Thermogenic methane release as a cause for the long duration of the PETM
The Paleocene–Eocene Thermal Maximum (PETM) was a period of global warming associated with rapid massive 13C-depleted carbon input, often mentioned as a paleoanalog for future climate change and associated feedbacks. One hypothesized carbon source is intrusive volcanism in the North Atlantic region,...
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ftpubmed:oai:pubmedcentral.nih.gov:5087067 2023-05-15T17:31:46+02:00 Thermogenic methane release as a cause for the long duration of the PETM Frieling, Joost Svensen, Henrik H. Planke, Sverre Cramwinckel, Margot J. Selnes, Haavard Sluijs, Appy 2016-10-25 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5087067/ http://www.ncbi.nlm.nih.gov/pubmed/27790990 https://doi.org/10.1073/pnas.1603348113 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5087067/ http://www.ncbi.nlm.nih.gov/pubmed/27790990 http://dx.doi.org/10.1073/pnas.1603348113 Physical Sciences Text 2016 ftpubmed https://doi.org/10.1073/pnas.1603348113 2017-04-30T00:00:46Z The Paleocene–Eocene Thermal Maximum (PETM) was a period of global warming associated with rapid massive 13C-depleted carbon input, often mentioned as a paleoanalog for future climate change and associated feedbacks. One hypothesized carbon source is intrusive volcanism in the North Atlantic region, but rigid dating lacks. We date thermogenic methane release from a hydrothermal vent and find that it postdates the onset of the PETM but correlates to a period of additional carbon injection within the PETM. This study provides evidence of carbon release during the PETM from a reservoir (i.e., organic matter in sedimentary rocks) and implies that carbon release from the vent systems should be included in all future considerations regarding PETM carbon cycling. Text North Atlantic PubMed Central (PMC) Proceedings of the National Academy of Sciences 113 43 12059 12064 |
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English |
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Physical Sciences |
spellingShingle |
Physical Sciences Frieling, Joost Svensen, Henrik H. Planke, Sverre Cramwinckel, Margot J. Selnes, Haavard Sluijs, Appy Thermogenic methane release as a cause for the long duration of the PETM |
topic_facet |
Physical Sciences |
description |
The Paleocene–Eocene Thermal Maximum (PETM) was a period of global warming associated with rapid massive 13C-depleted carbon input, often mentioned as a paleoanalog for future climate change and associated feedbacks. One hypothesized carbon source is intrusive volcanism in the North Atlantic region, but rigid dating lacks. We date thermogenic methane release from a hydrothermal vent and find that it postdates the onset of the PETM but correlates to a period of additional carbon injection within the PETM. This study provides evidence of carbon release during the PETM from a reservoir (i.e., organic matter in sedimentary rocks) and implies that carbon release from the vent systems should be included in all future considerations regarding PETM carbon cycling. |
format |
Text |
author |
Frieling, Joost Svensen, Henrik H. Planke, Sverre Cramwinckel, Margot J. Selnes, Haavard Sluijs, Appy |
author_facet |
Frieling, Joost Svensen, Henrik H. Planke, Sverre Cramwinckel, Margot J. Selnes, Haavard Sluijs, Appy |
author_sort |
Frieling, Joost |
title |
Thermogenic methane release as a cause for the long duration of the PETM |
title_short |
Thermogenic methane release as a cause for the long duration of the PETM |
title_full |
Thermogenic methane release as a cause for the long duration of the PETM |
title_fullStr |
Thermogenic methane release as a cause for the long duration of the PETM |
title_full_unstemmed |
Thermogenic methane release as a cause for the long duration of the PETM |
title_sort |
thermogenic methane release as a cause for the long duration of the petm |
publisher |
National Academy of Sciences |
publishDate |
2016 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5087067/ http://www.ncbi.nlm.nih.gov/pubmed/27790990 https://doi.org/10.1073/pnas.1603348113 |
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North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5087067/ http://www.ncbi.nlm.nih.gov/pubmed/27790990 http://dx.doi.org/10.1073/pnas.1603348113 |
op_doi |
https://doi.org/10.1073/pnas.1603348113 |
container_title |
Proceedings of the National Academy of Sciences |
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113 |
container_issue |
43 |
container_start_page |
12059 |
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12064 |
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1766129501073309696 |