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Cyclocryostratigraphy of yedoma. Part 2
Vasil'chuk Yurii Kirillovich

Doctor of Geology and Mineralogy

Professor, the department of Geochemistry of Landscapes and Soil Geography, Lomonosov Moscow State University

119991, Russia, Moscow, ul. Leninskie Gory, 1, of. 2009

vasilch_geo@mail.ru
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Abstract.

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.

Keywords: geo-cryo-cycles, Cryostratigraphy, Chronostratigraphy, yedoma, isotopes, radiocarbon, Late Pleistocene, macro-cycles, meso-cycles, micro-cycles

DOI:

10.7256/2453-8922.2017.2.22328

Article was received:

22-05-2017


Review date:

22-05-2017


Publish date:

24-06-2017


This article written in Russian. You can find full text of article in Russian here .

References
1.
Froese D.G., Westgate J.A., Reyes A.V., Enkin R.J., Preece S.J. Ancient Permafrost and a Future, Warmer Arctic // Science. 2008. Vol. 321. No. 5896. P. 1648.
2.
Zimov S.A. Implications of ancient ice // Science. 2009. Vol. 323, N 5915. P. 714–715.
3.
Vasil'chuk Yu.K. Povtorno-zhil'nye l'dy; geterotsiklichnost', geterokhronnost', geterogennost'. M.: Izd-vo Mosk. un-ta. 2006. – 404 c. (Vasil'chuk Yu.K. Ice Wedge: Heterocyclity, Heterogeneity, Heterochroneity)
4.
Vasil'chuk Yu.K. Model' tsiklicheski-pul'siruyushchego formirovaniya singeneticheskikh tolshch s moshchnymi povtorno-zhil'nymi l'dami // Kriosfera Zemli. 1999. Tom 3. № 2. S. 50–61 (Vasil'chuk Yu.K. The model of cyclic-pulsing formation of syngenetic permafrost thickness with ice wedges. Kriosfera Zemli (Earth's Cryosphere). 1999. Vol. III. No. 2. P. 50–61)
5.
Vasil'chuk Yu.K. Izotopno-kislorodnyi sostav podzemnykh l'dov (opyt paleogeokriologicheskikh rekonstruktsii). Izd. Otdel Teoreticheskikh problem RAN. Geol. f-t. MGU, PNIIIS. 1992. V 2-kh tomakh. Tom 1 – 420 s. Tom 2 – 264 s. (Vasil'chuk Yu.K. Oxygen Isotope Composition of Ground Ice (Application to Paleogeocryological Reconstructions).
6.
Vasil'chuk Yu.K., Vasil'chuk A.C. The model of thick syngenetic ice-wedge formation // The 28th International arctic workshop. Arctic and alpine environments, Past and Present. March 12–14, 1998, Boulder, Colorado. Abstracts. P. 157–159.
7.
Vasil'chuk Yu.K., Vasil'chuk A.K. Povtorno-zhil'nye l'dy doliny reki Main i rekonstruktsii zimnikh paleotemperatur vozdukha Yuzhnoi Chukotki 38-12 tys. let nazad // Kriosfera Zemli. 2017. №6 (Vasil'chuk Yu.K., Vasil'chuk A.C. Ice wedges of Mayn River valley and past winter air temperatures records of the Southern Chukotka Peninsula during 38-12 ka BP. Kriosfera Zemli (Earth's Cryosphere). 2017. Vol. XXI. No. 6).
8.
Kotov A.N., Ryabchun V.K. Kriogennyi kompleks pozdnepleistotsenovykh otlozhenii doliny r.Main, chast' 1: Ledovyi obryv, Magadan: SVKNII DVNTs AN SSSR, 1986, 54 s.
9.
Kaplina T.N., Kartashova G.G., Nikitin V.P. Novye dannye o peschanoi tolshche Tuostakhskoi vpadiny // Byulleten' komissii po izucheniyu chetvertichnogo perioda, vyp. 52. M.: Nauka. 1983. S. 107–122.
10.
Lavrushin Yu.A. Allyuvii ravninnykh rek subarkticheskogo poyasa i periglyatsial'nykh oblastei materikovykh oledenenii // Trudy Geolog. in-ta AN SSSR, vyp. 87. M.: izd-vo AN SSSR. 1963, 267 c
