Biome changes and their inferred climatic drivers in northern and eastern continental Asia at selected times since 40 cal ka bp : научное издание

Описание

Тип публикации: статья из журнала

Год издания: 2017

Идентификатор DOI: 10.1007/s00334-017-0653-8

Ключевые слова: China, Model-data comparison, Northern Asia, Permafrost, Pollen, Siberia, Vegetation-climate disequilibrium

Аннотация: Recent global warming is pronounced in high-latitude regions (e.g. northern Asia), and will cause the vegetation to change. Future vegetation trends (e.g. the “arctic greening”) will feed back into atmospheric circulation and the global climate system. Understanding the nature and causes of past vegetation changes is important for Показать полностьюpredicting the composition and distribution of future vegetation communities. Fossil pollen records from 468 sites in northern and eastern Asia were biomised at selected times between 40 cal ka bp and today. Biomes were also simulated using a climate-driven biome model and results from the two approaches compared in order to help understand the mechanisms behind the observed vegetation changes. The consistent biome results inferred by both approaches reveal that long-term and broad-scale vegetation patterns reflect global- to hemispheric-scale climate changes. Forest biomes increase around the beginning of the late deglaciation, become more widespread during the early and middle Holocene, and decrease in the late Holocene in fringe areas of the Asian Summer Monsoon. At the southern and southwestern margins of the taiga, forest increases in the early Holocene and shows notable species succession, which may have been caused by winter warming at ca. 7 cal ka bp. At the northeastern taiga margin (central Yakutia and northeastern Siberia), shrub expansion during the last deglaciation appears to prevent the permafrost from thawing and hinders the northward expansion of evergreen needle-leaved species until ca. 7 cal ka bp. The vegetation-climate disequilibrium during the early Holocene in the taiga-tundra transition zone suggests that projected climate warming will not cause a northward expansion of evergreen needle-leaved species. © 2017 Springer-Verlag GmbH Germany, part of Springer Nature

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Издание

Журнал: Vegetation History and Archaeobotany

Номера страниц: 1-15

ISSN журнала: 09396314

Издатель: Springer New York LLC

Персоны

  • Tian F. (Research Unit Potsdam, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Telegrafenberg A43, Potsdam, Germany, Max Planck Institute for Meteorology, KlimaCampus, Bundesstraße 53, Hamburg, Germany)
  • Cao X. (Research Unit Potsdam, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Telegrafenberg A43, Potsdam, Germany)
  • Dallmeyer A. (Max Planck Institute for Meteorology, KlimaCampus, Bundesstraße 53, Hamburg, Germany)
  • Lohmann G. (Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, Bremerhaven, Germany, MARUM-Center for Marine Environmental Sciences, University of Bremen, Leobener Straße 8, Bremen, Germany)
  • Zhang X. (Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, Bremerhaven, Germany)
  • Ni J. (College of Chemistry and Life Sciences, Zhejiang Normal University, Yingbin Avenue 688, Jinhua, China)
  • Andreev A. (Institute of Geology and Mineralogy, University of Cologne, Zülpicher Straße 49a, Cologne, Germany, Institute of Geology and Petroleum Technologies, Kazan Federal University, Kazan, Russian Federation)
  • Anderson P.M. (Earth and Space Sciences and Quaternary Research Center, University of Washington, Seattle, WA, United States)
  • Lozhkin A.V. (North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Sciences, Magadan, Russian Federation)
  • Bezrukova E. (Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences, ul. Favorskogo 1a, Irkutsk, Russian Federation, Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, pr. Akad. Lavrentieva 17, Novosibirsk, Russian Federation)
  • Rudaya N. (Institute of Geology and Petroleum Technologies, Kazan Federal University, Kazan, Russian Federation, Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, pr. Akad. Lavrentieva 17, Novosibirsk, Russian Federation, Department of Archaeology and Ethnography, Novosibirsk State University, Pirogova 2, Novosibirsk, Russian Federation, Department of Archaeology and Ethnography, Altai State University, Str. Lenina, 61, Barnaul, Russian Federation)
  • Xu Q. (College of Resources and Environment Sciences, Hebei Normal University, Shijiazhuang, China)
  • Herzschuh U. (Research Unit Potsdam, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Telegrafenberg A43, Potsdam, Germany, Institute of Earth and Environment Science, University of Potsdam, Karl-Liebknecht-Straße 24, Potsdam, Germany, Institute of Biochemistry and Biology, University of Potsdam, Karl-Liebknecht-Straße 24, Potsdam, Germany)

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