The Holocene palaeoecology of the palsa mire near Igarka (Yenisei Siberia) | Научно-инновационный портал СФУ

The Holocene palaeoecology of the palsa mire near Igarka (Yenisei Siberia)

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

Конференция: 6th International Field Symposium on West Siberian Peatlands and Carbon Cycle: Past and Present

Год издания: 2022

Идентификатор DOI: 10.1088/1755-1315/1093/1/012029

Аннотация: The paper presents a new paleoecological evidence covering the last 6500 years based on detailed AMS radiocarbon dating, plant macrofossils, loss on ignition and macroscopic charcoal records from a 8 m long peat sequence, obtained from the palsa mire situated near Igarka (Yenisei Siberia). The obtained data show that the peatland initiation, development of the perennial frost mound and local vegetation history were strongly influenced by the Holocene climatic fluctuations and permafrost dynamics. The main stages of palsa uplift occurred at about 5360 cal yr BP and 2250 cal yr BP and coincided with the periods of cooling in the Russian Arctic region. According to the radiocarbon dating and plant macrofossil analysis of the upper part of peat sequences the peat accumulation rate in the palsa decreased significantly during the last 2000 years. Nevertheless, we consider that the rate of the peat vertical growth could be underestimated due to the disturbance of the frost mound, water erosion and wildfires. © 2022 Institute of Physics Publishing. All rights reserved.

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Издание

Журнал: IOP Conference Series: Earth and Environmental Science

Выпуск журнала: Vol. 1093, Is. 1

Номера страниц: 12029

ISSN журнала: 17551307

Издатель: Institute of Physics

Персоны

  • Novenko E.Yu. (Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991, Russian Federation, Institute of Geography, Russian Academy of Science, Staromonetny lane, 29, Moscow, 119017, Russian Federation)
  • Mazei N.G. (Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991, Russian Federation)
  • Prokushkin A.S. (Sukachev Institute of Forest SB RAS, Federal Research Center “Krasnoyarsk Science Center SB RAS”, Academgorodok 50/28, Krasnoyarsk, 660036, Russian Federation, Siberian Federal University, pr. Svobodny 79, Krasnoyarsk, 660041, Russian Federation)
  • Kupryanov D.A. (Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991, Russian Federation)
  • Shatunov A.E. (Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991, Russian Federation)
  • Andreev R.A. (Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, 119991, Russian Federation)
  • Serikov S.I. (Igarka Geocryology Laboratory, Melnikov Institute of Permafrost SB RAS, 1-st District, Igarka, 663200, Russian Federation)

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