Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land
One of the major issues in (palaeo-) climatology is the response of Antarctic ice sheets to global climate changes. Antarctic ice volume has varied in the past but the extent and timing of these fluctuations are not well known. In this study, we address the question of amplitude and timing of past A...
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-Cambridge University Press / New York:40 West 20th Street:New York, NY 10011:(800)872-7423, (212)924-3900, EMAIL: journals_subscriptions@cup.org, INTERNET: http://www.journals.cambridge.org, Fax: (212)691-3239 -Oxford: Blackwell Scientific Publications.
2009
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Online Access: | http://hdl.handle.net/11573/37666 https://doi.org/10.1017/s0954102008001478 http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=000263389100005&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=0c7ff228ccbaaa74236f48834a34396a http://www.scopus.com/inward/record.url?eid=2-s2.0-67649226448&partnerID=65&md5=a8d7288bdc46887bd5f9bd4f69d6fbaf |
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ftunivromairis:oai:iris.uniroma1.it:11573/37666 2024-04-14T08:04:10+00:00 Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land Stefan Strasky Luigia Di Nicola Carlo Baroni Heinrich Baur Peter W. Kubik C. Schluechter Rainer Wieler SALVATORE, Maria Cristina Stefan, Strasky Luigia Di, Nicola Carlo, Baroni Salvatore, Maria Cristina Heinrich, Baur Peter W., Kubik C., Schluechter Rainer, Wieler 2009 STAMPA http://hdl.handle.net/11573/37666 https://doi.org/10.1017/s0954102008001478 http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=000263389100005&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=0c7ff228ccbaaa74236f48834a34396a http://www.scopus.com/inward/record.url?eid=2-s2.0-67649226448&partnerID=65&md5=a8d7288bdc46887bd5f9bd4f69d6fbaf eng eng -Cambridge University Press / New York:40 West 20th Street:New York, NY 10011:(800)872-7423, (212)924-3900, EMAIL: journals_subscriptions@cup.org, INTERNET: http://www.journals.cambridge.org, Fax: (212)691-3239 -Oxford: Blackwell Scientific Publications. info:eu-repo/semantics/altIdentifier/wos/WOS:000263389100005 volume:21 issue:1 firstpage:59 lastpage:69 numberofpages:11 journal:ANTARCTIC SCIENCE http://hdl.handle.net/11573/37666 doi:10.1017/s0954102008001478 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-67649226448 http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=000263389100005&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=0c7ff228ccbaaa74236f48834a34396a http://www.scopus.com/inward/record.url?eid=2-s2.0-67649226448&partnerID=65&md5=a8d7288bdc46887bd5f9bd4f69d6fbaf cosmogenic nuclide erosion rate glacial drift landscape evolution surface exposure dating info:eu-repo/semantics/article 2009 ftunivromairis https://doi.org/10.1017/s0954102008001478 2024-03-21T18:37:23Z One of the major issues in (palaeo-) climatology is the response of Antarctic ice sheets to global climate changes. Antarctic ice volume has varied in the past but the extent and timing of these fluctuations are not well known. In this study, we address the question of amplitude and timing of past Antarctic ice level changes by surface exposure dating using in situ produced cosmogenic nuclides (10Be and 21Ne). The study area lies in the Ricker Hills, a nunatak at the boundary of the East Antarctic Ice Sheet in southern Victoria Land. By determining exposure ages of erratic boulders from glacial drifts we directly date East Antarctic Ice Sheet variations. Erosion-corrected neon and beryllium exposure ages indicate that a major ice advance reaching elevations of about 500 m above present ice levels occurred between 1.125 and 1.375 million years before present. Subsequent ice fluctuations were of lesser extent but timing is difficult as all erratic boulders from related deposits show complex exposure histories. Sample-specific erosion rates were on the order of 20–45 cm Ma-1 for a quartzite and 10–65 cm Ma-1 for a sandstone boulder and imply that the modern cold, arid climate has persisted since at least the early Pleistocene. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Victoria Land Sapienza Università di Roma: CINECA IRIS Antarctic East Antarctic Ice Sheet Ricker Hills ENVELOPE(159.167,159.167,-75.683,-75.683) Victoria Land Antarctic Science 21 1 59 69 |
institution |
Open Polar |
collection |
Sapienza Università di Roma: CINECA IRIS |
op_collection_id |
ftunivromairis |
language |
English |
topic |
