Microbial and mineral interactions decouple litter quality from soil organic matter formation

Current understanding of soil carbon dynamics suggests that plant litter quality and soil mineralogy control the formation of mineral-associated soil organic carbon (SOC). Due to more efficient microbial anabolism, high-quality litter may produce more microbial residues for stabilisation on mineral surfaces. To test these fundamental concepts, we manipulate soil mineralogy using pristine minerals, characterise microbial communities and use stable isotopes to measure decomposition of low- and high-quality litter and mineral stabilisation of litter-C. We find that high-quality litter leads to less (not more) efficient formation of mineral-associated SOC due to soil microbial community shifts which lower carbon use efficiency. Low-quality litter enhances loss of pre-existing SOC resulting in no effect of litter quality on total mineral-associated SOC. However, mineral-associated SOC formation is primarily controlled by soil mineralogy. These findings refute the hypothesis that high-quality plant litters form mineral-associated SOC most efficiently and advance our understanding of how mineralogy and litter-microbial interactions regulate SOC formation.

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Publication Details

Journal
Nature Communications
Published
2024-11-20
DOI
https://doi.org/10.1038/s41467-024-54446-0
Citations
57
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
19.02

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article

Microbial and mineral interactions decouple litter quality from soil organic matter formation

Ashley C. Taylor, Niall P. McNamara, Tim Goodall, Caroline L. Peacock et al.
57 citations
Nature Communications
Soil Carbon and Nitrogen Dynamics
19.02
article

Microbial and mineral interactions decouple litter quality from soil organic matter formation

Ashley C. Taylor, Niall P. McNamara, Tim Goodall, Caroline L. Peacock, Robert I. Griffiths, Steven A. Banwart, Alba Otero-Fariña, Joseph Holden, Nick Ostle, Pengzhi Zhao, Kelly E. Mason, Pippa J. Chapman, Jeanette Whitaker, Dafydd Elias, Hongmei Chen
article en
57 citations

Abstract

Current understanding of soil carbon dynamics suggests that plant litter quality and soil mineralogy control the formation of mineral-associated soil organic carbon (SOC). Due to more efficient microbial anabolism, high-quality litter may produce more microbial residues for stabilisation on mineral surfaces. To test these fundamental concepts, we manipulate soil mineralogy using pristine minerals, characterise microbial communities and use stable isotopes to measure decomposition of low- and high-quality litter and mineral stabilisation of litter-C. We find that high-quality litter leads to less (not more) efficient formation of mineral-associated SOC due to soil microbial community shifts which lower carbon use efficiency. Low-quality litter enhances loss of pre-existing SOC resulting in no effect of litter quality on total mineral-associated SOC. However, mineral-associated SOC formation is primarily controlled by soil mineralogy. These findings refute the hypothesis that high-quality plant litters form mineral-associated SOC most efficiently and advance our understanding of how mineralogy and litter-microbial interactions regulate SOC formation.

Nature CommunicationsVol. 15(1)
University of Leeds (GB), Bangor University (GB), Universidade de Santiago de Compostela (ES), UK Centre for Ecology & Hydrology (GB), Lancaster University (GB), UCLouvain (BE)
Sight Research UK, University of Leeds, Natural Environment Research Council
Life in Land
Openalex Percentile: Top 0%
Soil Carbon and Nitrogen Dynamics
19.02
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