Friday, August 1, 2014

[Geology2] Stories in Amber



Chinese mosquitoes on the Baltic Sea: Ancient insect inclusions in East-Asian amber

Date:
July 30, 2014
Source:
Universität Bonn
Summary:
The analysis of the roughly 3,000 pieces is still in its infant stage. But it is already evident that the results will be of major significance. The Baltic amber comes from the Baltic Sea region, which is almost 10,000 kilometers from Fushun. Sites rich in finds are, e.g., the coastal regions of Mecklenburg, Poland and Belarus. The pieces from the Baltic region are slightly younger than the ones from Fushun–according to estimates, about 40 to 50 million years.

Golden coffin: An insect is trapped in Fushun amber.
Credit: Copyright Bo Wang / Universität Bonn



The analysis of the roughly 3,000 pieces is still in its infant stage. But it is already evident that the results will be of major significance. "Amazingly often, we are finding-in addition to Asian forms-the same insect species in Fushun amber that we found in Baltic amber," explained Bonn paleontologist Professor Dr. Jes Rust.

The Baltic amber comes from the Baltic Sea region, which is almost 10,000 kilometers from Fushun. Sites rich in finds are, e.g., the coastal regions of Mecklenburg, Poland and Belarus. The pieces from the Baltic region are slightly younger than the ones from Fushun-according to estimates, about 40 to 50 million years. At that time, Europe and Asia were divided by the Strait of Turgay, a wide arm of the ocean. Many researchers had assumed until now that this body of saltwater prevented species migrations between the continents-or at least, made it much harder. "Consequently, the great similarity of the included insects has been a great surprise to us," said Rust. "We don't know yet how that fits together."

A neglected treasure

In the vicinity of the Northeast Chinese city of Fushun, there are large lignite deposits. Humans have been digging up this fuel from the ground for more than a century already. And in doing so, they also kept finding pieces of amber. Traditionally, the locals made jewelry from it. Particularly beautiful finds with interesting inclusions are highly sought after among collectors.

Until now, the inclusions had not been studied systematically. It was the Chinese paleontologist Dr. Bo Wang who finally recognized the scientific potential of Fushun amber. Wang, who is currently at the Bonn University on a research grant from the Alexander von Humboldt Foundation, used his good contacts with institutes and collectors to start systematically cataloguing the finds. An analysis is currently underway in collaboration with paleontologists from Europe and the USA.

And it is beginning to become clear how rich this deposit is. So far, the researchers have been able to identify arachnids and insects from more than 80 families-a snapshot of the past that provides a detailed view of what tiny animals populated East Asia 53 million years ago.

In addition, the Fushun deposit is filling in one of the blank spots on the map. With the exception of India, it constitutes the only significant site where amber has been found in Asia. Rust regrets that the open pit mining in Fushun will soon stop. "But despite that, the detailed analysis of the finds will probably keep us busy for quite some time."


Story Source:

The above story is based on materials provided by Universität Bonn. Note: Materials may be edited for content and length.


Journal Reference:

  1. Bo Wang, Jes Rust, Michael S. Engel, Jacek Szwedo, Suryendu Dutta, André Nel, Yong Fan, Fanwei Meng, Gongle Shi, Edmund A. Jarzembowski, Torsten Wappler, Frauke Stebner, Yan Fang, Limi Mao, Daran Zheng, Haichun Zhang. A Diverse Paleobiota in Early Eocene Fushun Amber from China. Current Biology, 2014; 24 (14): 1606 DOI: 10.1016/j.cub.2014.05.048


Universität Bonn. "Chinese mosquitoes on the Baltic Sea: Ancient insect inclusions in East-Asian amber." ScienceDaily. ScienceDaily, 30 July 2014. <www.sciencedaily.com/releases/2014/07/140730093827.htm>.

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Decades-old amber collection offers new views of a lost world: Tiny grasshopper encased in amber

Date:
July 30, 2014
Source:
University of Illinois at Urbana-Champaign
Summary:
Scientists are searching through a massive collection of 20-million-year-old amber found in the Dominican Republic more than 50 years ago, and the effort is yielding fresh insights into ancient tropical insects and the world they inhabited. Perhaps the most striking discovery thus far is that of a pygmy locust, a tiny grasshopper the size of a rose thorn that lived 18- to 20-million years ago and fed on moss, algae and fungi.

