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首页> 外文期刊>Biology and Fertility of Soils >Are humus forms, mesofauna and microflora in subalpine forest soils sensitive to thermal conditions?
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Are humus forms, mesofauna and microflora in subalpine forest soils sensitive to thermal conditions?

机译:亚高山森林土壤中的腐殖质形式,中动物群和微生物区系对热条件敏感吗?

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This study focuses on the biological and morphological development of humus profiles in forested Italian Alpine soils as a function of climate. Humus form description, systematic investigation of microannelid communities and polyphasic biochemical fingerprinting of soil microbial communities (denaturing gradient gel electrophoresis (DGGE) and phospholipid fatty acid analysis (PLFA)) were performed to compare sites differing in mean annual temperature due to different altitude and exposure. Although the soil biota showed complex responses, several differences in soil biological properties seem to be due to thermal differences. Although soil acidity also determines biological properties, it is not a state factor but rather influenced by them. The thickness of the organic layer and the acidification of the subjacent mineral horizon increased under cooler conditions (north-exposure; higher altitude), whereas the thickness of the A horizon inversely decreased. Species richness of microannelid assemblages was higher under warmer conditions (south-exposure; lower altitude) and the vertical distribution of microannelids shifted along the gradient to lower temperatures from predominant occurrence in the mineral soil to exclusive occurrence in the organic layer. Microbial biomass (total PLFA) was higher at the cooler sites; the prevalence of Gram-negative bacteria could be ascribed to their better adaptation to lower temperature, pH and nutrient contents. The δ13C signatures of the PLFA markers suggested a lower decomposition rate at the cooler sites, resulting in a lower respiratory loss and an accumulation of weakly decomposed organic material. DGGE data supported the PLFA results. Both parameters reflected the expected thermal sequence. This multidisciplinary case study provided indications of an association of climate, mesofauna and microbiota using the humus form as an overall link. More data are however needed and further investigations are encouraged.
机译:这项研究着眼于气候变化对意大利森林高山土壤中腐殖质剖面的生物学和形态发展的影响。进行了腐殖质形式描述,系统化的微生物和微生物群落的多相生化指纹图谱(变性梯度凝胶电泳(DGGE)和磷脂脂肪酸分析(PLFA)),以比较不同海拔和暴露条件下年平均温度不同的部位。尽管土壤生物区系显示出复杂的响应,但土壤生物学特性的一些差异似乎是由于温度差异引起的。尽管土壤酸度也决定了生物学特性,但它不是状态因素,而是受其影响。在较冷的条件下(北向暴露;更高的海拔),有机层的厚度和邻近矿层的酸化作用增加,而A层的厚度则反之减少。在较温暖的条件下(南暴露;较低的海拔),微动物群的物种丰富度较高,并且微动物群的垂直分布沿梯度向较低的温度移动,从矿物土壤中的主要发生变为有机层中的排他性发生。较凉爽的地方微生物量(总PLFA)较高。革兰氏阴性细菌的流行可以归因于它们对较低温度,pH和营养成分的更好适应性。 PLFA标记的δ 13 C特征表明在较凉爽的部位分解速率较低,从而导致呼吸损失降低和弱分解有机物质的积累。 DGGE数据支持PLFA结果。这两个参数均反映了预期的热序。这项多学科的案例研究提供了使用腐殖质形式作为整体联系的气候,中型动物群和微生物群的关联的迹象。但是,需要更多数据,并鼓励进一步研究。

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