Plasmid Profiles of Acidithiobacillus ferrooxidans Strains Adapted to Different Oxidation Substrates

Plasmid profiles were studied in five Acidithiobacillus ferrooxidans strains of various origin cultivated on a medium with Fe²⁺, as well as adapted to such oxidation substrates as S⁰, FeS₂, and sulfide concentrate. The method used revealed plasmids in all A. ferrooxidans strains grown on a medium with Fe²⁺. One plasmid was found in strain TFL-2; two plasmids, in strains TFO, TFBk, and TFV-1; and three plasmids were detected in strain TFN-d. The adaptation of strain TFN-d to sulfide concentrate and the adaptation of strain TFV-1 to S⁰, FeS₂, or sulfide concentrate resulted in a change in the number of plasmids occurring in cells. In cells of strain TFN-d adapted to sulfide concentrate, the number of plasmids decreased from three to two. The number of plasmids in cells of strain TFV-1 adapted to different substrates varied from three to six depending on the energy source present in the medium: three plasmids were found after growth on FeS₂, four after growth on S⁰, and six after growth on sulfide concentrate. The possible role of plasmids in the adaptation of A. ferrooxidans to new energy substrates and in the regulation of the intensity of their oxidation is discussed.     

Phenotypic characteristics of Thiobacillus ferrooxidans strains

Phenotypic polymorphism of strains of Thiobacillus ferrooxidans isolated from various ecological niches was studied. The strains differed both in rates of growth and oxidation of Fe2+, S0, FeS2, and sulfide minerals contained in concentrate. Each strain, irrespective of its original environment, required a period of adaptation to a new substrate. Strains TFN-d, TFBk, TFO, and TFL-2, isolated from ores and concentrates rich in oxidized substrates, showed an equal adaptation pace (five culture transfers) but differed in their adaptation efficiency. Strain TFV-1, isolated from base ore and showing the lowest rates of growth and oxidation of all the substrates, required five culture transfers to adapt to S0 and FeS2 and seven culture transfers to adapt to the concentrate. It is concluded that the phenotypic properties of the strains correlate with their genotypic polymorphism and the environmental conditions under which their microevolution took place.     

Characteristics of the restriction profile of chromosomal DNA in strains of Acidithiobacillus ferroxidans,adapted to various oxidation substrates

Restriction profiles of chromosomal DNA were studied in different Acidithiobacillus ferrooxidans strains grown on medium with Fe2+ and further adapted to another oxidation substrate (S0, FeS2, or sulfide ore concentrates). The restriction endonuclease XbaI digested the chromosomal DNA from different strains into different numbers of fragments of various sizes. Adaptation of two strains (TFBk and TFN-d) to new oxidation substrates resulted in structural changes in XbaI-restriction patterns of their chromosomal DNA. Such changes in the DNA restriction patterns occurred in strain TFBk after the adaptation to precyanidated gravitational pyrite-arsenopyrite concentrate (no. 1) from the Nezhdaninskoe deposit or to copper-containing ore from the Udokanskoe deposit and also in strain TFN-d adapted to untreated pyrite-arsenopyrite concentrate (no. 2) from the Nezhdaninskoe deposit. No changes in the number or size of the XbaI-restriction patterns of chromosomal DNA were revealed in either strain TFBk cultivated on media with pyrite from the Angren and Tulun deposits or in strains TFN-d and TFO grown on media with S0 and pyrite. Neither were changes observed in the XbaI-restriction patterns of the DNA from strain TFV-1, isolated from the copper ore of the Volkovskoe deposit, when Fe2+ was substituted with alternative substrates--S0, pyrite or concentrate no. 2 from the ore of Nezhdaninskoe deposit. In strain TFO, no differences in the XbaI-restriction patterns of the chromosomal DNA were revealed between the culture grown on medium containing concentrate no. 2 or the concentrate of surface-lying ore from Olimpiadinskoe deposit and the culture grown on medium with Fe2+. When strain TFO was cultivated on the ore concentrate from deeper horizons of the Olimpiadinskoe deposit, which are characterized by lower oxidation degree and high antimony content, mutant TFO-2 differing from the parent strain in the chromosomal DNA structure was isolated. The correlation between the lability of chromosomal DNA structure in A. ferrooxidans strains and the physical and chemical peculiarities of the isolation substrate and habitat is discussed.     

