The color of feathers on dinosaurs

The color of some feathers on dinosaurs and early birds has been identified for the first time, reports a paper published in Nature this week.

The research found that the theropod dinosaur Sinosauropteryx had simple bristles – precursors of feathers – in alternate orange and white rings down its tail, and that the early bird Confuciusornis had patches of white, black and orange-brown coloring. Future work will allow precise mapping of colors and patterns across the whole bird.

Mike Benton, Professor of Palaeontology at the University of Bristol, said, “Our research provides extraordinary insights into the origin of feathers. In particular, it helps to resolve a long-standing debate about the original function of feathers – whether they were used for flight, insulation, or display. We now know that feathers came before wings, so feathers did not originate as flight structures.

“We therefore suggest that feathers first arose as agents for color display and only later in their evolutionary history did they become useful for flight and insulation.”

Fossil of a theropod dinosaur Sinosauropteryx - Photo by © The Nanjing Institute

Fossil of a theropod dinosaur Sinosauropteryx – Photo by © The Nanjing Institute

The team of palaeontologists from the University of Bristol, UK, the Institute of Vertebrate Paleontology and Paleoanthropology (IVPP) in Beijing, University College Dublin and the Open University report two kinds of melanosomes found in the feathers of numerous birds and dinosaurs from the world-famous Jehol beds of NE China.

Melanosomes are colour-bearing organelles buried within the structure of feathers and hair in modern birds and mammals, giving black, grey, and rufous tones such as orange and brown. Because melanosomes are an integral part of the tough protein structure of the feather, they survive when a feather survives, even for hundreds of millions of years.

This is the first report of melanosomes found in the feathers of dinosaurs and early birds. It is also the first report of phaeomelanosomes in fossil feathers, the organelles that provide rufous and brown colors.

These discoveries confirm the substantial body of evidence that suggests birds evolved through a long line of theropod (flesh-eating) dinosaurs. It also demonstrates that the unique assemblage of characters that make a modern bird – feathers, wings, lightweight skeleton, enhanced metabolic system, enlarged brain and visual systems – evolved step-by-step over some 50 million years of dinosaur evolution, through the Jurassic and Cretaceous periods.

“These discoveries open up a whole new area of research”, said Benton, “allowing us to explore aspects of the life and behavior of dinosaurs and early birds that lived over 100 million years ago.

“Furthermore, we now know that the simplest feathers in dinosaurs such as Sinosauropteryx were only present over limited parts of its body – for example, as a crest down the midline of the back and round the tail – and so they would have had only a limited function in thermoregulation.

“Feathers are key to the success of birds and we can now dissect their evolutionary history in detail and see how each feather type – and the fine detail of feather structure – was acquired through time. This will link with current work on how the genome controls feather development.”

Note: This story has been adapted from a news release issued by the University of Bristol


The color of feathers on dinosaurs

The color of some feathers on dinosaurs and early birds has been identified for the first time, reports a paper published in Nature this week.

The research found that the theropod dinosaur Sinosauropteryx had simple bristles – precursors of feathers – in alternate orange and white rings down its tail, and that the early bird Confuciusornis had patches of white, black and orange-brown coloring. Future work will allow precise mapping of colors and patterns across the whole bird.

Mike Benton, Professor of Palaeontology at the University of Bristol, said, “Our research provides extraordinary insights into the origin of feathers. In particular, it helps to resolve a long-standing debate about the original function of feathers – whether they were used for flight, insulation, or display. We now know that feathers came before wings, so feathers did not originate as flight structures.

“We therefore suggest that feathers first arose as agents for color display and only later in their evolutionary history did they become useful for flight and insulation.”

The team of palaeontologists from the University of Bristol, UK, the Institute of Vertebrate Paleontology and Paleoanthropology (IVPP) in Beijing, University College Dublin and the Open University report two kinds of melanosomes found in the feathers of numerous birds and dinosaurs from the world-famous Jehol beds of NE China.

Melanosomes are colour-bearing organelles buried within the structure of feathers and hair in modern birds and mammals, giving black, grey, and rufous tones such as orange and brown. Because melanosomes are an integral part of the tough protein structure of the feather, they survive when a feather survives, even for hundreds of millions of years.

This is the first report of melanosomes found in the feathers of dinosaurs and early birds. It is also the first report of phaeomelanosomes in fossil feathers, the organelles that provide rufous and brown colors.

