Late Quaternary CaCO3 production and preservation in the Southern Ocean: Implications for oceanic and atmospheric carbon cycling

Recent geochemical models invoke ocean alkalinity changes, particularly in the surface Southern Ocean, to explain glacial age pCO2 reduction. In such models, alkalinity increases in glacial periods are driven by reductions in North Atlantic Deep Water (NADW) supply, which lead to increases in deepwa...

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Bibliographic Details
Published in:Paleoceanography
Main Authors: Howard, W, Prell, WL
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 1994
Subjects:
Online Access:https://doi.org/10.1029/93PA03524
http://ecite.utas.edu.au/35726