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   <subfield code="a">10.1007/s11104-014-2254-y</subfield>
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   <subfield code="a">Litter decomposition and soil microbial community composition in three Korean pine ( Pinus koraiensis ) forests along an altitudinal gradient</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Yong Zhou, Michele Clark, Jiaqi Su, Chunwang Xiao]</subfield>
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   <subfield code="a">Background and aims: : The factors controlling litter decomposition and soil microbial community are important regulators of biogeochemical processes. Here we aim to explore controls on litter decomposition dynamics and soil microbial community composition in temperate forest by comparing three Korean pine forests along an altitudinal gradient. Methods: : Single- and mixed-species litter decomposition rates were determined by the litterbag method and soil microbial community composition was characterized by PLFAs. Results: : Litter decomposition rates decreased with altitude regardless of litter type, and were controlled by temperature. Generally, fine root litter decomposed more rapidly than leaf litter, and mixed-species litter decomposed faster than single-species. Soil microbial biomass C and N decreased with altitude and varied differently among forest types in response to soil temperature and nutrient status. Fungal: bacterial PLFA ratios were significantly larger in forests receiving relatively poor litter quality inputs. Soil temperature, soil water content, total soil N and P were all directly related to the changes in total PLFAs among three forests. Conclusions: : In these Korean pines dominated temperate forests, environmental changes associated with altitude gradient drive decomposition dynamics and soil microbial community composition. This implies that climate change might be an important factor affecting these systems in the future.</subfield>
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   <subfield code="a">Springer International Publishing Switzerland, 2014</subfield>
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   <subfield code="a">Korean pine forest</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Altitudinal gradient</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Litter decomposition</subfield>
   <subfield code="2">nationallicence</subfield>
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   <subfield code="a">Soil microbial biomass</subfield>
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   <subfield code="a">PLFA</subfield>
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   <subfield code="a">Zhou</subfield>
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   <subfield code="u">State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, the Chinese Academy of Sciences, No. 20 Nanxincun, Xiangshan, 100093, Beijing, China</subfield>
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   <subfield code="u">Department of Ecosystem Science and Management, Texas A&amp;M University, College Station, 77843-2138, Texas, USA</subfield>
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   <subfield code="u">State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, the Chinese Academy of Sciences, No. 20 Nanxincun, Xiangshan, 100093, Beijing, China</subfield>
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   <subfield code="u">State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, the Chinese Academy of Sciences, No. 20 Nanxincun, Xiangshan, 100093, Beijing, China</subfield>
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   <subfield code="t">Plant and Soil</subfield>
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   <subfield code="g">386/1-2(2015-01-01), 171-183</subfield>
   <subfield code="x">0032-079X</subfield>
   <subfield code="q">386:1-2&lt;171</subfield>
   <subfield code="1">2015</subfield>
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   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <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>
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