Advanced Search

Journal Navigation

Journal Home

Subscriptions

Archive

Contact Us

Table of Contents

Environmental Sciences: A Students Companion

Sign In to gain access to subscriptions and/or personal tools.
The Holocene
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to Saved Citations
Right arrow Download to citation manager
Right arrowRequest Permissions
Right arrow Request Reprints
Right arrow Add to My Marked Citations
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Right arrow Citing Articles via Scopus
Google Scholar
Right arrow Articles by Hendon, D.
Right arrow Articles by Charman, D. J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Social Bookmarking
 Add to CiteULike   Add to Complore   Add to Connotea   Add to Del.icio.us   Add to Digg   Add to Reddit   Add to Technorati   Add to Twitter  
What's this?

High-resolution peatland water-table changes for the past 200 years: the influence of climate and implications for management

Dawn Hendon

Department of Geography, University of Exeter, Amory Building, Rennes Drive, Exeter EX4 4RJ, UK; D.Lees{at}exeter.ac.uk

Dan J. Charman

School of Geography, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK

Management of peatlands for conservation purposes is often directed at mitigation of damaging impacts of past and present human activity. Assessment of such impacts is often based on perspectives from short-term ecological data. Here we test a series of hypotheses for the causes of changes in mire hydrology and vegetation on the Border Mires in northern England using palaeoecological data for the last 200 years. Ecological data suggest peatlands surrounded by plantation forestry have become drier over the last 40 years. This could be caused by direct hydrological impacts of the growing trees and associated drainage or indirectly by the cessation of grazing and burning. A third hypothesis is that hydrological changes are the result of recent climatic change. High-resolution water-table reconstructions from testate amoebae analysis supported by plant macrofossil analysis and dated by 210Pb, spheroidal carbonaceous particles (SCPs) and pollen data demonstrate that a site outside the direct in‘ uence of forestry has also become drier during the twentieth century. This suggests that forestry is not the main cause of changes observed on other sites. Water-table declines began earlier than the main phase of forest planting and the magnitude of change appears to be similar to that on a site within the forest. Subjective comparisons of reconstructed water tables with meteorological data suggest that hydrological changes on the mires are primarily driven by summer temperature changes. If future regional climatic change predictions are correct, further water-table decline will follow and current management activities are unlikely to restore mires to their former condition.

Key Words: Testate amoebae • mires • peatlands • management • forestry • climate • water table • human impact

The Holocene, Vol. 14, No. 1, 125-134 (2004)
DOI: 10.1191/0959683604hl695rp


Add to CiteULike CiteULike   Add to Complore Complore   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg   Add to Reddit Reddit   Add to Technorati Technorati   Add to Twitter Twitter    What's this?


This article has been cited by other articles:


Home page
The HoloceneHome page
M. A. Tweiten, S. C. Hotchkiss, R. K. Booth, R. R. Calcote, and E. A. Lynch
The response of a jack pine forest to late-Holocene climate variability in northwestern Wisconsin
The Holocene, November 1, 2009; 19(7): 1049 - 1061.
[Abstract] [PDF]


Home page
The HoloceneHome page
E. L. McClymont, D. Mauquoy, D. Yeloff, P. Broekens, B. van Geel, D. J. Charman, R. D. Pancost, F. M. Chambers, and R. P. Evershed
The disappearance of Sphagnum imbricatum from Butterburn Flow, UK: a reply to comments by Bjorn Robroek et al
The Holocene, November 1, 2009; 19(7): 1094 - 1097.
[Abstract] [PDF]


Home page
The HoloceneHome page
E. L. McClymont, D. Mauquoy, D. Yeloff, P. Broekens, B. van Geel, D. J. Charman, R. D. Pancost, F. M. Chambers, and R. P. Evershed
The disappearance of Sphagnum imbricatum from Butterburn Flow, UK
The Holocene, September 1, 2008; 18(6): 991 - 1002.
[Abstract] [PDF]


Home page
The HoloceneHome page
D. Yeloff, B. van Geel, P. Broekens, J. Bakker, and D. Mauquoy
Mid- to late-Holocene vegetation and land-use history in the Hadrian's Wall region of northern England: the record from Butterburn Flow
The Holocene, May 1, 2007; 17(4): 527 - 538.
[Abstract] [PDF]


Home page
The HoloceneHome page
D. J. Charman
Summer water deficit variability controls on peatland water-table changes: implications for Holocene palaeoclimate reconstructions
The Holocene, February 1, 2007; 17(2): 217 - 227.
[Abstract] [PDF]


Home page
The HoloceneHome page
K. Schoning, K. Schoning, D. J. Charman, and S. Wastegoard
Reconstructed water tables from two ombrotrophic mires in eastern central Sweden compared with instrumental meteorological data
The Holocene, January 1, 2005; 15(1): 111 - 118.
[Abstract] [PDF]