Kinetics of ferrous iron oxidation by batch and continuous cultures of thermoacidophilic Archaea at extremely low pH of 1.1-1.3.

The extreme acid conditions required for scorodite (FeAsO4·2H2O) biomineralization (pH below 1.3) are suboptimal for growth of most thermoacidophilic Archaea. With the objective to develop a continuous process suitable for biomineral production, this research focuses on growth kinetics of thermoacidophilic Archaea at low pH conditions. Ferrous iron oxidation rates were determined in batch-cultures at pH 1.3 and a temperature of 75°C for Acidianus sulfidivorans, Metallosphaera prunea and a mixed Sulfolobus culture. Ferrous iron and CO2 in air were added as sole energy and carbon source. The highest growth rate (0.066 h⁻¹) was found with the mixed Sulfolobus culture. Therefore, this culture was selected for further experiments. Growth was not stimulated by increase of the CO2 concentration or by addition of sulphur as an additional energy source. In a CSTR operated at the suboptimal pH of 1.1, the maximum specific growth rate of the mixed culture was 0.022 h⁻¹, with ferrous iron oxidation rates of 1.5 g L⁻¹ d⁻¹. Compared to pH 1.3, growth rates were strongly reduced but the ferrous iron oxidation rate remained unaffected. Influent ferrous iron concentrations above 6 g L⁻¹ caused instability of Fe²âº oxidation, probably due to product (Fe³âº) inhibition. Ferric-containing, nano-sized precipitates of K-jarosite were found on the cell surface. Continuous cultivation stimulated the formation of an exopolysaccharide-like substance. This indicates that biofilm formation may provide a means of biomass retention. Our findings showed that stable continuous cultivation of a mixed iron-oxidizing culture is feasible at the extreme conditions required for continuous biomineral formation.

Isolation and distribution of a novel iron-oxidizing crenarchaeon from acidic geothermal springs in Yellowstone National Park.

Novel thermophilic crenarchaea have been observed in Fe(III) oxide microbial mats of Yellowstone National Park (YNP); however, no definitive work has identified specific microorganisms responsible for the oxidation of Fe(II). The objectives of the current study were to isolate and characterize an Fe(II)-oxidizing member of the Sulfolobales observed in previous 16S rRNA gene surveys and to determine the abundance and distribution of close relatives of this organism in acidic geothermal springs containing high concentrations of dissolved Fe(II). Here we report the isolation and characterization of the novel, Fe(II)-oxidizing, thermophilic, acidophilic organism Metallosphaera sp. strain MK1 obtained from a well-characterized acid-sulfate-chloride geothermal spring in Norris Geyser Basin, YNP. Full-length 16S rRNA gene sequence analysis revealed that strain MK1 exhibits only 94.9 to 96.1% sequence similarity to other known Metallosphaera spp. and less than 89.1% similarity to known Sulfolobus spp. Strain MK1 is a facultative chemolithoautotroph with an optimum pH range of 2.0 to 3.0 and an optimum temperature range of 65 to 75 degrees C. Strain MK1 grows optimally on pyrite or Fe(II) sorbed onto ferrihydrite, exhibiting doubling times between 10 and 11 h under aerobic conditions (65 degrees C). The distribution and relative abundance of MK1-like 16S rRNA gene sequences in 14 acidic geothermal springs containing Fe(III) oxide microbial mats were evaluated. Highly related MK1-like 16S rRNA gene sequences (>99% sequence similarity) were consistently observed in Fe(III) oxide mats at temperatures ranging from 55 to 80 degrees C. Quantitative PCR using Metallosphaera-specific primers confirmed that organisms highly similar to strain MK1 comprised up to 40% of the total archaeal community at selected sites. The broad distribution of highly related MK1-like 16S rRNA gene sequences in acidic Fe(III) oxide microbial mats is consistent with the observed characteristics and growth optima of Metallosphaera-like strain MK1 and emphasizes the importance of this newly described taxon in Fe(II) chemolithotrophy in acidic high-temperature environments of YNP.

Metallosphaera sedula TA-2, a calditoglycerocaldarchaeol deletion strain of a thermoacidophilic archaeon.

A spherical thermoacidophilic archaeon, strain TA-2, was obtained from acidic hot springs located in Ohwaku Valley, Hakone, Japan. This isolate is an obligate aerobic chemoorganoheterotroph that grows optimally at about 75 degrees C, pH 2.8. The G + C content of DNA from TA-2 is 47 mol%. The 16S rRNA gene from TA-2 showed more than 99% similarity with those of Metallosphaera sedula and Metallosphaera prunae and less than 92% similarity with other members of the order Sulfolobales. DNA-DNA hybridization experiments showed more than 93% genomic DNA homology among TA-2, M. sedula DSM5348T, and M. prunae DSM10039T. However, TA-2 lacks calditoglycerocaldarchaeol derivatives, which are usually found in the membrane lipids of members of the order Sulfolobales. Therefore, calditoglycerocaldarchaeol may not be essential for survival in thermophilic and acidophilic environments. The isolate was deposited as Metallosphaera sedula TA-2 (JCM 9064, IFO 15160).

The alcohol dehydrogenase gene: distribution among Sulfolobales and regulation in Sulfolobus solfataricus.

The distribution of the alcohol dehydrogenase gene (adh) among different Archaea was investigated by Southern blot analysis revealing the potentiality of the adh gene as a specific marker for the genus Sulfolobus. Moreover, the in vivo expression of the adh gene from a new isolate of Sulfolobus solfataricus, G theta, was studied to investigate gene regulation in Archaea. Primer extension analysis allowed the identification of a single initiation site and the TATA box element. Comparison of the G theta adh promoter with the corresponding Ssadh (adh from S. solfataricus) and RC3adh (adh from Sulfolobus RC3) also revealed the presence of two putative regulatory inverted repeats at the 5' of the TATA element. Northern blot analysis and enzymatic assays demonstrated that the transcription and expression of the G theta adh gene is regulated by different carbon and energy sources or by the natural substrate of the ADH enzyme.