Friday, October 30, 2015

[Geology2] Dinos, Early Mammals News 10.30.2015



It's a Tyrannosaur-eat-Tyrannosaur world

Date:
October 29, 2015
Source:
Geological Society of America
Summary:
A nasty little 66-million-year-old family secret has been leaked by a recently unearthed tyrannosaur bone. The bone has peculiar teeth marks that strongly suggest it was gnawed by another tyrannosaur. The find could be some of the best evidence yet that tyrannosaurs were not shy about eating their own kind.

This is a recently unearthed tyrannosaur bone with peculiar teeth marks that strongly suggest it was gnawed by another tyrannosaur.
Credit: Photos by Matthew McLain.

A nasty little 66-million-year-old family secret has been leaked by a recently unearthed tyrannosaur bone. The bone has peculiar teeth marks that strongly suggest it was gnawed by another tyrannosaur. The find could be some of the best evidence yet that tyrannosaurs were not shy about eating their own kind.

"We were out in Wyoming digging up dinosaurs in the Lance Formation," said paleontologist Matthew McLain of Loma Linda University in California. "Someone found a tyrannosaur bone that was broken at both ends. It was covered in grooves. They were very deep grooves."

The grooves were clearly those of an animal pulling the flesh off the bone -- pulling in a direction perpendicular to the bone, in the same way humans eat a piece of fried chicken. But one groove stood out. It was located at the larger end of the bone and contained smaller parallel grooves caused by the diner's head turning, so that the serrated edges of its teeth dragged across the bone.

Serrated teeth rule out crocodiles and point directly to a theropod dinosaur like T. rex. The fact that the only large theropods found in the Lance Formation are two tyrannosaurs --Tyrannosaurus rex or Nanotyrannus lancensis -- eliminates all interpretations but cannibalism, explained McLain, who will be presenting the discovery on 1 Nov. at the annual meeting of the Geological Society of America in Baltimore.

"This has to be a tyrannosaur," said McLain. "There's just nothing else that has such big teeth."

The direction of the grooves is consistent with getting flesh from bones off an animal that was quite dead at the time. The bones don't reveal whether the cannibal was scavenging or was also the killer of the tyrannosaur.

"Exactly who did the eating that day, in the Late Cretaceous, could still be sorted out by the same grooves," McLain said.

The serration grooves are a valuable clue to the size of the animal who owned the teeth. Previous work using Komodo dragon teeth has demonstrated the relationship between serration sizes and the size of the animal. This approach has been used on tyrannosaurs, and McLain thinks it will work in this case, too.

"It only works if you know what species it is," he said. "And since tyrannosauruses are the only large predators in these formations, it's pretty straightforward."

Even without knowing the size of the eater, it may be easy to say which species of tyrannosaur was eating, because, according to McLain, many paleontologists believe Nanotyrannus were really juvenile T. rex.


Story Source:

The above post is reprinted from materials provided by Geological Society of America. Note: Materials may be edited for content and length.



Geological Society of America. "It's a Tyrannosaur-eat-Tyrannosaur world." ScienceDaily. ScienceDaily, 29 October 2015. <www.sciencedaily.com/releases/2015/10/151029134652.htm>.

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300 million-year-old 'supershark' fossils found in Texas

Date:
October 29, 2015
Source:
Society of Vertebrate Paleontology
Summary:
Even before the age of dinosaurs, big toothy predators were roaming Texas. 300 million years ago, during a time called the Carboniferous, the area surrounding what is now Dallas, Texas was flooded by a shallow sea. Fossils from this ancient environment were recently recovered from Jacksboro, Texas. Among these were two fossil braincases from massive extinct relatives of modern-day sharks.

Previously, giant sharks had only been recovered from rock dating back 130 million years, during the age of the dinosaurs. The largest shark that ever lived, commonly called "Megalodon," is much younger, with an oldest occurrence at about 15 million years ago. This means the new fossils from Texas indicate giant sharks go much further back into the fossil record.

After the generous donation of these fossils and careful study with Dr. John Maisey of the American Museum of Natural History in New York, the team was able to estimate how big the entire sharks would have been by comparison with smaller and more complete fossils of closely related sharks. The results were very impressive.

The size range estimated for these two Texas 'supersharks' was between 18 and 26 feet in length (5.5 to 8 meters). The largest of these specimens was 25% bigger than today's largest predatory shark, the Great White. Although not nearly as large as Megalodon, which might have reached up to 67 feet in length (about 20 meters), the fossil sharks from Texas would have been by far the biggest sharks in the sea.

These fossil braincases may belong to an extinct species of shark called Glikmanius occidentalis, or they may represent a new and larger related species that is new to science. Closely related sharks are known from as far off as Scotland, showing this group of sharks was capable of dispersing across great distances.

Maisey, McKinzie, and Williams timed their research results very well, being able to present their Texas 'supershark' at the annual meeting for the Society of Vertebrate Paleontology in Dallas, Texas. According to Maisey, even 300 million years ago, "everything is bigger in Texas!"


Story Source:

The above post is reprinted from materials provided by Society of Vertebrate Paleontology. Note: Materials may be edited for content and length.


Society of Vertebrate Paleontology. "300 million-year-old 'supershark' fossils found in Texas." ScienceDaily. ScienceDaily, 29 October 2015. <www.sciencedaily.com/releases/2015/10/151029112238.htm>.

