期刊
QUATERNARY SCIENCE REVIEWS
卷 100, 期 -, 页码 87-110出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quascirev.2014.06.023
关键词
Antarctic Peninsula Ice Sheet; Last Glacial Maximum; Deglaciation; Antarctica; Glacial geology
资金
- Scientific Committee for Antarctic Research Antarctic Climate Evolution Programme (SCAR-ACE)
- UK Natural Environment Research Council (NERC)
- USA National Science Foundation (Office of Polar Programs)
- Spanish National Antarctic Program and MINECO Polar Research Area
- Catalonian government
- NERC [bas0100024, NE/J005673/1, bas0100027, NE/F014260/1, NE/J008176/1] Funding Source: UKRI
- Natural Environment Research Council [bas0100027, NE/J008176/1, NE/F014260/1, bas0100024, NE/J005673/1] Funding Source: researchfish
- Directorate For Geosciences
- Office of Polar Programs (OPP) [1430002] Funding Source: National Science Foundation
- Office of Polar Programs (OPP)
- Directorate For Geosciences [1246353] Funding Source: National Science Foundation
This paper compiles and reviews marine and terrestrial data constraining the dimensions and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum (LGM) through deglaciation to the present day. These data are used to reconstruct grounding-line retreat in 5 ka time-steps from 25 ka BP to present. Glacial landforms and subglacial tills on the eastern and western Antarctic Peninsula (AP) shelf indicate that the APIS was grounded to the outer shelf/shelf edge at the LGM and contained a series of fast-flowing ice streams that drained along cross-shelf bathymetric troughs. The ice sheet was grounded at the shelf edge until similar to 20 cal ka BP. Chronological control on retreat is provided by radiocarbon dates on glacimarine sediments from the shelf troughs and on lacustrine and terrestrial organic remains, as well as cosmogenic nuclide dates on erratics and ice moulded bedrock. Retreat in the east was underway by about 18 cal ka BP. The earliest dates on recession in the west are from Bransfield Basin where recession was underway by 17.5 cal ka BP. Ice streams were active during deglaciation at least until the ice sheet had pulled back to the mid-shelf. The timing of initial retreat decreased progressively southwards along the western AP shelf; the large ice stream in Marguerite Trough may have remained grounded at the shelf edge until about 14 cal ka BP, although terrestrial cosmogenic nuclide ages indicate that thinning had commenced by 18 ka BP. Between 15 and 10 cal ka BP the APIS underwent significant recession along the western AP margin, although retreat between individual troughs was asynchronous. Ice in Marguerite Trough may have still been grounded on the mid-shelf at 10 cal ka BP. In the Larsen-A region the transition from grounded to floating ice was established by 10.7-10.6 cal ka BP. The APIS had retreated towards its present configuration in the western AP by the mid-Holocene but on the eastern peninsula may have approached its present configuration several thousand years earlier, by the start of the Holocene. Mid to late-Holocene retreat was diachronous with stillstands, re-advances and changes in ice-shelf configuration being recorded in most places. Subglacial topography exerted a major control on grounding-line retreat with grounding-zone wedges, and thus by inference slow-downs or stillstands in the retreat of the grounding line, occurring in some cases on reverse bed slopes. (C) 2014 Durham University. Published by Elsevier Ltd.
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