanism events and an increase in atmospheric oxygen.

Oxygen may not be the cause of gigantism

According to the results of the study, oxygen may indirectly influence the climate. This in turn may also affect the evolution of life on Earth. A well-known example are dinosaurs: Many theories about animal gigantism offer high levels of atmospheric oxygen as an explanation. Tappert now suggests to reconsider these theories: “We do not want to negate the influence of oxygen for the evolution of life in general with our study, but the gigantism of dinosaurs cannot be explained by those theories.” The research team highly recommends conducting further studies and intends to analyze even older plant resins.

Fossil of New Big Cat Species Discovered: Oldest Ever Found

The oldest big cat fossil ever found — which fills in a significant gap in the fossil record — was discovered on a paleontological dig in Tibet, scientists announced today.

A skull from the new species, named Panthera blytheae, was excavated and described by a team led by Jack Tseng — a PhD student at the USC Dornsife College of Letters, Arts and Sciences at the time of the discovery, and now a postdoctoral fellow at the American Museum of Natural History (AMNH) in New York.

“This find suggests that big cats have a deeper evolutionary origin than previously suspected,” Tseng said.

The announcement was made in a scientific paper published by the Proceedings of the Royal Society B: Biological Sciences, on Nov. 13.

Tseng’s coauthors include Xiaoming Wang, who has joint appointments at USC, the Natural History Museum of Los Angeles County (NHM) and the Page Museum at the La Brea Tar Pits, the AMNH, and the Chinese Academy of Sciences (CAS); Graham Slater of the Smithsonian Institution; Gary Takeuchi of the NHM and the Page Museum at the La Brea Tar Pits; Qiang Li of the CAS; Juan Liu of the University of Alberta and the CAS; and Guangpu Xie of the Gansu Provincial Museum.

At left is: Life reconstruction of Panthera blytheae based on skull CT data; illustrated by Mauricio Antón. At Right are images of the holotype specimen and reconstructed facial bones based on CT data; Figure 1 from the paper. (Credit: Mauricio Antón (left) and Figure 1 from the paper (right).)

At left is: Life reconstruction of Panthera blytheae based on skull CT data; illustrated by Mauricio Antón. At Right are images of the holotype specimen and reconstructed facial bones based on CT data; Figure 1 from the paper. (Credit: Mauricio Antón (left) and Figure 1 from the paper (right).)

DNA evidence suggests that the so-called “big cats” — the Pantherinae subfamily, including lions, jaguars, tigers, leopards, snow leopards, and clouded leopards — diverged from their nearest evolutionary cousins, Felinae (which includes cougars, lynxes, and domestic cats), about 6.37 million years ago. However, the oldest fossils of big cats previously found are tooth fragments uncovered at Laetoli in Tanzania (the famed hominin site excavated by Mary Leakey in the 1970s), dating to just 3.6 million years ago.

Using magnetostratigraphy — dating fossils based on the distinctive patterns of reversals in Earth’s magnetic field, which are recorded in layers of rock — Tseng and his team were able to estimate the age of the skull at between 4.10 and 5.95 million years old.

The new cat takes its name from Blythe, the snow-leopard-loving daughter of Paul and Heather Haaga, who are avid supporters of the Natural History Museum of Los Angeles County.

The find not only challenges previous suppositions about the evolution of big cats, it also helps place that evolution in a geographical context. The find occurs in a region that overlaps the majority of current big cat habitats, and suggests that the group evolved in central Asia and spread outward.

In addition, recent estimates suggested that the genus Panthera (lions, tigers, leopards, jaguars, and snow leopards) did not split from genus Neofelis (clouded leopards) until 3.72 million years ago — which the new find disproves.

Tseng, his wife Juan Liu, and Takeuchi discovered the skull in 2010 while scouting in the remote border region between Pakistan and China — an area that takes a bumpy seven-day car ride to reach from Beijing.

Liu found over one hundred bones that were likely deposited by a river eroding out of a cliff. There, below the antelope limbs and jaws, was the crushed — but largely complete — remains of the skull.

“It was just lodged in the middle of all that mess,” Tseng said.