A specimen from the 20-million-year-old amber collection at the Illinois Natural History Survey at Illinois.
Credit: Photo courtesy of Kaitlin and Kevin Southworth



Scientists are searching through a massive collection of 20-million-year-old amber found in the Dominican Republic more than 50 years ago, and the effort is yielding fresh insights into ancient tropical insects and the world they inhabited.

When the collection is fully curated, a task that will take many years, it will be the largest unbiased Dominican amber collection in the world, the researchers report.

Perhaps the most striking discovery thus far is that of a pygmy locust, a tiny grasshopper the size of a rose thorn that lived 18- to 20-million years ago and fed on moss, algae and fungi. The specimen is remarkable because it represents an intermediate stage of evolution in the life of its subfamily of locusts (known as the Cladonotinae). The most ancient representatives of this group had wings, while modern counterparts do not. The newly discovered locust has what appear to be vestigial wings -- remnant structures that had already lost their primary function.

The discovery is reported in the journal ZooKeys.

"Grasshoppers are very rare in amber and this specimen is extraordinarily well-preserved," said Sam Heads, a paleontologist at the Illinois Natural History Survey, a division of the Prairie Research Institute at the University of Illinois.

Heads, laboratory technician Jared Thomas and study co-author Yinan Wang found the new specimen a few months after the start of their project to screen more than 160 pounds of Dominican amber collected in the late 1950s by former INHS entomologist Milton Sanderson. Sanderson described several specimens from the collection in a paper in Science in 1960, a report that inspired a generation of scientists to seek out and study Dominican amber, Heads said.

The bulk of the Sanderson amber collection remained in storage, however, until Heads uncovered it in 2010.

Heads has named the new pygmy locust Electrotettix attenboroughi, the genus name a combination of electrum (Latin from Greek, meaning "amber") and tettix (Greek, meaning "grasshopper"). The species is named for Sir David Attenborough, a British naturalist and filmmaker (not to be confused with Richard Attenborough, David's actor brother who appeared in the movie "Jurassic Park").

"Sir David has a personal interest in amber, and also he was one of my childhood heroes and still is one of my heroes and so I decided to name the species in his honor -- with his permission of course," Heads said. (Attenborough narrates and appears in a new video about the Sanderson collection and the specimen that bears his name.)

The process of screening the amber is slow and painstaking. Much of the amber is clouded with oxidation, and the researchers must carefully cut and polish "windows" in it to get a good look at what's inside. In addition to the pygmy locust, Heads and his colleagues have found mating flies, stingless bees, gall midges, Azteca ants, wasps, bark beetles, mites, spiders, plant parts and even a mammal hair.

The pygmy locust was found in a fragment that also contained wasps, ants, midges, plant remnants and fungi. Such associations are rich in information, Heads said, offering clues about the creatures' physiological needs and the nature of their habitat.

"Fossil insects can provide lots of insight into the evolution of specific traits and behaviors, and they also tell us about the history of the time period," Heads said. "They're a tremendous resource for understanding the ancient world, ancient ecosystems and the ancient climate -- better even, perhaps, than dinosaur bones."

The National Science Foundation supports this work. Heads and his colleagues are digitizing the best specimens, and will upload the images onto a publicly available website.


Story Source:

The above story is based on materials provided by University of Illinois at Urbana-Champaign. Note: Materials may be edited for content and length.


Journal Reference:

  1. Sam Heads, M. Thomas, Yinan Wang. A remarkable new pygmy grasshopper (Orthoptera, Tetrigidae) in Miocene amber from the Dominican Republic. ZooKeys, 2014; 429: 87 DOI: 10.3897/zookeys.429.8020


University of Illinois at Urbana-Champaign. "Decades-old amber collection offers new views of a lost world: Tiny grasshopper encased in amber." ScienceDaily. ScienceDaily, 30 July 2014. <www.sciencedaily.com/releases/2014/07/140730104138.htm>.



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



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[Geology2] Antarctic ice sheet is result of carbon dioxide decrease, not continental breakup



Antarctic ice sheet is result of carbon dioxide decrease, not continental breakup

Date:
July 30, 2014
Source:
University of New Hampshire
Summary:
Climate modelers have shown that the most likely explanation for the initiation of Antarctic glaciation during a major climate shift 34 million years ago was decreased carbon dioxide levels. The finding counters a 40-year-old theory suggesting massive rearrangements of Earth's continents caused global cooling and the abrupt formation of the Antarctic ice sheet. It will provide scientists insight into the climate change implications of current rising global carbon dioxide levels.

