Impact of Environmental Changes on Microbes in Arctic Soils
As the Arctic continues to warm at about twice the rate of the rest of the world, scientists expect its frozen soils—known as permafrost—to thaw, activating microbes capable of decomposing soil and releasing carbons and other nutrients to the atmosphere and water. Berkeley Lab scientists in the Earth and Environmental Systems Area (EESA), led by microbial ecologist Neslihan Taş, set out to learn more about how Arctic soil microbes can contribute to greenhouse gas emissions under a warming climate. Taş’s research team collaborated with Susannah Tringe, Deputy for User Programs at the Joint Genome Institute (JGI), to conduct their study, funded by the Department of Energy’s Office of Biological and Environmental Research (BER). The results were published in Nature Communications.
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