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
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/1885/50775 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 |
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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