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Non-contiguous finished genome sequence and description of Sulfurimonas hongkongensis sp. nov., a strictly anaerobic denitrifying, hydrogen- and sulfur-oxidizing chemolithoautotroph isolated from marine sediment


Here, we report a type strain AST-10 representing a novel species Sulfurimonas hongkongensis within Epsilonproteobacteria, which is involved in marine sedimentary sulfur oxidation and denitrification. Strain AST-10T (= DSM 22096T = JCM 18418T) was isolated from the coastal sediment at the Kai Tak Approach Channel connected to Victoria Harbour in Hong Kong. It grew chemolithoautotrophically using thiosulfate, sulfide or hydrogen as the sole electron donor and nitrate as the electron acceptor under anoxic conditions. It was rod-shaped and grew at 15–35°C (optimum at 30°C), pH 6.5–8.5 (optimum at 7.0–7.5), and 10–60 g L−1 NaCl (optimum at 30 g L−1). Genome sequencing and annotation of strain AST-10T showed a 2,302,023 bp genome size, with 34.9% GC content, 2,290 protein-coding genes, and 42 RNA genes, including 3 rRNA genes.


The genus Sulfurimonas was formally proposed in 2003, and included only one species, Sulfurimonas autotrophica OK10T, at that time [1]. Since then, several novel species have been identified, such as Sulfurimonas paralvinellae GO25T [2], Sulfurimonas denitrificans DSM 1251T (reclassified, previously known as Thiomicrospira denitrificans) [2], and Sulfurimonas gotlandica GD1T [3]. Here, we report another novel species, Sulfurimonas hongkongensis AST-10T, isolated from coastal sediment, and describe its features, together with the genome sequencing and annotation.

Currently, all known Sulfurimonas members were isolated from marine sediments except for strain GD1 from deep seawater [4]. The most widely shared feature of Sulfurimonas members is chemolithoautotrophy; strains can grow by oxidizing hydrogen gas, elemental sulfur, hydrogen sulfide, or thiosulfate [17]. In our previous studies, anoxic sulfur-oxidizing bacteria were demonstrated to dominate the nitrate induced marine sediment remediation process [810]. Phylogenetic analysis based on 16S rRNA genes showed that Epsilonproteobacteria closely related to S. denitrificans constituted the major bacterial population during such remediation of the sediment at Kai Tak Approach Channel, Hong Kong, China. Strain AST-10T was isolated from the sediment and named Sulfurimonas hongkongensis sp. nov., based on its unique physiological and phylogenetic characteristics.

Classification and features

Sediment was collected 10–50 cm below the seawater/sediment interface at the Kai Tak Approach Channel connected to Victoria Harbor in Hong Kong, China. Sewage and industrial effluent had been discharged there for decades until the installation of a new sewage collection system in the late 1990s. The long lasting sulfate-reducing conditions resulted in a high sulfide concentration in the sediment, where an AVS (Acid-Volatile Sulfide) of 198 µmol g−1 had been measured [8]. The pore water after centrifugation at 4,000 rpm for 15 min had a pH of 7.89 and a salinity of 2.9%.

Enrichments were prepared by adding 20 g of wet sediment (32.0% dry matter) to serum bottles containing 70 mL of sterilized seawater, purged with N2 and incubated for at least 24 h at room temperature. Potassium nitrate (1 g L−1) and sodium phosphate, monobasic (0.1 mmol L−1), were then added from sterilized stock solutions. The bottles were incubated at 28°C in a water bath for 72 h. The enrichments were plated onto agar plates of DSM113-S medium, a salinity modified version of DM113 medium that is recommended by DSMZ for nitrate-reducing and sulfide-oxidizing bacteria. One liter of DSM113-S contained: KH2PO4 (2.0 g), KNO3 (4.0 g), NH4Cl (1.0 g), MgSO4·7H2O (0.8 g), Na2S2O3·5H2O (5.0 g), NaHCO3 (1.0 g), FeSO4·7H2O (2.0 mg), NaCl (25.0 g) and 2 ml of trace element solution SL-4. Solid media contained 1.5% bacterial agar from Difco. All media were sterilized by autoclaving and cooled under N2 atmosphere. Colonies formed on plates were picked and further purified by re-streaking single colonies on agar plates for more than 20 rounds (4–10 d round−1). A colony isolated and purified from the above process was defined as strain AST-10T.

