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   <subfield code="a">10.1007/s10533-015-0138-8</subfield>
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   <subfield code="a">NanoSIMS investigation of glycine-derived C and N retention with soil organo-mineral associations</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Pierre-Joseph Hatton, Laurent Remusat, Bernd Zeller, Elizabeth Brewer, Delphine Derrien]</subfield>
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   <subfield code="a">While microbial-mineral-organic matter interactions are key features controlling the fates of low molecular-weight compounds in soils, direct investigations of how they control their fine-scale spatial distribution are scant. Here, we addressed how microbial transformations affect the retention of 13C/15N-labeled glycine in a forest topsoil 8h after application. We assessed the contribution of soil microorganisms to glycine-derived 13C and 15N retention using γ-irradiated and non-irradiated soils. We tracked down the glycine-derived 13C and 15N at the surface of particles randomly isolated from soil density fractions using nano-scale secondary ions mass spectrometry (NanoSIMS) imaging. Eight hours after addition, 7% of the glycine-derived 13C and 15N initially applied was recovered among soil density fractions, mainly via the activity of soil microorganisms (&gt;85% of total retention). Glycine-derived 13C and 15N distribution among density fractions was correlated with that of soil organic matter (SOM) determined by NanoSIMS (R≥0.85), suggesting that the spatial patterns of the mineral-attached SOM controls the spatial distribution of the glycine-derived 13C and 15N. NanoSIMS images showed largely decoupled glycine-derived 13C and 15N spots preferentially attached to aggregated particles. We speculate that the glycine-derived 13C was principally found within or in the vicinity of microbial cells, whereas the glycine-derived 15N was mostly found as NH4 + and/or exoenzymes spread across soil surfaces. The C:N ratios determined by NanoSIMS suggest that local chemical properties of mineral-attached SOM drive glycine-derived 15N attachment, with the preferential attachment to mineral-attached SOM rich in N (C:N ratios mostly &lt;16). Few exceptions were found in presence of Al and Fe (hydr)oxides (&gt;2.65gcm−3).</subfield>
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   <subfield code="a">Springer International Publishing Switzerland, 2015</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Soil</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Density</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">NanoSIMS</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Glycine</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Biotic</subfield>
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   <subfield code="a">Retention</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Hatton</subfield>
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   <subfield code="a">Remusat</subfield>
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   <subfield code="u">Institut de Minéralogie, de Physique des Matériaux, et de Cosmochimie. UMR CNRS 7590, Sorbonne Universités, Muséum National d'Histoire Naturelle, UPMC, IRD, 61 rue Buffon, 75005, Paris, France</subfield>
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   <subfield code="a">Brewer</subfield>
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   <subfield code="u">Department of Crop and Soil Science, Oregon State University, 97331, Corvallis, OR, USA</subfield>
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   <subfield code="t">Biogeochemistry</subfield>
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   <subfield code="g">125/3(2015-09-01), 303-313</subfield>
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   <subfield code="a">BK010053</subfield>
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   <subfield code="c">XK010000</subfield>
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   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
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