Environmental Biophysics and Molecular Ecology Program, Department of Marine and Coastal Sciences, Rutgers, The State University of New Jersey, 71 Dudley Road, New Brunswick, NJ, 08901, USA; Department of Ecology, Evolution, and Natural Resources, Rutgers, The State University of New Jersey, 59 Dudley Road, New Brunswick, NJ 08901, USA.
Department of Ecology, Evolution, and Natural Resources, Rutgers, The State University of New Jersey, 59 Dudley Road, New Brunswick, NJ 08901, USA.
Curr Biol. 2015 Mar 2;25(5):628-34. doi: 10.1016/j.cub.2014.12.061. Epub 2015 Feb 12.
The Great Oxidation Event (GOE) ∼2.4 billion years ago resulted from the accumulation of oxygen by the ancestors of cyanobacteria [1-3]. Cyanobacteria continue to play a significant role in primary production [4] and in regulating the global marine and limnic nitrogen cycles [5, 6]. Relatively little is known, however, about the evolutionary history and gene content of primordial cyanobacteria [7, 8]. To address these issues, we used protein similarity networks [9], containing proteomes from 48 cyanobacteria as the test group, and reference proteomes from 84 microbes representing four distinct metabolic groups from most reducing to most oxidizing: methanogens, obligate anaerobes (nonmethanogenic), facultative aerobes, and obligate aerobes. These four metabolic groups represent extant bioinformatic proxies for ancient redox chemistries, extending from an anoxic origin through the GOE and ultimately to obligate aerobes [10-13]. Analysis of the network metric degree showed a strong relationship between cyanobacteria and obligate anaerobes, from which cyanobacteria presumably arose, for core functions that include translation, photosynthesis, energy conservation, and environmental interactions. These data were used to reconstruct primordial functions in cyanobacteria that included nine gene families involved in photosynthesis, hydrogenases, and proteins involved in defense from environmental stress. The presence of 60% of these genes in both reaction center I (RC-I) and RC-II-type bacteria may be explained by selective loss of either RC in the evolutionary history of some photosynthetic lineages. Finally, the network reveals that cyanobacteria occupy a unique position among prokaryotes as a hub between anaerobes and obligate aerobes.
大约 24 亿年前的大氧化事件(GOE)是由蓝细菌的祖先积累氧气引起的[1-3]。蓝细菌继续在初级生产[4]和调节全球海洋和淡水氮循环[5,6]中发挥重要作用。然而,关于原始蓝细菌的进化历史和基因组成相对知之甚少[7,8]。为了解决这些问题,我们使用了蛋白质相似性网络[9],该网络包含 48 种蓝细菌的蛋白质组作为测试组,以及 84 种微生物的参考蛋白质组,这些微生物代表了从最还原到最氧化的四个不同代谢组:产甲烷菌、专性厌氧菌(非产甲烷菌)、兼性需氧菌和专性需氧菌。这四个代谢组代表了现存的生物信息学代理,代表了从缺氧起源到 GOE 最终到专性需氧菌的古代氧化还原化学[10-13]。网络度量度数的分析表明,蓝细菌与专性厌氧菌之间存在很强的关系,蓝细菌可能就是从专性厌氧菌中起源的,核心功能包括翻译、光合作用、能量守恒和环境相互作用。这些数据用于重建蓝细菌中的原始功能,包括涉及光合作用、氢化酶和抵御环境压力的蛋白质的九个基因家族。这些基因的 60%存在于 RC-I 和 RC-II 型细菌中,这可能是由于在某些光合谱系的进化历史中,RC 选择性丢失。最后,该网络揭示了蓝细菌在原核生物中占据着独特的位置,是专性厌氧菌和专性需氧菌之间的枢纽。