In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 36, No. 9 ( 2021-09)
Kurzfassung:
Deglacial authigenic manganese peaks in the Southern Ocean and abyssal Pacific are attributable to changing bottom water oxygen Low‐O 2 bottom waters occupied the entirety of the deep Pacific during the Last Glacial Maximum Respired CO 2 storage in the deep Pacific is a characteristic feature of late‐Pleistocene glacial cycles since Marine Isotope Stage 12
Materialart:
Online-Ressource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2021PA004226
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2021
ZDB Id:
2916554-4