Sultan Qaboos University, College of Science, Biology Department, P.O. Box: 36, postal code 123, Al Khoud, Sultanate of Oman.
Multiphase Chemistry Department, Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, D-55128, Mainz, Germany.
Sci Rep. 2019 Apr 23;9(1):6468. doi: 10.1038/s41598-019-42911-6.
Biological soil crusts (biocrusts) occur within drylands throughout the world, covering ~12% of the global terrestrial soil surface. Their occurrence in the deserts of the Arabian Peninsula has rarely been reported and their spatial distribution, diversity, and microbial composition remained largely unexplored. We investigated biocrusts at six different locations in the coastal and central deserts of Oman. The biocrust types were characterized, and the bacterial and fungal community compositions of biocrusts and uncrusted soils were analysed by amplicon sequencing. The results were interpreted based on the environmental parameters of the different sites. Whereas at lowland sites, mainly cyanobacteria-dominated biocrusts were observed, both cyanobacteria- and lichen-dominated biocrusts occurred at mountain sites. The majority of bacterial sequences (32-83% of total sequences) belonged to Actinobacteria, Cyanobacteria, Alphaproteobacteria, and Bacteroidetes, whereas fungal sequences belonged to Ascomycota, Basidiomycota, and Chytridiomycota (>95%). With biocrust development, a notable increase in cyanobacterial and decrease in actinobacterial proportions was observed for cyanobacteria-dominated crusts. In coastal areas, where salinity is high, biocrusts were replaced by a unique marine mat-like microbial community, dominated by halotolerant taxa. Redundancy analysis revealed a significant contribution of soil texture, cover type, carbon content, and elevation to the variations in bacterial and fungal communities. Multivariate analysis placed microbial communities in significantly separated clusters based on their carbon content, elevation and electrical conductivity. We conclude that Oman hosts a variety of cyanobacteria- and lichen-dominated crusts with their bacterial and fungal communities being largely dictated by soil properties and environmental parameters.
生物土壤结皮(biocrusts)广泛存在于世界各地的干旱地区,覆盖了全球陆地土壤表面的约 12%。它们在阿拉伯半岛沙漠中的出现很少被报道,其空间分布、多样性和微生物组成在很大程度上仍未得到探索。我们在阿曼的沿海和内陆沙漠的六个不同地点调查了生物结皮。我们对生物结皮类型进行了特征描述,并通过扩增子测序分析了生物结皮和未结皮土壤的细菌和真菌群落组成。我们根据不同地点的环境参数对结果进行了解释。在低地,主要观察到以蓝藻为主的生物结皮,而在山区则同时存在蓝藻和地衣为主的生物结皮。大多数细菌序列(总序列的 32-83%)属于放线菌门、蓝藻门、α变形菌门和拟杆菌门,而真菌序列则属于子囊菌门、担子菌门和壶菌门(>95%)。随着生物结皮的发展,以蓝藻为主的结皮中蓝藻的比例显著增加,而放线菌的比例显著减少。在盐分较高的沿海地区,生物结皮被一种独特的海洋垫状微生物群落所取代,该群落主要由耐盐类群组成。冗余分析显示,土壤质地、覆盖类型、碳含量和海拔高度对细菌和真菌群落的变化有显著贡献。多元分析根据微生物群落的碳含量、海拔和电导率将其分为明显分离的聚类。我们得出结论,阿曼拥有多种以蓝藻和地衣为主的结皮,其细菌和真菌群落主要由土壤性质和环境参数决定。