Holocene deglacial history of the northeast Antarctic Peninsula - A review and new chronological constraints

The northeast Antarctic Peninsula (NEAP) region is currently showing signs of significant environmental change, evidenced by acceleration of glacial retreat and collapse of both Larsen-A and -B ice shelves within the past 15 years. However, data on the past extent of the eastern margin of the Antarc...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Johnson, Joanne, Bentley, Michael, Roberts, Stephen, Binnie, Steven A., Freeman, Stewart P.H.T.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2011
Subjects:
Antarctic
The Antarctic
Antarctic Peninsula
Ross Island
Seymour
Seymour Island
Prince Gustav Channel
Lachman
Terrapin
Terrapin Hill
Cape Lachman
Johnson Mesa
Antarc*
Ice cap
Ice Sheet
Ice Shelf
Ice Shelves
James Ross Island
Online Access:http://nora.nerc.ac.uk/id/eprint/16998/
http://www.journals.elsevier.com/quaternary-science-reviews/
Description
Summary:The northeast Antarctic Peninsula (NEAP) region is currently showing signs of significant environmental change, evidenced by acceleration of glacial retreat and collapse of both Larsen-A and -B ice shelves within the past 15 years. However, data on the past extent of the eastern margin of the Antarctic Peninsula Ice Sheet (APIS) and its Holocene retreat history are sparse, and hence we cannot yet put the recent changes into a long-term context. In order to investigate the timing of deglaciation, we present 16 new cosmogenic 10Be surface exposure ages from sites on northern James Ross Island (Cape Lachman, Johnson Mesa and Terrapin Hill) and Seymour Island. The majority of the ages cluster around 6e10 ka, with three significantly older (25e31 ka). We combine these ages with existing terrestrial and marine radiocarbon deglaciation ages, and a compilation of existing swath bathymetry data, to quantify the temporal and spatial character of the regional glacial history. Ice had begun to retreat from the outer shelf by 18.3 ka, reaching Seymour Island by w8 ka. Northern James Ross Island began to deglaciate around the time of the Early Holocene Climatic Optimum (c. 11e9.5 ka). Deglaciation continued, and a transition from grounded to floating ice in Prince Gustav Channel occurred around 8 ka, separating the James Ross Island ice cap from the APIS. This occurred shortly before Prince Gustav Channel ice shelf began to disintegrate at 6.2 ka. Our results suggest there may be a bathymetric control on the spatial pattern of deglaciation in the NEAP.

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