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首页> 外文期刊>Soil Biology & Biochemistry >Rainfall frequency, not quantity, controls isopod effect on litter decomposition
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Rainfall frequency, not quantity, controls isopod effect on litter decomposition

机译:降雨频率,而不是数量,控制ISopod对垃圾分解的影响

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Increasing climate variability is one of the dominant components of climate change, resulting particularly in altered rainfall patterns. Yet, the consequences of rainfall variability on biogeochemical processes that contribute to greenhouse gas emissions has received far less attention than have changes in long-term mean rainfall. In particular, it remains unclear how leaf litter decomposition responds to changes in rainfall frequency compared to changes in cumulative rainfall quantity, and if changes in rainfall patterns will differentially affect organisms in the decomposer food web (e.g., microbial decomposers that break down leaf litter through saprotrophic processes versus detritivores that directly ingest leaf litter). To address this knowledge gap, we disentangled the relative importance of cumulative rainfall quantity and rainfall frequency on both microbial and detritivore-driven litter decomposition, using the isopod Arrnadillidium vulgare as a model macro-detritivore species and simulating rainfall in a full-factorial microcosm experiment. We found that microbially-driven decomposition was positively related to cumulative rainfall quantity, but tended to saturate with increasing cumulative rainfall quantity when rainfall events were large and infrequent. This saturation appeared to result from two mechanisms. First, at high level of cumulative rainfall quantity, large and infrequent rainfall events induce lower litter moisture compared to smaller but more frequent ones. Second, microbial activity saturated with increasing litter moisture, suggesting that water was no longer limiting. In contrast, isopod-driven decomposition was unaffected by cumulative rainfall quantity, but was strongly controlled by the rainfall frequency, with higher isopod-driven decomposition at low rainfall frequency. We found that isopod-driven decomposition responded positively to an increase in the weekly range of soil moisture and not to mean soil or litter moisture, suggesting that an alternation of dry and moist conditions enhances detritivore activity. Collectively, our results suggest that A. vulgare morphological and behavioral characteristics may reduce its sensitivity to varying moisture conditions relative to microbial decomposers. We conclude that the activity of microorganisms and isopods are controlled by distinct aspects of rainfall patterns. Consequently, altered rainfall patterns may change the relative contribution of microbial decomposers and detritivores to litter decomposition.
机译:越来越多的气候变化是气候变化的主要成分之一,特别是在改变的降雨模式中。然而,降雨变异对有助于温室气体排放的生物地球化学过程的后果受到远比长期平均降雨的变化更少的关注。特别是,与累积降雨量的变化相比,叶子凋落物分解如何应对降雨频率的变化,以及降雨模式的变化会差异地影响分解食品网中的生物(例如,通过叶片垃圾分解垃圾的微生物分解器具有直接摄取叶子的肌脂营养过程与Detritivores)。为了解决这一知识差距,我们使用ISopod Arrnadillidium Vulgare作为模型宏观碎屑物种和在全因子微观实验中的模拟降雨中的累积降雨量和降雨频率对微生物和Detriverviver的垃圾分解进行累积降雨量和降雨频率的相对重要性。 。我们发现微生物驱动的分解与累积降雨量呈正相关,但是当降雨事件大而不常见时,随着累计降雨量的增加而趋于饱和。这种饱和度似乎是由两个机制产生的。首先,在高水平的累积降雨量,大而不常见的降雨事件与较小但更频繁的降雨液诱导较低的垃圾湿度。其次,微生物活性随着凋落水分的增加而饱和,表明水不再限制。相比之下,异常驱动的分解不受累积降雨量的影响,但受到降雨频率强烈控制的,在低降雨频率下具有更高的ISopod驱动的分解。我们发现Isopod驱动的分解对土壤水分的每周水分范围的增加而不是指土壤或垃圾湿度的响应,表明干燥和潮湿条件的交替增强了Detrivore活性。统称,我们的结果表明A.Vulgare形态和行为特征可以降低其相对于微生物分解的不同水分条件的敏感性。我们得出结论,微生物和等因素的活性由降雨模式的独特方面控制。因此,改变的降雨模式可以改变微生物分解器和DEDRITIVORE与凋落物分解的相对贡献。

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