Late Paleocene‐middle Eocene benthic foraminifera on a Pacific seamount (Allison Guyot, ODP Site 865): Greenhouse climate and superimposed hyperthermal events-Reference-Cited by-同舟云学术

Late Paleocene‐middle Eocene benthic foraminifera on a Pacific seamount (Allison Guyot, ODP Site 865): Greenhouse climate and superimposed hyperthermal events

Published:2016-03 Issue:3 Volume:31 Page:346-364
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Arreguín‐Rodríguez Gabriela J.¹,Alegret Laia¹²,Thomas Ellen³⁴

Affiliation:

1. Departamento de Ciencias de la Tierra Universidad de Zaragoza Zaragoza Spain

2. Instituto Universitario de Ciencias Ambientales Universidad de Zaragoza Zaragoza Spain

3. Department of Geology and Geophysics Yale University New Haven Connecticut USA

4. Department of Earth and Environmental Sciences Wesleyan University Middletown Connecticut USA

Funder

Spanish Ministry of Economy and Competitiveness and FEDER funds

Consolidated Group E05 (Government of Aragon/European Social Fund)

NSF

the Leverhulme Trust

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015PA002837

Reference163 articles.

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4. Food supply to the seafloor in the Pacific Ocean after the Cretaceous/Paleogene boundary event

5. Extinction and recovery of benthic foraminifera across the Paleocene–Eocene Thermal Maximum at the Alamedilla section (Southern Spain)

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