Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy
Age information from ancient permafrost is key for understanding permafrost formation, stability and decay, and allows for interpreting past climate and environmental conditions over Pleistocene timescales. However, reliable permafrost geochronology is challenging, especially for deposits beyond the...
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Società Geologica Italiana
2021
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Online Access: | https://epic.awi.de/id/eprint/54175/ https://epic.awi.de/id/eprint/54175/1/SWetterich_Batagay_PalaeoArc21_Poster.pdf https://www.socgeol.it/N3668/paleoarc-2021-2nd-international-conference-on-processes-and-palaeo-environmental-changes-in-the-arctic-from-past-to-present.html https://hdl.handle.net/10013/epic.01472b6c-7012-4435-8a4f-af55ff166e08 https://hdl.handle.net/ |
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ftawi:oai:epic.awi.de:54175 |
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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 |
Age information from ancient permafrost is key for understanding permafrost formation, stability and decay, and allows for interpreting past climate and environmental conditions over Pleistocene timescales. However, reliable permafrost geochronology is challenging, especially for deposits beyond the radiocarbon dating limit at about 50,000 years before present. The headwall of the world’s largest retrogressive thaw slump at Batagay in the Yana Upland, East Siberia (67.58 °N, 134.77 °E), exposes four generations of ice and sand–ice (composite) wedges that formed synchronously with permafrost aggradation (Opel et al., 2019). The exposed Batagay stratigraphy separates into a lower ice complex that is covered by a lower sand unit, an upper ice complex and an upper sand unit. Two woody beds below and above the lower sand are remarkable (Murton et al., 2017). We apply four dating methods to disentangle the chronology of the Batagay permafrost archive: opticallystimulated luminescence (OSL) dating of quartz and post-infrared infrared stimulated luminescence (pIR-IRSL) dating of K-feldspar as well as accelerator mass spectrometry-based Cl-36/Cl dating of wedge ice and radiocarbon dating of organic material (Murton et al., under review). All four chronometers produce stratigraphically consistent and comparable ages. However, OSL appears to date Marine Isotope Stage (MIS) 3 to MIS 2 deposits more reliably than pIR-IRSL, whereas the latter is more consistent with Cl-36/Cl ages for older deposits. The age information obtained so far indicates that the Batagay permafrost sequence is discontinuous. The lower ice complex developed at least 650,000 years ago, potentially during MIS 16 and represents the oldest dated permafrost in western Beringia and the second oldest known ice in the Northern Hemisphere. The age of the overlying lower sand is poorly constrained, indicating formation some time during MIS 16–4. The upper ice complex formed during MIS 4–2 and the upper sand during MIS 3–2, respectively. Thus, the ancient ... |
format |
Conference Object |
author |
Wetterich, Sebastian Murton, Julian B. Toms, Phil Wood, Jamie Blinov, Alexander Opel, Thomas Fuchs, Margret Merchel, Silke Rugel, Georg Gärtner, Andreas Savvinov, Grigoriy N. |
spellingShingle |
Wetterich, Sebastian Murton, Julian B. Toms, Phil Wood, Jamie Blinov, Alexander Opel, Thomas Fuchs, Margret Merchel, Silke Rugel, Georg Gärtner, Andreas Savvinov, Grigoriy N. Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy |
author_facet |
Wetterich, Sebastian Murton, Julian B. Toms, Phil Wood, Jamie Blinov, Alexander Opel, Thomas Fuchs, Margret Merchel, Silke Rugel, Georg Gärtner, Andreas Savvinov, Grigoriy N. |
author_sort |
Wetterich, Sebastian |
title |
Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy |
title_short |
Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy |
title_full |
Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy |
title_fullStr |
Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy |
title_full_unstemmed |
Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy |
title_sort |
ancient permafrost of the batagay megaslump (east siberia) – first insights into chronostratigraphy |
publisher |
Società Geologica Italiana |
publishDate |
2021 |
url |
https://epic.awi.de/id/eprint/54175/ https://epic.awi.de/id/eprint/54175/1/SWetterich_Batagay_PalaeoArc21_Poster.pdf https://www.socgeol.it/N3668/paleoarc-2021-2nd-international-conference-on-processes-and-palaeo-environmental-changes-in-the-arctic-from-past-to-present.html https://hdl.handle.net/10013/epic.01472b6c-7012-4435-8a4f-af55ff166e08 https://hdl.handle.net/ |
genre |
Arctic Ice permafrost wedge* Beringia Siberia |
genre_facet |
Arctic Ice permafrost wedge* Beringia Siberia |
op_source |
EPIC3PALAEOARC 2021, 2nd International Conference on ‘Processes and Palaeo-environmental changes in the Arctic: from past to present’, online conference, 2021-05-24-2021-05-28Dipartimento di Scienze della Terra, Università di Pisa, Italia, Società Geologica Italiana |
