Tipping, R. (1995). Holocene evolution of a lowland Scottish landscape. The Holocene. Vol 5(1), pp. 69-81. https://doi.org/10.1177/095968369500500108 .
Title The title of the publication or report |
Holocene evolution of a lowland Scottish landscape | |||||
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Subtitle The sub title of the publication or report |
Kirkpatrick Fleming. Part I, peat- and pollen-stratigraphic evidence for raised moss development and climatic change | |||||
Issue The name of the volume or issue |
The Holocene | |||||
Series The series the publication or report is included in |
The Holocene | |||||
Volume Volume number and part |
5 (1) | |||||
Page Start/End The start and end page numbers. |
69 - 81 | |||||
Biblio Note This is a Bibliographic record only. |
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Publication Type The type of publication - report, monograph, journal article or chapter from a book |
Journal | |||||
Abstract The abstract describing the content of the publication or report |
This series of papers addresses the principal natural and anthropogenic environmental changes that have transformed a typical lowland Scottish landscape during the Holocene. Sediment- and pollen- stratigraphic techniques, together with radiocarbon dating, are applied in this paper to the stratigraphy of a raised bog at Burnfoothill Moss, eastern Dumfriesshire, to deduce changes in groundwater levels within the bog, and by inference, changes in effective precipitation. The basin, initially a shallow pond, was rapidly colonized by fen peat at 9600 BP, possibly during a phase of drier climate, which ended at c. 8700 BP. Short-lived fluctuations in bog-surface wetness are identified before a major change to a wetter bog surface at around 7700 cal. BP, representing the transformation from fen peat to raised moss. Anthropogenic interference with surrounding woodland is believed to have destabilized the water balance within the peat. Drier bog-surface conditions occur at c. 6700 cal. BP, and a shift to a wetter climate at around 5250 cal. BP, but a perhaps more substantial wet shift is recorded at c. 4000 cal. BP. At c. 1900 cal. BP a dry climate shift is recognized, ending at c. 1200 cal. BP. Slightly prior to the 'Little Ice Age', represented by a very wet phase before c. 400 cal. BP, is a dry period between c. 600 and 400 cal. BP. | |||||
Year of Publication The year the book, article or report was published |
1995 | |||||
Locations Any locations covered by the publication or report. This is not the place the book or report was published. |
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Source Where the record has come from or which dataset it was orginally included in. |
BIAB
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Relations Other resources which are relevant to this publication or report |
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Created Date The date the record of the pubication was first entered |
20 Sep 2012 |