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 Показать полностьюhumid. 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