In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 35, No. 12 ( 2020-12)
Abstract:
Paired δ 13 C‐δ 18 O data are used to identify water mass end‐members outside the sampled range In past oceans, a ternary mixing model using δ 13 C‐δ 18 O may outperform a binary δ 13 C mixing model AMOC was relatively deep during the M2 glacial compared to the late Pliocene interglacials
Type of Medium:
Online Resource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2019PA003804
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
2916554-4
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