Antarctic Peninsula.
Credit: © adfoto / Fotolia


Climate modelers from the University of New Hampshire have shown that the most likely explanation for the initiation of Antarctic glaciation during a major climate shift 34 million years ago was decreased carbon dioxide (CO2) levels. The finding counters a 40-year-old theory suggesting massive rearrangements of Earth's continents caused global cooling and the abrupt formation of the Antarctic ice sheet. It will provide scientists insight into the climate change implications of current rising global CO2 levels.

In a paper published today in Nature, Matthew Huber of the UNH Institute for the Study of Earth, Oceans, and Space and department of Earth sciences provides evidence that the long-held, prevailing theory known as "Southern Ocean gateway opening" is not the best explanation for the climate shift that occurred during the Eocene-Oligocene transition when Earth's polar regions were ice-free.

"The Eocene-Oligocene transition was a major event in the history of the planet and our results really flip the whole story on its head," says Huber. "The textbook version has been that gateway opening, in which Australia pulled away from Antarctica, isolated the polar continent from warm tropical currents, and changed temperature gradients and circulation patterns in the ocean around Antarctica, which in turn began to generate the ice sheet. We've shown that, instead, CO2-driven cooling initiated the ice sheet and that this altered ocean circulation."

Huber adds that the gateway theory has been supported by a specific, unique piece of evidence -- a "fingerprint" gleaned from oxygen isotope records derived from deep-sea sediments. These sedimentary records have been used to map out gradient changes associated with ocean circulation shifts that were thought to bear the imprint of changes in ocean gateways.

Although declining atmospheric levels of CO2 has been the other main hypothesis used to explain the Eocene-Oligocene transition, previous modeling efforts were unsuccessful at bearing this out because the CO2 drawdown does not by itself match the isotopic fingerprint. It occurred to Huber's team that the fingerprint might not be so unique and that it might also have been caused indirectly from CO2 drawdown through feedbacks between the growing Antarctic ice sheet and the ocean.

Says Huber, "One of the things we were always missing with our CO2 studies, and it had been missing in everybody's work, is if conditions are such to make an ice sheet form, perhaps the ice sheet itself is affecting ocean currents and the climate system -- that once you start getting an ice sheet to form, maybe it becomes a really active part of the climate system and not just a passive player."

For their study, Huber and colleagues used brute force to generate results: they simply modeled the Eocene-Oligocene world as if it contained an Antarctic ice sheet of near-modern size and shape and explored the results within the same kind of coupled ocean-atmosphere model used to project future climate change and across a range of CO2 values that are likely to occur in the next 100 years (560 to 1200 parts per million).

"It should be clear that resolving these two very different conceptual models for what caused this huge transformation of the Earth's surface is really important because today as a global society we are, as I refer to it, dialing up the big red knob of carbon dioxide but we're not moving continents around."

Just what caused the sharp drawdown of CO2 is unknown, but Huber points out that having now resolved whether gateway opening or CO2 decline initiated glaciation, more pointed scientific inquiry can be focused on answering that question.

Huber notes that despite his team's finding, the gateway opening theory won't now be shelved, for that massive continental reorganization may have contributed to the CO2 drawdown by changing ocean circulation patterns that created huge upwellings of nutrient-rich waters containing plankton that, upon dying and sinking, took vast loads of carbon with them to the bottom of the sea.


Story Source:

The above story is based on materials provided by University of New Hampshire. Note: Materials may be edited for content and length.


Journal Reference:

  1. A. Goldner, N. Herold, M. Huber. Antarctic glaciation caused ocean circulation changes at the Eocene–Oligocene transition. Nature, 2014; 511 (7511): 574 DOI: 10.1038/nature13597


University of New Hampshire. "Antarctic ice sheet is result of carbon dioxide decrease, not continental breakup." ScienceDaily. ScienceDaily, 30 July 2014. <www.sciencedaily.com/releases/2014/07/140730141020.htm>.

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



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[californiadisasters] On This Date In California Weather History (August 1)



2003: Thunderstorms developed in the Borrego Valley and dropped an estimated 2.5" to 3'' of rain in 2 hours.
Flash flooding occurred, including 4' of water running in San Felipe Wash.
One car and family were stranded in Borrego Palm Canyon.
Half of Ocotillo Wells Airport runway was inundated and debris was deposited on Hwy. 78.

2000: Thunderstorms produced heavy rain and gusty winds as well as golf ball size hail about 6 miles east of Tehachapi.

