| Literature DB >> 33203689 |
Liangzhi Li1,2, Zhenghua Liu1,2, Min Zhang1,2, Delong Meng1,2, Xueduan Liu1,2, Pei Wang3, Xiutong Li3, Zhen Jiang3, Shuiping Zhong4,5, Chengying Jiang6, Huaqun Yin7,2.
Abstract
Here, we report three new Acidiphilium genomes, reclassified existing Acidiphilium species, and performed the first comparative genomic analysis on Acidiphilium in an attempt to address the metabolic potential, ecological functions, and evolutionary history of the genus Acidiphilium In the genomes of Acidiphilium, we found an abundant repertoire of horizontally transferred genes (HTGs) contributing to environmental adaption and metabolic expansion, including genes conferring photosynthesis (puf, puh), CO2 assimilation (rbc), capacity for methane metabolism (mmo, mdh, frm), nitrogen source utilization (nar, cyn, hmp), sulfur compound utilization (sox, psr, sqr), and multiple metal and osmotic stress resistance capacities (czc, cop, ect). Additionally, the predicted donors of horizontal gene transfer were present in a cooccurrence network of Acidiphilium Genome-scale positive selection analysis revealed that 15 genes contained adaptive mutations, most of which were multifunctional and played critical roles in the survival of extreme conditions. We proposed that Acidiphilium originated in mild conditions and adapted to extreme environments such as acidic mineral sites after the acquisition of many essential functions.IMPORTANCE Extremophiles, organisms that thrive in extreme environments, are key models for research on biological adaption. They can provide hints for the origin and evolution of life, as well as improve the understanding of biogeochemical cycling of elements. Extremely acidophilic bacteria such as Acidiphilium are widespread in acid mine drainage (AMD) systems, but the metabolic potential, ecological functions, and evolutionary history of this genus are still ambiguous. Here, we sequenced the genomes of three new Acidiphilium strains and performed comparative genomic analysis on this extremely acidophilic bacterial genus. We found in the genomes of Acidiphilium an abundant repertoire of horizontally transferred genes (HTGs) contributing to environmental adaption and metabolic ability expansion, as indicated by phylogenetic reconstruction and gene context comparison. This study has advanced our understanding of microbial evolution and biogeochemical cycling in extreme niches.Entities:
Keywords: Acidiphiliumzzm321990; acid mine drainage; comparative genomics; evolution; horizontal gene transfer
Year: 2020 PMID: 33203689 PMCID: PMC7677001 DOI: 10.1128/mSystems.00867-20
Source DB: PubMed Journal: mSystems ISSN: 2379-5077 Impact factor: 6.496
General features of bacterial genomes used in this study
| Organism and strain | GenBank/IMG-ER accession no. | Level | Contig | No. of plasmids | Completeness (%) | Size (Mb) | Coding density (%) | GC (%) | Clade assigned | No. of genes | No. of proteins | Source | Geographic location | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 2828882166 | Draft | 301 | 124,801 | 95.3 | 4.39 | 90.6 | 66.5 | IV | 4,330 | 4,245 | Acid mine drainage | Fujian, China | ||
| 2824045439 | Complete | 1 | 4,058,204 | 7 | 100 | 4.18 | 90.6 | 66.7 | IV | 4,304 | 4,224 | Acid mine drainage | Guangdong, China | |
| 2824049744 | Draft | 716 | 93,659 | 98.0 | 4.69 | 89.4 | 65.5 | IV | 4,352 | 4,347 | Acid mine drainage | Guangdong, China | ||
| GCA_000701585.1/2561511102 | Draft | 206 | 71,968 | 98.5 | 4.07 | 89.6 | 63.6 | II | 3,851 | 3,731 | Acid mine | |||
| GCA_000016725.1/640427101 | Complete | 1 | 3,389,227 | 8 | 100 | 3.96 | 90.8 | 67.1 | IV | 3,747 | 3,574 | Acid mine | ||
| GCA_000202835.1 | Complete | 1 | 3,749,411 | 8 | 100 | 4.21 | 89.8 | 67.0 | IV | 3,991 | 3,803 | Acid mine water | Iwate, Matsuo, Japan | |
| GCA_900156265.1/2681812815 | Draft | 78 | 136,338 | 98.6 | 3.98 | 89.9 | 63.7 | II | 3,752 | 3,692 | Acidic coal mine drainage | Pennsylvania, USA | ||
| GCA_002255515.1 | Draft | 119 | 80,126 | 98.6 | 3.41 | 89.4 | 66.6 | III | 3,199 | 3,073 | Mine wastewater | Ontario, Canada | ||
