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Sökning: id:"swepub:oai:lup.lub.lu.se:44d5a88b-28d5-4ede-b1e0-472fa3b5cb56" > Decoding the rhizod...

Decoding the rhizodeposit-derived carbon's journey into soil organic matter

Teixeira, Pedro P.C. (författare)
Technical University of Munich,Federal University of Viçosa
Vidal, Alix (författare)
Wageningen University
Teixeira, Ana P.M. (författare)
Federal University of Viçosa
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Souza, Ivan F. (författare)
Federal University of Viçosa
Hurtarte, Luís C.C. (författare)
European Synchrotron Radiation Facility,Diamond Light Source
Silva, Danilo H.S. (författare)
Federal University of Viçosa
Almeida, Luís F.J. (författare)
Federal University of Viçosa
Buegger, Franz (författare)
Helmholtz Zentrum München
Hammer, Edith C. (författare)
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,LU profilområde: Naturbaserade framtidslösningar,Lunds universitets profilområden,Department of Biology,Faculty of Science,Centre for Environmental and Climate Science (CEC),Microbial Ecology,Lund University Research Groups,LU Profile Area: Nature-based future solutions,Lund University Profile areas
Jansa, Jan (författare)
Institute of Microbiology of the Academy of Sciences of the Czech Republic
Mueller, Carsten W. (författare)
University of Copenhagen,Technical University of Berlin
Silva, Ivo R. (författare)
Federal University of Viçosa
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 (creator_code:org_t)
2024
2024
Engelska.
Ingår i: Geoderma. - 0016-7061. ; 443
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Net rhizodeposition corresponds to the portion of living root carbon (C) that remains in the soil after microbial processing and partial decomposition. Although it is assumed that this C input exerts an important role in the formation of soil organic matter (SOM), its contribution to distinct SOM pools is still not fully understood. In this study, we aimed to (i) quantify the retention of net rhizodeposition C in the different SOM fractions and in reactive Al and Fe mineral phases and (ii) investigate how rhizodeposition drives the spatial distribution of microbial communities in the rhizosphere. To track the transfer of net rhizodeposition into the soil, we used artificially labeled eucalypt (Eucalyptus spp.) seedlings under a 13C-CO2 atmosphere (multiple-pulse labeling). Combining physical SOM fractionation and the chemical extraction of aluminum (Al) and iron (Fe) reactive phases, we studied the distribution of net rhizodeposition into different soil fractions. We also assessed the 13C incorporation into microbial phospholipid fatty acids (PLFAs) at different distances from the roots. Our results show that 76 % of the net rhizodeposition 13C was retained within the mineral-associated organic matter (MAOM) fraction. About 28 % of net rhizodeposition 13C within the MAOM fraction was retained within the Al and Fe reactive phases, indicating that this is a sizeable mechanism for the retention of net rhizodeposition in soil. Rhizodeposition increased the abundance of microbial PLFAs exclusively in the soil close to the roots (0–4 mm), with prominent incorporation of net rhizodeposition 13C into fungal biomarkers. Overall, our findings underscore the importance of mineral associations for the retention of net rhizodeposition in the soil. We also highlight the role of fungi in transferring the root-derived C beyond the root vicinity and promoting the formation of occluded SOM.

Ämnesord

LANTBRUKSVETENSKAPER  -- Lantbruksvetenskap, skogsbruk och fiske -- Markvetenskap (hsv//swe)
AGRICULTURAL SCIENCES  -- Agriculture, Forestry and Fisheries -- Soil Science (hsv//eng)

Nyckelord

C pulse labeling
Eucalypt
Metal-organic complexes
Mineral-associated organic matter (MAOM)
Net rhizodeposition
Phospholipid fatty acids
Rhizosphere
Short-range order minerals
Tropical soils

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