Strain polymorphism of the plasmid profiles in Acidithiobacillus ferrooxidans

Plasmid profiles were studied in 27 Acidithiobacillus ferrooxidans strains isolated from different geographic zones and substrates differing in the composition of the main sulfide minerals, and also in experimentally obtained strains with acquired enhanced resistance to the ions of heavy metals (Fe, Ni, Cu, Zn, As). In 16 out of 20 strains isolated from different substrates, one to four 2- to 20-kb and larger plasmids were revealed. Plasmids were found in all five strains isolated from gold-containing pyrite-arsenopyrite ores and concentrates, in nine of 11 strains isolated from the ores and concentrates containing nonferrous metals, and in two of four strains isolated from the oxidation substrates of simple composition (mine waters, pyritized coals, active sludge). Changes in the plasmid profiles in some A. ferrooxidans strains (TFZ, TFI-Fe, TFV-1-Cu) with experimentally enhanced resistance to Zn2+, Fe3+, and Cu2+, respectively, were noted as compared with the initial strains. After 30 passages on S0-containing medium, strain TFBk showed changes in the copy number of plasmids. The role of plasmids in the processes of oxidation of energy substrates and in the acquired enhanced resistance to the heavy metal ions is discussed.     

Interaction of chromosomal and plasmid DNA in Acidithiobacillus ferrooxidans strains adapted to different oxidation substrates

Restriction analysis of plasmids pTFK1 and pTFK2 of the Acidithiobacillus ferrooxidans strain TFBk was carried out, and the sizes of these plasmids were determined (13.5 and 30 kb, respectively). A macrorestriction map was built for plasmid pTFK1. DNA-DNA hybridization revealed that the plasmids contained homologous nucleotide sequences. Plasmid pTFK2 labeled with 32P was used as a probe for Southern hybridization with blots of XbaI-generated fragments of the chromosomal DNA of A. ferrooxidans strains grown on a medium containing Fe2+ or adapted to different oxidation substrates. Low-intensity hybridization signals were observed for many fragments of the chromosomal DNA of the strains studied. In the process of adaptation to new oxidation substrates, the localization of bands producing the low-intensity hybridization signals changed in a number of cases. Certain fragments of the chromosomal DNA of the strains adapted to different oxidation substrates produced strong hybridization signals with pTFK2. The data obtained are discussed in terms of the possible role of IST elements and plasmids in the adaptation of A. ferrooxidans to new energy substrates, microevolution, and strain polymorphism.     

Phenotypic Characteristics of Thiobacillus ferrooxidansStrains

Phenotypicpolymorphism of Thiobacillus ferrooxidansstrains isolated from various ecological niches was studied. The strains differed both in rates of growth and oxidation of Fe²⁺, S⁰, FeS₂, and sulfide minerals contained in concentrate. Each strain, irrespective of its original environment, required a period of adaptation to a new substrate. Strains TFN-d, TFBk, TFO, and TFL-2, isolated from ores and concentrates rich in oxidizable substrates, showed an equal adaptation rate (five culture transfers) but differed in their adaptation efficiency. Strain TFV-1, isolated from low-grade ore and showing the lowest rates of growth and oxidation of all the substrates, required five culture transfers to adapt to S⁰and FeS₂and seven culture transfers to adapt to the concentrate. It is concluded that the phenotypic properties of the strains correlate with their genotypic polymorphism and the environmental conditions under which their microevolution took place.     

Restriction Profiles of the Chromosomal DNA from Acidithiobacillus ferrooxidans Strains Adapted to Different Oxidation Substrates

