Literature DB >> 31743595

Physiological and genomic features of Paraoceanicella profunda gen. nov., sp. nov., a novel piezophile isolated from deep seawater of the Mariana Trench.

Ping Liu1,2, Wanzhen Ding1,2, Qiliang Lai3, Rulong Liu1,2, Yuli Wei1,2, Li Wang1,2, Zhe Xie1,2, Junwei Cao1,2, Jiasong Fang1,4,5.   

Abstract

A novel piezophilic alphaproteobacterium, strain D4M1T , was isolated from deep seawater of the Mariana Trench. 16S rRNA gene analysis showed that strain D4M1T was most closely related to Oceanicella actignis PRQ-67T (94.2%), Oceanibium sediminis O448T (94.2%), and Thioclava electrotropha ElOx9T (94.1%). Phylogenetic analyses based on both 16S rRNA gene and genome sequences showed that strain D4M1T formed an independent monophyletic branch paralleled with the genus Oceanicella in the family Rhodobacteraceae. Cells were Gram-stain-negative, aerobic short rods, and grew optimally at 37°C, pH 6.5, and 3.0% (w/v) NaCl. Strain D4M1T was piezophilic with the optimum pressure of 10 MPa. The principal fatty acids were C18:1 ω7c/C18:1 ω6c and C16:0 , major respiratory quinone was ubiquinone-10, and predominant polar lipids were phosphatidylglycerol, phosphatidylethanolamine, and an unidentified aminophospholipid. The complete genome contained 5,468,583-bp with a G + C content of 70.2 mol% and contained 4,855 protein-coding genes and 78 RNA genes. Genomic analysis revealed abundant clues on bacterial high-pressure adaptation and piezophilic lifestyle. The combined evidence shows that strain D4M1T represents a novel species of a novel genus in the family Rhodobacteraceae, for which the name Paraoceanicella profunda gen. nov., sp. nov. is proposed (type strain D4M1T  = MCCC 1K03820T  = KCTC 72285T ).
© 2019 The Authors. MicrobiologyOpen published by John Wiley & Sons Ltd.

Entities:  

Keywords:  zzm321990Paraoceanicella profundazzm321990; genome sequencing; high-pressure adaptation; piezophilic; polyphasic taxonomy

Year:  2019        PMID: 31743595      PMCID: PMC7002103          DOI: 10.1002/mbo3.966

Source DB:  PubMed          Journal:  Microbiologyopen        ISSN: 2045-8827            Impact factor:   3.139


INTRODUCTION

The deep sea, accounting for approximately 75% of the total ocean volume and hosting 62% of the global biosphere (Fang, Zhang, & Bazylinski, 2010), is a reservoir of remarkably diverse archaea and bacteria. The extreme physical–chemical factors (high salinity, high pressure, and low temperature) in the deep sea may have considerable influences on microbial life. For example, high pressure, the most unique physical parameter in the deep sea, decreases membrane permeability and stability, impedes energy metabolism, and inactivates proteins (Jebbar, Franzetti, Girard, & Oger, 2015; Picard & Daniel, 2013). Thus, piezophiles must evolve physiological and genomic adaptations to grow under high‐pressure conditions. Microorganisms use different strategies to thrive in high‐pressure conditions, such as synthesizing piezolytes, improving permeability and stability of cell membrane, regulating gene expression, and modifying genome features (Oger & Jebbar, 2010; Simonato et al., 2006). Despite the fact that greater than 88% of the ocean's biosphere is above 10 MPa (water depths of 1,000 m or more), a limited number of piezophiles have been isolated and characterized (Picard & Daniel, 2013; Zhang, Wu, & Zhang, 2018). During our recent campaign of investigating the diversity of culturable microbes in the deep ocean, we isolated a novel piezophilic bacterium D4M1T, which was closely related to the species in the family Rhodobacteraceae within the class Alphaproteobacteria. The family Rhodobacteraceae (type genus, Rhodobacter) contains more than 130 genera (http://www.bacterio.net/), many members of which have been isolated from the marine environment (Albuquerque, Rainey, Nobre, & da Costa, 2012; Chang et al., 2018; Chang, Meng, Du, & Du, 2019). Additionally, some members have been isolated from deep‐sea environment, such as members belonging to the genera Acidimangrovimonas (Jiang, Xu, Shao, & Long, 2014), Brevirhabdus (Wu et al., 2015), Celeribacter (Lai, Cao, Yuan, Li, & Shao, 2014), Citreicella (Lai et al., 2011), Marinibacterium (Li, Lai, et al., 2015), Meridianimarinicoccus (Ren et al., 2019), Pararhodobacter (Lai, Liu, Yuan, Xie, & Shao, 2019), Profundibacterium (Lai et al., 2013), and Thiobacimonas (Li, Tang, Liu, & Jiao, 2015). In this study, the marine bacterial strain D4M1T was characterized using a polyphasic approach, along with the genome sequence analysis and high‐pressure adaptation.

MATERIALS AND METHODS

Strains and culture conditions

A deep seawater sample was collected at a depth of 10,890 m from the Mariana Trench (142.4°E, 11.4°N; site MT) in December 2016. The sample (1 ml) was serially diluted with 10 ml sterilized natural seawater and spread onto a selective D4 agar medium (1.0 L seawater, 0.2 g yeast extract, 3.0 g HEPES, 2.0 g xylose, 17.0 g agar, and pH 7.0) under atmospheric pressure. Subsequently, a white‐colored strain D4M1T was isolated by restreaking single colonies onto D4 agar plates at 10°C. The strains grew well on marine agar 2216 (MA; BD Difco) or in marine broth 2216 (MB; BD Difco) medium and were routinely cultivated on MA or MB in this study, unless noted otherwise. Stock cultures were stored at −80°C with 20% (v/v) glycerol. The phylogenetically related type strains, Oceanicella actignis DSM 22673T (=PRQ‐67T), Thioclava electrotropha DSM 103712T (=ElOx9T), and Oceanibium sediminis MCCC 1H00233T (=O448T), were obtained from the Leibniz Institute DSMZ–German Collection of Microorganisms and Cell Cultures (DSMZ) and Marine Culture Collection of China (MCCC), respectively.

