In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 19, No. 5 ( 2018-05), p. 1447-1463
Abstract:
The deep hydrographic structure of the SCS during the LGM was similar to the modern conditions, but with greater vertical δ 18 O gradient Pacific δ 13 C profiles suggest a northward deep water flow (∼1,200–2,600 m) from the Southern Ocean to the SCS during the LGM The relative contributions of northern versus southern‐sourced deep water for the western Pacific are different between the LGM and Holocene
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2017GC007377
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2018
detail.hit.zdb_id:
2027201-7
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