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terça-feira, 13 de setembro de 2011

Planet Earth under attack?

       
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Earth Day                                                                                                                            
RUI SANTOS DE SOUZA
Brazil, Curitiba, September 13, 2011 - 22h: 17

domingo, 17 de julho de 2011

What keeps the Earth cooking? @BreakingScience

>> What keeps the Earth cooking? << via

http://www.physorg.com/

physorg — What spreads the sea floors and moves the continents? What melts iron in the outer core and enables the Earth's magnetic field? Heat. Geologists have used temperature measurements from more than 20,000 boreholes around the world to estimate that some 44 terawatts (44 trillion watts) of heat continually flow from...

terça-feira, 12 de julho de 2011

"worms from hell." @physorg via @BreakingScience

Onstott's discovery of worms in Earth's depths raises questions about life in space via


physorg — After digging holes in the Earth's crust for nearly two decades, Princeton University geoscientist Tullis Onstott is now making headlines for unearthing "worms from hell."


Onstott's discovery of worms in Earth's depths raises questions about life in space

July 12, 2011 By Nick DiUlio


http://www.physorg.com/


The species of nematode discovered by Onstott's research team can tolerate very high temperatures, reproduce asexually and feed on bacteria from the subsurface. It's a degree of unprecedented complexity that has prompted Onstott to say that finding these nematodes at such depths was akin to "finding Moby Dick in Lake Ontario." Credit: Gaetan Borgonie

After digging holes in the Earth's crust for nearly two decades, Princeton University geoscientist Tullis Onstott is now making headlines for unearthing "worms from hell."

Onstott's research team, which he led with Gaetan Borgonie of the University of Ghent in Belgium, recently made a startling discovery: microscopic roundworms known as nematodes living nearly two-and-a-half miles beneath the Earth's surface in several South African . The worms are roughly a quarter of the diameter of the head of a pin. Although have been known to live as far as 20 feet below the surface, scientists generally assumed there was no reason to believe the organisms would be found anywhere near the depths of those found by Onstott's team, he noted.

The discovery, which was published in the June 2 issue of the journal Nature in an article titled "Nematoda From the Terrestrial Deep Subsurface of South Africa," has attracted the attention of national media outlets such as The Washington Post, National Geographic and Time. Moreover, it has raised questions about not only the possibility of even more complex organisms miles below the Earth's surface, but also the likelihood of far into space.

"The potential to look for alien exists, in a way, right here on Earth," said Onstott, a professor of geosciences who joined the Princeton faculty in 1985. "What we're looking for are 'extremophiles' deep within the Earth, living in an environment that could also occur on other planets."

This particular extremophile -- a word used to describe forms of found in habitats previously thought uninhabitable -- is remarkable not only for the depth at which it was found, but also for its .

A wide range of previously has been known to thrive as far down as these worms. It was thought, however, that the constraints of temperature, energy, oxygen and space would make it impossible for a multicellular organism to live in such a place. These half-millimeter-long worms can apparently tolerate very high temperatures, prompting the researchers to nickname them "worms from hell." The worms also reproduce asexually and feed on bacteria from the subsurface. Given their size, Onstott said that finding these nematodes at such depths was akin to "finding Moby Dick in Lake Ontario."

Immersed in explorations below the Earth

An explorer at heart, Onstott has been searching for this type of biological revelation ever since he was "bitten badly by the subsurface bug" as an associate professor of geosciences at Princeton in 1994. That year he was first introduced to the strange world of deep, subsurface bacteria, and less than two years later he found himself thoroughly immersed in microbiology, plunging far beneath the Earth's surface on what he likes to call "underground safaris."

It's ironic that Onstott developed such passion for the underground world, considering that since he was a boy growing up in New Mexico he only ever wanted to go into space. In high school, shortly after watching Apollo 8 launch from the Kennedy Space Center on television in 1968, Onstott read Carl Sagan's "Intelligent Life in the Universe." The book had a significant impact on him, and he was convinced he'd become an interstellar expert once he graduated.

Enduring 90-plus degree temperatures, Onstott turns a valve while working at a depth of more than three kilometers in a South African gold mine where he found the subterranean roundworms. Credit: Lisa Pratt

While earning his bachelor's degree at the California Institute of Technology in the mid-1970s, however, Onstott's interests veered away from planetary science and toward geophysics. By the time he started working on his Ph.D. at Princeton, which he completed in 1980, Onstott no longer saw space -- or Mars in particular -- as a viable avenue of research.

"I was very much interested in traveling to other countries," Onstott recalled. "I couldn't very well travel to Mars, could I?"

However, what fueled Onstott's passion for the deepest of subsurface extremophiles was, more or less, the same question that fueled his fascination with space: He wanted to know how it's possible for life to exist in conditions so radically different from those on the surface of the Earth.

"Finding any life form in a strange place where normal people don't go and you would never expect to find it? That's always going to be something that appeals to the imagination," Onstott said. "It's almost science fiction in that regard. The search for life in these strange environments itself is something that broadens human perspective on life, and that's very important in helping us better understand how life evolves and how bizarre life can be."

Digging for further answers

The last 15 years of Onstott's subterranean explorations, research and study have taken him to myriad locales across the globe. Not only does he frequent the gold mines of South Africa -- where temperatures often approach 95 very humid degrees -- he has also taken several trips to the gold mines of Canada, where the warm air from the Earth's depths collides so quickly with sub-freezing surface temperatures that "snowflakes the size of chandeliers" form inside the mine, he said.

