Cause of Dinosaur Boom relating to rise of Rocky mountain

The evolution of new dinosaur species may have surged due to the rise of the Rocky Mountains and the emergence of a prehistoric inner sea in North America, researchers say.

Duck-billed and horned dinosaurs flourished in North America, reaching a peak about 75 million years ago, a time known as the Campanian. For instance, one Campanian region known as the Dinosaur Park formation in what is now Canada saw seven different duck-billed dinosaur species and five horned dinosaur species emerge.

dinosaur

dinosaur

A comparable region known as the Hell Creek formation in the United States from the Maastrichtian, the time that led up to the end of the Age of Dinosaurs 65 million years ago, saw only a single duck-billed dinosaur species and maybe three horned dinosaur species at most.

“The reason for this discrepancy in dinosaur diversity has never been adequately explained,” said researcher Terry Gates, a vertebrate paleontologist at Ohio University.

Dinosaurs and geology

To help solve the mystery behind this pattern of evolution, Gates and colleagues analyzed the ancient geology of western North America, since environmental alterations often influence evolution. After focusing on trends in mountain and ocean formation 70 million to 80 million years ago, they found the landscape experienced profound changes back then that may have influenced dinosaur evolution.

During the early to middle Cretaceous, geological forces lifted the western United States, creating a huge mountain range  known as the Sevier Mountains. This extended in a line from the American southwest through Alberta, Canada. Later, one of the tectonic plates under North America’s crust shifted, building another mountain range farther east — the Laramide Orogeny, the infant stage of the modern-day Rocky Mountains.

Rocky Mountain

Rocky Mountain

The area just to the east of the new Sevier Mountains dipped downward, creating a shallow inner sea known as the Western Interior Seaway that flooded the continent from the Canadian Arctic to the Gulf of Mexico. This seaway divided the continent into three large islands to the north, east and west that were densely populated with dinosaurs.

The wild west

The dinosaurs of the west dwelled on an island called Laramidia. “Western North America has been a hotbed for dinosaur discoveries for more than a century, but the recent explosion of new dinisaur species coming out of Utah is sending waves through the paleontological community and revolutionized our understanding of dinosaur evolution on the continent,”  researcher Lindsay Zanno said in a statement. Zanno is the director of the Paleontology and Geology Research Laboratory at the Nature Research Center of the North Carolina Museum of Natural Sciences.

Specifically, the new finds helped illustrate how dinosaurs evolved on an island with changing geography. The growth of the Sevier Mountains and the Western Interior Seaway caused dinosaur habitat to shrink on Laramidia.

“It appears that geographic as well as probably also ecological barriers created by the rise of mountain ranges and the seaway caused isolation of the northern and southern populations of the crested duck-billed and horned plant-eating dinosaurs,” researcher Albert Prieto-Márquez at the Bavarian State Collection for Paleontology and Geology in Munich, Germany, said in a statement. “We hypothesize that such isolation facilitated rapid speciation and increased diversity in these animals.”

New species of duck-billed and horned dinosaurs were being born at an explosive rate of every few hundred thousand years during the brief time when the two mountain ranges and the seaway coexisted. Isolated populations often evolve new features more rapidly, Gates said.

Eventually, the continued rise of the Rocky Mountains kept the sea away from the continent’s interior. This change opened up a vast territory for these dinosaurs to roam. This, in turn, reduced how fast new species evolved in the region to every few million years, the researchers suggest.

“Our data suggests that changing geography contributed to the pattern we see in western North America,” Gates said.

During the times of isolation, a number of species of giant duck-billed dinosaurs “roamed a much smaller area than you might think given that many were larger than elephants,” Gates said. It may be possible these dinosaurs evolved to eat specialized plants found only in certain regions, explaining why they lived in relatively tight confines.

Dinosaur diversity dip

Researchers had suggested that dicosaurs were declining  before their mass extinction, due to a dip in diversity in the years leading up to the calamity.

“The major question I’ve been thinking about for 10 years was, ‘Were dinosaurs really declining before they went extinct?'” Gates told LiveScience. “It turns out the time period of dinosaur diversity we were looking at, the Campanian, was a bit of an anomaly. It saw three converging geologic structures all coming together to form perfect conditions for a dinosaur species boom. Everyone was using this time as a baseline for dinosaur diversity, when it should have been seen as an anomaly, and the decrease in diversity later on was really a return to the status quo.”

The mountain and seaway changes not only influenced dinosaur diversity in North America , but they also may have had effects elsewhere in the world. For instance, the rise of the predecessor to the Rocky Mountains created a barrier, meaning that only species living in the southern part of Laramidia could get to South America, and only species living north of the mountains could reach Asia across modern-day Alaska.

“These giant herbivores were truly invasive species that seemingly came to dominate these other continents,” Gates said.

Gates and his colleagues are now exploring the western United States to better understand patterns of dinosaur evolution and diversity there, as well as how other groups of animals, such as mammals and amphibians, might have been affected by these geological changes. They detailed their findings online  in the journal PLoS ONE August ,2012.

