Abstract
Halophilic microorganisms abound in numerous hypersaline environments, such as salt lakes, salt mines, solar salterns, and salted seafood. In the northwest of Dingbian county (Shaanxi province, China), there exists a belt of hypersaline habitats extending from the west to the north consisting of saline-alkali soil and salt lakes. Theoretically, such a hypersaline environment has a high probability of containing abundant halophilic archaea communities. Nevertheless, there is nearly no systematic research on halophilic archaea in this area. Here, we employed a combination of culture-dependent and culture-independent methods to analyze the collected samples. The high-throughput sequencing results of the archaeal 16S rRNA gene indicated that the richness of halophilic archaea in saline-alkali soils was significantly higher than that in salt lakes. In saline-alkali soils, the Natronomonas genus of archaea was more predominant compared to other genera, while in salt lakes, the Halonotius, Halorubrum, and Haloarcula genera of archaea had relatively higher abundances. However, the dominant families of halophilic archaea in both environments were mainly Haloferacaceae (30.96-72%), Halomicrobiaceae (17-53.19%) and Nanosalinaceae (1-19.08%). Based on the outcomes of pure culture experiments, a total of 26 genera and 98 strains were identified. Among the identified halophilic microorganisms, the predominant species were Halorubrum and Fodinibius, accounting for 33.67% and 13.27%, respectively. The remainder were mostly low-abundance groups within the community, and 22 potential novel taxa were discovered. Additionally, metagenomic technology was employed in our research. The analysis results demonstrated that the microorganisms in this area possess metabolic pathways capable of degrading various pollutants such as atrazine, methane, and dioxins, suggesting that some microorganisms in this area play a positive role in environmental remediation. This study roughly reveals the diversity composition and dominant species of halophilic archaea in these hypersaline environments and provides a scientific basis for the possible ecological functions of microorganisms in this area during long-term survival. It also offers scientific evidence for the development and utilization of halophilic microbial resources and ecological protection.