cosmogenic nuclide erosion rate glacial drift landscape evolution surface exposure dating |
spellingShingle |
cosmogenic nuclide erosion rate glacial drift landscape evolution surface exposure dating Stefan Strasky Luigia Di Nicola Carlo Baroni Heinrich Baur Peter W. Kubik C. Schluechter Rainer Wieler SALVATORE, Maria Cristina Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land |
topic_facet |
cosmogenic nuclide erosion rate glacial drift landscape evolution surface exposure dating |
description |
One of the major issues in (palaeo-) climatology is the response of Antarctic ice sheets to global climate changes. Antarctic ice volume has varied in the past but the extent and timing of these fluctuations are not well known. In this study, we address the question of amplitude and timing of past Antarctic ice level changes by surface exposure dating using in situ produced cosmogenic nuclides (10Be and 21Ne). The study area lies in the Ricker Hills, a nunatak at the boundary of the East Antarctic Ice Sheet in southern Victoria Land. By determining exposure ages of erratic boulders from glacial drifts we directly date East Antarctic Ice Sheet variations. Erosion-corrected neon and beryllium exposure ages indicate that a major ice advance reaching elevations of about 500 m above present ice levels occurred between 1.125 and 1.375 million years before present. Subsequent ice fluctuations were of lesser extent but timing is difficult as all erratic boulders from related deposits show complex exposure histories. Sample-specific erosion rates were on the order of 20–45 cm Ma-1 for a quartzite and 10–65 cm Ma-1 for a sandstone boulder and imply that the modern cold, arid climate has persisted since at least the early Pleistocene. |
author2 |
Stefan, Strasky Luigia Di, Nicola Carlo, Baroni Salvatore, Maria Cristina Heinrich, Baur Peter W., Kubik C., Schluechter Rainer, Wieler |
format |
Article in Journal/Newspaper |
author |
Stefan Strasky Luigia Di Nicola Carlo Baroni Heinrich Baur Peter W. Kubik C. Schluechter Rainer Wieler SALVATORE, Maria Cristina |
author_facet |
Stefan Strasky Luigia Di Nicola Carlo Baroni Heinrich Baur Peter W. Kubik C. Schluechter Rainer Wieler SALVATORE, Maria Cristina |
author_sort |
Stefan Strasky |
title |
Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land |
title_short |
Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land |
title_full |
Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land |
title_fullStr |
Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land |
title_full_unstemmed |
Surface exposure ages imply multiple low-amplitude Pleistocene variations in East Antarctic Ice Sheet, Ricker Hills, Victoria Land |
title_sort |
surface exposure ages imply multiple low-amplitude pleistocene variations in east antarctic ice sheet, ricker hills, victoria land |
publisher |
-Cambridge University Press / New York:40 West 20th Street:New York, NY 10011:(800)872-7423, (212)924-3900, EMAIL: journals_subscriptions@cup.org, INTERNET: http://www.journals.cambridge.org, Fax: (212)691-3239 -Oxford: Blackwell Scientific Publications. |
publishDate |
2009 |
url |
http://hdl.handle.net/11573/37666 https://doi.org/10.1017/s0954102008001478 http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=000263389100005&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=0c7ff228ccbaaa74236f48834a34396a http://www.scopus.com/inward/record.url?eid=2-s2.0-67649226448&partnerID=65&md5=a8d7288bdc46887bd5f9bd4f69d6fbaf |
long_lat |
ENVELOPE(159.167,159.167,-75.683,-75.683) |
geographic |
Antarctic East Antarctic Ice Sheet Ricker Hills Victoria Land |
geographic_facet |
Antarctic East Antarctic Ice Sheet Ricker Hills Victoria Land |
genre |
Antarc* Antarctic Ice Sheet Victoria Land |
genre_facet |
Antarc* Antarctic Ice Sheet Victoria Land |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/WOS:000263389100005 volume:21 issue:1 firstpage:59 lastpage:69 numberofpages:11 journal:ANTARCTIC SCIENCE http://hdl.handle.net/11573/37666 doi:10.1017/s0954102008001478 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-67649226448 http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=000263389100005&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=0c7ff228ccbaaa74236f48834a34396a http://www.scopus.com/inward/record.url?eid=2-s2.0-67649226448&partnerID=65&md5=a8d7288bdc46887bd5f9bd4f69d6fbaf |
op_doi |
https://doi.org/10.1017/s0954102008001478 |
container_title |
Antarctic Science |
container_volume |
21 |
container_issue |
1 |
container_start_page |
59 |
op_container_end_page |
69 |
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