op_relation |
https://epic.awi.de/id/eprint/54175/1/SWetterich_Batagay_PalaeoArc21_Poster.pdf https://hdl.handle.net/ Wetterich, S. orcid:0000-0001-9234-1192 , Murton, J. B. orcid:0000-0002-9469-5856 , Toms, P. orcid:0000-0003-2149-046X , Wood, J. orcid:0000-0003-0923-5511 , Blinov, A. , Opel, T. orcid:0000-0003-1315-8256 , Fuchs, M. orcid:0000-0001-7210-1132 , Merchel, S. orcid:0000-0002-8755-3980 , Rugel, G. orcid:0000-0002-0176-8842 , Gärtner, A. and Savvinov, G. N. (2021) Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy , PALAEOARC 2021, 2nd International Conference on ‘Processes and Palaeo-environmental changes in the Arctic: from past to present’, online conference, 24 May 2021 - 28 May 2021 . doi:10.3301/ABSGI.2021.02 <https://doi.org/10.3301/ABSGI.2021.02> , hdl:10013/epic.01472b6c-7012-4435-8a4f-af55ff166e08 |
op_doi |
https://doi.org/10.3301/ABSGI.2021.02 |
_version_ |
1766301077830893568 |
spelling |
ftawi:oai:epic.awi.de:54175 2023-05-15T14:27:22+02:00 Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy Wetterich, Sebastian Murton, Julian B. Toms, Phil Wood, Jamie Blinov, Alexander Opel, Thomas Fuchs, Margret Merchel, Silke Rugel, Georg Gärtner, Andreas Savvinov, Grigoriy N. 2021-05 application/pdf https://epic.awi.de/id/eprint/54175/ https://epic.awi.de/id/eprint/54175/1/SWetterich_Batagay_PalaeoArc21_Poster.pdf https://www.socgeol.it/N3668/paleoarc-2021-2nd-international-conference-on-processes-and-palaeo-environmental-changes-in-the-arctic-from-past-to-present.html https://hdl.handle.net/10013/epic.01472b6c-7012-4435-8a4f-af55ff166e08 https://hdl.handle.net/ unknown Società Geologica Italiana https://epic.awi.de/id/eprint/54175/1/SWetterich_Batagay_PalaeoArc21_Poster.pdf https://hdl.handle.net/ Wetterich, S. orcid:0000-0001-9234-1192 , Murton, J. B. orcid:0000-0002-9469-5856 , Toms, P. orcid:0000-0003-2149-046X , Wood, J. orcid:0000-0003-0923-5511 , Blinov, A. , Opel, T. orcid:0000-0003-1315-8256 , Fuchs, M. orcid:0000-0001-7210-1132 , Merchel, S. orcid:0000-0002-8755-3980 , Rugel, G. orcid:0000-0002-0176-8842 , Gärtner, A. and Savvinov, G. N. (2021) Ancient permafrost of the Batagay megaslump (East Siberia) – first insights into chronostratigraphy , PALAEOARC 2021, 2nd International Conference on ‘Processes and Palaeo-environmental changes in the Arctic: from past to present’, online conference, 24 May 2021 - 28 May 2021 . doi:10.3301/ABSGI.2021.02 <https://doi.org/10.3301/ABSGI.2021.02> , hdl:10013/epic.01472b6c-7012-4435-8a4f-af55ff166e08 EPIC3PALAEOARC 2021, 2nd International Conference on ‘Processes and Palaeo-environmental changes in the Arctic: from past to present’, online conference, 2021-05-24-2021-05-28Dipartimento di Scienze della Terra, Università di Pisa, Italia, Società Geologica Italiana Conference notRev 2021 ftawi https://doi.org/10.3301/ABSGI.2021.02 2022-10-02T23:12:39Z Age information from ancient permafrost is key for understanding permafrost formation, stability and decay, and allows for interpreting past climate and environmental conditions over Pleistocene timescales. However, reliable permafrost geochronology is challenging, especially for deposits beyond the radiocarbon dating limit at about 50,000 years before present. The headwall of the world’s largest retrogressive thaw slump at Batagay in the Yana Upland, East Siberia (67.58 °N, 134.77 °E), exposes four generations of ice and sand–ice (composite) wedges that formed synchronously with permafrost aggradation (Opel et al., 2019). The exposed Batagay stratigraphy separates into a lower ice complex that is covered by a lower sand unit, an upper ice complex and an upper sand unit. Two woody beds below and above the lower sand are remarkable (Murton et al., 2017). We apply four dating methods to disentangle the chronology of the Batagay permafrost archive: opticallystimulated luminescence (OSL) dating of quartz and post-infrared infrared stimulated luminescence (pIR-IRSL) dating of K-feldspar as well as accelerator mass spectrometry-based Cl-36/Cl dating of wedge ice and radiocarbon dating of organic material (Murton et al., under review). All four chronometers produce stratigraphically consistent and comparable ages. However, OSL appears to date Marine Isotope Stage (MIS) 3 to MIS 2 deposits more reliably than pIR-IRSL, whereas the latter is more consistent with Cl-36/Cl ages for older deposits. The age information obtained so far indicates that the Batagay permafrost sequence is discontinuous. The lower ice complex developed at least 650,000 years ago, potentially during MIS 16 and represents the oldest dated permafrost in western Beringia and the second oldest known ice in the Northern Hemisphere. The age of the overlying lower sand is poorly constrained, indicating formation some time during MIS 16–4. The upper ice complex formed during MIS 4–2 and the upper sand during MIS 3–2, respectively. Thus, the ancient ... Conference Object Arctic Ice permafrost wedge* Beringia Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |