NSF award 2621189 · University of North Carolina at Chapel Hill

Lag-time thermochronology as a possible proxy for changes in erosion rates over the Paleocene-Eocene Thermal Maximum, Tremp-Graus Basin, Spain

Final report due

28 February 2027

in 133 days · The award ends on 31 October 2026.

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No-cost extension notice21 Oct 2026in 3 days
award ending 2026-10-31 · Research.gov
PAPPG 24-1: “at least ten calendar days prior to the end date”
Final report due28 Feb 2027in 133 days
award ending 2026-10-31 · Research.gov
PAPPG 24-1: “no later than 120-days following the end date of the award”
Project outcomes report due28 Feb 2027in 133 days
award ending 2026-10-31 · Research.gov
PAPPG 24-1: “no later than 120 days following the end date”
Award is closed out28 Feb 2027in 133 days
award ending 2026-10-31 · Research.gov
PAPPG 24-1: “financially closed out 120 days after their expiration date”

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NSF lists this award's end date as 31 October 2026.
NSF rules say the final report is due no later than 120 days after that.
So the final report is due by 28 February 2027.

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Award card

Award number: 2621189
Period of support: 1 Jan 2026 – 31 Oct 2026
Amount: $219,167
Awardee: University of North Carolina at Chapel Hill, Chapel Hill, NC
Program: P4CLIMATE
Directorate: GEO

Abstract

The global climate is rapidly warming as a function of elevated green-house gas emissions. Earth’s climate has fluctuated between periods of warming and cooling across it’s ~4.5-billion-year history. One prominent period of past global warming that is similar to what we are observing today is the Paleocene-Eocene Thermal Maximum (PETM, ~56 million years ago) – where Earth’s climate warmed, and then cooled rapidly…

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