Institute of Soil and Water Conservation, Northwest A & F University, Yangling, Shaanxi, 712100, China.
Institute of Soil and Water Conservation, CAS & MWR, Yangling, Shaanxi, 712100, China.
Microb Ecol. 2023 Jul;86(1):497-508. doi: 10.1007/s00248-022-02077-7. Epub 2022 Jul 22.
Biological soil crusts (biocrusts) are distributed in arid and semiarid regions across the globe. Microorganisms are an essential component in biocrusts. They add and accelerate critical biochemical processes. However, little is known about the functional genes and metabolic processes of microbiomes in lichen and moss biocrust. This study used shotgun metagenomic sequencing to compare the microbiomes of lichen-dominated and moss-dominated biocrust and reveal the microbial genes and metabolic pathways involved in carbon and nitrogen cycling. The results showed that Actinobacteria, Bacteroidetes, and Acidobacteria were more abundant in moss biocrust than lichen biocrust, while Proteobacteria and Cyanobacteria were more abundant in lichen biocrust than moss biocrust. The relative abundance of carbohydrate-active enzymes and enzymes associated with carbon and nitrogen metabolism differed significantly between microbiomes of the two biocrust types. However, in the microbial communities of both biocrust types, respiration pathways dominated over carbon fixation pathways. The genes encoding carbon monoxide dehydrogenase were more abundant than those encoding ribulose 1,5-bisphosphate carboxylase/oxygenase (RuBisCo) involved in carbon fixation. Similarly, metabolic N-pathway diversity was dominated by nitrogen reduction, followed by denitrification, with nitrogen fixation the lowest proportion. Gene diversity involved in N cycling differed between the microbiomes of the two biocrust types. Assimilatory nitrate reduction genes had higher relative abundance in lichen biocrust, whereas dissimilatory nitrate reduction genes had higher relative abundance in moss biocrust. As dissolved organic carbon and soil organic carbon are considered the main drivers of the community structure in the microbiome of biocrust, these results indicate that biocrust type has a pivotal role in microbial diversity and related biogeochemical cycling.
生物土壤结皮(biocrusts)广泛分布于全球干旱和半干旱地区。微生物是生物结皮的重要组成部分,它们促进并加速了关键的生化过程。然而,对于地衣和苔藓生物结皮中微生物组的功能基因和代谢过程,我们知之甚少。本研究采用高通量宏基因组测序,比较了地衣和苔藓生物结皮的微生物组,揭示了参与碳氮循环的微生物基因和代谢途径。结果表明,放线菌、拟杆菌门和酸杆菌门在苔藓生物结皮中的丰度高于地衣生物结皮,而变形菌门和蓝细菌门在地衣生物结皮中的丰度高于苔藓生物结皮。两种生物结皮微生物组的碳水化合物活性酶和与碳氮代谢相关的酶的相对丰度差异显著。然而,在两种生物结皮的微生物群落中,呼吸途径均占主导地位,而碳固定途径则处于劣势。编码一氧化碳脱氢酶的基因丰度高于参与碳固定的核酮糖 1,5-二磷酸羧化酶/加氧酶(RuBisCo)的基因丰度。同样,代谢 N 途径多样性以氮还原为主,随后是反硝化作用,而固氮作用的比例最低。两种生物结皮微生物组的 N 循环相关基因多样性存在差异。同化硝酸盐还原基因在地衣生物结皮中的相对丰度较高,而异化硝酸盐还原基因在苔藓生物结皮中的相对丰度较高。由于溶解有机碳和土壤有机碳被认为是生物结皮微生物组群落结构的主要驱动因素,这些结果表明生物结皮类型在微生物多样性和相关生物地球化学循环中起着关键作用。