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dc.contributor.authorKarhu, Kristiina
dc.contributor.authorFritze, Hannu
dc.contributor.authorHämäläinen, Kai
dc.contributor.authorVanhala, Pekka
dc.contributor.authorJungner, Högne
dc.contributor.authorOinonen, Markku
dc.contributor.authorSonninen, Eloni
dc.contributor.authorTuomi, Mikko
dc.contributor.authorSpetz, Peter
dc.contributor.authorKitunen, Veikko
dc.contributor.authorLiski, Jari
dc.date.accessioned2017-03-09T17:41:40Z
dc.date.available2017-03-09T17:41:40Z
dc.date.issued2010-02-01
dc.identifier.citationKarhu , K , Fritze , H , Hämäläinen , K , Vanhala , P , Jungner , H , Oinonen , M , Sonninen , E , Tuomi , M , Spetz , P , Kitunen , V & Liski , J 2010 , ' Temperature sensitivity of soil carbon fractions in boreal forest soil ' , Fungal Ecology , vol. 91 , no. 2 , pp. 370-376 . https://doi.org/10.1890/09-0478.1
dc.identifier.issn0012-9658
dc.identifier.otherPURE: 11129761
dc.identifier.otherPURE UUID: 27e46a19-1c72-4f64-8826-159a83e04578
dc.identifier.otherScopus: 77949295671
dc.identifier.otherPubMed: 20392002
dc.identifier.urihttp://hdl.handle.net/2299/17704
dc.descriptionKristiina Karhu, et al, 'Temperature sensitivity of soil carbon fractions in boreal forest soil', Ecology, Vol. 91 (2): 370-376, first published online 1 February 2010. The version of record is available online at doi: 10.1890/09-0478.1 © 2010 by the Ecological Society of America
dc.description.abstractFeedback to climate warming from the carbon balance of terrestrial ecosystems depends critically on the temperature sensitivity of soil organic carbon (SOC) decomposition. Still, the temperature sensitivity is not known for the majority of the SOC, which is tens or hundreds of years old. This old fraction is paradoxically concluded to be more, less, or equally sensitive compared to the younger fraction. Here, we present results that explain these inconsistencies. We show that the temperature sensitivity of decomposition increases remarkably from the youngest annually cycling fraction (Qio < 2) to a decadally cycling one (Qio = 4.2-6.9) but decreases again to a centennially cycling fraction (Qio = 2.4-2.8) in boreal forest soil. Compared to the method used for current global estimates (temperature sensitivity of all SOC equal to that of the total heterotrophic soil respiration), the soils studied will lose 30-45% more carbon in response to climate warming during the next few decades, if there is no change in carbon input. Carbon input, derivative of plant productivity, would have to increase by 100-120%, as compared to the earlier estimated 70-80%), in order to compensate for the accelerated decomposition.en
dc.format.extent7
dc.language.isoeng
dc.relation.ispartofFungal Ecology
dc.subjectBoreal forest
dc.subjectDecomposition
dc.subjectFinland
dc.subjectSoil organic carbon
dc.subjectSoil organic matter
dc.subjectTemperature sensitivity
dc.subjectEcology, Evolution, Behavior and Systematics
dc.titleTemperature sensitivity of soil carbon fractions in boreal forest soilen
dc.contributor.institutionSchool of Physics, Astronomy and Mathematics
dc.description.statusPeer reviewed
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=77949295671&partnerID=8YFLogxK
dc.relation.schoolSchool of Physics, Astronomy and Mathematics
dcterms.dateAccepted2009-08-13
rioxxterms.versionofrecordhttps://doi.org/10.1890/09-0478.1
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue
herts.rights.accesstypeclosedAccess


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