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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

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


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

CollectionsANU Research Publications
Date published: 2004
Type: Journal article
Source: Paleoceanography
DOI: 10.1029/2004PA001047


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