Huber, Gertrud

Huber, Harald

Stetter, Karl Otto

English

University of Regensburg Publication Server

Isolation and Characterization of New Metal-Mobilizing Bacteria G. H U B E R , H . HUBER, and K. O. STETTER Lehrstuhl fur Mikrobiologie, Universität Regensburg, Universitätsstrasse 31, 8400 Regensburgf Fed. Rep. Germany Summary In a screening program, novel mesophilic, thermophilic and extremely thermophilic chem-olithotrophic bacteria able to grow by mobilization of metals from natural ores were isolated from geothermal areas and from ore deposits. A first characterization revealed 3 groups of mesophiles differing in morphology, physiology, and biochemical properties from each other and from Thiobacillus ferrooxidans, although their taxonomic position is still unknown. Among the thermophiles, a Sulfolobus-shapeá isolate is growing on ores at temperatures up to 85°C and is therefore the most extremely thermophilic leaching organism known to date. INTRODUCTION In spite of the increasing interest in microbial leaching, the variety of organisms known to be able to extract metals from ores is still very small. Within the mesophilic temperature range, mainly strains of Thiobacillus ferrooxidans and Thiobacillus thiooxidans are known to be involved in hydrometallurgical processes [1,2], although the latter is only able to attack sulfidic ores in combination with Th. ferrooxidans [3]. In addition, Leptospirillum ferrooxidans and L. ferrooxidans-like organisms have been described which grow by oxidation of F e 2 + or pyrite at mesophilic tem-peratures [4,5]. The upper temperature for bacterial leaching has been reported to be around 75°C for Sulfolobus brierleyi [6] and related orga-nisms [7]. Here, we present novel isolates from ore-containing biotopes growing chemolithotrophically on natural ores within the mesophilic, ther-mophilic, and extremely thermophilic temperature range. Biotechnology and Bioengineering Symp. No. 16 (1986) © 1986 John Wiley & Sons, Inc. CCC 0572-6565/86/160239-13$04.00 MATERIALS AND METHODS Strains The type strains of Thiobacillus ferrooxidans (ATCC 23270) and Thio-bacillus thiooxidans (ATCC 19377) were obtained from the American Type Culture Collection. Leptospirillum ferrooxidans (DSM 2705) was supplied by the Deutsche Sammlung von Mikroorganismen. Culture Conditions The type strains and isolate SP5/1 were cultivated in 9K-medium [8]. For the isolates L7, LM1, LM3, MSB9, MSB11, MSB12, and Hö3, Hö5 we used a mineral salt medium (Ml) containing in g per liter: K C l 0.33; MgCl2-6 H 2 0 2.75; MgS04-7 H 2 0 3.45; NH 4C1 1.25; CaCl2-2 H 2 0 0.14; K 2 H P 0 4 0.14; K H 2 P 0 4 0.14; NaCl 0.5 and 10 ml trace mineral solution [9]. The pH was adjusted to 3.5 with H 2 S 0 4 . The thermophilic isolates (TH2, SP3a, Kra23, NA4, VE2) were grown in Allen's medium [10]. To 100-ml Erlenmeyer flasks were added 30 ml of medium supplemented with 4 ml of a 20% ferrous sulfate solution or with 0.1 g S° or with 1 g ore mixture (Gl) containing 0.25 g pyrite (Grube Bayerland, Oberpfalz), 0.25 g chalcopyrite (Bad Grund, Harz), 0.25 g sphalerite (Grube Lüderich, Fig. 1. Submarine isolate L7. EM-micrograph. Pt-shadowing. Bar, 1 /xm. Nordrhein-Westfalen) and 0.25 g pitch blend (Grube Höhenstein, Oberp-falz) as energy source. The particle size of this mixture was below 1 mm. The culture media were sterilized by autoclaving. Sulfur was sterilized by steaming for 30 min on three consecutive days at 100°C. The cultures were incubated in rotary shakers (New Brunswick) at 150 rpm. Analysis of Cell Proteins In order to obtain protein patterns, cells from 30-ml cultures (grown for 3 to 4 weeks) were harvested by centrifugation and washed twice with culture medium at pH 6.5 which did not contain ore. The washed cells were then sonicated after suspension in 50 /xl of Laemmli's sample buffer [11]. The homogenates were heated for 15 min at 100°C, and 20 fxg of protein were loaded on to an exponential Polyacrylamide gel [11,12]. The electrophoresis was carried out at 100 V for 15 hours and then the gel was stained with Coomassie blue. Metal Analyses Metal ion concentrations within solutions were determined employing an ICP instrument (Lab Test). Fig. 2. Coccoid isolate SP5/1 from Pisciarelli Solfatara. EM-micrograph. Pt-shadowing. Bar, 1 fim. RESULTS AND DISCUSSION Collection of Samples Within the area of Porto di Levante (Vulcano, Italy), 20-ml samples of pyrite-containing [13] geothermally heated sandy sediments of the beach and the shallow sea floor with original temperatures between 30 and 50°C