DNA extraction, genomic, and phylogenetic analyses

Genomic DNA was extracted from liquid cultures of strain D4M1T after being cultivated in MB for 36 hr using the ChargeSwitch® gDNA Mini Bacteria Kit (Life Technologies) according to the manufacturer's instructions. The 16S rRNA gene of strain D4M1T was amplified and sequenced by using conserved primers Bac8F (5′‐AGAGTTTGATCATGGCTCAG‐3′) and U1492R (5′‐GGTTACCTTGTTACGACTT‐3′), as reported previously (Cao et al., 2016). The 16S rRNA gene sequence was identified using global alignment algorithm implemented at the EzBioCloud server (https://www.ezbiocloud.net/; (Yoon et al., 2017)). Phylogenetic analysis of 16S rRNA gene was conducted with MEGA 5.0 package (Tamura et al., 2011), using the Kimura two‐parameters model with the neighbor‐joining (Saitou & Nei, 1987) and maximum‐likelihood (Felsenstein, 1981) algorithms, respectively. The tree topology was calculated by bootstrap analysis based on 1,000 bootstraps. Purified genomic DNA was quantified by TBS‐380 fluorometer (Turner BioSystems Inc.). The complete genome was sequenced using a combination of Pacific Biosciences (PacBio) RS and Illumina sequencing platforms (Shanghai Majorbio Bio‐pharm Technology Co., Ltd.). For PacBio sequencing, 8–10 k insert whole‐genome shotgun libraries were generated and sequenced on a PacBio RS instrument using standard methods. For Illumina sequencing, 500 bp paired‐end library were generated and sequenced using Illumina Hiseq Xten. The genome was assembled using Velvet assembler (v1.2.09) with a kmer length of 17 and “PacBioToCA with Celera Assembler” pipeline (Chin et al., 2013; Koren et al., 2012) with both the PacBio reads and Illumina reads. The genome sequences of Thioclava electrotropha Elox9T (NBXF00000000), Thioclava pacifica DSM 10166T (AUND00000000), Rhodobacter megalophilus DSM 18937T (FZOV00000000), Rhodobacter johrii JA192T (PZZW00000000), Paenirhodobacter enshiensis DW2‐9T (JFZB00000000), Oceanicella actignis CGMCC 1.10808 (FRDL00000000), and Oceanibium sediminis O448T (QGNX00000000) were obtained from the NCBI website. The Oceanicella actignis DSM 22673T genome sequence (IMG Genome ID: 2593339287) was downloaded from the Genome portal of the Joint Genome Institute (JGI) (http://genome.jgi.doe.gov/). The genomic DNA G + C content was estimated from the genome sequence. A whole‐genome‐based phylogenetic tree was reconstructed based on the whole‐genome protein sequences using CVTree3 (http://tlife.fudan.edu.cn/cvtree/cvtree/) with K‐value = 6 (Zuo & Hao, 2015). The genomic analyses were performed as described previously (Cao, Lai, Yuan, & Shao, 2015) using the tools available on the Integrated Microbial Genomes (IMG) server (https://img.jgi.doe.gov) (Chen et al., 2019).

Phenotypic, physiologic, and biochemical analyses

Images of cells of strain D4M1T were obtained with a transmission electron microscopy (JEM‐1230; Jeol) after glutaraldehyde prefixation and uranyl acetate staining of cells grown on MA at 37°C for 30 hr. Growth characteristics were determined by the measurement of optical density at 600 nm (OD600) using a NanoDrop 2000c spectrophotometer (Thermo Scientific). The growth temperature was evaluated at 4, 10, 20, 25, 30, 37, 40, 45, and 50°C in duplicates in 10 days. The salinity range (0, 0.5, and 1%–10% (intervals of 1%) of NaCl, w/v) and pH range (pH 4.0–11.0 (intervals of 1 unit), added with 20 μmol/L HOMOPIPES, MES, PIPES, HEPES and CAPS buffers, respectively) were investigated as previously described in duplicates (Lai et al., 2014). Gram‐staining, oxidase, and catalase activity were carried out according to the test procedures described by Dong and Cai (2001). Growth under anaerobic condition was tested in LB liquid medium (for fermentation) and in LB supplemented with Na2SO4 or NaNO3 (10 mmol/L, for anaerobic respiration) with oxygen‐free N2 gas phase (200 kPa) in sealed sterile vials at 37°C for 7 days. Poly‐β‐hydroxybutyrate (PHB) production was determined by using Nile blue A staining and an upright fluorescence microscope (ECLIPSE Ni‐U; Nikon) according to a previous study (Ostle & Holt, 1982). Determination of the hydrostatic pressure range for growth was carried out in hydrostatic pressure vessels under a pressure range of 0.1–80 MPa (intervals of 10 MPa) at the optimal temperature (37°C), with oxygen‐saturated Fluorinert (FC‐40, 3M Company. 25% of total volume) added to supply oxygen (Kato, Sato, & Horikoshi, 1995). Other biochemical tests were carried out using API 20NE, API ZYM strips (bioMérieux) and GEN III microplates by Biolog system (Biolog Microstation™) according to the manufacturer's instructions. Some tests in API strips, such as reduction of nitrate, fermentation of D‐glucose, hydrolysis of aesculin, and utilization of citrate, were also re‐examined by conventional biochemical identification as described by Dong and Cai (2001).

Chemotaxonomic analysis

The fatty acid and polar lipid profiles of strain D4M1T were analyzed on exponential growth phase of cultures grown in MB at 37°C for 48 hr. Fatty acids in whole cells were saponified, extracted, and methylated using the standard protocol of Microbial IDentification Inc. (MIDI, Sherlock Microbial Identification System, version 6.0B). The fatty acids were analyzed by gas chromatography (GC, Agilent Technologies 6850) and identified by using the TSBA 6.0 database of the Microbial Identification System (Sasser, 1990). Polar lipids were extracted from 100 mg of freeze‐dried cells using a chloroform/methanol system, separated by two‐dimensional thin‐layer chromatography (TLC) on silica gel 60 F254 plates (Merck), and then identified with molybdophosphoric acid as the spray reagent according to a previously described method (Tindall, Sikorski, Smibert, & Krieg, 2007). The fatty acid and polar lipid profiles of reference strains Oceanicella actignis DSM 22673T and Thioclava electrotropha DSM 103712T were performed in parallel with strain D4M1T under the same condition. The respiratory quinone was extracted from freeze‐dried cells with chloroform/methanol (2:1, v/v) and evaporated to dryness at 35°C. The extracts were resuspended in chloroform/methanol (2:1, v/v) and subsequently purified by TLC on GF254 silica gel plates (Branch of Qingdao Haiyang Chemical Co. Ltd.) with n‐hexane/ether (17:3, v/v). The respiratory quinones were measured by HPLC‐MS system (Agilent) (Wu et al., 2015).

