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AMS 14C DATING OF SEYAKHA YEDOMA AND JANUARY AIR PALAEOTEMPERATURES FOR 25–21 CAL KA BP BASED ON THE STABLE ISOTOPE COMPOSITIONS OF SYNGENETIC ICE WEDGES

Published online by Cambridge University Press:  08 April 2022

Yurij Vasil’chuk*
Affiliation:
Department of Geography, Lomonosov Moscow State University, 119991, Moscow, Russia
Alla Vasil’chuk
Affiliation:
Department of Geography, Lomonosov Moscow State University, 119991, Moscow, Russia
Nadine Budantseva
Affiliation:
Department of Geography, Lomonosov Moscow State University, 119991, Moscow, Russia
*
*Corresponding author. Email: [email protected]

Abstract

Yedoma sediments with thick syngenetic ice wedges have been studied on the Yamal Peninsula, northwestern Siberia. The accumulation of yedoma strata occurred under alternating subaqueous-subaerial conditions, and three tiers of ice wedge were formed mainly on subaerial stages. The ice wedges and enclosing sediments were dated, revealing that the ice wedges were formed between 29 and 18 cal ka BP, while the enclosing sediments are generally older, possibly due to contamination with ancient material (especially in the central part of the yedoma). However, the termination of yedoma complex formation was dated not later than 13.5 cal ka BP. Stable oxygen-isotope data for the ice wedges indicate more severe winter climate conditions during 25–21 cal ka BP, when mean January air temperatures were at least 10°C lower that modern ones, favoring syngenetic ice wedge growth. Yedoma accumulation in the western part of northern Siberia does not support the existence here of an ice sheet during the LGM.

Type
Conference Paper
Copyright
© The Author(s), 2022. Published by Cambridge University Press for the Arizona Board of Regents on behalf of the University of Arizona

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Footnotes

Selected Papers from the 3rd Radiocarbon in the Environment Conference, Gliwice, Poland, 5–9 July 2021