These discoveries confirm the substantial body of evidence that suggests birds evolved through a long line of theropod (flesh-eating) dinosaurs. It also demonstrates that the unique assemblage of characters that make a modern bird – feathers, wings, lightweight skeleton, enhanced metabolic system, enlarged brain and visual systems – evolved step-by-step over some 50 million years of dinosaur evolution, through the Jurassic and Cretaceous periods.

Fossil of a theropod dinosaur Sinosauropteryx - Photo by © The Nanjing Institute

Fossil of a theropod dinosaur Sinosauropteryx – Photo by © The Nanjing Institute

“These discoveries open up a whole new area of research”, said Benton, “allowing us to explore aspects of the life and behavior of dinosaurs and early birds that lived over 100 million years ago.

“Furthermore, we now know that the simplest feathers in dinosaurs such as Sinosauropteryx were only present over limited parts of its body – for example, as a crest down the midline of the back and round the tail – and so they would have had only a limited function in thermoregulation.

“Feathers are key to the success of birds and we can now dissect their evolutionary history in detail and see how each feather type – and the fine detail of feather structure – was acquired through time. This will link with current work on how the genome controls feather development.”

Note: This story has been adapted from a news release issued by the University of Bristol


Origin Of Claws Seen In Fossil 390 Million Years Old

A missing link in the evolution of the front claw of living scorpions and horseshoe crabs was identified with the discovery of a 390 million-year-old fossil by researchers at Yale and the University of Bonn, Germany.

The specimen, named Schinderhannes bartelsi, was found fossilized in slate from a quarry near Bundenbach in Germany, a site that yields spectacularly durable pyrite-preserved fossils — findings collectively known as the Hunsrück Slate. The Hunsrück Slate has previously produced some of the most valuable clues to understanding the evolution of arthropods – including early shrimp-like forms, a scorpion and sea spiders as well as the ancient arthropods trilobites.

Schinderhannes bartelsi

Schinderhannes bartelsi

“With a head like the giant Cambrian aquatic predator Anomalocaris and a body like a modern arthropod, the specimen is the only known example of this unusual creature,” said Derek Briggs, director of Yale’s Peabody Museum of Natural History and an author of the paper appearing in the journal Science.

Scientists have puzzled over the origins of the paired grasping appendages found on the heads of scorpions and horseshoe crabs. The researchers suggest that Schinderhannes gives a hint. Their appendages may be an equivalent to those found in the ancient predatory ancestor, Anomalocaris — even though creatures with those head structures were thought to have become extinct by the middle of the Cambrian Period, 100 million years before Schinderhannes lived.

The fossil’s head section has large bulbous eyes, a circular mouth opening and a pair of segmented, opposable appendages with spines projecting inward along their length. The trunk section is made up of 12 segments, each with small appendages, and a long tail spine. Between the head and trunk, there is a pair of large triangular wing-like limbs — that likely propelled the creature like a swimming penguin, according to Briggs. Unlike its ancestors from the Cambrian period, which reached three feet in length, Schinderhannes is only about 4 inches long.

This finding caps almost 20 years of study by Briggs on the Hunsrück Slate. “Sadly, the quarry from which this fabulous material comes has closed for economic reasons, so the only additional specimens that are going to appear now are items that are already in collectors’ hands and that may not have been fully prepared or realized for what they are,” said Briggs.

Other authors of the paper are Gabriele Kühl and Jes Rust at the University of Bonn, Germany. Funding for the research was from the German Science Foundation and the Humboldt Foundation.

 

A mysterious seed fern, Lepidopteris, discovered from the Upper Permian of China

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

Lepidopteris baodensis sp

Lepidopteris baodensis sp

Since Schimper erected the genus Lepidopteris in 1869, its epidermal structure of subepidermal swellings (formerly called “blisters”) had long been an unsolved mystery. Excitingly, we found subepidermal swellings not only on the lower surfaces of the ultimate rachis and midrib, but also on the lower surfaces of secondary veins. In addition, the unique epidermal structures of subepidermal swellings on the ultimate rachis, midrib and secondary veins were revealed. The epidermis of a subepidermal swelling on an ultimate rachis was composed of ordinary epidermal cells and stomatal apparatuses forming longitudinal rows and numerous groups. The epidermal cells and stomatal apparatuses in each group were set in a concentric pattern. The epidermis of a subepidermal swelling on the midrib was also composed of ordinary epidermal cells and stomatal apparatuses that formed only 30 groups, and were set in a concentric pattern. The epidermis of a subepidermal swelling on a secondary vein was composed of ordinary epidermal cells and stomatal apparatuses, forming a concentric pattern. Because, unlike the lower surface, the upper surface lacked subepidermal swellings, the difference in epidermal structures between the upper and lower surfaces is remarkable. This situation is very rare in plants.

