Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic
The Paleocene-Eocene thermal maximum (PETM) has been attributed to a sudden release of carbon dioxide and/or methane. 40 Ar/ 39 Ar age determinations show that the Danish Ash-17 deposit, which overlies the PETM by about 450,000 years in the Atlantic, and the Skraenterne Formation Tuff, representing...
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American Association for the Advancement of Science (AAAS)
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craaas:10.1126/science.1135274 2024-09-30T14:34:17+00:00 Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic Storey, Michael Duncan, Robert A. Swisher, Carl C. 2007 http://dx.doi.org/10.1126/science.1135274 https://www.science.org/doi/pdf/10.1126/science.1135274 en eng American Association for the Advancement of Science (AAAS) Science volume 316, issue 5824, page 587-589 ISSN 0036-8075 1095-9203 journal-article 2007 craaas https://doi.org/10.1126/science.1135274 2024-09-12T04:01:06Z The Paleocene-Eocene thermal maximum (PETM) has been attributed to a sudden release of carbon dioxide and/or methane. 40 Ar/ 39 Ar age determinations show that the Danish Ash-17 deposit, which overlies the PETM by about 450,000 years in the Atlantic, and the Skraenterne Formation Tuff, representing the end of 1 ± 0.5 million years of massive volcanism in East Greenland, are coeval. The relative age of Danish Ash-17 thus places the PETM onset after the beginning of massive flood basalt volcanism at 56.1 ± 0.4 million years ago but within error of the estimated continental breakup time of 55.5 ± 0.3 million years ago, marked by the eruption of mid-ocean ridge basalt–like flows. These correlations support the view that the PETM was triggered by greenhouse gas release during magma interaction with basin-filling carbon-rich sedimentary rocks proximal to the embryonic plate boundary between Greenland and Europe. Article in Journal/Newspaper East Greenland Greenland Northeast Atlantic AAAS Resource Center (American Association for the Advancement of Science) Greenland Science 316 5824 587 589 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
The Paleocene-Eocene thermal maximum (PETM) has been attributed to a sudden release of carbon dioxide and/or methane. 40 Ar/ 39 Ar age determinations show that the Danish Ash-17 deposit, which overlies the PETM by about 450,000 years in the Atlantic, and the Skraenterne Formation Tuff, representing the end of 1 ± 0.5 million years of massive volcanism in East Greenland, are coeval. The relative age of Danish Ash-17 thus places the PETM onset after the beginning of massive flood basalt volcanism at 56.1 ± 0.4 million years ago but within error of the estimated continental breakup time of 55.5 ± 0.3 million years ago, marked by the eruption of mid-ocean ridge basalt–like flows. These correlations support the view that the PETM was triggered by greenhouse gas release during magma interaction with basin-filling carbon-rich sedimentary rocks proximal to the embryonic plate boundary between Greenland and Europe. |
format |
Article in Journal/Newspaper |
author |
Storey, Michael Duncan, Robert A. Swisher, Carl C. |
spellingShingle |
Storey, Michael Duncan, Robert A. Swisher, Carl C. Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic |
author_facet |
Storey, Michael Duncan, Robert A. Swisher, Carl C. |
author_sort |
Storey, Michael |
title |
Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic |
title_short |
Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic |
title_full |
Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic |
title_fullStr |
Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic |
title_full_unstemmed |
Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic |
title_sort |
paleocene-eocene thermal maximum and the opening of the northeast atlantic |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
2007 |
url |
http://dx.doi.org/10.1126/science.1135274 https://www.science.org/doi/pdf/10.1126/science.1135274 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland Northeast Atlantic |
genre_facet |
East Greenland Greenland Northeast Atlantic |
op_source |
Science volume 316, issue 5824, page 587-589 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.1135274 |
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Science |
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316 |
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5824 |
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587 |
op_container_end_page |
589 |
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1811637958540787712 |