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

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

Bibliographic Details
Published in:Paleoceanography
Main Authors: Bostock, Helen, Opdyke, Bradley, Gagan, Michael, Fifield, L Keith
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union
Subjects:
Keywords: carbon isotope
deglaciation
foraminifera
intermediate water
Last Glacial Maximum
paleoceanography
oceanic regions
Pacific Ocean
Pacific Ocean (Northwest)
World
Foraminifera d13C
AAIW
Antarctic
Pacific
Antarc*
Online Access:http://hdl.handle.net/1885/86792
https://doi.org/10.1029/2004PA001047
https://openresearch-repository.anu.edu.au/bitstream/1885/86792/5/MigratedxPub15783_2004.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/86792/7/01_Bostock_Carbon_isotope_evidence_for_2004.pdf.jpg
Description
Summary: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

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