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New Phytol 72
Title
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Title:
New Phytol 72
Series
The series the publication or report is included in
Series:
New Phytologist
Volume
Volume number and part
Volume:
72
Publication Type
The type of publication - report, monograph, journal article or chapter from a book
Publication Type:
Journal
Year of Publication
The year the book, article or report was published
Year of Publication:
1973
Note
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Note:
Date Of Issue From: 1973
Source
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Source:
BIAB (British Archaeological Abstracts (BAA))
Created Date
The date the record of the pubication was first entered
Created Date:
05 Dec 2008
Please click on an Article link to go to the Article Details.
Article Title
Access Type
Author / Editor
Page
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Abstract
Long range transmission of tree pollen to Shetland: I, sampling and trajectories; II, calculation of pollen deposition
J B Tyldesley
175 - 181
Recent work has shown that tree pollen is arriving in Shetland from sources overseas, and although a lengthy research project is needed to investigate this, there are strong indications that long-distance transport of pollen has always been important.
Pollen analyses and radiocarbon dating of a peat on Slieve Gallion, Co Tyrone, N Ireland
Jonathan R Pilcher
681 - 689
[H 7987]. A radiocarbon-dated pollen diagram is presented from 430m altitude on Slieve Gallion, a mountain situated 13km from the Beaghmore circles and 8km from Ballynagilly. Deposits of reedswamp peat overlain by blanket peat cover the period 8000 BC to the present. The analyses indicate more open conditions throughout the Post-Glacial than are found in the lowlands, and the lack of herb pollen suggests areas of bare rock on the mountain top before c 7650 BC. There is an elm decline just after 3000 BC; also, in common with other sites in this area, a decline of pine pollen at c 2000 BC, for which man was at least partly responsible.
Radiocarbon dates and vegetational history of the British Isles
A G Smith
Jonathan R Pilcher
903 - 914
Radiocarbon dates for a number of pollen analytic features marking important vegetational changes in the Post-Glacial of the British Isles are plotted. Despite the limitations of the radiocarbon method it becomes clear, where sufficient dates are available, that most of the vegetational developments of the earlier part of the Post-Glacial are diachronous. Some of these changes have been used as pollen zone boundaries. The elm decline appears synchronous, however, within the limits of the methods, and the final pine decline in Ireland, which at c 2000 BC is shown to be older than supposed by Jessen (1949), appears to be one of the least diachronous of the horizons examined. Marked differences in the dates of similar vegetational changes within a small area, and between upland and lowland, are pointed out. Au