Research Unit Comparative Microbiome Analysis, Helmholtz Zentrum München Research Center for Environmental Health (GmbH), Ingolstädter Landstraße 1, 85764, Neuherberg, Germany.
Section for Bioinformatics, Department of Health Technology, Technical University of Denmark, 2800, Lyngby, Denmark.
Microb Ecol. 2020 Feb;79(2):326-341. doi: 10.1007/s00248-019-01415-6. Epub 2019 Aug 1.
Biological soil crusts (biocrusts) play an important role in improving soil stability and resistance to erosion by promoting aggregation of soil particles. During initial development, biocrusts are dominated by bacteria. Some bacterial members of the biocrusts can contribute to the formation of soil aggregates by producing exopolysaccharides and lipopolysaccharides that act as "glue" for soil particles. However, little is known about the dynamics of "soil glue" producers during the initial development of biocrusts. We hypothesized that different types of initial biocrusts harbor distinct producers of adhesive polysaccharides. To investigate this, we performed a microcosm experiment, cultivating biocrusts on two soil substrates. High-throughput shotgun sequencing was used to obtain metagenomic information on microbiomes of bulk soils from the beginning of the experiment, and biocrusts sampled after 4 and 10 months of incubation. We discovered that the relative abundance of genes involved in the biosynthesis of exopolysaccharides and lipopolysaccharides increased in biocrusts compared with bulk soils. At the same time, communities of potential "soil glue" producers that were highly similar in bulk soils underwent differentiation once biocrusts started to develop. In the bulk soils, the investigated genes were harbored mainly by Betaproteobacteria, whereas in the biocrusts, the major potential producers of adhesive polysaccharides were, aside from Alphaproteobacteria, either Cyanobacteria or Chloroflexi and Acidobacteria. Overall, our results indicate that the potential to form exopolysaccharides and lipopolysaccharides is an important bacterial trait for initial biocrusts and is maintained despite the shifts in bacterial community composition during biocrust development.
生物土壤结皮(biocrusts)在促进土壤颗粒团聚方面对提高土壤稳定性和抗侵蚀能力起着重要作用。在初始发育阶段,生物结皮主要由细菌组成。生物结皮中的一些细菌成员可以通过产生作为土壤颗粒“胶”的胞外多糖和脂多糖来促进土壤团聚体的形成。然而,对于生物结皮初始发育过程中“土壤胶”产生菌的动态变化,人们知之甚少。我们假设不同类型的初始生物结皮拥有不同的粘性多糖产生菌。为了研究这一点,我们进行了一个微宇宙实验,在两种土壤基质上培养生物结皮。高通量 shotgun 测序用于获得实验开始时大块土壤微生物组的宏基因组信息,以及培养 4 个月和 10 个月后采集的生物结皮样本。我们发现,与大块土壤相比,生物结皮中参与胞外多糖和脂多糖生物合成的基因相对丰度增加。与此同时,在生物结皮开始发育时,大块土壤中高度相似的潜在“土壤胶”产生菌群落发生了分化。在大块土壤中,研究的基因主要由 Betaproteobacteria 携带,而在生物结皮中,除了 Alphaproteobacteria 外,粘性多糖的主要潜在产生菌是蓝细菌或绿弯菌门和酸杆菌门。总的来说,我们的研究结果表明,形成胞外多糖和脂多糖的潜力是生物结皮初始发育的一个重要细菌特征,尽管在生物结皮发育过程中细菌群落组成发生了变化,但这种特征仍然得以维持。