Wednesday, September 30, 2015

[Volcano_Vista_HS] VVHS Announcements--Wednesday, September 30, 2015



This week is Ally Week. What is Ally Week, you ask? Every year, the Gay, Lesbian, and Straight Education Network and students across the country, often as members of Gay-Straight Alliances (GSAs) or similar student clubs, celebrate Ally Week. Here at VVHS we are focusing this week on educating our school community on ways to be better allies.

 

What is an Ally? We refer to allies as people who support the LGBT community by advocating against the bullying and harassment LGBT youth face in school. Anyone can be an ally!

 

What can you do? During lunch, come to the A hall or F hall and create an Ally sign. We are trying to fill the wall outside A120 with Ally signs...we have a great start, but can always use more signs and more allies.

 

In addition, there will be a brown bag lunch for teachers on Thursday in Ms. Phaneuf's room, A120.  The topic presented by our GSA Hawks will be "How to Be a Better Ally to Your Students".  And who better to learn from than our students. So I encourage all faculty and staff to come on Thursday and support the students.  Dessert will be provided. Contact MS. Phaneuf for more information.

 

Wing Squad: There is a meeting today in H107, at lunch. New members are welcome!

The Volcano Vista Drama Department presents Arthur Miller's The Crucible, a classic play about the Salem Witch Trials, on October 1, 2, and 3. Performances are at 7PM, with a matinee at 2pm on October 3. Tickets are $5 for adults, $3 for students, and $1 for active Thespians.

 

 

COUNSELING:

  • A representative from New Mexico State will be on campus Friday October 2nd, at lunch, in lower E-Hall. Stop by to get information about admissions and financial aid.

 

ATHLETICS

  • FOOTBALL plays West Mesa at 7 on Friday at Community Stadium.  We are on the visitor side.

  • BOYS SOCCER plays Cleveland today at 3:30. 

  • GIRLS SOCCER plays at Cleveland today at 4 

VOLLEYBALL: Congratulations to our Lady Hawks for defeating the Cougars 3-1 in their Pink-Out game last night. They will play at Rio Rancho tomorrow at 6

 

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 simulate Earth's middle crust to understand earthquakes



Scientists simulate Earth's middle crust to understand earthquakes

Date:
September 29, 2015
Source:
University of Texas at Austin
Summary:
Researchers have for the first time been able to measure a material's resistance to fracturing from various types of tectonic motions in Earth's middle crust, a discovery that may lead to better understanding of how large earthquakes and slower moving events interact.

Researchers have for the first time been able to measure a material's resistance to fracturing from various types of tectonic motions in Earth's middle crust, a discovery that may lead to better understanding of how large earthquakes and slower moving events interact.

The University of Texas Institute for Geophysics (UTIG), research unit of the Jackson School of Geosciences, spearheaded the discovery. The study was published in the September edition of Nature Geoscience.

Scientists conducted the research using Carbopol, a gel-like substance that can simulate the characteristics of rock formations in Earth's middle crust because it is simultaneously brittle and malleable.

Researchers performed shear tests on the Carbopol, where a portion of the material is pulled one direction and a portion is pulled in the opposite direction. This is similar to what happens to rock formations in the middle crust during earthquakes or slow-slip events, a type of tectonic movement that resembles an earthquake but happens over a much longer period of time.

Previously, nearly all research into such movements of Earth's crusts was done by measuring tectonic movement using GPS readings and linking these findings with friction laws. Those observations did not address how rock behaves when it softens under heat and pressure.

"It is not really clear how slow-slip events interact with earthquakes, whether they can trigger earthquakes or it's the other way around -- that earthquakes trigger slow-slip events," said Jacqueline Reber, the study's lead author who performed this research as postdoctoral fellow at UTIG, and who is now an assistant professor at Iowa State University.

The research also adds insight into middle crust strain transients, temporary stress on surrounding rock that's caused by tectonic motion.

"By understanding the mechanics of strain transients a little bit better, we eventually hope to get better insight into how they relate to big, catastrophic earthquakes."

Unlike slow slips events, earthquakes -- or stick-slip events -- occur when surfaces quickly alternate between sticking to each other and sliding over each other.

"While earlier studies focused mostly on frictional behavior as an explanation for strain transients we focus in our work on the impact of rheology (how a material flows under stress), especially when it is semi-brittle," said Reber.

The semi-brittle middle crust can be compared to a candy bar made of nuts and caramel. The nuts represent the brittle rock. The caramel represents the ductile rock.

Researchers exposed Carbopol, in which the ratio between brittle and ductile parts determines how much stress it can take before being permanently deformed or breaking, to forces created by a simple spring-powered shearing apparatus. Lower yield stress induced the Carbonol to imitate hotter, more viscous rock from deeper in Earth's crust by making it more ductile; at higher yield stress it imitated cooler, more brittle rock.

The tests showed viscous deformation and constant creep movement at lower yield stress and slip-stick behavior at higher yield stress. This highlights the importance of a material's often complex properties for determining the manner and speed it will respond to stress.


Story Source:

The above post is reprinted from materials provided by University of Texas at Austin. Note: Materials may be edited for content and length.


Journal Reference:

  1. Jacqueline E. Reber, Luc L. Lavier, Nicholas W. Hayman. Experimental demonstration of a semi-brittle origin for crustal strain transients. Nature Geoscience, 2015; 8 (9): 712 DOI: 10.1038/ngeo2496


University of Texas at Austin. "Scientists simulate Earth's middle crust to understand earthquakes." ScienceDaily. ScienceDaily, 29 September 2015. <www.sciencedaily.com/releases/2015/09/150929092855.htm>.

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



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[Geology2] Rare early Jurassic corals of North America



Rare early Jurassic corals of North America

Date:
September 29, 2015
Source:
Geological Society of America
Summary:
Mass extinction events punctuate the evolution of marine environments, and recovery biotas paved the way for major biotic changes. Understanding the responses of marine organisms in the post-extinction recovery phase is paramount to gaining insight into the dynamics of these changes, many of which brought sweeping biotic reorganizations.

Mass extinction events punctuate the evolution of marine environments, and recovery biotas paved the way for major biotic changes. Understanding the responses of marine organisms in the post-extinction recovery phase is paramount to gaining insight into the dynamics of these changes, many of which brought sweeping biotic reorganizations.

In the October issue of GSA Today, Montana Hodges and George Stanley Jr. of the University of Montana Paleontology Center report on coral recovery after the end-Triassic mass extinction event at the Triassic-Jurassic (T/J) mass extinction boundary. The authors examined Jurassic corals in a continuous depositional section of the Gabbs and Sunrise Formations near New York Canyon in west-central Nevada, USA.

Because Early Jurassic corals from North America are so rare, newly discovered occurrences are vital to understanding biotic responses in the post-mass extinction interval. In this paper, Hodges and Stanley make a preliminary report of the earliest Jurassic corals from the U.S., which are also some of the earliest in North America. These examples occur at New York Canyon in west-central Nevada's Sunrise Formation.

This site has attracted international attention because it is among the best-documented T/J sections in North America. The coral occurrences in this section are near the T/J boundary, making the Nevada site ideal for understanding the dynamics of coral recovery and comparing them with the Tethys.

The authors write that these New York Canyon corals offer additional information on recovery in eastern Panthalassa along the craton of North America. "Paleogeographically, the New York Canyon corals show a strong connection with the Tethys, but in contrast are exclusively solitary and exclusively stylophyllid taxa. Hettangian corals are unknown from North America, so for the present, the New York Canyon site may be the earliest North American Jurassic example."

According to Hodges and Stanley, analysis of these corals fills a neglected but important part of the T/J recovery phase in North America, while lending support for an earlier opening of the Hispanic Corridor.


Story Source:

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


Journal Reference:

  1. Montana S. Hodges, George D. Stanley. North American coral recovery after the end-Triassic mass extinction, New York Canyon, Nevada, USA. GSA Today, 2015; 15 (10): 4 DOI: 10.1130/GSATG249A.1


Geological Society of America. "Rare early Jurassic corals of North America." ScienceDaily. ScienceDaily, 29 September 2015. <www.sciencedaily.com/releases/2015/09/150929142520.htm>.

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



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[Geology2] Bacteria in ancient flea may be ancestor of the Black Death



Bacteria in ancient flea may be ancestor of the Black Death

Date:
September 28, 2015
Source:
Oregon State University
Summary:
A 20-million-year-old flea, entombed in amber with tiny bacteria attached to it, provides what researchers believe may be the oldest evidence on Earth of a dreaded and historic killer -- an ancient strain of the bubonic plague.

This flea preserved about 20 million years ago in amber may carry evidence of an ancestral strain of the bubonic plague.
Credit: Photo by George Poinar, Jr., courtesy of Oregon State University

About 20 million years ago a single flea became entombed in amber with tiny bacteria attached to it, providing what researchers believe may be the oldest evidence on Earth of a dreaded and historic killer -- an ancient strain of the bubonic plague.

