Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia)
The chronology of Quaternary paleoenvironment and climate in northeastern Siberia is poorly understood due to a lack of reliable numerical age determinations. The best climatic archives are ice-rich permafrost sequences, which are widely distributed in northeastern Siberia. For this study, 230Th/U-a...
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Cambridge University Press (CUP)
2002
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Online Access: | https://epic.awi.de/id/eprint/57874/ https://epic.awi.de/id/eprint/57874/1/Schirrmeister_2002_QR.pdf https://hdl.handle.net/10013/epic.e79a4765-cfba-400f-ac65-4f29c930baae |
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ftawi:oai:epic.awi.de:57874 2024-09-15T18:11:28+00:00 Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) Schirrmeister, L Oezen, D Geyh, MA 2002-01-01 application/pdf https://epic.awi.de/id/eprint/57874/ https://epic.awi.de/id/eprint/57874/1/Schirrmeister_2002_QR.pdf https://hdl.handle.net/10013/epic.e79a4765-cfba-400f-ac65-4f29c930baae unknown Cambridge University Press (CUP) https://epic.awi.de/id/eprint/57874/1/Schirrmeister_2002_QR.pdf Schirrmeister, L. orcid:0000-0001-9455-0596 , Oezen, D. and Geyh, M. (2002) Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) , Quaternary Research, 57 (2), pp. 253-258 . doi:10.1006/qres.2001.2306 <https://doi.org/10.1006/qres.2001.2306> , hdl:10013/epic.e79a4765-cfba-400f-ac65-4f29c930baae EPIC3Quaternary Research, Cambridge University Press (CUP), 57(2), pp. 253-258, ISSN: 0033-5894 Article isiRev 2002 ftawi https://doi.org/10.1006/qres.2001.2306 2024-06-24T04:30:12Z The chronology of Quaternary paleoenvironment and climate in northeastern Siberia is poorly understood due to a lack of reliable numerical age determinations. The best climatic archives are ice-rich permafrost sequences, which are widely distributed in northeastern Siberia. For this study, 230Th/U-ages were determined by thermal ionization mass spectrometry (TIMS) from frozen peat in a permafrost deposit at the southern cliff of the Bol'shoy Lyakhovsky Island (New Siberian Archipelago), west of the Zimov'e River. These yielded a Pre-Eemian "isochron"-corrected 230Th/U- age of 200,900 ± 3400 yr. This result is reliable because permafrost deposits behave as closed systems with respect to uranium and thorium. Our findings suggest that 230Th/U dating of frozen peat in permafrost deposits is a useful tool for the reconstruction of the Middle Quaternary environment of northern Siberia and of the whole Arctic. © 2002 University of Washington. Article in Journal/Newspaper Ice permafrost Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Quaternary Research 57 2 253 258 |
institution |
Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
The chronology of Quaternary paleoenvironment and climate in northeastern Siberia is poorly understood due to a lack of reliable numerical age determinations. The best climatic archives are ice-rich permafrost sequences, which are widely distributed in northeastern Siberia. For this study, 230Th/U-ages were determined by thermal ionization mass spectrometry (TIMS) from frozen peat in a permafrost deposit at the southern cliff of the Bol'shoy Lyakhovsky Island (New Siberian Archipelago), west of the Zimov'e River. These yielded a Pre-Eemian "isochron"-corrected 230Th/U- age of 200,900 ± 3400 yr. This result is reliable because permafrost deposits behave as closed systems with respect to uranium and thorium. Our findings suggest that 230Th/U dating of frozen peat in permafrost deposits is a useful tool for the reconstruction of the Middle Quaternary environment of northern Siberia and of the whole Arctic. © 2002 University of Washington. |
format |
Article in Journal/Newspaper |
author |
Schirrmeister, L Oezen, D Geyh, MA |
spellingShingle |
Schirrmeister, L Oezen, D Geyh, MA Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) |
author_facet |
Schirrmeister, L Oezen, D Geyh, MA |
author_sort |
Schirrmeister, L |
title |
Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) |
title_short |
Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) |
title_full |
Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) |
title_fullStr |
Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) |
title_full_unstemmed |
Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) |
title_sort |
th/u dating of frozen peat, bol'shoy lyakhovsky island (northern siberia) |
publisher |
Cambridge University Press (CUP) |
publishDate |
2002 |
url |
https://epic.awi.de/id/eprint/57874/ https://epic.awi.de/id/eprint/57874/1/Schirrmeister_2002_QR.pdf https://hdl.handle.net/10013/epic.e79a4765-cfba-400f-ac65-4f29c930baae |
genre |
Ice permafrost Siberia |
genre_facet |
Ice permafrost Siberia |
op_source |
EPIC3Quaternary Research, Cambridge University Press (CUP), 57(2), pp. 253-258, ISSN: 0033-5894 |
op_relation |
https://epic.awi.de/id/eprint/57874/1/Schirrmeister_2002_QR.pdf Schirrmeister, L. orcid:0000-0001-9455-0596 , Oezen, D. and Geyh, M. (2002) Th/U dating of frozen peat, Bol'shoy Lyakhovsky Island (northern Siberia) , Quaternary Research, 57 (2), pp. 253-258 . doi:10.1006/qres.2001.2306 <https://doi.org/10.1006/qres.2001.2306> , hdl:10013/epic.e79a4765-cfba-400f-ac65-4f29c930baae |
op_doi |
https://doi.org/10.1006/qres.2001.2306 |
container_title |
Quaternary Research |
container_volume |
57 |
container_issue |
2 |
container_start_page |
253 |
op_container_end_page |
258 |
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1810449068971786240 |