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微生物群落调控英国盐沼木质纤维素分解的机制策略。

Mechanistic strategies of microbial communities regulating lignocellulose deconstruction in a UK salt marsh.

机构信息

Centre for Novel Agricultural Products, Department of Biology, University of York, York, YO10 5DD, UK.

Bioscience Technology Facility, Department of Biology, University of York, York, YO10 5DD, UK.

出版信息

Microbiome. 2021 Feb 17;9(1):48. doi: 10.1186/s40168-020-00964-0.

Abstract

BACKGROUND

Salt marshes are major natural repositories of sequestered organic carbon with high burial rates of organic matter, produced by highly productive native flora. Accumulated carbon predominantly exists as lignocellulose which is metabolised by communities of functionally diverse microbes. However, the organisms that orchestrate this process and the enzymatic mechanisms employed that regulate the accumulation, composition and permanence of this carbon stock are not yet known. We applied meta-exo-proteome proteomics and 16S rRNA gene profiling to study lignocellulose decomposition in situ within the surface level sediments of a natural established UK salt marsh.

RESULTS

Our studies revealed a community dominated by Gammaproteobacteria, Bacteroidetes and Deltaproteobacteria that drive lignocellulose degradation in the salt marsh. We identify 42 families of lignocellulolytic bacteria of which the most active secretors of carbohydrate-active enzymes were observed to be Prolixibacteracea, Flavobacteriaceae, Cellvibrionaceae, Saccharospirillaceae, Alteromonadaceae, Vibrionaceae and Cytophagaceae. These families secreted lignocellulose-active glycoside hydrolase (GH) family enzymes GH3, GH5, GH6, GH9, GH10, GH11, GH13 and GH43 that were associated with degrading Spartina biomass. While fungi were present, we did not detect a lignocellulolytic contribution from fungi which are major contributors to terrestrial lignocellulose deconstruction. Oxidative enzymes such as laccases, peroxidases and lytic polysaccharide monooxygenases that are important for lignocellulose degradation in the terrestrial environment were present but not abundant, while a notable abundance of putative esterases (such as carbohydrate esterase family 1) associated with decoupling lignin from polysaccharides in lignocellulose was observed.

CONCLUSIONS

Here, we identify a diverse cohort of previously undefined bacteria that drive lignocellulose degradation in the surface sediments of the salt marsh environment and describe the enzymatic mechanisms they employ to facilitate this process. Our results increase the understanding of the microbial and molecular mechanisms that underpin carbon sequestration from lignocellulose within salt marsh surface sediments in situ and provide insights into the potential enzymatic mechanisms regulating the enrichment of polyphenolics in salt marsh sediments. Video Abstract.

摘要

背景

盐沼是封存有机碳的主要天然储存库,具有高有机质埋藏率,由高生产力的本地植物产生。积累的碳主要以木质纤维素的形式存在,由功能多样的微生物群落代谢。然而,协调这一过程的生物和用于调节这种碳储量的积累、组成和持久性的酶机制尚不清楚。我们应用元外蛋白质组学和 16S rRNA 基因谱分析来研究英国天然建立的盐沼表面沉积物中木质纤维素的原位分解。

结果

我们的研究表明,一种以γ变形菌门、拟杆菌门和δ变形菌门为主的群落驱动盐沼中的木质纤维素降解。我们确定了 42 个木质纤维素分解细菌家族,其中最活跃的碳水化合物活性酶分泌菌是 Prolixibacteracea、Flavobacteriaceae、Cellvibrionaceae、Saccharospirillaceae、Alteromonadaceae、Vibrionaceae 和 Cytophagaceae。这些家族分泌木质纤维素活性糖苷水解酶(GH)家族酶 GH3、GH5、GH6、GH9、GH10、GH11、GH13 和 GH43,这些酶与降解 Spartina 生物量有关。虽然真菌存在,但我们没有检测到真菌对木质纤维素分解的贡献,真菌是陆地木质纤维素分解的主要贡献者。氧化酶,如漆酶、过氧化物酶和溶菌多糖单加氧酶,对陆地环境中木质纤维素的降解很重要,但并不丰富,而大量与木质纤维素中木质素与多糖解耦相关的假定酯酶(如碳水化合物酯酶家族 1)被观察到。

结论

在这里,我们确定了一组以前未定义的细菌,它们在盐沼环境的表面沉积物中驱动木质纤维素的降解,并描述了它们用来促进这一过程的酶机制。我们的研究结果增加了对盐沼表面沉积物中木质纤维素碳封存的微生物和分子机制的理解,并为调节盐沼沉积物中多酚富集的潜在酶机制提供了见解。视频摘要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0498/7890819/39412f4dc264/40168_2020_964_Fig1_HTML.jpg

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