This research was carried out by Dr. Zhang Yi, Associate Professor at the College of Paleontology, Shenyang Normal University, Mr. Zheng Shaolin, Adjunct Professor at the College of Paleontology, Shenyang Normal University, and Dr. Naugolnykh, Professor at the Geological Institute, Russian Academy of Sciences. This article was published as a cover article on Chinese Science Bulletin (Chinese Edition) 2012, 57(24) and Chinese Science Bulletin (English Edition) 2012, 57(27).

In 2004, the noted paleontologists and biostratigraphers Rong Jiayu (Academician Professor of NIGPAS) and Fang Zongjie (Professor of NIGPAS) pointed out in the book “Mass Extinction and Recovery” that the Earth experienced a mass extinction and recovery between the Late Permian and the Triassic, traced back to 260 Ma. The climate became extremely hot and arid at the end of the Permian. The mass extinction, which was the largest in Earth’s history, destroyed most terrestrial and marine ecosystems. On land, coal-forming floras, represented by Lepidodendron and Cordaites, went extinct. The Euramerican, Cathaysian, Gondwanan and Angaran floras disappeared, and a new flora, represented by Pleuromeia, flourished after the disaster. The recovery of coal-forming floras on a large scale did not begin until the Late Triassic.

Although the terrestrial and marine ecosystems of the Earth experienced their largest mass extinction in the Late Permian, the seed fern Lepidopteris became an important element of remnant vegetation and persisted through the Triassic. Thus, the study of Lepidopteris plays a very important role in understanding this mass extinction and recovery.

Which adaptations allowed Lepidopteris to survive the harsh environment? The authors believe its persistence was probably related to the subepidermal swellings, which were special tissues unique to Lepidopteris. Based on analysis of the cuticle, the lower surfaces of the ultimate rachis, midrib and secondary veins, which are related to conducting tissues, were covered with subepidermal swellings. These subepidermal swellings were probably small water storage features that absorbed water during high flows in conducting tissues and released it during low flows, like an irrigation system. In this way, Lepidopteris, a seed fern that originally needed much water to live, probably survived the hot and arid environment. Of course, subepidermal swellings are likely to have had other functions as well.

Although Lepidopteris was a typical element of the Late Permian Euramerican flora, the species L. ottonis was considered to be an index fossil for the Upper Triassic in China. As a result, the stratigraphic distribution of this very important genus in the Upper Permian of China was long neglected. The new species L. baodensis not only expands our knowledge of the biology and taxonomy of Lepidopteris and the stratigraphy of the Upper Permian of China, but also provides an opportunity to understand the relationship between Euramerican and Cathaysian floras in a paleoclimatic, paleoenvironmental and paleogeographic context.

The experimental works were accomplished in the newly established laboratory of the College of Paleontology, Shenyang Normal University, Liaoning Province, China. Specimens are housed at the College of Paleontology, Shenyang Normal University. The Baijiagou of Baode, Shanxi, China, the locality where Lepidopteris baodensis was discovered, has become an area of intense research for Chinese and foreign geologists.

Note: This story has been adapted from a news release issued by the Science in China Press

new species of raptor dinosaur Found By Students

A new species of dinosaur, a relative of the famousVelociraptor, has been discovered in Inner Mongolia by two PhD students.

The exceptionally well preserved dinosaur, named Linheraptor exquisitus, is the first near complete skeleton of its kind to be found in the Gobi desert since 1972, and will help scientists work out the appearance of other closely related dinosaur species.

linheraptor exquisitus

linheraptor exquisitus

Linheraptor is in the Dromaeosauridae family of the carnivorous theropod dinosaurs and lived during the Late Cretaceous period. In addition to Linheraptor and Velociraptor, theropod dinosaurs include charismatic meat-eaters like Tyrannosaurus rex and modern birds.

The two PhD students, Michael Pittman from UCL (University College London) and Jonah Choiniere from George Washington University (GWU), found the dinosaur sticking out of a cliff face during a field project in Inner Mongolia, China.Their research is published online today in the journal Zootaxa.

