TY - JOUR
T1 - Effects of forest degradation on microbial communities and soil carbon cycling
T2 - A global meta-analysis
AU - Zhou, Zhenghu
AU - Wang, Chuankuan
AU - Luo, Yiqi
N1 - Funding Information:
We thank all the researchers whose data were used in this meta-analysis, and Brian McGill, Maria Dornelas, Richard Field, Xiaofeng Xu and three anonymous referees for their valuable comments. This work was financially supported by the National Key Technology Research and Development Program of China (No. 2011BAD37B01) and the Program for Changjiang Scholars and Innovative Research Team in University (IRT_15R09) to C.K.W., and the Fundamental Research Funds for the Central Universities (2572016AA08) to Z.H.Z.
Publisher Copyright:
© 2017 John Wiley & Sons Ltd
PY - 2018/1
Y1 - 2018/1
N2 - Aim: The aim was to explore how conversions of primary or secondary forests to plantations or agricultural systems influence soil microbial communities and soil carbon (C) cycling. Location: Global. Time period: 1993–2017. Major taxa studied: Soil microbes. Methods: A meta-analysis was conducted to examine effects of forest degradation on soil properties and microbial attributes related to microbial biomass, activity, community composition and diversity based on 408 cases from 119 studies in the world. Results: Forest degradation decreased the ratios of K-strategists to r-strategists (i.e., ratios of fungi to bacteria, Acidobacteria to Proteobacteria, Actinobacteria to Bacteroidetes and Acidobacteria + Actinobacteria to Proteobacteria + Bacteroidetes). The response ratios (RRs) of the K-strategist to r-strategist ratios to forest degradation decreased and increased with increased RRs of soil pH and soil C to nitrogen ratio (C:N), respectively. Forest degradation increased the bacterial alpha-diversity indexes, of which the RRs increased and decreased as the RRs of soil pH and soil C:N increased, respectively. The overall RRs across all the forest degradation types ranked as microbial C (−40.4%) > soil C (−33.3%) > microbial respiration (−18.9%) > microbial C to soil C ratio (qMBC; −15.9%), leading to the RRs of microbial respiration rate per unit microbial C (qCO2) and soil C decomposition rate (respiration rate per unit soil C), on average, increasing by +43.2 and +25.0%, respectively. Variances of the RRs of qMBC and qCO2 were significantly explained by the soil C, soil C:N and mean annual precipitation. Main conclusions: Forest degradation consistently shifted soil microbial community compositions from K-strategist dominated to r-strategist dominated, altered soil properties and stimulated microbial activity and soil C decomposition. These results are important for modelling the soil C cycling under projected global land-use changes and provide supportive evidence for applying the macroecology theory on ecosystem succession and disturbance in soil microbial ecology.
AB - Aim: The aim was to explore how conversions of primary or secondary forests to plantations or agricultural systems influence soil microbial communities and soil carbon (C) cycling. Location: Global. Time period: 1993–2017. Major taxa studied: Soil microbes. Methods: A meta-analysis was conducted to examine effects of forest degradation on soil properties and microbial attributes related to microbial biomass, activity, community composition and diversity based on 408 cases from 119 studies in the world. Results: Forest degradation decreased the ratios of K-strategists to r-strategists (i.e., ratios of fungi to bacteria, Acidobacteria to Proteobacteria, Actinobacteria to Bacteroidetes and Acidobacteria + Actinobacteria to Proteobacteria + Bacteroidetes). The response ratios (RRs) of the K-strategist to r-strategist ratios to forest degradation decreased and increased with increased RRs of soil pH and soil C to nitrogen ratio (C:N), respectively. Forest degradation increased the bacterial alpha-diversity indexes, of which the RRs increased and decreased as the RRs of soil pH and soil C:N increased, respectively. The overall RRs across all the forest degradation types ranked as microbial C (−40.4%) > soil C (−33.3%) > microbial respiration (−18.9%) > microbial C to soil C ratio (qMBC; −15.9%), leading to the RRs of microbial respiration rate per unit microbial C (qCO2) and soil C decomposition rate (respiration rate per unit soil C), on average, increasing by +43.2 and +25.0%, respectively. Variances of the RRs of qMBC and qCO2 were significantly explained by the soil C, soil C:N and mean annual precipitation. Main conclusions: Forest degradation consistently shifted soil microbial community compositions from K-strategist dominated to r-strategist dominated, altered soil properties and stimulated microbial activity and soil C decomposition. These results are important for modelling the soil C cycling under projected global land-use changes and provide supportive evidence for applying the macroecology theory on ecosystem succession and disturbance in soil microbial ecology.
KW - carbon decomposition
KW - forest degradation
KW - land use
KW - microbial community
KW - microbial diversity
KW - microbial metabolic quotient
KW - soil carbon
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U2 - 10.1111/geb.12663
DO - 10.1111/geb.12663
M3 - Article
AN - SCOPUS:85031754625
SN - 1466-822X
VL - 27
SP - 110
EP - 124
JO - Global Ecology and Biogeography
JF - Global Ecology and Biogeography
IS - 1
ER -