The 16S phylogenetic tree shown in Figure 1 indicated that strain AST-1T is a member of the genus Sulfurimonas, (Table 1). An online BLAST query in NCBI using the 16S rRNA gene sequence from strain AST-1T showed a relatively low identity to all currently identified Sulfurimonas species, including S. denitrificans DSM 1251T (97% identity), S. gotlandica GD1T (95% identity), S. autotrophica OK10T (95% identity), and S. paralvinellae GO25T (94% identity). Using the commonly accepted criterion of a 97% 16S rDNA sequence similarity cut-off for defining species [19,20], strain AST-10T could accordingly be identified as a novel species within the genus Sulfurimonas.

Figure 1.

Phylogenetic tree highlighting the position of Sulfurimonas hongkongensis relative to the other species within the Helicobacteriaceae. The neighbor-joining tree was constructed using MEGA 5.05 and tested with 1,000 bootstrap replicates. Bootstrap values over 50% are shown and the scale bar 0.02 represents 2% nucleotide substitution. All reference sequences can be exactly searched and retrieved from NCBI GenBank based on the full name of each strain.

Table 1. Classification and general features of Sulfurimonas hongkongensis AST-10 based on the MIGS recommendations [11]

Cell morphology was examined by Scanning Electron Microscopy (SEM). As shown in Figure 2, the cells of AST-10T were rod-shaped, 0.2–0.4 µm in diameter, and 0.5–1.2 µm in length. On solid medium, AST-10T grew and formed small, white, transparent, round shaped colonies with smooth boundaries.

Figure 2.

Scanning electron micrograph of Sulfurimonas hongkongensis AST-10T. The scale bar represents 1.0 µm.


Effects of temperature, pH, and salinity on the growth of strain AST-10T were investigated, showing that it grew at 15–35°C (optimum at 30°C), pH 6.5–8.5 (optimum at 7.0–7.5), and 10–60 g L−1 NaCl (optimum at 30 g L−1). The generation time of strain AST-10T under optimal conditions was tested as 6.1 h. It was significantly shorter than other species, such as S. paralvinellae GO25T and S. denitrificans DSM 1251T. The cell yield of strain AST-10T was 5.2 g dry weight per mole of S2O32−. This value is similar to that of its Epsilonproteobacterial relative S. denitrificans DSM 1251T (5.72 g), but only about one-half of the Betaproteobacterial Thiobacillus denitrificans (11.6 g). Such difference in growth efficiency might be attributed to the different pathways used for carbon fixation and metabolism.

To determine whether electron acceptors other than NO3 would sustain the growth of strain AST-10T, SO42−, NO2, Fe3+, and O2 were separately tested with S2O32− as the sole electron donor. No growth was observed using any of these electron acceptors. S2O32−, HS, and H2 can support the growth of strain AST-10T as electron donors, however, acetate, lactate, malate, formate, pyruvate, glucose, glycerol, and yeast extract cannot. Hence, strain AST-10T was a chemolithoautotroph, using NO3 as an electron acceptor and S2O32−, HS, or H2 as an electron donor. The time course of S2O32− oxidation and NO3 reduction during strain AST-10T growth was monitored. N2 was the dominant denitrification product, no accumulation of N2O and NO2 was detected, when it was cultivated using DSM113-S at 30°C and pH 7.5. Significant production of insoluble S0 occurred when it was cultured with an excess amount of S2O32− (molar ratio of S2O32−/NO3 > 2). SO42− became the dominant oxidation product under excess NO3 conditions (molar ratio of S2O32−/NO3 < 0.25). This was quite similar to the well-characterized strain Thiomicrospira CVO [21]. But for S. denitrificans DSM 1251T, no accumulation of insoluble S0 was observed even under a high molar ratio of S2O32−/NO3 [5].


Cellular fatty acid composition was analyzed using the cells grown in DSM113-S medium at 30°C in the late-exponential phase. The major cellular fatty acids of strain AST-10T were C14:0 (4.8%), C16:0 (32.8%), 2-OH C16:0 (9.5%), C16:1 (14.6%), C18:0 (16.9%), and C18:1 (19.2%). This composition was generally similar to those of S. paralvinellae GO25T and S. autotrophica OK10T. However, 2-OH C16:0 was a unique fatty acid, differentiating AST-10T from other species within the genus of Sulfurimonas.

