In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 35, No. 7 ( 2020-07)
Kurzfassung:
The highest mid‐depth negative δ 13 C excursions occurred in the western tropical South Atlantic and dissipated further south Reduced Northern Component Water ventilation in the western tropical South Atlantic mid‐depth during Heinrich Stadials Decreased Northern Component Water δ 13 C source signal and accumulation of respired carbon drove mid‐depth negative excursions in δ 13 C
Materialart:
Online-Ressource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2020PA003876
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2020
ZDB Id:
2916554-4