Fossil Java Sea corals record Laurentide ice sheet disappearance
The Laurentide ice sheet was the largest late Pleistocene ice mass and the largest contributor to Holocene pre-industrial sea-level rise. While glaciological dates suggest final ice sheet melting between 8 and 6 ka, inversion of sea-level data indicates deglaciation at ca. 7 ka. Here, we present new...
Published in: | Geology |
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Geological Society of America
2023
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Online Access: | http://hdl.handle.net/10754/691520 https://doi.org/10.1130/g51038.1 |
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Open Polar |
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King Abdullah University of Science and Technology: KAUST Repository |
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ftkingabdullahun |
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unknown |
description |
The Laurentide ice sheet was the largest late Pleistocene ice mass and the largest contributor to Holocene pre-industrial sea-level rise. While glaciological dates suggest final ice sheet melting between 8 and 6 ka, inversion of sea-level data indicates deglaciation at ca. 7 ka. Here, we present new chronostratigraphic constraints on Laurentide ice sheet disappearance based on Holocene relative sea-level observations from the tectonically stable north coast of Java, Indonesia. Age-elevation data from the flat upper surfaces of 13 fossil intertidal corals (i.e., microatolls) indicate that the Java Sea experienced a relative sea level of 1.3 ± 0.7 m above present between 6.9 and 5.3 ka. To determine uncaptured relative sea-level trends within the observational uncertainties of this apparently constant highstand, we analyzed the internal structure of three sliced microatolls from the same site to produce a high-resolution data set. These data were used to statistically model relative sea-level rates and trends. Employing the data with the model provided evidence for a short-lived rise of relative sea level from 1.0 ± 0.3 m above present at 6.7 ± 0.1 ka to 1.9 ± 0.3 m above present at 6.4 ± 0.1 ka. The end of this rise likely represents the last input of meltwater from the vast Laurentide ice sheet, which, consequently, collapsed at least 400 yr later than assumed by some widely used models of glacial isostatic adjustment. Incorporating these new results into such predictive models will help to better understand the geographical variability of future sea-level rise as a result of global warming. Financial support for H. Westphal came from the VW foundation through the funding line “Schlüsselthemen,” and for T. Mann from the German Research Foundation (MA 6967/2-1). We thank the Zentrum für moderne Diagnostik (ZEMODI, Bremen) for the X-ray images, Bayu Triyogo Widyantoro and Badan Informasi Geospasial (Indonesia) for providing tide gauge data from Jepara, and RISTEK for providing a research permit (no. ... |
author2 |
Physical Science and Engineering (PSE) Division Leibniz Centre for Tropical Marine Research (ZMT), 28359 Bremen, Germany Helmholtz-Zentrum Potsdam, Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany Department of Geography, National University of Singapore, 117568, Singapore The Australian National University, Research School of Earth Sciences, Canberra, ACT 0200, Australia Department of Earth and Planetary Sciences, Rutgers University, New Brunswick, New Jersey 08901, USA Alfred Wegener Institute for Polar and Marine Research, Wadden Sea Station Sylt, 25992 List, Germany Tonkin and Taylor International Ltd., Auckland 1010, New Zealand Department of Environmental Sciences, Informatics and Statistics, Università Ca’ Foscari, 30172 Venice, Italy Geography Faculty, Gadjah Mada University, 55284 Yogyakarta, Indonesia Department of Geosciences, Universität Bremen, 28359 Bremen, Germany |
format |
Article in Journal/Newspaper |
author |
Mann, Thomas Schöne, Tilo Kench, Paul Lambeck, Kurt Ashe, Erica Kneer, Dominik Beetham, Eddie Illigner, Julia Rovere, Alessio Marfai, Muh Aris Westphal, Hildegard |
spellingShingle |
Mann, Thomas Schöne, Tilo Kench, Paul Lambeck, Kurt Ashe, Erica Kneer, Dominik Beetham, Eddie Illigner, Julia Rovere, Alessio Marfai, Muh Aris Westphal, Hildegard Fossil Java Sea corals record Laurentide ice sheet disappearance |
author_facet |
Mann, Thomas Schöne, Tilo Kench, Paul Lambeck, Kurt Ashe, Erica Kneer, Dominik Beetham, Eddie Illigner, Julia Rovere, Alessio Marfai, Muh Aris Westphal, Hildegard |
author_sort |
Mann, Thomas |
title |
Fossil Java Sea corals record Laurentide ice sheet disappearance |
title_short |
Fossil Java Sea corals record Laurentide ice sheet disappearance |
title_full |
Fossil Java Sea corals record Laurentide ice sheet disappearance |
title_fullStr |
Fossil Java Sea corals record Laurentide ice sheet disappearance |
title_full_unstemmed |
Fossil Java Sea corals record Laurentide ice sheet disappearance |
title_sort |
fossil java sea corals record laurentide ice sheet disappearance |
publisher |
Geological Society of America |
publishDate |
