Middle-late Pleistocene deep water circulation in the southwest subtropical Pacific

The modern δ13CDIC distribution in southwest subtropical Pacific deep waters is consistent with a regional mixing regime between water masses of open Pacific Ocean and Tasman Sea origin. This mixing regime is reconstructed across the middle-late Pleistoc

Bibliographic Details
Published in:Paleoceanography
Main Authors: Russon, T., Elliot, M., Kissel, C, Cabioch, Guy, De Deckker, Patrick, Correge, T.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union
Subjects:
Keywords: benthic foraminifera
carbon isotope
deep water
mixing
oceanic circulation
Pleistocene
sediment core
New Caledonia [Melanesia]
Pacific Ocean
Southern Ocean
Tasman Sea
Pacific
Online Access:http://hdl.handle.net/1885/50775
https://doi.org/10.1029/2009PA001755
https://openresearch-repository.anu.edu.au/bitstream/1885/50775/5/Russon_DeDeckker_Middle-late_Pleistocene_2009.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/50775/7/01_Russon_Middle-late_Pleistocene_deep_2009.pdf.jpg
Description
Summary:The modern δ13CDIC distribution in southwest subtropical Pacific deep waters is consistent with a regional mixing regime between water masses of open Pacific Ocean and Tasman Sea origin. This mixing regime is reconstructed across the middle-late Pleistoc

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