hdl:10013/epic.11661
publisher:10.2973/odp.proc.sr.113.193.1990
Oligocene to Quaternary Sedimentation Processes on the Antarctic Continental Margin|ODP Leg 113|Site 693
Grobe, H and Fütterer, DK
;
Contact
hgrobe [ at ] awi-bremerhaven.de
Abstract
During the middle Oligocene, increasing glacial conditions on the continent are indicated by the presence of glauconitic sands, that are interpreted to have formed on the shelf and then transported down the continental slope by advancing glaciers or as a result of sea-level lowering. Primary productivity decreased at about 3 Ma due to the development of a permanent sea-ice cover close to the continent. -from Authors
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Article
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Grobe, H and Fütterer, DK
;
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Peer-reviewed
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1074
DOI
https://www.doi.org/10.2973/odp.proc.sr.113.193.1990
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Grobe, H.
and
Fütterer, D.
(1990):
Oligocene to Quaternary Sedimentation Processes on the Antarctic Continental Margin|ODP Leg 113|Site 693
,
Proc., scientific results, ODP, Leg 113, Weddell Sea, Antarctica,
113
,
pp. 121-131
.
doi: https://www.doi.org/10.2973/odp.proc.sr.113.193.1990
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