Large Scale Anthropogenic Reduction of Forest Cover in Last Glacial Maximum Europe

Type Article
Date 2016-11
Language English
Author(s) Kaplan Jed O.1, Pfeiffer Mirjam2, Kolen Jan C. A.3, Davis Basil A. S.1
Affiliation(s) 1 : Univ Lausanne, Inst Earth Surface Dynam, Geopolis, Lausanne, Switzerland.
2 : Biodivers & Climate Res Ctr BiK F, Frankfurt, Germany.
3 : Leiden Univ, Fac Archaeol, Leiden, Netherlands.
Source Plos One (1932-6203) (Public Library Science), 2016-11 , Vol. 11 , N. 11 , P. e0166726 (1-17)
DOI 10.1371/journal.pone.0166726
WOS© Times Cited 49
Abstract

Reconstructions of the vegetation of Europe during the Last Glacial Maximum (LGM) are an enigma. Pollen-based analyses have suggested that Europe was largely covered by steppe and tundra, and forests persisted only in small refugia. Climate-vegetation model simulations on the other hand have consistently suggested that broad areas of Europe would have been suitable for forest, even in the depths of the last glaciation. Here we reconcile models with data by demonstrating that the highly mobile groups of hunter-gatherers that inhabited Europe at the LGM could have substantially reduced forest cover through the ignition of wildfires. Similar to hunter-gatherers of the more recent past, Upper Paleolithic humans were masters of the use of fire, and preferred inhabiting semi-open landscapes to facilitate foraging, hunting and travel. Incorporating human agency into a dynamic vegetation-fire model and simulating forest cover shows that even small increases in wildfire frequency over natural background levels resulted in large changes in the forested area of Europe, in part because trees were already stressed by low atmospheric CO2 concentrations and the cold, dry, and highly variable climate. Our results suggest that the impact of humans on the glacial landscape of Europe may be one of the earliest large-scale anthropogenic modifications of the earth system.

Full Text
File Pages Size Access
Publisher's official version 17 2 MB Open access
S1 Fig. Tree cover in simulations with and without human burning. 1 5 MB Open access
S2 Fig. Simulated forager population density and associated reduction in tree cover. 1 5 MB Open access
S3 Fig. Change in burned area fraction between LGM and the Preindustrial Holocene (PIH). 1 9 MB Open access
S1 Table. 150-year mean burned area for the map area covered by Fig 1 for the eight different GCM climate input scenarios, and one scenario using the mean climatology of the 8 different scenarios. 1 70 KB Open access
S2 Table. 150-year mean tree cover for the map area covered by Fig 2 for the eight different GCM climate input scenarios, and one scenario using the mean climatology of the 8 different scenarios. 1 98 KB Open access
S3 Table. List of samples used to create the pollen-based reconstruction of tree cover at LGM presented in Fig 1. 5 168 KB Open access
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