Peatland development and paleoclimate records from the Holocene peat archive in the foothills of the Eastern Sayan Mountains
URI (for links/citations):http://iopscience.iop.org/article/10.1088/1755-1315/138/1/012014/pdf
Родионова, Александра Борисовна
Гренадерова, Анна Валентиновна
Институт экологии и географии
Кафедра экологии и природопользования
Journal Name:IOP Conference Series
Journal Quartile in Scopus:без квартиля
Bibliographic Citation:Родионова, Александра Борисовна. Peatland development and paleoclimate records from the Holocene peat archive in the foothills of the Eastern Sayan Mountains [Текст] / Александра Борисовна Родионова, Анна Валентиновна Гренадерова // IOP Conference Series: Earth and Environmental Science. — 2018. — № 138.
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).