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Loss of carbon from the deep sea since the last glacial maximum

Date

Authors

Yu, Jimin

Broeker, Wally S.

Elderfield, H

Jin, Zhangdong

McManus, Jerry

Zhang, Fei

Publisher

American Association for the Advancement of Science

Abstract

Deep-ocean carbonate ion concentrations ([CO32-]) and carbon isotopic ratios (δ13C) place important constraints on past redistributions of carbon in the ocean-land-atmosphere system and hence provide clues to the causes of atmospheric CO2 concentration c

Keywords

Keywords: boron; calcium; carbonic acid; absorption; air-sea interaction; benthic environment; biosphere; boron; calcium; carbon isotope; carbonate; concentration (composition); deep sea; deglaciation; foraminifera; Last Glacial Maximum; paleoceanography; paleoenvi

URI

http://hdl.handle.net/1885/65274

Collections

ANU Research Publications

Source

Science

Type

Journal article

DOI

10.1126/science.1193221

Restricted until

2037-12-31

Downloads

File

Description

01_Yu_Loss_of_carbon_from_the_deep_2010.pdf (299.34 KB)