| Literature DB >> 33281797 |
Dimitry Y Sorokin1,2, Damon Mosier3, Jackie K Zorz3, Xiaoli Dong3, Marc Strous3.
Abstract
A new haloalkaliphilic species of Wenzhouxiangella, strain AB-CW3, was isolated from a system of hypersaline alkaline soda lakes in the Kulunda Steppe using cells of Staphylococcus aureus as growth substrate. AB-CW3's complete, circular genome was assembled from combined nanopore and Illumina sequencing and its proteome was determined for three different experimental conditions. AB-CW3 is an aerobic gammaproteobacterium feeding mainly on proteins and peptides. Unique among Wenzhouxiangella, it uses a flagellum for motility, fimbria for cell attachment and is capable of complete denitrification. AB-CW3 can use proteins derived from living or dead cells of Staphylococcus and other Gram-positive bacteria as the carbon and energy source. It encodes and expresses production of a novel Lantibiotic, a class of antimicrobial peptides which have so far only been found to be produced by Gram-positive bacteria. AB-CW3 likely excretes this peptide via a type I secretion system encoded upstream of the genes for production of the Lanthipeptide. Comparison of AB-CW3's genome to 18 other Wenzhouxiangella genomes from marine, hypersaline, and soda lake habitats indicated one or two transitions from marine to soda lake environments followed by a transition of W. marina back to the oceans. Only 19 genes appear to set haloalkaliphilic Wenzhouxiangella apart from their neutrophilic relatives. As strain AB-CW3 is only distantly related to other members of the genus, we propose to provisionally name it "Wenzhouxiangella alkaliphila".Entities:
Keywords: Wenzhouxiangella; bacteriovores; comparative genomics; denitrification; lantibiotic; nanopore sequencing; proteolytic alkaline soda lake
Year: 2020 PMID: 33281797 PMCID: PMC7691419 DOI: 10.3389/fmicb.2020.597686
Source DB: PubMed Journal: Front Microbiol ISSN: 1664-302X Impact factor: 5.640
Accession numbers and genome properties of Wenzhouxiangella and two Marinicella whole genome sequences and metagenome assembled genomes (MAGs).
| Genome properties | Checkm estimates | ||||||||
| Description | Accession # | Origin | Size (Mb) | % GC | N50 (kb) | #contigs | # 16S rRNA genes | Completeness | Contamination |
| CP061368 | Kulunda soda lakes, Russia | 3.84 | 61.8 | 3845 | 1 | 1 | 98.6 | 2.5 | |
| GCF_001187785 | Indian Ocean | 3.68 | 65.3 | 3675 | 1 | 1 | 99.6 | 1.1 | |
| GCF_011008905 | Lake sediment, Shanxi, China | 3.13 | 63.1 | 566 | 27 | 1 | 97.5 | 0.8 | |
| GCF_010499265 | Lake sediment, Shanxi, China | 3.35 | 63.7 | 372 | 52 | 1 | 98.0 | 2.2 | |
| GCF_008725655 | Sediment, Weihai, China | 3.43 | 64.4 | 340 | 18 | 1 | 97.2 | 1.0 | |
| GCF_011064545 | Sediment, Shanxi, China | 3.29 | 66.5 | 316 | 37 | 1 | 95.9 | 2.8 | |
| GCF_003410055 | Harbor sediment, China | 3.51 | 65.4 | 136 | 54 | 1 | 97.8 | 1.2 | |
| GCF_003410035 | Lake water, Xinjiang, China | 3.13 | 62.9 | 107 | 55 | 1 | 97.1 | 2.0 | |
| GCF_003417465 | Lake water, Xinjiang, China | 3.13 | 62.9 | 107 | 55 | 1 | 97.1 | 2.0 | |
| GCF_012272825 | Salt lake sediment, Shanxi, China | 3.75 | 67.8 | 94 | 200 | 1 | 99.6 | 2.0 | |
| MAG | GCA_003567685 | Soda lake sediment, Kulunda, Russia | 2.74 | 61.7 | 55 | 107 | 0 | 97.6 | 2.1 |
| MAG | GCA_003560975 | Soda lake sediment, Kulunda, Russia | 3.08 | 65.2 | 17 | 286 | 0 | 96.6 | 3.1 |
| MAG Probe Lake 43 | GCA_007695005 | Soda Lake microbial mat, Cariboo, Canada | 3.31 | 62.6 | 25 | 218 | 0 | 95.0 | 2.5 |
| MAG | GCA_003565625 | Soda lake sediment, Kulunda, Russia | 2.81 | 63.6 | 63 | 95 | 0 | 94.9 | 3.1 |
| MAG Deer Lake 32 | GCA_007694055 | Soda lake microbial mat, Cariboo, Canada | 4.15 | 62.4 | 12 | 459 | 0 | 94.8 | 4.3 |
| MAG Probe Lake 80 | GCA_007694885 | Soda lake microbial mat, Cariboo, Canada | 2.60 | 65.0 | 21 | 215 | 0 | 91.9 | 3.9 |
| MAG Hydrothermal Chimney 1 | GCA_003233115 | Hydrothermal Chimney Wall, Mid Atlantic Ridge | 3.19 | 54.3 | 25 | 225 | 1 | 92.7 | 8.2 |
| MAG Hydrothermal Chimney 2 | GCA_003233095 | Hydrothermal Chimney Wall, Mid Atlantic Ridge | 2.89 | 55.4 | 18 | 232 | 0 | 92.3 | 2.5 |
