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[Contributions of soil fauna to litter decomposition in alpine/subalpine forests].

Identifieur interne : 001127 ( Main/Corpus ); précédent : 001126; suivant : 001128

[Contributions of soil fauna to litter decomposition in alpine/subalpine forests].

Auteurs : Rui-Long Liu ; Wei-Min Li ; Wan-Qin Yang ; Bo Tan ; Wen-Jun Wang ; Zhen-Feng Xu ; Fu-Zhong Wu

Source :

RBID : pubmed:24697051

English descriptors

Abstract

A field experiment was conducted using the litterbag method to quantify the contribution of soil fauna to litter mass loss of Salix paraplesia, Sabina saltuaria, Betula albosinensis and Abies faxoniana during different key periods of the decomposition process of the first year (from November 2011 to October 2012). The results showed that the mass loss rate showed S. paraplesia > B. albosinensis > A. faxoniana > S. saltuaria, and the rate in the growing season was greater than in the freeze-thaw season. The contribution rate of soil fauna to the mass decomposition displayed as S. saltuaria (26.7%) > A. faxoniana (18.8%) > B. albosinensis (15.7%) > S. paraplesia (13.2%), which was higher in the freeze-thaw season than in the growing season for litter of B. albo-sinensis and A. faxoniana while vice versa for litter of B. albosinensis and A. faxoniana. The contribution of soil fauna was mainly related to organic C, P and N/P in the freeze-thaw season, while N, C/N, lignin and lignin/cellulose in the growing season.

PubMed: 24697051

Links to Exploration step

pubmed:24697051

Le document en format XML

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<title xml:lang="en">[Contributions of soil fauna to litter decomposition in alpine/subalpine forests].</title>
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<name sortKey="Liu, Rui Long" sort="Liu, Rui Long" uniqKey="Liu R" first="Rui-Long" last="Liu">Rui-Long Liu</name>
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<name sortKey="Li, Wei Min" sort="Li, Wei Min" uniqKey="Li W" first="Wei-Min" last="Li">Wei-Min Li</name>
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<name sortKey="Yang, Wan Qin" sort="Yang, Wan Qin" uniqKey="Yang W" first="Wan-Qin" last="Yang">Wan-Qin Yang</name>
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<name sortKey="Tan, Bo" sort="Tan, Bo" uniqKey="Tan B" first="Bo" last="Tan">Bo Tan</name>
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<name sortKey="Wang, Wen Jun" sort="Wang, Wen Jun" uniqKey="Wang W" first="Wen-Jun" last="Wang">Wen-Jun Wang</name>
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<name sortKey="Xu, Zhen Feng" sort="Xu, Zhen Feng" uniqKey="Xu Z" first="Zhen-Feng" last="Xu">Zhen-Feng Xu</name>
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<div type="abstract" xml:lang="en">A field experiment was conducted using the litterbag method to quantify the contribution of soil fauna to litter mass loss of Salix paraplesia, Sabina saltuaria, Betula albosinensis and Abies faxoniana during different key periods of the decomposition process of the first year (from November 2011 to October 2012). The results showed that the mass loss rate showed S. paraplesia > B. albosinensis > A. faxoniana > S. saltuaria, and the rate in the growing season was greater than in the freeze-thaw season. The contribution rate of soil fauna to the mass decomposition displayed as S. saltuaria (26.7%) > A. faxoniana (18.8%) > B. albosinensis (15.7%) > S. paraplesia (13.2%), which was higher in the freeze-thaw season than in the growing season for litter of B. albo-sinensis and A. faxoniana while vice versa for litter of B. albosinensis and A. faxoniana. The contribution of soil fauna was mainly related to organic C, P and N/P in the freeze-thaw season, while N, C/N, lignin and lignin/cellulose in the growing season.</div>
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<AbstractText>A field experiment was conducted using the litterbag method to quantify the contribution of soil fauna to litter mass loss of Salix paraplesia, Sabina saltuaria, Betula albosinensis and Abies faxoniana during different key periods of the decomposition process of the first year (from November 2011 to October 2012). The results showed that the mass loss rate showed S. paraplesia > B. albosinensis > A. faxoniana > S. saltuaria, and the rate in the growing season was greater than in the freeze-thaw season. The contribution rate of soil fauna to the mass decomposition displayed as S. saltuaria (26.7%) > A. faxoniana (18.8%) > B. albosinensis (15.7%) > S. paraplesia (13.2%), which was higher in the freeze-thaw season than in the growing season for litter of B. albo-sinensis and A. faxoniana while vice versa for litter of B. albosinensis and A. faxoniana. The contribution of soil fauna was mainly related to organic C, P and N/P in the freeze-thaw season, while N, C/N, lignin and lignin/cellulose in the growing season.</AbstractText>
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