“Jonah saw a claw protruding from the cliff face. He carefully removed it and handed it to me. We went through its features silently but he wanted my identification first. I told him it was from a carnivorous dinosaur and when he agreed I’m surprised nobody in London heard us shouting,” said Michael Pittman, a PhD student in the UCL Department of Earth Sciences who was the co-discoverer of the dinosaur.

“I’ve always wanted to discover a dinosaur since I was a kid, and I’ve never given up on the idea. It was amazing that my first discovery was from a Velociraptor relative. My thesis is on the evolution and biomechanics of dinosaur tails but the carnivorous dinosaurs are my favourite and my specialty,” he added.

At approximately 2.5 metres long and 25 kilograms, the researchers believe Linheraptor would have been a fast, agile predator that preyed on small horned dinosaurs related to Triceratops. Like other dromaeosaurids, it possessed a large “killing claw” on the foot, which may have been used to capture prey. Within the Dromaeosauridae family, Linheraptor is most closely related to another recently discovered species Tsaagan mangas.

Linheraptor differs from all other dromaeosaurs because of a triangular hole in front of the eye socket called the antorbital fenestra, which is a space in the skull that sinuses would have occupied. In Linheraptor this triangular hole is divided into two cavities – one of which is particularly big.

“This is a really beautiful fossil and it documents a transitional stage in dromaeosaurid evolution,” said Dr. Xu Xing, Professor of Palaeontology at the Institute of Vertebrate Paleontology & Paleoanthropology (IVPP).

Linheraptor was found in rocks of the Wulansuhai Formation, part of a group of red sandstone rocks found in Inner Mongolia, China during a field expedition by the researchers in 2008. It is the fifth dromaeosaurid discovered in these rocks, which are famous for their preservation of uncrushed, complete skeletons.

The research was done as part of the Inner Mongolia Research project, led by Dr. Xu, which aims to better understand the Late Cretaceous ecosystem of Inner Mongolia, China which is analogous but less well-studied than the well known Late Cretaceous ecosytem of Outer Mongolia. The research was funded by the Geological Society of London, the US National Science Foundation, the Chinese National Science Foundation, and George Washington University.

Note: This story has been adapted from a news release issued by the University College London

 

Can the morphology of fossil leaves tell us how early flowering plants grew?

Fossils and their surrounding matrix can provide insights into what our world looked like millions of years ago. Fossils of angiosperms, or flowering plants (which are the most common plants today), first appear in the fossil record about 140 million years ago. Based on the material in which these fossils are deposited, it is thought that early angiosperms must have been weedy, fast-growing shrubs and herbs found in highly disturbed riparian stream channels and crevasses.

Dana Royer from Wesleyan University, Connecticut, and colleagues wanted to see if aspects of a fossil plant’s life history, such as its growth strategy, could be determined from its morphology rather than from the matrix in which it was deposited. Could this technique corroborate the idea that these ancient plants were fast-growing species? And, importantly, how common was this life history strategy for plants 100 Ma? The results of their research are published in the March issue of the American Journal of Botany(http://www.amjbot.org/cgi/content/full/97/3/438).

Scale bar = 1 cm. The specimen is from the Smithsonian Institution (USNM 222855A). - Courtesy of Dana Royer, Wesleyan University, Middletown, Conn.

Scale bar = 1 cm. The specimen is from the Smithsonian Institution (USNM 222855A). – Courtesy of Dana Royer, Wesleyan University, Middletown, Conn.

The authors first needed to assess whether aspects of leaf morphology in living plants today could accurately predict their life-history strategies. In previous research, Royer and colleagues had found that two simple measurements-petiole width and leaf area-could tell a lot about the ecophysiology of a plant. They found that the ratio of petiole width (squared) to leaf area is correlated to a leaf’s dry mass per area.

“Leaf mass per area is a measure of the density or thickness of leaves, and it is strongly linked to how quickly a plant turns over its nutrient resources,” Royer said. “Thin, cheaply built leaves (low leaf mass per area) are typically associated with plants with fast growth rates, and plants like these are usually most competitive in highly disturbed environments such as riparian corridors because their rapid growth allows them to be more opportunistic.”

The authors measured the petioles and leaf areas of 93 species of living conifers and 58 species of herbaceous angiosperms and compared the resulting leaf mass per areas to those of previously published woody angiosperms. They found that these three groups could be distinguished based on their leaf mass per areas: for a given petiole width, herbaceous herbs tended to have 43%-75% lower leaf mass per area than woody angiosperms, and conifers had 19%-58% higher leaf mass per area than woody angiosperms.

