Department of Ecosystem and Conservation Sciences, University of Montana, Missoula, MT 59812, USA.
Ecol Lett. 2011 Sep;14(9):939-47. doi: 10.1111/j.1461-0248.2011.01658.x. Epub 2011 Jul 12.
Tropical rain forests play a dominant role in global biosphere-atmosphere CO(2) exchange. Although climate and nutrient availability regulate net primary production (NPP) and decomposition in all terrestrial ecosystems, the nature and extent of such controls in tropical forests remain poorly resolved. We conducted a meta-analysis of carbon-nutrient-climate relationships in 113 sites across the tropical forest biome. Our analyses showed that mean annual temperature was the strongest predictor of aboveground NPP (ANPP) across all tropical forests, but this relationship was driven by distinct temperature differences between upland and lowland forests. Within lowland forests (< 1000 m), a regression tree analysis revealed that foliar and soil-based measurements of phosphorus (P) were the only variables that explained a significant proportion of the variation in ANPP, although the relationships were weak. However, foliar P, foliar nitrogen (N), litter decomposition rate (k), soil N and soil respiration were all directly related with total surface (0-10 cm) soil P concentrations. Our analysis provides some evidence that P availability regulates NPP and other ecosystem processes in lowland tropical forests, but more importantly, underscores the need for a series of large-scale nutrient manipulations - especially in lowland forests - to elucidate the most important nutrient interactions and controls.
热带雨林在全球生物圈-大气 CO2 交换中发挥着主导作用。尽管气候和养分供应调节着所有陆地生态系统的净初级生产力 (NPP) 和分解,但这种控制在热带森林中的性质和程度仍未得到很好的解决。我们对热带森林生物群落中的 113 个地点的碳-养分-气候关系进行了荟萃分析。我们的分析表明,年平均温度是所有热带森林中地上 NPP (ANPP) 的最强预测因子,但这种关系是由高地和低地森林之间明显的温度差异驱动的。在低地森林 (<1000 m) 中,回归树分析表明,叶片和土壤磷 (P) 的测量是唯一能够解释 ANPP 变化的重要变量,尽管关系较弱。然而,叶片 P、叶片 N、凋落物分解率 (k)、土壤 N 和土壤呼吸都与总表层 (0-10 cm) 土壤 P 浓度直接相关。我们的分析提供了一些证据,表明 P 供应调节着低地热带森林的 NPP 和其他生态系统过程,但更重要的是,强调需要进行一系列大规模的养分处理 - 特别是在低地森林中 - 以阐明最重要的养分相互作用和控制。