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

Peñalver-Clavel, Irene; Westerhold, Thomas; Alegret, Laia

doi:10.5194/jm-44-713-2025

Articles | Volume 44, issue 2

https://doi.org/10.5194/jm-44-713-2025

© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/jm-44-713-2025

© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 44, issue 2

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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Cited articles

Alegret, L. and Thomas, E.: Upper cretaceous and lower Paleogene benthic foraminifera from northeastern Mexico, Micropaleontology, 47, 269–316, 2001.

Alegret, L. and Thomas, E.: Food supply to the seafloor in the Pacific Ocean after the Cretaceous/Paleogene boundary event, Mar. Micropaleontol., 73, 105–116, https:// doi.org/10.1016/j.marmicro.2009.07.005, 2009.

Alegret, L., Ortiz, S., Orue-Etxebarria, X., Bernaola, G., Baceta, J.I., Monechi, S., Apellaniz, E., and Pujalte, V.: The Paleocene–Eocene thermal maximum: new data from the microfossil turnover at Zumaia section, Palaios, 24, 318–328, https://doi.org/10.2110/palo.2008.p08-057r, 2009.

Alegret, L., Ortiz, S., Arenillas, I., and Molina, E.: What happens when the ocean is overheated? The foraminiferal response across the Paleocene-Eocene Thermal Maximum at the Alamedilla section (Spain), GSA Bull., 122, 1616–1624, 2010.

Alegret, L., Reolid, M., and Vega Pérez, M.: Environmental instability during the latest Paleocene at Zumaia (Basque-Cantabric Basin): the herald of the Paleocene Eocene Thermal Maximum, Palaeogeogr. Palaeoclimatol. Palaeoecol., 497, 186–200, https://doi.org/10.1016/j.palaeo.2018.02.018, 2018.