Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP
Tephrochronology is a powerful tool to correlate and improve the chronology of sedimentaryarchives in the Arctic Ocean. The Aniakchak Caldera Forming Eruption (CFE) in Alaska at3.6 cal kyr BP ejected ash that were found in a widespread layer in Alaska, and as cryptotephrain the Chukchi Sea, Newfound...
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Stockholms universitet, Institutionen för naturgeografi
2019
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ftstockholmuniv:oai:DiVA.org:su-193090 2023-05-15T14:57:56+02:00 Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP Geels, Alexis 2019 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-193090 eng eng Stockholms universitet, Institutionen för naturgeografi http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-193090 info:eu-repo/semantics/openAccess Cryptotephra Aniakchak CFE II Arctic Ocean Chukchi Sea Marine Reservoir Effect Physical Geography Naturgeografi Student thesis info:eu-repo/semantics/bachelorThesis text 2019 ftstockholmuniv 2023-02-23T21:40:47Z Tephrochronology is a powerful tool to correlate and improve the chronology of sedimentaryarchives in the Arctic Ocean. The Aniakchak Caldera Forming Eruption (CFE) in Alaska at3.6 cal kyr BP ejected ash that were found in a widespread layer in Alaska, and as cryptotephrain the Chukchi Sea, Newfoundland, and Greenland. This study presents data from the coreSWERUS-L2-4-PC1 (4PC) taken at a water depth of 120 m in the Chukchi Sea. The sharp peakin tephra shards concentration permitted to clearly place the isochron. Unfortunately, the microprobeanalyses were unsuccessful, however measurements of trace elements were performedwith Laser Ablated-Inductively Coupled Plasma-Mass Spectrometry (LA-ICP-MS). The geochemicalsignature of the Aniakchak 3.6 eruption was ensured with significant trace elementratios. The isochron of the eruption combined with the radiocarbon dates from 4PC permittedto calculate the local marine radiocarbon reservoir age offset DR=36446 years. This value isrelatively low compared to recent estimates in the Chukchi Sea, especially to the neighbouringcore SWERUS-L2-2-PC1 were DR=47760. The DR value of this study is explained by theinfluence of the "young" Atlantic water mixing with the "old" Pacific water at the depth wherethe core was taken. Bachelor Thesis Arctic Arctic Ocean Chukchi Chukchi Sea Greenland Newfoundland Alaska Stockholm University: Publications (DiVA) Arctic Arctic Ocean Chukchi Sea Greenland Pacific |
institution |
Open Polar |
collection |
Stockholm University: Publications (DiVA) |
op_collection_id |
ftstockholmuniv |
language |
English |
topic |
Cryptotephra Aniakchak CFE II Arctic Ocean Chukchi Sea Marine Reservoir Effect Physical Geography Naturgeografi |
spellingShingle |
Cryptotephra Aniakchak CFE II Arctic Ocean Chukchi Sea Marine Reservoir Effect Physical Geography Naturgeografi Geels, Alexis Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP |
topic_facet |
Cryptotephra Aniakchak CFE II Arctic Ocean Chukchi Sea Marine Reservoir Effect Physical Geography Naturgeografi |
description |
Tephrochronology is a powerful tool to correlate and improve the chronology of sedimentaryarchives in the Arctic Ocean. The Aniakchak Caldera Forming Eruption (CFE) in Alaska at3.6 cal kyr BP ejected ash that were found in a widespread layer in Alaska, and as cryptotephrain the Chukchi Sea, Newfoundland, and Greenland. This study presents data from the coreSWERUS-L2-4-PC1 (4PC) taken at a water depth of 120 m in the Chukchi Sea. The sharp peakin tephra shards concentration permitted to clearly place the isochron. Unfortunately, the microprobeanalyses were unsuccessful, however measurements of trace elements were performedwith Laser Ablated-Inductively Coupled Plasma-Mass Spectrometry (LA-ICP-MS). The geochemicalsignature of the Aniakchak 3.6 eruption was ensured with significant trace elementratios. The isochron of the eruption combined with the radiocarbon dates from 4PC permittedto calculate the local marine radiocarbon reservoir age offset DR=36446 years. This value isrelatively low compared to recent estimates in the Chukchi Sea, especially to the neighbouringcore SWERUS-L2-2-PC1 were DR=47760. The DR value of this study is explained by theinfluence of the "young" Atlantic water mixing with the "old" Pacific water at the depth wherethe core was taken. |
format |
Bachelor Thesis |
author |
Geels, Alexis |
author_facet |
Geels, Alexis |
author_sort |
Geels, Alexis |
title |
Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP |
title_short |
Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP |
title_full |
Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP |
title_fullStr |
Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP |
title_full_unstemmed |
Assessing the late Holocene14C reservoir age of theChukchi Sea with the AniakchakCFE II tephra 3.6 kyr BP |
title_sort |
assessing the late holocene14c reservoir age of thechukchi sea with the aniakchakcfe ii tephra 3.6 kyr bp |
publisher |
Stockholms universitet, Institutionen för naturgeografi |
publishDate |
2019 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-193090 |
geographic |
Arctic Arctic Ocean Chukchi Sea Greenland Pacific |
geographic_facet |
Arctic Arctic Ocean Chukchi Sea Greenland Pacific |
genre |
Arctic Arctic Ocean Chukchi Chukchi Sea Greenland Newfoundland Alaska |
genre_facet |
Arctic Arctic Ocean Chukchi Chukchi Sea Greenland Newfoundland Alaska |
op_relation |
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-193090 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766330025024421888 |