Interactive effects of global change factors on soil respiration and its components : a meta-analysis

© 2016 John Wiley & Sons Ltd.

Détails bibliographiques
Publié dans:Global change biology. - 1999. - 22(2016), 9 vom: 19. Sept., Seite 3157-69
Auteur principal: Zhou, Lingyan (Auteur)
Autres auteurs: Zhou, Xuhui, Shao, Junjiong, Nie, Yuanyuan, He, Yanghui, Jiang, Liling, Wu, Zhuoting, Hosseini Bai, Shahla
Format: Article en ligne
Langue:English
Publié: 2016
Accès à la collection:Global change biology
Sujets:Journal Article Meta-Analysis drought elevated CO2 irrigation nitrogen addition soil respiration warming Soil Nitrogen N762921K75
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520 |a As the second largest carbon (C) flux between the atmosphere and terrestrial ecosystems, soil respiration (Rs) plays vital roles in regulating atmospheric CO2 concentration ([CO2 ]) and climatic dynamics in the earth system. Although numerous manipulative studies and a few meta-analyses have been conducted to determine the responses of Rs and its two components [i.e., autotrophic (Ra) and heterotrophic (Rh) respiration] to single global change factors, the interactive effects of the multiple factors are still unclear. In this study, we performed a meta-analysis of 150 multiple-factor (≥2) studies to examine the main and interactive effects of global change factors on Rs and its two components. Our results showed that elevated [CO2 ] (E), nitrogen addition (N), irrigation (I), and warming (W) induced significant increases in Rs by 28.6%, 8.8%, 9.7%, and 7.1%, respectively. The combined effects of the multiple factors, EN, EW, DE, IE, IN, IW, IEW, and DEW, were also significantly positive on Rs to a greater extent than those of the single-factor ones. For all the individual studies, the additive interactions were predominant on Rs (90.6%) and its components (≈70.0%) relative to synergistic and antagonistic ones. However, the different combinations of global change factors (e.g., EN, NW, EW, IW) indicated that the three types of interactions were all important, with two combinations for synergistic effects, two for antagonistic, and five for additive when at least eight independent experiments were considered. In addition, the interactions of elevated [CO2 ] and warming had opposite effects on Ra and Rh, suggesting that different processes may influence their responses to the multifactor interactions. Our study highlights the crucial importance of the interactive effects among the multiple factors on Rs and its components, which could inform regional and global models to assess the climate-biosphere feedbacks and improve predictions of the future states of the ecological and climate systems 
650 4 |a Journal Article 
650 4 |a Meta-Analysis 
650 4 |a drought 
650 4 |a elevated CO2 
650 4 |a irrigation 
650 4 |a nitrogen addition 
650 4 |a soil respiration 
650 4 |a warming 
650 7 |a Soil  |2 NLM 
650 7 |a Nitrogen  |2 NLM 
650 7 |a N762921K75  |2 NLM 
700 1 |a Zhou, Xuhui  |e verfasserin  |4 aut 
700 1 |a Shao, Junjiong  |e verfasserin  |4 aut 
700 1 |a Nie, Yuanyuan  |e verfasserin  |4 aut 
700 1 |a He, Yanghui  |e verfasserin  |4 aut 
700 1 |a Jiang, Liling  |e verfasserin  |4 aut 
700 1 |a Wu, Zhuoting  |e verfasserin  |4 aut 
700 1 |a Hosseini Bai, Shahla  |e verfasserin  |4 aut 
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773 1 8 |g volume:22  |g year:2016  |g number:9  |g day:19  |g month:09  |g pages:3157-69 
856 4 0 |u http://dx.doi.org/10.1111/gcb.13253  |3 Volltext 
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