Choice between autotrophy and heterotrophy in Pseudomonas oxalaticus. Growth in mixed substrates

Genomic Evidence for Formate Metabolism by Chloroflexi as the Key to Unlocking Deep Carbon in Lost City Microbial Ecosystems

Primitive forms of life may have originated around hydrothermal vents at the bottom of the ancient ocean. The Lost City hydrothermal vent field, fueled by just rock and water, provides an analog for not only primitive ecosystems but also potential extraterrestrial rock-powered ecosystems. The microscopic life covering the towering chimney structures at the Lost City has been previously documented, yet little is known about the carbon cycling in this ecosystem. These results provide a better understanding of how carbon from the deep subsurface can fuel rich microbial ecosystems on the seafloor.

The Lost City hydrothermal field on the Mid-Atlantic Ridge supports dense microbial life on the lofty calcium carbonate chimney structures. The vent field is fueled by chemical reactions between the ultramafic rock under the chimneys and ambient seawater. These serpentinization reactions provide reducing power (as hydrogen gas) and organic compounds that can serve as microbial food; the most abundant of these are methane and formate. Previous studies have characterized the interior of the chimneys as a single-species biofilm inhabited by the Lost City Methanosarcinales, but they also indicated that this methanogen is unable to metabolize formate. The new metagenomic results presented here indicate that carbon cycling in these Lost City chimney biofilms could depend on the metabolism of formate by Chloroflexi populations. Additionally, we present evidence for metabolically diverse, formate-utilizing Sulfurovum populations and new genomic and phylogenetic insights into the unique Lost City Methanosarcinales.

IMPORTANCE Primitive forms of life may have originated around hydrothermal vents at the bottom of the ancient ocean. The Lost City hydrothermal vent field, fueled by just rock and water, provides an analog for not only primitive ecosystems but also potential extraterrestrial rock-powered ecosystems. The microscopic life covering the towering chimney structures at the Lost City has been previously documented, yet little is known about the carbon cycling in this ecosystem. These results provide a better understanding of how carbon from the deep subsurface can fuel rich microbial ecosystems on the seafloor.

Isolation and characterization of oxalotrophic bacteria from tropical soils

The oxalate-carbonate pathway (OCP) is a biogeochemical set of reactions that involves the conversion of atmospheric CO2 fixed by plants into biomass and, after the biological recycling of calcium oxalate by fungi and bacteria, into calcium carbonate in terrestrial environments. Oxalotrophic bacteria are a key element of this process because of their ability to oxidize calcium oxalate. However, the diversity and alternative carbon sources of oxalotrophs participating to this pathway are unknown. Therefore, the aim of this study was to characterize oxalotrophic bacteria in tropical OCP systems from Bolivia, India, and Cameroon. Ninety-five oxalotrophic strains were isolated and identified by sequencing of the 16S rRNA gene. Four genera corresponded to newly reported oxalotrophs (Afipia, Polaromonas, Humihabitans, and Psychrobacillus). Ten strains were selected to perform a more detailed characterization. Kinetic curves and microcalorimetry analyses showed that Variovorax soli C18 has the highest oxalate consumption rate with 0.240 µM h(-1). Moreover, Streptomyces achromogenes A9 displays the highest metabolic plasticity. This study highlights the phylogenetic and physiological diversity of oxalotrophic bacteria in tropical soils under the influence of the oxalate-carbonate pathway.

Identification of active oxalotrophic bacteria by Bromodeoxyuridine DNA labeling in a microcosm soil experiments

The oxalate-carbonate pathway (OCP) leads to a potential carbon sink in terrestrial environments. This process is linked to the activity of oxalotrophic bacteria. Although isolation and molecular characterizations are used to study oxalotrophic bacteria, these approaches do not give information on the active oxalotrophs present in soil undergoing the OCP. The aim of this study was to assess the diversity of active oxalotrophic bacteria in soil microcosms using the Bromodeoxyuridine (BrdU) DNA labeling technique. Soil was collected near an oxalogenic tree (Milicia excelsa). Different concentrations of calcium oxalate (0.5%, 1%, and 4% w/w) were added to the soil microcosms and compared with an untreated control. After 12 days of incubation, a maximal pH of 7.7 was measured for microcosms with oxalate (initial pH 6.4). At this time point, a DGGE profile of the frc gene was performed from BrdU-labeled soil DNA and unlabeled soil DNA. Actinobacteria (Streptomyces- and Kribbella-like sequences), Gammaproteobacteria and Betaproteobacteria were found as the main active oxalotrophic bacterial groups. This study highlights the relevance of Actinobacteria as members of the active bacterial community and the identification of novel uncultured oxalotrophic groups (i.e. Kribbella) active in soils.

