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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1,686
367
82
2,135
155
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102
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PDF: 367
XML: 82
Total: 2,135
Supplement: 155
BibTeX: 400
EndNote: 102
Views and downloads (calculated since 27 May 2024)
Cumulative views and downloads
(calculated since 27 May 2024)
Total article views: 921 (including HTML, PDF, and XML)
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755
135
31
921
74
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HTML: 755
PDF: 135
XML: 31
Total: 921
Supplement: 74
BibTeX: 354
EndNote: 35
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
51
1,214
81
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67
HTML: 931
PDF: 232
XML: 51
Total: 1,214
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: 2,135 (including HTML, PDF, and XML)
Thereof 2,135 with geography defined
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Total article views: 921 (including HTML, PDF, and XML)
Thereof 921 with geography defined
and 0 with unknown origin.
Total article views: 1,214 (including HTML, PDF, and XML)
Thereof 1,212 with geography defined
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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...