Restriction profiles of chromosomal DNA were studied in different Acidithiobacillus ferrooxidans strains grown on medium with Fe²⁺ and further adapted to another oxidation substrate (S⁰, FeS₂, or sulfide ore concentrates). The restriction endonuclease XbaI digested the chromosomal DNA from different strains into different numbers of fragments of various sizes. Adaptation of two strains (TFBk and TFN-d) to new oxidation substrates resulted in structural changes in XbaI-restriction patterns of their chromosomal DNA. Such changes in the DNA restriction patterns occurred in strain TFBk after the adaptation to precyanidated gravitational pyrite-arsenopyrite concentrate (no. 1) from the Nezhdaninskoe deposit or to copper-containing ore from the Udokanskoe deposit and also in strain TFN-d adapted to untreated pyrite-arsenopyrite concentrate (no. 2) from the Nezhdaninskoe deposit. No changes in the number or size of the XbaI-restriction patterns of chromosomal DNA were revealed in either strain TFBk cultivated on media with pyrite from the Angren and Tulun deposits or in strains TFN-d and TFO grown on media with S⁰ and pyrite. Neither were changes observed in the XbaI-restriction patterns of the DNA from strain TFV-1, isolated from the copper ore of the Volkovskoe deposit, when Fe²⁺ was substituted with alternative substrates—S⁰, pyrite or concentrate no. 2 from the ore of the Nezhdaninskoe deposit. In strain TFO, no differences in the XbaI-restriction patterns of the chromosomal DNA were revealed between the culture grown on medium containing concentrate no. 2 or the concentrate of surface-lying ore from the Olimpiadinskoe deposit and the culture grown on medium with Fe²⁺. When strain TFO was cultivated on the ore concentrate from deeper horizons of the Olimpiadinskoe deposit, which are characterized by lower oxidation degrees and high antimony content, mutant TFO-2 differing from the parent strain in the chromosomal DNA structure was isolated. The correlation between the lability of the chromosomal DNA structure in A. ferrooxidans strains and the physical and chemical peculiarities of the isolation substrate and habitat is discussed.     

Dependence of the Genotypic Characteristics of <Emphasis Type="Italic">Acidithiobacillus ferrooxidans</Emphasis> on the Physical,Chemical, and Electrophysical Properties of Pyrites

This study focused on the effect of physical, chemical, and electrophysical properties of two pyrites, pyrite 1, which had electron-type (n-type) conductivity, and pyrite 2, with hole-type (p-type) conductivity, on the genotypic characteristics of Acidithiobacillus ferrooxidans strains TFV-1 and TFBk, which were isolated from different substrates. After the adaptation of the strains to the pyrites at a pulp density of 1%, pulsed-field electrophoresis revealed changes in the chromosomal DNA of strain TFV-1 adapted to pyrite 1, and strain TFBk adapted to either of the pyrite types. In pyrite-adapted strain TFBk, the plasmid composition was the same as after growth on a medium containing ferrous iron, whereas, in strain TFV-1, changes in plasmid sizes or both in plasmid sizes and plasmid number occurred. After an increase in the density of the pyrite 2 pulp from 1 to 10%, the plasmid number increased from three to four, and, after an increase in the density of the pyrite 1 pulp from 1 to 7%, the plasmid number increased from two to six.     

Patterns of growth and oxidation of natural pyrites by the representatives of acidophilic chemolithotrophic microorganisms

The patterns of the growth and oxidation of different types of natural pyrites were studied for the three microbial species adapted to these substrates and belonging to phylogenetically remote groups: gram-negative bacterium Acidithiobacillus ferrooxidans, gram-positive bacterium Sulfobacillus thermotolerans, and the archaeon Ferroplasma acidiphilum. For both A. ferrooxidans strains, TFV-1 and TFBk, pyrite 4 appeared to be the most difficult to oxidize and grow; pyrite 5 was oxidized by both strains at an average rate, and pyrite 3 was the most readily oxidized. On each of the three pyrites, growth and oxidation by TFBk were more active than by TFV-1. The effectiveness of the adaptation of S. thermotolerans Kr1^T was low compared to the A. ferrooxidans strains; however, the adapted strain Kr1^T showed the highest growth rate on pyrite 3 among all the cultures studied. No adaptation of strain Kr1^T to pyrite 5 was observed; the rates of growth and pyrite oxidation in the third transfer were lower than in the first transfer. The strain F. acidiphilum Y^T was not adapted to pyrites 3 and 5; the rates of growth and pyrite oxidation were the same in the first five transfers. The strains of three species of the microorganisms studied, A. ferrooxidans, S. thermotolerans, and F. acidiphilum, grew on pyrite 3 (holetype (p) conductivity) and oxidized it better than pyrite 5 (mixed-type (n-p) conductivity). The most readily oxidized were the pyrites with a density of 5.6–5.7 g/cm³ and high resistance values (ln R = 8.8). The pyrite oxidation rate did not depend on the type of conductivity. Changes in the chromosomal DNA structure were revealed in strain TFBk on adaptation to pyrites 3 and 4 and in the TFV-1 plasmid profile on adaptation to pyrite 3. Correlation between genetic variability and adaptive capabilities was shown for A. ferrooxidans. No changes in the chromosomal DNA structure were found in S. thermotolerans Kr1^T and F. acidiphilum Y^T on adaptation to pyrites 3 and 5. Plasmids were absent in the cells of these cultures.     

