esoilБюллетень Почвенного института имени В.В. ДокучаеваDokuchaev Soil Bulletin0136-16942312-4202V.V. Dokuchaev Soil Science Institute10.19047/0136-1694-2010-66-29-52esoil-485Research ArticleСтатьиИсследование палеоклимата горных экосистем с помощью метода комплексного группового биологического анализаPALAEOCLIMATE RESEARCH OF MOUNTANEOUS ECOSYSTEMS BY USING THE METHOD OF INTEGRATED GROUP BIOLOGICAL ANALYSISСкрипниковаМарина ИгоревнаSkripnikovaM.noemail@neicon.ruУспенскаяО. Н.UspenskayaO.noemail@neicon.ruПочвенный институт им. В.В. Докучаева РоссельхозакдемииРоссияV.V. Dokuchaev Soil Science InstituteRussian FederationВсероссийский институт овощеводства РоссельхозакадемииРоссияVNIISOKRussian Federation2010111220100662952Copyright © Скрипникова М.И., Успенская О.Н., 20102010Скрипникова М.И., Успенская О.Н.Skripnikova M., Uspenskaya O.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://bulletin.esoil.ru/jour/article/view/485

Рассмотрены методологические вопросы реконструкции изменений климата в различные периоды голоцена методом комплексного группового биологического анализа торфяно-сапропелевых отложений. Возможности метода демонстрируются путем реконструкции климата Карпатской и Алтайской горных систем. Для Сколевских Бескид Карпат палеоклиматические сценарии составлялись с целью уточнения климатических обстановок в периоды массового террасирования горных склонов. Для Западного Алтая построен климатический палеосценарий с целью прогноза сохранности курганов бронзового времени с вечной мерзлотой внутри конструкции.

Methodological issues of climate change reconstruction in different Holocene periods are considered by the method of complex group biological analysis of peat and sapropel deposits. The possibilities of the method are demonstrated by reconstructing the climate of the Carpathian and the Altai mountain systems. For the Skolevsky Beskids of the Carpathians, paleoclimatic scenarios were prepared in order to clarify the climatic conditions during the periods of mass terracing of mountain slopes. A climatic paleoscenario was built for the Western Altai to forecast the safety of the bronze barrows with permafrost inside designs.

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The authors declare that there are no conflicts of interest present.