Story Of Prehistoric Climates From Fossil Wood

New research into a missing link in climatology shows that the Earth was not overcome by a greenhouse period when dinosaurs dominated, but experienced rapid fluctuations in temperature and sea level change that resulted in a balance of the global carbon cycle. The study is being published in the March issue of Geology.

Fossil Wood - Stock Photo From World Fossil Society

Fossil Wood – Stock Photo From World Fossil Society

“Most people think the mid-Cretaceous period was a super-greenhouse,” says Darren Gröcke, assistant professor and Director of the Stable Isotope Biogeochemistry Laboratory at McMaster University. “But in fact it was not to dissimilar to the climates over the past 5 million years.”

By using high-resolution stable-isotope analysis from 95-million-year-old fossilized wood collected from Nebraska, Gröcke and his team were able to precisely correlate the terrestrial carbon cycle with that from deep-sea records. However, when they compared the carbon curves from both records, it was evident that a chunk of about 500,000 years was missing from the terrestrial record. Other records already indicated a drop in sea level, a 2-4ºC drop in oceanic temperature and a breakdown in oceanic stratification coincident with a marine extinction event.

“Rapid, large falls in sea-level in the ancient record are typically only produced by a glaciation, and so the combination of all the data during the mid-Cretaceous period suggests a short-lived glaciation during a period generally considered to be a super-greenhouse,” says Gröcke.

“Whatever hits the water causes a ripple effect on land,” says Gröcke. “Earth often undergoes rapid temperature fluctuations, and this new information may help us to understand how the biosphere will respond to human-generated alterations of CO2 concentration.”

He said the research not only challenges conventional wisdom surrounding ancient climates, it makes a case for the use of high-resolution sampling in order to reconstruct a more accurate picture of the ancient climate and its affect on the Earth.

Funding for this study was provided in part by the Natural Science and Engineering Research Council of Canada, Canada Foundation for Innovation, and the Ontario Innovation Trust.

Debate on Dinosaur life

INTRODUCTION

Some people think dinosaurs were cold-blooded; other people think dinosaurs were warm-blooded. Lots of scientists have studied the problem. There is information about posture, bone structure, and brain/body size. This essay will consider the evidence and try to come to a reasonable conclusion.

THE BIG DEBATE

They were reptiles, so they must have been cold-blooded

In the old days, before about 1960, everybody thought dinosaurs were cold-blooded, that is, their temperature was determined by that of the external environment. Scientists thought this because they had decided that dinosaurs were reptiles, and all modern reptiles are cold-blooded. (It should be noted that the term “reptile” has fallen out of favor in the modern, cladistic view, denoting as it does a paraphyletic group; however, most people still understand what is meant by a reptile, and I will use the term throughout in its traditional sense, making no pretense that it designates a natural clade.) Alligators and crocodiles are the most closely related non-dinosaurian archosaurs, and they are cold-blooded.

Then people began to look further, and some of them decided that it was not so easy. Dinosaurs were unusual reptiles at best. They do not look like modern reptiles. They did not walk like modern reptiles. It had been suggested almost a century ago that birds were the direct descendants of dinosaurs, and they are indisputably warm-blooded; in fact, in the cladistic view, birds are dinosaurs. Maybe there was more to the story.

They held the heat because they were so big

stegosaurus

stegosaurus

Several scientists proposed the “inertial homeotherm” idea. They said a big dinosaur could keep an even body temperature just because it was so big. According to Colbert and colleagues, a medium-sized dinosaur exposed to day and night temperatures similar to those found in Florida today would take 86 hours to change its temperature by 1°C. They based their estimates on experiments with alligators tied up out in the sun. Mesozoic climates were far more equable than they are now. Clearly, by moving from sun to shade, as modern ectotherms do, a fine degree of temperature control could be achieved without invoking a high metabolism.

They might have been warm-blooded

Postural evidence

Bakker was the first scientist to come out strongly in favor of warm-blooded dinosaurs. He had several arguments. He noticed that dinosaurs all had an upright posture, instead of a sprawling one like modern reptiles. Bakker divided today’s animals into three groups, based on their stance.

Group 1 is the sprawlers. They have their bellies on the ground most of the time. This group includes salamanders, frogs, snakes, lizards, turtles, the tuatara, and monotremes.

Group 2 is the semi-erect animals. They lie down on their bellies, except when they want to go somewhere. Then they walk pretty much upright. This group includes chameleons, alligators, and crocodiles.

Group 3 is the fully erect animals. They usually stand up unless they are resting. This group includes birds, marsupials, and placental mammals.

Bakker noticed that the fully erect animals were all warm-blooded. Monotremes are warm-blooded even though they sprawl. He couldn’t prove that only warm-blooded animals could be fully erect, but it was an interesting correspondence.

Bakker said that fully erect animals spend more time moving around than sprawlers do. Lizards can raise their metabolism by moving around . Bakker proposed that the evolution of erect posture was connected to activity level and warm-bloodedness.

Monotremes are thought to be the most primitive living mammals. Their resting metabolic rate is lower than other mammals. Their body temperature is also lower than that of other mammals. Obviously, an animal can be a sprawler and still be warm-blooded. But can a cold-blooded animal maintain a fully erect posture?

