A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM)
Abstract The response of Arctic Ocean biogeochemistry to subsurface flow driven by permafrost thaw is poorly understood. We present dissolved chloride and water isotopic data from the Chukchi Sea Shelf sediments that reveal the presence of a meteoric subsurface flow enriched in cations with a radiog...
Published in: | Geochemistry, Geophysics, Geosystems |
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Online Access: | https://doi.org/10.1029/2021GC009750 https://doaj.org/article/6860096e25734091bd3e9a4064c7d606 |
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ftdoajarticles:oai:doaj.org/article:6860096e25734091bd3e9a4064c7d606 2023-12-03T10:17:22+01:00 A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) Ji‐Hoon Kim Wei‐Li Hong Marta E. Torres Jong‐Sik Ryu Moo‐Hee Kang Dukki Han Seung‐Il Nam Jin Hur Dong‐Chan Koh Frank Niessen Dong‐Hun Lee Kwangchul Jang James William Buchanan Rae Meilian Chen 2021-08-01T00:00:00Z https://doi.org/10.1029/2021GC009750 https://doaj.org/article/6860096e25734091bd3e9a4064c7d606 EN eng Wiley https://doi.org/10.1029/2021GC009750 https://doaj.org/toc/1525-2027 1525-2027 doi:10.1029/2021GC009750 https://doaj.org/article/6860096e25734091bd3e9a4064c7d606 Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021) subsurface meteoric fluid discharge Arctic element/carbon cycle permafrost EHTM Chukchi Sea Geophysics. Cosmic physics QC801-809 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.1029/2021GC009750 2023-11-05T01:35:57Z Abstract The response of Arctic Ocean biogeochemistry to subsurface flow driven by permafrost thaw is poorly understood. We present dissolved chloride and water isotopic data from the Chukchi Sea Shelf sediments that reveal the presence of a meteoric subsurface flow enriched in cations with a radiogenic Sr fingerprint. This subsurface fluid is also enriched in dissolved inorganic carbon and methane that bear isotopic compositions indicative of a carbon reservoir modified by reactions in a closed system. Such fluid characteristics are in stark contrast with those from other sites in the Chukchi Sea where the pore water composition shows no sign of meteoric input, but reflect typical biogeochemical reactions associated with early diagenetic sequences in marine sediment. The most likely source of the observed subsurface flow at the Chukchi Sea Shelf is from the degradation of permafrost that had extended to the shelf region during the Last Glacial Maximum. Our data suggest that the permafrost‐driven subsurface flow most likely took place during the 2–3°C warming in the Early Holocene Thermal Maximum. This time scale is supported by numerical simulation of pore water profiles, which indicate that a minimum of several thousand years must have passed since the cessation of the subsurface methane‐bearing fluid flow. Article in Journal/Newspaper Arctic Arctic Ocean Chukchi Chukchi Sea permafrost Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Chukchi Sea Geochemistry, Geophysics, Geosystems 22 8 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
subsurface meteoric fluid discharge Arctic element/carbon cycle permafrost EHTM Chukchi Sea Geophysics. Cosmic physics QC801-809 Geology QE1-996.5 |
spellingShingle |
subsurface meteoric fluid discharge Arctic element/carbon cycle permafrost EHTM Chukchi Sea Geophysics. Cosmic physics QC801-809 Geology QE1-996.5 Ji‐Hoon Kim Wei‐Li Hong Marta E. Torres Jong‐Sik Ryu Moo‐Hee Kang Dukki Han Seung‐Il Nam Jin Hur Dong‐Chan Koh Frank Niessen Dong‐Hun Lee Kwangchul Jang James William Buchanan Rae Meilian Chen A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) |
topic_facet |
subsurface meteoric fluid discharge Arctic element/carbon cycle permafrost EHTM Chukchi Sea Geophysics. Cosmic physics QC801-809 Geology QE1-996.5 |
description |
Abstract The response of Arctic Ocean biogeochemistry to subsurface flow driven by permafrost thaw is poorly understood. We present dissolved chloride and water isotopic data from the Chukchi Sea Shelf sediments that reveal the presence of a meteoric subsurface flow enriched in cations with a radiogenic Sr fingerprint. This subsurface fluid is also enriched in dissolved inorganic carbon and methane that bear isotopic compositions indicative of a carbon reservoir modified by reactions in a closed system. Such fluid characteristics are in stark contrast with those from other sites in the Chukchi Sea where the pore water composition shows no sign of meteoric input, but reflect typical biogeochemical reactions associated with early diagenetic sequences in marine sediment. The most likely source of the observed subsurface flow at the Chukchi Sea Shelf is from the degradation of permafrost that had extended to the shelf region during the Last Glacial Maximum. Our data suggest that the permafrost‐driven subsurface flow most likely took place during the 2–3°C warming in the Early Holocene Thermal Maximum. This time scale is supported by numerical simulation of pore water profiles, which indicate that a minimum of several thousand years must have passed since the cessation of the subsurface methane‐bearing fluid flow. |
format |
Article in Journal/Newspaper |
author |
Ji‐Hoon Kim Wei‐Li Hong Marta E. Torres Jong‐Sik Ryu Moo‐Hee Kang Dukki Han Seung‐Il Nam Jin Hur Dong‐Chan Koh Frank Niessen Dong‐Hun Lee Kwangchul Jang James William Buchanan Rae Meilian Chen |
author_facet |
Ji‐Hoon Kim Wei‐Li Hong Marta E. Torres Jong‐Sik Ryu Moo‐Hee Kang Dukki Han Seung‐Il Nam Jin Hur Dong‐Chan Koh Frank Niessen Dong‐Hun Lee Kwangchul Jang James William Buchanan Rae Meilian Chen |
author_sort |
Ji‐Hoon Kim |
title |
A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) |
title_short |
A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) |
title_full |
A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) |
title_fullStr |
A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) |
title_full_unstemmed |
A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) |
title_sort |
pulse of meteoric subsurface fluid discharging into the chukchi sea during the early holocene thermal maximum (ehtm) |
publisher |
Wiley |
publishDate |
2021 |
url |
https://doi.org/10.1029/2021GC009750 https://doaj.org/article/6860096e25734091bd3e9a4064c7d606 |
geographic |
Arctic Arctic Ocean Chukchi Sea |
geographic_facet |
Arctic Arctic Ocean Chukchi Sea |
genre |
Arctic Arctic Ocean Chukchi Chukchi Sea permafrost |
genre_facet |
Arctic Arctic Ocean Chukchi Chukchi Sea permafrost |
op_source |
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021) |
op_relation |
https://doi.org/10.1029/2021GC009750 https://doaj.org/toc/1525-2027 1525-2027 doi:10.1029/2021GC009750 https://doaj.org/article/6860096e25734091bd3e9a4064c7d606 |
op_doi |
https://doi.org/10.1029/2021GC009750 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
22 |
container_issue |
8 |
_version_ |
1784264323636396032 |