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Structure and evolution of dune massifs in the Vilyui River Basin over the Late Quaternary Period (by the example of the Makhatta and Kysyl-Syr Tukulans). / Pavlova, M. R.; Rudaya, N. A.; Galanin, A. A. et al.

In: Contemporary Problems of Ecology, Vol. 10, No. 4, 01.07.2017, p. 411-422.

Research output: Contribution to journal › Article › peer-review

Harvard

Pavlova, MR, Rudaya, NA, Galanin, AA & Shaposhnikov, GI 2017, 'Structure and evolution of dune massifs in the Vilyui River Basin over the Late Quaternary Period (by the example of the Makhatta and Kysyl-Syr Tukulans)', Contemporary Problems of Ecology, vol. 10, no. 4, pp. 411-422. https://doi.org/10.1134/S1995425517040072

APA

Pavlova, M. R., Rudaya, N. A., Galanin, A. A., & Shaposhnikov, G. I. (2017). Structure and evolution of dune massifs in the Vilyui River Basin over the Late Quaternary Period (by the example of the Makhatta and Kysyl-Syr Tukulans). Contemporary Problems of Ecology, 10(4), 411-422. https://doi.org/10.1134/S1995425517040072

Vancouver

Pavlova MR, Rudaya NA, Galanin AA, Shaposhnikov GI. Structure and evolution of dune massifs in the Vilyui River Basin over the Late Quaternary Period (by the example of the Makhatta and Kysyl-Syr Tukulans). Contemporary Problems of Ecology. 2017 Jul 1;10(4):411-422. doi: 10.1134/S1995425517040072

Author

Pavlova, M. R. ; Rudaya, N. A. ; Galanin, A. A. et al. / Structure and evolution of dune massifs in the Vilyui River Basin over the Late Quaternary Period (by the example of the Makhatta and Kysyl-Syr Tukulans). In: Contemporary Problems of Ecology. 2017 ; Vol. 10, No. 4. pp. 411-422.

BibTeX

@article{1f32a30d1cfb4fbcb314c420bed79dff,
title = "Structure and evolution of dune massifs in the Vilyui River Basin over the Late Quaternary Period (by the example of the Makhatta and Kysyl-Syr Tukulans)",
abstract = "The data of the comprehensive study of deposits of dune sand massifs—the Makhatta and Kysyl-Syr Tukulans—in the Vilyui River Basin (Central Yakutia) are given. We have revealed the structure and preliminarily reconstructed the evolution of tukulans in the Vilyui River basin and the environmental conditions of the surrounding area in the Late Pleistocene–Holocene period (the chronological period of the formation of tukulans) on the basis of lithological and palynological data and 17 radiocarbon datings. It has been revealed that the tukulans should be assigned to eolian deposits formed on sediments of complicated facial structure. We have distinguished four stages in the vegetation evolution within the last 40000-year period and three chronostratigraphical phases in the development of dune massifs.",
keywords = "age model, Central Yakutia, Holocene, lithology, palynology, Pleistocene, radiocarbon dating, tukulan",
author = "Pavlova, {M. R.} and Rudaya, {N. A.} and Galanin, {A. A.} and Shaposhnikov, {G. I.}",
year = "2017",
month = jul,
day = "1",
doi = "10.1134/S1995425517040072",
language = "English",
volume = "10",
pages = "411--422",
journal = "Contemporary Problems of Ecology",
issn = "1995-4255",
publisher = "MAIK NAUKA/INTERPERIODICA/SPRINGER",
number = "4",

}

RIS

TY - JOUR

T1 - Structure and evolution of dune massifs in the Vilyui River Basin over the Late Quaternary Period (by the example of the Makhatta and Kysyl-Syr Tukulans)

AU - Pavlova, M. R.

AU - Rudaya, N. A.

AU - Galanin, A. A.

AU - Shaposhnikov, G. I.

PY - 2017/7/1

Y1 - 2017/7/1

N2 - The data of the comprehensive study of deposits of dune sand massifs—the Makhatta and Kysyl-Syr Tukulans—in the Vilyui River Basin (Central Yakutia) are given. We have revealed the structure and preliminarily reconstructed the evolution of tukulans in the Vilyui River basin and the environmental conditions of the surrounding area in the Late Pleistocene–Holocene period (the chronological period of the formation of tukulans) on the basis of lithological and palynological data and 17 radiocarbon datings. It has been revealed that the tukulans should be assigned to eolian deposits formed on sediments of complicated facial structure. We have distinguished four stages in the vegetation evolution within the last 40000-year period and three chronostratigraphical phases in the development of dune massifs.

AB - The data of the comprehensive study of deposits of dune sand massifs—the Makhatta and Kysyl-Syr Tukulans—in the Vilyui River Basin (Central Yakutia) are given. We have revealed the structure and preliminarily reconstructed the evolution of tukulans in the Vilyui River basin and the environmental conditions of the surrounding area in the Late Pleistocene–Holocene period (the chronological period of the formation of tukulans) on the basis of lithological and palynological data and 17 radiocarbon datings. It has been revealed that the tukulans should be assigned to eolian deposits formed on sediments of complicated facial structure. We have distinguished four stages in the vegetation evolution within the last 40000-year period and three chronostratigraphical phases in the development of dune massifs.

KW - age model

KW - Central Yakutia

KW - Holocene

KW - lithology

KW - palynology

KW - Pleistocene

KW - radiocarbon dating

KW - tukulan

UR - http://www.scopus.com/inward/record.url?scp=85028035604&partnerID=8YFLogxK

U2 - 10.1134/S1995425517040072

DO - 10.1134/S1995425517040072

M3 - Article

AN - SCOPUS:85028035604

VL - 10

SP - 411

EP - 422

JO - Contemporary Problems of Ecology

JF - Contemporary Problems of Ecology

SN - 1995-4255

IS - 4

ER -

ID: 9962659