Palaeoecological evidence for the prehistoric settlement of Bodmin Moor, Cornwall, Southwest England, part 1, The status of woodland and early human impacts

Citation
Br. Gearey et al., Palaeoecological evidence for the prehistoric settlement of Bodmin Moor, Cornwall, Southwest England, part 1, The status of woodland and early human impacts, J ARCH SCI, 27(5), 2000, pp. 423-438
Citations number
60
Categorie Soggetti
Archeology
Journal title
JOURNAL OF ARCHAEOLOGICAL SCIENCE
ISSN journal
03054403 → ACNP
Volume
27
Issue
5
Year of publication
2000
Pages
423 - 438
Database
ISI
SICI code
0305-4403(200005)27:5<423:PEFTPS>2.0.ZU;2-T
Abstract
Bodmin Moor is one of the most complete and best preserved upland prehistor ic landscapes in Britain. The field archaeology has been described in some detail, although on the basis of comparatively little excavation, but this has nevertheless been used to generate hypotheses concerning the nature and timing of human settlement and impacts on the Moor. In contrast, there has been relatively little palaeoenvironmental work, due to a perceived lack o f suitable deposits. These two articles present new palynological data from a series of recently discovered undisturbed profiles. This first paper des cribes the physical and archeological settings of the sites and discusses t he nature of the early Holocene vegetation on the Moor. Although previous w ork has suggested a dominance of open moorland throughout the Holocene, the two high-altitude (280 m OD) profiles presented here show that dense woodl and dominated by Corylus avellana and Quercus was present until around 6500 BP and probably extended to the very highest points of the Moor. Other tax a, such as Ulmus, Betula, and Tilia cordata, were also subordinate componen ts of the vegetation. Alnus glutinosa became established later, possibly af ter disturbance to the vegetation by human activity, although the nature an d extent of Mesolithic disturbance to the vegetation is unclear. Thus, the early Holocene vegetation of the Moor was not predominantly open heath or g rassland as has previously been assumed, but more probably a dense cover of hazel and oak woodland.