| Literature DB >> 26592761 |
Konstantin V Starostin1, Evgeny A Demidov1, Alla V Bryanskaya1, Vadim M Efimov1, Alexey S Rozanov1, Sergey E Peltek1.
Abstract
Microorganism identification by MALDI TOF mass-spectrometry is based on the comparison of the mass spectrum of the studied organism with those of reference strains. It is a rapid and reliable method. However, commercial databases and programs are mostly designed for identification of clinically important strains and can be used only for particular mass spectrometer models. The need for open platforms and reference databases is obvious. In this study we describe a geometric approach for microorganism identification by mass spectra and demonstrate its capabilities by analyzing 24 strains belonging to the Bacillus pumilus group. This method is based on representing mass spectra as points on a multidimensional space, which allows us to use geometric distances to compare the spectra. Delimitation of microorganisms performed by geometric approach correlates well with the results of molecular phylogenetic analysis and clustering using Biotyper 3.1. All three methods used allowed us to reliably divide the strains into two groups corresponding to closely related species, Bacillus pumilus and Bacillus altitudinis. The method developed by us will be implemented in a Web interface designed for using open reference databases for microorganism identification. The data is available at http://www.bionet.nsc.ru/mbl/database/database.html.Entities:
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Year: 2015 PMID: 26592761 PMCID: PMC4655313 DOI: 10.1038/srep16989
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Figure 1Phylogenetic analysis.
(a) Phylogenetic tree constructed using the Maximum Likelihood algorithm for the 16S rRNA gene sequences. Numbers above branches indicate bootstrap support. Sequence distances represent the number of substitutions per 1000 nucleotides. The following type strains sequences were used for comparison: B. pumilus (AY456263), B. safensis (AB681259), and B. altitudinis (AJ831842); B. licheniformis (EF433410) was used as an outgroup. (b) Fragments of the alignment containing marker substitutions. Numbers in the bottom line indicate their positions in the B. altitudinis sequence (AJ831842).
Figure 2Phyloproteomic analysis.
Position of spectra centroids on the principal coordinates plane: (a) PCo1, PCo2; (b) PCo1, PCo3. The proportions of the total variance for those axes were 29.2% for PCo1, 13.2% for PCo2, and 10.4% for PCo3, which sums up to 52.9%. The groups A and P are framed. Dendrograms constructed based on the distances among spectra centroids by the Ward’s method (c) and by MSPs clustering in Biotyper 3.1 (d). Strains were divided into two clusters that correspond to B. altitudinis (A) and B. pumilus (P); (e) Wet-lab experiment: identification of the studied centroids for two biological replicates using JC, Euclidean distances, and Biotyper 3.1 (cutoff criteria - 2.0, wich is defined Bruker as “secure genus identification, probable species identification”). (e) Wet-lab experiment: identification of the studied centroids for two biological replicates using JC, Euclidean distances, and Biotyper 3.1 (cutoff criteria - 2.0, wich is defined Bruker as “secure genus identification, probable species identification”). Strain-level match - case when centroid of tested specimen and closest centroid in data base belong to the one and the same strain.
Figure 3Gel view of averaged mass spectra.
Common peaks are indicated by asterisks; peaks characteristic for the A group, by (a); peaks characteristic for the P group, by (p). A group of high-intensity peaks in the 6032–6117 Da range is framed.
