4.8 Article

CO2 fertilization of terrestrial photosynthesis inferred from site to global scales

出版社

NATL ACAD SCIENCES
DOI: 10.1073/pnas.2115627119

关键词

CO2 fertilization effect; photosynthesis; GPP; optimization theory; carbon and water coupling

资金

  1. US Department of Energy Office of Science Biological and Environmental Research, Reducing Uncertainties in Biogeochemical Interactions through Synthesis and Computation Scientific Focus Area
  2. NASA Terrestrial Ecology Program [NNH17AE86I, 80NSSC21K1705]
  3. LEMONTREE (Land Ecosystem Models based On New Theory, obseRvations and ExperimEnts) project

向作者/读者索取更多资源

Global photosynthesis is increasing due to elevated atmospheric CO2 concentrations, primarily as a result of the CO2 fertilization effect. Soil moisture and specific humidity play important roles in plant hydraulics. The global CO2-induced GPP trend is stronger than previously modeled or observed, mainly because of variations in the magnitude of the CO2 fertilization effect in evergreen broad-leaf forests.
Global photosynthesis is increasing with elevated atmospheric CO2 concentrations, a response known as the CO2 fertilization effect (CFE), but the key processes of CFE are not constrained and therefore remain uncertain. Here, we quantify CFE by combining observations from a globally distributed network of eddy covariance measurements with an analytical framework based on three well-established photosynthetic optimization theories. We report a strong enhancement of photosynthesis across the observational network (9.1 gC m(-2) year(-2)) and show that the CFE is responsible for 44% of the gross primary production (GPP) enhancement since the 2000s, with additional contributions primarily from warming (28%). Soil moisture and specific humidity are the two largest contributors to GPP interannual variation through their influences on plant hydraulics. Applying our framework to satellite observations and meteorological reanalysis data, we diagnose a global CO2-induced GPP trend of 4.4 gC m(-2) year(-2), which is at least one-third stronger than the median trends of 13 dynamic global vegetation models and eight satellite-derived GPP products, mainly because of their differences in the magnitude of CFE in evergreen broad-leaf forests. These results highlight the critical role that CFE has played in the global carbon cycle in recent decades.

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