The full programme book (PDF) - Royal Geographical Society
The full programme book (PDF) - Royal Geographical Society
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T9<br />
When was Europe deforested? Large-scale Holocene land-cover reconstruction<br />
using a pollen-based pseudo-biomisation approach<br />
Neil Roberts 1 *, Jessie Woodbridge 1 and Ralph Fyfe 1<br />
1 School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth, PL4 8AA<br />
<strong>The</strong> need for accurate land-cover datasets extending beyond the period covered by<br />
remote-sensing has encouraged the development of various reconstruction approaches to<br />
past vegetation (e.g. Kaplan et al., 2009). <strong>The</strong> pseudo-biomisation (PBM) approach (Fyfe<br />
et al., 2010; Woodbridge et al. 2013) has been developed to provide a simple and easily<br />
applied transformation of fossil pollen data into land-cover classes in order to reconstruct<br />
broad-scale anthropogenic land-use change through time. <strong>The</strong> PBM has been tested and<br />
refined through application to an extensive modern pollen dataset (Davis et al., 2013) and<br />
comparison with Corine remote-sensed land cover maps (Woodbridge et al., in review).<br />
<strong>The</strong> method has now been applied to 982 records from the European Pollen Database<br />
and synthesised at 200-year time steps from 11,000 BP to the present. Regional<br />
comparisons indicate that forest decline and increased semi-open and open land cover<br />
can be detected since at least ~6000 BP in Central and Northwest Europe. In Southeast<br />
Europe and the Mediterranean, closed forest was part of a regional vegetation mosaic that<br />
always included significant areas of open and semi-open land cover. In consequence,<br />
here it is harder to separate, for example, natural grassland from pasture-land of anthropic<br />
origin. In addition to a Europe-wide synthesis, we present a number of case study areas<br />
in order to explore regionally-specific land-use change, and compare these with other,<br />
non-pollen based estimates of past land cover and demographic change. Our results are<br />
consistent with farming and other human actions having been the primary cause of landcover<br />
change across most of Europe since the mid-Holocene. This in turn gives at least<br />
partial support to Ruddiman’s (2013) early anthropogenic greenhouse hypothesis for the<br />
pre-industrial rise in atmospheric CO 2 concentration.<br />
Keywords: pollen; land cover; anthropogenic; Europe; carbon dioxide; deforestation<br />
Davis B.A.S, Zanon M, Collins P., et al. (online first: 2013) <strong>The</strong> European Modern Pollen Database<br />
(EMPD) project. Vegetation History and Archaeobotany.<br />
Fyfe, R.M., Roberts, N., and Woodbridge, J. (2010) A pseudo-biomisation approach to anthropogenic<br />
land cover change. Holocene. 20: 1165-1171<br />
Kaplan J.O., Krumhardt, K.M. and Zimmerman N. (2009) <strong>The</strong> prehistorical and preindustrial<br />
deforestation of Europe. Quat. Sci. Rev. 28: 3016–34<br />
Ruddiman, W.F. (2013) <strong>The</strong> Anthropocene. Annu. Rev. Earth Planet. Sci. 41: 4.1–4.24<br />
Woodbridge, J., Fyfe, R.M. and Roberts, N. (in review) A comparison of remotely-sensed and pollenbased<br />
approaches to mapping Europe’s land cover. Submitted to J. Biogeography<br />
Woodbridge, J., Fyfe, R.M., Roberts, N., Downey, S., Edinborough, K., and Shennan, S. (online first:<br />
2013) <strong>The</strong> impact of the Neolithic agricultural transition in Britain: a comparison of pollen-based landcover<br />
and archaeological 14C date-inferred population change. Journal of Archaeological Science.