School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, 100083, China.
Laboratory division, Eighth Medical Center of Chinese People's Liberation Army General Hospital, Beijing, 100000, People's Republic of China.
BMC Microbiol. 2021 Apr 20;21(1):119. doi: 10.1186/s12866-021-02190-6.
Salinization damages the health of soil systems and reduces crop yields. Responses of microbial communities to salinized soils and their functional maintenance under high salt stress are valuable scientific problems. Meanwhile, the microbial community of the salinized soil in the plateau environment is less understood. Here, we applied metagenomics technology to reveal the structure and function of microorganisms in salinized soil of the Tibetan Plateau.
The diversity of composition and function of microbial community in saline soil have changed significantly. The abundances of chemoautotrophic and acidophilic bacteria comprising Rhodanobacter, Acidobacterium, Candidatus Nitrosotalea, and Candidatus Koribacter were significantly higher in saline soil. The potential degradation of organic carbon in the saline soil, as well as the production of NO and NO via denitrification, and the production of sulfate by sulfur oxidation were significantly higher than the non-saline soil. Both types of soils were rich in genes encoding resistance to environmental stresses (i.e., cold, ultraviolet light, and hypoxia in Tibetan Plateau). The resistance of the soil microbial communities to the saline environment is based on the absorption of K as the main mechanism, with cross-protection proteins and absorption buffer molecules as auxiliary mechanisms in our study area. Network analysis showed that functional group comprising chemoautotrophic and acidophilic bacteria had significant positive correlations with electrical conductivity and total sulfur, and significant negative correlations with the total organic carbon, pH, and available nitrogen. The soil moisture, pH, and electrical conductivity are likely to affect the bacterial carbon, nitrogen, and sulfur cycles.
These results indicate that the specific environment of the Tibetan Plateau and salinization jointly shape the structure and function of the soil bacterial community, and that the bacterial communities respond to complex and harsh living conditions. In addition, environmental feedback probably exacerbates greenhouse gas emissions and accelerates the reduction in the soil pH. This study will provide insights into the microbial responses to soil salinization and the potential ecological risks in the special plateau environment.
土壤盐渍化会损害土壤系统的健康,并降低作物产量。了解微生物群落对盐渍土壤的响应及其在高盐胁迫下的功能维持是具有价值的科学问题。同时,高原环境下盐渍土壤的微生物群落了解较少。在这里,我们应用宏基因组学技术来揭示青藏高原盐渍土壤中微生物的结构和功能。
盐渍土壤微生物群落的组成和功能多样性发生了显著变化。在盐渍土壤中,化能自养菌和嗜酸菌(包括 Rhodanobacter、Acidobacterium、Candidatus Nitrosotalea 和 Candidatus Koribacter)的丰度显著更高。盐渍土壤中有机碳的潜在降解以及通过反硝化作用产生的 NO 和 NO、通过硫氧化产生的硫酸盐的能力明显高于非盐渍土壤。两种类型的土壤都富含编码对环境胁迫(即青藏高原的寒冷、紫外线和缺氧)的抗性基因。土壤微生物群落对盐环境的抗性基于对 K 的吸收作为主要机制,在我们的研究区域中,使用了交叉保护蛋白和吸收缓冲分子作为辅助机制。网络分析表明,包含化能自养菌和嗜酸菌的功能组与电导率和总硫呈显著正相关,与总有机碳、pH 和有效氮呈显著负相关。土壤水分、pH 和电导率可能会影响细菌的碳、氮和硫循环。
这些结果表明,青藏高原的特殊环境和盐渍化共同塑造了土壤细菌群落的结构和功能,而细菌群落对复杂和恶劣的生活条件做出了响应。此外,环境反馈可能会加剧温室气体排放,并加速土壤 pH 值的降低。本研究将为微生物对土壤盐渍化的响应以及特殊高原环境中的潜在生态风险提供新的见解。