In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 35, No. 2 ( 2020-02)
Abstract:
The southwest Pacific Ocean stored more respired CO 2 during the Last Glacial Maximum than during the Holocene Carbonate ion concentration of intermediate water initially increases in tandem with inferred early deglacial Southern Ocean upwelling Release of respired CO 2 from the interior Pacific Ocean contributed to the deglacial rise in atmospheric CO 2
Type of Medium:
Online Resource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2019PA003766
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
2916554-4
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