RESULTS AND DISCUSSION

Phylogenetic and phylogenomic analyses

16S rRNA gene sequence analysis showed that strain D4M1T had the highest 16S rRNA gene sequence similarity of 94.2% with Oceanicella actignis PRQ‐67T and Oceanibium sediminis O448T, followed by Thioclava electrotropha ElOx9T (94.1%). Genera are generally described as agglomerates of nodal species and internodal strains (Gillis, Vandamme, De Vos, Swings, & Kersters, 2001), for which similarity values around 94.5%–95% are commonly used for genus differentiation (Ludwig et al., 1998; Yarza et al., 2014). Based on these criteria, strain D4M1T likely represent a novel genus in the family Rhodobacteraceae. Phylogenetic analysis based on 16S rRNA gene sequence showed that strain D4M1T formed an independent monophyletic branch paralleled with the genus Oceanicella within the family Rhodobacteraceae, suggesting that it may represent a novel genus within the family Rhodobacteraceae (Figure 1 and Figure A1).
Figure 1

Neighbor‐joining tree showing the phylogenetic positions of strain D4M1T and related species, based on 16S rRNA gene sequence. Chromatocurvus halotolerans EG19T was used as outgroup. Filled circles indicate nodes that were also recovered in the maximum‐likelihood (Figure A1) tree for the same sequences. Bootstrap values (expressed as percentages of 1,000 replications) greater than 50% are shown at branch nodes. Bar, 0.01 nucleotide substitution rate (K nuc) units

Figure A1

Maximum‐likelihood tree showing the phylogenetic positions of strain D4M1T and related species, based on 16S rRNA gene sequence. Chromatocurvus halotolerans EG19T was used as outgroup. Bootstrap values (expressed as percentages of 1,000 replications) are shown at branch nodes. Bar, 0.02 nucleotide substitution rate (K nuc) units

Neighbor‐joining tree showing the phylogenetic positions of strain D4M1T and related species, based on 16S rRNA gene sequence. Chromatocurvus halotolerans EG19T was used as outgroup. Filled circles indicate nodes that were also recovered in the maximum‐likelihood (Figure A1) tree for the same sequences. Bootstrap values (expressed as percentages of 1,000 replications) greater than 50% are shown at branch nodes. Bar, 0.01 nucleotide substitution rate (K nuc) units Phylogenomic analysis, previously suggested to provide a better taxonomic framework at the genus and higher levels (Chun et al., 2018), was further carried out to provide a better taxonomic characterization. A total of 2.36 Gb of clean data were generated from the genome sequencing of D4M1T. The final assembly has 431‐fold coverage for the complete genome, which contains 5,468,583‐bp with a G + C content of 70.2 mol%. The complete genome consists of a circular chromosome of 4,417,125 bp and six plasmids ranging from 112,235 bp to 586,520 bp in length (Table 1 and Figure 2). The assembled and annotated genome of D4M1T has been deposited in GenBank (accession numbers: CP040818–CP040824) and JGI portal (GOLD ID: Gp0432545; IMG Taxon ID: 2828513066). A whole‐genome‐based phylogenomic tree (Figure 3) showed that strain D4M1T formed an independent monophyletic branch within the family Rhodobacteraceae. This result supports that strain D4M1T represents a genus‐level taxon in agreement with the result of 16S rRNA gene phylogeny.
Table 1

General features of the complete genome sequence of strain D4M1T

ContentChromosomePlasmids
pD4M1ApD4M1BpD4M1CpD4M1DpD4M1EpD4M1F
Size (bp)4039866586520288677189758137471114056112235
G + C content (mol%)70.071.071.571.771.161.271.4
Protein‐coding genes358852524117111112495
Average gene size (bp)9409671037100110288091011
Coding density (%)83.5%86.6%86.6%90.2%83.0%88.0%85.6%
Gene assigned to COG2996462211154748476
tRNA54300000
rRNA operon (23S, 16S and 5S)3100000
ncRNA9000000
GenBank accession CP040818 CP040819 CP040820 CP040821 CP040822 CP040823 CP040824
Figure 2

Circular maps of the chromosome and six plasmids of strain D4M1T. Plasmids pD4M1A, pD4M1B, pD4M1C, pD4M1D, pD4M1E, and pD4M1F are shown at 3, 6, 8, 8, 8, and 8 × scale, respectively, relative to the chromosome scale. From the outside to the center: protein‐coding genes on forward strand (color by COG categories), total genes on forward strand, total genes on reverse strand, protein‐coding genes on reverse strand, G + C content, and G + C skew

Figure 3

Whole‐genome based phylogenetic tree constructed using CVTree3 showing the phylogenetic relationship of strain D4M1T with reference species in the family Rhodobacteraceae. The tree constructed using protein sequences, and K = 6. Numbers in bracket stand for the numbers of strains used for phylogenetic analysis. Abbreviation: , Family; , Genus; , Species; , sTrain

General features of the complete genome sequence of strain D4M1T Circular maps of the chromosome and six plasmids of strain D4M1T. Plasmids pD4M1A, pD4M1B, pD4M1C, pD4M1D, pD4M1E, and pD4M1F are shown at 3, 6, 8, 8, 8, and 8 × scale, respectively, relative to the chromosome scale. From the outside to the center: protein‐coding genes on forward strand (color by COG categories), total genes on forward strand, total genes on reverse strand, protein‐coding genes on reverse strand, G + C content, and G + C skew Whole‐genome based phylogenetic tree constructed using CVTree3 showing the phylogenetic relationship of strain D4M1T with reference species in the family Rhodobacteraceae. The tree constructed using protein sequences, and K = 6. Numbers in bracket stand for the numbers of strains used for phylogenetic analysis. Abbreviation: , Family; , Genus; , Species; , sTrain