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Transitional species of duckbilled dinosaurs illuminate relationship between evolution and growth

Date:
October 29, 2015
Source:
Society of Vertebrate Paleontology
Summary:
The discovery of two new transitional species is helping reveal the pattern of evolution in duckbilled dinosaurs, providing key insight into the intricate relationship between changes during growth and the evolution of elaborate display structures.

An emergent field of research in dinosaur paleobiology investigates the relative importance of linear, non-branching evolution (anagenesis) compared with branching evolution (cladogenesis). Increasingly, paleontologists are discovering that many dinosaur species are arranged into anagenetic lineages of rapidly evolving "transitional" species which do not overlap in time. These transitional species usually differ only slightly from their forebears, typically in the shape and size of display structures such as horns or crests.

At the SVP 2015 annual meeting, Dr Elizabeth Freedman Fowler of the Museum of the Rockies, and Great Plains Dinosaur Museum, Montana, presented on two new transitional species of duckbilled (hadrosaurid) dinosaurs from the Upper Cretaceous Judith River Formation of northern Montana.

"This particular part of the Judith River Formation is important because it yields a dinosaur fauna that is intermediate in age between an older fauna from the Two Medicine Formation of western Montana, and a younger fauna from the famous Oldman and Dinosaur Park Formations of Alberta." Dr Freedman Fowler continued, "because the formation is intermediate in age, then it is exactly where we might expect to find new, intermediate kinds of dinosaur."

The first new dinosaur described by Dr. Freedman Fowler is a transitional form of Brachylophosaurus, a large hadrosaurid with a broad paddle shaped crest over the back of its head. The second, a transitional Gryposaurus hadrosaurid, has an arched nasal crest on its snout, and is known from a bonebed of at least 10 individuals, ranging from juvenile to adult.

"The Gryposaurus bonebed is a fantastic site because the different growth stages show us that as Gryposaurus grew, the arch on its nose gets larger and moves backward, so that the nose of a one year old looks very different from the nose of a three year old," Dr. Freedman Fowler explained, "the most interesting thing is that we see the same morphological trend through time as Gryposaurus evolves. The preceding species from the Two Medicine Formation has a low crest over the middle of the nose, whereas in the succeeding species the crest is taller and more retracted towards the eyes"

This suggests that successive generations of Gryposaurus grew larger crests by changing the timing or pace of crest development during growth. Fragmentary juveniles of the transitional Brachylophosaurus species suggest that this same process is also occurring in that lineage. Changing of timing or rate of development is called heterochrony, a process which is being increasingly recognized as a major driving force in evolution.

"Heterochrony is key to understanding how evolution actually occurs in these dinosaurs, but to study heterochrony we need large collections of dinosaurs with multiple growth stages, and a really precise time framework for the rock formations that we collect them from" said Dr. Freedman Fowler.

This kind of research has only really become possible with recent technical advances in the radiometric dating of rocks, coupled with increased intensity of fossil collecting in North America.

"The Late Cretaceous of western North America is the only place in the world where we can do these kinds of intense paleobiological studies on dinosaurs. Nowhere else combines the precise dating of rocks coupled with an exceptional fossil record that has been so extensively collected."

Dr. Freedman Fowler predicts that many more transitional species remain to be discovered; "We've been collecting dinosaurs in this region for over a century, yet there are still exciting discoveries being made every year."


Story Source:

The above post is reprinted from materials provided by Society of Vertebrate Paleontology. Note: Materials may be edited for content and length.



Society of Vertebrate Paleontology. "Transitional species of duckbilled dinosaurs illuminate relationship between evolution and growth." ScienceDaily. ScienceDaily, 29 October 2015. <www.sciencedaily.com/releases/2015/10/151029112232.htm>.

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Mammal body-size responds to climate change in ancient Wyoming

Date:
October 29, 2015
Source:
Society of Vertebrate Paleontology
Summary:
Evidence from fossils suggests that multiple global warming events, which occurred over 50 million years ago, impacted the evolution of mammals living in ancient Wyoming. Using over seven thousand fossilized teeth, paleontologists found a reduction in body size of mammal populations, hypothesized to be related to warming events. This work provides a unique glimpse at the long-term impact of climatic change on mammal populations.

To unravel the link between past climates and animal faunas requires an exceptional fossil record. Chew, an associate professor at Western University of Health Sciences, California, used fossils from the Bighorn Basin of Wyoming, a nearly complete record of around 5 million years of mammalian evolution, to study responses of mammal communities through time. "The Bighorn Basin fossil record, particularly from this part of the basin, is one of the best early Cenozoic terrestrial records in the world." remarks Chew. "My colleagues have been assembling the fossil samples on which this work is based for more than 30 years. Their efforts have produced a superb, highly resolved, thoroughly studied record that is unparalleled. This record allows us to examine more sophisticated questions about faunal response to climate and environmental change than was previously possible."

Information on past climate in the Bighorn basin comes from the structure of carbon atoms, known as isotopes, preserved in the rock. This technique revealed three global warming events. The first occurred 55 million years ago, and has been previously linked to decreasing body-size. However, data from the next two events, occurring two million years later, is required to test if this forms part of a larger evolutionary pattern. "No other terrestrial record exists with the density of fossils necessary to test faunal response to the later hyperthermals [climatic warming]. The central Bighorn Basin record essentially documents a set of repeated, natural experiments in climate warming." Chew explains.

