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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004643naa a2200409 4500
001oai:lup.lub.lu.se:06e6968b-900b-45ed-a7ab-f421059535af
003SwePub
008220608s2022 | |||||||||||000 ||eng|
024a https://lup.lub.lu.se/record/06e6968b-900b-45ed-a7ab-f421059535af2 URI
024a https://doi.org/10.1016/j.soilbio.2022.1086152 DOI
040 a (SwePub)lu
041 a engb eng
042 9 SwePub
072 7a art2 swepub-publicationtype
072 7a ref2 swepub-contenttype
100a Karhu, Kristiinau University of Helsinki4 aut
2451 0a Microbial carbon use efficiency and priming of soil organic matter mineralization by glucose additions in boreal forest soils with different C:N ratios
264 1b Elsevier BV,c 2022
520 a During the last decade it has been increasingly acknowledged that carbon (C) contained in root exudates can accelerate decomposition of soil organic matter (SOM), a phenomenon known as rhizosphere priming effect (RPE). However, the controlling factors and the role of different soil microorganisms in RPE are not yet well understood. There are some indications that the response of the soil microbial decomposers to labile C input in the rhizosphere depends on microbial demand of nutrients for growth and maintenance, especially that of C and nitrogen (N). To test this hypothesis, we assessed SOM decomposition induced by 13C-glucose additions during one week in forest soils with different C:N ratios (11.5–22.2). We estimated SOM respiration, the potential activity (concentration) of a range of extracellular enzymes, and incorporation of 13C and deuterium (D) in microbial phospholipid fatty acids (PLFAs). Glucose additions induced positive priming (a 12–52% increase in SOM respiration) in all soil types, but there was no linear relationship between priming and the soil C:N ratio. Instead, priming of SOM respiration was positively linked to the C:N imbalance, where a higher C:N imbalance implies stronger microbial N limitation. The total oxidative enzyme activity and the ratio between the activities of C and N acquiring enzymes were lower in soil with higher C:N ratios, but these findings could not be quantitatively linked to the observed priming rates. It appears as if glucose addition resulted in priming by stimulating the activity rather than the concentration of oxidative enzymes. Microbial incorporation of D and 13C into in PLFAs demonstrated that glucose additions stimulated both fungal and bacterial growth. The increased growth was mainly supported by glucose assimilation in fungi, while the increase in bacterial growth partly was a result of increased availability of C or N released from SOM. Taken together, the findings suggest that the soil C:N ratio is a poor predictor of priming and that priming is more dependent on the C:N imbalance, which reflects both microbial nutrient demand and nutrient provision.
650 7a LANTBRUKSVETENSKAPERx Lantbruksvetenskap, skogsbruk och fiskex Markvetenskap0 (SwePub)401062 hsv//swe
650 7a AGRICULTURAL SCIENCESx Agriculture, Forestry and Fisheriesx Soil Science0 (SwePub)401062 hsv//eng
653 a 13C
653 a Carbon use efficiency
653 a D
653 a N mining
653 a PLFA
653 a Priming effect
700a Alaei, Saeedu Lund University,Lunds universitet,MEMEG,Biologiska institutionen,Naturvetenskapliga fakulteten,Department of Biology,Faculty of Science4 aut0 (Swepub:lu)biol-sda
700a Li, Jianu Lund University,Lunds universitet,Mikrobiologisk ekologi,Forskargrupper vid Lunds universitet,Microbial Ecology,Lund University Research Groups4 aut0 (Swepub:lu)ji7426li
700a Merilä, Päiviu Natural Resources Institute Finland (Luke)4 aut
700a Ostonen, Ivikau University of Tartu4 aut
700a Bengtson, Peru Lund University,Lunds universitet,MEMEG,Biologiska institutionen,Naturvetenskapliga fakulteten,BECC: Biodiversity and Ecosystem services in a Changing Climate,Centrum för miljö- och klimatvetenskap (CEC),Mikrobiologisk ekologi,Forskargrupper vid Lunds universitet,Department of Biology,Faculty of Science,Centre for Environmental and Climate Science (CEC),Microbial Ecology,Lund University Research Groups4 aut0 (Swepub:lu)ekol-pbe
710a University of Helsinkib MEMEG4 org
773t Soil Biology and Biochemistryd : Elsevier BVg 167q 167x 0038-0717
856u http://dx.doi.org/10.1016/j.soilbio.2022.108615x freey FULLTEXT
8564 8u https://lup.lub.lu.se/record/06e6968b-900b-45ed-a7ab-f421059535af
8564 8u https://doi.org/10.1016/j.soilbio.2022.108615

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