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Soil fauna, microbes and plant litter decomposition in tropical and subalpine forests.

机译:热带和亚高山森林中土壤动物,微生物和植物凋落物的分解。

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Studies of latitudinal gradients of decomposition have focused on substrate quality and climate effects on decomposition and have excluded explicit recognition of the soil organisms involved in the process. This work addresses the effects of soil organisms on litter decomposition along a wide climatic gradient: in dry and wet tropical forests and north- and south-facing subalpine forests.; I quantified decomposition rates and N fluxes in control and fauna-excluded treatments to test whether soil fauna exhibit different effects under diverse climate and/or substrates. Litterbags contained two different plant species varying in lignin content. All three factors (climate, substrate quality, and soil fauna) independently influenced the decomposition rate of plant litter in the tropical and subalpine forests. The faunal effects on decay rates and N mineralization of both litter species were higher in the tropical wet forest than the tropical dry and subalpine forests, and no significant interaction of fauna and litter species on the annual decay rates was found. There was a higher density of soil fauna per gram of litter in the tropical wet forest as compared to all sites.; Little consensus has been reached on the extent to which soil fauna can regulate microbial activities. This uncertainty is due to the complexity of the functional roles of fauna and their effects on microbes. To test whether soil fauna exhibit different effects on microbes under diverse climatic conditions, I quantified soil microbial biomass and maximum growth rates in control and defaunated treatments across the study sites. It was found that exclusion of soil fauna resulted in a higher total microbial biomass and lower maximum growth rate in the subalpine forests. No effect of fauna exclusion on microbes was found in the tropics.; This study indicates differential mechanisms by which soil fauna affect soil ecosystem processes in tropical and temperate systems. In the subalpine forest, soil fauna play a more significant role in ecosystem processes through selective interactions with the microbial community. In the wet tropics, soil fauna have a direct effect on ecosystem processes through comminution of organic matter and the modification of the soil environment.
机译:分解的纬度梯度研究集中在基质质量和气候对分解的影响上,并且没有明确认识到参与该过程的土壤生物。这项工作解决了土壤有机物在广泛的气候梯度上对凋落物分解的影响:在干燥和湿润的热带森林以及朝北和朝南的亚高山森林中。我量化了控制和动物隔离处理中的分解速率和N通量,以测试土壤动物在不同的气候和/或基质下是否表现出不同的影响。垃圾袋包含两种不同的木质素含量不同的植物。这三个因素(气候,基质质量​​和土壤动物群)均独立影响热带和亚高山森林植物凋落物的分解速率。在热带湿林中,这两种凋落物对凋落率和氮矿化的动物学影响均高于热带干燥和亚高山森林,并且没有发现动物和凋落物对年衰减率的显着影响。与所有地点相比,热带湿润森林中每克垃圾的土壤动物密度更高。关于土壤动物可以调节微生物活动的程度,尚未达成共识。这种不确定性是由于动物的功能角色的复杂性及其对微生物的影响。为了测试在不同的气候条件下土壤动物对微生物的影响是否不同,我在整个研究地点进行了对照和弱化处理后,对土壤微生物量和最大生长速率进行了量化。研究发现,土壤动物的排斥导致亚高山森林中总微生物量的增加和最大生长率的降低。在热带地区,没有发现动物被排斥对微生物的影响。这项研究表明了土壤动物影响热带和温带系统中土壤生态系统过程的不同机制。在亚高山森林中,土壤动物通过与微生物群落的选择性相互作用在生态系统过程中发挥着更重要的作用。在湿热带地区,土壤动物通过粉碎有机物和改变土壤环境对生态系统过程产生直接影响。

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