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   <subfield code="a">10.1007/s11104-014-2299-y</subfield>
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   <subfield code="a">Effect of plant communities on aggregate composition and organic matter stabilisation in young soils</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Anna Gunina, Irina Ryzhova, Maxim Dorodnikov, Yakov Kuzyakov]</subfield>
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   <subfield code="a">Objectives: Carbon (C) content in pools of very young soils that developed during 45years from loess was analysed in relation to vegetation: deciduous and coniferous forests and cropland. We hypothesised that variations in the amount of particulate organic matter (POM) can explain the C accumulation and also affects the C bound to mineral surfaces in soil under various vegetation. Methods: Soil samples were collected under three vegetation types of a 45-year-old experiment focused on initial soil development. Aggregate and density fractionations were combined to analyse C accumulation in large and small macro- and microaggregates as well as in free and occluded POM and mineral factions. Results: Deciduous forest soil accumulated the highest C content in the 0-5cm layer (43g C kg−1), whereas values in coniferous forest and arable soils were lower (30 and 12g C kg−1, respectively). The highest portion of C in arable soil was accumulated in the mineral fraction (80%), whereas 50-60% of the C in forest soils were in POM. More C was associated with minerals in deciduous forest soil (16g C kg−1 soil) than under coniferous forest and arable land (8-10g C kg−1 soil). Conclusions: Particulate organic matter explains most of the differences in organic C accumulation in soils developed during 45years under the three vegetation types on identical parent material. The C content of the mineral soil fraction was controlled by plant cover and contributed the most to differences in C accumulation in soils developed under similar vegetation type (forest).</subfield>
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   <subfield code="a">Springer International Publishing Switzerland, 2014</subfield>
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   <subfield code="a">Carbon sequestration</subfield>
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   <subfield code="a">Initial soil formation</subfield>
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   <subfield code="a">Carbon accumulation rates</subfield>
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   <subfield code="a">Aggregate turnover</subfield>
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   <subfield code="a">Organic matter stabilisation</subfield>
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   <subfield code="a">Gunina</subfield>
   <subfield code="D">Anna</subfield>
   <subfield code="u">Department of Agricultural Soil Science, Georg-August-University of Göttingen, Büsgenweg 2, 37077, Göttingen, Germany</subfield>
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   <subfield code="a">Ryzhova</subfield>
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   <subfield code="u">Faculty of Soil Science, Moscow Lomonosov State University, Moscow, Russian Federation</subfield>
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   <subfield code="a">Dorodnikov</subfield>
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   <subfield code="u">Department of Soil Science of Temperate Ecosystems, Georg-August-University of Göttingen, Göttingen, Germany</subfield>
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   <subfield code="u">Department of Agricultural Soil Science, Georg-August-University of Göttingen, Büsgenweg 2, 37077, Göttingen, Germany</subfield>
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   <subfield code="g">387/1-2(2015-02-01), 265-275</subfield>
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   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
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