Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia
Abstract Understanding sea level during the peak of the Last Interglacial (125,000 yrs ago) is important for assessing future ice-sheet dynamics in response to climate change. The coasts and continental shelves of northeastern Australia (Queensland) preserve an extensive Last Interglacial record in...
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Online Access: | https://doi.org/10.1038/s43247-023-00967-3 https://doaj.org/article/25edbd72a97749deb7e6e7d164642941 |
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ftdoajarticles:oai:doaj.org/article:25edbd72a97749deb7e6e7d164642941 2023-10-29T02:37:08+01:00 Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia Alessio Rovere Tamara Pico Fred Richards Michael J. O’Leary Jerry X. Mitrovica Ian D. Goodwin Jacqueline Austermann Konstantin Latychev 2023-09-01T00:00:00Z https://doi.org/10.1038/s43247-023-00967-3 https://doaj.org/article/25edbd72a97749deb7e6e7d164642941 EN eng Nature Portfolio https://doi.org/10.1038/s43247-023-00967-3 https://doaj.org/toc/2662-4435 doi:10.1038/s43247-023-00967-3 2662-4435 https://doaj.org/article/25edbd72a97749deb7e6e7d164642941 Communications Earth & Environment, Vol 4, Iss 1, Pp 1-12 (2023) Geology QE1-996.5 Environmental sciences GE1-350 article 2023 ftdoajarticles https://doi.org/10.1038/s43247-023-00967-3 2023-10-01T00:41:35Z Abstract Understanding sea level during the peak of the Last Interglacial (125,000 yrs ago) is important for assessing future ice-sheet dynamics in response to climate change. The coasts and continental shelves of northeastern Australia (Queensland) preserve an extensive Last Interglacial record in the facies of coastal strandplains onland and fossil reefs offshore. However, there is a discrepancy, amounting to tens of meters, in the elevation of sea-level indicators between offshore and onshore sites. Here, we assess the influence of geophysical processes that may have changed the elevation of these sea-level indicators. We modeled sea-level change due to dynamic topography, glacial isostatic adjustment, and isostatic adjustment due to coral reef loading. We find that these processes caused relative sea-level changes on the order of, respectively, 10 m, 5 m, and 0.3 m. Of these geophysical processes, the dynamic topography predictions most closely match the tilting observed between onshore and offshore sea-level markers. Article in Journal/Newspaper Ice Sheet Directory of Open Access Journals: DOAJ Articles Communications Earth & Environment 4 1 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Geology QE1-996.5 Environmental sciences GE1-350 |
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Geology QE1-996.5 Environmental sciences GE1-350 Alessio Rovere Tamara Pico Fred Richards Michael J. O’Leary Jerry X. Mitrovica Ian D. Goodwin Jacqueline Austermann Konstantin Latychev Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia |
topic_facet |
Geology QE1-996.5 Environmental sciences GE1-350 |
description |
Abstract Understanding sea level during the peak of the Last Interglacial (125,000 yrs ago) is important for assessing future ice-sheet dynamics in response to climate change. The coasts and continental shelves of northeastern Australia (Queensland) preserve an extensive Last Interglacial record in the facies of coastal strandplains onland and fossil reefs offshore. However, there is a discrepancy, amounting to tens of meters, in the elevation of sea-level indicators between offshore and onshore sites. Here, we assess the influence of geophysical processes that may have changed the elevation of these sea-level indicators. We modeled sea-level change due to dynamic topography, glacial isostatic adjustment, and isostatic adjustment due to coral reef loading. We find that these processes caused relative sea-level changes on the order of, respectively, 10 m, 5 m, and 0.3 m. Of these geophysical processes, the dynamic topography predictions most closely match the tilting observed between onshore and offshore sea-level markers. |
format |
Article in Journal/Newspaper |
author |
Alessio Rovere Tamara Pico Fred Richards Michael J. O’Leary Jerry X. Mitrovica Ian D. Goodwin Jacqueline Austermann Konstantin Latychev |
author_facet |
Alessio Rovere Tamara Pico Fred Richards Michael J. O’Leary Jerry X. Mitrovica Ian D. Goodwin Jacqueline Austermann Konstantin Latychev |
author_sort |
Alessio Rovere |
title |
Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia |
title_short |
Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia |
title_full |
Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia |
title_fullStr |
Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia |
title_full_unstemmed |
Influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in Northeastern Australia |
title_sort |
influence of reef isostasy, dynamic topography, and glacial isostatic adjustment on sea-level records in northeastern australia |
publisher |
Nature Portfolio |
publishDate |
2023 |
url |
https://doi.org/10.1038/s43247-023-00967-3 https://doaj.org/article/25edbd72a97749deb7e6e7d164642941 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-12 (2023) |
op_relation |
https://doi.org/10.1038/s43247-023-00967-3 https://doaj.org/toc/2662-4435 doi:10.1038/s43247-023-00967-3 2662-4435 https://doaj.org/article/25edbd72a97749deb7e6e7d164642941 |
op_doi |
https://doi.org/10.1038/s43247-023-00967-3 |
container_title |
Communications Earth & Environment |
container_volume |
4 |
container_issue |
1 |
_version_ |
1781061546277863424 |