This, too, made Onstott think of Mars, where the conditions match those of the Canadian mines quite remarkably in certain spots.

"Everything is frozen on the Martian surface, but you go down a half-kilometer or so and things get warmer," said Onstott. "Also, you have caves on Mars where water might have risen through evaporation and frozen and crystalized. That's where you want to go looking for life on Mars."

Even though he still remains interested in space, Onstott is particularly excited to see how the discovery of these "worms from hell" further informs scientists' understanding of this planet. For instance, Onstott wants to figure out what relationship these South African nematodes -- dubbed Halicephalobus mephisto in honor of the sinister, darkness-loving demon Mephistopheles of literary lore -- may have with subsurface radiation as a means of energy.

Onstott would also like to complete the gene sequence for H. mephisto and compare it to the genomes of closely related species found near the surface of the mines. This should give him a better sense of whether or not the nematode has adapted or evolved in the subsurface, and help him answer the pressing question of whether or not life can originate so far down, he said.

Questions like these are what compel Onstott to go even deeper, continually plunging himself ever further into the shrouded mysteries of the Earth's black, sweltering, sunless interior.

"We still don't know how far down the biosphere goes," Onstott said. "We have an expectation that it stops at a certain temperature, but we haven't found that particular boundary yet. And if we do, the next question becomes: What lies beyond that?"

Provided by Princeton University (news : web)



quarta-feira, 6 de julho de 2011

New force driving Earth's tectonic plates @BreakingScience

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New force driving Earth's tectonic plates discovered via


New force driving Earth's tectonic plates discovered


physorg — Bringing fresh insight into long-standing debates about how powerful geological forces shape the planet, from earthquake ruptures to mountain formations, scientists at Scripps Institution of Oceanography at UC San Diego have identified a new mechanism driving Earth's

http://www.physorg.com/

A view of the bends of the fracture zones on the Southwest Indian Ridge caused by the slowdown of Africa in response to the Reunion plume head. The image shows the gravity field. Credit: Scripps Institution of Oceanography,UC San Diego
Bringing fresh insight into long-standing debates about how powerful geological forces shape the planet, from earthquake ruptures to mountain formations, scientists at Scripps Institution of Oceanography at UC San Diego have identified a new mechanism driving Earth's massive tectonic plates.

Scientists who study tectonic motions have known for decades that the ongoing "pull" and "push" movements of the plates are responsible for sculpting continental features around the planet. Volcanoes, for example, are generally located at areas where plates are moving apart or coming together. Scripps scientists Steve Cande and Dave Stegman have now discovered a new force that drives plate tectonics: Plumes of hot magma pushing up from Earth's deep interior. Their research is published in the July 7 issue of the journal Nature.
Using analytical methods to track plate motions through Earth's history, Cande and Stegman's research provides evidence that such mantle plume "hot spots," which can last for tens of millions of years and are active today at locations such as Hawaii, Iceland and the Galapagos, may work as an additional tectonic driver, along with push-pull forces.

Reconstruction of the Indo-Atlantic Ocean at 63 million years, during the time of the superfast motion of India which Scripps scientists attribute to the force of the Reunion plume head. The arrows show the relative convergence rate of Africa (black arrows) and India (dark blue) relative to Eurasia before, during and after (from left to right) the period of maximum plume head force. The jagged red and brown lines northeast of India show two possible positions of the trench (the subduction zone) between India and Eurasia depending on whether the India-Eurasia collision occurred at 52 million years or 43 million years. Credit: Scripps Institution of Oceanography, UC San Diego
Their new results describe a clear connection between the arrival of a powerful mantle plume head around 70 million years ago and the rapid motion of the Indian plate that was pushed as a consequence of overlying the plume's location. The arrival of the plume also created immense formations of volcanic rock now called the "Deccan flood basalts" in western India, which erupted just prior to the mass extinction of dinosaurs. The Indian continent has since drifted north and collided with Asia, but the original location of the plume's arrival has remained volcanically active to this day, most recently having formed Réunion island near Madagascar.
The team also recognized that this "plume-push" force acted on other tectonic plates, and pushed on Africa as well but in the opposite direction.
"Prior to the plume's arrival, the African plate was slowly drifting but then stops altogether, at the same time the Indian speeds up," explains Stegman, an assistant professor of geophysics in Scripps' Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics. "It became clear the motion of the Indian and African plates were synchronized and the Réunion hotspot was the common link."

Images of the satellite derived gravity field over the Central Atlantic (top) and Southwest Indian Ridge (right) showing the zones of rough topography and sharp bends in the fracture zones that were caused by the slowing of Africa's motion as the Reunion plume head reached its maximum force. The inset globe shows the location of the gravity maps as well as the extent of the parallel zones of rough topography (outlined in red) on the flanks of the Mid-Atlantic and Southwest Indian ridges caused by the change in Africa's motion. Credit: Scripps Institution of Oceanography, UC San Diego
After the force of the plume had waned, the African plate's motion gradually returned to its previous speed while India slowed down.
"There is a dramatic slow down in the northwards motion of the Indian plate around 50 million years ago that has long been attributed to the initial collision of India with the Eurasian plate," said Cande, a professor of marine geophysics in the Geosciences Research Division at Scripps. "An implication of our study is that the slow down might just reflect the waning of the mantle plume-the actual collision might have occurred a little later."
Provided by University of California - San Diego (news : web)