Bakker’s critics say yes. They point out that upright posture is more efficient, and big animals need to stand upright to support their large weight. (Then why could Permo-Triassic rhynchosaurs and parieasaurs grow to the size of rhinos and still retain a sprawling posture?). The critics say Bakker has not proven a causal relationship between posture and body temperature. But then, it’s pretty hard to prove a causal relationship in paleontology. You can’t do any experiments on the animals you are investigating.

Bone histology

A couple of years later, some new evidence came to light. De Ricqles studied the structure of fossil and recent bones under the microscope. He noticed that the bones of modern warm-blooded animals had a lot more Haversian canals than the bones of cold-blooded ones. The cold-blooded animals’ bones also had growth rings in them, forming what he called a “lamellar-zonal” pattern. He called the warm-blooded type “fibro-lamellar” structure.

De Ricqles said that the distinction between the two types was really the effect of growth rate. Fast-growing animals have to remodel their bones more extensively than slow-growing ones. Based on the bones of living animals, he concluded that only warm-blooded ones had a high enough metabolism to support the fast growth leading to fibro-lamellar bone.

The group of diapsid reptiles called archosaurs includes the ornithischian and saurischian dinosaurs, and also pterosaurs and crocodilians. De Ricqles found fibro-lamellar bone in the first two groups. The dinosaurs he examined included carnosaurs, prosauropods, sauropods, and ornithischians. He found lamellar-zonal bone only in crocodilians. He also found evidence of fibro-lamellar bone in the advanced thecodonts ancestral to the first three groups of archosaurs, and in the advanced therapsids ancestral to mammals. Bakker and Feduccia both suggested perhaps endothermy arose as a response to the rigorous climates of the Permian southern hemisphere glaciations.

De Ricqles notes that warm-bloodedness need not denote a body temperature of 37°C. Monotremes maintain about 28° to 30°C. Marsupials and primitive placentals like hedgehogs and tenrecs have metabolic rates about 3/4 those of other placental mammals and body temperatures 3° to 5°C lower. It is also possible that the degree of warm-bloodedness varied among dinosaur groups. It has recently been suggested that some dinosaurs may have had high metabolisms and growth rates while young, slowing to become inertial homeotherms as they reached adult size.

Bouvier claims that slow-growing mammals like monotremes and bats have poorly vascularized bone. However, this does not negate the value of Haversian bone in diagnosing warm-bloodedness.

Insulation

Everyone seems to agree there is no need to insulate a cold-blooded animal. It keeps the same temperature as its environment and doesn’t care. Fossils of pterosaurs have been found with hairlike structures on the skin. Besides, scientists believe an animal must be warm-blooded to support the activity of flight. So they do not argue too much about pterosaurs having been warm-blooded.

The earliest widely acknowledged bird is called Archaeopteryx. It is from the Jurassic Period, about 140 million years ago. It had feathers, but a skeleton indistinguishable from a small dinosaur called Compsognathus. So it is a matter of semantics whether it is called the first bird or a feathered dinosaur. Recently, another, slightly younger dinosaur fossil was unearthed in China that sported a row of proto-feathers down its spine, and dinosaurs with indisputable feathers attached to the forelimbs were described in 1998. These finds have convinced scientists that the first birds evolved from small, meat-eating dinosaurs. Warm-bloodedness must have arisen in this lineage sometime prior to the appearance of Archaeopteryx, since it was insulated with feathers. Who is to say exactly how early on? Were there feathered tyrannosaurs?

Other dinosaur fossils do not bear feathers or fur. In some cases, it may be because delicate structures do not preserve well. Most fossils of mammals don’t show fur either. In other cases, skin impressions are known, and they are of a scaly, reptilian type. This doesn’t mean there can’t be smooth-skinned endotherms, though. Bakker points to hippos and elephants. They live in warm climates maybe similar to those in the Mesozoic, and don’t need fur to keep themselves warm. Aquatic mammals like whales live in cold environments and use blubber for insulation, leaving the skin smooth. There has been some suggestion recently of fat storage structures in dinosaurs. Insulation is not as important in big, warm-blooded animals as in small ones because of the difference in surface area-to-volume ratios.

Arctic and Antarctic dinosaurs

In the past decade, evidence has come to light regarding the existence of dinosaurs inside the Antarctic and Arctic circles). Fossils have been found in parts of Australia, Antarctica, and Alaska known to have experienced at least three months of annual darkness during the Cretaceous Period. Temperatures are thought to have hovered only slightly above the freezing point during the winter. The Alaskan hadrosaur herds included juveniles without much thermal inertia and probably without the capability of undertaking long migrations, yet they made it through the winter all right, possibly by hibernation. This is far from proof of warm-bloodedness in those dinosaurs, but it is suggestive.

BRAIN/BODY RELATIONSHIPS

Although it is less direct, there is another piece of evidence pertinent to the ectothermic vs. endothermic debate. This is the relationship between brain size and body size.

brain body relation of dinosaurs

brain body relation of dinosaurs

It is often said that an animal’s brain size is a function of its body size according to the allometric equation

ya = b (x )

This means that when the logarithm of brain size is plotted on the y axis, and the log of body size is plotted on the x axis, you get a straight line. Linear regression is frequently used to fit the straight line to the data.