Strain Polymorphism of the Plasmid Profiles in Acidithiobacillus ferrooxidans

Plasmid profiles were studied in 27 Acidithiobacillus ferrooxidans strains isolated from different geographic zones and substrates differing in composition of the main sulfide minerals, and also in experimentally obtained strains with acquired enhanced resistance to the ions of heavy metals (Fe, Ni, Cu, Zn, As). In 16 out of 20 strains isolated from different substrates, one to four 2- to 20-kb and larger plasmids were revealed. Plasmids were found in all five strains isolated from gold-containing pyrite–arsenopyrite ores and concentrates, in nine of 11 strains isolated from the ores and concentrates containing nonferrous metals, and in two of four strains isolated from the oxidation substrates of simple composition (mine waters, pyritized coals, active sludge). Changes in the plasmid profiles in some A. ferrooxidans strains (TFZ, TFI-Fe, TFV-1-Cu) with experimentally enhanced resistance to Zn²⁺, Fe³⁺, and Cu²⁺, respectively, were noted as compared with the initial strains. After 30 passages on a S⁰-containing medium, strain TFBk showed changes in the copy number of plasmids. The role of plasmids in the processes of oxidation of energy substrates and in the acquired enhanced resistance to heavy metal ions is discussed.     

Strain polymorphism of the plasmid profiles in <Emphasis Type="Italic">Sulfobacillus</Emphasis> species

Plasmids were discovered for the first time in strains belonging to different species of the genus Sulfobacillus: S. thermosulfidooxidans, S. sibiricus, S. thermotolerans, “S. olympiadicus”, and S. acidophilus. The plasmids were detected in the cells of four out of eight strains grown on a medium with ferrous iron. Adaptation to elementary sulfur was accompanied by changes in the plasmid profiles in two out of seven strains. Plasmids were detected in all the studied strains of sulfobacilli after adaptation to the pyrite-arsenopyrite ore concentrate from the Nezhdaninskoe deposit containing gold, silver, zinc, copper, and lead. No plasmids were found in S. thermotolerans Kr1^T after four transfers on a medium containing iron and 0.018 mM Ag⁺. After adaptation of the same strain to 765 mM Zn²⁺, only one plasmid was found in the cells, the largest among those detected earlier in this culture adapted to the Nezhdaninskoe ore concentrate. The strain S. thermotolerans Kr1^T, after four transfers on media with either 78 mM Cu²⁺ or 2 mM Pb²⁺, did not contain plasmids. The presence of plasmids in the cells of sulfobacilli did not influence their resistance to the ions of the studied metals.     

Identification of IS elements in <Emphasis Type="Italic">Acidithiobacillus ferrooxidans</Emphasis> strains grown in a medium with ferrous iron or adapted to elemental sulfur

IS elements were identified in the genomes of five Acidithiobacillus ferrooxidans strains isolated from various media. IST2 elements were revealed in all the strains grown in a medium with ferrous iron, ISAfe1 elements were detected in four strains (TFBk, TFL-2, TFV-1 and TFO). Three strains (TFV-1, TFN-d and TFO) were found to contain IS elements, ~600 bp long. These were named preliminary as ISAfe600. Partial sequencing of the 5′- and 3′-terminal nucleotide stretches of an ISAfe1 element in TFBk and TFL-2 strains and complete sequencing of the ISAfe1 element in the TFBk strain has revealed nucleotide substitutions as compared to the prototype, i.e., the ISAfe1 element of an ATCC 19859 strain. Partial sequencing of the 5′- and 3′-terminal nucleotide stretches of the IST2 elements in TFO, TFBk and TFL-2 strains has shown numerous nucleotide substitutions when compared to the IST2 element of an ATCC 19859 strain. Complete sequencing of the IST2 element in the TFBk strain has revealed: the divergence between the IST2 elements in the TFBk strain and the prototype was 21.2%. Southern hybridization of EcoRI fragments of the chromosomal DNA from five A. ferrooxidans strains grown in a medium with ferrous iron using an internal region of ISAfe1, a full-length ISAfe1 or a full-length IST2 as probes has shown them to differ in the number of copies of IS elements and their localization on the chromosomes. Adaptation to elemental sulfur in A. ferrooxidans strains caused changes in the number, intensity and localization of hybridization bands. The authors discuss the role of IS elements in the adaptation of A. ferrooxidans to the new energy substrate. The nucleotide sequence data reported in this paper were deposited in GenBank under accession numbers: AY823401, the ISAfe1 from A. ferrooxidans TFBk; AY825254, the IST2 from TFBk; DQ002894, the 5′-terminal nucleotide sequence of ISAfe1 from TFL-2; DQ002895, the 3′-terminal nucleotide sequence of ISAfe1 from TFL-2; DQ005952, the 5′-terminal nucleotide sequence of IST2 from TFV-1; DQ005953, the 3′-terminal nucleotide sequence of IST2 from TFV-1.     

