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      C-STABILITY an innovative modeling framework to leverage the continuous representation of organic matter

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          Abstract

          The understanding of soil organic matter (SOM) dynamics has considerably advanced in recent years. It was previously assumed that most SOM consisted of recalcitrant compounds, whereas the emerging view considers SOM as a range of polymers continuously processed into smaller molecules by decomposer enzymes. Mainstreaming this new paradigm in current models is challenging because of their ill-adapted framework. We propose the C-STABILITY model to resolve this issue. Its innovative framework combines compartmental and continuous modeling approaches to accurately reproduce SOM cycling processes. C-STABILITY emphasizes the influence of substrate accessibility on SOM turnover and makes enzymatic and microbial biotransformations of substrate explicit. Theoretical simulations provide new insights on how depolymerization and decomposers ecology impact organic matter chemistry and amount during decomposition and at steady state. The flexible mathematical structure of C-STABILITY offers a promising foundation for exploring new mechanistic hypotheses and supporting the design of future experiments.

          Abstract

          Soil organic matter (SOM) is a huge sink of carbon, but the varied flux dynamics are challenging to predict. Here, the authors present a new model with the complexities of SOM cycling, including parameters for substrate accessibility, microbe diversity, and enzymatic substrate depolymerization.

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          Persistence of soil organic matter as an ecosystem property.

          Globally, soil organic matter (SOM) contains more than three times as much carbon as either the atmosphere or terrestrial vegetation. Yet it remains largely unknown why some SOM persists for millennia whereas other SOM decomposes readily--and this limits our ability to predict how soils will respond to climate change. Recent analytical and experimental advances have demonstrated that molecular structure alone does not control SOM stability: in fact, environmental and biological controls predominate. Here we propose ways to include this understanding in a new generation of experiments and soil carbon models, thereby improving predictions of the SOM response to global warming.
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            The contentious nature of soil organic matter.

            The exchange of nutrients, energy and carbon between soil organic matter, the soil environment, aquatic systems and the atmosphere is important for agricultural productivity, water quality and climate. Long-standing theory suggests that soil organic matter is composed of inherently stable and chemically unique compounds. Here we argue that the available evidence does not support the formation of large-molecular-size and persistent 'humic substances' in soils. Instead, soil organic matter is a continuum of progressively decomposing organic compounds. We discuss implications of this view of the nature of soil organic matter for aquatic health, soil carbon-climate interactions and land management.
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              Microbial control over carbon cycling in soil

              A major thrust of terrestrial microbial ecology is focused on understanding when and how the composition of the microbial community affects the functioning of biogeochemical processes at the ecosystem scale (meters-to-kilometers and days-to-years). While research has demonstrated these linkages for physiologically and phylogenetically “narrow” processes such as trace gas emissions and nitrification, there is less conclusive evidence that microbial community composition influences the “broad” processes of decomposition and organic matter (OM) turnover in soil. In this paper, we consider how soil microbial community structure influences C cycling. We consider the phylogenetic level at which microbes form meaningful guilds, based on overall life history strategies, and suggest that these are associated with deep evolutionary divergences, while much of the species-level diversity probably reflects functional redundancy. We then consider under what conditions it is possible for differences among microbes to affect process dynamics, and argue that while microbial community structure may be important in the rate of OM breakdown in the rhizosphere and in detritus, it is likely not important in the mineral soil. In mineral soil, physical access to occluded or sorbed substrates is the rate-limiting process. Microbial community influences on OM turnover in mineral soils are based on how organisms allocate the C they take up – not only do the fates of the molecules differ, but they can affect the soil system differently as well. For example, extracellular enzymes and extracellular polysaccharides can be key controls on soil structure and function. How microbes allocate C may also be particularly important for understanding the long-term fate of C in soil – is it sequestered or not?
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                Author and article information

                Contributors
                julien.sainte-marie@agroparistech.fr
                delphine.derrien@inrae.fr
                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group UK (London )
                2041-1723
                5 February 2021
                5 February 2021
                2021
                : 12
                : 810
                Affiliations
                [1 ]GRID grid.503480.a, Université de Lorraine, AgroParisTech, INRAE, SILVA, ; F-54000 Nancy, France
                [2 ]INRAE, BEF, F-54000 Nancy, France
                [3 ]GRID grid.29172.3f, ISNI 0000 0001 2194 6418, Université de Lorraine, CNRS, IECL, ; F-54000 Nancy, France
                [4 ]GRID grid.503276.5, ISNI 0000 0004 1763 486X, Université de Lorraine, INRAE, IAM, ; F-54000 Nancy, France
                [5 ]GRID grid.66741.32, ISNI 0000 0001 1456 856X, Beijing Advanced Innovation Center for Tree Breeding by Molecular Design, Beijing Forestry University, ; Beijing, China
                Author information
                http://orcid.org/0000-0002-8108-3519
                Article
                21079
                10.1038/s41467-021-21079-6
                7864906
                33547289
                b0a70728-df1c-48af-95cb-e6a0bcf9bf1f
                © The Author(s) 2021

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 21 April 2020
                : 11 January 2021
                Funding
                Funded by: Laboratory of Excellence ARBRE (ANR-11-LABX-0002-01)
                Categories
                Article
                Custom metadata
                © The Author(s) 2021

                Uncategorized
                ecological modelling,microbial ecology,soil microbiology,carbon cycle,geochemistry
                Uncategorized
                ecological modelling, microbial ecology, soil microbiology, carbon cycle, geochemistry

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