Zhejiang Tiantong Forest Ecosystem National Observation and Research Station, Center for Global Change and Ecological Forecasting, School of Ecological and Environmental Sciences, East China Normal University, Shanghai 200241, China.
Physical and Life Sciences Directorate, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA; Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Boston, MA, USA.
Sci Total Environ. 2022 Dec 10;851(Pt 1):158243. doi: 10.1016/j.scitotenv.2022.158243. Epub 2022 Aug 23.
Plants may slow global warming through enhanced growth, because increased levels of photosynthesis stimulate the land carbon (C) sink. However, how climate warming affects plant C storage globally and key drivers determining the response of plant C storage to climate warming remains unclear, causing uncertainty in climate projections. We performed a comprehensive meta-analysis, compiling 393 observations from 99 warming studies to examine the global patterns of plant C storage responses to climate warming and explore the key drivers. Warming significantly increased total biomass (+8.4 %), aboveground biomass (+12.6 %) and belowground biomass (+10.1 %). The effect of experimental warming on plant biomass was best explained by the availability of soil nitrogen (N) and water. Across the entire dataset, warming-induced changes in total, aboveground and belowground biomass all positively correlated with soil C:N ratio, an indicator of soil N availability. In addition, warming stimulated plant biomass more strongly in humid than in dry ecosystems, and warming tended to decrease root:shoot ratios at high soil C:N ratios. Together, these results suggest dual controls of warming effects on plant C storage; warming increases plant growth in ecosystems where N is limiting plant growth, but it reduces plant growth where water availability is limiting plant growth.
植物可能会通过促进生长减缓全球变暖,因为光合作用水平的提高会刺激陆地碳(C)汇。然而,气候变暖如何影响全球植物 C 储存以及决定植物 C 储存对气候变暖响应的关键驱动因素仍不清楚,这导致了气候预测的不确定性。我们进行了一项全面的荟萃分析,综合了 99 项变暖研究中的 393 个观测结果,以检验植物 C 储存对气候变暖响应的全球模式,并探讨关键驱动因素。变暖显著增加了总生物量(+8.4%)、地上生物量(+12.6%)和地下生物量(+10.1%)。实验变暖对植物生物量的影响最好由土壤氮(N)和水的可用性来解释。在整个数据集内,总生物量、地上生物量和地下生物量的变暖诱导变化均与土壤 C:N 比呈正相关,土壤 C:N 比是土壤 N 可用性的一个指标。此外,在湿润生态系统中,变暖对植物生物量的刺激作用比在干燥生态系统中更强,而且在高土壤 C:N 比下,变暖往往会降低根冠比。综上所述,这些结果表明变暖对植物 C 储存的影响存在双重控制;在 N 限制植物生长的生态系统中,变暖会促进植物生长,但在水分限制植物生长的地方,变暖会减少植物生长。