For the past three years, Tseng and his team have used both anatomical and DNA data to determine that the skull does, in fact, represent a new species.

They plan to return to the site where they found the skull in the summer to search for more specimens.

“We are in the business of discovery,” said Wang, curator of vertebrate paleontology at the NHM; adjunct professor of geoscience and biology at USC; and research associate at AMNH. “We go out into the world in search of new fossils to illuminate the past.”

Rutile Mineral Can Reveal the History of a Rock

Researchers can use the mineral rutile to learn about rock types and their history. Two articles published in the journal Geology now present a new application of a method for more easily tracing the mineral rutile. The co-authors of the articles are researchers at the University of Gothenburg.

Rutile is used in ceramics and paints, but is particularly useful for finding out about the history of a rock.

Where mineral deposits are found, rutile is often also present. The new methods therefore bring opportunities for strategies to find other mineral deposits, such as gold.

"We can identify the rock from which the rutile originates, even if we only have a tiny grain of rutile,” says researcher Thomas Zack, University of Gothenburg. (Credit: Image courtesy of University of Gothenburg)

“We can identify the rock from which the rutile originates, even if we only have a tiny grain of rutile,” says researcher Thomas Zack, University of Gothenburg. (Credit: Image courtesy of University of Gothenburg)

Until now, rutile has been a relatively unknown mineral, despite not being rare. For example, rutile can be found on most sandy beaches around the world, including in Sweden.

“It’s incredible to see how little attention was paid to rutile until around five years ago,” says geologist and researcher Thomas Zack, from the University of Gothenburg’s Department of Earth Sciences, who has devoted much of his scientific career to studying the mineral.

Now, geologists can identify rock types containing rutile and follow the changes in temperature and pressure that they have been exposed to throughout its history, even if rutile is barely visible to the naked eye. Previously, researchers had to investigate considerably more rutile-bearing samples in order to carry out analyses.

“But now we can identify the rock from which the rutile originates, even if we only have a tiny grain of rutile,” adds Thomas Zack.

The new method is called “Laser Ablation ICP-MS,” and produces results much faster than previous methods.

“In analytical terms, this is one of the most important analytical instruments at the Department of Earth Sciences here in Gothenburg,” concludes Thomas Zack.

Biomechanics of Running Indicates Endothermy in Bipedal Dinosaurs

One of the great unresolved controversies in paleobiology is whether extinct dinosaurs were endothermic, ectothermic, or some combination thereof, and when endothermy first evolved in the lineage leading to birds. Although it is well established that high, sustained growth rates and, presumably, high activity levels are ancestral for dinosaurs and pterosaurs (clade Ornithodira), other independent lines of evidence for high metabolic rates, locomotor costs, or endothermy are needed. For example, some studies have suggested that, because large dinosaurs may have been homeothermic due to their size alone and could have had heat loss problems, ectothermy would be a more plausible metabolic strategy for such animals.

Schematic of extensor fascicle length (lfasc), the GRF vector moment arm (R; segmental gravitational, but not inertial, moments were also included but not shown here; see [48]), and the extensor (antigravity) muscle moment arm (r) for the hip joint. show more  These parameters were calculated at midstance for the antigravity muscle groups at the hip, knee, and ankle, and combined with step length (estimated from hip height) to estimate the volume of muscle activated per meter travelled (Vmusc); see Methods. Joint angles and position of the center of mass (yellow circle) are taken from Hutchinson [40]. Adapted with permission from original artwork by Scott Hartman.  doi:10.1371/journal.pone.0007783.g001

Schematic of extensor fascicle length (lfasc), the GRF vector moment arm (R; segmental gravitational, but not inertial, moments were also included but not shown here; see [48]), and the extensor (antigravity) muscle moment arm (r) for the hip joint.
These parameters were calculated at midstance for the antigravity muscle groups at the hip, knee, and ankle, and combined with step length (estimated from hip height) to estimate the volume of muscle activated per meter travelled (Vmusc); see Methods. Joint angles and position of the center of mass (yellow circle) are taken from Hutchinson [40]. Adapted with permission from original artwork by Scott Hartman.
doi:10.1371/journal.pone.0007783.g001

Methodology/Principal Findings

Here we describe two new biomechanical approaches for reconstructing the metabolic rate of 14 extinct bipedal dinosauriforms during walking and running. These methods, well validated for extant animals, indicate that during walking and slow running the metabolic rate of at least the larger extinct dinosaurs exceeded the maximum aerobic capabilities of modern ectotherms, falling instead within the range of modern birds and mammals. Estimated metabolic rates for smaller dinosaurs are more ambiguous, but generally approach or exceed the ectotherm boundary.

