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首页> 外文期刊>Global change biology >Experimental litterfall manipulation drives large and rapid changes in soil carbon cycling in a wet tropical forest.
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Experimental litterfall manipulation drives large and rapid changes in soil carbon cycling in a wet tropical forest.

机译:实验性的凋落物处理驱动着湿热带森林中土壤碳循环的快速变化。

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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 CO2 fluxes; the relative decline in CO2 production was greater in the litter removal plots (-22%) than the increase in the litter addition plots (+15%). Our analysis showed that variations in CO2 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.CAS Registry Numbers 7440-44-0 124-38-9 7723-14-0 7727-37-9
机译:全球变化,例如植物净初级生产力的变化,可能会促使落叶凋落物输入森林土壤,但这种变化对土壤碳(C)循环和存储的影响仍然未知,尤其是在富含碳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落叶凋落物处理实验,以测试地表土壤碳库和通量对不同凋落物输入的敏感性。经过仅2年的处理,凋落物投入增加一倍,使表层土壤C浓度增加了31%,从森林地带清除凋落物在同一时期内减少了26%,这些土壤C浓度的变化与溶解有机物的变化有关物质通量,细根生物量,微生物生物量,土壤水分和养分通量。然而,凋落物的处理对土壤有机碳(SOC)的化学影响很小,这表明随着凋落物的处理,碳循环,养分循环和微生物过程的变化反映了SOC的数量而不是质量的变化。操作还影响了土壤CO 2 通量。去除垫料地的CO 2 产量的相对下降(-22%)大于添加垫料地的增加(+ 15%)。我们的分析表明,CO 2 通量的变化与微生物生物量库,土壤碳和氮(N)库,土壤无机P通量,溶解的有机C通量以及细根生物量密切相关。总之,我们的数据表明,应对局部人为干扰和全球环境变化而造成的凋落物输入的变化可能会对地下C的储量和热带雨林的通量产生快速而重要的影响,并强调热带和温带生态系统之间的差异,其中地下C自行车对凋落物变化的反应通常较慢且较细微.CAS注册号7440-44-0 124-38-9 7723-14-0 7727-37-9

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