Geography and Environmental Science, School of Archaeology, Geography and Environmental Science (SAGES), University of Reading, Whiteknights, Reading, RG6 6AH, UK
Leverhulme Centre for Wildfires, Environment and Society, Imperial College London, South Kensington, London, SW7 2BW, UK
Geography and Environmental Science, School of Archaeology, Geography and Environmental Science (SAGES), University of Reading, Whiteknights, Reading, RG6 6AH, UK
Leverhulme Centre for Wildfires, Environment and Society, Imperial College London, South Kensington, London, SW7 2BW, UK
Marc Vander Linden
Institute for the Modelling of Socio-Environmental Transitions, Bournemouth University, Christchurch House, Talbot Campus, Poole, BH12 5BB, UK
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Total article views: 2,039 (including HTML, PDF, and XML)
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1,625
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131
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PDF: 341
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Total: 2,039
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EndNote: 96
Views and downloads (calculated since 27 May 2024)
Cumulative views and downloads
(calculated since 27 May 2024)
Total article views: 825 (including HTML, PDF, and XML)
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694
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22
825
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Total: 825
Supplement: 50
BibTeX: 349
EndNote: 29
Views and downloads (calculated since 24 Sep 2025)
Cumulative views and downloads
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Total article views: 1,214 (including HTML, PDF, and XML)
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931
232
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1,214
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Total: 1,214
Supplement: 81
BibTeX: 46
EndNote: 67
Views and downloads (calculated since 27 May 2024)
Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 2,039 (including HTML, PDF, and XML)
Thereof 2,039 with geography defined
and 0 with unknown origin.
Total article views: 825 (including HTML, PDF, and XML)
Thereof 825 with geography defined
and 0 with unknown origin.
Total article views: 1,214 (including HTML, PDF, and XML)
Thereof 1,212 with geography defined
and 2 with unknown origin.
Changes in tree cover across Europe during the Holocene are reconstructed from fossil pollen data using a model developed with modern observations of tree cover and modern pollen assemblages. There is a rapid increase in tree cover after the last glacial period, with maximum cover during the mid-Holocene and a decline thereafter; the timing of the maximum and the speed of the increase and subsequent decrease vary regionally, likely reflecting differences in climate trajectories and human influence.
Changes in tree cover across Europe during the Holocene are reconstructed from fossil pollen...