References

REFERENCES

Andreev, AA, Tarasov, PE, Siegert, C, Ebel, T, Klimanov, VA, Melles, M, Bobrov, AA, Dereviagin, AYu, Lubinski, DJ, Hubberten, HW. 2003. Late Pleistocene and Holocene vegetation and climate on the northern Taymyr Peninsula, Arctic Russia. Boreas 32:484505.CrossRefGoogle Scholar
Bronk Ramsey, C. 2009. Bayesian analysis of radiocarbon dates. Radiocarbon 51(1):337360.CrossRefGoogle Scholar
Derevyagin, AY, Chizhov, AB, Brezgunov, VS, Siegert, C, Hubberten, HW. 1999. Isotopic composition of ice wedges of Cape Sabler (Lake Taymyr). Kriosfera Zemli 3(3):4149. In Russian with English abstract.Google Scholar
Forman, SL, Ingólfsson, Ó, Gataullin, V, Manley, W, Lokrantz, H. 2002. Late Quaternary stratigraphy, glacial limits, and paleoenvironments of the Marresale Area, western Yamal Peninsula, Russia. Quaternary Research 57(3):355370.CrossRefGoogle Scholar
Forman, SL, Ingólfsson, Ó, Manley, WF, Lokrantz, H. 1999. Late Quaternary stratigraphy of Western Yamal Peninsula, Russia: New constraints on the configuration of the Eurasian ice-sheet. Geology 27(9):807810. doi: 10.1130/0091-7613(1999)027<0807:LQSOWY>2.3.CO;2.2.3.CO;2>CrossRefGoogle Scholar
Forsstrom, L, Greve, R. 2004. Simulation of the Eurasian ice sheet dynamics during the last glaciation. Global and Planetary Change 42(1–4):5981.CrossRefGoogle Scholar
Hughes, ALC, Gyllencreutz, R, Lohne, ØS, Mangerud, J, Svendsen, JI. 2016. The last Eurasian ice sheets—a chronological database and time-slice reconstruction, DATED-1. Boreas 45(1):145.CrossRefGoogle Scholar
Oblogov, GE, Streletskaya, ID, Vasiliev, AA, Gusev, EA, Arslanov, HA. 2012. Quaternary deposits and geocryological conditions of Gydan Bay Coast of the Kara Sea. In: Mel’nikov VP, Drozdov DD, Romanovsky V, editors. Proceedings of the 10th International Conference on Permafrost. Salekhard, June 25–29, 2012. Salekhard. Northern Publisher. p. 293–296.Google Scholar
Reimer, PJ, Austin, WEN, Bard, E, Bayliss, A, Blackwell, PG, Bronk Ramsey, C, Butzin, M, et al. 2020. The IntCal20 Northern Hemisphere radiocarbon age calibration curve (0–55 cal ka BP). Radiocarbon 62(4):725757.CrossRefGoogle Scholar
Streletskaya, ID, Vasiliev, AA, Oblogov, GE, Matyukhin, AG. 2013. Isotope composition of ground ice of Western Yamal (Marre-Sale). Led i sneg 2(122):8392. In Russian with English abstract.Google Scholar
Sulerzhitsky, LD. 1982. The accuracy of radiocarbon ages and reliability of dates. In: Kind N, editor. The Antropogene of the Taimyr Peninsula. Moscow: Nauka. p. 10–17. In Russian.Google Scholar
Svendsen, JI, Alexanderson, H, Astakhov, VI, Demidov, I, Dowdeswell, JA, Funder, S, Gataullin, V, Henriksen, M, Hjort, C, Houmark-Nielsen, M, Hubberten, HW, Ingolfsson, O, Jakobsson, M, Kjaer, KH, Larsen, E, Lokrantz, H, Lunkka, JP, Lysa, A, Mangerud, J, Matiouchkov, A, Murray, A, Moller, P, Niessen, F, Nikolskaya, O, Polyak, L, Saarnisto, M, Siegert, C, Siegert, MJ, Spielhagen, RF, Stein, R. 2004. Late Quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews 23(11–13):12291271.CrossRefGoogle Scholar
Svendsen, JI, Krüger, LC, Mangerud, J, Astakhov, VI, Paus, A, Nazarov, D, Murray, A. 2014. Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5–2. Quaternary Science Reviews 92:409428.CrossRefGoogle Scholar
van der Plicht, J, Aerts, A, Wijma, S, Zonder, A. 1995. First results from the Groningen AMS facility. In Proceedings of the 15th International 14C Conference. Radiocarbon 37(2):657–661.CrossRefGoogle Scholar
Vasil’chuk, YK. 1991. Reconstruction of the paleoclimate of the Late Pleistocene and Holocene on the basis of isotope studies of subsurface ice and waters of the permafrost zone. Water Resources 17(6):640647.Google Scholar
Vasil’chuk, YK. 1992. Oxygen isotope composition of ground ice (application to paleogeocryological reconstructions). 2-vols. Theoretical Problems Department, Moscow, Russian Academy of Sciences and Lomonosov Moscow University Publ. In Russian with English contents section.Google Scholar
Vasil’chuk, YK, Budantseva, NA, Vasil’chuk, AC. 2019. High-resolution oxygen isotope diagram of Late Pleistocene ice wedges of Seyaha yedoma, eastern Yamal Peninsula. Doklady Earth Sciences 487(1):823826.CrossRefGoogle Scholar
Vasil’chuk, YK, Trofimov, VT. 1984. Isotope-oxygen diagram of ice wedges of Western Siberia, its radiological age and paleogeocryological interpretation. Doklady of the Academy of Sciences of the USSR. 275(2): 425428. In Russian.Google Scholar
Vasil’chuk, YK, van der Plicht, J, Jungner, H, Sonninen, E, Vasil’chuk, AC. 2000a. First direct dating of Late Pleistocene ice-wedges by AMS. Earth and Planetary Science Letters 179(2):237242.CrossRefGoogle Scholar
Vasil’chuk, YK, van der Plicht, J, Jungner, H, Vasil’chuk, AC. 2000b. AMS-dating of Late Pleistocene and Holocene syngenetic ice-wedges. Nuclear Instruments and Methods in Physics Research B (172):637–641.CrossRefGoogle Scholar
Vasil’chuk, YK, Vasil’chuk, AC. 2017. Validity of radiocarbon ages of Siberian yedoma. GeoResJ 13: 8395.CrossRefGoogle Scholar
Vasil’chuk, YK, Vasil’chuk, AC. 2020. Syngenetic ice wedges and age of slope yedoma deposits of the foothills of the Kular Ridge. Earth’s Cryosphere XXIV(2):313.Google Scholar
Vasil’chuk, YK, Vasil’chuk, AC, Jungner, H, Korneeva, GA, Budantseva, NA. 1998. Hydrobiochemical composition of syngenetic ices of Seyakha thickness as indicator of Ob Bay level in the Late Pleistocene. Kriosfera Zemli II (1):4854. In Russian with English abstract.Google Scholar