2000: A thunderstorm dropped half inch hail on Lake Arrowhead.

2000: The high temperature at Hawthorne, NV, was 104° F.

1993: It was an amazing 123° in Palm Springs, the highest temperature on record.
This also occurred on 7.28 and 7.29 of 1995, and on 7.10.1979.

1986: Fresno had a low of 86°, its' highest minimum temperature on record for the month of August.

1983: A tornado in Landers caused property damage.

1977: Susanville had a high temperature of 105° F.

1972:
It was 100° F in Palomar Mountain (San Diego Co.), the highest temperature on record.
This also occurred on eight other days.

1930: 2.03" of rain fell in Palm Springs, the greatest daily amount for August.

1900: Santa Cruz hit 108° F, tying its all-time record which was also set on September 7, 1904.

Source: NWS San Francisco/Monterey, Hanford, Reno, & San Diego

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Posted by: Kim Noyes <kimnoyes@gmail.com>


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[Geology2] Ostensibly For Hawaii But Relevant In California, Too!



Prepare for Earthquakes & Tsunamis in Hawaii

https://www.youtube.com/watch?v=S7PHtsocXCA




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Posted by: Kim Noyes <kimnoyes@gmail.com>



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[Geology2] Australian volcanoes form case study for dating technique



Australian volcanoes form case study for dating technique

Jul 31, 2014 by Geoff Vivian
Australian volcanoes form case study for dating technique
The Blue Lake occupies one of the craters of Mount Gambier and famously changes colour each year, going from a dull grey to a vibrant blue. Credit: Keith McGann

Volcanos in south-eastern Australia are still considered active, and a PhD candidate is hoping to determine whether we might expect more eruptions any time soon.

The Newer Volcanics Province includes more than 400 volcanoes, stretching from the Central Highlands north of Melbourne to South Australia's Mount Gambier district.

Curtin University Geologist and PhD candidate Korien Oostingh says it is a very young geological province.

"It started erupting 4.6 million years ago and the last eruption [at Mount Gambier] is actually thought to have been witnessed by Aboriginal people around 5,000 years ago," she says.

She is using the province as a case study as she develops a new technique that makes use of cosmogenic radiation for dating purposes.

Ms Oostingh has travelled to many locations throughout the Newer Volcanics Province, collecting samples that she is subjecting to tests at Curtin University's Argon Laboratory.

"I'm looking at olivine in basalts," she says.

"Part of the calcium in olivine will be converted into an isotope of Argon, [Argon 38] that we can measure here for the first time quite reliably in Curtin University.

"I will also combine that with chemistry data on the rocks from the new volcanic province so that I can look at some trends in the area and hopefully answer two big questions.

"One of them is if we can expect new eruptions in an area in the near future.

"Also, where the basalts were actually coming from at some point, so what is the source in the deep sub-surface?"

The province is more than 2000km from the edge of the Australian tectonic plate.

Ranging theories behind region's volcanic activity

She says there are two current hypotheses proposed to explain this "intra-plate" volcanism.

"One possibility is that it is caused by the principle of a mantle plume," she says.

"A is rising magma from very deep in the earth—a little bit like if you are making a soup, the very hot material in the middle starts to rise.

"Very hot magma rises in pockets and it all starts to rise to the surface and creates a volcanic province or volcano.

"Some other people propose some local inhomogeneities in the underlying mantle."

Ms Oostingh says she is not yet inclined to support either hypothesis.

"I am hoping to gain completely new data and to put forward my own model, I will do some advanced modelling here," she says.

Explore further: New volcanos found in Victoria

Provided by Science Network WA search and more info website

http://phys.org/news/2014-07-australian-volcanoes-case-dating-technique.html
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Posted by: Lin Kerns <linkerns@gmail.com>



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[Geology2] Research team sets out for Islands of the Four Mountains



Research team sets out for Islands of the Four Mountains

By KTOO News Department
Posted on July 30, 2014

Estimated reading time: 3 minutes, 13 seconds

The Islands of the Four Mountains as seen from the International Space Station in 2013. Cleveland Volcano is at center. (Photo courtesy NASA)

The Islands of the Four Mountains as seen from the International Space Station in 2013. Cleveland Volcano is at center. (Photo courtesy NASA)

A group of researchers left Unalaska this past weekend for a remote part of the central Aleutians: the Islands of the Four Mountains.

The 16 scientists are beginning a three-year mission in territory that's unpredictable — and largely unexplored.