Use of an isothermal microcalorimetry assay to characterize microbial oxalotrophic activity

Isothermal microcalorimetry (IMC) has been used in the past to monitor metabolic activities in living systems. A few studies have used it on ecological research. In this study, IMC was used to monitor oxalotrophic activity, a widespread bacterial metabolism found in the environment, and particularly in soils. Six model strains were inoculated in solid angle media with K-oxalate as the sole carbon source. Cupriavidus oxalaticus, Cupriavidus necator, and Streptomyces violaceoruber presented the highest activity (91, 40, and 55 μW, respectively) and a maximum growth rate (μmax h(-1) ) of 0.264, 0.185, and 0.199, respectively, among the strains tested. These three strains were selected to test the incidence of different oxalate sources (Ca, Cu, and Fe-oxalate salts) in the metabolic activity. The highest activity was obtained in Ca-oxalate for C. oxalaticus. Similar experiments were carried out with a model soil to test whether this approach can be used to measure oxalotrophic activity in field samples. Although measuring oxalotrophic activity in a soil was challenging, there was a clear effect of the amendment with oxalate on the metabolic activity measured in soil. The correlation between heat flow and growth suggests that IMC analysis is a powerful method to monitor bacterial oxalotrophic activity.

Choice between autotrophy and heterotrophy in Pseudomonas oxalaticus. Utilization of oxalate by cells after adaptation from growth on formate to growth on oxalate

1. The labelling patterns of phosphoglycerate obtained from formate-grown or oxalate-grown Pseudomonas oxalaticus after exposure for 15sec. to [(14)C]formate or [(14)C]oxalate respectively were determined. 2. The phosphoglycerate obtained from the formate-grown cells contained 78% of the radioactivity in the carboxyl group. This is in accord with that predicted for operation of the ribulose diphosphate cycle of carbon dioxide fixation. 3. The labelling pattern of the phosphoglycerate obtained from the oxalate-grown cells approached uniformity, as predicted for the heterotrophic pathway of oxalate assimilation. The departure from complete uniformity may have been due to concurrent (14)CO(2) fixation into C(4) dicarboxylic acids. 4. The labelling pattern of phosphoglycerate obtained from cells that had just started to grow on oxalate after adaptation from formate was determined after incubation of the cells for 15sec. with [(14)C]oxalate. This pattern approached uniformity. 5. The pathway of incorporation of (14)CO(2) into cells that had just started to grow on oxalate after adaptation from formate, in the presence of either formate or oxalate as energy source, was studied by chromatographic and radio-autographic analysis. 6. It is concluded from the isotopic data that a mixed heterotrophic-autotrophic metabolism, with the former mode predominating, operates in the initial stages of growth on oxalate after adaptation from growth on formate.

Oxalotrophic bacteria

Oxalic acid and its salts are widespread in nature, as they are produced by many species of plants, algae and fungi. The bacteria, which are capable of using oxalate as a sole carbon and energy source, are described as being "oxalotrophic". Oxalotrophic bacteria do not constitute a homogeneous taxonomic group, but they do constitute a well-defined physiological group. A limited number of aerobic bacteria which are able to utilize oxalate as sole carbon and energy source have been completely described. Most of them are facultative methylotrophs and/or facultative hydrogen-oxidizing chemolithoautotrophs. In this review, the current status of the taxonomy and biodiversity of oxalotrophic bacteria in various environments, and aspects of their biotechnological potential, are briefly summarized.

Isolation and characterization of a new type of aerobic, oxalic acid utilizing bacteria, and proposal of Oxalicibacterium flavum gen. nov., sp. nov

A mesophilic, aerobic oxalic acid utilizing yellow-pigmented bacterium has been isolated from litter of oxalate producing plants in the region of Izmir (Turkey). It is motile by means of 1-3 polar flagella. Optimal growth occurred between 25-30 degrees C at pH 6.9. The G+C content of DNA is 62-64 mol % (Tm). Based on its morphological and biochemical features the organism belongs to the genus Pseudomonas, but differs from all the previously described species. The taxonomic relationships among strains described as or previously tentatively assigned to the genus Pseudomonas were investigated using numerical classification, DNA base composition and DNA-DNA hybridization. 16S rDNA sequences were determined for the strain TA17. On the basis of 16S rDNA sequence comparisons, physiological and biochemical characteristics, it is proposed to classify TA17T in a new genus and species for which the name Oxalicibacterium flavum gen. nov., sp. nov. is proposed. The type strain is TA17T (= NEU98T, = LMG 21571T).

