Department of Ecosystem and Conservation Sciences, University of Montana, CHCB423, Missoula, MT, 59812, USA.
Glob Chang Biol. 2012 Sep;18(9):2969-79. doi: 10.1111/j.1365-2486.2012.02749.x. Epub 2012 Jun 25.
Global changes such as variations in plant net primary production are likely to drive shifts in leaf litterfall inputs to forest soils, but the effects of such changes on soil carbon (C) cycling and storage remain largely unknown, especially in C-rich tropical forest ecosystems. We initiated a leaf litterfall manipulation experiment in a tropical rain forest in Costa Rica to test the sensitivity of surface soil C pools and fluxes to different litter inputs. After only 2 years of treatment, doubling litterfall inputs increased surface soil C concentrations by 31%, removing litter from the forest floor drove a 26% reduction over the same time period, and these changes in soil C concentrations were associated with variations in dissolved organic matter fluxes, fine root biomass, microbial biomass, soil moisture, and nutrient fluxes. However, the litter manipulations had only small effects on soil organic C (SOC) chemistry, suggesting that changes in C cycling, nutrient cycling, and microbial processes in response to litter manipulation reflect shifts in the quantity rather than quality of SOC. The manipulation also affected soil CO 2 fluxes; the relative decline in CO 2 production was greater in the litter removal plots (-22%) than the increase in the litter addition plots (+15%). Our analysis showed that variations in CO 2 fluxes were strongly correlated with microbial biomass pools, soil C and nitrogen (N) pools, soil inorganic P fluxes, dissolved organic C fluxes, and fine root biomass. Together, our data suggest that shifts in leaf litter inputs in response to localized human disturbances and global environmental change could have rapid and important consequences for belowground C storage and fluxes in tropical rain forests, and highlight differences between tropical and temperate ecosystems, where belowground C cycling responses to changes in litterfall are generally slower and more subtle.
全球变化,如植物净初级生产力的变化,可能会导致森林土壤中凋落物输入的变化,但这种变化对土壤碳(C)循环和储存的影响在很大程度上仍然未知,尤其是在富含 C 的热带森林生态系统中。我们在哥斯达黎加的热带雨林中启动了一项凋落物凋落物处理实验,以测试不同凋落物输入对表层土壤 C 库和通量的敏感性。在仅 2 年的处理后,凋落物输入量增加一倍使表层土壤 C 浓度增加了 31%,同期从林地上移除凋落物使 C 浓度降低了 26%,而这些土壤 C 浓度的变化与溶解有机物质通量、细根生物量、微生物生物量、土壤水分和养分通量的变化有关。然而,凋落物处理对土壤有机 C(SOC)化学性质的影响很小,这表明凋落物处理对 C 循环、养分循环和微生物过程的影响反映了 SOC 数量的变化,而不是质量的变化。该处理还影响土壤 CO 2 通量;在凋落物移除区,CO 2 产生的相对下降(-22%)大于凋落物添加区的增加(+15%)。我们的分析表明,CO 2 通量的变化与微生物生物量池、土壤 C 和氮(N)库、土壤无机 P 通量、溶解有机 C 通量和细根生物量密切相关。总之,我们的数据表明,响应局部人类干扰和全球环境变化而导致的凋落物输入的变化可能会对热带雨林的地下 C 储存和通量产生快速而重要的影响,并突出了热带和温带生态系统之间的差异,在这些生态系统中,凋落物变化对地下 C 循环的响应通常较慢且更微妙。