A 35-million-year record of seawater stable Sr isotopes reveals a fluctuating global carbon cycle.


Journal

Science (New York, N.Y.)
ISSN: 1095-9203
Titre abrégé: Science
Pays: United States
ID NLM: 0404511

Informations de publication

Date de publication:
26 03 2021
Historique:
received: 27 12 2019
accepted: 17 02 2021
entrez: 26 3 2021
pubmed: 27 3 2021
medline: 27 3 2021
Statut: ppublish

Résumé

Changes in the concentration and isotopic composition of the major constituents in seawater reflect changes in their sources and sinks. Because many of the processes controlling these sources and sinks are tied to the cycling of carbon, such records can provide insights into what drives past changes in atmospheric carbon dioxide and climate. Here, we present a stable strontium (Sr) isotope record derived from pelagic marine barite. Our δ

Identifiants

pubmed: 33766882
pii: 371/6536/1346
doi: 10.1126/science.aaz9266
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S.

Langues

eng

Sous-ensembles de citation

IM

Pagination

1346-1350

Informations de copyright

Copyright © 2021 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works.

Auteurs

Adina Paytan (A)

Institute of Marine Science, University of California Santa Cruz, Santa Cruz, CA 95064, USA. apaytan@ucsc.edu.

Elizabeth M Griffith (EM)

School of Earth Sciences, The Ohio State University, Columbus, OH 43210, USA.

Anton Eisenhauer (A)

GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany.

Mathis P Hain (MP)

Institute of Marine Science, University of California Santa Cruz, Santa Cruz, CA 95064, USA.

Klaus Wallmann (K)

GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany.

Andrew Ridgwell (A)

Department of Earth Sciences and Planetary Sciences, University of California Riverside, Riverside, CA 92521, USA.

Classifications MeSH