Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula
A reconstruction of deglaciation and associated sea-level changes on northern James Ross Island, Antarctic Peninsula, based on lithostratigraphical and geomorphological studies, shows that the initial deglaciation of presently ice-free areas occurred slightly before 7400 14C yr BP. Sea-level in conn...
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John Wiley & Sons Inc.
1997
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ftulundlup:oai:lup.lub.lu.se:3e0a23a5-46ee-4af9-9eba-dce523830e1f 2023-05-15T13:40:19+02:00 Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula Hjort, Christian Ingólfsson, Ólafur Möller, Per Lirio, J M 1997 https://lup.lub.lu.se/record/3e0a23a5-46ee-4af9-9eba-dce523830e1f https://doi.org/10.1002/(SICI)1099-1417(199707/08)12:4<259::AID-JQS307>3.0.CO;2-6 eng eng John Wiley & Sons Inc. https://lup.lub.lu.se/record/3e0a23a5-46ee-4af9-9eba-dce523830e1f http://dx.doi.org/10.1002/(SICI)1099-1417(199707/08)12:4<259::AID-JQS307>3.0.CO;2-6 scopus:0000925307 Journal of Quaternary Science; 12(4), pp 259-273 (1997) ISSN: 1099-1417 Geology contributiontojournal/article info:eu-repo/semantics/article text 1997 ftulundlup https://doi.org/10.1002/(SICI)1099-1417(199707/08)12:4<259::AID-JQS307>3.0.CO;2-6 2023-02-01T23:39:04Z A reconstruction of deglaciation and associated sea-level changes on northern James Ross Island, Antarctic Peninsula, based on lithostratigraphical and geomorphological studies, shows that the initial deglaciation of presently ice-free areas occurred slightly before 7400 14C yr BP. Sea-level in connection with the deglaciation was around 30 m a.s.l. A glacier readvance in Brandy Bay, of at least 7 km, with the initial 3 km over land, reached a position off the present coast at ca. 4600 yr BP. The culmination of the advance was of short duration, and by 4300 yr BP the coastal lowlands again were ice-free. A distinct marine level at 16–18 m a.s.l. was contemporaneous with or slightly post-dates the Brandy Bay advance, thus indicating the relative sea-level around 4600–4500 yr BP. Our results from James Ross Island confirm that over large areas in this part of Antarctica the last deglaciation occurred late. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica James Ross Island Ross Island Lund University Publications (LUP) Antarctic Antarctic Peninsula Brandy Bay ENVELOPE(-58.000,-58.000,-63.700,-63.700) Ross Island |
institution |
Open Polar |
collection |
Lund University Publications (LUP) |
op_collection_id |
ftulundlup |
language |
English |
topic |
Geology |
spellingShingle |
Geology Hjort, Christian Ingólfsson, Ólafur Möller, Per Lirio, J M Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula |
topic_facet |
Geology |
description |
A reconstruction of deglaciation and associated sea-level changes on northern James Ross Island, Antarctic Peninsula, based on lithostratigraphical and geomorphological studies, shows that the initial deglaciation of presently ice-free areas occurred slightly before 7400 14C yr BP. Sea-level in connection with the deglaciation was around 30 m a.s.l. A glacier readvance in Brandy Bay, of at least 7 km, with the initial 3 km over land, reached a position off the present coast at ca. 4600 yr BP. The culmination of the advance was of short duration, and by 4300 yr BP the coastal lowlands again were ice-free. A distinct marine level at 16–18 m a.s.l. was contemporaneous with or slightly post-dates the Brandy Bay advance, thus indicating the relative sea-level around 4600–4500 yr BP. Our results from James Ross Island confirm that over large areas in this part of Antarctica the last deglaciation occurred late. |
format |
Article in Journal/Newspaper |
author |
Hjort, Christian Ingólfsson, Ólafur Möller, Per Lirio, J M |
author_facet |
Hjort, Christian Ingólfsson, Ólafur Möller, Per Lirio, J M |
author_sort |
Hjort, Christian |
title |
Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula |
title_short |
Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula |
title_full |
Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula |
title_fullStr |
Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula |
title_full_unstemmed |
Holocene glacial history and sea level changes on James Ross Island, Antarctic Peninsula |
title_sort |
holocene glacial history and sea level changes on james ross island, antarctic peninsula |
publisher |
John Wiley & Sons Inc. |
publishDate |
1997 |
url |
https://lup.lub.lu.se/record/3e0a23a5-46ee-4af9-9eba-dce523830e1f https://doi.org/10.1002/(SICI)1099-1417(199707/08)12:4<259::AID-JQS307>3.0.CO;2-6 |
long_lat |
ENVELOPE(-58.000,-58.000,-63.700,-63.700) |
geographic |
Antarctic Antarctic Peninsula Brandy Bay Ross Island |
geographic_facet |
Antarctic Antarctic Peninsula Brandy Bay Ross Island |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica James Ross Island Ross Island |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica James Ross Island Ross Island |
op_source |
Journal of Quaternary Science; 12(4), pp 259-273 (1997) ISSN: 1099-1417 |
op_relation |
https://lup.lub.lu.se/record/3e0a23a5-46ee-4af9-9eba-dce523830e1f http://dx.doi.org/10.1002/(SICI)1099-1417(199707/08)12:4<259::AID-JQS307>3.0.CO;2-6 scopus:0000925307 |
op_doi |
https://doi.org/10.1002/(SICI)1099-1417(199707/08)12:4<259::AID-JQS307>3.0.CO;2-6 |
_version_ |
1766132212554530816 |