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Collaborative Research: Disentangling paleoclimate signals with individual foraminiferal analyses from a new record of the Paleocene-Eocene Thermal Maximum

Organization Utah State UniversityLocation LOGAN, United StatesPosted 15 Aug 2025Deadline 31 Jul 2028
NSFUS FederalResearch GrantScience FoundationUT
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The Paleocene-Eocene Thermal Maximum (PETM, 56 million years ago) is an important paleoclimate event used to understand how Earth’s climate system responded to rapid increases in atmospheric methane and carbon dioxide. One approach to study this interval is chemical analysis of microfossils known as foraminifera preserved in deep-sea sediment.…

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