Genome sequencing and annotation

Genome project history

The strain was selected for genome sequencing on the basis of its 16S rRNA gene-based phylogenetic position within the genus Sulfurimonas (Table 1). It is the first sequenced genome of Sulfurimonas hongkongensis sp. nov. A summary of the genome sequencing project information is shown in Table 2. The genome consists of 28 contigs, which has been deposited at DDBJ/EMBL/GenBank under accession number AUPZ00000000. The version described in the present study is the first version.

Table 2. Genome sequencing project information

Growth conditions and DNA isolation

As described above, the strain was grown in DSM113-S medium under anoxic condition with optimal growth at 30°C, pH7.0-7.5, and NaCl 30 g L−1. The genomic DNA used for shotgun sequencing was prepared by DSMZ.

Genome sequencing and assembly

The genome shotgun sequencing project was finished by BGI (Beijing Genomics Institute). Briefly, DNA was first mechanically fragmented with an enrichment size of 500 bp. Then the DNA fragmentation was gel purified and quality checked. The recycled DNA was used for shotgun library construction, which was finally sequenced on an Illumina HiSeq 2000 platform using the paired-end 150 bp sequencing strategy.

A total of 6,932,096,700 bp of raw sequence was obtained, which was assembled with CLC Genomics Workbench 6.0.2 using a word size of 40 bp. The draft genome was finally assembled into 28 contigs with a 2,302,023 bp genome size and more than 3,000 fold genome coverage (Table 3).

Table 3. Nucleotide content and gene count levels of the genome

Genome annotation

The draft genome was annotated by NCBI Prokaryotic Genome Annotation Pipeline (PGAP). Protein-coding genes with function prediction were calculated based on the PGAP result. The COGs (Clusters of Orthologous Groups) functional annotation was conducted by PRSBLAST search against COGs database with an E-value cutoff 1e-10 [22,23]. Pfam domains were annotated using HMMER 3.0 program on Pfam database with an E-value cutoff 1e-10 [24,25]. SignalP 4.1 Server was employed to analyze proteins with signal peptide [26]. TMHMM Server 2.0 was used to predict transmembrane helices in proteins [27].

Genome properties

The draft genome of Sulfurimonas hongkongensis AST-10T was assembled into 28 contigs with a total size of 2,302,023 bp and a GC content of 34.9%. 2,332 genes were annotated, 2,290 of which were protein-coding genes. The remaining 42 genes were RNA genes including 3 rRNA genes. A total of 1,146 of the protein-coding genes were assigned putative functions. The remaining 1,144 protein-coding genes were annotated as hypothetical proteins. The AST-10T genome properties and statistics are summarized in Tables 24 and Figure 3.

Figure 3.

Graphical circular map of the Sulfurimonas hongkongensis AST-10 genome. Seen from the outside to the inside: genes on forward strand, genes on reverse strand, GC content, GC skew. The graphical map was plotted on the CGview Server.

Table 4. Number of genes associated with the 25 general COG functional categories


Description of Sulfurimonas hongkongensis sp. nov.

Sulfurimonas hongkongensis (hong.kong.en’sis. N.L. fem. adj. hongkongensis pertaining to Hong Kong, the city where the type strain was isolated).

Strain AST-10T is rod-shaped with size of 0.2–0.4 µm × 0.5–1.2 µm. It is an obligate anaerobe and occurs singly. The temperature range for growth is 15–35°C, optimum at 30°C. The pH range for growth is 6.5–8.5, optimum at 7.0–7.5. The salinity range for growth is 10–60 g L−1, and optimum at 30 g L−1. Strictly chemolithoautotrophic growth occurs with H2, HS or S2O32− as an electron donor and with nitrate as an electron acceptor. Nitrate is reduced to N2, and reduced sulfur compounds are oxidized into S0 or SO42− (depending on molar ratio of S2O32−/NO3). The major cellular fatty acids are C14:0, C16:0, 2-OH C16:0, C16:1, C18:0, and C18:1, with C16:0 2-OH as a unique fatty acid different from other species in the genus Sulfurimonas.

The type strain AST-10T = DSM 2096T = JCM 18418T, was isolated from coastal sediment at the Kai Tak Approach Channel connected to Victoria Harbour in Hong Kong, China. The GC content of the genome is 34.9%. The genome sequence has been deposited at DDBJ/EMBL/GenBank under accession number AUPZ00000000.