Chew examined the size of over 7500 fossil teeth from over one hundred types of mammals, and compared them before, during and after the climatic warming events. On average, the Bighorn Basin teeth were 10-20% smaller during the warm periods. Some lineages of mammals became smaller themselves, in a process known as dwarfing. However, mostly size change was driven by an increase in the abundance of small species relative to large ones in the basin during warm periods.

These findings add to the increasing evidence for the strong link between climatic change and animal populations. "The ability to compare faunal response between events is critical for establishing mechanisms of change and predicting the consequences of future warming."


Story Source:

The above post is reprinted from materials provided by Society of Vertebrate Paleontology. Note: Materials may be edited for content and length.


Society of Vertebrate Paleontology. "Mammal body-size responds to climate change in ancient Wyoming." ScienceDaily. ScienceDaily, 29 October 2015. <www.sciencedaily.com/releases/2015/10/151029112230.htm
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Adolescent T. rex unraveling controversy about growth changes in Tyrannosaurus

Date:
October 29, 2015
Source:
Society of Vertebrate Paleontology
Summary:
A much-anticipated study of an adolescent Tyrannosaurus rex is poised to help resolve long-standing controversies over the growth of tyrannosaurid dinosaurs.
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FULL STORY

In 2001, a paleontology field crew from Burpee Museum of Natural History (Rockford, IL) were prospecting for dinosaur fossils near Ekalaka, Montana, when they discovered bones of a half-grown T. rex weathering out from exposures of the Hell Creek Formation. "Jane," as she was later named, turned out to be the most complete adolescent T. rex ever discovered, filling a critical gap between juvenile and adult that had caused decades of scientific debate.

Prior to Jane's discovery, a small lightly built tyrannosaur skull collected near Ekalaka in 1942 had been at the center of a controversy over how much T. rex changed during growth. The skull had spent an uneventful half century on display at Cleveland Museum of Natural History, Ohio, when in 1988, famed paleontologist Dr. Robert Bakker redescribed the fossil as a new species, Nanotyrannus lancensis, proposing that it represented a smaller, more sleek cousin of T. rex.

This interpretation has been controversial since 1999 when Dr. Thomas Carr showed that the differences between "Nanotyrannus" and those of adult T. rex are also seen during growth in other species of tyrannosaurids. This suggested that the Cleveland skull was from a juvenile T. rex rather than being a separate species in its own right. However, this hypothesis met with surprising resistance. Could a dinosaur really change that much during growth?

"The extreme changes from the sleek skull of juveniles to the robust skull of adults were too much for some people to believe; for example, they didn't like to hear that T. rex lost tooth positions as it grew from a juvenile with many teeth, to an adult with fewer teeth. Regardless, the search was on for a transitional specimen that could test the hypothesis."

Enter Jane. Her fine skull and skeleton was intermediate in size and shape between the Cleveland skull and fully adult T. rex. Carr's research team presented a detailed study of Jane at the Society of Vertebrate Paleontology 2015 annual meeting in Dallas.

"Jane shows us that the gap is in fact bridgeable because many features seen in her are more similar to adult T. rex than to the Cleveland skull. The features are exactly what we'd predict are necessary to make the change to a full adult." said Carr.

Another important dimension of the "Jane" story is that she was discovered on public lands, then collected and mounted for display by a public museum. "Dinosaur fossils such as this emphasize the importance of accredited institutions collecting on public lands, which makes the specimens on them available for scientific study," asserts Dr Carr.

In a world where commercially collected dinosaurs demand ever upwardly spiralling prices, Jane is a world-class dinosaur that didn't come with a million dollar price tag. Burpee Museum director of science and exhibits, Scott Williams, summed up:

"Jane is simply the best preserved and most complete example of a publicly accessible, subadult Tyrannosaurus rex in the world. For the last 10 years she has been available to qualified researchers as well as exhibited to the general public. The quality of the specimen and its availability will undoubtedly provide researchers decades of important data regarding the ontogeny of the most recognized dinosaur species in the world."

Regardless of Jane's completeness and growth stage, she doesn't close the book on T. rex growth and evolution; there is still a gap for yet undiscovered fossils to fill between her sleek form and the deep, imposing skulls of adults.


Story Source:

The above post is reprinted from materials provided by Society of Vertebrate Paleontology. Note: Materials may be edited for content and length.



Society of Vertebrate Paleontology. "Adolescent T. rex unraveling controversy about growth changes in Tyrannosaurus." ScienceDaily. ScienceDaily, 29 October 2015. <www.sciencedaily.com/releases/2015/10/151029102249.htm>.


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Dinosaurs used nasal passages to keep brains cool

Date:
October 29, 2015
Source:
Society of Vertebrate Paleontology
Summary:
Dinosaur nasal passages were certainly nothing to sneeze at. Possessing among the largest and most complex nasal passages seen in animals, their function has puzzled paleontologists. New research suggests that the size and shape of these nasal passages would have allowed incoming air to cool the blood making its way to the brain, maintaining the brain at an optimum temperature.

"My work represents the first test of the hypothesis that the elaborated nasal passages of large dinosaurs functioned as efficient heat exchangers," explained Jason Bourke, doctoral student researcher at Ohio University and lead author of the study. Using a branch of engineering known as computational fluid dynamics, Bourke simulated the movement of air and heat through the nasal passages of various dinosaur species.

Nasal passages act as air conditioners, warming and humidifying air as it is breathed in, and cooling and drying it as air leaves the body. This process cools blood destined for the brain. Modern mammals, birds, lizards, and crocodiles use a variety of structures -- some simple, and some complex -- to accomplish heat exchange efficiently. However, detailed reconstruction of the 3-dimensional shape of the nasal passages in dinosaurs have shown that large dinosaurs, whose bodies would have held on to more heat than smaller-bodied animals, needed elaborate and specialized nasal passages to avoid overheating their brains.

"For most dinosaurs that I looked at, there would have been a substantial amount of physiologically active soft tissues in their noses," continued Bourke. "This strongly suggests that dinosaur airways were more than capable of changing the attributes of respired air." These findings provide an answer to the mystery of how dinosaurs avoided having their large bodies overheat their small brains, a question that has plagued paleontologists reconstructing dinosaur physiology.

" By having this blood detour through the nasal passages and dump some of that excess heat before reaching the brain, dinosaurs were able to keep their brains at an optimum temperature for their bodies," said Bourke.


Story Source:

The above post is reprinted from materials provided by Society of Vertebrate Paleontology. Note: Materials may be edited for content and length.



Society of Vertebrate Paleontology. "Dinosaurs used nasal passages to keep brains cool." ScienceDaily. ScienceDaily, 29 October 2015. <www.sciencedaily.com/releases/2015/10/151029102247.htm>.

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Meet the first Iberian lynx on the Iberian Peninsula

Date:
October 28, 2015
Source:
FECYT - Spanish Foundation for Science and Technology
Summary:
The remains of an Iberian lynx specimen which lived 1.6 million years ago -- the oldest ever discovered -- were found resting in a cave in Barcelona. This discovery not only allows us to shed light on the origins of one of the world's most endangered feline species, but it also means that the emergence of this species on the Iberian Peninsula dates back half a million years earlier than what was originally believed.

Reconstruction of the Iberian lynx that lived in the Iberian Peninsula 1.6 million years ago.
Credit: José Antonio Peñas (Sinc)

The remains of an Iberian lynx specimen which lived 1.6 million years ago -- the oldest ever discovered -- were found resting in a cave in Barcelona (Spain). This discovery not only allows us to shed light on the origins of one of the world's most endangered feline species, but it also means that the emergence of this species on the Iberian Peninsula dates back half a million years earlier than what was originally believed.

This newly discovered specimen was 10 to 20 centimetres larger and around 10 kilograms heavier than the Iberian lynx that currently inhabits Doñana National Park in Spain. Its coat was also longer than it is today in order to withstand continuous near-freezing temperatures. This description of the feline was formulated after a study was carried out on one of the first Iberian lynxes that ever lived in Spain.

Part of a cranial fossil belonging to an Iberian lynx (Lynx pardinus) was uncovered among the horse, goat, deer, woolly mammoth, fox and wolf bones preserved in the Avenc Marcel Cave located in the Garraf massif of Barcelona. This is the oldest Iberian lynx that has been found on the Iberian Peninsula to date and it was discovered by the scientist Manel Llenas in 2003.

The fossil remains of this feline are proof of its presence on the Iberian Peninsula as early as 1.6 to 1.7 million years ago. Up until now scientists had dated the appearance of the Iberian lynx to between 1 and 1.1 million years ago. Thus, this discovery means that the emergence of this feline on the Iberian Peninsula actually dates back 500,000 years earlier than what scientists originally thought.

"We have confirmed this earlier appearance of the Iberian lynx based on initial molecular studies that estimate the emergence of this feline during the Early Pleistocene in the Iberian Peninsula," asserts Alberto Boscaini, a researcher at the Miquel Crusafont Catalan Institute of Palaeontology (ICP) and the main author of this study published by Quaternary Science Reviews.

Timeline of the evolution of this species

In order to understand the origins of the Iberian Peninsula's most emblematic species and one of the world's most endangered felines according to the International Union for Conservation of Nature (UICN), we must first go back in time.

The common ancestor of all the species belonging to the Lynx genus, Lynx issiodorensis, first appeared in North America about four million years ago before spreading to the continents of Asia and Europe where it persisted throughout time. These species underwent few changes, with the most evident being a decrease in size.

The first species of lynx to evolve was Lynx rufus about 2.5 million years ago when it scattered across North America. In Asia Lynx lynx emerged, the species that would later spread across Europe. This feline also spread across North America about 200,000 years ago, thus giving rise to Lynx canadensis which displaced Lynx rufus towards the south.

The European population of L. issiodorensis led to the appearance of Lynx pardinus one and half million years ago. Since then, this species has endured few changes to its genetics and continues to inhabit the Iberian Peninsula today. According to scientists, this evolution may have taken place when the Iberian Peninsula became isolated due to one or several consecutive glacial periods.

The new date provided by the study -1.6 million years ago- lines up with the period of time when all of southern Europe, especially the Iberian Peninsula, became a refuge from the Quaternary glaciation.

Glacial periods alternated with interglacial periods that "greatly influenced wildlife, especially mammals, in that habitat," the expert adds.

This refuge was also home to the European rabbit (Oryctolagus cunilus), the Iberian lynx's primary prey more than 75% of the time. The morphological analyses carried out on the cranium found in Catalonia confirm the type of diet consumed by this feline.

"Other cranial features -- such as those related to this carnivore's diet -- are proof that the Iberian lynx hunted small-sized prey such as lagomorphs and rodents which had a great presence during that time period," the researcher states.

According to the study, speciation of the Iberian lynx could therefore be related to the special diet still followed by these specimens inhabiting our planet today, including the rabbit as their primary prey.


Story Source:

The above post is reprinted from materials provided by FECYT - Spanish Foundation for Science and Technology. Note: Materials may be edited for content and length.


Journal Reference:

  1. Alberto Boscaini, Joan Madurell-Malapeira, Manel Llenas, Bienvenido Martínez-Navarro. The origin of the critically endangered Iberian lynx: Speciation, diet and adaptive changes. Quaternary Science Reviews, 2015; 123: 247 DOI: 10.1016/j.quascirev.2015.07.001


FECYT - Spanish Foundation for Science and Technology. "Meet the first Iberian lynx on the Iberian Peninsula." ScienceDaily. ScienceDaily, 28 October 2015. <www.sciencedaily.com/releases/2015/10/151028130851.htm>.




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Posted by: Lin Kerns <linkerns@gmail.com>



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[Geology2] ‘Something Big Moving Out There’



Seismic Station in Alaska Records a Disturbance That Wasn't an Earthquake: 'Something Big Moving Out There'

Oct. 29, 2015  Liz Klimas

Recordings taken at a station that detects seismic activity at Kultieth River Mountain in southeast Alaska would suggest that the area experienced a strong disturbance earlier this month.

But it was no earthquake.

The incident recorded by the Alaska Earthquake Center's seismic sensor, according to KTUU-TV, was actually the work of a bear, or at least that's what scientists think.

"We aren't sure for certain it was a bear, but the data shows indicates it was something big moving out there before the data stopped coming in," field engineer Scott Dalton told the news station.

The shaking detected by the station lasted for eight minutes and then transmission stopped.

"We still have power out there so we think that means that an animal dug up the cables between the sensor and the fiberglass hut that provides power," Dalton told KTUU.


Evidence of chewing was discovered on the lids of containers that hold the seismic sensors.

"Ever wonder what it looks like when a bear takes out a seismic station?" the center tweeted this week.


It appears that this station has been the target of other animal attacks the past as well.

"This same station was damaged last year by what we think was a goat," Dalton told the news station.

KTUU reported the station will not undergo repair until next year.

http://www.theblaze.com/stories/2015/10/29/seismic-station-in-alaska-records-a-disturbance-that-wasnt-an-earthquake-something-big-moving-out-there/
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Posted by: Lin Kerns <linkerns@gmail.com>



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[Geology2] Official behind earthquake advice to stand trial in Italy




In ruins: The 2009 L'Aquila earthquake killed over 300 people.

Joanna Faure Walker/Flickr (CC BY 2.0)

In ruins: The 2009 L'Aquila earthquake killed over 300 people.

Official behind earthquake advice to stand trial in Italy

By Edwin Cartlidge
29 October 2015

A high-ranking public official who sent a group of scientists to L'Aquila to assess seismic risk ahead of the deadly earthquake that struck the city in 2009 is to stand trial on charges of manslaughter, a judge ruled today. His trial follows the October 2012 conviction and sentencing to 6 years in prison of the seven experts, and the acquittal of all bar one of them last November.

Guido Bertolaso, who at the time of the earthquake was head of Italy's civil protection department, set up a meeting of the experts as full or acting members of an official panel known as the National Commission for the Forecast and Prevention of Major Risks on 31 March 2009, ostensibly to analyze the risk posed by a series of small- and medium-sized earthquakes that had been shaking the region around L'Aquila for several months. But following the earthquake, which struck 6 days later leaving 309 dead, the scientists were accused of having provided the public with a false and fatal sense of security.

The experts—Bertolaso's deputy together with three seismologists, a volcanologist, and two seismic engineers—were put on trial in L'Aquila in September 2011 and charged with having carried out a superficial risk analysis during their 2009 meeting. The prosecution alleged that they made a series of unjustifiably reassuring statements that led some people to abandon traditional precaution and remain indoors during the quake.

The new trial centers on a telephone call that Bertolaso made to a local official the evening before the experts' meeting, a police recording of which was released by the newspaper La Repubblica during the original trial. In the call, Bertolaso described the meeting as a "media operation" that he was setting up in order to "shut up" a technician from a nearby physics laboratory who had allegedly made a series of alarmist predictions that had panicked the local population.

During the call, Bertolaso also told the official what the scientists would say in their meeting—that the ongoing tremors were positive because they discharged energy and so made a major earthquake less likely. Many witnesses during the trial said that it was this idea of an energy discharge that had particularly reassured their relatives, leading them to remain inside and perish on the fateful night.

Manslaughter investigations against Bertolaso started just a few days after the recording of the phone call came to light in January 2012 but it is only now that judge Guendalina Buccella has ordered him to stand trial. The prosecutor in the original trial, Fabio Picuti, twice requested that the case against Bertolaso be dropped, and on both occasions that request was contested by lawyers representing relatives of some of the victims. But judge Buccella today ruled that the former civil protection boss should be tried, and that the first hearing should take place in L'Aquila on 20 November, just a day after the trial of the seven scientists reaches the Supreme Court of Cassation, Italy's highest appeal court.


