A sensitive high-resolution record of late Holocene climatic change from a raised bog in northern England

Barber, K E, Chambers, Frank M ORCID: 0000-0002-0998-2093, Maddy, D, Stoneman, R and Brew, J S (1994) A sensitive high-resolution record of late Holocene climatic change from a raised bog in northern England. Holocene, 4 (2). pp. 198-205. doi:10.1177/095968369400400209

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Proxy-climatic data in the form of plant macrofossils have been analysed from a 5 m core from Bolton Fell Moss, Cumbria, UK. Detailed analysis of peat from the upper 50 cm of this core is used to demonstrate a strong correlation between changes in the relative proportion of taxa and known climatic changes over the last 1000 years. The record of changes in bog vegetation contained within the peat profile is used to reconstruct changes in bog-surface wetness for the latter half of the Holocene. As bog- surface wetness is directly controlled by the prevailing climatic conditions, this reconstruction can be viewed as a proxy-climate record. Twelve radiocarbon age estimates on the 5m core suggest that between 50 and 500 cm peat accumulated at a relatively constant rate of 12.4 yr cm-1 . The regular sampling intervals thus provide a time series of past bog-surface wetness; spectral analyses of this series indicates that wetness changes are cyclic, with a ca. 800 year periodicity.

Item Type: Article
Article Type: Article
Subjects: G Geography. Anthropology. Recreation > G Geography (General)
G Geography. Anthropology. Recreation > GE Environmental Sciences
Divisions: Schools and Research Institutes > School of Education and Science
Research Priority Areas: Place, Environment and Community
Depositing User: Anne Pengelly
Date Deposited: 06 Jan 2015 15:23
Last Modified: 31 Aug 2023 08:59
URI: https://eprints.glos.ac.uk/id/eprint/1159

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