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A multimethod dating study of ancient permafrost, Batagay megaslump, east Siberia

Datos Bibliográficos

ID24087947
AutoresJulian B Murton (0000-0002-9469-5856, University of Sussex, autor de correspondencia), Thomas Opel (0000-0003-1315-8256, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Phillip Toms (0000-0003-2149-046X, University of Gloucestershire), Alexander Blinov (Peter the Great St. Petersburg Polytechnic University), Margret Fuchs (0000-0001-7210-1132, Helmholtz-Zentrum Dresden-Rossendorf), Jamie Wood (0000-0003-0923-5511, University of Gloucestershire), Andreas Gärtner (0000-0002-1670-7305, Helmholtz-Zentrum Dresden-Rossendorf), Silke Merchel (0000-0002-8755-3980, Helmholtz-Zentrum Dresden-Rossendorf), Georg Rugel (0000-0002-0176-8842, Helmholtz-Zentrum Dresden-Rossendorf), Grigoriy Savvinov (0000-0002-5324-5410, North-Eastern Federal University), Sebastian Wetterich (0000-0001-9234-1192, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung)
Año2022
Volumen105
Páginas1-22
Fecha de publicación2022-01-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaQuaternary Research (JOURNAL)
Identificadores de la revistaISSN: 0033-5894 • E-ISSN: 1096-0287
EditorialCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/qua.2021.27
OpenAlexW3157885670
IdiomaEN
Citas recibidas5
Referencias citadas99

Dating of ancient permafrost is essential for understanding long-term permafrost stability and interpreting palaeoenvironmental conditions but presents substantial challenges to geochronology. Here, we apply four methods to permafrost from the megaslump at Batagay, east Siberia: (1) optically stimulated luminescence (OSL) dating of quartz, (2) post-infrared infrared-stimulated luminescence (pIRIR) dating of K-feldspar, (3) radiocarbon dating of organic material, and (4) 36 Cl/Cl dating of ice wedges. 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 pIRIR, whereas the latter is more consistent with 36 Cl/Cl ages for older deposits. The lower ice complex developed at least 650 ka, potentially during MIS 16, and represents the oldest dated permafrost in western Beringia and the second-oldest known ice in the Northern Hemisphere. It has survived multiple interglaciations, including the super-interglaciation MIS 11c, though a thaw unconformity and erosional surface indicate at least one episode of permafrost thaw and erosion occurred sometime between MIS 16 and 6. The upper ice complex formed from at least 60 to 30 ka during late MIS 4 to 3. The sand unit above the upper ice complex is dated to MIS 3–2, whereas the sand unit below formed at some time between MIS 4 and 16.

Geochemistry · Geochronology · Geomorphology · Holocene · Interglacial · Marine isotope stage · Optically stimulated luminescence · Permafrost · Quartz · Quaternary · Radiocarbon dating · Radiometric dating · Stadial · Thermoluminescence dating · Climate change and permafrost · Geology · Geology and Paleoclimatology Research · Methane Hydrates and Related Phenomena · Oceanography · Paleontology

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Obras citantes distintas5
Citas por año1,25
Intervalo de citas2022 - 2025 (4)
Velocidad de citaciónrecent
Altamente citadoNo
Tipos de citaNeutras: 3
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