If indeed the fossil bacteria are related to plague bacteria, Yersinia pestis, the discovery would show that this scourge, which killed more than half the population of Europe in the 14th century, actually had been around for millions of years before that, traveled around much of the world, and predates the human race.

Findings on this extraordinary amber fossil have been published in the Journal of Medical Entomology by George Poinar, Jr., an entomology researcher in the College of Science at Oregon State University, and a leading expert on plant and animal life forms found preserved in this semi-precious stone.

It can't be determined with certainty that these bacteria, which were attached to the flea's proboscis in a dried droplet and compacted in its rectum, are related to Yersinia pestis, scientists say. But their size, shape and characteristics are consistent with modern forms of those bacteria. They are a coccobacillus bacteria; they are seen in both rod and nearly spherical shapes; and are similar to those of Yersinia pestis. Of the pathogenic bacteria transmitted by fleas today, only Yersinia has such shapes.

"Aside from physical characteristics of the fossil bacteria that are similar to plague bacteria, their location in the rectum of the flea is known to occur in modern plague bacteria," Poinar said. "And in this fossil, the presence of similar bacteria in a dried droplet on the proboscis of the flea is consistent with the method of transmission of plague bacteria by modern fleas."

These findings are in conflict with modern genomic studies indicating that the flea-plague-vertebrate cycle evolved only in the past 20,000 years, rather than 20 million. However, today there are several strains of Yersinia pestis, and there is evidence that past outbreaks of this disease were caused by still different strains, some of which are extinct today.

While human strains of Yersinia could well have evolved some 10,000 to 20,000 years ago, Poinar said, ancient Yersinia strains that evolved as rodent parasites could have appeared long before humans existed. These ancient strains would certainly be extinct by now, he said.

The complex mode of transmission of plague is also reflected in the flea seen in this fossil.

When a flea feeds on a plague-infected animal, the Yersinia pestis bacteria taken up with the blood often form a viscous mass in the flea's proventriculus, located between the stomach and esophagus. When this happens, the fleas can't obtain enough blood, and as they attempt to feed again, bacteria are often forced back out through the proboscis and into the wound.

This blockage is in part what makes them effective vectors of the plague, and the dried droplets on the proboscis of the fossil flea could represent a sample of the sticky bacterial mass that was regurgitated.

"If this is an ancient strain of Yersinia, it would be extraordinary," Poinar said. "It would show that plague is actually an ancient disease that no doubt was infecting and possibly causing some extinction of animals long before any humans existed. Plague may have played a larger role in the past than we imagined."

The fossil flea originated from amber mines in what is now the Dominican Republic, between Puerto Plata and Santiago. Millions of years ago the area was a tropical moist forest.

Very few fleas of any type have been found preserved in amber, Poinar said, and none have been reported with associated microorganisms, as in this case. This specimen had some other unique morphological features that indicate it's a species that long ago went extinct.

But it was the associated bacteria that fascinated the researchers.

"Since the dried droplet with bacteria is still attached to the tip of the proboscis, the flea may have become entrapped in resin shortly after it had fed on an infected animal," Poinar said. "This might have been one of the rodents that occurred in the Dominican amber forest. Rodent hair has been recovered from that amber source."

Flea-like creatures found in conventional stone fossils date back to the time of the dinosaurs, Poinar said, and the role of insects in general, and as carriers of disease, may have played a role in the demise of the ancient reptiles.

In 2008, Poinar and his wife, Roberta Poinar, wrote a book "What Bugged the Dinosaurs? Insects, Disease and Death in the Cretaceous." It explored the evolutionary rise of insects around the same time that dinosaurs went extinct. The thesis developed in the book added insect-borne diseases as a likely component, that, along with other biotic and abiotic factors such as climate change, asteroid impacts and volcanic eruptions, led to the extinction of the dinosaurs. Some modern diseases such as leishmaniasis and malaria clearly date to those times.

Bubonic plague in modern times can infect and kill a wide range of animals, in addition to humans. It is still endemic in many countries, including the United States where it's been found in prairie dogs and some other animals. Even though today it is treatable with antibiotics, in the U.S. four people have died from plague so far this year.

During the Middle Ages, however, three phases of the disease -- bubonic, septicemic and pneumonic plague -- earned a feared reputation. Periodic waves of what was called the Black Death, for the gruesome condition in which it left its victims, swept through Europe and Asia, altogether killing an estimated 75 to 200 million people.

Scholars say that religious, social and economic changes caused by the plague altered the course of world history.


Story Source:

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


Journal Reference:

  1. George Poinar. A New Genus of Fleas with Associated Microorganisms in Dominican Amber. Journal of Medical Entomology, 2015; tjv134 DOI: 10.1093/jme/tjv134

Oregon State University. "Bacteria in ancient flea may be ancestor of the Black Death." ScienceDaily. ScienceDaily, 28 September 2015. <www.sciencedaily.com/releases/2015/09/150928152503.htm>.

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



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Tuesday, September 29, 2015

[Volcano_Vista_HS] VVHS Wrestling Team Rummage Sale This Saturday [1 Attachment]

[Attachment(s) from ssteckbeck@yahoo.com [Volcano_Vista_HS] included below]

The VVHS Wrestling Booster Club is sponsoring a multi-family Rummage Sale this Saturday from 7AM-2PM at Volcano Vista. Spaces available to rent!  See attached flyer for details!!



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Attachment(s) from ssteckbeck@yahoo.com [Volcano_Vista_HS] | View attachments on the web

1 of 1 File(s)


Posted by: ssteckbeck@yahoo.com


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




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[Geology2] Spectacular footage of erupting Ubinas volcano in Peru – video





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



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[californiadisasters] Wildfire Scars California Towns September 23, 2015



Wildfire Scars California Towns
False Color (SWIR)
acquired September 20, 2015 download large False Color (SWIR) image (10 MB, JPEG, 3500x3500)
acquired September 20, 2015

Devastation of the sort that the fast-moving Valley Fire unleashed rarely has a single cause. Long before the blaze started burning through Boggs Mountain State Forest, decades of aggressive firefighting—and too few prescribed fires—left the woodlands overloaded with brush and other fuel. Meanwhile, extreme drought over the past four years has sucked the forests dry of moisture, leaving the trees unusually combustible. An army of destructive bark beetles also has made the pine forests vulnerable.

So when a weather system delivered abnormally hot temperatures and gusty winds to Napa, Sonoma, and Lake counties in northern California, the forests were primed to burn intensely. The first spark likely came from a shed fire in the town of Cobb on September 12, 2015. Once it had escaped the shed, the fire spread with such speed and intensity that firefighters could do little to slow it. Within 48 hours, the inferno had burned an area twice as large as Manhattan as it raced southeast along ridges in Boggs Mountain State Forest toward the communities of Harbin Springs, Anderson Springs, and Middletown.

As flames pushed toward these towns, thousands of people were forced to flee their homes with little warming. In all, authorities report that 1,910 structures were destroyed, including many at a popular hot springs resort in Harbin Springs. At least three civilians lost their lives; four firefighters were injured. The Valley Fire has already become one of California's most damaging fires. Only two other blazes—the Cedar fire in 2003 and the Tunnel Fire in 1991—destroyed more structures.

The Operational Land Imager (OLI) on Landsat 8 captured false-color view of the charred landscape on September 20, 2015. The image is a composite based on data OLI collected with its short-wave infrared and near-infrared bands. Newly burned land has a strong signal in short-wave infrared bands, visible as dark red-orange areas. Unburned forests appear gray. Buildings are white. The second image below shows a broader view. According to the California Department of Forestry, the fire had burned 76,067 acres (30,783 hectares) as of September 22, 2015, and it was 75 percent contained.

The image at the bottom of the page shows a natural-color view of Middletown. Burned areas appear gray. To see ground photography showing the extent of the damage in Anderson Springs and Middletown, see these reports from the Los Angeles Times and Newsweek. A resident fleeing Anderson Springs captured harrowing video from inside the fire perimeter on September 12, 2015.

acquired September 20, 2015 download large Natural Color image (11 MB, JPEG, 3500x3500)
NASA Earth Observatory images by Joshua Stevens, using Landsat data from the U.S. Geological Survey. Caption by Adam Voiland.

http://earthobservatory.nasa.gov/IOTD/view.php?id=86663&src=eoa-iotd

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


Be sure to check out our Links Section at http://groups.yahoo.com/group/californiadisasters/links
Please join our Discussion Group at http://groups.yahoo.com/group/californiadisasters_discussion/ for topical but extended discussions started here or for less topical but nonetheless relevant messages.