The surface-to-volume model

Jerison said the regression lines for lower and higher vertebrates have a slope of 2/3. Surface area is a function of linear dimension squared, and volume is a function of linear dimension cubed. Jerison speculated that the reason for the 2/3 slope was because brain volume scaled as a surface area function. Jerison’s data showed similar slopes for two groups of measurements. One group was for the “higher vertebrates” (mammals and birds), while the other group covered the “lower vertebrates” (fish, amphibians, and reptiles). The two groups were separated by a tenfold difference in absolute brain size. However, in the graph he shows, Jerison admits to fitting a line with 2/3 slope into both the “higher” and “lower” vertebrate polygons, rather than performing a regression analysis on the data points.

The metabolic model

More recent authors have said that the slope of the brain/body line is 3/4 and that it reflects metabolism instead. According to this model, the reason for the tenfold difference in the absolute brain size for “higher” and “lower” vertebrates is their difference in metabolism, warm-blooded vs. cold-blooded. Resting metabolic rates for mammals are usually reported as four to ten times those of amphibians and reptiles of the same body size.

Dinosaur brain/body size

There is good data on brain size for many types of dinosaurs. However, there is not enough data over a wide enough range of body sizes to determine whether the regression line has a slope of 2/3 or 3/4. In view of the possibility that metabolism may have varied considerably among different dinosaur groups, it is perhaps unwise to attempt to construct a model to cover dinosaurs as a whole, anyway.

Our information about the sizes of dinosaur brains comes from natural and artificial casts of the brain cavities of fossils. Natural sedimentary endocasts are occasionally preserved. More commonly, fossil skulls are sectioned and cast with latex in the lab. The volume of the braincase is then determined by graphic double integration or by water immersion.

For mammals, the volume of the endocast closely reflects the volume of the brain in life. This is also taken to be the case for birds, pterosaurs, and sauropod dinosaurs, because of well-preserved surface features on the endocast. This is not the case for living reptiles. Their brains usually only fill about half the volume of the endocranial cavity. Data on theropod and ornithischian dinosaurs used in this analysis has been adjusted for this.

It is commonly said that dinosaurs had unusually small brains and must have been very stupid. Ostrom and Jerison say dinosaur brains were appropriate for reptiles once the negative allometric (scaling) relationship is taken into account. Data from dinosaurs added to the brain size/body size graph only extend the “lower vertebrate” polygon into larger body sizes without distorting its shape.

What can be gleaned from fitting a regression line to the data is a measure called the “encephalization quotient” or EQ. This is the ratio of a given dinosaur’s brain size to the value predicted by the regression line. Living crocodilians have an EQ of 1.

If, indeed, brain/body size reflects metabolism, we shoud expect those archosaurs who have EQs greater than 1 to have been the ones with the highest metabolisms. Perhaps not coincidentally, the dinosaurs with the highest EQs also had the highest speed and agility as inferred from morphological characters. The ones with EQs less than 1 might have had the lowest metabolisms.

INFERRED METABOLIC RATES OF ARCHOSAURS

Now I will try to pull all the evidence together and draw some conclusions about warm- or cold-bloodedness for various types of extinct archosaurs.

Large sauropods

This group contains the familiar Apatosaurus (brontosaurus) type forms like what is seen on the Sinclair Oil signs. They were huge dinosaurs with big bodies, long necks, and small heads. They also have the lowest EQs of any of the dinosaurs studied (.25 or less). Some say they couldn’t have eaten enough with their peglike teeth to fuel an endothermic metabolism. Others say their teeth functioned only for cropping vegetation, not chewing it up. Many dinosaurs used gizzard stones to grind up their food, like birds do. Such gastroliths are sometimes found inside the rib cage of fossil skeletons. Therefore, I do not believe the weak teeth argument holds much water. However, I do think the evidence for warm-bloodedness is unconvincing for the large sauropods. My guess is that they were inertial homeotherms.

Large ornithischians

This group contains the ankylosaurs, stegosaurs, ceratopsians, and ornithopods. Based on low EQs and locomotor information, I consider the stegosaurs and ankylosaurs (EQs between .5 and 1.0) to have been good candidates for inertial homeothermy as well.

Ceratopsians and ornithopods have EQs from 0.6 to 1.5. These dinosaurs had highly developed shearing and grinding teeth, like might be useful for dinosaurs who needed to fuel a higher metabolism. This group includes the Arctic hadrosaurs. Although the evidence is somewhat equivocal, my guess is that some of this group of dinosaurs were at least rudimentary endotherms. Horner’s suggestion of a high metabolism for hadrosaurs when young, decreasing to inertial homeothermy as ontogeny progressed, is appealing.

Pterosaurs

Since pterosaurs were furry and capable of sustained flight, there is no question in my mind but what they were warm-blooded. Their EQs plot right around 1, indicating that this is probably the lower limit for a warm-blooded animal.

