Articles | Volume 44, issue 2
https://doi.org/10.5194/jm-44-713-2025
https://doi.org/10.5194/jm-44-713-2025
Research article
 | 
19 Dec 2025
Research article |  | 19 Dec 2025

Deep-sea benthic foraminiferal response to the Late Lutetian Thermal Maximum at Demerara Rise (ODP Site 1260, equatorial western Atlantic)

Irene Peñalver-Clavel, Thomas Westerhold, and Laia Alegret

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Short summary
A study in the equatorial Atlantic Ocean (Ocean Drilling Program Site 1260) reveals the deep-sea biotic response to a middle Eocene warming event 41.52 million years ago. Low-diversity benthic foraminiferal assemblages indicate environmental stress during the warming event. We argue that the biotic response in the deep sea and carbonate dissolution at this site were likely related to its paleoceanographic setting.
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