Abiotic drivers and their interactive effect on the flux and carbon isotope (14C and δ13C) composition of peat-respired CO2

Hardie, S.M.L., Garnett, M.H. , Fallick, A.E., Rowland, A.P., Ostle, N.J. and Flowers, T.H. (2011) Abiotic drivers and their interactive effect on the flux and carbon isotope (14C and δ13C) composition of peat-respired CO2. Soil Biology and Biochemistry, 43(12), pp. 2432-2440. (doi: 10.1016/j.soilbio.2011.08.010)

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Publisher's URL: http://dx.doi.org/10.1016/j.soilbio.2011.08.010


Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO<sub>2</sub> emissions, thus exacerbating climate change. The contribution that soil respiration makes to these terrestrial emissions, particularly from carbon-rich soils such as peatlands, is of significant importance and its response to changing climatic conditions is of considerable debate.We collected intact soil cores from an upland blanket bog situated within the northern Pennines, England, UK and investigated the individual and interactive effects of three primary controls on soil organic matter decomposition: (i) temperature(5, 10 and 15 °C); (ii) moisture (50 and 100% field capacity e FC); and (iii) substrate quality, using increasing depth from the surface (0-10, 10-20 and 20-30 cm) as an analogue for increased recalcitrance of soil organic material. Statistical analysis of the results showed that temperature, moisture and substrate quality all significantly affected rates of peat decomposition. <i>Q</i><sub>10</sub> values indicated that the temperature sensitivity of older/more recalcitrant soil organic matter significantly increased (relative to more labile peat) under reduced soil moisture (50% FC) conditions, but not under 100% FC, suggesting that soil microorganisms decomposing the more recalcitrant soil material preferred more aerated conditions. Radiocarbon analyses revealed that soil decomposers were able to respire older, more recalcitrant soil organic matter and that the source of the material (deduced from the δ<sup>13</sup>C analyses) subject to decomposition, changed depending on depth in the peat profile.

Item Type:Articles
Glasgow Author(s) Enlighten ID:Flowers, Dr Hugh and Garnett, Dr Mark and Fallick, Professor Anthony
Authors: Hardie, S.M.L., Garnett, M.H., Fallick, A.E., Rowland, A.P., Ostle, N.J., and Flowers, T.H.
College/School:College of Science and Engineering > School of Chemistry
College of Science and Engineering > Scottish Universities Environmental Research Centre
Journal Name:Soil Biology and Biochemistry

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