The beauty of this methodology is that leaf petiole width and leaf area are measurable in many fossil specimens. Royer stated that they then used this methodology to “estimate the leaf mass per area for some of the oldest known angiosperm leaf fossils.” They measured 179 fossil specimens representing 30 species from three Albian (110-105 Ma) sites across the United States.

“The majority of the fossils measured in our study have low leaf mass per area,” noted Royer, supporting the idea that early angiosperms were fast-growing species similar to the flora found in riparian habitats today. If a similar relationship as today is assumed, then all of the fossil angiosperm species had leaf lifespans of less than 12 months. “This means the unrivalled capacity for fast growth observed today in many angiosperms was in place by no later than the Albian (110 Ma ago).”

“While this doesn’t tell us anything directly about the earliest angiosperms-the oldest angiosperm pollen is around 140 Ma old-the Albian marks the time when angiosperms begin to be very diverse and important ecologically,” Royer concludes. “It is likely that explosive growth is one reason for the success of angiosperms.”

Note: This story has been adapted from a news release issued by the American Journal of Botany

 

Rare 95 million-year-old flying reptile Aetodactylus halli is new pterosaur genus, species

A 95 million-year-old fossilized jaw discovered in Texas has been identified as a new genus and species of flying reptile, Aetodactylus halli.

Aetodactylus halli is a pterosaur, a group of flying reptiles commonly referred to as pterodactyls.

A 95 million-year-old fossilized jaw discovered in Texas has been identified as a new genus and species of flying reptile, Aetodactylus halli, says paleontologist Timothy S. Myers, who identified and named Aetodactylus halli. The rare pterosaur -- literally winged lizard -- is also one of the youngest members of the pterosaur family Ornithocheiridae in the world. It's only the second ornithocheirid ever documented in North America, says Myers, a postdoctoral fellow at Southern Methodist University, Dallas. - Illustration by Karen Carr

A 95 million-year-old fossilized jaw discovered in Texas has been identified as a new genus and species of flying reptile, Aetodactylus halli, says paleontologist Timothy S. Myers, who identified and named Aetodactylus halli. The rare pterosaur — literally winged lizard — is also one of the youngest members of the pterosaur family Ornithocheiridae in the world. It’s only the second ornithocheirid ever documented in North America, says Myers, a postdoctoral fellow at Southern Methodist University, Dallas. – Illustration by Karen Carr

The rare pterosaur – literally a winged lizard – is also one of the youngest members in the world of the pterosaur familyOrnithocheiridae, according to paleontologist Timothy S. Myers, who identified and named Aetodactylus halli. The newly identified reptile is only the second ornithocheirid ever documented in North America, says Myers, a postdoctoral fellow in the Huffington Department of Earth Sciences at Southern Methodist University in Dallas.

Aetodactylus halli would have soared over what is now the Dallas-Fort Worth area during the Cretaceous Period when much of the Lone Star state was under water, covered by a vast ancient sea.

While rare in North America, toothed pterosaurs belonging to the Ornithocheiridae are a major component of Cretaceous pterosaur faunas elsewhere in the world, Myers says. The Texas specimen – a nearly complete mandible with most of its 54 teeth missing – is definitively younger than most other ornithocheirid specimens from Brazil, England and China, he says. It is five million years younger than the only other known North American ornithocheirid.

Myers describes the new species in the latest issue of the Journal of Vertebrate Paleontology. Go towww.smuresearch.com to see illustrations of Aetodactylus halli and the Cretaceous marine environment, an image of the fossilized jaw and links to more information.

Myers named the pterosaur Aetodactylus halli after Lance Hall, a member of the Dallas Paleontological Society who hunts fossils for a hobby. Hall found the specimen in 2006 in North Texas. It was embedded in a soft, powdery shale exposed by excavation of a hillside next to a highway. The site was near the city of Mansfield, southwest of Dallas. Hall donated the specimen to SMU.

Pterosaurs ruled the skies from the late Triassic, more than 200 million years ago, to the end of the Cretaceous, about 65 million years ago, when they went extinct. They represent the earliest vertebrates capable of flying.

Fossil hunter saw long row of teeth sockets

The Aetodactylus halli jaw was discovered in the geologic unit known as the Eagle Ford Group, which comprises sediments deposited in a shallow sea, Myers says. Outcrop of the Eagle Ford Group extends northward from southwestern Texas into southern Oklahoma and southwestern Arkansas.

