Сибирский федеральный университет

Тип публикации: статья из журнала

Год издания: 2012

Идентификатор DOI: 10.1134/S1028334X12060244

Ключевые слова: Forest decline, Holocenes, Tree line, Earth sciences, Forestry, climate variation, dendrochronology, glacier advance, Holocene, humid environment, paleoclimate, radiocarbon dating, reconstruction, treeline, warming, Forests, Humidification, Altai Mountains

Аннотация: Variations in the tree line position and glacier activity in the Central and Eastern Altai regions in the Holocene were reconstructed on the basis of analysis of sixty radiocarbon and eighteen dendrochronological dates. The tree line was higher than now in the Early and Middle Holocene, and the climate was warmer and, likely, more humid. Glaciers advanced in the forests 300, 1400, and 3000-6000 years ago. In the last millennium the forest decline at the upper tree limit occurred in 1206-1256, 1445-1501, and 1642-1736.

Журнал: DOKLADY EARTH SCIENCES

Выпуск журнала: Vol. 444, Is. 2

Номера страниц: 787-790

ISSN журнала: 1028334X

Место издания: NEW YORK

Издатель: MAIK NAUKA/INTERPERIODICA/SPRINGER

• Nazarov N. (Siberian Federal University)
• Myglan V.S. (Siberian Federal University)
• Solomina O.N. (Institute of Geography,Russian Academy of Sciences)

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