Linz Alexandra M, He Shaomei, Stevens Sarah L R, Anantharaman Karthik, Rohwer Robin R, Malmstrom Rex R, Bertilsson Stefan, McMahon Katherine D
Department of Bacteriology, University of Wisconsin-Madison, Madison, WI, USA.
Department of Geoscience, University of Wisconsin-Madison, Madison, WI, USA.
PeerJ. 2018 Dec 10;6:e6075. doi: 10.7717/peerj.6075. eCollection 2018.
Although microbes mediate much of the biogeochemical cycling in freshwater, the categories of carbon and nutrients currently used in models of freshwater biogeochemical cycling are too broad to be relevant on a microbial scale. One way to improve these models is to incorporate microbial data. Here, we analyze both genes and genomes from three metagenomic time series and propose specific roles for microbial taxa in freshwater biogeochemical cycles. Our metagenomic time series span multiple years and originate from a eutrophic lake (Lake Mendota) and a humic lake (Trout Bog Lake) with contrasting water chemistry. Our analysis highlights the role of polyamines in the nitrogen cycle, the diversity of diazotrophs between lake types, the balance of assimilatory vs. dissimilatory sulfate reduction in freshwater, the various associations between types of phototrophy and carbon fixation, and the density and diversity of glycoside hydrolases in freshwater microbes. We also investigated aspects of central metabolism such as hydrogen metabolism, oxidative phosphorylation, methylotrophy, and sugar degradation. Finally, by analyzing the dynamics over time in nitrogen fixation genes and genomes, we show that the potential for nitrogen fixation is linked to specific populations in Lake Mendota. This work represents an important step towards incorporating microbial data into ecosystem models and provides a better understanding of how microbes may participate in freshwater biogeochemical cycling.
尽管微生物介导了淡水生态系统中大部分的生物地球化学循环,但目前淡水生物地球化学循环模型中所使用的碳和营养物质类别过于宽泛,无法在微生物尺度上体现其相关性。改进这些模型的一种方法是纳入微生物数据。在此,我们分析了三个宏基因组时间序列中的基因和基因组,并提出了微生物分类群在淡水生物地球化学循环中的具体作用。我们的宏基因组时间序列跨越多年,来源于富营养化湖泊(门多塔湖)和腐殖质湖泊(鳟鱼沼泽湖),二者具有截然不同的水化学性质。我们的分析突出了多胺在氮循环中的作用、不同湖泊类型中固氮菌的多样性、淡水生态系统中同化性硫酸盐还原与异化性硫酸盐还原之间的平衡、不同类型光合作用与碳固定之间的各种关联,以及淡水微生物中糖苷水解酶的密度和多样性。我们还研究了中心代谢的各个方面,如氢代谢、氧化磷酸化、甲基营养和糖降解。最后,通过分析固氮基因和基因组随时间的动态变化,我们表明门多塔湖的固氮潜力与特定种群有关。这项工作是将微生物数据纳入生态系统模型的重要一步,有助于更好地理解微生物如何参与淡水生物地球化学循环。