  1. 1.

    Inagaki F, Takai K, Kobayashi H, Nealson KH, Horikoshi K. Sulfurimonas autotrophica gen. nov., sp. nov., a novel sulfur-oxidizing epsilonproteobacterium isolated from hydrothermal sediments in the Mid-Okinawa Trough. Int J Syst Evol Microbiol 2003; 53:1801–1805. PubMed

  2. 2.

    Takai K, Suzuki M, Nakagawa S, Miyazaki M, Suzuki Y, Inagaki F, Horikoshi K. Sulfurimonas paralvinellae sp. nov., a novel mesophilic, hydrogen- and sulfur-oxidizing chemolithoautotroph within the Epsilonproteobacteria isolated from a deep-sea hydrothermal vent polychaete nest, reclassification of Thiomicrospira denitrificans as Sulfurimonas denitrificans comb. nov. and emended description of the genus Sulfurimonas. Int J Syst Evol Microbiol 2006; 56:1725–1733. PubMed

  3. 3.

    Labrenz M, Grote J, Mammitzsch K, Boschker HT, Laue M, Jost G, Glaubitz S, Jurgens K. Sulfurimonas gotlandica sp. nov., a chemoautotrophic and psychrotolerant epsilonproteobacterium isolated from a pelagic Baltic Sea redoxcline, and an emended description of the genus Sulfurimonas. Int J Syst Evol Microbiol 2013; 63:4141–4148. PubMed

  4. 4.

    Grote J, Schott T, Bruckner CG, Glockner FO, Jost G, Teeling H, Labrenz M, Jurgens K. Genome and physiology of a model Epsilonproteobacterium responsible for sulfide detoxification in marine oxygen depletion zones. Proc Natl Acad Sci USA 2012; 109:506–510. PubMed

  5. 5.

    Sievert SM, Scott KM, Klotz MG, Chain PS, Hauser LJ, Hemp J, Hugler M, Land M, Lapidus A, Larimer FW, et al. Genome of the epsilonproteobacterial chemolithoautotroph Sulfurimonas denitrificans. Appl Environ Microbiol 2008; 74:1145–1156. PubMed

  6. 6.

    Sikorski J, Munk C, Lapidus A, Ngatchou Djao OD, Lucas S, Glavina Del Rio T, Nolan M, Tice H, Han C, Cheng JF, et al. Complete genome sequence of Sulfurimonas autotrophica type strain (OK10). Stand Genomic Sci 2010; 3:194–202. PubMed

  7. 7.

    Bruckner CG, Mammitzsch K, Jost G, Wendt J, Labrenz M, Jurgens K. Chemolithoautotrophic denitrification of Epsilonproteobacteria in marine pelagic redox gradients. Environ Microbiol 2013; 15:1505–1513. PubMed

  8. 8.

    Shao M, Zhang T, Fang HH. Autotrophic denitrification and its effect on metal speciation during marine sediment remediation. Water Res 2009; 43:2961–2968. PubMed

  9. 9.

    Zhang M, Zhang T, Shao MF, Fang HH. Autotrophic denitrification in nitrate-induced marine sediment remediation and Sulfurimonas denitrificans-like bacteria. Chemosphere 2009; 76:677–682. PubMed

  10. 10.

    Shao MF, Zhang T, Fang HH, Li X. The effect of nitrate concentration on sulfide-driven autotrophic denitrification in marine sediment. Chemosphere 2011; 83:1–6. PubMed

  11. 11.

    Field D, Garrity G, Gray T, Morrison N, Selengut J, Sterk P, Tatusova T, Thomson N, Allen MJ, Angiuoli SV, et al. The minimum information about a genome sequence (MIGS) specification. Nat Biotechnol 2008; 26:541–547. PubMed

  12. 12.

    Woese CR, Kandler O, Wheelis ML. Towards a natural system of organisms: proposal for the domains Archaea, Bacteria, and Eucarya. Proc Natl Acad Sci USA 1990; 87:4576–4579. PubMed

  13. 13.

    Garrity GM, Bell JA, Lilburn T. Phylum XIV. Proteobacteria phyl. nov. In: Garrity GM, Brenner DJ, Krieg NR, Staley JT (eds), Bergey’s Manual of Systematic Bacteriology, Second Edition, Volume 2, Part B, Springer, New York, 2005, p. 1.

