References

gesj

GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY

2071-93882542-1565

Russian Geographical Society

10.24057/2071-9388-2014-7-2-49-70

gesj-21

Research Article

ENVIRONMENT

Окружающая среда

14C AGE, STABLE ISOTOPE COMPOSITION AND POLLEN ANALYSIS OF MASSIVE ICE, BOVANENKOVO GAS FIELD, CENTRAL YAMAL PENINSULA

Vasil’Chuk

Yurij K.

vasilch@geol.msu.ru; vasilch_geo@mail.ru

Vasil’Chuk

Alla C.

alla-vasilch@yandex.ru

Budantseva

Nadine A.

nadin.budanceva@mail.ru

Chizhova

Julia N.

eacentr@yandex.ru

Papesch

Wolfgang

wolfgang.papesch@arcs.ac.at

Podborny

Yevgenij Ye.

podborniy@yandex.ru

Department of Landscape Geochemistry and Soil Geography, Lomonosov Moscow State UniversityRussian FederationLaboratory of Geoecology of the North, Lomonosov Moscow State UniversityRussian FederationARC Seibersdorf research GmbH, Abt. Umweltforschung, Seibersdorf, AustriaRussian FederationCenter for Hydro-Ecological Research, St. PetersburgRussian Federation

2014

01062014

724970

2014

Vasil’Chuk Y.K., Vasil’Chuk A.C., Budantseva N.A., Chizhova J.N., Papesch W., Podborny Y.Y.

Данная работа распространяется под лицензией Creative Commons Attribution 4.0.

This work is licensed under a Creative Commons Attribution 4.0 License.

https://ges.rgo.ru/jour/article/view/21

The origin of the massive ice is important for understanding the Quaternary history of the Yamal region and to predict the occurrence of massive ice, which is important for gas exploration and the development of infrastructure. Massive ice bodies occur in the Bovanenkovo gas field area within sediments such as layers, laccoliths, rods and lenses. Maximal thickness of the tabular ice is 28,5 m; mean thickness is about 8 m. Deposits of the third terrace underlying and overlapping the tabular ice had been formed from 25 ka BP to 20 ka BP, according to 14C dates. Oxygen-isotope values (δ18О) of massive ices are ranged from 12, 49‰ up to -22, 95‰. Deuterium (δD) values vary from -91, 7‰ up to -177, 1‰. Deuterium excess (dexc) changes from 3, 4 to 10, 6‰. Both homogenous and contrast distribution δ18О and (δD) vs. depths in massive ice bodies evidences the segregated and/or infiltrated-segregated manner of ice formation. Pollen, spores and algae spectra from ice are similar to pollen characteristics of modern lacustrine and coastal floodplain sediments in the area. The ingression of cold seawaters on a coastal flood plain caused freezing and ice segregation, with the formation of extensive ice layers under the large but shallow lakes. As a result, syngenetic and genetically heterogeneous ice, such as: segregated, infiltrated-segregated, lake bottom congelation ice etc. was formed.

massive icestable isotope compositionpollen14C ageYamal Peninsula

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The authors declare that there are no conflicts of interest present.