Late Quaternary palaeoceanography of the Circumpolar Deep Water from South Tasman Rise
We use sediment cores from the South Tasman Rise (STR) to reconstruct deepwater circulation in the southwest Pacific sector of the Southern Ocean. Sediment cores MD972106 (45° 09′ S, 146° 17′ E, 3310 m water depth) and GC34 (45° 06′ S, 147° 45�
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Wiley-VCH Verlag GMBH
2015
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Online Access: | http://hdl.handle.net/1885/22693 |