Explicit microrelief-controlled decoupling of initial aerobic decay and leaching (in hummocks) and anaerobic decay (in hollows) in surface layers of a Sphagnum-dominated peatland

IF 6.2 2区 化学 Q1 CHEMISTRY, ANALYTICAL
M. Pérez-Rodríguez , A. Alten , M. Miler , J. Kaal
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引用次数: 0

Abstract

Understanding decay processes in peat deposits is fundamental for predicting their role as sources or sinks of atmospheric carbon in a changing environment. It is known that the distribution of microhabitats –hummock, lawn and hollow– within peatlands affects organic matter quality and degradation, but microtopography-dependent carbon dynamics are poorly understood on the molecular level. We studied early decomposition across microtopography levels through analyses of superficial moss cores from a Sphagnum-dominated ombrotrophic peatland in Central Germany, and a 400-day incubation experiment, using analytical pyrolysis. Interpretations were aided by analysis of living vegetation and a deep peat core as reference. Stable and labile pools of polysaccharides dominated the pyrolyzates and played a crucial role in decay dynamics. Two distinct degradation processes emerged: 1) anaerobic decay, characterized by loss of polysaccharides and selective preservation of lignin and aliphatic OM; and 2) leaching of labile phenolic compounds (including sphagnum acid) and free carbohydrates with concomitant initial aerobic degradation and selective preservation of structural polysaccharides. The relative importance of these initial decay processes is spatially dependent; anaerobic decay was detectable in only some of the more evolved hollow layers, while aerobic degradation and leaching dominated in hummocks. Sphagnum acid’s molecular markers appeared useful tracers of early decay as it probably has a leaching-sensitive component in hyaline cells (corroborated by SEM micrographs) that is lost rapidly from hummocks, but not from hollows. Hence, the occurrence of sphagnum acid in peat cores is influenced by microrelief position during peat accretion. This study highlights how microhabitat variations within peatlands influence decay mechanisms on the molecular level.
以泥炭为主的泥炭地表层初始好氧衰变和淋滤(在小丘中)和厌氧衰变(在洼地中)的明显微地形控制解耦
了解泥炭沉积物的衰变过程是预测其在不断变化的环境中作为大气碳源或汇的作用的基础。众所周知,泥炭地内微生境(丘状、草坪和空心)的分布影响有机质质量和降解,但在分子水平上对微地形依赖的碳动力学知之甚少。我们通过分析德国中部以sphagnumm为主的全养泥炭地的浅表苔藓岩芯,以及400天的孵化实验,研究了微地形水平上的早期分解。通过分析活的植被和一个深泥炭岩心作为参考,帮助解释。稳定和不稳定的多糖池主导着热解产物,在衰变动力学中起着至关重要的作用。出现了两种不同的降解过程:1)厌氧衰变,其特征是多糖的损失和木质素和脂肪族OM的选择性保存;2)溶出不稳定的酚类化合物(包括磷酸)和游离碳水化合物,同时进行初始好氧降解和结构多糖的选择性保存。这些初始衰变过程的相对重要性是空间依赖性的;厌氧腐烂只在一些较进化的空心层中被检测到,而好氧降解和浸出在小丘中占主导地位。sphaspum酸的分子标记似乎是早期腐烂的有用示踪剂,因为它可能在透明细胞中具有浸出敏感成分(通过扫描电镜显微照片证实),这种成分在丘状物中迅速丢失,而在空心中则不会。因此泥炭岩心中泥炭酸的赋存受泥炭吸积过程中微起伏位置的影响。本研究强调了泥炭地微生境变化如何影响分子水平上的衰变机制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
9.10
自引率
11.70%
发文量
340
审稿时长
44 days
期刊介绍: The Journal of Analytical and Applied Pyrolysis (JAAP) is devoted to the publication of papers dealing with innovative applications of pyrolysis processes, the characterization of products related to pyrolysis reactions, and investigations of reaction mechanism. To be considered by JAAP, a manuscript should present significant progress in these topics. The novelty must be satisfactorily argued in the cover letter. A manuscript with a cover letter to the editor not addressing the novelty is likely to be rejected without review.
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