| Literature DB >> 22294481 |
D Y Sorokin1, T P Tourova, A N Panteleeva, E N Kaparullina, G Muyzer.
Abstract
Anaerobic enrichments at pH 10, with pectin and polygalacturonates as substrates and inoculated with samples of sediments of hypersaline soda lakes from the Kulunda Steppe (Altai, Russia) demonstrated the potential for microbial pectin degradation up to soda-saturating conditions. The enrichments resulted in the isolation of six strains of obligately anaerobic fermentative bacteria, which represented a novel deep lineage within the order Clostridiales loosely associated with the family Lachnospiraceae. The isolates were rod-shaped and formed terminal round endospores. One of the striking features of the novel group is a very narrow substrate spectrum for growth, restricted to galacturonic acid and its polymers (e.g. pectin). Acetate and formate were the final fermentation products. Growth was possible in a pH range from 8 to 10.5, with an optimum at pH 9.5-10, and in a salinity range from 0.2 to 3.5 M Na(+). On the basis of unique phenotypic properties and distinct phylogeny, the pectinolytic isolates are proposed to be assigned to a new genus Natranaerovirga with two species N. hydrolytica (APP2(T)=DSM24176(T)=UNIQEM U806(T)) and N. pectinivora (AP3(T)=DSM24629(T)=UNIQEM U805(T)).Entities:
Year: 2012 PMID: 22294481 PMCID: PMC3325495 DOI: 10.1007/s00792-012-0431-6
Source DB: PubMed Journal: Extremophiles ISSN: 1431-0651 Impact factor: 2.395
Fig. 1Morphology of haloalkaliphilic pectinolytic isolates grown at pH 10. a Formation of clearance zones around colonies of strain AP3 during growth on polygalacturonate. Cell morphology (phase-contrast microphotographs): b strain APP2, c strain AP3, d strain APG1, e strain APG2, f strain APA1
Pectinolytic strains isolated from soda lakes and soda soils in Kulunda Steppe at pH 10
| Strain | Source | Enrichment conditions | DSM number | 16S rRNA gene accession number | |
|---|---|---|---|---|---|
| Total Na+ (M) | Polymer substrate | ||||
| APG1 | Lake sediments | 0.6 | Polygalacturonate | DSM24177 | GQ863486 |
| APG2 | Soda soils | 0.6 | Polygalacturonate | JN801139 | |
| APA1 | Lake sediments | 0.6 | Pectic acid | JN801138 | |
| APP2T | Lake sediments | 3.0 | Polypectate | DSM24176 | GQ863487 |
| AP2 | Lake sediments | 2.0 | Apple pectin | GQ922845 | |
| AP3T | Soda soils | 0.6 | Apple pectin | DSM24629 | GQ922846 |
Fig. 2Phylogenetic position of haloalkaliphilic pectinolytic strains within the order Clostridiales based on 16S rRNA gene sequence analysis. Tree topography and evolutionary distances are obtained by the neighbor-joining method with Jukes and Cantor distances. The scale bar represents 5 nucleotide changes per 100 nucleotides. The numbers on the nodes indicate bootstrap values above 70%
Comparison of the PLFA profiles of strains AP3 and APP2 and its closest relative (Cotta et al. 2009) and a typical clostridial species (Park et al. 2001)
| Fatty acid | AP3 | APP2 |
|
|
|---|---|---|---|---|
| 11:0 | 1.3 | |||
| 13:1 | 2.7 | |||
| 3-OH13:0 |
| |||
| 14:0 |
|
| ||
| a15 | 2.2 | 3.5 | ||
| 15:0 | 1.6 | 2.0 | 4.9 | |
| 15:0a | 1.8 | |||
| 16:1ω5 | 0.8 | 1.3 | ||
| 16:1ω7a | 1.4 | |||
| 16:1ω7c |
|
|
| |
| 16:1ω7t | 0.6 | |||
| 16:1ω9 | 2.4 | 3.7 | ||
| 16:1ω9a | 1.7 |
| ||
| 16:0 |
|
|
|
|
| 16:0a | 1.1 | |||
| a17 | 0.5 | |||
| 17:1 | 0.6 | 4.3 | ||
| i17:1 |
| |||
| 17:0 | 1.6 | |||
| 18:1ω9 | 0.8 | 1.4 |
| |
| 18:1ω7c |
| 3.7 |
|
|
| 18:1ω7t |
| |||
| 18:0 | 1.5 | 1.3 |
| |
| 18:1ω7a | 1.5 | 2.3 | ||
| 19:0 | 2.4 | 2.7 | ||
| 19cyc | 2.1 | 0.8 | ||
| 20:1 | 1.5 |
The dominant FA is in bold. Only the values above 0.5% are presented. The alkaliphilic strains were grown up to late logarithmic phase at 30°C, 0.6 M total Na+ and pH 10 with galacturonic acid as substrate
Fig. 3Influence of pH at 0.6 M Na+ (a) and of sodium carbonate at pH 10 (b) on anaerobic growth of strains AP3 (open circles) and APP2 (closed circles) with galacturonic acid. The experiments were performed in duplicates and the points represent the average values with standard deviations below 10%. The initial pH values were the following: 8.0 (final 8.1); 8.5 (final 8.5–8.7); 9.0 (final 9.0–9.18); 9.5 (final 9.53–9.66); 9.75 (final 9.73); 10.0 (final 9.91–10.02); 10.25 (final 10.18–10.20); 10.5 (final 10.37); 10.65 (final 10.48); 10.8 (final 10.59–10.61)
Phenotypic comparison of strains AP3T and APP2T with the members of the family Lachnospiraceae
| Characteristic | AP3T | APP2T |
|
|
|---|---|---|---|---|
| Cell size (µm) | 0.25–0.3 × 3–10 | 0.25–0.4 × 4–10 | 0.2–0.4 × 4.0–22.0 | 0.3–0.5 × 2–6 |
| Endospores | +, terminal, round | +, terminal, round | +, subterminal | +, subterminal, round |
| Motility | – | – | – | + |
| Major fermentation products | Acetate, formate | Acetate, formate | Acetate, formate, succinate, lactate, ethanol | Acetate, formate |
| Substrates | ||||
| Galacturonic acid | + | + | n.d. | – |
| Pectin | + | – | n.d. | + |
| Polygalacturonates | + | + | n.d. | + |
| Other sugars | – | Glucuronic acid, fructose | Multiple | Fructose, lactose, cellobiose |
| Maximal growth temperature | 43 | 45 | n.d. | 45 |
| pH range (optimum) | 8.0–10.5 (9.5–9.7) | 8.2–10.6 (10) | 6.9–9.3 (7.8) | Neutrophile |
| Salt range (M Na+) | 0.2–2.5 | 0.2–3.5 | Non-halophilic | Non-halophilic |
| Polar lipids | PG, DPG, PL, GL, APL | PG, DPG, PL, GL, APL | PG, DPG, GL, APL, APGL, PE | n.d. |
| Dominant fatty acids in polar lipids | 16:0, 16:1ω7c, 18:1ω7c | 16:0, 16:1ω7c, | 14:0, 16:0, 16:1ω7c, 18:1ω7c | n.d. |
| G+C content (mol%) | 30.7 | 32.0 | 48.7 | 42.0 |
| Habitat | Soda soils | Soda lake sediments | Marine | Marine |
n.d. not determined, PG phosphatidylglycerol, DPG diphosphatidylglycerol, PE phosphatidylethanolamine, PL phospolipids, APL aminophospholipids, GL glycolipids, APGL aminophosphoglycolipids
aCornick et al. (1994)
bCotta et al. (2009)