 

Conclusions/Significance

Our results support the hypothesis that endothermy was widespread in at least larger non-avian dinosaurs. It was plausibly ancestral for all dinosauriforms (perhaps Ornithodira), but this is perhaps more strongly indicated by high growth rates than by locomotor costs. The polarity of the evolution of endothermy indicates that rapid growth, insulation, erect postures, and perhaps aerobic power predated advanced “avian” lung structure and high locomotor costs.

Citation: Pontzer H, Allen V, Hutchinson JR (2009) Biomechanics of Running Indicates Endothermy in Bipedal Dinosaurs. PLoS ONE 4(11): e7783. doi:10.1371/journal.pone.0007783

Editor: Andrew Allen Farke, Raymond M. Alf Museum of Paleontology, United States of America

Dogs Likely Originated in Europe More Than 18,000 Years Ago, Biologists Report

Wolves likely were domesticated by European hunter-gatherers more than 18,000 years ago and gradually evolved into dogs that became household pets, UCLA life scientists report.

“We found that instead of recent wolves being closest to domestic dogs, ancient European wolves were directly related to them,” said Robert Wayne, a professor of ecology and evolutionary biology in UCLA’s College of Letters and Science and senior author of the research. “This brings the genetic record into agreement with the archaeological record. Europe is where the oldest dogs are found.”

Ancient dog fossil A fossil of a dog that lived approximately 8,500 years ago, from the Koster archaeological site in Illinois. (Credit: Del Baston)

Ancient dog fossil A fossil of a dog that lived approximately 8,500 years ago, from the Koster archaeological site in Illinois. (Credit: Del Baston)

The UCLA researchers’ genetic analysis is published Nov. 15 in the journal Science and featured on the journal’s cover.

In related research last May, Wayne and his colleagues reported at the Biology of Genomes meeting in New York the results of their comparison of the complete nuclear genomes of three recent wolf breeds (from the Middle East, East Asia and Europe), two ancient dog breeds and the boxer dog breed.

“We analyzed those six genomes with cutting-edge approaches and found that none of those wolf populations seemed to be closest to domestic dogs,” Wayne said. “We thought one of them would be, because they represent wolves from the three possible centers of dog domestication, but none was. All the wolves formed their own group, and all the dogs formed another group.”

The UCLA biologists also hypothesized at that conference that a now-extinct population of wolves was more directly related to dogs.

For the current study in Science, the researchers studied 10 ancient “wolf-like” animals and eight “dog-like” animals, mostly from Europe. These animals were all more than 1,000 years old, most were thousands of years old, and two were more than 30,000 years old.

The biologists studied the mitochondrial DNA of the animals, which is abundant in ancient remains. (Mitochondria are tiny sub-cellular structures with their own small genome.) By comparing this ancient mitochondrial DNA with the modern mitochondrial genomes of 77 domestic dogs, 49 wolves and four coyotes, the researchers determined that the domestic dogs were genetically grouped with ancient wolves or dogs from Europe — not with wolves found anywhere else in the world or even with modern European wolves. Dogs, they concluded, derived from ancient wolves that inhabited Europe and are now extinct.

Wayne said that that the domestication of predatory wolves likely occurred among ancient hunter-gatherer groups rather than as part of humans’ development of sedentary, agricultural-based communities.

“The wolf is the first domesticated species and the only large carnivore humans ever domesticated,” Wayne said. “This always seemed odd to me. Other wild species were domesticated in association with the development of agriculture and then needed to exist in close proximity to humans. This would be a difficult position for a large, aggressive predator. But if domestication occurred in association with hunter-gatherers, one can imagine wolves first taking advantage of the carcasses that humans left behind — a natural role for any large carnivore — and then over time moving more closely into the human niche through a co-evolutionary process.”

