Effects of burning and grazing on carbon sequestration in a Pennine blanket bog, UK

Bibliographic Data

ID12265275
AuthorsM H Garnett (0000-0001-6486-2126, Department of Geography, University of Newcastle, Newcastle-upon-Tyne, NE1 7RU, UK; Institute of Terrestrial Ecology, Merlewood Research Station, Grange-over-Sands, Cumbria, LA11 6JU, UK; NERC Radiocarbon Lab, Scottish Enterprise Technology Park, Rankine Avenue, East Kilbride G75 0QF, UK, corresponding author), Phil Ineson (University of Cumbria), A C Stevenson (Department of Geography, University of Newcastle, Newcastle-upon-Tyne, NE1 7RU, UK), Tony Stevenson (0000-0002-8870-1041, Newcastle University)
Year2000
Volume10
Issue6
Pages729-736
Publication date2000-09-01
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1191/09596830094971
OpenAlexW2134733569
LanguageEN
Citations received8
References cited22

Terrestrial ecosystems contain large amounts of carbon (C) and have the potential to significantly increase atmospheric carbon dioxide (CO 2 ) concentrations. Peatlands are particularly important for C storage, although little is known about the effects of anthropogenic activities on C balance in these ecosystems. Sheep-grazing and rotational burning are widely practised on blanket peat moorlands in the United Kingdom. The effects of these activities on C sequestration in peat has been investigated with a long-term randomized block experiment with treatments: (a) grazed + unburnt; (b) grazed + burnt every ten years; (c) ungrazed + unburnt. C accumulation under these treatments was compared by identifying a chronologically synchronous horizon within the peat common to all treatment plots. This fixed point was defined by the ‘take-off’ in concentration of spheroidal carbonaceous particles and was supported by the record of charcoal fragments. There was no significant difference in recent C accumulation rates between lightly grazed and ungrazed plots. In contrast, after 30 years there was significantly less C stored in the blanket peat in plots which had been burned every ten years. The results indicate that light sheep-grazing at this site did not affect rates of C accumulation in blanket peat, but decadal burning of moorland reduced C sequestration

Biology · Bog · Carbon dioxide · Carbon sequestration · Charcoal · Ecosystem · Grazing · Hydrology (agriculture · Moorland · Peat · Botany and Plant Ecology Studies · Chemistry · Coastal wetland ecosystem dynamics · Environmental Science · Peatlands and Wetlands Ecology · Ecology · Geology

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