In:
Paleoceanography, American Geophysical Union (AGU), Vol. 32, No. 4 ( 2017-04), p. 351-370
Abstract:
We present modern SNW‐Δ[CO 3 2− ] calibrations and assess their reliability as an alkalinity proxy Rising [CO 3 2− ] from MIS 5e to 3 and from MIS 7 to 6 implies a shift in CaCO 3 deposition from shelves to the deep ocean A decline in [CO 3 2− ] during MIS 4 may record increased deep‐ocean carbon storage
Type of Medium:
Online Resource
ISSN:
0883-8305
,
1944-9186
DOI:
10.1002/2016PA003039
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
637876-6
detail.hit.zdb_id:
2015231-0
detail.hit.zdb_id:
2916554-4
SSG:
16,13
SSG:
13
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