In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 34, No. 7 ( 2019-07), p. 1218-1233
Abstract:
Carbonate ion increased at the intermediate‐depth SW Atlantic during HS1, coeval with initial atmospheric CO 2 rise Carbonate ion signal is most likely due to reduction in remineralized carbon, pointing to a biological pump driver Tracer inversion results suggest intermediate‐depth sites in subtropical South Atlantic can be used to infer SAZ productivity
Type of Medium:
Online Resource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2018PA003537
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2916554-4
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