TY - JOUR
T1 - Responses of AM fungal abundance to the drivers of global climate change
T2 - A meta-analysis
AU - Hu, Han
AU - He, Liyuan
AU - Ma, Huanfei
AU - Wang, Jieying
AU - Li, Yi
AU - Wang, Jun
AU - Guo, Yaoxin
AU - Ren, Chengjie
AU - Bai, Hongying
AU - Zhao, Fazhu
N1 - Publisher Copyright:
© 2021 Elsevier B.V.
PY - 2022/1/20
Y1 - 2022/1/20
N2 - Arbuscular mycorrhizal fungi (AMF), playing critical roles in carbon cycling, are vulnerable to climate change. However, the responses of AM fungal abundance to climate change are unclear. A global-scale meta-analysis was conducted to investigate the response patterns of AM fungal abundance to warming, elevated CO2 concentration (eCO2), and N addition. Both warming and eCO2 significantly stimulated AM fungal abundance by 18.6% (95%CI: 5.9%–32.8%) and 21.4% (15.1%–28.1%) on a global scale, respectively. However, the response ratios (RR) of AM fungal abundance decreased with the degree of warming while increased with the degree of eCO2. Furthermore, in warming experiments, as long as the warming exceeded 4 °C, its effects on AM fungal abundance changed from positive to negative regardless of the experimental durations, methods, periods, and ecosystem types. The effects of N addition on AM fungal abundance are −5.4% (−10.6%–0.2%), and related to the nitrogen fertilizer input rate and ecosystem type. The RR of AM fungal abundance is negative in grasslands and farmlands when the degree of N addition exceeds 33.85 and 67.64 kg N ha−1 yr−1, respectively; however, N addition decreases AM fungal abundance in forests only when the degree of N addition exceeds 871.31 kg N ha−1 yr−1. The above results provide an insight into predicting ecological functions of AM fungal abundance under global changes.
AB - Arbuscular mycorrhizal fungi (AMF), playing critical roles in carbon cycling, are vulnerable to climate change. However, the responses of AM fungal abundance to climate change are unclear. A global-scale meta-analysis was conducted to investigate the response patterns of AM fungal abundance to warming, elevated CO2 concentration (eCO2), and N addition. Both warming and eCO2 significantly stimulated AM fungal abundance by 18.6% (95%CI: 5.9%–32.8%) and 21.4% (15.1%–28.1%) on a global scale, respectively. However, the response ratios (RR) of AM fungal abundance decreased with the degree of warming while increased with the degree of eCO2. Furthermore, in warming experiments, as long as the warming exceeded 4 °C, its effects on AM fungal abundance changed from positive to negative regardless of the experimental durations, methods, periods, and ecosystem types. The effects of N addition on AM fungal abundance are −5.4% (−10.6%–0.2%), and related to the nitrogen fertilizer input rate and ecosystem type. The RR of AM fungal abundance is negative in grasslands and farmlands when the degree of N addition exceeds 33.85 and 67.64 kg N ha−1 yr−1, respectively; however, N addition decreases AM fungal abundance in forests only when the degree of N addition exceeds 871.31 kg N ha−1 yr−1. The above results provide an insight into predicting ecological functions of AM fungal abundance under global changes.
KW - AM fungal abundance
KW - Ecological consequence
KW - Elevated CO concentration
KW - N addition
KW - Warming
KW - meta-analysis
UR - http://www.scopus.com/inward/record.url?scp=85115082617&partnerID=8YFLogxK
U2 - 10.1016/j.scitotenv.2021.150362
DO - 10.1016/j.scitotenv.2021.150362
M3 - Article
C2 - 34818817
AN - SCOPUS:85115082617
SN - 0048-9697
VL - 805
JO - Science of the Total Environment
JF - Science of the Total Environment
M1 - 150362
ER -