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A pollen-based pseudobiomisation approach to anthropogenic land-cover change

Bibliographic Data

ID12266305
AuthorsRalph Fyfe (0000-0002-5676-008X, University of Plymouth, corresponding author), Neil Roberts (0000-0001-5538-8653), John Woodbridge (0000-0003-0756-3538, University of Plymouth), Jessie Woodbridge (University of Plymouth)
Year2010
Volume20
Issue7
Pages1165-1171
Publication date2010-07-12
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683610369509
OpenAlexW2030022653
LanguageEN
Citations received19
References cited46

The degree of anthropogenic modification of land cover through the mid to late Holocene is of significant interest for archaeologists, climate modellers and conservation ecologists, amongst others. Spatially extensive pollen data provide an appropriate resource for the reconstruction of land-cover change; however, traditional simple methods (e.g. the AP/NAP ratio) do not provide the degree of detail required for these user groups. A range of more sophisticated methods have been developed (e.g. mechanistic model-based methods), but they require a high degree of understanding of the pollen—vegetation relationship, which is resource- and time-consuming. This paper proposes a method of intermediate complexity by which major land-cover changes can be assessed for individual sites and regions. A pseudobiomisation approach is used, in which pollen taxa are assigned to different land-cover classes (LCC), and the sum of adjusted pollen proportions for each class used to determine an LCC affinity score for individual pollen samples within stratigraphic pollen sequences. In a pilot study, data from pollen core sites from northwest Scotland and southwest England for the last 8000 cal. BP have been classified into ten land-cover classes, including predominantly wooded, semi-open and open types. Results highlight how land-cover change was punctuated rather than gradual through the mid to late Holocene, and show how habitat diversity increased after ~6000 cal. BP with the arrival of agriculture, before reaching a minimum in early modern times. This pollen-based method is potentially applicable to the reconstruction of long-term land-cover change within Europe and other temperate-zone regions

Archaeology · Biology · Climate change · Environmental change · Geography · Holocene · Land cover · Land use · Physical geography · Pollen · Resource (disambiguation · Taxon · Vegetation (pathology · Archaeology and ancient environmental studies · Computer Science · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Ecology

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Citations per year1.27
Citation span2011 - 2025 (15)
Highly citedNo

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