Stable Isotope Constraints on Marine Productivity Across the Cretaceous‐Paleogene Mass Extinction

Author:

Sepúlveda Julio1ORCID,Alegret Laia2,Thomas Ellen34ORCID,Haddad Emily5,Cao Changqun6,Summons Roger E.7ORCID

Affiliation:

1. Organic Geochemistry Laboratory, Department of Geological Sciences and Institute of Arctic and Alpine Research (INSTAAR)University of Colorado Boulder Boulder CO USA

2. Departamento de Ciencias de la Tierra and Instituto Universitario de Ciencias Ambientales de AragónUniversidad de Zaragoza Zaragoza Spain

3. Department of Geology and GeophysicsYale University New Haven CT USA

4. Department of Earth and Environmental SciencesWesleyan University Middletown CT USA

5. Department of Earth SciencesUniversity of California Riverside CA USA

6. State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and PalaeontologyChinese Academy of Sciences Nanjing China

7. Department of Earth, Atmospheric, and Planetary SciencesMassachusetts Institute of Technology Cambridge MA USA

Funder

Ministerio de Ciencia e Innovación

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Reference177 articles.

1. The Cretaceous-Tertiary extinction: Modeling carbon flux and ecological response

2. AlegretL.(2003).Sedimentología y Micropaleontología (foraminíferos bentónicos)del tránsitoCretácico‐Terciario:Correlación entre las áreas del Golfo de México y del Tethys. Bell Howell Ed. N° 3073947 476 pp. ISBN: 84‐95480‐87‐5.

3. Recovery of the deep-sea floor after the Cretaceous−Paleogene boundary event: The benthic foraminiferal record in the Basque–Cantabrian basin and in South-eastern Spain

4. Evolución paleoambiental durante el tránsito Cretácico/Paleógeno basada en foraminíferos bentónicos;Alegret L.;Revista Española de Paleontología,2008

5. Paleoenvironmental Recovery After the Cretaceous/ Paleogene Boundary Crisis: Evidence From the Marine Bidart Section (SW France)

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