A new study by MIT researchers uncovers evidence that more than a quadrillion tons of diamonds are located in the Earth’s upper mantle, reports Katie Camero for The Boston Globe. Camero explains that, “researchers came to this conclusion after they found in global records over the past few decades a ‘glitch’ in seismic wave activity.”
A team including MIT research scientist Ulrich Faul has discovered that the Earth’s interior contains 1,000 times more diamonds than was previously thought, writes Sarah Emerson for Motherboard. The researchers believe that one to two percent of “craton roots,” which are the deepest sections of the “rock layers extending upwards of 200 miles through the Earth’s crust and mantle,” may contain diamonds.
MIT researchers have discovered a cache of diamonds below the surface of the Earth, deeper than any drilling expedition has ventured, reports the Agence France-Presse wire. This discovery was made after “scientists were puzzled by observations that sound waves would speed up significantly when passing through the roots of ancient cratons.”
Using “recorded sound waves from seismic activity like earthquakes and tsunamis,” MIT researchers have found that there may be a quadrillion tons of diamonds under the Earth’s surface, reports Sarah Gray for Fortune. The seismic data provided this information, “because the speed of sound waves changes depending on the temperature, density and composition of the earth they travel through,” explains Gray.
MIT research scientist Ulrich Faul used seismic data to determine that there may be diamonds underneath the Earth’s surface. “Located over 100 miles below Earth's tectonic plates are ancient, hard rocks called ‘cratonic roots’ that potentially consist of one to two percent diamond — totaling a quadrillion tons,” writes Lilly Price for USA Today.
A study led by MIT research scientist Ulrich Faul finds that diamonds are about 1,000 times more common in the Earth than previously thought, report Ayana Archie and Ralph Ellis for CNN. “The deposits sit some 90 to 150 miles below the Earth's surface, much deeper than current mining machinery allows,” write Archie and Ellis.
By using sound waves, MIT researchers have discovered that part of Earth’s stable crust may contain diamonds, reports Abbey Interrante for Newsweek. “This shows that diamond is not perhaps this exotic mineral, but on the [geological] scale of things, it’s relatively common,” says research scientist Ulrich Faul.
Writing in The Boston Globe, Elise Takahama describes new research by MIT’s Sukrit Ranjan and colleagues that suggests sulfudic anion molecules provide evidence for the origins of life. Takahama also highlights the varying disciplines in the research team, which joined molecular chemistry experts with planetary scientists. “One of the most exciting things,” says Ranjan, is “how different communities, when they talk to each other, can really make dramatic advances.”
A study by MIT researchers examines molecules present in the early atmosphere to better understand how living things came into existence, reports David Grossman of Popular Mechanics. “Preliminary work by the researchers show that sulfidic anions would likely have quickened the chemical reactions required to convert extremely basic prebiotic molecules into RNA,” explains Grossman.
A study by Prof. Daniel Rothman shows that there could be enough carbon in the Earth’s oceans by 2100 to trigger a sixth mass extinction, reports Mark Fischetti and Jen Christiansen for Scientific American.
In this video, Nicholas Cardona reports for USA Today that Prof. Daniel Rothman has predicted that the Earth’s next mass extinction event could begin in 2100, based on an analysis of the last five mass extinction events. Rothman found that, “each of the events saw high increases in global carbon. That leads to a destabilized ecosystem,” Cardona reports.
In a new study, Prof. Daniel Rothman has predicted that the oceans may hold enough carbon to trigger a sixth mass extinction by 2100, reports Trevor Nace for Forbes. Rothman’s analysis showed that, “given the current rate of carbon being emitted into the atmosphere, we will likely reach a mass extinction threshold by the year 2100.”
HuffPost reporter Thomas Tamblyn writes that Prof. Daniel Rothman has analyzed the Earth’s five previous mass extinctions and found that a sixth could be triggered by 2100. Rothman found that, “if a certain amount of carbon dioxide was added to the oceans on top of its existing levels it would result in a sixth mass extinction event.”
A new study by Prof. Daniel Rothman provides evidence that by 2100 the world’s oceans may hold enough carbon to trigger a sixth mass extinction, reports Alyssa Meyers for The Boston Globe. Rothman found that if, “310 gigatons of carbon dioxide are added to the oceans, it could be a crucial tipping point for the carbon cycle.”
An MIT study finds that the Earth’s mantle was 200 degrees Celsius hotter three billion years ago than it is today. That finding shows “that the Earth's ancient crust was made up of a much denser, iron- and magnesium-enriched material than today's rocky mantle,” writes Amy Wallace for UPI.