Institute of Oceanography, Minjiang University, Fuzhou 350108, China; Key Laboratory of Marine Genetic Resources, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen 361005, China.
Institute of Oceanography, Minjiang University, Fuzhou 350108, China.
Sci Total Environ. 2022 Mar 1;810:152266. doi: 10.1016/j.scitotenv.2021.152266. Epub 2021 Dec 9.
Ocean acidification (OA) is a pressing issue currently and in the future for coral reefs. The importance of maintenance interactions among partners of the holobiont association in the stress response is well appreciated; however, the candidate molecular and microbial mechanisms that underlie holobiont stress resilience or susceptibility remain unclear. Here, to assess the effects of rapid pH change on coral holobionts at both the protein and microbe levels, combined proteomics and microbiota analyses of the scleractinian coral Galaxea fascicularis exposed to three relevant OA scenarios, including current (pH = 8.15), preindustrial (pH = 8.45) and future IPCC-2100 scenarios (pH = 7.85), were conducted. The results demonstrated that pH changes had no significant effect on the physiological calcification rate of G. fascicularis in a 10-day experiment; however, significant differences were recorded in the proteome and 16S profiling. Proteome variance analysis identified some of the core biological pathways in coral holobionts, including coral host infection and immune defence, and maintaining metabolic compatibility involved in energy homeostasis, nutrient cycling, antibiotic activity and carbon budgets of coral-Symbiodiniaceae interactions were key mechanisms in the early OA stress response. Furthermore, microbiota changes indicate substantial microbial community and functional disturbances in response to OA stress, potentially compromising holobiont health and fitness. Our results may help to elucidate many complex mechanisms to describe scleractinian coral holobiont responses to OA and raise interesting questions for future studies.
海洋酸化(OA)是当前和未来珊瑚礁面临的一个紧迫问题。人们充分认识到维持共生体伙伴之间相互作用在压力反应中的重要性;然而,潜在的分子和微生物机制,即共生体对压力的弹性或敏感性的基础,仍然不清楚。在这里,为了评估快速 pH 值变化对珊瑚共生体在蛋白质和微生物水平上的影响,对暴露于三种相关 OA 情景(包括当前(pH = 8.15)、前工业化(pH = 8.45)和未来 IPCC-2100 情景(pH = 7.85)的石珊瑚 Galaxea fascicularis 进行了联合蛋白质组学和微生物组分析。结果表明,在为期 10 天的实验中,pH 值变化对 G. fascicularis 的生理钙化率没有显著影响;然而,在蛋白质组和 16S 分析中记录到了显著差异。蛋白质组方差分析确定了珊瑚共生体中的一些核心生物学途径,包括珊瑚宿主感染和免疫防御,以及维持代谢兼容性涉及的能量稳态、营养循环、抗生素活性和珊瑚-共生藻相互作用的碳预算是早期 OA 应激反应的关键机制。此外,微生物群变化表明,微生物群落和功能受到 OA 胁迫的显著干扰,可能损害共生体的健康和适应性。我们的研究结果可能有助于阐明许多复杂的机制,以描述石珊瑚共生体对 OA 的反应,并为未来的研究提出有趣的问题。