Interaction of Chromosomal and Plasmid DNA in Acidithiobacillus ferrooxidans Strains Adapted to Different Oxidation Substrates

Restriction analysis of plasmids pTFK1 and pTFK2 of theAcidithiobacillus ferrooxidans strain TFBk was carried out, and the sizes of these plasmids were determined (13.5 and 30 kb, respectively). A macrorestriction map was built for plasmid pTFK1. DNA–DNA hybridization revealed that the plasmids contained homologous nucleotide sequences. Plasmid pTFK2 labeled with ³²P was used as a probe for Southern hybridization with blots of XbaI-generated fragments of the chromosomal DNA of A. ferrooxidans strains grown on a medium containing Fe²⁺ or adapted to different oxidation substrates. Low-intensity hybridization signals were observed for many fragments of the chromosomal DNA of the strains studied. In the process of adaptation to new oxidation substrates, the localization of bands producing the low-intensity hybridization signals changed in a number of cases. Certain fragments of the chromosomal DNA of the strains adapted to different oxidation substrates produced strong hybridization signals with pTFK2. The data obtained are discussed in terms of the possible role of IST elements and plasmids in the adaptation of A. ferrooxidans to new energy substrates, microevolution, and strain polymorphism.     

Oxidation of gallium sulfides by Thiobacillus ferrooxidans.

The bacterial oxidation of naturally occurring gallium-bearing chalcopyrite concentrate and a pure synthetic gallium (III) sulfide has been investigated at pH 1.8 and 35 degree C, using an active culture of Thiobacillus ferrooxidans. This oxidation process may proceed by direct or by indirect bacterial action. The highest dissolved gallium and copper concentrations were about 2.2 and 40.2 g/l, respectively. The order of the specific rate of oxygen uptake by T. ferrooxidans in approximately CuFES2 greater than or equal to gallium-bearing CuFeS2 greater than FeS2 greater than Cu2S greater than Cu2S greater than Ga2S3.     

Dependence of the genotypic characteristics of Acidithiobacillus ferrooxidans on the physical, chemical, and electrophysical properties of pyrites

Comparison of Acidithiobacillus ferrooxidans strains TFV-1 and TFBk with respect to their capacity to oxidize pyrite 1, with hole-type (p-type) conductivity, or pyrite 2, with an electron-type (n-type) conductivity, showed that, at a pulp density of 1%, both before and after its adaptation to the pyrites, strain TFBk, isolated from a substrate with a more complex mineral composition, grew faster and oxidized the pyrites of both conductivity types more efficiently than strain TFV-1, which was isolated from a mineralogically simple ore. At a pulp density of 3-5%, the oxidation of pyrite 1 by strain TFV-1 and both of the pyrites by strain TFBk began only after an artificial increase in Eh to 600 mV. If the pulp density was increased gradually, strain TFBk could oxidize the pyrites at its higher values than strain TFV-1, with the rate of pyrite 2 oxidation being higher than that of pyrite 1. During chemical oxidation of both of the pyrites, an increase was observed in the absolute values of the coefficients of thermoelectromotive force (KTEMF); during bacterial-chemical oxidation, the KTEMF of pyrite 1 changed insignificantly, whereas the KTEMF of pyrite 2 decreased.     