The idea of wolves following hunter-gatherers also helps to explain the eventual genetic divergence that led to the appearance of dogs, he said. Wolves following the migratory patterns of these early human groups would have given up their territoriality and would have been less likely to reproduce with resident territorial wolves. Wayne noted that a group of modern wolves illustrates this process.

“We have an analog of this process today, in the only migratory population of wolves known existing in the tundra and boreal forest of North America,” he said. “This population follows the barren-ground caribou during their thousand-kilometer migration. When these wolves return from the tundra to the boreal forest during the winter, they do not reproduce with resident wolves there that never migrate. We feel this is a model for domestication and the reproductive divergence of the earliest dogs from wild wolves.

“We know also that there were distinct wolf populations existing ten of thousands of years ago,” Wayne added. “One such wolf, which we call the megafaunal wolf, preyed on large game such as horses, bison and perhaps very young mammoths. Isotope data show that they ate these species, and the dog may have been derived from a wolf similar to these ancient wolves in the late Pleistocene of Europe.”

In research published in the journal nature in 2010, Wayne and colleagues reported that dogs seem to share more genetic similarity with living Middle Eastern gray wolves than with any other wolf population, which suggested a Middle East origin for modern dogs. The new genetic data have convinced him otherwise.

“When we previously found some similarity between Middle Eastern wolves and domestic dogs, that similarity, we are now able to show, likely was the result of interbreeding between dog and wolves during dog history. It does not necessarily suggest an origin in the Middle East,” Wayne said. “This alternative hypothesis, in retrospect, is one that we should have considered more closely. As hunter-gatherers moved around the globe, their dogs trailing behind probably interbred with wolves.”

Wayne considers the new genetic data “persuasive” but said they need to be confirmed with an analysis of genetic sequences from the nucleus of the cell (roughly 2 billion base pairs) — a significantly larger sample than that found in mitochondrial DNA (approximately 20,000 base pairs). This is challenging because the nuclear DNA of ancient remains tends to become degraded.

While Wayne plans to pursue this follow-up research, he said he does not expect a nuclear genome analysis to change the central finding. However, he said, it will fill in more of the details.

“This is not the end-story in the debate about dog domestication, but I think it is a powerful argument opposing other hypotheses of origin,” he said.

There is a scientific debate over when dogs were domesticated and whether it was linked with the development of agriculture fewer than 10,000 years ago, or whether it occurred much earlier. In the new Science research, Wayne and his colleagues estimate that dogs were domesticated between 18,000 and 32,000 years ago.

The research was federally funded by the National Science Foundation.

Co-authors on the Science paper include Olaf Thalmann, a former postdoctoral scholar in Wayne’s laboratory who is currently the Marie Curie Postdoctoral Fellow at Finland’s University of Turku; Daniel Greenfield, a former technician in Wayne’s laboratory; Francesc López-Giráldez, a former graduate student in Wayne’s laboratory who is currently a postdoctoral scholar at Yale University; Adam Freedman, a former postdoctoral scholar in Wayne’s laboratory; Rena Schweizer, a current UCLA graduate student in Wayne’s laboratory; Klaus Koepfli, a former postdoctoral scholar in Wayne’s laboratory; and Jennifer Leonard, who earned her doctorate from UCLA.

Approximately 80 percent of dog breeds are modern breeds that evolved in the last few hundred years, Wayne said. But some dog breeds have ancient histories that go back thousands of years.

Wolves have been in the Old World for hundreds of thousands of years. The oldest dogs from the archaeological record come from Europe and Western Russia. A dog from Belgium dates back approximately 36,000 years, and a group of dogs from Western Russia is approximately 15,000 years old, Wayne said.

Evidence of 3.5-Billion-Year-Old Bacterial Ecosystems Found in Australia

Reconstructing the rise of life during the period of Earth’s history when it first evolved is challenging. Earth’s oldest sedimentary rocks are not only rare, but also almost always altered by hydrothermal and tectonic activity. A new study from a team including Carnegie’s Nora Noffke, a visiting investigator, and Robert Hazen revealed the well-preserved remnants of a complex ecosystem in a nearly 3.5 billion-year-old sedimentary rock sequence in Australia.