Theropods

This group includes the large carnosaurs and the smaller coelurosaurs. They all have EQs greater than 1, and in some cases (Archaeopteryx), above those enclosed by the reptilian polygon. Oviraptor and Stenonychosaurus have EQs well within the bird range. They were the most agile and active dinosaurs. Theirs is the lineage which gave rise to birds. I consider it unequivocal that advanced coelurosaurs were endotherms. Possibly all theropods were.

Birds as archosaurs

Hopefully I will not ruffle any feathers by declaring birds to be warm-blooded. Their high metabolism was bequeathed to them by their dinosaurian ancestors. Endothermy and insulation may have been the decisive factors in their escaping the wave of Late Cretaceous extinctions when their cousins could not. Dingus and Rowe, in their book The Mistaken Extinction, state that birds are “card-carrying, avialian, maniraptoran, coelurosaurian, tetanurine, theropod, saurischian dinosaurs, and don’t you forget it!” They would include birds with other dinosaurs in a cladistic classification which uses groups of hierarchical rank that do not conform to the traditional Linnaean system of Class, Order, etc. However you want to look at it, the conclusion is inescapable that dinosaurs didn’t really become extinct at the end of the Cretaceous; only the large ones did. That’s comforting news for those of us who have been dinophiles since our preschool years.

CONCLUSIONS

Indisputable evidence does not exist for warm-bloodedness in all types of dinosaurs. However, it is highly unlikely that all dinosaurs were cold-blooded, either. Morphological and postural evidence, bone histology, ecological information, and brain/body size relationships indicate that we cannot make sweeping generalizations about dinosaurian metabolism. Most likely it varied between groups. Dinosaurs spanned the spectrum from inertial homeotherms to active, endothermic birds.

Courtesy: Essay By Lynne M Clos in Fossilnews.com

 

The Origin and Initial Rise of Pelagic Cephalopods in the Ordovician

During the Ordovician the global diversity increased dramatically at family, genus and species levels. Partially the diversification is explained by an increased nutrient, and phytoplankton availability in the open water. Cephalopods areamong the top predators of todays open oceans. Their Ordovician occurrences, diversity evolution and abundance patternpotentially provides information on the evolution of the pelagic food chain.

Methodology/Principal Findings: reconstructed the cephalopod departure fromoriginally exclusively neritic habitats into the pelagic zone by the compilation of occurrence data in offshore paleoenvironments from the Paleobiology Database, and fromown data, by evidence of the functional morphology, and the taphonomy of selected cephalopod faunas. The occurrence data show, that cephalopod associations in offshore depositional settings and black shales are characterized by a specific composition, often dominated by orthocerids and lituitids. The siphuncle and conch form of these cephalopods indicate a dominant lifestyle as pelagic, vertical migrants. The frequency distribution of conch sizes and the pattern of epibionts indicate an autochthonous origin of the majority of orthocerid and lituitid shells. The consistent concentration of these cephalopods in deep subtidal sediments, starting from the middle Tremadocian indicates the occupation of the pelagic zone early in the Early Ordovician and a subsequent diversification which peaked during the Darriwilian.

Conclusions/Significance: The exploitation of the pelagic realm started synchronously in several independent invertebrate clades during the latest Cambrian to Middle Ordovician. The initial rise and diversification of pelagic cephalopods during the Early and Middle Ordovician indicates the establishment of a pelagic food chain sustainable enough for the development of a diverse fauna of large predators. The earliest pelagic cephalopods were slowly swimming vertical migrants. The appearance and early diversification of pelagic cephalopods is interpreted as a consequence of the increased food availability in the open water since the latest Cambrian.

Bjo¨ rn Kro¨ ger1*, Thomas Servais2, Yunbai Zhang3
1 Museum fu¨ r Naturkunde, Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, Berlin, Germany,

2 Universite´ de Lille 1, UMR 8157 du CNRS Ge´osyste´mes, Villeneuve d’ Ascq, France,

3 Nanjing Institute of Geology and Paleontology, Nanjing, China

Ocean Floor Sediments May Be Window on World’s Warmer Future

Analysis of seafloor sediment reveals lower oxygen levels in the ocean when the planet heated up 55.9 million years ago

Digging into our planet’s past could help us prepare for a hot future. One dramatic spike in historical temperatures, the Paleocene–Eocene Thermal Maximum (PETM), occurred around 55.9 million years ago. That time was marked by changes in ocean productivity, the water cycle, ocean acidification and land animal migrations. Now a new study by researchers in the U.K. confirms the ocean held less dissolved oxygen.

ocean floor sediments

ocean floor

Similarly, low oxygen zones caused by modern climate change threaten marine life and humans who depend on the ocean for food. Deoxygenated zones in the North Pacific and tropical oceans have expanded in the last 50 years, according to a 2009 review from researchers in Europe and the U.S.

To peek into ancient climate for a possible clue to our future, Alex Dickson, a paleoceanographer, and his colleagues at The Open University in England analyzed sediment samples gathered by the Integrated Ocean Drilling Program, an ongoing international marine research project. The sediment cores were pulled from the Lomonosov Ridge in the Arctic Ocean. The team estimated the extent of low-oxygen seawater in global oceans by measuring the ratio of molybdenum isotopes in the sediment samples. The ratios “imply a small but significantly higher level of low-oxygen marine environments compared with the present day,” the team wrote in the July issue of Geology.