Inactivation of clostridial ferredoxin and pyruvate-ferredoxin oxidoreductase by sodium nitrite

Clostridial ferredoxin and pyruvate-ferredoxin oxidoreductase activity was investigated after in vitro or in vivo treatment with sodium nitrite. In vitro treatment of commercially available Clostridium pasteurianum ferredoxin with sodium nitrite inhibited ferredoxin activity. Inhibition of ferredoxin activity increased with increasing levels of sodium nitrite. Ferredoxin was isolated from normal C. pasteurianum and Clostridium botulinum cultures and from cultures incubated with 1,000 micrograms of sodium nitrite per ml for 45 min. The activity of in vivo nitrite-treated ferredoxin was decreased compared with that of control ferredoxin. Pyruvate-ferredoxin oxidoreductase isolated from C. botulinum cultures incubated with 1,000 micrograms of sodium nitrite per ml showed less activity than did control oxidoreductase. It is concluded that the antibotulinal activity of nitrite is due at least in part to inactivation of ferredoxin and pyruvate-ferredoxin oxidoreductase.

Metabolic regulation in Pseudomonas oxalaticus OX1. Enzyme and coenzyme concentration changes during substrate transition experiments

Metabolic control associated with diauxic growth of Pseudomonas oxalaticus in batch cultures on mixtures of formate and oxalate was investigated by measuring intracellular enzyme and coenzyme concentrations and QO2 values during transition experiments from oxalate to formate and vice versa. In transition from oxalate to formate oxalyl-CoA reductase concentration declined after the exhaustion of oxalate and ribulose-1,5-diphosphate carboxylase and 14CO2 fixation appeared upon addition of formate. In the reciprocal transition, ribulose-1,5-diphosphate carboxylase and 14CO2 fixation rate declined sharply after formate exhaustion, and oxalyl-CoA reductase appeared only after addition of oxalate. The intracellular NAD and NADP concentrations measured in the same experiments are reported. At substrate exhaustion the proportion of NAD in the reduced form fell from 15-20% to 2%. On addition of formate to an oxalate-starved culture there was an immediate increase in the proportion of NADH to 50%; such an increase was not observed in the reverse experiment.

Oxalate, formate, formamide, and methanol metabolism in Thiobacillus novellus

Thiobacillus novellus was able to grow with oxalate, formate, formamide, and methanol as sole sources of carbon and energy. Extensive growth on methanol required yeast extract or vitamins. Glyoxylate carboligase was detected in extracts of oxalate-grown cells. Ribulose bisphosphate carboxylase was found in extracts of cells grown on formate, formamide, and thiosulfate. These data indicate that oxalate is utilized heterotrophically in the glycerate pathway, and formate and formamide are utilized autotrophically in the ribulose bisphosphate pathway. Nicotinamide adenine dinucleotide-linked formate dehydrogenase was present in extracts of oxalate-, formate-, formamide-, and methanol-grown cells but was absent in thiosulfate- and acetate-grown cells.

Lipoic acid content of Escherichia coli and other microorganisms

A mutant strain of Escherichia coli K-12 requiring lipoic acid. W1485lip 2 (ATCC 25645), was used to develop a turbidimetric assay for lipoic acid and a polarographic assay based on the oxidation of pyruvate by suspensions of lipoic acid-deficient organisms. The turbidmetric assay was more sensitive with a working range equivalent to 0.2-2.0 ng of DL-alpha-lipoic acid compared with 5-50 ng for the polarographic method. The mutant responded equally to racemic mixtures of alpha-lipoic acid, beta-lipoic acid and dihydrolipoic acid but gave little response to lipoamide, and other derivatives without prior hydrolysis; 8-methyllipoic acid was a competitive inhibitor of the response to lipoic acid. A high specificity of the mutant for the natural steroisomer was indicated by the fact that (+)-alpha-lipoic acid had twice the activity of the racemic mixture. Escherichia coli K12 contained less than 0.05 ng of free (+)-alpha-lipoic acid per mg dry weight but, depending on the growth substrate, the equivalent of between 13 and 47 ng of (+)-alpha-lipoic acid per mg dry weight after acid extraction. There was a strong correlation between the lipoic acid content and the sum of the specific activities for the pyruvate and alpha-ketoglutarate dehydrogenase complexes. Experiments with washed suspensions of Escherichia coli showed only small increases in lipoic acid content (18%) when incubated with pyruvate, cysteine and methionine. When supplied with exogenous lipoic acid the mutant, W1485lip2, accumulated very little more than was demanded by its metabolism. The lipoic acid contents of several organisms were measured and correlated with their metabolism.

