Peatland development and paleoclimate records from the Holocene peat archive in the foothills of the Eastern Sayan Mountains

Тип публикации: доклад, тезисы доклада, статья из сборника материалов конференций

Конференция: International field symposium on West Siberian Peatlands and Carbon Cycle - Past and Present / International Conference on Carbon Balance of Western Siberian Mires in the Context of Climate Change; Khanty Mansiysk, RUSSIA; Khanty Mansiysk, RUSSIA

Год издания: 2018

Идентификатор DOI: 10.1088/1755-1315/138/1/012014

Аннотация: Plant macrofossils data were used to identify the successive peatland communities during the last 3500 years in the floodplain of the Mana River (foothills of the Eastern Sayan Mountains). The reconstruction of the peatland development indicated that the peatland in the Mana River basin formed about 3500 years ago. The peatland formed as a result of overgrowing floodplain and water logging of terrace lows. The authors observed three successive changes: birch forest with sedge and hypnum mosses in the second half of the Subboreal period, wood-marsh plant association at the start of the Middle Subatlantic period (1600 years BP), the herb-wort phytocoenosis with inclusions of mezoeutrophycal plant species have been growing since the Late Subboreal period (950 years BP). © Published under licence by IOP Publishing Ltd.

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Издание

Журнал: IOP Conference Series: Earth and Environmental Science

Выпуск журнала: Vol. 138, Is. 1

ISSN журнала: 17551307

Издатель: Institute of Physics Publishing

Авторы

  • Rodionova A.B. (Siberian Fed Univ, Inst Ecol & Geog, Dept Ecol & Environm Studies, 79 Svobodny Pr, Krasnoyarsk 660041, Russia)
  • Grenaderova A.V (Siberian Fed Univ, Inst Ecol & Geog, Dept Ecol & Environm Studies, 79 Svobodny Pr, Krasnoyarsk 660041, Russia)

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