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
Published in: | Paleoceanography |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
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Subjects: | |
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 |
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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