Their work is published in Astrobiology.

The Pilbara district of Western Australia constitutes one of the famous geological regions that allow insight into the early evolution of life. Mound-like deposits created by ancient photosynthetic bacteria, called stromatolites, and microfossils of bacteria have been described by scientists in detail. However, a phenomenon called microbially induced sedimentary structures, or MISS, had not previously been seen in this region. These structures are formed from mats of microbial material, much like mats seen today on stagnant waters or in coastal flats.

A rock surface is displaying "polygonal oscillation cracks" in the 3.48 billion years old Dresser Formation, Pilbara region, Western Australia. Such and similar sedimentary structures are of biological origin. They document ancient microorganisms that formed carpet-like microbial mats on the former sediment surface. The Dresser Formation records an ancient playa-like setting -- similar environments are occurring on Mars as well. The MISS constitute a novel approach to detect and to understand Earth's earliest life. (Credit: Nora Noffke)

A rock surface is displaying “polygonal oscillation cracks” in the 3.48 billion years old Dresser Formation, Pilbara region, Western Australia. Such and similar sedimentary structures are of biological origin. They document ancient microorganisms that formed carpet-like microbial mats on the former sediment surface. The Dresser Formation records an ancient playa-like setting — similar environments are occurring on Mars as well. The MISS constitute a novel approach to detect and to understand Earth’s earliest life. (Credit: Nora Noffke)

The team included Noffke, Hazen, Daniel Christian of Old Dominion University, and David Wacey of the University of Western Australia. They described various MISS preserved in the region’s Dresser Formation. Advanced chemical analyses point toward a biological origin of the material. The Dresser MISS fossils resemble strongly in form and preservation the MISS from several other younger rock samples, such as a 2.9 billion-year-old ecosystem Noffke and her colleagues found in South Africa.

“This work extends the geological record of MISS by almost 300 million years,” said Noffke, who is also a professor at ODU. “Complex mat-forming microbial communities likely existed almost 3.5 billion years ago.”

The team proposes that the sedimentary structures arose from the interactions of bacterial films with shoreline sediments from the region.

“The structures give a very clear signal on what the ancient conditions were, and what the bacteria composing the biofilms were able to do,” Noffke said.

MISS are among the targets of Mars rovers, which search for similar formations on that planet’s surface. Thus, the team’s findings could have relevance for studies of our larger Solar System as well.

Visualizing the Past: Nondestructive Imaging of Ancient Fossils

By integrating high-resolution X-ray imaging (termed microCT), 3D image segmentation, and computer animation, a new study conducted by Carole Gee at the University of Bonn, Germany, demonstrates the visualization of fossils without destroying the material. Traditional techniques, such as thin-sectioning, require investigators to physically cut up the fossil in order to observe internal structures. Dr. Gee, however, has now successfully applied microCT to visualize silicified conifer seed cones as old as 150 million years without cutting, sawing, or damaging the specimens in any way.

Well-preserved, informative plant fossils are few and far between. Specimens with reproductive organs are especially scarce but are invaluable to understanding plant evolution and ancient diversity. When such fossils are unearthed, they are lucky finds and often only single specimens are present.

“Because each specimen is precious, the main goal of this research was to study the internal structure of fossil conifer seed cones without destroying or damaging them,” explains Gee.

Using this technique, X-ray images, similar to those used in the medical field, are captured, providing virtual cross-sections of the specimen, without ever cutting into the sample. These images are then combined, producing a 3D reconstruction. This study, along with computer animations and detailed figures presenting microCT imaging, is freely available for viewing in the November issue of Applications in Plant Sciences.

