Permafrost and ground ice of the Arctic
Vasil'chuk Y.K. —
Cyclocryostratigraphy of yedoma. Part 2
// Arctic and Antarctica.
– 2017. – ¹ 2.
– P. 54 - 99.
DOI: 10.7256/2453-8922.2017.2.22328 URL: https://en. nbpublish.com/library_read_article.php?id=22328
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The author shows that the purpose of cyclocryostratigraphy is to determine, characterize and interpret periodic or quasiperiodic variations in the cryostratigraphy of permafrost sections (mainly syncriogenic ones) and their use for refining the features of the formation of permafrost. The author formulates the concept of cryocyclitis as a complex of permafrost layers and their associations with ice wedges, characterized by the direction and continuity of the change in the cryostructures properties of the ground ice and its surrounding sediments, reflected in the location of the boundaries between them, which can be seen in a vertical section (in a borehole, outcrop, bore pit, etc.). The main research methods are the radiocarbon, stable isotope and geochemical ones. The study shows that often in the yedoma strata individual cyclites duplicate each other, thus demonstrating a continuous process. The author performs the cyclocryostratigraphic research of the structural features and development of the Late Pleistocene syngenetic ice wedge in the cyclical yedoma of the Asian Arctic: Western Siberia, Yakutia, Chukotka, Novosibirsk Islands, Alaska and northern Canada.Three cycles can be distinguished in the development of syngenetic ice wedges. Microcycles result from the changes in active-layer depth and the accumulation of a thin sedimentlayer over several years. Their vertical scale varies from centimetres to tens of centimetres, and their formation time ranges from one to hundreds of years. Mesocycles result from a change in the lake water level if ice-wedge formation took place on the banks or beneath shallow water. The vertical scale of mesocycles is a few metres, and their timescale usually varies from several hundred to a few thousand years. Macrocycles relate to a major change in the sedimentationregime or rarely – and mostly at the southern border of ice-wedge formation – with major climatic oscillations. The vertical scale of macrocycles numbers tens of metres, and their duration varies usually from many tens to sometimes hundreds of thousands of years.
geo-cryo-cycles, Cryostratigraphy, Chronostratigraphy, yedoma, isotopes, radiocarbon, Late Pleistocene, macro-cycles, meso-cycles, micro-cycles
Vasil'chuk Yu.K., Vasil'chuk A.C., Jungner H., Geyh M., van der Plicht J., Sonninen E., Budantseva N.A. Southern limit of syngenetic ice-wedge formation during the Holocene climatic optimum in north-west Siberia // Earth Cryosphere. Special Issue. Russian Academy of Sciences and Scott Polar Research Institute, University of Cambridge. 2003. P. 19–31.
Kaplina T.N., Lakhtina O.V., Pavlova O.P. Povtorno-zhil'nye l'dy v dolinakh rek Severnogo Zabaykal'ya // Trudy PNIIIS, vyp. 18. M.: Stroyizdat. 1972. S. 183–195.
Gorbunov A.P. K izucheniyu povtorno-zhil'nykh l'dov Mongolii // Verkhniy gorizont tolshch merzlykh porod. Red. P.I.Mel'nikov, Yu.L.Shur. M.: Nauka. 1991. S. 70–76.
Solomatin V.I. Singeneticheskoe i epigeneticheskoe promerzanie morskikh otlozheniy na poberezh'e Pechorskogo morya // Podzemnyy led, vyp. 2. M.: Izd-vo Mosk. un-ta. 1965. S. 183–192.
Murton Ju.B., Edwards M.E., Lozhkin A.V., Anderson P.M., Savvinov G.N., Bakulina N., Bondarenko J.V., Cherepanova M.V., Danilov P.P., Boeskorov V., Goslar T., Grigoriev S.,