Weather was clear and sunny in Dutch Harbor on Saturday while the research team loaded up their charter vessel with food and supplies. As most of them know from experience in this part of Alaska, conditions can change in an instant.

Still, lead archaeologist Dixie West was hoping for the best.

"I'm expecting fair skies and wonderful winds, and that we're going to find some exciting information about how volcanic impacts and tsunamis impacted prehistoric humans," she said, standing on the spit dock Saturday afternoon.

West works with the University of Kansas. She headed out to the uninhabited Islands of the Four Mountains on Sunday — with her, a group of experts who study volcanoes, tsunamis, earthquakes, climate and biology and prehistoric settlements.

This will be the first year of a three-year expedition, funded in part by the National Science Foundation. Next year is more field work, and in year three, they'll write up their findings.

West and the others will stage their research on Chuginadak Island, near one of the most active volcanoes in the Aleutian chain — Mt. Cleveland. They'll be working in the volcano's shadow, studying how prehistoric Unangan peoples might have lived there.

"So hopefully we'll be able to add something to modern information about how people should expect volcanoes to behave, and how possibly better to react to them," she said.

Most of the researchers took a boat to the island group. A few followed by helicopter — the same one that'll transport them between the ship and the island's shore, since there isn't a dock in the Islands of the Four Mountains.

One who went on the chopper is Max Kaufman, a research technician with the Alaska Volcano Observatory. He's going to help install seismometers on Cleveland Volcano for the first time.

"Getting these stations in will really help us understand its sort of background behavior," he said on Saturday.

And through their work, he said, they also "hope to provide some degree of safety for the crew working out there, doing the archaeological studies" — because, he says, you never know when the volcano might wake up. It's been a little restless in recent days, but Kaufman's hoping it'll stick to its usual low-level behavior.

Still, he admitted that the Islands of the Four Mountains are a bit of a daunting destination.

"It seems quite remote, despite its proximity to Dutch Harbor," he laughed.

So Kaufman and the other researchers will have to be ready for anything the islands throw at them — and so will the crew of their charter vessel, the Maritime Maid. It's been used for scientific charters before. Skipper George Rains says he's used to navigating the Aleutians' tricky coastlines.

"It's a challenge — it's always probably been a challenge, from the days the natives were out there," Rains said as he stood in the wheelhouse of the Maritime Maid. "But basically, you just have to be careful of the weather, move around and stay out of it."

Twelve members of the team can stay aboard the ship, while the rest will be camping on shore. Most of them will stay out on-site for next three weeks — hoping to start uncovering some of the mysteries that the Islands of the Four Mountains have in store.

You can follow the researchers' progress on Facebook, or on Twitter @Islandsof4Mtns.

http://www.ktoo.org/2014/07/30/research-team-sets-islands-four-mountains/

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



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[Geology2] Mystery crater in Yamal peninsula probably caused by methane release



Jul 31, 2014

Mystery crater in Yamal peninsula probably caused by methane release

Thawing permafrost likely allowed methane gas to be released, creating the large hole in permafrost found in northern Russia, says the Russian team that investigated it.

The first mysterious crater spotted by helicopter in the Yamal region of northern Russia.  Image via Nature.

The first mysterious crater spotted by helicopter in the Yamal region of northern Russia. Image via Nature.

UPDATE July 31, 2014. Stories are popping up fast in various media this afternoon about a likely source of a reported, mysterious hole in permafrost in the Yamal region of northern Russia. This hole was spotted by a helicopter pilot in mid-July; reindeer herders reported a second hole some days later. Eric Holthaus of Slate said that there is now:

… new (and definitive) evidence … that the Siberian holes were created via methane released from warming permafrost.

The evidence has come via the journal Nature, which published a story on its website today (July 31) featuring the findings of Andrei Plekhanov, a senior researcher at the Scientific Centre of Arctic Studies in Salekhard, Russia, and his team. This is the team that was sent in to investigate the first hole shortly after it was found. Holthaus said:

That team measured methane concentrations up to 50,000 times standard levels inside the crater.

The story in Nature said:

Air near the bottom of the crater contained unusually high concentrations of methane — up to 9.6% — in tests conducted at the site on 16 July … Plekhanov, who led an expedition to the crater, says that air normally contains just 0.000179% methane …

Plekhanov and his team believe that it is linked to the abnormally hot Yamal summers of 2012 and 2013, which were warmer than usual by an average of about 5°C. As temperatures rose, the researchers suggest, permafrost thawed and collapsed, releasing methane that had been trapped in the icy ground.

Holthaus pointed out:

Last week, the New York Times' Andrew Revkin interviewed a Russian scientist who had also visited the hole and came to similar conclusions.

This newly reported evidence, just coming to light today, seems particularly scary given the story earlier this week about what the University of Stockholm called "vast methane plumes" found by scientists aboard the icebreaker Oden, which is now exploring and measuring methane release from the floor of the Arctic Ocean.

Read more: Scientists discover vast methane plumes escaping from Arctic seafloor

Andrei Plekhanov, senior researcher at the Scientific Research Centre of the Arctic, stands at the first large crater, discovered recently in the Yamalo-Nenets Autonomous Okrug region of northern Russia.  Image via China Post.

Andrei Plekhanov, senior researcher at the Scientific Research Centre of the Arctic, stands at the first large crater, discovered recently in the Yamalo-Nenets Autonomous Okrug region of northern Russia. Image via China Post.

Helicopters found the first crater.  Reindeer herders report a second.  Photo of first crater via Siberian Times.

Helicopters found the first crater. Reindeer herders reported a second. Photo of first crater via Siberian Times.

The Moscow Times reported this week that reindeer herders in far northern Russia have found a second mysterious giant hole. According to these unconfirmed reports, the second hole is about 30 kilometers (20 miles) away from a first large and mysterious hole in the Russian permafrost, which made a big splash in social media after the Siberian Times reported it in mid-July 2014.

Last week, Russian scientists estimated the first hole, which has smooth sides and a lake at its bottom, to be around 30-60 meters wide (100-200 feet) wide. The second crater is said to be smaller than the first, only about 15 meters (50 feet) wide, and it's reported to be filled with snow.

Both craters (assuming two exist) are located within the permafrost of the Yamalo-Nenets Autonomous Area (YNAO) of the Russian Arctic. Moscow Times said that both craters appear to have formed relatively recently.

In fact, according to the website Russia Behind the Headlines, the time of formation of the second crater might be known, from reports last year by reindeer herders. This website said the second crater might have formed in September 2013. Russia Behind the Headlines said:

News of the crater was first spread by local reindeer herders, who said a celestial body had fallen and then a flash had occurred on 27 September 2013 in this region (56 miles from the village of Antipayut).

A different reindeer herder only said that he saw smoke, haze, and then a flash.

The walls of the crater appear evenly cut.

Here is the first crater again. Its walls appear evenly cut, and there is water, from melting permafrost, cascading down their sides. Photo by Andrey-Naumenko via Siberian Times.

The crater, which is 70 meters deep, has an icy lake at its bottom.  Photo by Andrey-Naumenko via Siberian Times.

The first crater appears to be about 70 meters deep. It has an icy lake at its bottom. Photo by Andrey-Naumenko via Siberian Times.

Both Moscow Times and Russia Behind the Headlines seem to be favoring the idea that the mysterious holes in permafrost formed due to a geophysical process associated with global warming. Russia Behind the Headlines said:

The strange holes in the Earth found in the northern tundra on Russian territory in July could mean the beginning of irreversible changes in the climate of our planet. According to Russian scientists, the most likely reason for the formation of such holes is the emission of natural gas, which may be caused by global warming …

Glaciologists from the sub-Arctic research and study unit in Tyumen say that permafrost temperatures are rising steadily in the region of the Bovanenkovskoye gas field on the Yamal Peninsula in the Russian Arctic, near where the first hole was discovered. Forty years ago it was on average about eight degrees below zero, but now in certain areas it is only minus three.

Moscow Times said:

Scientists who examined the first hole theorized that it could have been created when a mixture of water, salt and gas exploded underground …

The area, which has one of Russia's richest deposits of natural gas, was covered by sea about 10,000 years ago, and vast salt deposits were left behind.

Moscow Times added that:

Global warming, causing an alarming melt in the ice under the soil, released gas causing an effect like the popping of a champagne cork.

Approximate location of mysterious craters in the Yamalo-Nenets Autonomous Area (YNAO) in the Russian Arctic.

Approximate location of two reported large holes in the permafrost in the Yamalo-Nenets Autonomous Area (YNAO) in the Russian Arctic.

Bottom line: A second mysterious crater has been found on the Yamal region of northern Russia, according to media reports.

http://earthsky.org/earth/second-mysterious-crater-reported-from-yamal?utm
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