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Криотрасологическая индикация палеопочв. / Sheinkman, V. S.; Sedov, S. N.; Rusakov, A. V.; Melnikov, V. P.

в: Earth's Cryosphere, Том 23, № 1, 01.01.2019, стр. 51-62.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Sheinkman, VS, Sedov, SN, Rusakov, AV & Melnikov, VP 2019, 'Криотрасологическая индикация палеопочв', Earth's Cryosphere, Том. 23, № 1, стр. 51-62. https://doi.org/10.21782/KZ1560-7496-2019-151-62

APA

Sheinkman, V. S., Sedov, S. N., Rusakov, A. V., & Melnikov, V. P. (2019). Криотрасологическая индикация палеопочв. Earth's Cryosphere, 23(1), 51-62. https://doi.org/10.21782/KZ1560-7496-2019-151-62

Vancouver

Sheinkman VS, Sedov SN, Rusakov AV, Melnikov VP. Криотрасологическая индикация палеопочв. Earth's Cryosphere. 2019 Янв. 1;23(1):51-62. https://doi.org/10.21782/KZ1560-7496-2019-151-62

Author

Sheinkman, V. S. ; Sedov, S. N. ; Rusakov, A. V. ; Melnikov, V. P. / Криотрасологическая индикация палеопочв. в: Earth's Cryosphere. 2019 ; Том 23, № 1. стр. 51-62.

BibTeX

@article{e4736b678cc7460c8e532e71b67f3793,
title = "Криотрасологическая индикация палеопочв",
abstract = "Freezing of rocks and formation of permafrost affect soils and produce specific signatures in their solid matrix. The macro- and micromorphological signatures of frost effects remain preserved in buried soils and can serve as explicit or implicit traces of past cryogenic environments. They are, respectively, cryoturbation, aggregation and size sorting of soil particles, gleying and peat formation in well drained soils upon impermeable permafrost. Such signatures are used, in terms of the cryotraceological approach, to reconstruct glacial environments during MIS-3 and MIS-2 events of the marine oxygen isotope stratigraphy in different regions.",
keywords = "Cryogenesis, Cryotraceology, Paleosol, Permafrost signatures, Quaternary, Cryogenesis, Cryotraceology, Paleosol, Permafrost signatures, Quaternary",
author = "Sheinkman, {V. S.} and Sedov, {S. N.} and Rusakov, {A. V.} and Melnikov, {V. P.}",
year = "2019",
month = jan,
day = "1",
doi = "10.21782/KZ1560-7496-2019-151-62",
language = "русский",
volume = "23",
pages = "51--62",
journal = "КРИОСФЕРА ЗЕМЛИ",
issn = "1560-7496",
publisher = "Российская академия наук",
number = "1",

}

RIS

TY - JOUR

T1 - Криотрасологическая индикация палеопочв

AU - Sheinkman, V. S.

AU - Sedov, S. N.

AU - Rusakov, A. V.

AU - Melnikov, V. P.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - Freezing of rocks and formation of permafrost affect soils and produce specific signatures in their solid matrix. The macro- and micromorphological signatures of frost effects remain preserved in buried soils and can serve as explicit or implicit traces of past cryogenic environments. They are, respectively, cryoturbation, aggregation and size sorting of soil particles, gleying and peat formation in well drained soils upon impermeable permafrost. Such signatures are used, in terms of the cryotraceological approach, to reconstruct glacial environments during MIS-3 and MIS-2 events of the marine oxygen isotope stratigraphy in different regions.

AB - Freezing of rocks and formation of permafrost affect soils and produce specific signatures in their solid matrix. The macro- and micromorphological signatures of frost effects remain preserved in buried soils and can serve as explicit or implicit traces of past cryogenic environments. They are, respectively, cryoturbation, aggregation and size sorting of soil particles, gleying and peat formation in well drained soils upon impermeable permafrost. Such signatures are used, in terms of the cryotraceological approach, to reconstruct glacial environments during MIS-3 and MIS-2 events of the marine oxygen isotope stratigraphy in different regions.

KW - Cryogenesis

KW - Cryotraceology

KW - Paleosol

KW - Permafrost signatures

KW - Quaternary

KW - Cryogenesis

KW - Cryotraceology

KW - Paleosol

KW - Permafrost signatures

KW - Quaternary

UR - http://www.scopus.com/inward/record.url?scp=85061935031&partnerID=8YFLogxK

UR - http://www.mendeley.com/research/evidence-permafrost-paleosols-cryotraceological-approach

U2 - 10.21782/KZ1560-7496-2019-151-62

DO - 10.21782/KZ1560-7496-2019-151-62

M3 - статья

AN - SCOPUS:85061935031

VL - 23

SP - 51

EP - 62

JO - КРИОСФЕРА ЗЕМЛИ

JF - КРИОСФЕРА ЗЕМЛИ

SN - 1560-7496

IS - 1

ER -

ID: 39858227