“I was scanning the exposure and noticed what at first I thought was a piece of oyster shell spanning across a small erosion valley,” Hall recalls of the discovery. “Only about an inch or two was exposed. I almost passed it up thinking it was oyster, but realized it was more tan-colored like bone. I started uncovering it and realized it was the jaw to something – but I had no idea what. It was upside down and when I turned over the snout portion it was nothing but a long row of teeth sockets, which was very exciting.”

SMU vertebrate paleontologist Louis L. Jacobs, a dinosaur expert internationally recognized for his fossil discoveries in Texas and Africa, and SMU paleontologist Michael J. Polcyn, recognized for his expertise on the extinct marine reptiles called mosasaurs, both told Hall it was a pterosaur and an important find.

Unique jaw differs from others

The 38.4-centimeter Aetodactylus jaw originally contained 54 slender, pointed teeth, but only two remain in their sockets, Myers says. The lower teeth were evenly spaced and extended far back along the jaw, covering nearly three quarters of the length of the mandible. The upper and lower teeth interlaced when the jaws were closed.

In Aetodactylus, changes in tooth size along the jaw follow a similar pattern to those of other ornithocheirids. However, Aetodactylus differs from all other ornithocheirids in that its jaws were thin and delicate, with a maximum thickness not much greater than 1 centimeter, Myers says. But the specimen does compare favorably with Boreopterus, a related pterosaur from the Early Cretaceous of China, in terms of the number of teeth present in the lower jaw, he says.

Myers has estimated the wingspan around roughly 3 meters, or about 9 feet, indicating Aetodactylus would have been a “medium-sized” pterosaur, he says. While it’s not known how Aetodactylus died, at the time of death the reptile was flying over the sea and fell into the water, perhaps while fishing, Jacobs says.

Find hints at new diversity of pterosaurs

North American pterosaurs that date from the Cretaceous are all toothless, except for Aetodactylus and Coloborhynchus, Myers says. The thinness of the jaws, the upward angle of the back half of the mandible and the lack of a pronounced expansion of the jaw tips indicate that Aetodactylus is different from other ornithocheirids and represents a new genus and species of pterosaur.

“Discovery of another ornithocheirid species in Texas hints at a diversity of pterosaurs in the Cretaceous of North America that wasn’t previously realized,” Myers says. “Aetodactylus also represents one of the final occurrences of ornithocheirids prior to the Late Cretaceous transition to pterosaur faunas that were dominated by the edentulous, or toothless, species.”

Texas now claims the only two of their kind

Much of Texas was once submerged under the Western Interior Seaway. The massive sea split North America from the Gulf of Mexico to the Arctic Ocean.

On shore, the terrain was flat and flowering plants were already dominating flora communities in this part of North America, according to paleobotanist Bonnie Jacobs, associate professor of Earth Sciences at SMU.

“There were still conifers and ferns as well, but mostly of the sort that had tiny needle leaves, like junipers, says Bonnie Jacobs. “Sycamores and their relatives would have been among the flowering plants.”

The first ornithocheirid remains from North America, discovered in Fort Worth, were described by former SMU student Young-Nam Lee and donated by amateur collector Chris Wadleigh, says SMU’s Louis Jacobs.

“The ancient sea that covered Dallas provided the right conditions to preserve marine reptiles and other denizens of the deep, as well as the delicate bones of flying reptiles that fell from their flight to the water below,” says Louis Jacobs, a professor in SMU’s Huffington Department of Earth Sciences. “The rocks and fossils here record a time not well represented elsewhere in North America. That’s why two species of ornithocheirids have been found here but nowhere else, and that’s why discoveries of other new fossils are sure to be made by Lance Hall and other fossil lovers.”

Note: This story has been adapted from a news release issued by the Southern Methodist University

 

Images of 300 million old insects revealed

Writing in the journal PLoS One, the scientists have used a high resolution form of CT scanning to reconstruct two 305-million year old juvenile insects. Without the pioneering approach to imaging, these tiny insects – which are three-dimensional holes in a rock – would have been impossible to study.

By placing the fossils in a CT scanner, and taking over 3,000 X-rays from different angles, the scientists were able to create 2,000 slices showing the fossil in cross section.

Polyneoptera

Polyneoptera

From these slices the researchers created 3D digital reconstructions of the fossils. This process allows them to learn more about the lifestyle, biology and diet of the insects, one of which is similar to a modern day cockroach, and glimpse fascinating insights about how both were adapted for survival.

