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Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation

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Date

2004

Authors

Bostock, Helen
Opdyke, Bradley
Gagan, Michael
Fifield, L Keith

Journal Title

Journal ISSN

Volume Title

Publisher

American Geophysical Union

Abstract

Deep-sea sediment core FR1/97 GC-12 is located 990 mbsl in the northern Tasman Sea, southwest Pacific, where Antarctic Intermediate Water (AAIW) presently impinges the continental slope of the southern Great Barrier Reef. Analysis of carbon (δ13C) and ox

Description

Keywords

Keywords: carbon isotope; deglaciation; foraminifera; intermediate water; Last Glacial Maximum; paleoceanography; oceanic regions; Pacific Ocean; Pacific Ocean (Northwest); World; Foraminifera d13C; AAIW; Deglaciation

Citation

URI

http://hdl.handle.net/1885/86792

Collections

ANU Research Publications

Source

Paleoceanography

Type

Journal article

Book Title

Entity type

Access Statement

License Rights

DOI

10.1029/2004PA001047

Restricted until

2037-12-31

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Description
01_Bostock_Carbon_isotope_evidence_for_2004.pdf (669.84 KB)

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