List of the studied strains.
| Strain | Cultivation Medium | GenBank | Strain source | Geochemical characteristics | Coordinates |
|---|---|---|---|---|---|
| O48 | LB | KP699776 | NR, Solenoye l. (48). Water sample. | 190; 15–20; 8, 0 | 54°14′ |
| O32 | LB | KP699772 | NR, Gorkoye l. (42). Bottom sediments. | 280; 15–20; 7, 7 | 54°17′ |
| O19 | LB | KP699775 | NR, Dolgoye l. (44). Water sample. | 43; 15–20; 8, 3 | 54°10′ |
| O6 | LB | KP699774 | NR, Solenoye l. (48). Water sample. | 190; 15–20; 8, 0 | 54°14′ |
| 47(6)il | S4 | KP699765 | NR, Khorosheye l. (47). Bottom sediments. | 99; 15–20; 9, 2 | 54°05′ |
| 51(3)w | LB | KP699766 | NR, Gorkoye l. (51). Water sample. | 49; 15–20; 8, 9 | 54°12′ |
| O41 | LB | KP699767 | NR, Krugloe l. (45). Bottom sediments. | 290; 15–20; 7, 7 | 54°08′ |
| O33 | LB | KP699768 | NR, Gorkoye l. (42). Bottom sediments. | 280; 15–20; 7, 7 | 54°17′ |
| 48(1)w | LB | KP699778 | NR, Solenoye l. (48). Water sample. | 114; 15–20; 8, 0 | 54°14′ |
| 46(5)il | LB | KP699764 | NR, Razboynoye l. (46). Bottom sediments. | 14, 7; 15–20; 8, 7 | 54°07′ |
| 51(1)il | LB | KP699773 | NR, Gorkoye l. (51). Bottom sediments. | 133; 15–20; 8, 0 | 54°12′ |
| 51(5)il | LB | KP699777 | NR, Gorkoye l. (51). Bottom sediments. | 49; 15–20; 8, 9 | 54°12′ |
| 42(6)w | LB | KP699769 | NR, Gorkoye l. (42). Water sample. | 160; 15–20; 7, 6 | 54°17′ |
| 3U | MPA | KP699770 | KR, A swamp near t. Ursk. Bottom sediments. | N.D.; 25; 2, 6 | 54°27′ |
| 10U | MPA | KP699771 | KR, River Ur near t. Ursk. Water sample. | N.D.; 18; 7, 7 | 54°27′ |
| KH6 | MPA | KP699782 | KT, Geyser valley, G-16 (thermal cauldron). | N.D., 62; 3, 6 | 54°25′ |
| KU3-5(2) | MPA | KP699787 | KT, Uzon caldera, U3-5 (Oil field). | 0, 4; 79; 4, 7 | 54°30′ |
| KH2 | MPA | KP699786 | KT, Uzon caldera, U3-4-8 (Oil field). | 1, 1; 63; 2, 9 | 54°30′ |
| KG16(2) | MPA | KP699780 | KT, Geyser valley, G-16 (thermal cauldron). | N.D., 62; 3, 6 | 54°25′ |
| K6dt | MPA | KP699783 | KT, Uzon caldera, U-4 (Bannoye lake). | 0, 2; 36; 4, 6 | 54°30′ |
| KH3 | MPA | KP699785 | KT, Uzon caldera, Uskv2. | 0, 3; 95; 8, 4 | 54°30′ |
| KG16(3) | MPA | KP699781 | KT, Geyser valley, G-16 (thermal cauldron). | N.D., 62; 3, 6 | 54°25′ |
| Cd1 | MPA | KP699779 | RG, Novosibirsk water storage basin. | <1, 0; 21; N.D. | 55°04′ |
| Cu1 | MPA | KP699784 | RG, Novosibirsk water storage basin. | <1, 0; 21; N.D. | 55°04′ |
NR, Novosibirsk region, saline lakes (l.); KR, Kemerovo region, complex ore deposits; KT, Kamchatka thermal springs; RG, rhizosphere of the water hyacinth, Novosibirsk water storage basin. For mass spectrometry, bacterial strains were grown at 37 °C on the following agar media: Luria-Bertani broth (LB); meat-peptone agar (MPA), and S4 medium containing 1 g/l NaCl, 5 g/l MgCl2, 1 g/l KCl, 1 g/l CaCl2, 4 g/l tripthone, 2 g/l yeast extract. Geochemical characteristics of the source environments: salinity (g/l); temperature (C); pH.