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�

Bibliographic Details
Published in:	Journal of Quaternary Science
Main Authors:	Moy, Andrew D, Howard, William Robert, Gagan, Michael
Format:	Article in Journal/Newspaper
Language:	unknown
Published:	Wiley-VCH Verlag GMBH
Subjects:	Keywords: accelerator mass spectrometry benthic foraminifera carbon isotope circumpolar current deep water formation paleoceanography Quaternary radiocarbon dating stable isotope Southern Ocean Cibicidoides Foraminifera Benthic foraminiferal stable isotopes Circumpolar deep water Deep-water circulation Palaeoceanography Pacific South Tasman Rise
Online Access:	http://hdl.handle.net/1885/22693 https://doi.org/10.1002/jqs.1067 https://openresearch-repository.anu.edu.au/bitstream/1885/22693/5/Moy_JQS_2006.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/22693/7/01_Moy_Late_Quaternary_2006.pdf.jpg

Description
Summary:	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