Raich James W, Russell Ann E, Kitayama Kanehiro, Parton William J, Vitousek Peter M
Department of Ecology, Evolution and Organismal Biology, Iowa State University, Ames 50011, USA.
Ecology. 2006 Jan;87(1):76-87. doi: 10.1890/05-0023.
Evergreen broad-leaved tropical forests can have high rates of productivity and large accumulations of carbon in plant biomass and soils. They can therefore play an important role in the global carbon cycle, influencing atmospheric CO2 concentrations if climate warms. We applied meta-analyses to published data to evaluate the apparent effects of temperature on carbon fluxes and storages in mature, moist tropical evergreen forest ecosystems. Among forests, litter production, tree growth, and belowground carbon allocation all increased significantly with site mean annual temperature (MAT); total net primary productivity (NPP) increased by an estimated 0.2-0.7 Mg C x ha(-1) x yr(-1) x degrees C(-1). Temperature had no discernible effect on the turnover rate of aboveground forest biomass, which averaged 0.014 yr(-1) among sites. Consistent with these findings, forest biomass increased with site MAT at a rate of 5-13 Mg C x ha(-1) x degrees C(-1). Despite greater productivity in warmer forests, soil organic matter accumulations decreased with site MAT, with a slope of -8 Mg C x ha(-1) x degrees C(-1), indicating that decomposition rates of soil organic matter increased with MAT faster than did rates of NPP. Turnover rates of surface litter also increased with temperature among forests. We found no detectable effect of temperature on total carbon storage among moist-tropical evergreen forests, but rather a shift in ecosystem structure, from low-biomass forests with relatively large accumulations of detritus in cooler sites, to large-biomass forests with relatively smaller detrital stocks in warmer locations. These results imply that, in a warmer climate, conservation of forest biomass will be critical to the maintenance of carbon stocks in moist tropical forests.
热带常绿阔叶林具有较高的生产力,植物生物量和土壤中积累了大量碳。因此,它们在全球碳循环中可发挥重要作用,若气候变暖,会影响大气中的二氧化碳浓度。我们对已发表的数据进行荟萃分析,以评估温度对成熟湿润热带常绿森林生态系统中碳通量和碳储存的明显影响。在森林中,凋落物产量、树木生长和地下碳分配均随站点年均温度(MAT)显著增加;总净初级生产力(NPP)估计每升高1℃增加0.2 - 0.7 Mg C·ha⁻¹·yr⁻¹。温度对地上森林生物量的周转率没有明显影响,各站点的平均周转率为0.014 yr⁻¹。与这些发现一致,森林生物量随站点MAT以5 - 13 Mg C·ha⁻¹·℃⁻¹的速率增加。尽管温暖森林的生产力更高,但土壤有机质积累量随站点MAT下降,斜率为 - 8 Mg C·ha⁻¹·℃⁻¹,这表明土壤有机质的分解速率随MAT的增加速度比NPP的增加速度更快。森林中地表凋落物的周转率也随温度升高。我们发现温度对湿润热带常绿森林的总碳储存没有可检测到的影响,而是生态系统结构发生了变化,从较冷地区碎屑积累相对较多的低生物量森林,转变为较温暖地区碎屑存量相对较小的高生物量森林。这些结果意味着,在气候变暖的情况下,保护森林生物量对于维持湿润热带森林的碳储量至关重要。