Science| DOI: 10.1126/science.aad6144

http://news.sciencemag.org/europe/2015/10/official-behind-earthquake-advice-stand-trial-italy
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Thursday, October 29, 2015

[Geology2] Prehistoric plumage patterns



Prehistoric plumage patterns


An illustration of Ornithomimus based on the findings of preserved tail feathers and soft tissue
Credit: Julius Csotonyi
An undergraduate University of Alberta paleontology student has discovered an Ornithomimus dinosaur with preserved tail feathers and soft tissue. The discovery is shedding light on the convergent evolution of these dinosaurs with ostriches and emus relating to thermoregulation and is also tightening the linkages between dinosaurs and modern birds.

"We now know what the plumage looked like on the tail, and that from the mid-femur down, it had bare skin," says Aaron van der Reest. This is the first report of such preserved skin forming a web from the femoral shaft to the abdomen, never before seen in non-avian dinosaurs. "Ostriches use bare skin to thermoregulate. Because the plumage on this specimen is virtually identical to that of an ostrich, we can infer that Ornithomimus was likely doing the same thing, using feathered regions on their body to maintain body temperature. It would've looked a lot like an ostrich." In fact, this group of animals—referred to as ornithomimids—is commonly referred to as "ostrich mimics."
Although the preserved feathers are extremely crushed due to sediment compaction, scanning electron microscopy reveals a three-dimensional keratin structure to the feathers on the tail and body. van der Reest made the initial discovery during his first year as an undergraduate student, supervised by Philip Currie, Canada's leading palentologist."It's pretty remarkable. I don't know if I've stopped smiling since."

Predicting future adaptations to environmental changes

This new specimen—one of only three feathered Ornithomimus specimens in the world—is shedding light on the animal's evolutionary adaptation to different environments. "We are getting the newest information on what these animals may have looked like, how they maintained body temperatures, and the stages of feather evolution." van der Reest notes that the findings may be used to further understand why animals have adapted the way they have and to predict how animals will have to adapt in the future in order to survive environmental changes.

"This specimen also tightens the linkages between dinosaurs and birds, in particular with respect to theropods," says Alex Wolfe, second author on the paper. "There are so many components of the morphology of this fossil as well as the chemistry of the feathers that are essentially indistinguishable from modern birds."

The discovery may also alter future excavation techniques, explains van der Reest. "If we can better understand the processes behind the preservation of the feathers in this specimen, we can better predict whether other fossilized animals in the ground will have soft tissues, feathers, or skin impressions preserved."

Reference:
A densely feathered ornithomimid (Dinosauria: Theropoda) from the Upper Cretaceous Dinosaur Park Formation, Alberta, Canada, DOI: 10.1016/j.cretres.2015.10.004

Note: The above post is reprinted from materials provided by University of Alberta.

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[Volcano_Vista_HS] VVHS Announcements--Thursday, October 29, 2015



Best Buddies will have its Halloween match party on Friday during lunch in room H115. Come by and meet your buddy! 

 

SPOOK-O-GRAM Want to give your friend a trick or treat for Halloween? Buy a spook-o-gram for $1.00 during lunch in the lower E- hall eatery the week of October 26th. 

 

CANNED FOOD DRIVE: Senate is sponsoring a canned food drive to benefit Road Runner Food Bank. You may bring donations to the activities office. The drive will end on November 6th.

 

Hip Hop Club will have the next meeting this Friday at 2:30- 3:30 after school MEETING IN H HALL. Please bring appropriate dance attire, and also anyone still interest is still welcomed to come!

 

Food in Classrooms - Students and Staff:  please do not eat, drink or leave food in the classrooms.  This is a health concern and may cause insects to gather in your rooms.  Thank you in advance.

 

ATHLETICS:

  • GIRLS BASKETBALL tryouts will be November 2-4 after school 2:45-4:30pm. Anyone interested needs to have a current APS physical and insurance information turned in to be able to try out. See Coach Villareal in F202 or Coach Dominguez in E104. 

  • THE VOLLEYBALL TEAM will have a playoff match for the District Championship on Tuesday against Cibola.  The game will be at 5pm at Rio Rancho High School. We'd love to have a great student section at the game! Thanks for your support!!!!

  • FOOTBALL has their last game of the regular season on Friday at Santa Fe High School at 7pm.

  • XC has their district meet on Saturday at 10am 

  • GIRLS SOCCER plays Clovis at the Soccer Complex at 5pm on Friday. This is the first round of the state tournament. Good Luck Ladies.

  • WRESTLING: For those interested in wrestling please contact Coach Ahren Griego for wrestling information. Wrestling season starts this upcoming Monday, NOV 2nd. 

 

And finally Day light savings time ends this weekend. Turn your clocks back one hour. Yes you will gain one hour of sleep.


Have a great day

And remember                                                      

As always…

It's great to be a Hawk!



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Posted by: ssteckbeck@yahoo.com


For more information, go to our web site: http://www.volcanovistahawks.com




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[Geology2] Scientists develop a new method for predicting volcanic eruptions



Scientists develop a new method for predicting volcanic eruptions

Date:
October 28, 2015
Source:
University of Royal Holloway London
Summary:
Researchers have developed a new method which could more accurately determine the conditions needed for a volcano to erupt.

