青藏高原牦牛粪降解动态及微生物过程

IF 9.8 1区 农林科学 Q1 SOIL SCIENCE
Zhiyang Zhang, Yi Jiao, Steffen Kolb
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引用次数: 0

摘要

牦牛粪是维持青藏高原生态系统功能的碳(C)和养分循环的输入。牦牛粪是富含碳和营养的排泄物,有利于细菌群落的生长和代谢活动,因此预测细菌过程比真菌过程更多地负责牦牛粪的降解。在放牧牦牛的高寒草地上进行了为期3年的牦牛粪降解实验,研究了牦牛粪在降解过程中水分含量、酶化学性质、细菌和真菌群落的变化,并探讨了这些参数对牦牛粪降解的调控作用。牦牛粪经过3年的分解,质量下降了79%,其中大部分质量损失发生在前2年。纤维素聚合物,特别是纤维素和半纤维素,决定了牦牛粪的降解率。粪便细菌群落的主要变化发生在降解的前2年,主要与水分和有效底物(如溶解有机碳、溶解有机氮(N)、铵、硝酸盐和有效磷)的变化有关。相反,粪便真菌群落直到降解1.5-3年后才发生变化,这与总底物(如总C和总N)有关。变形菌门、拟杆菌门、厚壁菌门、担子菌门和子囊菌门的相对丰度以及与纤维素和半纤维素降解相关的内纤维素酶、外纤维素酶、β-1,4-葡萄糖苷酶和β-1,4-木糖苷酶的活性在分解过程中下降。放线菌相对丰度、过氧化物酶和多酚氧化酶活性与粪木质素含量呈正相关。结构方程模型表明,粪便中木质纤维素的降解主要是细菌群落活动的结果。此外,水分是影响木质纤维素降解的最重要的非生物因素,因为它可以直接影响粪便基质的有效性,最终影响细菌群落和相关酶的活性。由于牦牛粪便中木质纤维素的微生物降解与湿度密切相关,因此未来降雨模式的任何变化都将影响该高寒地区牦牛粪便的降解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Degradation dynamics and microbial processes in yak dung on the Tibetan Plateau

Degradation dynamics and microbial processes in yak dung on the Tibetan Plateau
Yak dung is an input to the carbon (C) and nutrient cycles that maintain ecosystem functions on the Tibetan Plateau. Yak dung is C and nutrient-rich excreta that is conducive to the growth and metabolic activities of bacterial communities, thus predicting that more bacterial than fungal processes are responsible for the degradation of yak dung. A three-year yak dung degradation experiment in a yak-grazing alpine rangeland was designed to investigate the changes in dung moisture content, chemical and enzymatic properties, and bacterial and fungal communities during degradation, as well as to explore how these parameters may regulate the degradation of yak dung. After three years of decomposition, yak dung had a 79 % reduction in mass, and most of the mass loss occurred within the first 2 years. Cellulosic polymers, especially cellulose and hemicellulose, determined the rate of yak dung degradation. The main changes in dung bacterial communities occurred during the first 2 years of degradation, largely related to changes in moisture and available substrates (e.g., dissolved organic C, dissolved organic nitrogen (N), ammonium, nitrate, and available phosphorus). In contrast, dung fungal communities did not change until 1.5–3 years of degradation, in response to the total substrates (e.g., total C and N). The relative abundances of Proteobacteria, Bacteroidota, Firmicutes, Basidiomycota, and Ascomycota, and the activities of endo-cellulases, exo-cellulases, β-1,4-glucosidase, and β-1,4-xylosidase, which were associated with cellulose and hemicellulose degradation, decreased during decomposition. The relative abundances of Actinobacteria, and activities of peroxidases and polyphenol oxidase were positively correlated with dung lignin content. Structural equation modeling suggested that degradation of lignocellulose in dung was mainly the consequence of bacterial community activities. Additionally, moisture was the most important abiotic factor influencing lignocellulose degradation, as it can directly affect dung substrate availability, and ultimately bacterial communities and associated enzyme activities. As the microbial degradation of lignocellulose in yak dung is strongly related to moisture, any change to the rainfall pattern in the future is expected to influence yak dung degradation in this alpine region.
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来源期刊
Soil Biology & Biochemistry
Soil Biology & Biochemistry 农林科学-土壤科学
CiteScore
16.90
自引率
9.30%
发文量
312
审稿时长
49 days
期刊介绍: Soil Biology & Biochemistry publishes original research articles of international significance focusing on biological processes in soil and their applications to soil and environmental quality. Major topics include the ecology and biochemical processes of soil organisms, their effects on the environment, and interactions with plants. The journal also welcomes state-of-the-art reviews and discussions on contemporary research in soil biology and biochemistry.
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