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    <titleInfo>
      <title>Crops for increasing soil organic carbon stocks : a global meta analysis</title>
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      <namePart type="family">Mathew</namePart>
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      <namePart type="family">Mutema</namePart>
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    <name type="personnal">
      <namePart type="family">Minasny</namePart>
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    <abstract>Quantifying the ability of plants to store atmospheric inorganic carbon (C) in their biomass and ultimately in the soil as organic C for long duration is crucial for climate change mitigation and soil fertility improvement. While many independent studies have been performed on the transfer of atmospheric C to soils for single crop types, the objective of this study was to compare the ability of crops, which are most commonly found worldwide, to transfer C to soils, and the associated controlling factors. We performed a meta-analysis of 227 research trials, which had reported C fluxes from plant to soil for different crops. On average, crops assimilated 4.5 Mg C ha(-1) yr(-1) from the atmosphere with values between 1.7 Mg C ha(-1) yr(-1), for barley (Hordeum vulgare) and 5.2 Mg C ha(-1) yr(-1) for maize (Zea mays). Sixty-one percent (61%) of the assimilated C was allocated to shoots, 20% to roots, 7% to soils while 12% was respired back into the atmosphere as autotrophic respiration by plants. Maize and ryegrass (Lolium perenne) had the greatest allocation to the soil (1.0 Mg C ha(-1) yr(-1) or 19% total assimilation), followed by wheat (Triticum aestivum). 0.8 Mg C ha(-1) yr(-1) , 23%) and rice (Oryza Sativa, 0.7 Mg C ha(-1) yr(-1) , 20%). Carbon allocation to the soil positively correlated to C allocation to roots (r = 0.33, P &lt; 0.05), while correlations between shoot and root biomass on the one hand and C allocation to shoots on the other hand were not significant. The question on the long-term stability of the C transferred to soils remains unanswered.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>Carbon transfer</topic>
      <topic>C assimilation</topic>
      <topic>Plant C</topic>
      <topic>C labeling</topic>
      <topic>C flux</topic>
    </subject>
    <subject authority="local">
      <geographic>MONDE</geographic>
    </subject>
    <classification authority="local">068</classification>
    <classification authority="local">076</classification>
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      <titleInfo>
        <title>Geoderma</title>
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      <part>
        <detail type="volume">
          <number>367</number>
        </detail>
        <extent unit="pages">
          <list> art. 114230 [12p.]</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2020</dateIssued>
      </originInfo>
      <identifier type="issn">0016-7061</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010078945</identifier>
    <identifier type="doi">10.1016/j.geoderma.2020.114230</identifier>
    <identifier type="issn">0016-7061</identifier>
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