Morphology and physiology properties

Cells of strain D4M1T are Gram‐stain‐negative, oxidase‐ and catalase‐positive, aerobic, short rods (1.0–1.5 × 0.6–0.8 μm, Figure A2). Growth of the novel strain occurs between pH 5.0–8.0 (optimum 6.5), 10–45°C (optimum 37°C), and in the presence of 0.5%–8.0% (w/v) NaCl (optimum 3.0%). The novel strain contains poly‐β‐hydroxybutyrate (PHB) inside the cells. Strain D4M1T is piezophilic, with the optimum growth pressure of 10 MPa and tolerance up to 70 MPa (Figure A3). Anaerobic growth was not observed in LB medium nor in LB medium supplemented with 10 mmol/L of Na2SO4 or NaNO3. Results of carbon utilization (Biolog GEN III), API ZYM and 20NE tests are given in Table 2 and the species description below. Strain D4M1T is distinguishable from their closest relatives in physiological characteristics as shown in Table 2.
Figure A2

Transmission electron microscopy image of cell of strain D4M1T grown on MA medium at 35°C for 24 hr

Figure A3

Growth rate of strain D4M1T under different pressures at 35°C

Table 2

Differentiating characteristics between strain D4M1T and its close relatives

 1234
Growth at 10°C++
Optimum temperature37503537
Growth in 8% NaCl+++
Growth at pH 5+
G + C content (mol %)70.272.363.865.8
Enzyme activity
Lipase (C14)w++
α‐Chymotrypsin+
α‐Galactosidase++
β‐Galactosidase++
β‐Glucuronidase++
α‐Glucosidasew++
β‐Glucosidase++
Utilization of:
D‐Glucoseww
L‐Arabinosew++
D‐Mannosew+
D‐Mannitol + ++
D‐Maltose++
Potassium gluconate+++
Malic acidw++
Trisodium citrate++
D‐Galactose+++
3‐Methyl glucose+w
L‐Rhamnose+
D‐Sorbitol+++
D‐Aspartic acid++
Glycyl‐L‐proline++
L‐Arginine++
L‐Aspartic acid+++
L‐Pyroglutamic acid+
p‐Hydroxy‐phenylacetic acid++
D‐Lactic acid methyl ester+
L‐Lactic acid+++
Bromo‐succinic acid++
Tween 40+
α‐Hydroxy‐butyric acid++
Sensitive to:
Lincomycin+
Guanidine HCl+++

Strains: 1, strain D4M1T; 2, Oceanicella actignis DSM 22673T; 3, Thioclava electrotropha DSM 103712T; 4, Oceanibium sediminis MCCC 1H00233T. All data were experimentally determined in this study under the same conditions. Characteristics are scored as: +, positive; ‐, negative; w, weakly positive.

Differentiating characteristics between strain D4M1T and its close relatives Strains: 1, strain D4M1T; 2, Oceanicella actignis DSM 22673T; 3, Thioclava electrotropha DSM 103712T; 4, Oceanibium sediminis MCCC 1H00233T. All data were experimentally determined in this study under the same conditions. Characteristics are scored as: +, positive; ‐, negative; w, weakly positive.

Fatty acids, polar lipids, and quinone composition

The predominant fatty acid of strain D4M1T was summed feature 8 (41.7%, C18:1 ω7c/C18:1 ω6c) and C16:0 (36.9%) (Table A1). There were obvious differences in fatty acid profile between strain D4M1T and reference strains DSM 22673T and DSM 103712T. C18:1 ω7c/C18:1 ω6c were present in a much higher amount in reference strains DSM 22673T and DSM 103712T than in strain D4M1T, but the amount of C16:0 was much lower in the reference strains than in strain D4M1T.
Table A1

Fatty acid contents of strain D4M1T and closely related species

Fatty acids123
C10:0 3‐OH1.9
iso‐C11:0 3‐OH1.6
iso‐C12:0 1.30.20.2
C12:0 0.2
Summed feature 23.72.5
Summed feature 31.70.22.0
C16:0 36.94.02.4
C17:1 ω7c 0.8
C17:1 ω8c 1.00.2
C17:0 2.51.4
Summed feature 841.765.182.7
C18:0 7.510.06.0
C18:1 ω7c 11‐methyl3.510.20.6
C18:0 3‐OH2.90.4

Taxa: 1, strain D4M1T; 2, Oceanicella actignis LMG 25334T; 3, Thioclava electrotropha DSM 103712T; data of all strains were from this study under the same condition. Values are percentages of total fatty acids; —, not detected. *Summed features represent groups of two or three fatty acids which could not be separated by GLC with the MIDI system. Summed feature 2, C14:0 3‐OH/iso‐C16:1 I; summed feature 3, C16:1 ω7c/ω6c; summed feature 8, C18:1 ω7c/ω6c

The major isoprenoid quinone of strain D4M1T was ubiquinone 10 (Q‐10), which was the same as its related taxa in the family Rhodobacteraceae (Albuquerque et al., 2012; Y. Q. Chang, Meng, Du, & Du, 2019; Lai et al., 2014). The polar lipids of strain D4M1T consisted of phosphatidylglycerol (PG), phosphatidylethanolamine (PE), an unidentified aminophospholipid (PN), an unidentified glycolipid (GL), and several unidentified phospholipids (PL) as shown in Figure A4, which were similar to those of reference strains DSM 22673T and DSM 103712T, except some minor differences in unidentified phospholipids.
Figure A4

Polar lipids of strain D4M1T (a), Oceanicella actignis LMG 25334T (b) and Thioclava electrotropha DSM 103712T (c) at the optimum growth conditions. AL, aminolipid; GL, glycolipid; PE, phosphatidylethanolamine; PG, phosphatidylglycerol; PL, phospholipid; PN, aminophospholipid

Genome annotation and analysis

The genome was shown to encode 4,942 predicted genes including 4,855 protein‐coding genes, 12 rRNAs (four 5S rRNA, four 16S rRNA, and four 23S rRNA), 57 tRNAs, and 9 ncRNAs. Complete genome analysis revealed that the 4,855 protein‐coding genes constituted 98.2% of the total genes in the genome, but only 79.3% were predicted with functions. Furthermore, there were 4,057 genes (82.1%) assigned to 24 different clusters of orthologous groups (COGs, Table A2), 1,489 genes (30.1%) connected to KEGG pathways, and 1,106 genes (22.4%) connected to MetaCyc pathways.
Table A2