11.
Kaplina T.N., Sher A.V. Kriogennoe stroenie, usloviya formirovaniya i vozrast konstrativnoi allyuvial'noi svity Sypnogo Yara na Indigirke // Merzlye porody i snezhnyi pokrov. M.: Nauka, 1977. S. 27–41.
12.
Danilov I.D. Merzlotnye i psevdomerzlotnye klinovidnye deformatsii v osadochnykh porodakh // Problemy kriolitologii, vyp. II. 1972. S. 31–48.
13.
Schirrmeister L., Grosse G., Schwamborn G., Andreev A. A., Meyer H. et al. Late Quaternary history of the accumulation plain north of the Chekanovsky Ridge (Lena Delta, Russia): a multidisciplinary approach // Polar Geography. 2003. Vol. 27. N4. P. 277 – 319.
14.
Schirrmeister L., Oezen D., Geyh M.A. 230Th/U Dating of Frozen Peat, Bol'shoy Lyakhovsky Island (Northern Siberia) // Quaternary Research. 2002. Vol. 57. P. 253–258.
15.
Meyer H., Dereviagin A., Siegert C., Schirmieister L., Hubberten H.-W. Palaeoclimate reconstruction on Big Lyakhovsky Island, North Siberia – hydrogen and oxygen isotopes in ice wedges // Permafrost and Periglacial Processes. 2002. Vol. 13. P. 91–105.
16.
Grosval'd M.G. Razvitie rel'efa Sayano-Tuvinskogo nagor'ya. M.: Nauka. 1965. – 166 s.
17.
Orlova L.A. Novye dannye po radiouglerodnoi khronologii (pozdnechetvertichnykh) ozernykh otlozhenii Todzhinskoi vpadiny (Tuva) // Doklady AN SSSR. 1980. Tom 250. № 6. S. 1427–1430.
18.
Yamskikh A.F., Yamskikh A.A. Dynamics of the Todza ice – dammed lake (Upper Yenisei River, Southern Siberia) during the Late Pleistocene and Holocene // Science Reports of Tohoku University. 7th Series (Geography). 1999. Vol. 49. N2 (Special Issue on the Third International Meeting on Global Continental Palaeohydrology, with an Emphasis on Humid, Temperate and Tectonically Active Zones. Graduate School of Science, Tohoku University Publ. Sendai. Japan. P. 143–159.
19.
Vasil’chuk Yu.K., Alexeev S.V., Arzhannikov S.G., Papesch W., Rank D., Vasil’chuk A.C. First data on isotopic dating of Holocene syngenetic ice wedges from the Myorzlyi Yar area, Upper reaches of Yenisei River // Doclady Earth Sciences. 2002. Vol. 383. N2. P. 225–229.
20.
Alekseev S.V., Arzhannikov S.G., Vasil'chuk Yu.K., Alekseeva L.P. Novye dannye o stroenii i evolyutsii merzlykh tolshch zapadnoi chasti Todzhinskoi kotloviny (Respublika Tyva) // Kriosfera Zemli. 2005. Tom 9. № 3. S. 3–9.
21.
Vasil'chuk Yu.K., Yesikov A.D., Oprunenko Yu.F., Petrova Ye.A., Vasil'chuk A.C. and Sulerzhitskiy L.D. New data on the concentrations of stable oxygen isotopes in syngenetic Late Pleistocene wedge ice of the lower Kolyma River // Transactions (Doclady) of the USSR Academy of Sciences. Earth Science Sections. Published by Scripta Technica, Inc. A Wiley Company. New York. 1985. Vol. 281. N2, P. 91–94.
22.
Vasil'chuk Yu.K., Vasil'chuk A.C. Radiocarbon dating and oxygen isotope variations in Late Pleistocene syngenetic ice-wedges, northern Siberia // Permafrost and Periglacial Processes. 1997. Vol.8. N3. P. 335–345.
23.
