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dc.contributor.authorRamirez, Michelle
dc.date.accessioned2025-05-13T21:03:09Z
dc.date.available2025-05-13T21:03:09Z
dc.date.issued2025-04-01
dc.identifier.urihttp://hdl.handle.net/11122/15907
dc.descriptionMentor: Dr. Mario Muscarella; Permafrost thaw is a major concern for the Arctic and sub-Arctic regions because it can emit large amounts of stored carbon into the atmosphere as carbon dioxide or methane. These greenhouse gasses (GHG) are controlled by microbial activities. Permafrost thaw will let the frozen and active layer soils mix, allowing the microbial communities to form new mixtures of organisms and organic compounds. With increasing temperatures, this could be vital to understand how microbes impact gas flux and their soil ecosystem.en_US
dc.language.isoen_USen_US
dc.titleMicrobial Response to Permafrost Thaw and Coalescenceen_US
dc.typePosteren_US
refterms.dateFOA2025-05-13T21:03:10Z


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