One of the insects reconstructed by the scientists is characterized by a large number of sharp spines. It is a new species and genus which does not exist today.

The other is an early predecessor of one of the great survivors of the insect world, the cockroach, and is one of the best preserved examples of this age ever seen by insect palaeontologists. Researchers suspect from its well preserved mouth-parts that it survived by eating rotting litter from the forest floor.

Both are members of a group called the Polyneoptera – which includes roaches, mantises, crickets, grasshoppers and earwigs. But analyzing the exact relationships of the insects will be difficult for the researchers, led by Dr Russell Garwood of the University of Manchester’s School of Materials, as insects have a habit of dramatically changing appearance as they develop.

Dr Garwood said: “The most dramatic change is seen in insects like butterflies, which change from a larva, to chrysalis, to adult. But relatively few people look to the fossils try and work out how such a life cycle may have evolved.

“We are hoping that work like this will allow us to better understand the biology and development of these early insects, and how major innovations may have come about.

“Around this time a number of early ‘amphibians’ were insectivores – they lived by eating a lot of insects. The spiney creature was a sitting duck, as it couldn’t fly, so the spines probably made it less palatable. It is bizarre – as far as we’re aware, quite unlike any members of the Polyneoptera alive today.”

“The roach nymph is much like modern day cockroaches – although it isn’t a ‘true’ cockroach, as it may well predate the split between true cockroaches and their sister group, the mantises.”

“This is very much a first step, and I’ll be spending the next few years looking at other fossil insects to build on this work.

Professor Philip Withers, co-author on the paper, added: “I am very excited by our fossil work which is providing unique information in 3D.”

Note: This story has been adapted from a news release issued by the University of Manchester

 

INDIAN OCEAN’S BREAK-UP SHOCKS US

Breaking up is hard to do. Even for Earth’s tectonic plates, separation is studded with sudden releases of pent up stress, such as the twin tremors that rocked the Indian Ocean on April 11, 2012.

The magnitude 8.7 and 8.2 earthquakes that struck off the coast of Sumatra that day herald the breakup of the Indo-Australian plate along an unclear boundary beneath the Indian Ocean southeast of India, according to two studies published online today in Nature.

boundaries of Earth’s tectonic plates near the epicenters

boundaries of Earth’s tectonic plates near the epicenters

In one of the reports, seismologists from the University of Utah and University of California, Santa Cruz, say the main shock—the combined outcries of four separate faults rupturing in a span of 160 seconds—measured 8.7 in magnitude. That’s about 40 times larger than the previous estimate of 8.6. The 8.2-magnitude quake followed along a fifth fault two hours later.

Two of the largest strike-slip earthquakes ever recorded, these earthquakes struck where the Indo-Australian plate is being torn asunder as it marches to the northeast. The trouble happens because the west of breakup region is not keeping pace with the segment to the east. The western portion of the plate is slowed by its ongoing collision with Asia, whle eastern part of the plate moves relatively unimpeded as it dives, or subducts, under the island of Sumatra.

It’s been five years since an 800-mile-long (1,300 km) section of colliding plates in Earth’s crust unzipped and unleashed a 9.3 megathrust earthquake from Sumatra to the Andaman Islands. The rupture moved a block of earth as long as California about 30 feet. At least 230,000 people perished from the quake and the tsunamis that followed. We’re remembering the disaster, as well as looking at the many lessons and discoveries been gleaned from it — lessons that should never be forgotten.

By changing stress patterns in the earth’s crust, that 2004 catastrophe probably helped to trigger the 2012 quakes, which were much less upsetting from humanity’s point of view: only ten people are known to have died as a result.

The difference? Among other reasons, the horizontal movements along the strike-slip faults out in the middle of the Indo-Australian plate simply cannot move as much water as the vertical motion along its subducting edges can. (The first April 11, 2012, quake did cause small tsunamis, but none more than 12 inches high, according to the U.S. Geological Survey.)

ANALYSIS: Earth Moved—Why No Big Tsunami?

That doesn’t mean last year’s twin strike-slip jolts were impotent. A third paper published online today in Nature reports a fivefold increase in the rate of remote earthquakes (those greater than 1,500 kilometers from the epicenter) with magnitudes of 5.5 or greater during the six days following the initial events.

RemoteQuakes
This map drives home the point. The four earthquakes of magnitude 6.0 or greater noted off western North America all occurred within the first 24 hours of the Indian Ocean events. Such a brazen cluster of tremors that size is highly unusual; the global average is one every three days.

