Evidence for a rapid sea-level rise 7600 yr ago
Dating the transgression and subsequent regression in marginal basins of the southeastern Swedish Baltic Sea provides a new perspective of global ice-volume changes and the isostatic adjustment of the mantle after the retreat of the Scandinavian Ice Sheet from this area. Super-imposed upon a smooth...
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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/21720 2024-01-14T10:07:41+01:00 Evidence for a rapid sea-level rise 7600 yr ago Yu, Shi-Yong Berglund, Björn E Sandgren, Per Lambeck, Kurt http://hdl.handle.net/1885/21720 https://doi.org/10.1130/G23859A.1 https://openresearch-repository.anu.edu.au/bitstream/1885/21720/5/u4352516xPUB18_Lambeck.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/21720/7/01_Yu_Evidence_for_a_rapid_sea-level_2007.pdf.jpg unknown Geological Society of America Inc 0091-7613 http://hdl.handle.net/1885/21720 doi:10.1130/G23859A.1 https://openresearch-repository.anu.edu.au/bitstream/1885/21720/5/u4352516xPUB18_Lambeck.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/21720/7/01_Yu_Evidence_for_a_rapid_sea-level_2007.pdf.jpg Geology Keywords: Crustal rebound Sea level rise Geochronology Hydrogeology Lakes Oceanography glacial rebound Holocene isostasy Scandinavian Ice Sheet sea level change transgression-regression cycle Atlantic Ocean Baltic Sea Baltic sea Crustal rebound Lake isolation Laurentide Ice Sheet decay Rapid sea-level rise Journal article ftanucanberra https://doi.org/10.1130/G23859A.1 2023-12-15T09:37:19Z Dating the transgression and subsequent regression in marginal basins of the southeastern Swedish Baltic Sea provides a new perspective of global ice-volume changes and the isostatic adjustment of the mantle after the retreat of the Scandinavian Ice Sheet from this area. Super-imposed upon a smooth pattern of local sea-level rise, acceleration occurred ca. 7600 calibrated (cal) yr B.P., evidenced as a nearly synchronous flooding in six elevated basins ranging from 3.0 to 7.2 m above present sea level. We ascribe this rapid local sea-level rise of ∼4.5 m to a sudden increase in ocean mass, most likely caused by the final decay of the Labrador sector of the Laurentide Ice Sheet. The subsequent monotonic fall of local sea level from ca. 6500 cal yr B.P. to the present is mainly an expression of the slow isostatic adjustment of the mantle. Article in Journal/Newspaper Ice Sheet Australian National University: ANU Digital Collections Geology 35 10 891 |
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Open Polar |
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Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
unknown |
topic |
Keywords: Crustal rebound Sea level rise Geochronology Hydrogeology Lakes Oceanography glacial rebound Holocene isostasy Scandinavian Ice Sheet sea level change transgression-regression cycle Atlantic Ocean Baltic Sea Baltic sea Crustal rebound Lake isolation Laurentide Ice Sheet decay Rapid sea-level rise |
spellingShingle |
Keywords: Crustal rebound Sea level rise Geochronology Hydrogeology Lakes Oceanography glacial rebound Holocene isostasy Scandinavian Ice Sheet sea level change transgression-regression cycle Atlantic Ocean Baltic Sea Baltic sea Crustal rebound Lake isolation Laurentide Ice Sheet decay Rapid sea-level rise Yu, Shi-Yong Berglund, Björn E Sandgren, Per Lambeck, Kurt Evidence for a rapid sea-level rise 7600 yr ago |
topic_facet |
Keywords: Crustal rebound Sea level rise Geochronology Hydrogeology Lakes Oceanography glacial rebound Holocene isostasy Scandinavian Ice Sheet sea level change transgression-regression cycle Atlantic Ocean Baltic Sea Baltic sea Crustal rebound Lake isolation Laurentide Ice Sheet decay Rapid sea-level rise |
description |
Dating the transgression and subsequent regression in marginal basins of the southeastern Swedish Baltic Sea provides a new perspective of global ice-volume changes and the isostatic adjustment of the mantle after the retreat of the Scandinavian Ice Sheet from this area. Super-imposed upon a smooth pattern of local sea-level rise, acceleration occurred ca. 7600 calibrated (cal) yr B.P., evidenced as a nearly synchronous flooding in six elevated basins ranging from 3.0 to 7.2 m above present sea level. We ascribe this rapid local sea-level rise of ∼4.5 m to a sudden increase in ocean mass, most likely caused by the final decay of the Labrador sector of the Laurentide Ice Sheet. The subsequent monotonic fall of local sea level from ca. 6500 cal yr B.P. to the present is mainly an expression of the slow isostatic adjustment of the mantle. |
format |
Article in Journal/Newspaper |
author |
Yu, Shi-Yong Berglund, Björn E Sandgren, Per Lambeck, Kurt |
author_facet |
Yu, Shi-Yong Berglund, Björn E Sandgren, Per Lambeck, Kurt |
author_sort |
Yu, Shi-Yong |
title |
Evidence for a rapid sea-level rise 7600 yr ago |
title_short |
Evidence for a rapid sea-level rise 7600 yr ago |
title_full |
Evidence for a rapid sea-level rise 7600 yr ago |
title_fullStr |
Evidence for a rapid sea-level rise 7600 yr ago |
title_full_unstemmed |
Evidence for a rapid sea-level rise 7600 yr ago |
title_sort |
evidence for a rapid sea-level rise 7600 yr ago |
publisher |
Geological Society of America Inc |
url |
http://hdl.handle.net/1885/21720 https://doi.org/10.1130/G23859A.1 https://openresearch-repository.anu.edu.au/bitstream/1885/21720/5/u4352516xPUB18_Lambeck.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/21720/7/01_Yu_Evidence_for_a_rapid_sea-level_2007.pdf.jpg |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geology |
op_relation |
0091-7613 http://hdl.handle.net/1885/21720 doi:10.1130/G23859A.1 https://openresearch-repository.anu.edu.au/bitstream/1885/21720/5/u4352516xPUB18_Lambeck.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/21720/7/01_Yu_Evidence_for_a_rapid_sea-level_2007.pdf.jpg |
op_doi |
https://doi.org/10.1130/G23859A.1 |
container_title |
Geology |
container_volume |
35 |
container_issue |
10 |
container_start_page |
891 |
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1788062083475046400 |