COG categories of the predicted W43T genes

COG categoriesCodeGene countPercent (%)
Amino acid transport and metabolismE64613.36
Carbohydrate transport and metabolismG3346.91
Cell cycle control, cell division, chromosome partitioningD440.91
Cell motilityN651.34
Cell wall/membrane/envelope biogenesisM2194.53
Chromatin structure and dynamicsB50.10
Coenzyme transport and metabolismH2134.40
CytoskeletonZ10.02
Defense mechanismsV931.92
Energy production and conversionC2795.77
Extracellular structuresW50.10
Function unknownS2615.40
General function prediction onlyR54211.21
Inorganic ion transport and metabolismP3066.33
Intracellular trafficking, secretion, and vesicular transportU581.20
Lipid transport and metabolismI2545.25
Mobilome: prophages, transposonsX521.08
Nucleotide transport and metabolismF1062.19
Posttranslational modification, protein turnover, chaperonesO1753.62
Replication, recombination, and repairL1342.77
Secondary metabolites biosynthesis, transport, and catabolismQ2254.65
Signal transduction mechanismsT1933.99
TranscriptionK4078.42
Translation, ribosomal structure, and biogenesisJ2194.53
Analysis of the complete genome indicated the presence of different genes that are most likely linked to life at high pressure. Microbes are thought to preserve membrane fluidization and functionality at high pressure and low temperature in the deep sea by increasing the proportion of unsaturated fatty acids in their membrane lipids (Cao et al., 2015; Simonato et al., 2006). Strain D4M1T contains high proportions of monounsaturated fatty acids, summed feature 8 (41.7%, C18:1 ω7c/C18:1 ω6c), probably for improving membrane piezo‐adaptation. Genomic analysis showed the presence of thirty‐seven genes involved in biosynthesis of unsaturated fatty acids, including four fatty acid desaturase genes (Table A3). Pressure‐induced chaperones proposed to help in maintaining protein folding (Oger & Jebbar, 2010) were also encoded adjacent to the unsaturated fatty acids biosynthesis genes in D4M1T genome, including the OmpH which was thought to function as a nutrient transporter in nutrient‐limited deep sea (Table A3).
Table A3

