A long-term perspective on ungulate–vegetation interactions

By Richard Bradshaw, G. Hannon, A. Lister. 2003

182 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science, Ecology

View Paper: https://www.semanticscholar.org/paper/e623fe8d5d4c69b4b1311ac304d399a740baf88e

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Citations in the corpus

Intensive game keeping, coppicing and butterflies: The story of Milovicky Wood, Czech Republic (2006, background): “The much-debated theory of wood pasture (Vera, 2000) proposes that prehistoric woodlands had been kept relatively open first by wild ungulates, later on by domestic animals (Hansson, 2001; Bradshaw et al., 2003; Bakker et al., 2004; but see Birks, 2005).”
Forest dynamics and ungulate herbivory: from leaf to landscape (2003, background): “Such a perspective emerges from several of the papers included in this special issue, and various research methodologies for developing longterm perspectives are demonstrated or explored (Bradshaw et al., 2003; Husheer et al., 2003; Motta, 2003; Rooney and Waller, 2003; Schütz et al., 2003; Senn and”
High white-tailed deer densities benefit graminoids and contribute to biotic homogenization of forest ground-layer vegetation (2009, background): “If white-tailed deer densities remain high in the region, grass and sedge dominated ground-layers expand, and tree seedling regeneration is suppressed, some existing forest might convert to a vegetation mosaic with open and wooded habitats, much like savanna or wood pasture (Bradshaw et al. 2003).”
Biodiversity in temperate European grasslands: origin and conservation. (2005, unknown): “Probably similar numbers have been present in all Quaternary interglacials except our own, the Holocene (Bradshaw et al. , 2003).”
The Holocene British and Irish ancient forest fossil beetle fauna: implications for forest history, biodiversity and faunal colonisation (2006, background): “…and debate amongst conservationists, biologists and palaeoecologists (e.g. Blumer, 2002; Eriksson et al., 2002; Sutherland, 2002; Svenning, 2002; Bradshaw et al., 2003; Kirby, 2003, 2004; Rackham, 2003; Bakker et al., 2004; Bradshaw and Hannon, 2004; Whitehouse and Smith, 2004; Birks, 2005;…”
Evidence for geographic variation in the diets of late Pleistocene and early Holocene Bison in North America, and differences from the diets of recent Bison (2007, background): “It is obvious that ungulate–vegetation interactions during the Pleistocene were primarily driven by climatic variation of the glacial-interglacial cycle (Comes and Kadereit, 1998; Bradshaw and Mitchell, 1999; Bradshaw et al., 2003).”