Zhang Shuangfei, Hill Russell T, Wang Hui
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, 511458 China.
Biology Department, College of Science, and Guangdong Provincial Key Laboratory of Marine Biotechnology, Shantou University, Shantou, 515063 China.
Mar Life Sci Technol. 2023 Feb 24;5(1):12-27. doi: 10.1007/s42995-023-00164-3. eCollection 2023 Feb.
The Permian Basin is a unique ecosystem located in the southwest of the USA. An unanswered question is whether the bacteria in the Permian Basin adapted to the changing paleomarine environment and survived in the remnants of Permian groundwater. In our previous study, a novel bacterial strain, HW001, was isolated from microalgae cultures incubated with Permian Basin waters, and was shown to originate from the Permian Ocean. In this study, strain HW001 was shown to be the representative strain of a novel family, classified as 'Permianibacteraceae'. The results of molecular dating suggested that the strain HW001 diverged ~ 447 million years ago (mya), which is the early Permian period (~ 250 mya). Genome analysis was used to access its potential energy utilization and biosynthesis capacity. A large number of transporters, carbohydrate-active enzymes and protein-degradation related genes have been annotated in the genome of strain HW001. In addition, a series of important metabolic pathways, such as peptidoglycan biosynthesis, osmotic stress response system and multifunctional quorum sensing were annotated, which may confer the ability to adapt to various unfavorable environmental conditions. Finally, the evolutionary history of strain HW001 was reconstructed and the horizontal transfer of genes was predicted, indicating that the adaptation of to a changing marine environment depends on the evolution of their metabolic capabilities, especially in signal transmission. In conclusion, the results of this study provide genomic information for revealing the adaptive mechanism of strain HW001 to the changing ancient oceans.
The online version contains supplementary material available at 10.1007/s42995-023-00164-3.
二叠纪盆地是位于美国西南部的一个独特生态系统。一个尚未解答的问题是,二叠纪盆地中的细菌是否适应了不断变化的古海洋环境,并在二叠纪地下水残余物中存活下来。在我们之前的研究中,从用二叠纪盆地水域培养的微藻中分离出了一种新型细菌菌株HW001,并表明其起源于二叠纪海洋。在本研究中,菌株HW001被证明是一个新科的代表菌株,被归类为“二叠纪杆菌科”。分子定年结果表明,菌株HW001在约4.47亿年前(mya)分化,即早二叠世时期(约2.5亿年前)。基因组分析用于评估其潜在的能量利用和生物合成能力。在菌株HW001的基因组中已注释了大量转运蛋白、碳水化合物活性酶和与蛋白质降解相关的基因。此外,还注释了一系列重要的代谢途径,如肽聚糖生物合成、渗透胁迫反应系统和多功能群体感应,这可能赋予其适应各种不利环境条件的能力。最后,重建了菌株HW001的进化历史并预测了基因的水平转移,表明其对不断变化的海洋环境的适应取决于其代谢能力的进化,尤其是在信号传递方面。总之,本研究结果为揭示菌株HW001对不断变化的古代海洋的适应机制提供了基因组信息。
在线版本包含可在10.1007/s42995-023-00164-3获取的补充材料。