Abstract
The palaeoecology of six Scottish blanket peat profiles containing pine stumps was investigated by means of peat stratigraphy, pollen analysis, and radiocarbon dating. In addition, several other pine and birch remains from peat in other areas of Scotland were radiocarbon dated. Three peat profiles were selected in each of two contrasting regions. The Cairngorm area is within the distributional area of native pine today and pollen analysis has shown that pine has been a major component of the upland forest since about 7000 b.p. The Galloway region in southwest Scotland is south of the native pine area, and pollen analysis has shown that pine has never been a major component of the upland forest. Despite the limitations of the methods used, it has been established that there were several different circumstances for the growth and death of the pines studied, and that their ages are asynchronous within and between the two areas. Thus little regional climatic significance can be assumed from their occurrence, and they cannot be taken as evidence in support of dry Boreal and sub-Boreal periods in the Blytt and Sernander climatic scheme. In the northwest Highlands dates from pine stumps and major declines of pollen in pollen diagrams are consistently around 4000 b.p. This overall demise of pine may have a regional climatic cause in this area.
Subject
Industrial and Manufacturing Engineering,General Agricultural and Biological Sciences,General Business, Management and Accounting,Materials Science (miscellaneous),Business and International Management
Reference61 articles.
1. Andersen S. Th. 1 9 6 1 Danm. geol. Unders. Ser. n 75 175 pp.
2. Bartley D. D. 1 9 6 7 Pollen Spores 9 101.
3. Berglund B. E. 1 9 6 6 Op. bot. Soc. bot. Lund 12 (2) 190 pp.
4. Birks H. H. 1 9 6 9 Ph.D. thesis University of Cambridge.
5. Birks H . H . 1 9 7 0
Cited by
114 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献