| Literature DB >> 19701714 |
Melike Balk1, Hans G H J Heilig, Miriam H A van Eekert, Alfons J M Stams, Irene C Rijpstra, Jaap S Sinninghe-Damsté, Willem M de Vos, Servé W M Kengen.
Abstract
A novel anaerobic, thermophilic, Gram-positive, spore-forming, and sugar-fermenting bacterium (strain TLO) was isolated from a geothermal spring in Ayaş, Turkey. The cells were straight to curved rods, 0.4-0.6 microm in diameter and 3.5-10 microm in length. Spores were terminal and round. The temperature range for growth was 40-80 degrees C, with an optimum at 70 degrees C. The pH optimum was between 6.3 and 6.8. Strain TLO has the capability to ferment a wide variety of mono-, di-, and polysaccharides and proteinaceous substrates, producing mainly lactate, next to acetate, ethanol, alanine, H(2), and CO(2). Remarkably, the bacterium was able to grow in an atmosphere of up to 25% of CO as sole electron donor. CO oxidation was coupled to H(2) and CO(2) formation. The G + C content of the genomic DNA was 35.1 mol%. Based on 16S rRNA gene sequence analysis and the DNA-DNA hybridization data, this bacterium is most closely related to Thermoanaerobacter thermohydrosulfuricus and Thermoanaerobacter siderophilus (99% similarity for both). However, strain TLO differs from Thermoanaerobacter thermohydrosulfuricus in important aspects, such as CO-utilization and lipid composition. These differences led us to propose that strain TLO represents a subspecies of Thermoanaerobacter thermohydrosulfuricus, and we therefore name it Thermoanaerobacter thermohydrosulfuricus subsp. carboxydovorans.Entities:
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Year: 2009 PMID: 19701714 PMCID: PMC2767516 DOI: 10.1007/s00792-009-0276-9
Source DB: PubMed Journal: Extremophiles ISSN: 1431-0651 Impact factor: 2.395
Fig. 1Dendrogram showing the position of strain TLO among the members of the order Thermoanaerobacteriales and related bacteria. Phylogenetic analysis based on 16S rRNA gene sequences available from GenBank data bases (accession numbers are given in parentheses). The neighbor-joining tree was reconstructed from distance matrices; bootstrap values (1000 replication) greater than 50% are listed at branching points. Bar evolutionary distance of 0.10
Fig. 2Phase-contrast micrograph of strain TLO (a). Elemental sulfur deposits in thiosulfate supplemented medium (b). Bar 2.5 μm
Fig. 3CO conversion by strain TLO performed at 65°C and shaken at 100 rpm with CO as sole substrate. The results represent the average of duplicate experiments. Carbon monoxide (filled diamond), hydrogen (filled circle) and OD (open triangle)
Lipid composition (in % of total quantified lipids) of strain TLO in comparison with phylogenetically closely related species
| Lipids | Strain TLO |
|
| |||
|---|---|---|---|---|---|---|
| FLF | BLF | FLF | BLF | FLF | BLF | |
| Summed concentration (mg/g dry weight) | 6.7 | 2.0 | 17.4 | 2.9 | 8.6 | 0.6 |
|
| 4 | 1 | n.d. | n.d. | 7 | 2 |
| Iso-C15 FA | 39 | 25 | 81 | 60 | 3 | 40 |
| Anteiso-C15 FA | 2 | 2 | 2 | 2 | 0 | 8 |
|
| 5 | 1 | 2 | 2 | 19 | 5 |
| Iso-C17 FA | 16 | 5 | 12 | 22 | 66 | 16 |
| Anteiso-C17 FA | 2 | 1 | 1 | 2 | 5 | 4 |
|
| n.d. | n.d. | n.d. | n.d. | n.d. | 1 |
| Iso-C15-OH | 10 | n.d. | 1 | n.d. | <1 | 3 |
|
| 7 | 1 | n.d. | n.d. | n.d. | 1 |
| Iso-C17-OH | 9 | 9 | 1 | n.d. | n.d. | n.d. |
| Anteiso-C17-OH | 4 | <1 | n.d. | n.d. | n.d. | n.d. |
|
| 2 | 50 | n.d. | 12 | n.d. | 20 |
|
| n.d. | 2 | n.d. | n.d. | n.d. | n.d. |
| 30-Hydroxy-13,16-dimethyl-triacontanoic acid | n.d. | 3 | n.d. | n.d. | n.d. | n.d. |
The strains were grown in glucose-containing bicarbonate-buffered (BM) medium at 65°C for 24 h
n.d. not detected, FA fatty acid, OH alcohol, FLF free lipid fraction, BLF bound lipid fraction
Phenotypic characteristics of strain TLO in comparison with phylogenetically closely related species
| Feature | Strain TLO |
|
|
|---|---|---|---|
| Source | Geothermal spring | Extraction juices of beet sugar factory | Hydrothermal vent |
| Gram reaction | + | V | + |
| Spores | + | + | + |
| Temperature range (oC) | 40–80 | 40–78 | 39–78 |
| Optimum temperature (°C) | 68–70 | 65–68 | 69–71 |
| pH range | 4.5–9 | 5–9 | 4.8–8.2 |
| Optimum pH | 6.3–6.8 | 6.9–7.5 | 6.3–6.5 |
| DNA G + C content (mol%) | 35.1 | 37.6 | 32 |
| Reduction of arsenate | + | +a | +a |
| Growth substrates | |||
| Ribose | + | + | NR |
| Mannitol | W | Wa | V |
| Starch | + | + | + |
| Pectin | + | + | NR |
| Xylan | + | + | – |
| Carboxymethylcellulose | W | + | – |
| CO (up to 25% v/v) | + | –a | –b |
Data for reference species were obtained from Klaushofer and Parkkinen (1965) and Slobodkin et al. (1999)
NR not reported, V variable, W weak
aTested in this report; b Data from Gavrilov et al. (2003)