Genes in the D4M1T genome involved in high‐pressure adaptation

IMG gene OIDLocus tagProtein
Biosynthesis of unsaturated fatty acids
2828513318Ga0392526_2533‐oxoacyl‐[acyl‐carrier protein] reductase
2828513436Ga0392526_371Glycerol‐3‐phosphate acyltransferase PlsY
2828513500Ga0392526_4361‐acyl‐sn‐glycerol‐3‐phosphate acyltransferase
2828513541Ga0392526_477acyl‐CoA thioesterase‐1
2828513884Ga0392526_8203‐oxoacyl‐[acyl‐carrier protein] reductase
2828514031Ga0392526_9673‐oxoacyl‐[acyl‐carrier protein] reductase
2828514243Ga0392526_11793‐oxoacyl‐[acyl‐carrier protein] reductase
2828514304Ga0392526_1240fatty acid desaturase
2828514475Ga0392526_1411acyl transferase domain‐containing protein/NADPH:quinone reductase‐like Zn‐dependent oxidoreductase/acyl carrier protein
2828514527Ga0392526_1463enoyl‐[acyl‐carrier protein] reductase I
2828514528Ga0392526_14643‐oxoacyl‐[acyl‐carrier‐protein] synthase‐1
2828514529Ga0392526_14653‐hydroxyacyl‐[acyl‐carrier protein] dehydratase/trans‐2‐decenoyl‐[acyl‐carrier protein] isomerase
2828514544Ga0392526_1480acyl‐CoA thioesterase YciA
2828514651Ga0392526_1587fatty acid desaturase
2828514809Ga0392526_1745fatty acid desaturase
2828515056Ga0392526_1992enoyl‐CoA hydratase
2828515178Ga0392526_21141‐acyl‐sn‐glycerol‐3‐phosphate acyltransferase
2828515283Ga0392526_22193‐hydroxyacyl‐CoA dehydrogenase/enoyl‐CoA hydratase/3‐hydroxybutyryl‐CoA epimerase
2828515303Ga0392526_22391‐acyl‐sn‐glycerol‐3‐phosphate acyltransferase
2828515340Ga0392526_2276long‐chain acyl‐CoA synthetase
2828515835Ga0392526_27713‐hydroxyacyl‐[acyl‐carrier‐protein] dehydratase
2828515979Ga0392526_29153‐oxoacyl‐[acyl‐carrier protein] reductase
2828516231Ga0392526_31673‐oxoacyl‐[acyl‐carrier‐protein] synthase II
2828516233Ga0392526_31693‐oxoacyl‐[acyl‐carrier protein] reductase
2828516304Ga0392526_32403‐oxoacyl‐[acyl‐carrier protein] reductase
2828516395Ga0392526_33313‐oxoacyl‐[acyl‐carrier protein] reductase
2828516464Ga0392526_34003‐oxoacyl‐[acyl‐carrier protein] reductase
2828516468Ga0392526_34043‐oxoacyl‐[acyl‐carrier protein] reductase
2828516565Ga0392526_3501Glycerol‐3‐phosphate acyltransferase PlsX
2828516609Ga0392526_3545enoyl‐[acyl‐carrier protein] reductase I
2828516730Ga0392526_3666enoyl‐CoA hydratase
2828516791Ga0392526_37273‐oxoacyl‐[acyl‐carrier protein] reductase
2828516807Ga0392526_37433‐oxoacyl‐[acyl‐carrier protein] reductase
2828516926Ga0392526_3862enoyl‐CoA hydratase
2828517203Ga0392526_4139enoyl‐[acyl‐carrier protein] reductase I
2828517211Ga0392526_4147fatty acid desaturase
2828517574Ga0392526_45103‐oxoacyl‐[acyl‐carrier protein] reductase
Chaperone
2828513714Ga0392526_650molecular chaperone DnaK
2828513716Ga0392526_652molecular chaperone DnaJ
2828515281Ga0392526_2217Zn‐dependent protease with chaperone function
2828515832Ga0392526_2768regulator of sigma E protease
2828515833Ga0392526_2769outer membrane protein insertion porin family
2828515834Ga0392526_2770Skp family chaperone for outer membrane proteins, OmpH
2828516688Ga0392526_3624HSP20 family molecular chaperone IbpA
2828516690Ga0392526_3626molecular chaperone Hsp33
Respiratory chain
2828513683Ga0392526_619cytochrome d ubiquinol oxidase subunit I
2828513684Ga0392526_620cytochrome d ubiquinol oxidase subunit II
2828515783Ga0392526_2719cbb3‐type cytochrome oxidase maturation protein
2828515787Ga0392526_2723cytochrome c oxidase accessory protein FixG
2828515788Ga0392526_2724uncharacterized membrane protein
2828515789Ga0392526_2725cytochrome c oxidase cbb3‐type subunit 3
2828515790Ga0392526_2726cytochrome c oxidase cbb3‐type subunit 4
2828515791Ga0392526_2727cytochrome c oxidase cbb3‐type subunit 2
2828515792Ga0392526_2728cytochrome c oxidase cbb3‐type subunit 1
F1F0 ATP‐synthase
2828514969Ga0392526_1905F1F0 ATP‐synthase subunit delta
2828514970Ga0392526_1906F1F0 ATP‐synthase subunit alpha
2828514971Ga0392526_1907F1F0 ATP‐synthase subunit gamma
2828514972Ga0392526_1908F1F0 ATP‐synthase subunit beta
2828514973Ga0392526_1909F1F0 ATP‐synthase subunit epsilon
2828515088Ga0392526_2024F1F0 ATP‐synthase, membrane subunit b
2828515089Ga0392526_2025F1F0 ATP‐synthase, membrane subunit b
2828515090Ga0392526_2026F1F0 ATP‐synthase, membrane subunit c
2828515091Ga0392526_2027F1F0 ATP‐synthase, membrane subunit a
2828515092Ga0392526_2028F1F0 ATP‐synthaseprotein I
2828516954Ga0392526_3890F1F0 ATP‐synthase subunit beta
2828516955Ga0392526_3891F1F0 ATP‐synthase subunit epsilon
2828516956Ga0392526_3892F1F0 ATP‐synthaseprotein I
2828516957Ga0392526_3893F1F0 ATP‐synthase subunit 2
2828516958Ga0392526_3894F1F0 ATP‐synthase subunit a
2828516959Ga0392526_3895F1F0 ATP‐synthase subunit c
2828516960Ga0392526_3896F1F0 ATP‐synthase subunit b
2828516961Ga0392526_3897F1F0 ATP‐synthase subunit alpha
2828516962Ga0392526_3898F1F0 ATP‐synthase subunit gamma
PHA/PHB synthesis
2828513971Ga0392526_9073‐hydroxybutyrate dehydrogenase
2828514023Ga0392526_959putative acetyltransferase
2828514219Ga0392526_1155hydroxymethylglutaryl‐CoA lyase
2828514509Ga0392526_1445apolipoprotein N‐acyltransferase
2828514635Ga0392526_1571polyhydroxyalkanoate synthase
2828514700Ga0392526_1636polyhydroxybutyrate depolymerase
2828514800Ga0392526_1736poly(3‐hydroxybutyrate) depolymerase
2828514849Ga0392526_1785polyhydroxyalkanoate depolymerase
2828514923Ga0392526_18593‐hydroxyacyl‐CoA dehydrogenase
2828515161Ga0392526_2097acetoacetyl‐CoA reductase
2828515162Ga0392526_2098acetyl‐CoA C‐acetyltransferase
2828515163Ga0392526_2099polyhydroxyalkanoate synthase
2828515164Ga0392526_2100polyhydroxyalkanoate synthesis repressor PhaR
2828515217Ga0392526_21533‐hydroxybutyryl‐CoA dehydrogenase
2828515283Ga0392526_22193‐hydroxyacyl‐CoA dehydrogenase/enoyl‐CoA hydratase/3‐hydroxybutyryl‐CoA epimerase
2828515284Ga0392526_2220acetyl‐CoA C‐acetyltransferase
2828515305Ga0392526_22413‐hydroxybutyryl‐CoA dehydratase
2828515724Ga0392526_26603‐hydroxybutyryl‐CoA dehydrogenase
2828516037Ga0392526_29733‐oxoacyl‐(acyl‐carrier‐protein) synthase/nodulation protein E
2828516295Ga0392526_3231hydroxymethylglutaryl‐CoA lyase
2828516711Ga0392526_3647putative acetyltransferase
2828516927Ga0392526_38633‐hydroxybutyryl‐CoA dehydrogenase
2828517202Ga0392526_4138polyhydroxyalkanoate synthase
2828517335Ga0392526_4271acetyl‐CoA C‐acetyltransferase
2828517488Ga0392526_4424hydroxymethylglutaryl‐CoA lyase
2828517899Ga0392526_4835apolipoprotein N‐acyltransferase
2828517938Ga0392526_4874acetyl‐CoA C‐acetyltransferase
Glutamine synthesis and regulation
2828513735Ga0392526_671glutamine synthetase
2828514055Ga0392526_991glutamine synthetase
2828514780Ga0392526_1716glutamine synthetase
2828514889Ga0392526_1825glutamine synthetase
2828515862Ga0392526_2798glutamine synthetase
2828516007Ga0392526_2943ntrX two‐component system, NtrC family, nitrogen regulation response regulator NtrX
2828516008Ga0392526_2944ntrY two‐component system, NtrC family, nitrogen regulation sensor histidine kinase NtrY
2828516009Ga0392526_2945ntrC two‐component system, NtrC family, nitrogen regulation response regulator GlnG
