Division of Geological & Planetary Sciences, California Institute of Technologygrid.20861.3d, Pasadena, California, USA.
Division of Engineering & Applied Science, California Institute of Technologygrid.20861.3d, Pasadena, California, USA.
mBio. 2022 Apr 26;13(2):e0342121. doi: 10.1128/mbio.03421-21. Epub 2022 Mar 14.
Chemolithoautotrophic manganese oxidation has long been theorized but only recently demonstrated in a bacterial coculture. The majority member of the coculture, " Manganitrophus noduliformans," is a distinct but not yet isolated lineage in the phylum (). Here, we established two additional MnCO-oxidizing cultures using inocula from Santa Barbara (California) and Boetsap (South Africa). Both cultures were dominated by strains of a new species, designated " Manganitrophus morganii." The next most abundant members differed in the available cultures, suggesting that while " Manganitrophus" species have not been isolated in pure culture, they may not require a specific syntrophic relationship with another species. Phylogeny of cultivated " Manganitrophus" and related metagenome-assembled genomes revealed a coherent taxonomic family, " Manganitrophaceae," from both freshwater and marine environments and distributed globally. Comparative genomic analyses support this family being Mn(II)-oxidizing chemolithoautotrophs. Among the 895 shared genes were a subset of those hypothesized for Mn(II) oxidation (Cyc2 and PCC_1) and oxygen reduction (TO_1 and TO_2) that could facilitate Mn(II) lithotrophy. An unusual, plausibly reverse complex 1 containing 2 additional pumping subunits was also shared by the family, as were genes for the reverse tricarboxylic acid carbon fixation cycle, which could enable Mn(II) autotrophy. All members of the family lacked genes for nitrification found in species. The results suggest that " Manganitrophaceae" share a core set of candidate genes for the newly discovered manganese-dependent chemolithoautotrophic lifestyle and likely have a broad, global distribution. Manganese (Mn) is an abundant redox-active metal that cycles in many of Earth's biomes. While diverse bacteria and archaea have been demonstrated to respire Mn(III/IV), only recently have bacteria been implicated in Mn(II) oxidation-dependent growth. Here, two new Mn(II)-oxidizing enrichment cultures originating from two continents and hemispheres were examined. By comparing the community composition of the enrichments and performing phylogenomic analysis on the abundant therein, new insights are gleaned on cell interactions, taxonomy, and machineries that may underlie Mn(II)-based lithotrophy and autotrophy.
化能自养锰氧化作用长期以来一直被认为,但直到最近才在细菌共培养物中得到证实。共培养物中的主要成员“Manganitrophus noduliformans”是门()中一个独特但尚未分离的谱系。在这里,我们使用来自加利福尼亚州圣巴巴拉和南非 Boetsap 的接种物建立了另外两个 MnCO 氧化培养物。这两种培养物均由一种新物种的菌株主导,该物种被指定为“Manganitrophus morganii”。在可利用的培养物中,下一个最丰富的成员不同,这表明虽然“Manganitrophus”种没有在纯培养中分离出来,但它们可能不需要与另一种物种建立特定的共生关系。培养的“Manganitrophus”和相关宏基因组组装基因组的系统发育表明,来自淡水和海洋环境并分布在全球范围内的一个连贯的分类家族“Manganitrophaceae”。比较基因组分析支持这个家族是 Mn(II)氧化的化能自养生物。在 895 个共享基因中,有一部分是假设的 Mn(II)氧化(Cyc2 和 PCC_1)和氧还原(TO_1 和 TO_2)的基因,这些基因可能促进 Mn(II)的岩石营养。该家族还共享一个不寻常的、可能是反向复杂 1,其中包含另外两个泵送亚基,以及反向三羧酸碳固定循环的基因,这可能使 Mn(II)能够进行自养。该家族的所有成员都缺乏在种中发现的硝化基因。研究结果表明,“Manganitrophaceae”共享一组新发现的锰依赖化能自养生活方式的候选基因,并且可能具有广泛的、全球分布。锰 (Mn) 是一种丰富的氧化还原活性金属,在地球的许多生物群系中循环。虽然已经证明多种细菌和古菌可以呼吸 Mn(III/IV),但直到最近才发现细菌与 Mn(II)氧化依赖的生长有关。在这里,检查了来自两个大陆和两个半球的两个新的 Mn(II)-氧化富集培养物。通过比较富集物的群落组成,并对其中丰富的进行系统基因组分析,对基于 Mn(II)的岩石营养和自养的细胞相互作用、分类和机制有了新的认识。