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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1,990
461
115
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HTML: 1,990
PDF: 461
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Total: 2,566
Supplement: 185
BibTeX: 416
EndNote: 115
Views and downloads (calculated since 27 May 2024)
Cumulative views and downloads
(calculated since 27 May 2024)
Total article views: 1,351 (including HTML, PDF, and XML)
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1,058
229
64
1,351
104
370
48
HTML: 1,058
PDF: 229
XML: 64
Total: 1,351
Supplement: 104
BibTeX: 370
EndNote: 48
Views and downloads (calculated since 24 Sep 2025)
Cumulative views and downloads
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Total article views: 1,215 (including HTML, PDF, and XML)
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932
232
51
1,215
81
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67
HTML: 932
PDF: 232
XML: 51
Total: 1,215
Supplement: 81
BibTeX: 46
EndNote: 67
Views and downloads (calculated since 27 May 2024)
Cumulative views and downloads
(calculated since 27 May 2024)
Viewed (geographical distribution)
Total article views: 2,566 (including HTML, PDF, and XML)
Thereof 2,566 with geography defined
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Total article views: 1,351 (including HTML, PDF, and XML)
Thereof 1,351 with geography defined
and 0 with unknown origin.
Total article views: 1,215 (including HTML, PDF, and XML)
Thereof 1,213 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...