Liu Ying, Zeng Mengchu, Xie Zhe, Ning Daliang, Zhou Jizhong, Yu Xi, Liu Rulong, Zhang Li, Fang Jiasong
Hadal Science and Technology Research Center, Shanghai Ocean University, Shanghai 201306, China.
State Key Laboratory of Geological Process and Mineral Resources, Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China.
Microorganisms. 2022 Mar 17;10(3):639. doi: 10.3390/microorganisms10030639.
Microbial-mediated utilization of particulate organic matter (POM) during its downward transport from the surface to the deep ocean constitutes a critical component of the global ocean carbon cycle. However, it remains unclear as to how high hydrostatic pressure (HHP) and low temperature (LT) with the sinking particles affects community structure and network interactions of the particle-attached microorganisms (PAM) and those free-living microorganisms (FLM) in the surrounding water. In this study, we investigated microbial succession and network interactions in experiments simulating POM sinking in the ocean. Diatom-derived C- and C-labeled POM were used to incubate surface water microbial communities from the East China Sea (ECS) under pressure (temperature) of 0.1 (25 °C), 20 (4 °C), and 40 (4 °C) MPa (megapascal). Our results show that the diversity and species richness of the PAM and FLM communities decreased significantly with HHP and LT. Microbial community analysis indicated an increase in the relative abundance of Bacteroidetes at high pressure (40 MPa), mostly at the expense of Gammaproteobacteria, Alphaproteobacteria, and Gracilibacteria at atmospheric pressure. Hydrostatic pressure and temperature affected lifestyle preferences between particle-attached (PA) and free-living (FL) microbes. Ecological network analysis showed that HHP and LT enhanced microbial network interactions and resulted in higher vulnerability to networks of the PAM communities and more resilience of those of the FLM communities. Most interestingly, the PAM communities occupied most of the module hubs of the networks, whereas the FLM communities mainly served as connectors of the modules, suggesting their different ecological roles of the two groups of microbes. These results provided novel insights into how HHP and LT affected microbial community dynamics, ecological networks during POM sinking, and the implications for carbon cycling in the ocean.
微生物介导的颗粒有机物质(POM)从海洋表层向下运输过程中的利用,是全球海洋碳循环的一个关键组成部分。然而,下沉颗粒所携带的高静水压力(HHP)和低温(LT)如何影响附着在颗粒上的微生物(PAM)以及周围水体中自由生活微生物(FLM)的群落结构和网络相互作用,仍不清楚。在本研究中,我们通过模拟海洋中POM下沉的实验,研究了微生物演替和网络相互作用。利用硅藻衍生的碳和碳标记的POM,在0.1(25℃)、20(4℃)和40(4℃)兆帕(MPa)的压力(温度)下,培养来自东海(ECS)的表层水微生物群落。我们的结果表明,PAM和FLM群落的多样性和物种丰富度随着HHP和LT的增加而显著降低。微生物群落分析表明,在高压(40 MPa)下,拟杆菌门的相对丰度增加,主要是以常压下γ-变形菌纲、α-变形菌纲和薄菌门为代价。静水压力和温度影响了附着在颗粒上(PA)和自由生活(FL)微生物之间的生活方式偏好。生态网络分析表明,HHP和LT增强了微生物网络相互作用,导致PAM群落的网络更容易受到影响,而FLM群落的网络更具恢复力。最有趣的是,PAM群落在网络的大部分模块枢纽中占据主导地位,而FLM群落主要作为模块的连接者,这表明两组微生物具有不同的生态作用。这些结果为HHP和LT如何影响微生物群落动态、POM下沉过程中的生态网络以及对海洋碳循环的影响提供了新的见解。