2828516010Ga0392526_2946ntrB two‐component system, NtrC family, nitrogen regulation sensor histidine kinase GlnL
2828516194Ga0392526_3130glutamine synthetase
Betaine and trehalose biosynthesis and transport
2828513193Ga0392526_128choline dehydrogenase
2828513583Ga0392526_519choline dehydrogenase
2828513584Ga0392526_520choline‐sulfatase
2828513585Ga0392526_521TetR/AcrR family transcriptional repressor of bet genes
2828513586Ga0392526_522glycine betaine/proline transport system substrate‐binding protein
2828513587Ga0392526_523glycine betaine/proline transport system permease protein
2828513588Ga0392526_524glycine betaine/proline transport system ATP‐binding protein
2828513835Ga0392526_771glycine betaine/proline transport system substrate‐binding protein
2828513836Ga0392526_772drug/metabolite transporter (DMT)‐like permease
2828513837Ga0392526_773DNA‐binding Lrp family transcriptional regulator
2828513838Ga0392526_774DNA‐binding HxlR family transcriptional regulator
2828514400Ga0392526_1336choline monooxygenase
2828515533Ga0392526_2469BCCT family betaine/carnitine transporter
2828516142Ga0392526_3078glycine betaine/proline transport system substrate‐binding protein
2828516143Ga0392526_3079glycine betaine/proline transport system permease protein
2828516144Ga0392526_3080glycine betaine/proline transport system ATP‐binding protein
2828516539Ga0392526_3475choline dehydrogenase
2828514833Ga0392526_1769Acetyltransferase (isoleucine patch superfamily)
2828515886Ga0392526_2822glucosylglycerol‐phosphate synthase
2828516592Ga0392526_3528trehalose/maltose transport system substrate‐binding protein
2828516593Ga0392526_3529trehalose/maltose transport system permease protein
2828516594Ga0392526_3530trehalose/maltose transport system permease protein
2828516595Ga0392526_3531ABC‐type sugar transport system ATPase subunit
2828517438Ga0392526_4374trehalose 6‐phosphate synthase
2828517439Ga0392526_4375trehalose 6‐phosphate phosphatase
2828517440Ga0392526_4376(1‐>4)‐alpha‐D‐glucan 1‐alpha‐D‐glucosylmutase
2828517441Ga0392526_43774‐alpha‐glucanotransferase
2828517442Ga0392526_4378maltooligosyltrehalose trehalohydrolase
2828517443Ga0392526_4379glycogen operon protein
2828517444Ga0392526_43801,4‐alpha‐glucan branching enzyme
2828517445Ga0392526_4381maltose alpha‐D‐glucosyltransferase/alpha‐amylase
2828517644Ga0392526_4580multiple sugar transport system ATP‐binding protein
2828517645Ga0392526_4581multiple sugar transport system permease protein
2828517646Ga0392526_4582multiple sugar transport system permease protein
2828517647Ga0392526_4583multiple sugar transport system substrate‐binding protein
2828517648Ga0392526_4584LacI family transcriptional regulator
Cold and heat shock proteins
2828513475Ga0392526_411CspA family cold shock protein
2828513528Ga0392526_464ribosome‐associated heat shock protein Hsp15
2828513634Ga0392526_570heat shock protein HspQ
2828514209Ga0392526_1145heat shock gene repressor HrcA
2828514210Ga0392526_1146molecular chaperone GrpE (heat shock protein)
2828514746Ga0392526_1682heat shock protein HtpX
2828514758Ga0392526_1694CspA family cold shock protein
2828515042Ga0392526_1978CspA family cold shock protein
2828515213Ga0392526_2149heat shock protein HslJ
2828516605Ga0392526_3541cold shock CspA family protein
It is well known that many piezophiles change their respiratory chains in order to adapt to pressure (Oger & Jebbar, 2010). The genome was found to contain genes encoding cytochrome bd‐type quinol oxidase and cytochrome cbb protein complex (Table A3), which were involved in specific piezo‐adaptations in respiratory chain (Chikuma, Kasahara, Kato, & Tamegai, 2007; Qureshi, Kato, & Horikoshi, 1998). F1F0 ATP‐synthase was shown to facilitate energy‐yielding processes in high‐pressure adaptation (Souza, Creczynski‐Pasa, Scofano, Graber, & Mignaco, 2004). It was remarkable that two sets of the F1F0 ATP‐synthase genes were identified in the genome of strain D4M1T (Table A3). Deep‐sea bacteria were also found to accumulate protein‐stabilizing solutes at high pressure, such as piezolytes β‐hydroxybutyrate (β‐HB) and oligomers of β‐HB (Martin, Bartlett, & Roberts, 2002). PHB was detected in the cells of strain D4M1T in this study, and genes that encoded the enzymes required for β‐HB and PHB synthesis were present in the genome, including 1 β‐HB dehydrogenase and 3 polyhydroxyalkanoate synthase genes (Table A3). The PHB inside the cells could also serve as intracellular carbon and energy reserves, which have been linked to pressure adaptation (Martin et al., 2002; Methe et al., 2005). Genes involved in biosynthesis and transport of compatible solutes, such as glycine betaine, were also identified in the genome, including genes encoding choline dehydrogenase and transcriptional repressor BetI (Table A3). It was suggested that trehalose protects proteins and cellular membranes from inactivation or denaturation caused by a variety of stress conditions, including high hydrostatic pressure (Simonato et al., 2006). Nineteen genes in the genome were predicted to encode trehalose biosynthesis and trehalose‐specific transporters (Table A3), which were probably involved in pressure adaptation. Additionally, the genome of D4M1T has six copies of glnA, including the counterpart of the pressure‐upregulated glnA (IMG Gene OID: 2828515862) in piezophile Shewanella violacea DSS12 (Ikegami, Nakasone, Kato, Nakamura, et al., 2000). Furthermore, the pressure‐regulated regulator ntrBC in S. violacea DSS12 was also identified in the genome of D4M1T (Table A3), which was predicted to play a role in activation of transcription of pressure‐regulated promoters (Ikegami, Nakasone, Kato, Usami, & Horikoshi, 2000). The increasing number of rRNA operons in a bacterial genome was previously proposed to represent a strategy for adapting to specific selective pressures from the environment (Klappenbach, Dunbar, & Schmidt, 2000). The genome of the strain was found to contain four rRNA operons (Table 1), which may correlate with the adaptation to the deep‐sea environment. Pressure is thermodynamically coupled to temperature. One “universal” response to environmental pressures is the biosynthesis of stress proteins (Kültz, 2005). The genome encoded 6 heat shock protein genes and 4 cold shock protein genes (Table A3), which were previously reported to be induced when exposed to high pressure (Simonato et al., 2006). Our results suggest that hydrostatic pressure is an important environmental stress that drives the adaptation of heat shock protein genes and cold shock protein genes in deep‐sea microorganisms. The genome analysis revealed insights into the piezophilic lifestyle of the novel isolate and provided a reference for further phylogenomic, comparative genomic, and functional studies of the relative species in the deep ocean. However, further specific experiments need to be addressed in the future to find out the precise function of the genes involved in high‐pressure adaptation and the molecular adaptation mechanisms.