were taken (samples L7, LM1, LM3, MSB9, MSB11, MSB12). Further samples were obtained from continental solfatara fields at Pisciarelli (Italy) with temperatures between 30 and 52°C (samples SP5/1, TH2, SP3a) and from Kraffla, Namaskarth and Hveravellir (all situated in Iceland) with original temperatures between 94 and 100°C (samples Kra23, NA4, VE2). The samples were brought to the laboratory without temperature or pH control. In addition, ore samples (Hö3, Hö5) were taken from a mud pond within the area of the uranium mine Höhenstein (Oberpfalz, FRG). Enrichment and Isolation For enrichment, 30 ml of ore-containing medium were inoculated with about 1 ml of samples and incubated at 30, 37 and 65°C, depending on the original temperatures of the samples. After one (thermophiles) to two weeks (mesophiles), bacteria became visible, partially attached to the ores which could be detected microscopically after fluorescence staining [14]. Fig. 3. Isolate Hö5 from an uranium mine. EM-micrograph. Pt-shadowing. Bar, 1 /urn. TABLE I Energy Sources of Mesophilic Isolates S t r a i n s Substrate Th. f e r r o o x i d a n s ATCC 23270 L7 HÖ5 SP5/1 ore mixture G1 (3.3 %) + + + + FeS0 4 ( 2.5%) + + - + S q (0.3 %) + •f-y e a s t e x t r a c t (0.05 %) - - -sucrose (0.1 %) - - + n.d. The organisms were purified by serial dilution repeated at least 3 times. For this purpose, cells attached to the ores were detached by strongly shaking (about 1 min.) with a whirlimix. The enrichment culture of sample SP5/1 were successfully plated on polysilicate plates [15] with FeS0 4 as an energy source. Morphology From all six samples from Vulcano, slim irregular rods, about 2.5 to 4 fxm long and 0,3 jitm in diameter with one polar flagellum, about 4 /xm long and 17 nm in width were isolated (Fig. 1). From this group, isolate L7 was further characterized. A coccoid mesophilic isolate (SP5/1) varying in diameter between 0.8 to 2 fim (Fig. 2) was obtained from a source with an original temperature of 30°C and a pH of 1.5 from Pisciarelli Solfatara. The samples of the Höhenstein mine yielded a third group of mesophilic isolates consisting of short small rods about 1 /xm long and 0.3 /xm in diameter from which isolate Hö5 was further investigated (Fig. 3). The thermophilic and extremely thermophilic isolates are regular (isolates TH2 M — h- 1 H -H 1 H 01 10 20 30 t (days ) — • Fig. 5. pH profiles during growth of the new isolates on the sterile ore mixture Gl.C = uninoculated control. Th. f. = Thiobacillus ferrooxidans ATCC 23270. and SP3a; Fig. 4 a) or irregular (Kra23, NA4 and VE2; Fig. 4 b) spheres, about 0.7 to 1.5 /xm in diameter. Isolate VE2 possesses a flagellum-like structure, about 30 nm in diameter and 12 ¡xm long (not shown). Physiology All isolates are able to grow chemolithoautotrophically on natural ores, e.g. mixture G l (Table I). Isolate SP5/1 can also utilize FeS0 4 and S° as energy sources and therefore behaves like Th. ferrooxidans. The marine isolate L7 grows best on natural ores. On FeS0 4 and on S°, extremely slow and weak growth is obtained after a 2-months adaptation phase in the presence of both components together with ore mixture G l . In con-trast, isolate Hö5 does not grow lithotrophically on F e S Ö 4 or S° but only on natural ores. However, this organism also grows on yeast extract and Temp. CO — • Fig. 6. Temperature optima of mesophilic strains. Th. f. = Thiobacillus ferrooxidans ATCC 2327Ö. The strains were grown on ore mixture Gl as energy source in the basal media described under materials and methods. The doubling time was determined by direct count-ing in a Thoma counting chamber after vigorous shaking with a whirlimix. even on sucrose as energy sources and is therefore a facultatively het-erotrophic organism (Table I). The optimal pH for Hö5 is about 4.5. No growth occurs at pH 3 or below. During autotrophic growth on ores, the pH is only slightly lowered in contrast to all other isolates and Th. fer-rooxidans (Fig. 5). The temperature optima of the three new mesophilic isolates and Th. ferrooxidans are between 30 and 37°C (Fig. 6). The upper temperature limit of the thermophilic isolates is between 65 and 85°C, depending on the strains (Table II). The isolates SP3a and VE2 show the highest temperature maxima reported for ore-leaching bacteria. By their ability to grow lithoautotrophically on ores, the isolates are dif-ferent from S. brierleyi (DSM 1651) (Table III). They can be distinguished from each other by their ability to utilize S° and yeast extract (Table III). Chemotaxonomy