TY - JOUR
T1 - A keystone microbial enzyme for nitrogen control of soil carbon storage
AU - Chen, Ji
AU - Luo, Yiqi
AU - Van Groenigen, Kees Jan
AU - Hungate, Bruce A.
AU - Cao, Junji
AU - Zhou, Xuhui
AU - Wang, Rui wu
N1 - Publisher Copyright:
Copyright © 2018 The Authors,
PY - 2018/8/22
Y1 - 2018/8/22
N2 - Agricultural and industrial activities have increased atmospheric nitrogen (N) deposition to ecosystems worldwide. N deposition can stimulate plant growth and soil carbon (C) input, enhancing soil C storage. Changes in microbial decomposition could also influence soil C storage, yet this influence has been difficult to discern, partly because of the variable effects of added N on the microbial enzymes involved. We show, using meta-analysis, that added N reduced the activity of lignin-modifying enzymes (LMEs), and that this N-induced enzyme suppression was associated with increases in soil C. In contrast, N-induced changes in cellulase activity were unrelated to changes in soil C. Moreover, the effects of added soil N on LME activity accounted for more of the variation in responses of soil C than a wide range of other environmental and experimental factors. Our results suggest that, through responses of a single enzyme system to added N, soil microorganisms drive long-term changes in soil C accumulation. Incorporating this microbial influence on ecosystem biogeochemistry into Earth system models could improve predictions of ecosystem C dynamics.
AB - Agricultural and industrial activities have increased atmospheric nitrogen (N) deposition to ecosystems worldwide. N deposition can stimulate plant growth and soil carbon (C) input, enhancing soil C storage. Changes in microbial decomposition could also influence soil C storage, yet this influence has been difficult to discern, partly because of the variable effects of added N on the microbial enzymes involved. We show, using meta-analysis, that added N reduced the activity of lignin-modifying enzymes (LMEs), and that this N-induced enzyme suppression was associated with increases in soil C. In contrast, N-induced changes in cellulase activity were unrelated to changes in soil C. Moreover, the effects of added soil N on LME activity accounted for more of the variation in responses of soil C than a wide range of other environmental and experimental factors. Our results suggest that, through responses of a single enzyme system to added N, soil microorganisms drive long-term changes in soil C accumulation. Incorporating this microbial influence on ecosystem biogeochemistry into Earth system models could improve predictions of ecosystem C dynamics.
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U2 - 10.1126/sciadv.aaq1689
DO - 10.1126/sciadv.aaq1689
M3 - Article
C2 - 30140736
AN - SCOPUS:85052246155
SN - 2375-2548
VL - 4
JO - Science Advances
JF - Science Advances
IS - 8
M1 - eaaq1689
ER -