| GCA_002255745.1 | Draft | 132 | 63,048 | 98.6 | 3.06 | 90.8 | 60.2 | I | 2,940 | 2,828 | Mine wastewater | Ontario, Canada | ||
| GCA_002255545.1 | Draft | 433 | 1,584 | 16.2 | 0.69 | 85.0 | 61.7 | II | 910 | 832 | Mine wastewater | Ontario, Canada | ||
| GCA_002255645.1 | Draft | 542 | 1,752 | 11.5 | 1.02 | 82.6 | 65.7 | III | 1,316 | 1,189 | Mine wastewater | Ontario, Canada | ||
| GCA_002279225.1 | Draft | 884 | 2,201 | 44.6 | 1.81 | 82.3 | 67.9 | III | 2,291 | 1,999 | Mine wastewater | Ontario, Canada | ||
| GCA_002282645.1 | Draft | 89 | 65,514 | 83.8 | 3.11 | 90.6 | 60.1 | I | 3,029 | 2,695 | Mine wastewater | Ontario, Canada | ||
| GCA_002282635.1 | Draft | 180 | 38,599 | 93.9 | 3.86 | 88.6 | 63.7 | II | 3,623 | 3,413 | Mine wastewater | Ontario, Canada | ||
| GCA_002279355.1 | Draft | 98 | 72,002 | 96.6 | 3.07 | 90.9 | 60.0 | I | 2,916 | 2,791 | Mine wastewater | Ontario, Canada | ||
| GCA_002279345.1 | Draft | 211 | 43,062 | 97.3 | 4.03 | 88.3 | 63.5 | II | 3,799 | 3,620 | Mine wastewater | Ontario, Canada | ||
| GCA_002279335.1 | Draft | 937 | 3,121 | 62.2 | 2.48 | 89.9 | 67.0 | III | 2,942 | 2,632 | Mine wastewater | Ontario, Canada | ||
| 2734482270 | Draft | 74 | 76,901 | 97.3 | 3.08 | 92.7 | 68.8 | IV | 3,042 | 2,992 | Acid mine drainage | Guangdong, China | ||
| GCA_000437515.1 | Draft | 116 | 9,562 | 82.5 | 1.73 | — | 45.4 | — | 1,509 | 1,479 | Gut microbiota | |||
| GCA_000724705.2/2571042905 | Draft | 296 | 44,500 | 98.6 | 4.18 | 88.4 | 66.9 | IV | 4,059 | 3,719 | Acid mine drainage | Lusatia, Germany, Europe | ||
| GCA_000219295.2 | Draft | 627 | 12,446 | 91.2 | 3.93 | 86.4 | 66.4 | IV | 3,908 | 3,859 | Acidic, metal-rich water | Rio Tinto, Spain, Europe |
—, not available.
FIG 1(A) The evolutionary timeline of Acidiphilium was estimated (left) using RelTime on top of the rooted NJ tree based on the concatenated alignment of 133 core genes. Ancestral genome content reconstruction of Acidiphilium was performed with Count software, and the color depth represents the numbers of reconstructed gain, loss, expansion, and contraction events of each lineage. Data of asteroid impacts, solar luminosity, and fluctuations in atmospheric oxygen and carbon dioxide concentrations are displayed synchronously with divergence times in the form of time panels (left). A stack bar diagram (right) shows the number of genes shared by all strains (i.e., the core genome), the number of genes shared by partial strains (i.e., the accessory genome), and the number of strain-specific genes (i.e., the unique gene) in the tested strains. (B) Stack bar chart showing functional proportions of Acidiphilium gene families undergoing gain, loss, expansion, and contraction events as based on COG classes. (C) Mathematical modeling of the pangenome and core genome of Acidiphilium. (D) Bar chart showing functional proportions (based on COG categories) of different parts of the Acidiphilium pangenome (i.e., core, accessory, unique). Detailed descriptions of the COG categories are provided in Text S1 in the supplemental material.
FIG 2Overview of metabolic potentials in Acidiphilium as predicted from genome annotation; core/specific metabolic features are shown with different colors, and pathways containing predicted horizontally transferred genes are marked with black rectangles.
FIG 3Pie charts showing donors that putatively transferred genes to Acidiphilium spp., their relative contributions to total HGT events, and the functional proportions of the HGT functions derived from respective donors based on COG classes. Detailed descriptions of the COG categories are provided in Text S1 in the supplemental material.
FIG 4Cooccurrence network based on correlation analysis of 16S rRNA amplicon sequencing data sets of AMD samples (n = 205). Each node denotes a microbial OTU at a 97% cutoff. The first neighbors of Acidiphilium nodes (highlighted by a red rectangle) were selected using the tool “first neighbors of selected nodes” in Cytoscape.