Researchers from the Department of Earth Sciences at Royal Holloway, University of London, have developed a new method which could more accurately determine the conditions needed for a volcano to erupt. The study will be published on 28 October in Scientific Reports.

The team, composed of PhD students John Browning and Sandy Drymoni and Professor Agust Gudmundsson, used newly collected geological data and historical data on previous eruptions of the Santorini volcano in Greece, to work out the capacity of the volcano's magma-chamber. They were then able to build a model which allowed them to estimate the pressure increase in the magma-chamber when it's being refilled and therefore forecast when it's likely to rupture and potentially cause an eruption.

The team travelled to island of Santorini in Greece to collect data on the type of magma which feeds eruptions. They took measurements of magma-filled fractures (dykes) which are exposed in impressive form along the northern wall of the Santorini caldera. Using geodetic data from 2012, when the volcano was thought to be close to an eruption, the team determined, using their new method, that the magma chamber did, in fact, not rupture at that time. Thus, while great volume of new magma was received by the Santorini chamber in 2012, so that it came close to rupture (and possible eruption), the chamber did not quite reach the rupture stage.

The new model has the potential to forecast when magma chambers in other volcanoes could rupture and potentially lead to eruptions, which should aid emergency planning and risk assessments.

John Browning, said: "We have been able to provide constraints on the volume of magma stored in a shallow magma chamber underneath Santorini Caldera. We believe our new model can be used to forecast the timing of magma-chamber rupture at Santorini and, eventually, at well-monitored volcanoes worldwide. Whilst this is an important step towards reliable prediction of volcanic eruptions, a number of challenges still exist. For example, even if the magma chamber were to rupture we currently have no way of predicting whether the magma-filled fracture (the dyke) injected from the chamber will make it to the surface. In most cases the magma stalls or stops before it reaches the surface. Under which conditions magma stalls in volcanoes (preventing eruption) is among the most important unsolved problems in volcanology."


Story Source:

The above post is reprinted from materials provided by University of Royal Holloway London. Note: Materials may be edited for content and length.


Journal Reference:

  1. John Browning, Kyriaki Drymoni, Agust Gudmundsson. Forecasting magma-chamber rupture at Santorini volcano, Greece. Scientific Reports, 2015; 5: 15785 DOI: 10.1038/srep15785


University of Royal Holloway London. "Scientists develop a new method for predicting volcanic eruptions." ScienceDaily. ScienceDaily, 28 October 2015. <www.sciencedaily.com/releases/2015/10/151028084917.htm>.

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Posted by: Lin Kerns <linkerns@gmail.com>



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[Geology2] Mammoths might have survived except for bad 'mineral diet'



Mammoths might have survived except for bad 'mineral diet'

Date:
October 27, 2015
Source:
National Research Tomsk State University
Summary:
At the end of the Pleistocene mammoths of Northern Eurasia used to experience chronic mineral hunger. As a result they became extinct due to geochemical stress arising on a background of deep abiotic changes in ecosystems. Most likely they were receiving not enough of essential chemical elements.

This image shows a fragment of the calf scull.
Credit: Copyright TSU

At the end of the Pleistocene mammoths of Northern Eurasia used to experience chronic mineral hunger. As a result they became extinct due to geochemical stress arising on a background of deep abiotic changes in ecosystems. Most likely they were receiving not enough of essential chemical elements. This hypothesis was developed by TSU paleontologists and based on a large-scale, 15-years long research. Detailed information you can find in an article of Sergei Leshchinsky, Head of Laboratory of Mesozoic and Cenozoic continental ecosystems, TSU Faculty of Geology and Geography. This article was published in Archaeological and Anthropological Sciences.

Researchers around the world try to find out causes of extinction of the most prominent representatives of late Pleistocene megafauna -- the mammoths. There are two main versions: 1) changes in microclimate and anthropogenic pressure, and possibly simultaneous effect of both factors. There are other much less popular theories of their extinction: 1) infectious diseases or 2) fall of celestial bodies. However, hardly anybody has paid attention to geochemical changes of environment where Mammuthus primigenius lived.

Investigating remains of late mammoths, we frequently find obvious signs of skeletal diseases such as: osteoporosis, osteofibrosis, osteomalacia (softening and bending of bones), arthrosis, and other joint diseases -- says Sergei Leshchinsky. He also underlines that articular surface of extremity bones of some individuals are not only harmed but damaged and mutilated by these diseases. As for osteoporosis, in separate collections we found it in 90% of cases.

These diseases resulted in high traumatism of the animals; they got sprains and fractures even at very low loads. Mammoths with broken limbs or spine could not take food in sufficient quantities and could not follow herd. Such individuals died soon hunted by predators. As a result -- the nature was stronger than the giant animals, and mammoths became extinct.

From 2003 to 2013 Sergey Leshchinskiy analyzed over 23,500 bones and teeth of mammoths of Northern Eurasia to identify the symptoms of enzootic diseases. The destructive changes were revealed with the help of a magnifying glass (×10), in polished sections and histological sections under a stereomicroscope (magnification upto200×) and a scanning electron microscope (magnification upto10,000×), as well as by roentgenoscopy and densitometry.

We investigated mammoth bones and teeth, discovered in beast solonetzs lacustrine-alluvial localities of Russia, Poland and the Czech Republic.