“We’ve never seen an earthquake like this,” the University of Utah’s Keith Koper said in a press release. “This is part of the messy business of breaking up a plate….This is a geologic process. It will take millions of years to form a new plate boundary and, most likely, it will take thousands of similar large quakes for that to happen.”

IMAGES:

Map of the Indian Ocean region showing boundaries of Earth’s tectonic plates near the epicenters (red stars) of two great earthquakes that happened April 11, 2012. (Keith Koper, University of Utah Seismograph Stations)

Epicenters of four remote magnitude 6.0 or greater earthquakes (red beach balls) that occurred within 24 hours of the April 11, 2012, east Indian Ocean earthquake (black and white beach ball). (Fred Pollitz)


Geothermal energy through Wire

A proposed high voltage electrical cable running across the floor of the North Atlantic Ocean to tap Iceland’s surplus volcanic geothermal energy would become the world’s longest underwater electrical cable, if it goes ahead. The cable would be a significant step towards a pan-European super grid, which may one day tap renewable sources as far afield as Scandinavia, North Africa and the Middle East. It’s argued that such a grid would be able to widely transmit energy surpluses from active renewable sources, thereby alleviating the need for countries to use (or build) back-up fossil fuel power stations to cater for peaks in demand when more local renewable sources aren’t particularly productive.

Geothermal energy through Wire

Geothermal energy through Wire

If a European super grid comes to fruition, energy surpluses will be big business. So it’s hardly surprising that both Germany and the United Kingdom are jostling for position at the other end of the Icelandic cable, with Norway and the Netherlands also having been mooted as potential connectees. That would necessitate a cable at least 745 miles (1198 km) in length, making it easily the longest electrical cable in the world.

The scheme, first proposed in March of last year by Iceland’s largest energy producer Landsvirkjun, would aim to export five billion kilowatt-hours of energy per year for an estimated $350 to $448 million return. A feasibility study subsequently carried out has failed to find any terminal difficulties with the idea, and UK energy minister Charles Hendry is set to fly to Iceland in May to woo the relevant authorities.

An electrical link to Iceland is one of several international interconnectors either proposed or in progress in Europe, in addition to the fifteen or so routes that exist already (existing and planned connections can be seen on this map). Norway is a focal point for many of the confirmed forthcoming interconnectors which, unlike the proposed Iceland link, would see a two-way exchange of energy designed to further boost its energy security and that of its neighbors. The country is already linked via four North Sea interconnectors to Denmark, Germany, the UK, and the Netherlands—the latter being the current world record holder for longest submarine power link at 360 miles (580 km).

More ambitious are the proposed DESERTEC and Medgrid schemes to to interconnect countries and renewable energy sources on both the European and African sides of the Mediterranean Sea. German in origin, DESERTEC would involve the investment of more than $500 billion dollars by 2050, into 6500 square miles (nearly 17,000 sq km) of solar thermal collectors (plus a bit of wind) around the edge the Sahara Desert. The scheme could, it’s suggested, supply 15 percent of mainland Europe’s energy needs. Facts and figures for the French Medgrid scheme (conceptually very similar to DESERTEC) are rather more elusive, and interpretation varies as to whether the two schemes are complementary or in competition.

 

Conceptual sketch of the proposed DESERTEC energy system
Conceptual sketch of the proposed DESERTEC energy system.
the Trans-Mediterranean Renewable Energy Cooperation (TREC)

 

A problem inherent to all long-distance electrical transmission: energy loss due to the resistance of the cables. Thanks to Joule’s first law, the problem is minimized by stepping up voltage, with a ten-fold increase resulting in a 100-fold loss reduction. The Norway-Netherlands link transmits AC at 300,000 and 400,000 volts.

Even the proposed Iceland interconnector, accounting for the worst case scenario of a 930-mile (1500-km) cable, falls well within the bounds of profitability according to the findings of a 1980s study which calculated the longest cost-effective distances for electrical transmission to be 2500 miles (4000 km) for AC and 4300 miles (7000 km) for DC. Official costs are yet to be tabled for the project.

The exportation of renewable energy is a logical next step for Iceland, which has done a grand job of getting its own house in order. The country currently meets 81 percent of its energy needs with domestic renewable sources—thanks in no small part to the country’s tremendous geothermal assets, sitting as it does on the Mid-Atlantic Ridge (which can have occasional less welcome consequences). The country plans to be free of fossil fuels in the near future.