土壤深度对微生物群落和硫的生物循环产生更大的影响,而不是化土壤中的盐度
Yufeng Xin1, Yu Wu1, Honglin Zhang1
1School of Life Sciences, Qufu Normal University, Qufu, China.
The Science of the total environment
|June 21, 2023
概括
土壤深度对微生物群落和盐土中的硫循环产生重大影响,比盐度本身更重要. 与表面土壤相比,更深的土壤显示出不同的微生物结构和改变的硫代谢.
科学领域:
- 土壤微生物学 土壤微生物学
- 环境科学环境科学
- 地质化学 地质化学
背景情况:
- 在盐土中微生物群落的分布对表面层有很好的研究.
- 然而,深层土壤的模式以及深度,盐度和硫代谢的相互作用是不清楚的.
研究的目的:
- 研究微生物群落结构和硫代谢在土壤深度 (表面与深度) 和盐度 (高与低) 之间.
- 为了确定土壤深度和盐度对这些微生物和地化学过程的相对影响.
主要方法:
- 从表面 (5-10厘米) 和深层 (20-25厘米) 的土壤中进行大量土壤的元基因组和物理化学分析.
- 非度量多维缩放 (NMDS) 和冗余分析 (RDA) 用于社区结构和环境因素相关性.
主要成果:
- 土壤深度与硫化合物度有显著的相关性,比盐度有更大的影响.
- 微生物社区的结构,丰富性,同质性和多样性与土壤深度有显著差异.
- 古代生物主宰了表面土壤,而细菌则在深层土壤中丰富;硫代谢基因的丰富程度与深度明显不同.
结论:
- 土壤深度是塑造微生物群落和盐土中硫循环的比盐度更关键的因素.
- 微生物积极参与硫循环,在代谢基因丰度和社区结构中具有深度特定的适应性.
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