Vegetation of Central Transbaikalia in the Late Glacial period and Holocene

被引：10

作者：

Reshetova S.A. ^{[1
]}

Bezrukova E.V. ^{[2
]}

Panizzo V. ^{[3
]}

Henderson A. ^{[4
]}

Ptitsyn A.B. ^{[1
]}

Daryin A.V. ^{[5
]}

Kalugin I.A. ^{[5
]}

机构：

[1] Institute of Natural Resources, Ecology and Cryology, Siberian Branch, Russian Academy of Sciences, Chita

[2] Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, Novosibirsk

[3] Environmental Change Research Centre, University College London, London

[4] School of Geography, Politics and Sociology, Newcastle University, Newcastle

[5] Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk

来源：

Geography and Natural Resources | 2013年 / 34卷 / 2期

关键词：

Holocene; lacustrine bottom sediments; Late Glacial period; palynological analysis; radiocarbon dating;

D O I：

10.1134/S1875372813020108

中图分类号：

学科分类号：

摘要：

Presented are the latest findings from investigating bottom sediments in Lake Arakhlei, containing continuous records of the vegetation evolution in the Beklemishevskaya depression and its mountain surroundings for the last 13 500 years. © 2013 Pleiades Publishing, Ltd.

引用

页码：172 / 178

页数：6

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