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Seawater carbonate ion-d13C systematics and application to glacial-interglacial North Atlantic ocean circulation

Date

Authors

Yu, Jimin

Elderfield, H

Piotrowski, Alexander

Publisher

Elsevier

Abstract

Seawater carbonate ion and δ13C are affected by many processes including biology, air-sea exchange, alkalinity change, and mixing between different water masses. Study of modern ocean data shows that deep ocean carbonate ion and δ13C of dissolved inorga

Keywords

Keywords: Carbonate ions; Charged particles; Seawater; Electrons; benthic foraminifera; calcite; carbon dioxide; carbon sequestration; carbonate system; glacial-interglacial cycle; inorganic carbon; ion; Last Glacial; oceanic circulation; seawater; tracer; water co d13C; benthic foraminiferal B/Ca; carbonate ion concentration; North Atlantic; ocean circulation

URI

http://hdl.handle.net/1885/65375

Collections

ANU Research Publications

Source

Earth and Planetary Science Letters

Type

Journal article

DOI

10.1016/j.epsl.2008.04.010

Restricted until

2037-12-31

Downloads

File

Description

01_Yu_Seawater_carbonate_ion-d13C_2008.pdf (2.28 MB)

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