This work was funded by Natural Environment Research Council QUEST grant NE/D001578/ to ME and KW, and by grants 15-I-6-073 and 15-I-2-067 from the Russian Academy of Sciences and grant 15-05-06420 from the Russian Foundation for Fundamental Research, Far East Branch to AL. JOK was supported by the European Research Council (313797, COEVOLVE). Partial support for SK came from the Scientific Project of IGM SB RAS no. 0330-2016-0018 (Lab 284)
; this paper is a contribution to the Russian Foundation for Basic Research Project no. 15-05-00678 (SK). A Natural Environment Research Council Independent Research Fellowship (NE/L011859/1) funded M.M.-F.'s contribution. AA's contribution was partly sponsored by the Russian Government Program of Competitive Growth of Kazan Federal University. A data workshop in Southampton was funded by a supplement from the NERC-QUEST programme. A grant from IGBP-PAGES supported EB's and IK's travel. The links to the databases can be found at 10.5285/6aeba247-52d1-4e84-949f-603742af40c1 (NERC) and http://eprints.soton.ac.uk/id/eprint/403426.
Geography and Environment, University of Southampton, Highfield, Southampton, United Kingdom; School of Geography and the Environment, University of Oxford, South Parks Road, Oxford, United Kingdom; North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Science, Magadan, Russian Federation; Quaternary Research Center, University of Washington, Box 351360, Seattle, WA, United States; Institute of Earth Surface Dynamics, University of Lausanne, Lausanne, Switzerland; Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49a, Cologne, Germany; Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences, 1A, Favorsky Str., Irkutsk, Russian Federation; Institute for Monitoring Climatic and Ecological Systems, Siberian Branch, Russian Academy of Sciences, Akademicheski Ave 10/3, Tomsk, Russian Federation; Institute of Botany, CAS, Zámek 1, Průhonice, Czech Republic; Sobolev Institute of Geology and Mineralogy SB RAS, Koptyuga Ave. 3, Novosibirsk, Russian Federation; Novosibirsk State University, Pirogova St. 2, Novosibirsk, Russian Federation; Department of Geography, University of California-Los Angeles, Los Angeles, CA, United States; Faculty of Geography, Lomonosov Moscow State University, Moscow, Russian Federation; Institute of Problems of Development of the North, Siberian Branch of the Russian Academy of Sciences, Russian Federation; Environmental Change Research Centre, University College London, Gower Street, London, United Kingdom; Higher Colleges of Technologies, University City, PO Box 7947, Sharjah, United Arab Emirates; Institute of Natural Management, NAS of Belarus, F. Skorynu Str. 10, Minsk, Belarus
Recommended Citation:
Binney H.,Edwards M.,Macias-Fauria M.,et al. Vegetation of Eurasia from the last glacial maximum to present: Key biogeographic patterns[J]. Quaternary Science Reviews,2017-01-01,157