法国萨瓦一株高山白垩石楠的腐殖质剖面:高分辨率显微形态分析

Nicolas Bernier
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摘要

在腐殖质形态的各种分类中,用来区分摩尔和摩尔的特征是不同的。Mor通常与生长在高海拔或纬度,或生长在土壤营养贫乏、多沙和酸性的低地的白垩石楠有关。本研究采用一种新的显微形态学方法,对法国阿尔卑斯山(萨瓦,海拔1950米)的高寒石楠地的三个腐殖质剖面进行了研究,以更好地了解其潜在的过程。用解剖仪器逐渐切割的腐殖质单体水平切片的显微观察,使我们能够表征腐殖质成分的比例,每个成分的微观形态以及腐殖质的微观结构组织。分析结果表明,千足虫对高寒蕨类植被腐殖质剖面的生物活性具有重要意义。这些动物不分青红皂白地吃凋落物(白垩系、苔藓和草本植物的残骸),因此没有时间积累。当气候条件迫使这些动物生活在深海时,它们有时也以腐殖化的有机物为食。因此,腐殖质经历了宏观结构(聚集体和画廊)。当有机质积累水平高时,这种活动保持在整体有机环境的框架内,但当这个水平低时,千足虫消耗大量矿物质并产生矿物-有机混合物。这项工作说明了这些生态系统的独特特征,并强调了通过解决各种标准对腐殖质形式进行全面描述的重要性,这有助于对过渡腐殖质形式进行分类。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The humus profile of an alpine ericaceous heath (Savoie, France): A high-resolution micromorphological analysis

The humus profile of an alpine ericaceous heath (Savoie, France): A high-resolution micromorphological analysis

The characteristics used to distinguish between Mor and Moder differ among the various classifications of humus forms. Mor is often associated with ericaceous heathland that develops at high altitude or latitude, or in lowlands when soils are nutrient-poor, sandy, and acidic. This study applies a new micromorphological method on three humus profiles from an alpine heathland in the French Alps (Savoie, altitude 1950 m) to better understand the underlying processes. Microscopic observations of horizontal sections of humus monoliths, gradually cut with dissecting instruments, allow us to characterize the proportions of humus components, the micromorphology of each component, and the microstructural organization of the humus. The analysis shows the importance of millipedes for the biological activity of the humus profile in the alpine ericaceous heath. These animals feed indiscriminately on litter (remains of ericaceous, moss, and herb vegetation), which therefore does not have time to accumulate. They also sometimes feed on humified organic matter when climatic conditions force these animals to live at depth. As a result, humus undergoes macrostructuration (aggregates and galleries). When the level of organic matter accumulation is high, this activity remains within the framework of a holorganic context, but when this level is low, millipedes consume a significant proportion of minerals and create a mineral–organic mixture. This work illustrates the distinctive characteristics of these ecosystems and emphasizes the importance of a thorough description of the humus forms by addressing various criteria, which facilitates the classification of transition humus forms.

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