This shows fossil and recent araucarian cones sectioned in 2D by microCT (A, D, G), and showing one segmented spiral or row of seeds or seed locules produced by 3D imaging (B, C, E, F, H, I). The seed spirals or rows in A, D, and G are delineated by red arrows. Yellow lines in B, C, E, F, H, and I represent the polar axis through the cones. Scale bars = 1 cm. (A–C) Fossil cone of Araucaria sp. from Wyoming (specimen no. CG066, Flynn Collection). (A) Transverse section 294/1012; diameter = ca. 6 cm. (B) Lateral view showing the 360° revolution of a single seed spiral. (C) Oblique distal view. (D–F) Fossil cone of Araucaria mirabilis from the Middle Jurassic of Argentina (specimen no. K5640, Museum für Naturkunde Chemnitz collection). (D) Transverse section 280/933; diameter = ca. 7.5 cm. (E) Lateral view showing the 180° revolution of a single seed spiral. (F) Oblique distal view. (G–I) Recent cone of Araucaria araucana from the Economic Botany Garden, University of Bonn, Germany. (G) Transverse section 469/876; diameter = ca. 17 cm. (H) Lateral view showing the vertical (nonspiral) arrangement of a row of seeds. (I) Oblique distal view. (Credit: Image credit Carole T. Gee. From Gee, C. T. 2013. Applying microCT and 3D visualization to Jurassic silicified conifer seed cones: A virtual advantage over thin-sectioning. Applications in Plant Sciences 1(11): 1300039. doi:10.3732/apps.1300039.)

This shows fossil and recent araucarian cones sectioned in 2D by microCT (A, D, G), and showing one segmented spiral or row of seeds or seed locules produced by 3D imaging (B, C, E, F, H, I). The seed spirals or rows in A, D, and G are delineated by red arrows. Yellow lines in B, C, E, F, H, and I represent the polar axis through the cones. Scale bars = 1 cm. (A–C) Fossil cone of Araucaria sp. from Wyoming (specimen no. CG066, Flynn Collection). (A) Transverse section 294/1012; diameter = ca. 6 cm. (B) Lateral view showing the 360° revolution of a single seed spiral. (C) Oblique distal view. (D–F) Fossil cone of Araucaria mirabilis from the Middle Jurassic of Argentina (specimen no. K5640, Museum für Naturkunde Chemnitz collection). (D) Transverse section 280/933; diameter = ca. 7.5 cm. (E) Lateral view showing the 180° revolution of a single seed spiral. (F) Oblique distal view. (G–I) Recent cone of Araucaria araucana from the Economic Botany Garden, University of Bonn, Germany. (G) Transverse section 469/876; diameter = ca. 17 cm. (H) Lateral view showing the vertical (nonspiral) arrangement of a row of seeds. (I) Oblique distal view. (Credit: Image credit Carole T. Gee. From Gee, C. T. 2013. Applying microCT and 3D visualization to Jurassic silicified conifer seed cones: A virtual advantage over thin-sectioning. Applications in Plant Sciences 1(11): 1300039. doi:10.3732/apps.1300039.)

In the study, Gee demonstrates how this technique allows the observation of internal features such as seeds, vascular tissue, and cone scales. Furthermore, by adding artificial color to highlight certain structures or tissues, such as a row of seeds within a cone, the natural pattern of growth was evident. As Gee observes, “It’s amazing to visualize internal structures of dinosaur-aged fossils in such great detail without cutting up the fossil or damaging them at all.”

It was then possible to identify the fossils as belonging to three distinct families: Pinaceae — the pine family, Araucariaceae — a family of coniferous trees currently found only in the Southern Hemisphere, and Cheirolepidiaceae — a now-extinct family of conifers known only from the Mesozoic.

“This tells us that 150 million years ago, the ancient forests of western North America consisted of members of these three families. The fossil cones of the Araucariaceae from Utah confirm that this family, which now grows naturally in Australasia and South America, once had a worldwide distribution,” notes Gee.

Dr. Gee hopes this study will provide researchers with an alternative to traditional techniques such as thin-sectioning, which often leave the fossil completely destroyed. She concludes, “MicroCT was very effective in showing internal structure of several types of fossil cones and worked extremely well on recent specimens. Coupled with 3D reconstruction techniques in color, microCT and image segmentation can become powerful tools in the study of fossil plants and will certainly become more commonplace in paleobotany and botany, as it allows us to visualize the internal tissues of specimens without damaging them in the least.”