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

Author:

Paytan Adina1ORCID,Griffith Elizabeth M.2ORCID,Eisenhauer Anton3ORCID,Hain Mathis P.1ORCID,Wallmann Klaus3,Ridgwell Andrew4ORCID

Affiliation:

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

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

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

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

Abstract

Carbon cycle history Marine carbon includes organic and inorganic components, both of which must be accounted for to understand the global carbon cycle. Paytan et al. assembled a record of stable strontium isotopes ( 88 Sr and 86 Sr) derived from pelagic marine barite and used it to reconstruct changes in the deposition and burial of biogenic calcium carbonate in marine sediments. These data, when combined with measurements of 87 Sr/ 86 Sr, can help to reveal past changes in the sources and sinks of strontium, as well as variations in carbonate deposition that affect the carbon cycle. Science , this issue p. 1346

Funder

National Science Foundation

Heising Simons Foundation

Helmholtz Association and the German Science Funding Agency

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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