Ecosystem Carbon Use Efficiency Is Insensitive to Nitrogen Addition in an Alpine Meadow
Fangfang Ma, Bing Song, Fangyue Zhang, Quan Quan, Qingping Zhou, Shuli Niu
Abstract
Fangfang Ma, Bing Song, Fangyue Zhang, Quan Quan, Qingping Zhou, Shuli Niu
Abstract
Abstract Carbon use efficiency (CUE) is an important variable in carbon cycling and a key parameter in biogeochemical models, which is expected to increase with N availability. However, how CUE changes with N input rate remains elusive and lacks field evidence. We implemented a field manipulative experiment to examine effects of N addition with six levels of rate (0, 2, 4, 8, 16, and 32 g·N·m−2·year−1) on canopy CUE (the ratio of net primary productivity [NPP] to gross primary productivity [GPP]) and ecosystem CUE (the ratio of net ecosystem productivity [NEP] to GPP) in an alpine meadow on the Tibetan Plateau in 2014–2016. Over the 3 years, nitrogen addition treatments did not change canopy CUE or ecosystem CUE in comparing with the control, although it significantly increased GPP, NPP, and NEP; those components of CUE had the same response patterns to N addition rates, which shifted from linear responses in the first year to saturation responses thereafter. Moreover, GPP showed a positive linear relationship with NEP, NPP, ecosystem respiration, and autotrophic respiration under each N addition treatment with no changes in slope. The inherent coupling between GPP and ecosystem respiration, as well as GPP and autotrophic respiration, made CUE less sensitive to N addition than carbon fluxes themselves. The conclusions challenge the widely held hypothesis that ecosystem CUE increases with N addition. This study provides the first empirical evidences on the proposition that CUE is insensitive to N availability, which is of importance in model construction and parameterization.
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Abstract Carbon use efficiency (CUE) is an important variable in carbon cycling and a key parameter in biogeochemical models, which is expected to increase with N availability. However, how CUE changes with N input rate remains elusive and lacks field evidence. We implemented a field manipulative experiment to examine effects of N addition with six levels of rate (0, 2, 4, 8, 16, and 32 g·N·m−2·year−1) on canopy CUE (the ratio of net primary productivity [NPP] to gross primary productivity [GPP]) and ecosystem CUE (the ratio of net ecosystem productivity [NEP] to GPP) in an alpine meadow on the Tibetan Plateau in 2014–2016. Over the 3 years, nitrogen addition treatments did not change canopy CUE or ecosystem CUE in comparing with the control, although it significantly increased GPP, NPP, and NEP; those components of CUE had the same response patterns to N addition rates, which shifted from linear responses in the first year to saturation responses thereafter. Moreover, GPP showed a positive linear relationship with NEP, NPP, ecosystem respiration, and autotrophic respiration under each N addition treatment with no changes in slope. The inherent coupling between GPP and ecosystem respiration, as well as GPP and autotrophic respiration, made CUE less sensitive to N addition than carbon fluxes themselves. The conclusions challenge the widely held hypothesis that ecosystem CUE increases with N addition. This study provides the first empirical evidences on the proposition that CUE is insensitive to N availability, which is of importance in model construction and parameterization.
Key concepts: Primary production, Ecosystem respiration, Ecosystem, Environmental science, Biogeochemical cycle, Carbon cycle, Autotroph, Productivity