Loss of carbon from the deep sea since the last glacial maximum

Deep-ocean carbonate ion concentrations ([CO32-]) and carbon isotopic ratios (δ13C) place important constraints on past redistributions of carbon in the ocean-land-atmosphere system and hence provide clues to the causes of atmospheric CO2 concentration c

Bibliographic Details
Published in:Science
Main Authors: Yu, Jimin, Broeker, Wally S., Elderfield, H, Jin, Zhangdong, McManus, Jerry, Zhang, Fei
Format: Article in Journal/Newspaper
Language:unknown
Published: American Association for the Advancement of Science
Subjects:
Keywords: boron
calcium
carbonic acid
absorption
air-sea interaction
benthic environment
biosphere
boron
carbon isotope
carbonate
concentration (composition)
deep sea
deglaciation
foraminifera
Last Glacial Maximum
paleoceanography
paleoenvi
Carbonic acid
Online Access:http://hdl.handle.net/1885/65274
https://doi.org/10.1126/science.1193221
https://openresearch-repository.anu.edu.au/bitstream/1885/65274/5/Yu_J_2010_Loss_of_carbon.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/65274/7/01_Yu_Loss_of_carbon_from_the_deep_2010.pdf.jpg
Description
Summary:Deep-ocean carbonate ion concentrations ([CO32-]) and carbon isotopic ratios (δ13C) place important constraints on past redistributions of carbon in the ocean-land-atmosphere system and hence provide clues to the causes of atmospheric CO2 concentration c

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