The marine sediment the researchers analyzed is “black, gritty” and sulfur-rich, oxygen poor. The proportion of oxygen-rich and oxygen-poor seafloor sediments regulates the balance of molybdenum isotopes. In well-oxygenated environments, light molybdenum isotopes adhere to the surface of manganese oxides, Dickson explains. But that process, called adsorption, happens slowly. A single molybdenum atom can hang around in the ocean for several hundreds of thousands of years on average before it is adsorbed. In low-oxygen but high-sulfide marine sediments, however, all molybdenum isotopes are taken up quickly, regardless of weight. As a result, sulfur-rich, oxygen-poor sediments reflect the composition of molybdenum isotopes in seawater during the time the sediment was deposited. Once the seawater ratio has been estimated, it gives researchers a way to calculate the extent of differently oxygenated regions in the ancient ocean.

An intriguing secondary finding is a number of samples with isotope ratios outside the range typically observed. The extremely low values may reflect a period of hydrothermal volcanism, Dickson speculates, or unusual chemical conditions such as an altered seawater pH. The team would need to analyze other isotope signatures to find the answer. Dickson also hopes to analyze other sediment samples similar to the one studied. Drifting ice floes make drilling in the Arctic Ocean tricky, and the core the team analyzed was missing a section near the onset of the PETM.

Tim Lyons, a biogeochemistry professor at the University of California, Riverside, commends the researchers for the study’s thoroughness and calls it one of the first studies to experimentally validate the idea that warming during the PETM led to low oxygen levels in the ocean. Lyons, who was not involved in the study, specifies that the study does not prove that low oxygen levels were causing massive marine organism death, but it does indicate something in the ocean environment was “potentially quite different. And the missing part of the record could be even more dramatic.” (Lyons co-wrote a commentary on the team’s work.)

The findings are important in the face of today’s changing climate, Lyons says. “We hope it resonates,” he adds, “this kind of broad-scale phenomenon could potentially have a big effect on the ocean and our relationship with the ocean.”

Ancient fossils reveal how the mollusc got its teeth

The radula sounds like something from a horror movie — a conveyor belt lined with hundreds of rows of interlocking teeth. In fact, radulas are found in the mouths of most molluscs, from the giant squid to the garden snail. Now, a “prototype” radula found in 500-million-year-old fossils studied by University of Toronto graduate student Martin Smith, shows that the earliest radula was not a flesh-rasping terror, but a tool for humbly scooping food from the muddy sea floor.

Odontogriphus

Odontogriphus

The Cambrian animalsOdontogriphus and Wiwaxia might not have been much to look at — the former a naked slug, the latter a creeping bottom-dweller covered with spines and scales. Despite the hundreds of fossil specimens collected from the Canadian Rockies by the Royal Ontario Museum, scientists could not agree whether they represented early molluscs, relatives of the earthworm, or an evolutionary dead-end. Smith, a PhD candidate in U of T’s Department of Ecology and Evolutionary Biology and author of a study published this week in Proceedings of the Royal Society B, employed a new, non-destructive type of Electron Microscopy to reveal the new details.

mouth parts

mouth parts

“I put the fossils in the microscope, and the mouth parts just leaped out,” says Smith, a PhD candidate in U of T’s Department of Ecology and Evolutionary Biology. “You could see details you’d never guess were there if you just had a normal microscope.”

After examining some 300 fossils, Smith was able not just to reconstruct the mouthparts, but work out how they grew. “The fossils are squashed completely flat, which makes them really hard to reconstruct in 3D,” says Smith. “I surrounded myself with micrographs of the mouth parts and lumps of plasticine, and spent weeks trying to come up with a model that made sense of the fossils.”

The new observations demonstrated that the mouthparts consisted of two to three rows of 17 similarly-shaped teeth, with a symmetrical central tooth and smaller teeth on the edges. The teeth would have moved round the end of a tongue in the conveyor-belt fashion seen in molluscs today, scooping food — algae or detritus — from the muddy sea floor. By establishing how the teeth were arranged, moved, grew, and were replaced, Smith was able to demonstrate that they formed a shorter and squatter forerunner to the modern radula.

“When I set out, I just hoped to be a bit closer to knowing what these mysterious fossils were,” says Smith. “Now, with this picture of the earliest radula, we are one step closer to understanding where the molluscs came from and how they became so successful today.”

Protection of Fossil Site By World Fossil Society

CHENNAI: A writ plea has been made in the Madras High Court to declare Kolakkanatham fossil site in Ariyalur district as a paleontological heritage site.

A vacation bench comprising Justices S Rajeswaran and KBK Vasuki, before which the public interest writ petition from Rajashree of Kalamassery in Kerala came up for hearing on Wednesday, ordered notice to the Union Ministry of Mines, State Forest department, Geological Survey of India and the Ariyalur District� Collector, returnable by� June 15.

According to the petitioner,� the Kolakkanatham fossil site was the only one of its kind in South India.� It had valuable landscape and it was a rare treasure house of paleontology, which generated scientific interest and was visited by research scholars from all over the world.

