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
Main Authors: Bostock, Helen, Opdyke, Bradley, Gagan, Michael, Fifield, L Keith
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2015
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
id ftanucanberra:oai:digitalcollections.anu.edu.au:1885/86792
record_format openpolar
spelling ftanucanberra:oai:digitalcollections.anu.edu.au:1885/86792 2023-05-15T13:35:18+02:00 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 2015-12-13T23:08:56Z http://hdl.handle.net/1885/86792 unknown American Geophysical Union 0883-8305 http://hdl.handle.net/1885/86792 Paleoceanography Keywords: carbon isotope deglaciation foraminifera intermediate water Last Glacial Maximum paleoceanography oceanic regions Pacific Ocean Pacific Ocean (Northwest) World Foraminifera d13C AAIW Journal article 2015 ftanucanberra 2015-12-28T23:39:08Z 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 Article in Journal/Newspaper Antarc* Antarctic Australian National University: ANU Digital Collections Antarctic Pacific
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language unknown
topic Keywords: carbon isotope
deglaciation
foraminifera
intermediate water
Last Glacial Maximum
paleoceanography
oceanic regions
Pacific Ocean
Pacific Ocean (Northwest)
World
Foraminifera d13C
AAIW
spellingShingle Keywords: carbon isotope
deglaciation
foraminifera
intermediate water
Last Glacial Maximum
paleoceanography
oceanic regions
Pacific Ocean
Pacific Ocean (Northwest)
World
Foraminifera d13C
AAIW
Bostock, Helen
Opdyke, Bradley
Gagan, Michael
Fifield, L Keith
Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation
topic_facet Keywords: carbon isotope
deglaciation
foraminifera
intermediate water
Last Glacial Maximum
paleoceanography
oceanic regions
Pacific Ocean
Pacific Ocean (Northwest)
World
Foraminifera d13C
AAIW
description 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
format Article in Journal/Newspaper
author Bostock, Helen
Opdyke, Bradley
Gagan, Michael
Fifield, L Keith
author_facet Bostock, Helen
Opdyke, Bradley
Gagan, Michael
Fifield, L Keith
author_sort Bostock, Helen
title Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation
title_short Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation
title_full Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation
title_fullStr Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation
title_full_unstemmed Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation
title_sort carbon isotope evidence for changes in antarctic intermediate water circulation and ocean ventilation in the southwest pacific during the last deglaciation
publisher American Geophysical Union
publishDate 2015
url http://hdl.handle.net/1885/86792
geographic Antarctic
Pacific
geographic_facet Antarctic
Pacific
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Paleoceanography
op_relation 0883-8305
http://hdl.handle.net/1885/86792
_version_ 1766063986965479424

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