CONCLUSION

Strain D4M1T exhibits the typical characteristics of the family Rhodobacteraceae, but it is also distinguishable from its closest relatives in the phylogenetic analysis of 16S rRNA gene sequence, the phylogenomic analysis based on whole‐genome protein sequences, the fatty acids profiles, the enzyme activities, the carbon utilization, the G + C contents, and the low 16S rRNA gene sequence similarity (≤95.8%) to the type species of the closely related genera of the family Rhodobacteraceae. Therefore, from the polyphasic evidence, strain D4M1T represents a novel species of a novel genus for which the name Paraoceanicella profunda gen. nov., sp. nov. is proposed.

Description of Paraoceanicella gen. nov

Paraoceanicella (Pa.ra.o.ce.a.ni.cel'la. Gr. prep. para, beside, alongside of; N. L. fem. n. Oceanicella, a bacterial generic name; N. L. fem. n. Paraoceanicella, a genus adjacent to Oceanicella). Cells are aerobic, Gram‐stain‐negative, oxidase‐ and catalase‐positive, short rods (1.0–1.5 × 0.6–0.8 μm). The G + C content of the genomic DNA of the type strain of the type species is 70.2 mol%. The predominant fatty acids are summed feature 8 (C18:1 ω7c/C18:1 ω6c), and C16:0. PG, PE, and an unidentified PN are the predominant polar lipids. Q‐10 is the major isoprenoid quinone. The type species is Paraoceanicella profunda.

Description of Paraoceanicella profunda sp. nov

Paraoceanicella profunda (pro.fun'da. L. adj. profunda from the deep). Cells are aerobic, Gram‐stain‐negative, oxidase‐ and catalase‐positive, short rods (1.0–1.5 × 0.6–0.8 μm). Growth occurs at salinities from 0.5% to 8.0% (optimum 3.0%), from pH 5.0 to 8.0 (optimum 6.5), and at temperatures between 10 and 45°C (optimum 37°C). Anaerobic growth does not occur in LB medium nor in LB medium supplemented with 10 mM of Na2SO4 or NaNO3. The optimum pressure for growth was 10 MPa with tolerance up to 70 MPa. Positive for nitrate reduction, alkaline phosphatase, esterase(C4), esterase lipase (C8), lipase (C14), leucine arylamidase, valine arylamidase, cystine arylamidase, α‐chymotrypsin, acid phosphatase, naphthol‐AS‐Bl‐phosphohydrolase, α‐glucosidase, arginine dihydrolase, gelatin hydrolysis and urease activities; negative for trypsin, α‐galactosidase, β‐galactosidase, β‐glucuronidase, β‐glucosidase, beta‐glucosidase (aesculin hydrolysis), N‐acetyl‐β‐glucosaminidase, α‐mannosidase, α‐fucosidase, indole production, or D‐glucose fermentation. Utilizes the following carbon sources: D‐glucose, L‐arabinose, D‐sorbitol, D‐mannitol, D‐arabitol, malic acid, potassium gluconate, D‐fructose, D‐fructose‐6‐PO4, D‐galactose, D‐fucose, L‐fucose, glycerol, L‐alanine, L‐glutamic acid, D‐galacturonic acid, L‐galactonic acid lactone, D‐gluconic acid, D‐glucuronic acid, glucuronamide, p‐hydroxy‐phenylacetic acid, methyl pyruvate, α‐keto‐glutaric acid, bromo‐succinic acid, γ‐amino‐butyric acid, β‐hydroxy‐D,L‐butyric acid, L‐serine, glucuronamide, quinic acid, D‐saccharic acid, L‐lactic acid, acetoacetic acid, propionic acid, and acetic acid. The predominant fatty acid is summed feature 8 (C18:1 ω7c/C18:1 ω6c) and C16:0. Q‐10 is the major isoprenoid quinone. The predominant polar lipids consist of PG, PE, and an unidentified PN. The G + C content of the genomic DNA is 70.2 mol%. The type strain D4M1T (=MCCC 1K03820T = KCTC 72285T) was cultured from a deep‐water sample obtained at a depth of 10,890 m of the Mariana Trench (142.4°E, 11.4°N; site MT). The 16S rRNA and genome sequences are submitted to GenBank under accession numbers MK909903 and CP040818–CP040824, respectively.

ETHICS STATEMENT

None required.

CONFLICT OF INTERESTS

None declared.

AUTHOR CONTRIBUTIONS

JC supervised the project. PL, WD, and QL carried out the experiments. LP and JC analyzed the data. PL, JC, and JF wrote the manuscript with support from RL, YW, LW, and ZX.
  41 in total

Review 1.  Molecular and evolutionary basis of the cellular stress response.

Authors:  Dietmar Kültz
Journal:  Annu Rev Physiol       Date:  2005       Impact factor: 19.318

2.  Solute accumulation in the deep-sea bacterium Photobacterium profundum.

Authors:  Deana Desmarais Martin; Douglas H Bartlett; Mary F Roberts
Journal:  Extremophiles       Date:  2002-09-07       Impact factor: 2.395

3.  MEGA5: molecular evolutionary genetics analysis using maximum likelihood, evolutionary distance, and maximum parsimony methods.

Authors:  Koichiro Tamura; Daniel Peterson; Nicholas Peterson; Glen Stecher; Masatoshi Nei; Sudhir Kumar
Journal:  Mol Biol Evol       Date:  2011-05-04       Impact factor: 16.240

Review 4.  Bacterial phylogeny based on comparative sequence analysis.

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Journal:  Electrophoresis       Date:  1998-04       Impact factor: 3.535

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Review 6.  Uniting the classification of cultured and uncultured bacteria and archaea using 16S rRNA gene sequences.

Authors:  Pablo Yarza; Pelin Yilmaz; Elmar Pruesse; Frank Oliver Glöckner; Wolfgang Ludwig; Karl-Heinz Schleifer; William B Whitman; Jean Euzéby; Rudolf Amann; Ramon Rosselló-Móra
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7.  Thiobacimonas profunda gen. nov., sp. nov., a member of the family Rhodobacteraceae isolated from deep-sea water.

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Journal:  Int J Syst Evol Microbiol       Date:  2015-10       Impact factor: 2.747

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10.  Introducing EzBioCloud: a taxonomically united database of 16S rRNA gene sequences and whole-genome assemblies.

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1.  Physiological and genomic features of Paraoceanicella profunda gen. nov., sp. nov., a novel piezophile isolated from deep seawater of the Mariana Trench.

Authors:  Ping Liu; Wanzhen Ding; Qiliang Lai; Rulong Liu; Yuli Wei; Li Wang; Zhe Xie; Junwei Cao; Jiasong Fang
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