The Cauvery basin extended along the eastern coast of India, bounded by 08-12 degree north latitude and 78-80 east longitude.� It was formed as a result of Gondwanaland fragmentation during the drifting of Indian-Sri Lankan landmass system away from Antartica/Australia plate in the jurassic/early cretaceous period.� The abundant mineral resources and fossil remnants in this place were ample proof for the transgressions and regressions of the sea and the topographical changes occurred in the basin in early and late cretaceous period (before 65 million years ago).� There was proof of the existence of lives and their extinction due to the interference of various factors.

While so, the forest department was taking steps� to convert the site as forest area and dumping waste materials.� The proposal would change the landscape and gradually permit the land grabbers to intrude into the fossil site. Ultimately, it would result in the loss of a big treasure of fossils and close down one of the world’s richest fossil collections, the petitioner contended.

Green River Formation

Historical Background

In 1856 Dr. John Evans collected the first fossil fish known to science from the Green River Formation. The Knightia eocaena was described by Dr. Joseph Leidy in Philadelphia. Although fossils had been reported from the area, this was the first described. And so begins the story of one of the greatest fossil sites known to science.

Soon after, geologists, railroad workers, and others started reporting fossil sites in surrounding areas. Most of the fish collected were sent to Edward Drinker Cope, who did the majority of the work on the fish fauna of what became known as the Green River Formation. Cope travelled west and did some collecting of his own, and in 1871, published a major work on the fishes.

The Green River Formation outcrops in the states of Wyoming, Utah and Colorado and showcases the remains of a large lake system. Scientists have determined that the system was made up of three lakes that varied in size and depth through time. The system existed for just over twenty million years, forming about sixty million years ago and disappearing around the end of the Eocene.

The formation preserves the remains of a subtropical environment. The extremely fine-grained sediments produced beautiful fossils that grace the collections of museums around the world. They also grace the collections of many amateurs, the fish being for sale in almost every rock shop in the country, many museum shops and every souvenir shop in the Midwest. The formation has produced over a million specimens with over one half million in the last thirty years alone.

The Lakes

Fossil Lake was the deepest of the three lakes in the system. It had a small surface area and was short-lived. Fossil Lake produces the largest share of fish specimens of the three lakes.

green river formation area

green river formation area

Lake Gosiute produced a smaller variety of fossil fishes and a different state of preservation as well. It outcrops near the Fontenelle Reservoir and near the Farson Dam. The shales and fossils are not the typical Green River specimens most of us are familiar with.

Lake Uinta was the largest in surface area but was the shallowest. In existence for 17 million years, it was the longest-lived of the three lakes. Its sediments form one of the thickest lacustrine sediments known, almost 7000 feet in some places.

 The FishWhile the formation preserves over twenty species of fish, five constitute over 98% of collected specimens. We will confine our discussion to common types.KnightiaThis is probably one of the most common fossils in the world. [Editor’s note: I read recently that it is indeed the most common vertebrate fossil thus known.] The sheer numbers boggle the imagination. In 1978 alone, over 20,000 were collected. You can find them for sale at any place that offers natural history items.

knightia

knightia

Two species are known with K. eocaena being the most common. A member of the herring family, they average five inches in length with a maximum size of ten inches. They have a deeply forked tail and a single dorsal fin in front of the mid-body line. Knightia fed on algae, ostracods and insects and they were the major food source for many of the larger fish from the lakes. They were schooling fish and are frequently found in mass mortality or “death” layers. Fossils have been found packed as densely as several hundred fish per square meter of slab rock.

Mioplosus

Cope described two species of this perch-like fish, however, present-day researchers doubt the existence of M. sauvagenus. With the only specimen found having been lost, no further study is possible. M . labracoides is a fairly common predator easily distinguished by the two dorsal fins, large fan-shaped tail and an anal fin equal and opposite its second dorsal fin. A voracious predator, Mioplosus is the fish most commonly found eating other fish, something for which the Green River fish fossils are famous.

Diplomystus

Diplomystus

Diplomystus

The upturned mouth of this herring type fish indicates that it was probably a surface feeder. They have a wide anal fin, single dorsal fin, and a deeply forked tail. The maximum size is listed at twenty-six inches, but they are more commonly three to six inches. D. dentatus is also known from the Cretaceous of South America. When Cope originally erected the genus, he listed four species, however, more recent research has pared it down to D. dentatus only. Another Knightia predator, “Diplos” have been found containing fossils of their last meals.

Priscacara

piscaea

piscaea

Priscacara has grinding-type teeth, indicating that it probably fed on snails and crustaceans. It is easily identified by its stout dorsal and anal fin spines, which, in my opinion, make it the most attractive of the Green River fossils. Two species, P. serrata and P. liops, are the most common. Several others are under review by current researchers. Priscacara are known only from the Eocene. They have a large oval body and range in size from one inch to fifteen inches with four to six most common. They were schooling fishes and are more commonly found in the eighteen-inch layer.

