Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology (KIT), Garmisch-Partenkirchen, Germany.
Faculty of Natural Sciences and Mathematics, "Interactions Climate-Ecosystems (ICE)" Research Group, Universidad del Rosario, Bogotá, Colombia.
Glob Chang Biol. 2019 May;25(5):1839-1851. doi: 10.1111/gcb.14603. Epub 2019 Mar 19.
Climate warming will affect terrestrial ecosystems in many ways, and warming-induced changes in terrestrial carbon (C) cycling could accelerate or slow future warming. So far, warming experiments have shown a wide range of C flux responses, across and within biome types. However, past meta-analyses of C flux responses have lacked sufficient sample size to discern relative responses for a given biome type. For instance grasslands contribute greatly to global terrestrial C fluxes, and to date grassland warming experiments provide the opportunity to evaluate concurrent responses of both plant and soil C fluxes. Here, we compiled data from 70 sites (in total 622 observations) to evaluate the response of C fluxes to experimental warming across three grassland types (cold, temperate, and semi-arid), warming methods, and short (≤3 years) and longer-term (>3 years) experiment lengths. Overall, our meta-analysis revealed that experimental warming stimulated C fluxes in grassland ecosystems with regard to both plant production (e.g., net primary productivity (NPP) 15.4%; aboveground NPP (ANPP) by 7.6%, belowground NPP (BNPP) by 11.6%) and soil respiration (Rs) (9.5%). However, the magnitude of C flux stimulation varied significantly across cold, temperate and semi-arid grasslands, in that responses for most C fluxes were larger in cold than temperate or semi-arid ecosystems. In semi-arid and temperate grasslands, ecosystem respiration (Reco) was more sensitive to warming than gross primary productivity (GPP), while the opposite was observed for cold grasslands, where warming produced a net increase in whole-ecosystem C storage. However, the stimulatory effect of warming on ANPP and Rs observed in short-term studies (≤3 years) in both cold and temperate grasslands disappeared in longer-term experiments (>3 years). These results highlight the importance of conducting long-term warming experiments, and in examining responses across a wide range of climate.
气候变暖将在许多方面影响陆地生态系统,而陆地碳(C)循环的变暖诱导变化可能会加速或减缓未来的变暖。到目前为止,变暖实验已经表明 C 通量响应范围很广,跨越和在生物群落类型内。然而,过去对 C 通量响应的荟萃分析缺乏足够的样本量来辨别给定生物群落类型的相对响应。例如,草原对全球陆地 C 通量有很大贡献,迄今为止,草原变暖实验提供了评估植物和土壤 C 通量同时响应的机会。在这里,我们汇总了 70 个地点的数据(共 622 个观测值),以评估三种草原类型(寒冷、温带和半干旱)、变暖方法以及短期(≤3 年)和长期(>3 年)实验长度下 C 通量对实验变暖的响应。总体而言,我们的荟萃分析表明,实验变暖刺激了草原生态系统的 C 通量,无论是植物生产力(例如,净初级生产力(NPP)增加 15.4%;地上 NPP(ANPP)增加 7.6%,地下 NPP(BNPP)增加 11.6%)还是土壤呼吸(Rs)(增加 9.5%)。然而,C 通量刺激的幅度在寒冷、温带和半干旱草原之间差异显著,大多数 C 通量的响应在寒冷草原中大于温带或半干旱生态系统。在半干旱和温带草原中,生态系统呼吸(Reco)对变暖比总初级生产力(GPP)更敏感,而在寒冷草原中则相反,变暖导致整个生态系统 C 储存的净增加。然而,在寒冷和温带草原的短期研究(≤3 年)中,变暖对 ANPP 和 Rs 的刺激作用在长期实验(>3 年)中消失了。这些结果强调了进行长期变暖实验以及在广泛的气候范围内检查响应的重要性。