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dc.contributor.authorHartley, IP
dc.contributor.authorGarnett, Mark H.
dc.contributor.authorSommerkorn, M
dc.contributor.authorHopkins, DW
dc.contributor.authorWookey, PA
dc.date.accessioned2013-05-13T13:04:31Z
dc.date.issued2013-03-26
dc.description.abstractIn arctic ecosystems, winter soil respiration can contribute substantially to annual CO2 release, yet the source of this C is not clear. We analysed the 14C content of C released from plant-free plots in mountain birch forest and tundra-heath. Winter-respired CO2 was found to be a similar age (tundra) or older (forest) than C released during the previous autumn. Overall, our study demonstrates that the decomposition of older C can continue during the winter, in these two contrasting arctic ecosystems.en_GB
dc.identifier.citationVol. 63, pp. 1 - 4en_GB
dc.identifier.doi10.1016/j.soilbio.2013.03.011
dc.identifier.urihttp://hdl.handle.net/10871/9308
dc.language.isoenen_GB
dc.publisherElsevieren_GB
dc.subjectWinter respirationen_GB
dc.subjectTundra-heathen_GB
dc.subjectTree-lineen_GB
dc.subjectRadiocarbonen_GB
dc.subjectMountain birchen_GB
dc.subjectPassive samplingen_GB
dc.subjectCO2en_GB
dc.titleThe age of CO2 released from soils in contrasting ecosystems during the arctic winteren_GB
dc.typeArticleen_GB
dc.date.available2013-05-13T13:04:31Z
dc.identifier.issn0038-0717
dc.descriptionCopyright © 2013 Elsevier. NOTICE: This is the author’s version of a work accepted for publication by Elsevier. Changes resulting from the publishing process, including peer review, editing, corrections, structural formatting and other quality control mechanisms, may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Soil Biology and Biochemistry, Vol. 63, pp. 1 – 4 DOI: http://dx.doi.org/10.1016/j.soilbio.2013.03.011en_GB
dc.identifier.journalSoil Biology and Biochemistryen_GB


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