2023 |
url |
http://hdl.handle.net/10754/691520 https://doi.org/10.1130/g51038.1 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
https://pubs.geoscienceworld.org/geology/article/doi/10.1130/G51038.1/623223/Fossil-Java-Sea-corals-record-Laurentide-ice-sheet Mann, T., Schöne, T., Kench, P., Lambeck, K., Ashe, E., Kneer, D., Beetham, E., Illigner, J., Rovere, A., Marfai, M. A., & Westphal, H. (2023). Fossil Java Sea corals record Laurentide ice sheet disappearance. Geology. https://doi.org/10.1130/g51038.1 doi:10.1130/g51038.1 0091-7613 1943-2682 Geology http://hdl.handle.net/10754/691520 |
op_rights |
Archived with thanks to Geological Society of America. The version of record is available from Geology. © 2023 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1130/g51038.1 |
container_title |
Geology |
_version_ |
1787425254433357824 |
spelling |
ftkingabdullahun:oai:repository.kaust.edu.sa:10754/691520 2024-01-07T09:43:57+01:00 Fossil Java Sea corals record Laurentide ice sheet disappearance Mann, Thomas Schöne, Tilo Kench, Paul Lambeck, Kurt Ashe, Erica Kneer, Dominik Beetham, Eddie Illigner, Julia Rovere, Alessio Marfai, Muh Aris Westphal, Hildegard Physical Science and Engineering (PSE) Division Leibniz Centre for Tropical Marine Research (ZMT), 28359 Bremen, Germany Helmholtz-Zentrum Potsdam, Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany Department of Geography, National University of Singapore, 117568, Singapore The Australian National University, Research School of Earth Sciences, Canberra, ACT 0200, Australia Department of Earth and Planetary Sciences, Rutgers University, New Brunswick, New Jersey 08901, USA Alfred Wegener Institute for Polar and Marine Research, Wadden Sea Station Sylt, 25992 List, Germany Tonkin and Taylor International Ltd., Auckland 1010, New Zealand Department of Environmental Sciences, Informatics and Statistics, Università Ca’ Foscari, 30172 Venice, Italy Geography Faculty, Gadjah Mada University, 55284 Yogyakarta, Indonesia Department of Geosciences, Universität Bremen, 28359 Bremen, Germany 2023-05-03 application/pdf http://hdl.handle.net/10754/691520 https://doi.org/10.1130/g51038.1 unknown Geological Society of America https://pubs.geoscienceworld.org/geology/article/doi/10.1130/G51038.1/623223/Fossil-Java-Sea-corals-record-Laurentide-ice-sheet Mann, T., Schöne, T., Kench, P., Lambeck, K., Ashe, E., Kneer, D., Beetham, E., Illigner, J., Rovere, A., Marfai, M. A., & Westphal, H. (2023). Fossil Java Sea corals record Laurentide ice sheet disappearance. Geology. https://doi.org/10.1130/g51038.1 doi:10.1130/g51038.1 0091-7613 1943-2682 Geology http://hdl.handle.net/10754/691520 Archived with thanks to Geological Society of America. The version of record is available from Geology. © 2023 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. https://creativecommons.org/licenses/by/4.0/ Article 2023 ftkingabdullahun https://doi.org/10.1130/g51038.1 2023-12-09T20:20:40Z The Laurentide ice sheet was the largest late Pleistocene ice mass and the largest contributor to Holocene pre-industrial sea-level rise. While glaciological dates suggest final ice sheet melting between 8 and 6 ka, inversion of sea-level data indicates deglaciation at ca. 7 ka. Here, we present new chronostratigraphic constraints on Laurentide ice sheet disappearance based on Holocene relative sea-level observations from the tectonically stable north coast of Java, Indonesia. Age-elevation data from the flat upper surfaces of 13 fossil intertidal corals (i.e., microatolls) indicate that the Java Sea experienced a relative sea level of 1.3 ± 0.7 m above present between 6.9 and 5.3 ka. To determine uncaptured relative sea-level trends within the observational uncertainties of this apparently constant highstand, we analyzed the internal structure of three sliced microatolls from the same site to produce a high-resolution data set. These data were used to statistically model relative sea-level rates and trends. Employing the data with the model provided evidence for a short-lived rise of relative sea level from 1.0 ± 0.3 m above present at 6.7 ± 0.1 ka to 1.9 ± 0.3 m above present at 6.4 ± 0.1 ka. The end of this rise likely represents the last input of meltwater from the vast Laurentide ice sheet, which, consequently, collapsed at least 400 yr later than assumed by some widely used models of glacial isostatic adjustment. Incorporating these new results into such predictive models will help to better understand the geographical variability of future sea-level rise as a result of global warming. Financial support for H. Westphal came from the VW foundation through the funding line “Schlüsselthemen,” and for T. Mann from the German Research Foundation (MA 6967/2-1). We thank the Zentrum für moderne Diagnostik (ZEMODI, Bremen) for the X-ray images, Bayu Triyogo Widyantoro and Badan Informasi Geospasial (Indonesia) for providing tide gauge data from Jepara, and RISTEK for providing a research permit (no. ... Article in Journal/Newspaper Ice Sheet King Abdullah University of Science and Technology: KAUST Repository Geology |