Osorio-Pando Lizt Selene, Hernández-Guzmán Mario, Sidón-Ceseña Karla, Ortega-Saad Yamne, Camacho-Ibar Victor F, Chong-Robles Jennyfers, Lago-Lestón Asunción
Posgrado de Ciencias de la Vida, Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE), Ensenada 22860, Baja California, Mexico.
Departamento de Innovación Biomédica, Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE), Ensenada 22860, Baja California, Mexico.
Microorganisms. 2025 May 11;13(5):1106. doi: 10.3390/microorganisms13051106.
The Gulf of Mexico (GoM) is a complex oceanic basin with a maximum depth of 4000 m. It is a complex hydrodynamic system formed by different water masses with distinctive physical and biological characteristics that shape its rich biodiversity. In this study, as a contribution to better understanding the microbial communities inhabiting the meso- and bathypelagic zones of the Mexican Exclusive Economic Zone (EEZ) of the GoM, an extensive set of seawater samples was collected at three depths (350-3700 m) during three oceanographic cruises. The V4-16S rRNA gene analysis identified Pseudomonadota (27.1 ± 9.8%) and Nitrosopumilales (26.4 ± 2.3%) as the dominant bacterial and archaeal members, respectively. The depth, salinity, and apparent oxygen utilization were key environmental drivers, which explained 35% of the community variability. The mesopelagic zone presented a more homogeneous structure characterized by a nitrifier community, while the bathypelagic was more heterogeneous, with hydrocarbon-degrading bacteria and methanogens serving as the key players. This study is the first to report the archaeal community in the deeper waters of the Mexican EEZ of the GoM, playing crucial roles in the nitrogen and carbon cycles, highlighting the region's ecological complexity and the need for further research to understand the broader biogeochemical implications of these processes.
墨西哥湾是一个复杂的海洋盆地,最大深度为4000米。它是一个由具有独特物理和生物特征的不同水体形成的复杂水动力系统,塑造了其丰富的生物多样性。在本研究中,为了更好地了解墨西哥湾墨西哥专属经济区(EEZ)中、深层海域的微生物群落,在三次海洋学巡航期间,于三个深度(350 - 3700米)采集了大量海水样本。V4 - 16S rRNA基因分析确定,假单胞菌门(27.1 ± 9.8%)和硝化侏儒菌目(26.4 ± 2.3%)分别是主要的细菌和古菌成员。深度、盐度和表观氧利用率是关键的环境驱动因素,它们解释了群落变异性的35%。中层海域呈现出以硝化菌群落为特征的更均匀结构,而深层海域则更加异质,以烃降解细菌和产甲烷菌为主。本研究首次报道了墨西哥湾墨西哥专属经济区较深水域的古菌群落,它们在氮和碳循环中发挥着关键作用,突出了该区域的生态复杂性以及进一步开展研究以了解这些过程更广泛的生物地球化学影响的必要性。
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