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Fire accelerates assimilation and transfer of photosynthetic carbon from plants to soil microbes in a northern peatland

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Fire accelerates assimilation and transfer of photosynthetic carbon from plants to soil microbes in a northern peatland. / Ward, Sue; Ostle, Nick; Oakley, Simon et al.
In: Ecosystems, Vol. 15, No. 8, 12.2012, p. 1245-1257.

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Ward S, Ostle N, Oakley S, Quirk H, Stott A, Henrys P et al. Fire accelerates assimilation and transfer of photosynthetic carbon from plants to soil microbes in a northern peatland. Ecosystems. 2012 Dec;15(8):1245-1257. Epub 2012 Aug 9. doi: 10.1007/s10021-012-9581-8

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@article{8097f2bf24904b0bafbea2c808b71e82,
title = "Fire accelerates assimilation and transfer of photosynthetic carbon from plants to soil microbes in a northern peatland",
abstract = "Northern peatlands are recognized as globally important stores of terrestrial carbon (C), yet we have limited understanding of how global changes, including land use, affect C cycling processes in these ecosystems. Making use of a long-term (>50 year old) peatland land management experiment in the UK, we investigated, using a 13CO2 pulse chase approach, how managed burning and grazing influenced the short-term uptake and cycling of C through the plant–soil system. We found that burning affected the composition and growth stage of the plant community, by substantially reducing the abundance of mature ericoid dwarf-shrubs. Burning also affected the structure of the soil microbial community, measured using phospholipid fatty acid analysis, by reducing fungal biomass. There was no difference in net ecosystem exchange of CO2, but burning was associated with an increase in photosynthetic uptake of 13CO2 and increased transfer of 13C to the soil microbial community relative to unburned areas. In contrast, grazing had no detectable effects on any measured C cycling process. Our study provides new insight into how changes in vegetation and soil microbial communities arising from managed burning affect peatland C cycling processes, by enhancing the uptake of photosynthetic C and the transfer of C belowground, whilst maintaining net ecosystem exchange of CO2 at pre-burn levels.",
keywords = "peatland, burning , carbon cycle , stable isotope pulse labelling, 13C , respiration , photosynthesis, plant functional types , PLFA",
author = "Sue Ward and Nick Ostle and Simon Oakley and Helen Quirk and Andy Stott and Peter Henrys and Scott, {W. Andrew} and Richard Bardgett",
year = "2012",
month = dec,
doi = "10.1007/s10021-012-9581-8",
language = "English",
volume = "15",
pages = "1245--1257",
journal = "Ecosystems",
issn = "1432-9840",
publisher = "Springer New York LLC",
number = "8",

}

RIS

TY - JOUR

T1 - Fire accelerates assimilation and transfer of photosynthetic carbon from plants to soil microbes in a northern peatland

AU - Ward, Sue

AU - Ostle, Nick

AU - Oakley, Simon

AU - Quirk, Helen

AU - Stott, Andy

AU - Henrys, Peter

AU - Scott, W. Andrew

AU - Bardgett, Richard

PY - 2012/12

Y1 - 2012/12

N2 - Northern peatlands are recognized as globally important stores of terrestrial carbon (C), yet we have limited understanding of how global changes, including land use, affect C cycling processes in these ecosystems. Making use of a long-term (>50 year old) peatland land management experiment in the UK, we investigated, using a 13CO2 pulse chase approach, how managed burning and grazing influenced the short-term uptake and cycling of C through the plant–soil system. We found that burning affected the composition and growth stage of the plant community, by substantially reducing the abundance of mature ericoid dwarf-shrubs. Burning also affected the structure of the soil microbial community, measured using phospholipid fatty acid analysis, by reducing fungal biomass. There was no difference in net ecosystem exchange of CO2, but burning was associated with an increase in photosynthetic uptake of 13CO2 and increased transfer of 13C to the soil microbial community relative to unburned areas. In contrast, grazing had no detectable effects on any measured C cycling process. Our study provides new insight into how changes in vegetation and soil microbial communities arising from managed burning affect peatland C cycling processes, by enhancing the uptake of photosynthetic C and the transfer of C belowground, whilst maintaining net ecosystem exchange of CO2 at pre-burn levels.

AB - Northern peatlands are recognized as globally important stores of terrestrial carbon (C), yet we have limited understanding of how global changes, including land use, affect C cycling processes in these ecosystems. Making use of a long-term (>50 year old) peatland land management experiment in the UK, we investigated, using a 13CO2 pulse chase approach, how managed burning and grazing influenced the short-term uptake and cycling of C through the plant–soil system. We found that burning affected the composition and growth stage of the plant community, by substantially reducing the abundance of mature ericoid dwarf-shrubs. Burning also affected the structure of the soil microbial community, measured using phospholipid fatty acid analysis, by reducing fungal biomass. There was no difference in net ecosystem exchange of CO2, but burning was associated with an increase in photosynthetic uptake of 13CO2 and increased transfer of 13C to the soil microbial community relative to unburned areas. In contrast, grazing had no detectable effects on any measured C cycling process. Our study provides new insight into how changes in vegetation and soil microbial communities arising from managed burning affect peatland C cycling processes, by enhancing the uptake of photosynthetic C and the transfer of C belowground, whilst maintaining net ecosystem exchange of CO2 at pre-burn levels.

KW - peatland

KW - burning

KW - carbon cycle

KW - stable isotope pulse labelling

KW - 13C

KW - respiration

KW - photosynthesis

KW - plant functional types

KW - PLFA

U2 - 10.1007/s10021-012-9581-8

DO - 10.1007/s10021-012-9581-8

M3 - Journal article

VL - 15

SP - 1245

EP - 1257

JO - Ecosystems

JF - Ecosystems

SN - 1432-9840

IS - 8

ER -