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A 1300-year multi-proxy palaeoecological record from the northwest Putorana Plateau (Russian Subarctic)

Environmental changes, vegetation dynamics and fire history

Dados Bibliográficos

ID12266513
AutoresЕлена Новенко (0000-0003-2174-8467, Lomonosov Moscow State University, autor correspondente), Natalia Mazei (0000-0002-4759-8703, Lomonosov Moscow State University), Dmitry Kupriyanov (0000-0003-1441-4039, Lomonosov Moscow State University), Dmitry A Kupriyanov (Lomonosov Moscow State University), Kirill V Babeshko (0000-0003-4557-4908, Lomonosov Moscow State University), Maria V Kusilman (Lomonosov Moscow State University), I S Zyuganova (0000-0003-2582-8624, Institute of Geography), Andrey N Tsyganov (0000-0002-5660-8432, Lomonosov Moscow State University), Yuri Mazei (0000-0002-5443-8919, Lomonosov Moscow State University), Leanne N Phelps (0000-0002-7385-3907, University of Edinburgh), Basil A S Davis (University of Lausanne), Basil AS Davis (University of Lausanne)
Ano2022
Volume33
Fascículo2
Páginas181-193
Data de publicação2022-11-02
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoThe Holocene (JOURNAL)
Identificadores do periódicoISSN: 0959-6836 • E-ISSN: 1477-0911
EditoraSAGE Publishing (PUBLISHER • US)
DOI10.1177/09596836221131693
OpenAlexW4308137443
IdiomaEN
Referências citadas83

This paper presents a reconstruction of natural environmental dynamics, wildfires and vegetation change in northwest Putorana Plateau during the last 1300 years. The study area is a remote and poorly investigated region of subarctic Siberia, relatively untouched by human impacts, which offers a unique opportunity to examine natural environmental dynamics and climate-vegetation-fire relationships. The paleoenvironmental reconstructions are based on multi-proxy analysis of the Gervi peatland including pollen, plant macrofossil, testate amoebae and charcoal analysis, loss on ignition measurements and AMS radiocarbon dating. The results revealed the main phases of regional paleoenvironmental change: a warm period between 680 and 1200 C.E. (Common Era) corresponding to the Mediaeval Climate Anomaly (MCA), followed by climate cooling during the Little Ice Age (LIA, 1200–1850 C.E.) and subsequent centuries. Climate amelioration during the MCA led to afforestation of northwestern Putorana Plateau and an expansion of spruce extending 70 km northeast of its present geographical range. A quantitative water-table reconstruction was generated using a testate amoebae transfer function and suggested that relatively dry climate conditions during the MCA triggered high fire frequencies. The LIA appeared in the study area as a period of pronounced climate cooling and moderate moistening, which caused an extension of tundra vegetation and a dramatic decline of fire activity. Distinct environmental changes at the study site were detected since 1990 C.E., characterized by a high peat accumulation rate and rising water table. Since 1990 C.E., the macroscopic charcoal accumulation rate in the peat core increased abruptly, suggesting a recent increase in the fire frequency in the study region

Archaeology · Arctic · Climate change · Climatology · Ecosystem · Environmental change · Fire regime · Geography · Holocene · Ice core · Macrofossil · Paleoclimatology · Peat · Physical geography · Plateau (mathematics · Subarctic climate · Testate amoebae · Tundra · Vegetation (pathology · Archaeology and ancient environmental studies · Climate change and permafrost · Environmental Science · Geology and Paleoclimatology Research · Ecology · Geology · Oceanography

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