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Vegetation History and Archaeobotany

, Volume 27, Issue 2, pp 365–379 | Cite as

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

  • Fang Tian
  • Xianyong Cao
  • Anne Dallmeyer
  • Gerrit Lohmann
  • Xu Zhang
  • Jian Ni
  • Andrei Andreev
  • Patricia M. Anderson
  • Anatoly V. Lozhkin
  • Elena Bezrukova
  • Natalia Rudaya
  • Qinghai Xu
  • Ulrike Herzschuh
Original Article

Abstract

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 predicting 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.

Keywords

Siberia China Northern Asia Model-data comparison Pollen Permafrost Vegetation-climate disequilibrium 

Notes

Acknowledgements

The authors would like to express their gratitude to all the palynologists who, either directly or indirectly, contributed their pollen records to the pollen dataset. This research was supported by the German Research Foundation (DFG) and PalMod project (BMBF). Jian Ni was supported by the National Key Research and Development Program of China (2016YFC0502101). The work of Andrei Andreev was also partly performed under the Russian Government Program of Competitive Growth of Kazan Federal University. The work of Natalia Rudaya was founded by the Alexander von Humboldt Foundation (Ref 3.3-RUS-1151158-HFST-E); Ministry of Education and Science of the Russian Federation, Project no. 14.Z50.31.0010 of the Altai State University; Russian Government Program of Competitive Growth of Kazan Federal University; and the Russian Foundation for Basic Research (RFBR), Grant no. 16-55-44065. Additional support was provided to Anatoly Lozhkin by the Russian Foundation for Fundamental Research (15-05-06420) and Russian Academy of Sciences, Far East Branch (15-I-2-067). Cathy Jenks provided help with language editing.

Supplementary material

334_2017_653_MOESM1_ESM.pdf (10 mb)
Supplementary material 1 (PDF 10198 KB)

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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2017

Authors and Affiliations

  • Fang Tian
    • 1
    • 2
  • Xianyong Cao
    • 1
  • Anne Dallmeyer
    • 2
  • Gerrit Lohmann
    • 3
    • 4
  • Xu Zhang
    • 3
  • Jian Ni
    • 5
  • Andrei Andreev
    • 6
    • 7
  • Patricia M. Anderson
    • 8
  • Anatoly V. Lozhkin
    • 9
  • Elena Bezrukova
    • 10
    • 11
  • Natalia Rudaya
    • 7
    • 11
    • 12
    • 13
  • Qinghai Xu
    • 14
  • Ulrike Herzschuh
    • 1
    • 15
    • 16
  1. 1.Research Unit Potsdam, Alfred Wegener InstituteHelmholtz Centre for Polar and Marine ResearchPotsdamGermany
  2. 2.Max Planck Institute for MeteorologyHamburgGermany
  3. 3.Alfred Wegener InstituteHelmholtz Centre for Polar and Marine ResearchBremerhavenGermany
  4. 4.MARUM-Center for Marine Environmental SciencesUniversity of BremenBremenGermany
  5. 5.College of Chemistry and Life SciencesZhejiang Normal UniversityJinhuaChina
  6. 6.Institute of Geology and MineralogyUniversity of CologneCologneGermany
  7. 7.Institute of Geology and Petroleum TechnologiesKazan Federal UniversityKazanRussia
  8. 8.Earth and Space Sciences and Quaternary Research CenterUniversity of WashingtonSeattleUSA
  9. 9.North East Interdisciplinary Science Research InstituteFar East Branch Russian Academy of SciencesMagadanRussia
  10. 10.Vinogradov Institute of Geochemistry, Siberian BranchRussian Academy of SciencesIrkutskRussia
  11. 11.Institute of Archaeology and Ethnography, Siberian BranchRussian Academy of SciencesNovosibirskRussia
  12. 12.Department of Archaeology and EthnographyNovosibirsk State UniversityNovosibirskRussia
  13. 13.Department of Archaeology and EthnographyAltai State UniversityBarnaulRussia
  14. 14.College of Resources and Environment SciencesHebei Normal UniversityShijiazhuangChina
  15. 15.Institute of Earth and Environment ScienceUniversity of PotsdamPotsdamGermany
  16. 16.Institute of Biochemistry and BiologyUniversity of PotsdamPotsdamGermany

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