School of Civil Engineering and Geosciences, Newcastle University, Newcastle Upon Tyne, UK.
Shell International Exploration and Production Inc., Houston, Texas, USA.
Sci Rep. 2017 Nov 22;7(1):16015. doi: 10.1038/s41598-017-16375-5.
Oil and gas percolate profusely through the sediments of the Gulf of Mexico, leading to numerous seeps at the seafloor, where complex microbial, and sometimes animal communities flourish. Sediments from three areas (two cold seeps with contrasting hydrocarbon composition and a site outside any area of active seepage) of the Gulf of Mexico were investigated and compared. Consistent with the existence of a seep microbiome, a distinct microbial community was observed in seep areas compared to sediment from outside areas of active seepage. The microbial community from sediments without any influence from hydrocarbon seepage was characterized by Planctomycetes and the metabolic potential was consistent with detrital marine snow degradation. By contrast, in seep samples with methane as the principal hydrocarbon, methane oxidation by abundant members of ANME-1 was likely the predominant process. Seep samples characterized by fluids containing both methane and complex hydrocarbons, were characterized by abundant Chloroflexi (Anaerolinaceae) and deltaproteobacterial lineages and exhibited potential for complex hydrocarbon degradation. These different metabolic capacities suggested that microorganisms in cold seeps can potentially rely on other processes beyond methane oxidation and that the hydrocarbon composition of the seep fluids may be a critical factor structuring the seafloor microbial community composition and function.
墨西哥湾的沉积物中大量渗出石油和天然气,导致海底出现许多渗出点,那里有复杂的微生物群落,有时还有动物群落。研究了墨西哥湾三个地区(两个碳氢化合物组成截然不同的冷渗出区和一个没有任何活跃渗出区的地点)的沉积物并进行了比较。与渗出微生物组的存在一致,与来自活跃渗出区以外的沉积物相比,在渗出区观察到了明显不同的微生物群落。没有任何碳氢化合物渗出影响的沉积物中的微生物群落以浮霉菌门为特征,其代谢潜力与碎屑海洋雪的降解一致。相比之下,在以甲烷为主要碳氢化合物的渗出样品中,丰富的 ANME-1 成员进行甲烷氧化可能是主要过程。以同时含有甲烷和复杂碳氢化合物的流体为特征的渗出样品,富含绿弯菌门(Anaerolinaceae)和δ变形菌门的谱系,并表现出复杂碳氢化合物降解的潜力。这些不同的代谢能力表明,冷渗出中的微生物可能可以依靠除甲烷氧化以外的其他过程,并且渗出流体的碳氢化合物组成可能是构造海底微生物群落组成和功能的关键因素。