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Palaeoenvironments in the Vale of Pickering. Part 2: Environmental History at Seamer Carr

Published online by Cambridge University Press:  10 November 2022

E. W. Cloutman
E. W. Cloutman*
Affiliation:
Department of Plant Science, University College, Cardiff, UK
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Abstract

A three-dimensional study of the vegetational history of Seamer Carr from the Devensian Late-glacial to the Atlantic period has been made with the aid of six sites in the main basin. Five of these are close to the margins of the organic deposits and the sixth is from deep basin deposits. The Godwin zonation scheme has been used to allow a direct comparison with the survey of Walker and Godwin (1954). A composite section through the basin deposits, based on the detailed contour plan described in Part 1, shows that, pre-Zone IV, the open water margin abutted the dry land, and that during Zone IV reedswamp and carr gradually filled in the edges of the lake. Large expanses of fen carr occupied Seamer Carr during Zone V, but a rise in water level during Zone VI was responsible for the area reverting to reedswamp. At the Boreal/Atlantic transition, coincident with the rise in the alder pollen curve, there is a thick band of highly humified, acid peat, full of microscopic pieces of charcoal. Analysis through this band at one of the specially selected sites on East Island produced evidence of local disturbance, seemingly anthropogenic, at the wetland margin. There were two other special sites in West Embayment that were sampled for pollen analysis. The first was located over a radiocarbon dated Zone II organic deposit, sealed beneath a Zone III calcareous sand layer. The second was located in a late Mesolithic organic mud radiocarbon dated to c. 8000 BP and containing an assemblage of microliths of late Mesolithic type, identified tentatively as a composite tool (A. David pers. comm.).

Type
Research Article
Information
Proceedings of the Prehistoric Society , Volume 54 , Issue 1 , 1988 , pp. 21 - 36
Copyright
Copyright © The Prehistoric Society 1988

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Footnotes

1

Certain detailed records and data are given in a microfiche, together with similar data for Parts 1 and 3 (inside back cover).

References

BIBLIOGRAPHY

Clapham, A. R., Tutin, T. G. and Warburg, E. F., 1962. Flora of the British Isles. 2nd edn. Cambridge: Cambridge University Press.Google Scholar
Clark, J. G. D. and Godwin, H., 1956. A Maglemosian site at Brandesburton, Holderness, Yorkshire. Proceedings of the Prehistoric Society 22, 6–22.CrossRefGoogle Scholar
Cloutman, E. W., 1983. Studies of the vegetational history of the Black Mountain Range, South Wales. Ph.D. thesis, University of Wales.Google Scholar
Cloutman, E. W., 1987. A mini-monolith cutter for absolute pollen analysis and fine sectioning of peats and sediments. New Phytologist 107, 245–48.CrossRefGoogle Scholar
Coope, G. R., 1977. Fossil coleopteran assemblages as sensitive indicators of climatic changes during the Devensian (last) cold stage. Philosophical Transactions of the Royal Society of London B 280, 313–40.Google Scholar
Dresser, P. Q., 1985. University College Cardiff radiocarbon dates 1. Radiocarbon 27, 338–85.CrossRefGoogle Scholar
Erdtman, G., 1960. The acetolysis method. A revised description. Svensk Botanisk Tidskrift 54, 561–64.Google Scholar
Godwin, H., 1940. Pollen analysis and forest history of England and Wales. New Phytologist 39, 370–400.CrossRefGoogle Scholar
Godwin, H. and Willis, E. H., 1959. Cambridge University natural radiocarbon measurements I. American Journal of Science, Radiocarbon Supplement 1, 63–75.Google Scholar
Iversen, J., 1949. The influence of prehistoric man on vegetation. Danmarks Geologiske Undersøgelse Ser.4, 3 (6), 1–25.Google Scholar
Mamakova, K., 1968. Lille Bukken and Leroy: two pollen diagrams from western Norway. Arbok for Universitetet i Bergen 4, 5–42.Google Scholar
Pennington, W., 1977. The Late-Devensian flora and vegetation of Britain. Philosophical Transactions of the Royal Society of London B 280, 247–72.Google Scholar
Schadla-Hall, R. T., 1987. 3. Recent investigations of the early mesolithic landscape and settlement in the Vale of Pickering, North Yorkshire. In Rowley-Conwy, P., Zvelebil, M. and Blankholm, H. P. (eds), Mesolithic Northwest Europe: Recent Trends, 46–54. Sheffield: Dept of Archaeology and Prehistory, Sheffield University.Google Scholar
Simmons, I. G., 1969. Pollen diagrams from the North York Moors. New Phytologist 68, 807–27.CrossRefGoogle Scholar
Smith, A. G., 1984. Newferry and the Boreal-Atlantic Transition. New Phytologist 98, 35–55.CrossRefGoogle ScholarPubMed
Smith, A. G. and Cloutman, E. W. (in press). Reconstruction of Holocene vegetational history in three dimensions at Waun-Fignen-Felen, an upland site in South Wales. Philosophical Transactions of the Royal Society of London B.Google Scholar
Tinsley, H. M., 1976. Cultural influences on Pennine vegetation with particular reference to North Yorkshire. Transactions of the Institute of British Geographers NSI, 310–22.Google Scholar
Walker, D. and Godwin, H., 1954. Chapter 2: lake stratigraphy, pollen analysis and vegetational history. In Clark, J. G. D., Excavations at Star Carr, Cambridge University Press.Google Scholar