Phareodous

The largest of the common fishes is Phareodus. Two species, P. encaustus and P. testis, are known. They average fifteen inches, with a maximum of thirty inches. With the dorsal and anal fins located at the very back of the body, these fish cannot be confused with any other Green River species. They have large very sharp teeth and have been found with the remains of Mioplosus and Priscacara inside.

Courtesy: Tom Caggiano

Dinosaur Deaths Outsourced to India?

A series of monumental volcanic eruptions in India may have killed the dinosaurs 65 million years ago, not a meteor impact in the Gulf of Mexico. The eruptions, which created the gigantic Deccan Traps lava beds of India, are now the prime suspect in the most famous and persistent paleontological murder mystery, say scientists who have conducted a slew of new investigations honing down eruption timing.

“It’s the first time we can directly link the main phase of the Deccan Traps to the mass extinction,” said Princeton University paleontologist Gerta Keller. The main phase of the Deccan eruptions spewed 80 percent of the lava which spread out for hundreds of miles.

deccan trap area

deccan trap area

It is calculated to have released ten times more climate altering gases into the atmosphere than the nearly concurrent Chicxulub meteor impact, according to volcanologist Vincent Courtillot from the Physique du Globe de Paris.

Keller’s crucial link between the eruption and the mass extinction comes in the form of microscopic marine fossils that are known to have evolved immediately after the mysterious mass extinction event. The same telltale fossilized planktonic foraminifera were found at Rajahmundry near the Bay of Bengal, about 1000 kilometers from the center of the Deccan Traps near Mumbai. At Rajahmundry there are two lava “traps” containing four layers of lava each. Between the traps are about nine meters of marine sediments. Those sediments just above the lower trap, which was the mammoth main phase, contain the incriminating microfossils.

Keller and her collaborator Thierry Adatte from the University of Neuchatel, Switzerland, are scheduled to present the new findings on Tuesday, 30 October, at the annual meeting of the Geological Society of America in Denver. They will also display a poster on the matter at the meeting on Wednesday, 31 October.

 Previous work had first narrowed the Deccan eruption timing to within 800,000 years of the extinction event using paleomagnetic signatures of Earth’s changing magnetic field frozen in minerals that crystallized from the cooling lava. Then radiometric dating of argon and potassium isotopes in minerals narrowed the age to within 300,000 years of the 65-million-year-old Cretaceous-Tertiary (a.k.a. Cretaceous-Paleogene) boundary, sometimes called the K-T boundary.The microfossils are far more specific, however, because they demonstrate directly that the biggest phase of the eruption ended right when the aftermath of the mass extinction event began. That sort of clear-cut timing has been a lot tougher to pin down with Chicxulub-related sediments, which predate the mass extinction.”Our results are consistent and mutually supportive with a number of new studies, including Chenet, Courtillot and others (in press) and Jay and Widdowson (in press), that reveal a very short time for the main Deccan eruptions at or near the K-T boundary and the massive carbon dioxide and sulfur dioxide output of each major eruption that dwarfs the output of Chicxulub,” explained Keller. “Our K-T age control combined with these results strongly points to Deccan volcanism as the likely leading contender in the K-T mass extinction.” Keller’s study was funded by the National Science Foundation.The Deccan Traps also provide an answer to a question on which Chicxulub was silent: Why did it take about 300,000 years for marine species to recover from the extinction event? The solution is in the upper, later Deccan Traps eruptions.

“It’s been an enigma,” Keller said. “The very last one was Early Danian, 280,000 years after the mass extinction, which coincides with the delayed recovery.”

Keller and her colleagues are planning to explore the onset of the main phase of Deccan volcanism, that is, the rocks directly beneath the main phase lavas at Rajahmundry. That will require drilling into the Rajahmundry Traps, a project now slated for December-January 2007/2008.

Courtesy: a news release issued by the Geological Society of America 2007

Dinosaurian Soft Tissues Interpreted as Bacterial Biofilms

A scanning electron microscope survey was initiated to determine if the previously reported findings of “dinosaurian soft tissues” could be identified in situ within the bones. The results obtained allowed a reinterpretation of the formation and preservation of several types of these “tissues” and their content. Mineralized and non-mineralized coatings were found extensively in the porous trabecular bone of a variety of dinosaur and mammal species across time. They represent bacterial biofilms common throughout nature. Biofilms form endocasts and once dissolved out of the bone, mimic real blood vessels and osteocytes. Bridged trails observed in biofilms indicate that a previously viscous film was populated with swimming bacteria. Carbon dating of the film points to its relatively modern origin. A comparison of infrared spectra of modern biofilms with modern collagen and fossil bone coatings suggests that modern biofilms share a closer molecular make-up than modern collagen to the coatings from fossil bones. Blood cell size iron-oxygen spheres found in the vessels were identified as an oxidized form of formerly pyritic framboids. observations appeal to a more conservative explanation for the structures found preserved in fossil bone.

PLoS collections: Thomas G. Kaye1*, Gary Gaugler2, Zbigniew Sawlowicz3

1 Department of Paleontology, Burke Museum of Natural History, Seattle, Washington, United States of America,

2 Microtechnics Inc., Granite Bay, California, United States of America,

3 Department of Geology, Jagiellonian University, Krakow, Poland