| GCF_002000055 | Marine sediment, China | 3.99 | 48.1 | 315 | 45 | 98.6 | 1.9 | ||
| GCF_002591915 | Seawater, Japan/Russian coast | 3.35 | 42.4 | 857 | 36 | 97.8 | 1.9 | ||
| MAG* | GCA_003564575 | Soda lake sediment, Kulunda, Russia | 3.18 | 60.3 | 22 | 215 | 0 | 82.1 | 15.0 |
| MAG* | GCA_003556345 | Soda lake sediment, Kulunda, Russia | 3.42 | 60.4 | 18 | 277 | 0 | 80.8 | 12.0 |
| MAG* | GCA_002722315 | Pacific Ocean Water | 3.53 | 64.1 | 923 | 53 | 0 | 80.7 | 2.5 |
| MAG* | GCA_003558275 | Soda lake sediment, Kulunda, Russia | 2.85 | 61.7 | 6 | 520 | 0 | 76.0 | 5.6 |
| MAG* | GCA_003556425 | Soda lake sediment, Kulunda, Russia | 2.70 | 62.9 | 10 | 346 | 0 | 75.4 | 5.1 |
| MAG* | GCA_003556645 | Soda lake sediment, Kulunda, Russia | 2.62 | 60.3 | 12 | 308 | 0 | 73.5 | 2.6 |
| MAG* | GCA_003561495 | Soda lake sediment, Kulunda, Russia | 2.55 | 60.2 | 13 | 257 | 0 | 72.9 | 1.7 |
| MAG* | GCA_003557665 | Soda lake sediment, Kulunda, Russia | 3.34 | 63.2 | 14 | 345 | 0 | 70.8 | 6.9 |
| MAG* | GCA_003562675 | Soda lake sediment, Kulunda, Russia | 2.43 | 61.9 | 12 | 308 | 0 | 67.2 | 0.0 |
| MAG* | GCA_003556165 | Soda lake sediment, Kulunda, Russia | 1.95 | 62.6 | 15 | 176 | 0 | 66.4 | 1.8 |
| MAG* | GCA_003557225 | Soda lake sediment, Kulunda, Russia | 2.17 | 64.2 | 6 | 398 | 0 | 62.5 | 5.8 |
| MAG* | GCA_003568225 | Soda lake sediment, Kulunda, Russia | 4.41 | 59.2 | 8 | 681 | 0 | 61.8 | 5.3 |
| MAG* | GCA_003562715 | Soda lake sediment, Kulunda, Russia | 1.82 | 62.6 | 7 | 293 | 0 | 56.8 | 1.2 |
| MAG* | GCA_003568335 | Soda lake sediment, Kulunda, Russia | 1.43 | 61.9 | 5 | 295 | 0 | 51.0 | 1.7 |
FIGURE 1Cell morphology of strain AB-CW3 grown with Staphylococcus cells, shown as S-cell (a–c), casein (d) and peptone/yeast extract (e). Electron microscopy showed that cells of AB-CW3 often appeared attached to Staphylococcus cells and posses a single polar flagellum (b) and tufts of long thin fimbria-like filaments, shown as F (c).
Whole genome average nucleotide identity and 16S rRNA gene identity between strain AB-CW3 and other Wenzhouxiangella and Marinicella.
| Target organism | % average nucleotide identity | % of genomes aligned* | % identity of 16S rRNA gene |
| AB-CW3 | 100.0 | 100.0 | 100.0 |
| 78.8 | 29.2 | 97.2 | |
| 78.7 | 29.0 | 97.2 | |
| 78.7 | 29.9 | 97.0 | |
| 78.6 | 32.2 | 96.2 | |
| 78.2 | 27.5 | 95.6 | |
| MAG Deer Lake 32 | 78.0 | 24.7 | – |
| 78.0 | 24.6 | 96.7 | |
| MAG Kulunda 2 | 78.0 | 24.4 | – |
| MAG Kulunda 3 | 77.7 | 23.0 | – |
| 77.6 | 22.8 | 94.8 | |
| MAG Probe Lake 80 | 77.8 | 21.1 | – |
| MAG Probe Lake 43 | 77.6 | 20.8 | – |
| MAG Kulunda 1 | 77.6 | 20.0 | – |
| 77.1 | 10.0 | 91.0 | |
| 76.2 | 7.8 | 88.5 | |
| MAG Hydrothermal Chimney 1 | Below detection limit | 89.4 | |
| Below detection limit | 87.5 | ||
| Below detection limit | 87.3 | ||
FIGURE 2pH profile at 2 M total Na+ (A) and salt profile at pH 9.5 (B) for growth of AB-CW3 with peptone/yeast extract. Data represent mean values from duplicate parallel incubations at 37°C. The pH was measured at each sampling point.
FIGURE 3Bootstrapped maximum likelihood phylogenetic trees of Wenzhouxiangella and Marinicella isolates and metagenome assembled genomes (MAGs) based on a concatenated alignment of 126 conserved single copy genes (43,127 positions) (Parks et al., 2017) (A), and sodium-pumping NADH:ubiquinone oxidoreductase subunits NqrABC (1,098 positions) (B), and based on 16S rRNA genes (C). *indicate incomplete metagenome assembled genomes (<90% completeness, as estimated by CheckM), which generally do not include 16S rRNA genes. Bootstrap values are indicated at nodes when lower than 99%.
FIGURE 4Evidence for anaerobic growth of AB-CW3 by denitrification. (A) Gradual adaptation to anaerobic growth with nitrate (the third flask) after micro-aerophilic growth (the second flask); the direct transfer from an aerobic culture to anoxic conditions did not result in growth with nitrate (the first flask). (B) Anaerobic growth with nitrous oxide was rapid and effective. (C) Anaerobic growth occurred with nitrate and nitrous oxide, but not with nitrite. However, no nitrite accumulated during nitrate reduction. The data are mean values from duplicate experiments.