  14. 14.

    Validation List No. 107. List of new names and new combinations previously effectively, but not validly, published. Int J Syst Evol Microbiol 2006; 56:1–6. PubMed

  15. 15.

    Garrity GM, Bell JA, Lilburn T. Class V. Epsilonproteobacteria class. nov. In: Garrity GM, Brenner DJ, Krieg NR, Staley JT (eds), Bergey’s Manual of Systematic Bacteriology, Second Edition, Volume 2, Part C, Springer, New York, 2005, p. 1145.

  16. 16.

    Garrity GM, Bell JA, Lilburn T. Order I. Campylobacterales ord. nov. In: Garrity GM, Brenner DJ, Krieg NR, Staley JT (eds), Bergey’s Manual of Systematic Bacteriology, Second Edition, Volume 2, Part C, Springer, New York, 2005, p. 1145.

  17. 17.

    Garrity GM, Bell JA, Lilburn T. Family II. Helicobacteraceae fam. nov. In: Garrity GM, Brenner DJ, Krieg NR, Staley JT (eds), Bergey’s Manual of Systematic Bacteriology, Second Edition, Volume 2, Part C, Springer, New York, 2005, p. 1168.

  18. 18.

    Ashburner M, Ball CA, Blake JA, Botstein D, Butler H, Cherry JM, Davis AP, Dolinski K, Dwight SS, Eppig JT, et al. Gene ontology: tool for the unification of biology. Nat Genet 2000; 25:25–29. PubMed

  19. 19.

    Stackebrandt E, Goebel BM. A Place for DNADNA Reassociation and 16s Ribosomal-RNA Sequence-Analysis in the Present Species Definition in Bacteriology. Int J Syst Bacteriol 1994; 44:846–849.

  20. 20.

    RossellóoMora R. Amann R. The species concept for prokaryotes. FEMS Microbiol Rev 2001; 25:39–67. PubMed

  21. 21.

    Gevertz D, Telang AJ, Voordouw G, Jenneman GE. Isolation and characterization of strains CVO and FWKO B, two novel nitrate-reducing, sulfide-oxidizing bacteria isolated from oil field brine. Appl Environ Microbiol 2000; 66:2491–2501. PubMed

  22. 22.

    Tatusov RL, Galperin MY, Natale DA, Koonin EV. The COG database: a tool for genome-scale analysis of protein functions and evolution. Nucleic Acids Res 2000; 28:33–36. PubMed

  23. 23.

    Wu S, Zhu Z, Fu L, Niu B, Li W. WebMGA: a customizable web server for fast metagenomic sequence analysis. BMC Genomics 2011; 12:444. PubMed

  24. 24.

    Finn RD, Clements J, Eddy SR. HMMER web server: interactive sequence similarity searching. Nucleic Acids Res 2011; 39:W29–W37. PubMed

  25. 25.

    Punta M, Coggill PC, Eberhardt RY, Mistry J, Tate J, Boursnell C, Pang N, Forslund K, Ceric G, Clements J, et al. The Pfam protein families database. Nucleic Acids Res 2012; 40:D290–D301. PubMed

  26. 26.

    Petersen TN, Brunak S, von Heijne G, Nielsen H. SignalP 4.0: discriminating signal peptides from transmembrane regions. Nat Methods 2011; 8:785–786. PubMed

  27. 27.

    Krogh A, Larsson B, von Heijne G, Sonnhammer EL. Predicting transmembrane protein topology with a hidden Markov model: application to complete genomes. J Mol Biol 2001; 305:567–580. PubMed

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Dr. Lin Cai thanks The University of Hong Kong for the Postdoctoral Fellowship. This study was financially supported by the Research Grants Council of Hong Kong (HKU7201/11E).

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Correspondence to Tong Zhang.

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Cai, L., Shao, M. & Zhang, T. Non-contiguous finished genome sequence and description of Sulfurimonas hongkongensis sp. nov., a strictly anaerobic denitrifying, hydrogen- and sulfur-oxidizing chemolithoautotroph isolated from marine sediment. Stand in Genomic Sci 9, 1302–1310 (2014).

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  • Sulfurimonas hongkongensis
  • chemolithoautotroph
  • sulfur oxidation
  • denitrification
  • anaerobe
  • marine sediment
  • genome