Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula

The Antarctic Peninsula region is ideally suited to monitor how global change affects Antarctica because it is one of the most sensitive regions of the continent to rapid climate change. This has been clearly demonstrated by the recent break up of the Larsen A Ice Shelf. Drilling at Ocean Drilling P...

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Main Authors: Pike, J., Moreton, S.G., Allen, C.S.
Format: Article in Journal/Newspaper
Language:unknown
Published: Texas A & M University 2001
Subjects:
Online Access:http://eprints.gla.ac.uk/121708/
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spelling ftuglasgow:oai:eprints.gla.ac.uk:121708 2023-05-15T14:04:48+02:00 Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula Pike, J. Moreton, S.G. Allen, C.S. 2001 http://eprints.gla.ac.uk/121708/ unknown Texas A & M University Pike, J., Moreton, S.G. <http://eprints.gla.ac.uk/view/author/11570.html> and Allen, C.S. (2001) Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula. Ocean Drilling Program, Proceedings, Scientific Results <http://eprints.gla.ac.uk/view/journal_volume/Ocean_Drilling_Program,_Proceedings,_Scientific_Results.html>, 178, pp. 1-17. (doi:10.2973/odp.proc.sr.178.226.2001 <http://dx.doi.org/10.2973/odp.proc.sr.178.226.2001>) Articles PeerReviewed 2001 ftuglasgow https://doi.org/10.2973/odp.proc.sr.178.226.2001 2020-01-10T01:09:42Z The Antarctic Peninsula region is ideally suited to monitor how global change affects Antarctica because it is one of the most sensitive regions of the continent to rapid climate change. This has been clearly demonstrated by the recent break up of the Larsen A Ice Shelf. Drilling at Ocean Drilling Program Site 1098, Palmer Deep, western Antarctic Peninsula, recovered almost 50 m of sediments that record the paleoceanographic and paleoclimatic history of the region from the last glacial maximum through the rapid climate oscillations of deglaciation into the Holocene. This sedimentary section will provide a wealth of high-resolution paleoenvironmental data from Antarctica that will be useful for climate modelers and paleoceanographers alike. This data report presents the preliminary results of a high-resolution, microscale sediment fabric study of the postglacial sediments from Palmer Deep Site 1098. These sediments have previously been described as being annually laminated; however, this investigation shows that although the interpretation of this sequence as seasonal sediments is most likely correct, there are a number of features that indicate there is strong interannual variability affecting the laminations. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Ice Shelf University of Glasgow: Enlighten - Publications Antarctic Antarctic Peninsula Palmer Deep ENVELOPE(-64.400,-64.400,-64.950,-64.950) The Antarctic
institution Open Polar
collection University of Glasgow: Enlighten - Publications
op_collection_id ftuglasgow
language unknown
description The Antarctic Peninsula region is ideally suited to monitor how global change affects Antarctica because it is one of the most sensitive regions of the continent to rapid climate change. This has been clearly demonstrated by the recent break up of the Larsen A Ice Shelf. Drilling at Ocean Drilling Program Site 1098, Palmer Deep, western Antarctic Peninsula, recovered almost 50 m of sediments that record the paleoceanographic and paleoclimatic history of the region from the last glacial maximum through the rapid climate oscillations of deglaciation into the Holocene. This sedimentary section will provide a wealth of high-resolution paleoenvironmental data from Antarctica that will be useful for climate modelers and paleoceanographers alike. This data report presents the preliminary results of a high-resolution, microscale sediment fabric study of the postglacial sediments from Palmer Deep Site 1098. These sediments have previously been described as being annually laminated; however, this investigation shows that although the interpretation of this sequence as seasonal sediments is most likely correct, there are a number of features that indicate there is strong interannual variability affecting the laminations.
format Article in Journal/Newspaper
author Pike, J.
Moreton, S.G.
Allen, C.S.
spellingShingle Pike, J.
Moreton, S.G.
Allen, C.S.
Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula
author_facet Pike, J.
Moreton, S.G.
Allen, C.S.
author_sort Pike, J.
title Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula
title_short Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula
title_full Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula
title_fullStr Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula
title_full_unstemmed Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula
title_sort data report: microfabric analysis of postglacial sediments from palmer deep, western antarctic peninsula
publisher Texas A & M University
publishDate 2001
url http://eprints.gla.ac.uk/121708/
long_lat ENVELOPE(-64.400,-64.400,-64.950,-64.950)
geographic Antarctic
Antarctic Peninsula
Palmer Deep
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Palmer Deep
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice Shelf
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice Shelf
op_relation Pike, J., Moreton, S.G. <http://eprints.gla.ac.uk/view/author/11570.html> and Allen, C.S. (2001) Data Report: Microfabric Analysis of Postglacial Sediments from Palmer Deep, Western Antarctic Peninsula. Ocean Drilling Program, Proceedings, Scientific Results <http://eprints.gla.ac.uk/view/journal_volume/Ocean_Drilling_Program,_Proceedings,_Scientific_Results.html>, 178, pp. 1-17. (doi:10.2973/odp.proc.sr.178.226.2001 <http://dx.doi.org/10.2973/odp.proc.sr.178.226.2001>)
op_doi https://doi.org/10.2973/odp.proc.sr.178.226.2001
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