Isolation and characterization of Acidithiobacillus ferrooxidans strain D3-2 active in copper bioleaching from a copper mine in Chile

Acidithiobacillus ferrooxidans strain D3-2, which has a high copper bioleaching activity, was isolated from a low-grade sulfide ore dump in Chile. The amounts of Cu(2+) solubilized from 1% chalcopyrite (CuFeS(2)) concentrate medium (pH 2.5) by A. ferrooxidans strains D3-2, D3-6, and ATCC 23270 and 33020 were 1360, 1080, 650, and 600 mg x l(-1) x 30 d(-1). The iron oxidase activities of D3-2, D3-6, and ATCC 23270 were 11.7, 13.2, and 27.9 microl O(2) uptake x mg protein(-1) x min(-1). In contrast, the sulfite oxidase activities of strains D3-2, D3-6, and ATCC 23270 were 5.8, 2.9, and 1.0 mul O(2) uptake.mg protein(-1).min(-1). Both of cell growth and Cu-bioleaching activity of strains D3-6 and ATCC 23270, but not, of D3-2, in the chalcopyrite concentrate medium were completely inhibited in the presence of 5 mM sodium bisulfite. The sulfite oxidase of strain D3-2 was much more resistant to sulfite ion than that of strain ATCC 23270. Since sulfite ion is a highly toxic intermediate produced during sulfur oxidation that strongly inhibits iron oxidase activity, these results confirm that strain D3-2, with a unique sulfite resistant-sulfite oxidase, was able to solubilize more copper from chalcopyrite than strain ATCC 23270, with a sulfite-sensitive sulfite oxidase.     

Identification and characterization of four strains of Acidithiobacillus ferrooxidans isolated from different sites in China

Four strains of Acidithiobacillus ferrooxidans (A. ferrooxidans), AF1, AF2, AF3 and AFc, were isolated from samples with different geological sources using a 9K medium. These four isolates were identified as A. ferrooxidans by phenotypic and 16S rDNA sequence analyses. All four isolates were able to use ferrous ion (Fe(2+)), elemental sulfur (S0) or pyrite as a sole energy source, but they showed differences in pH optima and range of activity, optimum temperature of activity, resistance to chloride (KCl) and heavy metal ions, and oxidation rates of Fe(2+), S0 and pyrite. AF3 was the most active strain when using Fe(2+) as the energy source, while AFc grew best using pyrite as the energy source. AF2 appeared to differ from the other three strains in substrate utilization, as it oxidizes S0 and pyrite more effectively than Fe(2+). RAPD analysis of genomic DNA from these isolates showed that banding profiles of their genomic DNA exhibited some differences, and the genomic banding profile of AF2 was significantly different from that of others. To obtain an insight into the molecular biology of the process of the energy production of these strains, several genes involved in the iron respiratory chain were cloned and sequenced, including Fe(2+) oxidase (iro), rusticyanin (rus) and subunit III of aa3-type cytochrome oxidase (cox C) genes. The results revealed that the iro gene can be cloned from all of the four strains and the nucleotide sequences were shown to be completely identical in each. However, rus and coxC genes could be amplified only from AF1, AF3 and AFc, not from AF2. These results suggested that the phenotypic differences of the four strains of A. ferrooxidans from different sites correlated with their genetic polymorphism, which may result from the different environments in which they lived, and that the strain AF2 was phenotypically and genetically significantly different from the other three strains.     

Use of reduced sulfur compounds by Beggiatoa sp.

A strain of Beggiatoa cf. leptomitiformis (OH-75-B, clone 2a) was isolated which is unique among reported strains in its ability to deposit internal sulfur granules from thiosulfate. It also deposited these characteristic granules (as all BEggiatoa species do) from sulfide. In cultures where growth was limited by exhaustion of organic substrates, these granules generally comprised about 20% of the total cell weight. With medium containing acetate and thiosulfate, no measurable utilization of thiosulfate or deposition of elemental sulfur (S0) took place until after the exponential growth phase. Neither sulfide nor thiosulfate added an increment to heterotrophic growth yield except for the weight of the deposited S0. The deposition of S0 from thiosulfate was probably a disproportionation in which S0 and sulfate were produced in a 1:1 ratio. Some of the S0 was further oxidized to sulfate. No autotrophic or mixotrophic growth was demonstrated for this strain. When inoculated in small, well-dispersed quantities into yeast extract medium, this strain grew only after long lags. Addition of the enzyme catalase eliminated initial lags and increased growth rates slightly. In contrast, catalase had no influence on growth rate when added to mineral medium containing acetate. In yeast extract medium, the inhibition of growth rate was presumably because of peroxides. Addition of thiosulfate was almost as effective as catalase in eliminating this inhibition. The S0 granules which, in this case, were deposited during the exponential growth phase, appeared to be partly responsible for this relief. This strain of Beggiatoa sp. remained active for at least 5 days under strictly anaerobic conditions, and under those conditions, it increased its dry weight by about 2.5-fold. Anaerobic "growth" and maintenance required the presence of an energy source, such as acetate. When cells containing much internal S0 were transferred to an organic anaerobic medium, a substantial portion of the internal S0 was eventually converted to sulfide.     