All mesophilic isolates show a negative gram staining reaction and con-tain meso-diaminopimelic acid and are sensitive to the antibiotics ampi-cillin, vancomycin and kanamycin, indicating that they belong to the gram-negative eubacteria. As a first indication, patterns of SDS-soluble cell proteins were compared with those of the type strains of Th. ferroooxi-dansy Th. thiooxidans, and L. ferrooxidans (Fig. 7). It is obvious, that the protein patterns of isolates L7 and Hö5 are very different from each TABLE II Growth Temperatures of Thermophilic Isolates Temperatures 65°C 75°C 80°C 85°C Strains TH2 + -SP3a + + + n.d. Kra23 + - -NA4 + - -VE2 + + + + S. b r i e r l e y i DSM 1651 + + - -TABLE i n Energy Sources of Thermophilic Isolates Substrate ore mixture G1 S o yeast e x t r a c t S t r a i n s (3.3 %) • (0.3 %) (0. 1 %) TH2 + + + SP3a + - + Kra23 + + -NA4 + + -S. b r i e r l e y i + DSM 1651 1 2 3 4 5 6 7 8 9 Fig. 7. Protein patterns of cells of ore-leaching bacteria (1) MW standards (200; 116; 92; 65; 45 kD) (2) Th. ferrooxidans A T C C 23270 (3) L. ferrooxidans D S M 2705 (4) Th. thiooxidans A T C C 19377 (5) L7 (6) LM3 (7) Hö3 (8) Hö5 (9) SP5/1. other and from the type strains, while that of the coccoid isolate SP5/1 shows some similarity with Thiobacillus ferrooxidans. These findings are in agreement with the metabolic properties of these isolates and support the assumption that L7 and Hö5 may represent novel leaching organisms. The thermophiles possess protein subunit envelopes, suggesting that they belong to the sulfur-dependent archaebacteria [16]. Metal Mobilization During dissolution of the ore mixture G l , isolates L7 and SP5/1 and Th. ferrooxidans 23270 are similar in their ability to solubilize various metal ions, e.g. C u 2 + (Fig. 8 a), Z n 2 + (Fig. 8 b) and U 6 + (not shown). In 01 10 20 30 t (days) —-> 01 10 20 30 t (days) — » Fig. 8. Metal solubilization by the isolates from ore mixture Gl (a) C u 2 + (b) Z n 2 + Th. f. = Thiobacillus ferrooxidans ATCC 23270. contrast, isolate Hö5 shows practically no solubilization of Z n 2 + (Fig. 8 b) and uranium, but a pronounced preference for copper (Fig. 8 a), indicating a metal specificity unknown up to now. The excellent technical assistance of H. Nowarra is highly acknowledged. This work was supported" by a grant of the BMFT, Projektleitung Rohstofforschung. References [1] A. R. Colmer and M. E. Hinkle, Science, 106, 253 (1947). [2] L. C. Bryner and R. Anderson, Ind. Eng. Chem., 49, 1721 (1957). [3] H. L. Ehrlich, in Recent Progress in Biohydrometallurgy: Leaching of chromite ore and sulfide matte with dilute sulfuric acid generated by Thiobacillus ferrooxidans from sulfur, G. Rossi and A. E. Torma, Eds. International Symposium on Biohydrometal-lurgy (Associazione Mineraria Sarda, 1983) pp. 19-42. [4] V. V. Balashova, I. Ya. Vedenina, G. E. Markosyan and G. A. Zavarzin, Mikrobio-logiya, 43, 581 (english translation p. 491) (1974). [5] P. R. Norris, in Recent Progress in Biohydrometallurgy: Iron and mineral oxidation with Leptospirillum-like bacteria, G. Rossi and A. E. Torma, Eds. International Sym-posium on Biohydrometallurgy (Associazione Mineraria Sarda, 1983) pp. 83-96. [6] C. L. Brierley and J. A. Brieriey, Can. J. Microbiol., 19, 183 (1973). [7] R. M. Marsh, P. R. Norris and N. W. Le Roux, in Recent Progress in Biohydro-metallurgy: Growth and mineral oxidation studies with Sulfolobus, G. Rossi and A. E. Torma, Eds. International Symposium on Biohydrometallurgy (Associazione Mi-neraria Sarda, 1983) pp. 71-81. [8] M. P. Silverman and D. G. Lundgren, J. Bact., 77, 642 (1959). [9] W. E. Baich, G. E. Fox, L. J. Magrum, C. R. Woese and R. S. Wolfe, Microbiol Rev., 43, 260 (1979). [10] M. B. Allen, Arch. Microbiol., 32, 270 (1959). [11] U. K. Laemmli, Nature, 227, 680 (1970). [12] M. E. Mirault and K. Scherrer, Europ. J. Biochem., 23, 372 (1971). [13] A. Wauschkuhn and H. Gröpper, N. Jb. Miner., 126, 87 (1975). [14] H. Huber, G. Huber and K. O. Steuer, System. Appl. Microbiol., 6, 105 (1985). [15] W. W. Leathen, N. A. Kinsel and S. A. Braley, / . Bact., 72, 700 (1956). [16] K. O. Stetter and W. Zillig, in The Bacteria: Thermoplasma and the thermophilic sulfur-dependent archaebacteria, C. R. Woese and R. S. Wolfe, Eds. (Academic Press, New York, 1985), Vol. VIII., Chapter 2. 

Isolation and Characterization of New Metal-Mobilizing Bacteria

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Isolation and Characterization of New Metal-Mobilizing Bacteria

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