Effects of livestock grazing on grassland carbon storage and release override impacts associated with global climate change

© 2018 John Wiley & Sons Ltd.

Détails bibliographiques
Publié dans:Global change biology. - 1999. - 25(2019), 3 vom: 28. März, Seite 1119-1132
Auteur principal: Zhou, Guiyao (Auteur)
Autres auteurs: Luo, Qin, Chen, Yajie, He, Miao, Zhou, Lingyan, Frank, Douglas, He, Yanghui, Fu, Yuling, Zhang, Baocheng, Zhou, Xuhui
Format: Article en ligne
Langue:English
Publié: 2019
Accès à la collection:Global change biology
Sujets:Journal Article Research Support, Non-U.S. Gov't C-climate feedback N fertilization drought elevated CO2 increased precipitation soil respiration warming Soil plus... Carbon 7440-44-0
Description
Résumé:© 2018 John Wiley & Sons Ltd.
Predicting future carbon (C) dynamics in grassland ecosystems requires knowledge of how grazing and global climate change (e.g., warming, elevated CO2 , increased precipitation, drought, and N fertilization) interact to influence C storage and release. Here, we synthesized data from 223 grassland studies to quantify the individual and interactive effects of herbivores and climate change on ecosystem C pools and soil respiration (Rs). Our results showed that grazing overrode global climate change factors in regulating grassland C storage and release (i.e., Rs). Specifically, grazing significantly decreased aboveground plant C pool (APCP), belowground plant C pool (BPCP), soil C pool (SCP), and Rs by 19.1%, 6.4%, 3.1%, and 4.6%, respectively, while overall effects of all global climate change factors increased APCP, BPCP, and Rs by 6.5%, 15.3%, and 3.4% but had no significant effect on SCP. However, the combined effects of grazing with global climate change factors also significantly decreased APCP, SCP, and Rs by 4.0%, 4.7%, and 2.7%, respectively but had no effect on BPCP. Most of the interactions between grazing and global climate change factors on APCP, BPCP, SCP, and Rs were additive instead of synergistic or antagonistic. Our findings highlight the dominant effects of grazing on C storage and Rs when compared with the suite of global climate change factors. Therefore, incorporating the dominant effect of herbivore grazing into Earth System Models is necessary to accurately predict climate-grassland feedbacks in the Anthropocene
Description:Date Completed 11.04.2019
Date Revised 11.04.2019
published: Print-Electronic
Citation Status MEDLINE
ISSN:1365-2486
DOI:10.1111/gcb.14533