Are Antarctic Peninsula Ice Sheet grounding events manifest in sedimentary cycles on the adjacent continental rise?

Bart, P.J.; Hillenbrand, C.D. ORCID: https://orcid.org/0000-0003-0240-7317; Ehrmann, W.; Iwai, M.; Winter, D.; Warny, S.A.. 2007 Are Antarctic Peninsula Ice Sheet grounding events manifest in sedimentary cycles on the adjacent continental rise? Marine Geology, 236 (1-2). 1-13. 10.1016/j.margeo.2006.09.008

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Official URL: http://dx.doi.org/10.1016/j.margeo.2006.09.008

Abstract/Summary

The direct record of Late Miocene–Early Pliocene Antarctic Peninsula Ice Sheet expansions from a previously published seismostratigraphic study of the outer shelf at Ocean Drilling Program Site 1097 is compared to the glacial history we deduced from published proxy evidence within coeval sections on the adjacent continental rise. The proxies are sedimentary structures (laminated vs. massive/bioturbated facies) and clay minerals (predominantly smectite and chlorite contents) from Ocean Drilling Program Site 1095 located on the distal part of a large drift. The comparison shows that more sedimentary cycles are evident on the continental rise for three of the four diatom biozones we considered. This indicates that the continental-rise sedimentology may indeed be related to local or regional paleoenvironmental variability, including Antarctic Peninsula Ice Sheet grounding events on the adjacent outer continental shelf. If correct, this would be a promising result because unlike the outer continental shelf sequences drilled thus far, the continental rise record is relatively continuous and can be dated using paleomagnetic and biostratigraphic data. However, our study also shows that no objective criteria provide direct linkages between the glacial history we deduced from the two continental rise proxies and that previously derived from the continental-shelf seismic stratigraphy. Furthermore, the two sedimentologic proxies on the continental rise do not always provide a consistent picture of glacial history when compared against each other.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/j.margeo.2006.09.008
Programmes:	BAS Programmes > Global Science in the Antarctic Context (2005-2009) > Glacial Retreat in Antarctica and Deglaciation of the Earth System
ISSN:	0025-3227
Additional Keywords:	Antarctic Peninsula; glaciations; sedimentary cycles; grounding events; Late Miocene; Early Pliocene
NORA Subject Terms:	Earth Sciences
Date made live:	12 Nov 2007 10:18 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/1166

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/j.margeo.2006.09.008

Programmes:

BAS Programmes > Global Science in the Antarctic Context (2005-2009) > Glacial Retreat in Antarctica and Deglaciation of the Earth System

ISSN:

0025-3227

Additional Keywords:

Antarctic Peninsula; glaciations; sedimentary cycles; grounding events; Late Miocene; Early Pliocene

NORA Subject Terms:

Earth Sciences