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[Volcano_Vista_HS] VVHS Cross Country Goodwill Donation Event This Saturday [1 Attachment]

[Attachment(s) from ssteckbeck@yahoo.com [Volcano_Vista_HS] included below]

The Cross Country Booster Club is hosting a donation event Saturday, October 3rd at the school.  Bins will be at the school this Saturday, October 3rd in conjunction with the meet we host. Please advertise this to your friends. We will earn money based on how many bins we can fill. (Please see attached flyer)

 

 

GoodDeeds. GoodCommunity

Clean out those closets, bag up those clothes...

We need your donations!

Saturday, Oct 3.

9 a.m. to 1 p.m.

Volcano Vista High School

Cross Country Team

8100 Rainbow Road NW

 

Volcano Vista's Cross Country Booster Club is teaming up with Goodwill Industries of New Mexico (GINM). GINM provides skills training, job development and social services to New Mexicans at no charge to them. These services are vital to our community and funded by the sale of gently used items in Goodwill's thrift stores.  Drop off any of the following in new or gently used condition: Clothing, shoes, handbags, kitchen utensils, home decor, plates, cups, housewares, sporting equipment, toys, books, jewelry, small kitchen electrics, etc.

(*No televisions or mattresses please)

*Please note donation receipts cannot be provided for this event.



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Attachment(s) from ssteckbeck@yahoo.com [Volcano_Vista_HS] | View attachments on the web

1 of 1 File(s)


Posted by: ssteckbeck@yahoo.com


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




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[Volcano_Vista_HS] VVHS Announcements--Tuesday, September 29, 2015



Congratulations to this week's SOAR drawing winners.  Our staff has recognized the following students for exhibiting Volcano Vista core values - Safety, Organization, Achievement and Respect.  All winners this week receive lunch in the Lava Pit.

 

Marcelo Chavez-  Recognized by Mrs. Prangley

 

Selena Stewart - Recognized by Mr. Gallegos

 

James Anderson  - Recognized by Ms. Phaneuf

 

Nathan Trujillo- Recognized by Ms. Duran

 

Ashlynn Kellerstrass - Recognized by Ms. Minor

 

Jacklyn Gallegos - Recognized by Mrs. Lopez-Leger

 

SENATE: Congratulations to the freshmen who made senate. The list is posted outside the activities office. Your first day of class is Thursday, October 1 at 6:40 in the lecture hall

 

BSU There will be a BSU meeting today during lunch in Room H-206.

 

Wing Squad: There is a meeting this Wednesday the 30th in H107, at lunch. New members are welcome!

ANIME CLUB will meet today at lunch in E-207. Anyone is welcome to attend. 

 

The Volcano Vista Drama Department presents Arthur Miller's The Crucible, a classic play about the Salem Witch Trials, on October 1, 2, and 3. Performances are at 7PM, with a matinee at 2pm on October 3. Tickets are $5 for adults, $3 for students, and $1 for active Thespians.

 

Also in honor of Hispanic Heritage Month, the Spanish Club will be hosting a variety of cultural activities on Tuesdays at lunch from September 29 to October 15.  Meet today on the soccer field to play a short game of fútbol the most popular sport in the Spanish-Speaking world.

 

COUNSELING:

  • A representative from New Mexico State will be on campus Friday October 2nd , at lunch, in lower E-Hall. Stop by to get information about admissions and financial aid.

  • Seniors if you are interested in meeting with a rep from Notre Dame please come to E224 to sign up with Mr. Garcia. Go Irish!!!

  • JUNIORS if you signed up for the PSAT please come pick up a practice booklet today at lunch or after school in E224. Again only JUNIORS who signed up for PSAT. 

 

ATHLETICS

  • There is a mandatory wrestling meeting for all active and perspective wrestling athletes in the wrestling room during lunch today with Coach Crum.

  • BOYS SOCCER plays Cleveland on Wednesday at 3:30. 

  • GIRLS SOCCER plays at Cleveland on Wedensday at 4 

  • VOLLEYBALL plays Cibola tonight at 6:30 in the ring of fire. This is their annual pink-out game

 

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] Rare Video Captures Super-Charged Volcanic Ash Cloud Sparked By Lightning




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



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[Geology2] Pigment from fossils identified, revealing color of extinct animals



Pigment from fossils identified, revealing color of extinct animals

Fossil colors are here to stay

Date:
September 28, 2015
Source:
Virginia Tech
Summary:
Scientists have revealed how pigment can be detected in mammal fossils, a discovery that may end the guesswork in determining the colors of long extinct species.