The beast solonetz is the Russian term for a ground surface area characterized by a high content of certain macro- and microelements; as such it has a broader interpretation than "salt lick," "mineral lick" and "mineral source." Within the confines of the beast solonetz, animals eat soil and rocks and drink mineralized water from springs to maintain homeostasis, which is equivalent to the definition of "lithophagy."

Most of chemical elements are vital necessary for animals to retain health condition of skeleton, muscles, skin, hear, and others. Part of animals is doomed if they fail to satisfy a mineral starvation in time.

Lithophagy or geophagy practiced by primates is a commmon phenomenon in modern animal life; there is no doubt, therefore, that the mammoth was the largest of all lithophages in the Late Pleistocene of Northern Eurasia. This assertion is also confirmed by the frequent availability of mineral sub¬stances in the gastro-intestinal tract of mammoth carcasses and their coprolites, sometimes reaching 90% of their mass.

At the highest moment of mineral starvation they became some kind of activity hotbed of mammoths and other large mammals. The particular vulnerability of mammoth in mineral starvation can be reflected in specific mammoth "cemeteries" of the late Pleistocene.

TSU researchers found mass destructive changes in mammoth bones and teeth up to 70% or more of total number of remains in different collection. In most cases different destructions accompany one another which may indirectly show the same reasons of such consequences. In collection of some excavation areas (Krasnoyarskaya Kurya, Kraków Spadzista Street) probably the most common disease is osteoporosis. We can see rarefaction in all age groups including infant mammoths what means that disease development began in prenatal period since females suffered from mineral starvation. Above all since bone resorption in osteoporosis may be mild marked outwardly; it means that real proportion of remains with signs of osteodystrophy is likely to be higher than can be detected at a superficial examination.

Why did mammoths and other large herbivores with large skeleton experience strong geochemical stress of Pleistocene?

At that time there was a considerable expansion of acidic and acidic-gley geochemical landscapes, resulting in a drastic deficiency of Ca, Mg, Na, P, I, Co, Cu, Se, Zn and other vital chemical elements. The change in habitat is closely associated with the drastic replacement of favourable Ca-Mg-Na landscapes with acidic and acidic-gley ones. The latter reached its maximum range by the end of the Pleistocene, and are still the predominant landscape in most of Northern Eurasia today. This transition can be explained by the general neotectonic lift, which was subsequently followed (17-10 ka BP) by changes in the macroclimate, which became more humid and warmer. As a result, coastal lowlands were flooded and central areas were swamped (degrading permafrost being one of the reasons). The soils of the high plains and foothills were heavily leached due to a lowering of the ground water levels and increased precipitations. In this situation only rare beast solonetz could have served as geochemical oases where the large herbivores could satisfy their mineral hunger. However, by the early Holocene there may have been an insufficient number of these oases to support the viability of isolated mammoth populations. A similar abiotic scenario may be drawn for North America, where mammoths went extinct at the same time.

Mammoth body size decrease and massive destructive changes in their bones and teeth indicate negative impact of the abiotic environment. Osteoporosis, osteomalacia, diseases of the joints indicate a metabolic disorder of alimentary nature.

The analysis of the clinical picture of the diseases deserves special attention -how rapidly did the disturbances in homeostasis and the formation of osteodystrophy occur in unfavourable geochemical conditions? Based on this study, it appears that the destructive changes developed rapidly: extensive bone pathologies such as those found in the Taymyrskiy mammoth or in the Shestakovo-Kochegur, Berelyokh, Lugovskoe and Krakow Spadzista Street mammoth populations are incompatible with along developmental period. Under conditions of smaller and fewer geochemical oases and predominantly snow or acidic swampy-ground waters as drinking water in the winter, the "later" mammoths may have suffered from chronic mineral deficiency for 6- 10 months a year.

"It is highly probable that this severe natural condition lasted for more than 15 thousand years and may have proven fatal for the largest representative of the terrestrial fauna at high latitudes," Sergey Leshchinskiy said. "The wool lyrhinoceros and cave bear may have suffered the same fate. Other large herbivores (bisons, horses and deer) have overcome the Holocene border, perhaps due to their greater mobility, although with a significant reduction of habitat and population size. Large cats and hyenas went extinct probably because of drastic reduction of nutritional resources at the time of the disintegration of the single "mammoth" ecosystem."

The very high percentage of skeleton pathologies suggests a high murrain among mammoths, irrespective of anthropogenic impact, which could not lead to this species extermination throughout its huge territory. Man was a witness and one of the participants in the natural process of the Pleistocene megafauna's extinction.

10.1007/sl12520-014-0205-4


Story Source:

The above post is reprinted from materials provided by National Research Tomsk State University. Note: Materials may be edited for content and length.


Journal Reference:

  1. Sergey Leshchinskiy. Enzootic diseases and extinction of mammoths as a reflection of deep geochemical changes in ecosystems of Northern Eurasia. Archaeological and Anthropological Sciences, 2014; 7 (3): 297 DOI: 10.1007/s12520-014-0205-4


National Research Tomsk State University. "Mammoths might have survived except for bad 'mineral diet'." ScienceDaily. ScienceDaily, 27 October 2015. <www.sciencedaily.com/releases/2015/10/151027154937.htm>.

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Posted by: Lin Kerns <linkerns@gmail.com>



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