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Biogeochemistry

, Volume 140, Issue 1, pp 81–92 | Cite as

Microbial and plant-derived compounds both contribute to persistent soil organic carbon in temperate soils

  • Pierre BarréEmail author
  • Katell Quénéa
  • Alix Vidal
  • Lauric Cécillon
  • Bent T. Christensen
  • Thomas Kätterer
  • Andy Macdonald
  • Léo Petit
  • Alain F. Plante
  • Folkert van Oort
  • Claire Chenu
Article

Abstract

Our study tests the emerging paradigm that biochemical recalcitrance does not affect substantially long-term (50 years) SOC persistence. We analyzed the molecular composition of SOC in archived soils originating from four European long-term bare fallow experiments (Askov, Rothamsted, Versailles and Ultuna). The soils had been collected after various periods (up to 53 years) under bare fallow. With increasing duration of bare fallow without new organic inputs, the relative abundance of cutin- and suberin-derived compounds declined substantially, and the abundance of lignin-derived compounds was close to zero. Conversely, the relative abundance of plant-derived long-chain alkanes remained almost constant or increased during the bare fallow period. The relative abundance of N-containing compounds, considered to be abundant in SOC derived from microbial activity, increased consistently illustrating that microbial turnover of SOC continues even when plant inputs are stopped. The persistence of the different families of plant-derived compounds differed markedly over the scale of half a century, which may be ascribed to their contrasting chemical characteristics and recalcitrance, or to differences in their interactions with the soil mineral matrix, and likely some combination since chemical composition drives the degree of mineral association. Using soil from this unique set of long-term bare fallow experiments, we provide direct evidence that multi-decadal scale persistent SOC is enriched in microbe-derived compounds but also includes a substantial fraction of plant-derived compounds.

Keywords

TMAH-Py–GC–MS Long-term bare fallow Plant-derived compounds Soil organic carbon persistence 

Notes

Acknowledgements

The INSU EC2CO program is acknowledged for financial support (CARACAS Project). We thank Rothamsted Research and the Lawes Agricultural Trust for access to archived samples and the BBSRC for support under the Institute National Capabilities program grant. Related information and data can be found in the electronic Rothamsted Archive (era.rothamsted.ac.uk). The Danish contribution was financially supported by The Ministry of Environment and Food. The Swedish contribution was supported by the Faculty of Natural Resources and Agriculture at the Swedish University of Agricultural Sciences. We thank the two reviewers for their constructive comments on the manuscript.

Supplementary material

10533_2018_475_MOESM1_ESM.docx (20 kb)
Supplementary material 1 (DOCX 19 kb)
10533_2018_475_MOESM2_ESM.docx (23 kb)
Supplementary material 2 (DOCX 23 kb)

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Copyright information

© Springer Nature Switzerland AG 2018

Authors and Affiliations

  • Pierre Barré
    • 1
    Email author
  • Katell Quénéa
    • 2
  • Alix Vidal
    • 3
  • Lauric Cécillon
    • 4
  • Bent T. Christensen
    • 5
  • Thomas Kätterer
    • 6
  • Andy Macdonald
    • 7
  • Léo Petit
    • 2
  • Alain F. Plante
    • 8
  • Folkert van Oort
    • 9
  • Claire Chenu
    • 9
  1. 1.Laboratoire de Géologie de l’ENS - PSL Research University – CNRS UMR8538ParisFrance
  2. 2.Sorbonne Universités, UPMC Univ Paris 06, CNRS, EPHE, UMR 7619 MetisParis Cedex 05France
  3. 3.Lehrstuhl für BodenkundeTU MünchenFreisingGermany
  4. 4.Université Grenoble Alpes, Irstea, UR EMGRSt-Martin-d’HèresFrance
  5. 5.Department of AgroecologyAarhus UniversityTjeleDenmark
  6. 6.Department of EcologySwedish University of Agricultural SciencesUppsalaSweden
  7. 7.Department of Sustainable Agriculture SciencesRothamsted ResearchHarpendenUK
  8. 8.Earth and Environmental ScienceUniversity of PennsylvaniaPhiladelphiaUSA
  9. 9.AgroParisTech – INRA, UMR 1402 ECOSYSThiverval GrignonFrance

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