Vasil'chuk Yu.K., Vasil'chuk A.K. Izotopno-kislorodnyi sostav povtorno-zhil'nykh l'dov ostrova Aion i paleotemperaturnye rekonstruktsii pozdnego pleistotsena i golotsena severa Chukotki // Vestnik Mosk. un-ta. Seriya geologiya. 2017. N2. (Vasilchuk Yu.K., Vasilchuk A.C. Oxygen-isotope composition of ice wedge ice of the Ayon Island and palaeotemperature reconstructions of the Late Pleistocene and Holocene of the North of Chukotka Peninsula. Moscow University Geology Bulletin. 2017. N2.)
24.
Tumskoi V.E. Osobennosti kriolitogeneza otlozhenii Severnoi Yakutii v srednem neopleistotsene – golotsene // Kriosfera Zemli. 2012. Tom 16, № 1. S. 12–21.
25.
Wetterich S., Tumskoy V., Rudaya N., Kuznetsov V., Maksimov F., Opel T., Meyer H., Andreev A.A., Schirrmeister L. Ice Complex permafrost of MIS5 age in the Dmitry Laptev Strait coastal region (East Siberian Arctic) // Quaternary Science Reviews. 2016. Vol. 147. P. 298–311.
26.
Derevyagin A.Yu., Opel' T., Maier Kh., Shirrmaister L., Vetterikh S. Kriogennoe stroenie i izotopnyi sostav poligonal'no-zhil'nykh obrazovanii berega Oigosskii Yar // Materialy pyatoi konferentsii geokriologov Rossii. MGU imeni M.V.Lomonosova, 14-17 iyunya 2016 g. Tom 2. M.: Universitetskaya kniga. 2016. S. 175–182.
27.
Leffingwell E. de K. Ground-Ice Wedges: The Dominant Form of Ground-Ice on the North Coast of Alaska // The Journal of Geology. 1915. Vol. 23(7). P. 635–654.
28.
Pollard W. The nature and origin of ground ice in the Herschel Island area, Yukon territory // Permafrost – Canada. Proceedings of the Fifth Canadian Permafrost Conference, N54, Collection Nordicana, Centre d'etudes Nordiques, Universite Laval. Quebec: National Research Council of Canada, 1990. P. 23–30.
29.
Kanevskiy M., Shur Y., Fortier D., Jorgenson M. T., Stephani E. Cryostratigraphy of late Pleistocene syngenetic permafrost (yedoma) in northern Alaska, Itkillik River exposure // Quaternary Research. 2011. Vol. 75. P. 584–596.
30.
Lapointe Elmrabti L., Talbot J., Strauss J., Kanevskiy M., Shur Y., Frechette B., Fortier D. Apparent climate and ecological change during MIS 3-MIS 2 in northern Alaska, Itkillik River Yedoma // Arctic Net Annual Scientific Meeting, Poster. Ottawa, Ontario, Canada, 2014 DOI: 10.13140/RG.2.1.2647.2088
31.
Kunitskii V.V., Syromyatnikov I.I., Shirrmaister L., Skachkov Yu.B., Grosse G., Vetterikh S., Grigor'ev M.N. L'distye porody i termodenudatsiya v raione poselka Batagai (Yanskoe ploskogor'e, Vostochnaya Sibir') // Kriosfera Zemli. 2013. Tom 17. №1. S. 56–68.
32.
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., Gubin S.V., Korzun Ju.A., Lupachev A.V., Tikhonov A., Tsygankova V.I., Vasilieva G.V., Zanina O,G. Preliminary paleoenvironmental analysis of permafrost deposits at Batagaika megaslump, Yana Uplands, northeast Siberia |// Quaternary Research. 2017. Vol. 87, Iss.2. P. 314–330.
33.
Solomatin V.I. Singeneticheskoe i epigeneticheskoe promerzanie morskikh otlozhenii na poberezh'e Pechorskogo morya // Podzemnyi led, vyp. 2. M.: Izd-vo Mosk. un-ta. 1965. S. 183–192.
34.
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.
35.
Kaplina T.N., Lakhtina O.V., Pavlova O.P. Povtorno-zhil'nye l'dy v dolinakh rek Severnogo Zabaikal'ya // Trudy PNIIIS, vyp. 18. M.: Stroiizdat. 1972. S. 183–195.
36.
Gorbunov A.P. K izucheniyu povtorno-zhil'nykh l'dov Mongolii // Verkhnii gorizont tolshch merzlykh porod. Red. P.I.Mel'nikov, Yu.L.Shur. M.: Nauka. 1991. S. 70–76.