North atlantic versus southern ocean contributions to a deglacial surge in deep ocean ventilation

Past glacial-interglacial climate transitions were accompanied by millennial-scale pulses in atmospheric CO2 that are widely thought to have resulted from the release of CO2 via the Southern Ocean. However, direct proxy evidence for a Southern Ocean role

Bibliographic Details
Published in:Geology
Main Authors: Skinner, L. C., Scrivner, A E, Vance, Derek, Barker, S, Fallon, Stewart, Waelbroeck, Claire
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America Inc
Subjects:
Keywords: Air-sea exchange
Antarctic regions
Climate transition
Global climates
Last deglaciation
Neodymium isotopes
Ocean ventilations
Ocean-atmosphere
Carbon dioxide
Isotopes
Ventilation
Oceanography
air-sea interaction
deep water ven
Antarctic
Southern Ocean
Antarc*
North Atlantic
Online Access:http://hdl.handle.net/1885/72804
https://doi.org/10.1130/G34133.1
https://openresearch-repository.anu.edu.au/bitstream/1885/72804/5/f5625xPUB3436_2013.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/72804/7/01_Skinner_North_atlantic_versus_southern_2013.pdf.jpg
Description
Summary:Past glacial-interglacial climate transitions were accompanied by millennial-scale pulses in atmospheric CO2 that are widely thought to have resulted from the release of CO2 via the Southern Ocean. However, direct proxy evidence for a Southern Ocean role

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