Caitlin Colleary, a doctoral student of geosciences in the College of Science at Virginia Tech, says the original color patterns of ancient animals can be determined through fossils.
Credit: Virginia Tech

Scientists from Virginia Tech and the University of Bristol have revealed how pigment can be detected in mammal fossils, a discovery that may end the guesswork in determining the colors of extinct species.

The researchers discovered the reddish brown color of two extinct species of bat from fossils dating back about 50 million years, marking the first time the colors of extinct mammals have been described through fossil analysis.

The techniques can be used to determine color from well-preserved animal fossils that are up to 300 million years old, researchers said.

"We have now studied the tissues from fish, frogs, and tadpoles, hair from mammals, feathers from birds, and ink from octopus and squids," said Caitlin Colleary, a doctoral student of geosciences in the College of Science at Virginia Tech and lead author of the study. "They all preserve melanin, so it's safe to say that melanin is really all over the place in the fossil record. Now we can confidently fill in some of the original color patterns of these ancient animals."

The research involved scientists from the U.S., the United Kingdom, Germany, Ethiopia, and Denmark. It is being published this week (Sept. 28) in the Proceedings of the National Academy of Sciences.

The researchers said microscopic structures traditionally believed to be fossilized bacteria are in fact melanosomes -- organelles within cells that contain melanin, the pigment that gives colors to hair, feathers, skin, and eyes.

Fossil melanosomes were first described in a fossil feather in 2008 by Jakob Vinther, a molecular paleobiologist at the University of Bristol and the senior author of the current study.

Since then, the shapes of melanosomes have been used to look at how marine reptiles are related and identify colors in dinosaurs and, now, mammals.

"Very importantly, we see that the different melanins are found in organelles of different shapes: reddish melanosomes are shaped like little meatballs, while black melanosomes are shaped like little sausages and we can see that this trend is also present in the fossils," Vinther said. "This means that this correlation of melanin color to shape is an ancient invention, which we can use to easily tell color from fossils by simply looking at the melanosomes shape."

In addition to shape, melanosomes are chemically distinct.

Using an instrument called a time-of-flight secondary ion mass spectrometer, scientists identified the molecular makeup of the fossil melanosomes to compare with modern melanosomes.

In addition, researchers replicated the conditions under which the fossils formed to identify the chemical alteration of melanin, subjecting modern feathers to high temperatures and pressures to better understand how chemical signatures changed during millions of years of burial.

"By incorporating these experiments, we were able to see how melanin chemically changes over millions of years, establishing a really exciting new way of unlocking information previously inaccessible in fossils, Colleary said.

The work was carried out at the University of Bristol, where Colleary was a master's student working with Vinther, and the University of Texas at Austin. It was supported by funds from UT Austin, National Geographic, and the University of Bristol.

"It was important to bring microchemistry into the debate, because discussion has been going on for years over whether these structures were just fossilized bacteria or specific bodies where melanin is concentrated," said Roger Summons, the Schlumberger Professor of Earth Science at the Massachusetts Institute of Technology, who was not involved in the research. "These two things have very different chemical compositions."

Summons, who was part of a research team that studied fossils of squid to show that ink from the Jurassic period was chemically indistinguishable from modern cuttlefish ink, said the study further helps demonstrate how all living things on Earth have evolved in concert.

"How color is imparted and how we characterize it in fossils are important, because they inform us about a very specific aspect of the history of life on our planet," Summons said. "For complex animal life, color is a factor in how individuals recognize and respond to others, determine friend or foe, and find mates. This research provides another thread to understand how ancient life evolved. Color recognition was an important part of that process, and it goes far back in the history of animals."


Story Source:

The above post is reprinted from materials provided by Virginia Tech. Note: Materials may be edited for content and length.


Journal Reference:

  1. Caitlin Colleary, Andrei Dolocan, James Gardner, Suresh Singh, Michael Wuttke, Renate Rabenstein, Jörg Habersetzer, Stephan Schaal, Mulugeta Feseha, Matthew Clemens, Bonnie F. Jacobs, Ellen D. Currano, Louis L. Jacobs, Rene Lyng Sylvestersen, Sarah E. Gabbott, and Jakob Vinther. Chemical, experimental, and morphological evidence for diagenetically altered melanin in exceptionally preserved fossils. PNAS, September 28, 2015 DOI: 10.1073/pnas.1509831112

Virginia Tech. "Pigment from fossils identified, revealing color of extinct animals: Fossil colors are here to stay." ScienceDaily. ScienceDaily, 28 September 2015. <www.sciencedaily.com/releases/2015/09/150928155852.htm>.

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



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