Bacterial leaching of a sulfide ore by Thiobacillus ferrooxidans and Thiobacillus thiooxidans: I. Shake flask studies

Bacterial leaching of a sulfide ore containing pyrite, chalcopyrite, and sphalerite was studied in shake flask experiments using Thiobacillus ferrooxidans and Thiobacillus thiooxidans strains isolated from mine sites. The Fe(2+)grown T. ferrooxidans isolates solubilized sphalerite preferentially over chalcopyrite leaching 7-10% Cu, 68-76% Zn, and 10-22% Fe from the ore in 18 days. The sulfur grown T. thiooxidans isolates leached Zn much more slowly and very little Fe, with a Cu-Zn extraction ratio twice the value obtained with T. ferrooxidans. The ore adapted T. ferrooxidans started solubilizing Cu and Zn without a lag period. The ore-adapted T. thiooxidans extracted Cu as well as T. ferrooxidans, but the extraction of Zn or Fe was still much slower in the low-phosphate medium, while in the high-phosphate medium it approached the value obtained with T. ferrooxidans. A high Cu-Zn extraction ratio of 0.34 was obtained with T. thiooxidans in the low phosphate medium. In the mixed-culture experiments with T. ferrooxidans and T. thiooxidans, the culture behaved as T. thiooxidans in the low-phosphate medium with a higher Cu-Zn extraction ratio and as T. ferrooxidans in the high-phosphate medium with a lower Cu-Zn extraction ratio. It is concluded that T. ferrooxidans and T. thiooxidans solubilize sulfide minerals by different mechanisms.     

A new look at microbial leaching patterns on sulfide minerals

Leaching patterns on sulfide minerals were investigated by high-resolution scanning electron microscopy (SEM). Our goal was to evaluate the relative contributions of inorganic surface reactions and reactions localized by attached cells to surface morphology evolution. Experiments utilized pyrite (FeS(2)), marcasite (FeS(2)) and arsenopyrite (FeAsS), and two iron-oxidizing prokaryotes in order to determine the importance of cell type, crystal structure, and mineral dissolution rate in microbially induced pit formation. Pyrite surfaces were reacted with the iron-oxidizing bacterium Acidithiobacillus ferrooxidans (at 25 degrees C), the iron-oxidizing archaeon 'Ferroplasma acidarmanus' (at 37 degrees C), and abiotically in the presence of Fe(3+) ions. In all three experiments, discrete bacillus-sized (1-2 μm) and -shaped (elliptical) pits developed on pyrite surfaces within 1 week of reaction. Results show that attaching cells are not necessary for pit formation on pyrite. Marcasite and arsenopyrite surfaces were reacted with A. ferrooxidans (at 25 degrees C) and 'F. acidarmanus' (at 37 degrees C). Cell-sized and cell-shaped dissolution pits were not observed on marcasite or arsenopyrite at any point during reaction with A. ferrooxidans, or on marcasite surfaces reacted with 'F. acidarmanus'. However, individual 'F. acidarmanus' cells were found within individual shallow (<0.5 μm deep) pits. The size and shape (round rather than elliptical) of the pits conformed closely to the shape of F. acidarmanus (cells) pits on arsenopyrite. We infer these pits to be cell-induced. We attribute the formation of pits readily detectable (by SEM) to the higher reactivity of arsenopyrite compared to pyrite and marcasite under the conditions the experiment was conducted. These pits contributed little to the overall surface topographical evolution, and most likely did not significantly increase surface area during reaction. Our results suggest that overall sulfide mineral dissolution may be dominated by surface reactions with Fe(3+) rather than by reactions at the cell-mineral interface.