A decade of in situ cosmogenic 14 C in Antarctica
Abstract Cosmogenic nuclide measurements in glacial deposits extend our knowledge of glacier chronologies beyond the observational record. The short half-life of in situ cosmogenic 14 C makes it particularly useful for studying glacier chronologies, as resulting exposure ages are less sensitive to n...
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Online Access: | http://dx.doi.org/10.1017/aog.2023.13 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000137 |
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crcambridgeupr:10.1017/aog.2023.13 2024-06-09T07:38:32+00:00 A decade of in situ cosmogenic 14 C in Antarctica Nichols, Keir Alexander Natural Environment Research Council 2022 http://dx.doi.org/10.1017/aog.2023.13 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000137 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Annals of Glaciology volume 63, issue 87-89, page 67-72 ISSN 0260-3055 1727-5644 journal-article 2022 crcambridgeupr https://doi.org/10.1017/aog.2023.13 2024-05-15T13:12:39Z Abstract Cosmogenic nuclide measurements in glacial deposits extend our knowledge of glacier chronologies beyond the observational record. The short half-life of in situ cosmogenic 14 C makes it particularly useful for studying glacier chronologies, as resulting exposure ages are less sensitive to nuclide inheritance when compared with more commonly measured, long-lived nuclides. An increasing number of laboratories using an automated process to extract carbon from quartz has led to in situ 14 C measurements in Antarctic samples at an accelerating rate over the past decade, shedding light on deglaciation in Antarctica. In situ 14 C has had the greatest impact in the Weddell Sea Embayment, where inferences on the thickness of ice and timing of deglaciation were limited by inheritance in other cosmogenic nuclide systems. Future subglacial measurements of the nuclide hold much potential as they can provide direct evidence of proposed Holocene thinning and subsequent re-thickening of parts of the Antarctic ice sheets. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Antarctica Weddell Sea Cambridge University Press Antarctic The Antarctic Weddell Weddell Sea Annals of Glaciology 1 6 |
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Cambridge University Press |
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English |
description |
Abstract Cosmogenic nuclide measurements in glacial deposits extend our knowledge of glacier chronologies beyond the observational record. The short half-life of in situ cosmogenic 14 C makes it particularly useful for studying glacier chronologies, as resulting exposure ages are less sensitive to nuclide inheritance when compared with more commonly measured, long-lived nuclides. An increasing number of laboratories using an automated process to extract carbon from quartz has led to in situ 14 C measurements in Antarctic samples at an accelerating rate over the past decade, shedding light on deglaciation in Antarctica. In situ 14 C has had the greatest impact in the Weddell Sea Embayment, where inferences on the thickness of ice and timing of deglaciation were limited by inheritance in other cosmogenic nuclide systems. Future subglacial measurements of the nuclide hold much potential as they can provide direct evidence of proposed Holocene thinning and subsequent re-thickening of parts of the Antarctic ice sheets. |
author2 |
Natural Environment Research Council |
format |
Article in Journal/Newspaper |
author |
Nichols, Keir Alexander |
spellingShingle |
Nichols, Keir Alexander A decade of in situ cosmogenic 14 C in Antarctica |
author_facet |
Nichols, Keir Alexander |
author_sort |
Nichols, Keir Alexander |
title |
A decade of in situ cosmogenic 14 C in Antarctica |
title_short |
A decade of in situ cosmogenic 14 C in Antarctica |
title_full |
A decade of in situ cosmogenic 14 C in Antarctica |
title_fullStr |
A decade of in situ cosmogenic 14 C in Antarctica |
title_full_unstemmed |
A decade of in situ cosmogenic 14 C in Antarctica |
title_sort |
decade of in situ cosmogenic 14 c in antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
2022 |
url |
http://dx.doi.org/10.1017/aog.2023.13 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000137 |
geographic |
Antarctic The Antarctic Weddell Weddell Sea |
geographic_facet |
Antarctic The Antarctic Weddell Weddell Sea |
genre |
Annals of Glaciology Antarc* Antarctic Antarctica Weddell Sea |
genre_facet |
Annals of Glaciology Antarc* Antarctic Antarctica Weddell Sea |
op_source |
Annals of Glaciology volume 63, issue 87-89, page 67-72 ISSN 0260-3055 1727-5644 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1017/aog.2023.13 |
container_title |
Annals of Glaciology |
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1 |
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6 |
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1801373566389714944 |