Oxalate and formate in Alcaligenes and Pseudomonas species

Oxalate is metabolized by the glycerate pathway involving glyoxylate carboligase in Alcaligenes LOx and Pseudomonas KOx, and by the serine pathway involving hydroxypyruvate reductase in Ps.MOx and Ps.AM1 (var. 470). Although A.LOx does not grow on formate, stimulation of growth was observed in the presence of amino acids and a few Kreb's cycle intermediates. A.LOx possesses two different mechanisms for the oxidation of formate: (1) the constitutive formate oxidase which is present in the particulate fraction of oxalate-grown and succinate-plus-formate-grown cells; (2) the inducible NAD-linked formate dehydrogenase present in the 100 000 x g supernatant fraction of the cell-free extracts of oxalate-grown cells alone. The two systems occur simultaneously in oxalate-grown cells. The effect of inhibitors on formate oxidase activity and the other enzyme activities of the particulate formate-oxidizing fraction indicate that the oxidation of formate is linked to the respiratory chain.

Regulation of pathways degrading aromatic substrates in Pseudomonas putida. Enzymic response to binary mixtures of substrates

1. Induction constants (K(ind)) and repression constants (K(rep)), which are a measure of the affinity of the inducers or repressors for the induction systems, were measured for mandelate, benzoate and p-hydroxybenzoate in Pseudomonas putida. 2. From these results, the enzymic response of the organism to media containing pairs of these substrates was predicted. Nitrogen-limited chemostats, operated at high growth rates, were used to investigate these predictions in cells grown first on one aromatic substrate with the second added later. 3. In general, the values of K(ind) and K(rep) predicted quite accurately the response to substrate mixtures. Thus, in the presence of mandelate and either benzoate or p-hydroxybenzoate, the enzymes of mandelate metabolism were repressed almost completely, and the bacteria were fully induced for the alternative substrate (benzoate or p-hydroxybenzoate), which was preferentially utilized for growth. When benzoate and p-hydroxybenzoate were the two substrates in the mixture, the enzymes for metabolism of the latter were strongly repressed and growth took place mainly on benzoate. 4. The enzymic response to mixed substrates did not result in the metabolism of the better growth substrate, but in the substrate requiring the synthesis of fewer enzymes. Thus benzoate is used in preference to mandelate although the latter supports a faster growth rate. It is nevertheless considered that, with our present knowledge of the natural habitat of the organism, it is impossible to decide whether protein economy or growth rate was the factor determining the evolution of this control system.

Microbial growth on oxalate by a route not involving glyoxylate carboligase

1. The metabolism of oxalate by the pink-pigmented organisms, Pseudomonas AM1, Pseudomonas AM2, Protaminobacter ruber and Pseudomonas extorquens has been compared with that of the non-pigmented Pseudomonas oxalaticus. 2. During growth on oxalate, all the organisms contain oxalyl-CoA decarboxylase, formate dehydrogenase and oxalyl-CoA reductase. This is consistent with oxidation of oxalate to carbon dioxide taking place via oxalyl-CoA, formyl-CoA and formate as intermediates, and also reduction of oxalate to glyoxylate taking place via oxalyl-CoA. 3. The pink-pigmented organisms, when grown on oxalate, contain l-serine-glyoxylate aminotransferase and hydroxypyruvate reductase but do not contain glyoxylate carboligase. The converse of this obtains in oxalate-grown Ps. oxalaticus. This indicates that, in contrast with Ps. oxalaticus, synthesis of C(3) compounds from oxalate by the pink-pigmented organisms occurs by a variant of the ;serine pathway' used by Pseudomonas AM1 during growth on C(1) compounds. 4. Evidence in favour of this scheme is provided by the finding that a mutant of Pseudomonas AM1 that lacks hydroxypyruvate reductase is not able to grow on oxalate.