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Mike S M Jetten

Publications and source records attributed to Mike S M Jetten.

At least 19 recordsLinked to original sources

Expression and characterisation of a major c-type cytochrome encoded by gene kustc0563 from Kuenenia stuttgartiensis as a recombinant protein in Escherichia coli.

The purification of small quantities of a major small c-type cytochrome from the anammox bacterium Kuenenia stuttgartiensis has recently been reported. In order to characterise this protein further we have expressed the gene encoding this cytochrome in Escherichia coli and have purified the protein to homogeneity. The protein is directed to the E. coli periplasm using its native signal sequence suggesting that it may be translocated via a Sec-type system in K. stuttgartiensis. The cytochrome has the visible spectroscopic properties typical of a low-spin c-type cytochrome, but these spectroscopic features broaden in high salt solutions. The oxidised cytochrome was able to bind the ligands NO and cyanide. A redox potential of +230 mV suggests that the protein is suitable to act as an electron carrier protein that may be involved in the respiratory chain between hydrazine oxidation and the reduction of nitrite. The predicted protein sequence for the cytochrome suggests it to be a predominantly alpha-helical protein, and this is supported by circular dichroism.

Bacteria, Anaerobic↗

Evidence for complete denitrification in a benthic foraminifer.

Benthic foraminifera are unicellular eukaryotes found abundantly in many types of marine sediments. Many species survive and possibly reproduce in anoxic habitats, but sustainable anaerobic metabolism has not been previously described. Here we demonstrate that the foraminifer Globobulimina pseudospinescens accumulates intracellular nitrate stores and that these can be respired to dinitrogen gas. The amounts of nitrate detected are estimated to be sufficient to support respiration for over a month. In a Swedish fjord sediment where G. pseudospinescens is the dominant foraminifer, the intracellular nitrate pool in this species accounted for 20% of the large, cell-bound, nitrate pool present in an oxygen-free zone. Similarly high nitrate concentrations were also detected in foraminifera Nonionella cf. stella and a Stainforthia species, the two dominant benthic taxa occurring within the oxygen minimum zone of the continental shelf off Chile. Given the high abundance of foraminifera in anoxic marine environments, these new findings suggest that foraminifera may play an important role in global nitrogen cycling and indicate that our understanding of the complexity of the marine nitrogen cycle is far from complete.

Anaerobiosis↗

Adaptation of a freshwater anammox population to high salinity wastewater.

For the successful application of anaerobic ammonium oxidation (anammox) in wastewater practice it is important to know how to seed new anammox reactors with biomass from existing reactors. In this study, a new high salinity anammox reactor was inoculated with biomass from a freshwater system. The changes in activity and population shifts were monitored. It was shown that freshwater anammox bacteria could adapt to salt concentrations as high as 30 gl(-1) provided the salt concentration was gradually increased. Higher salt concentrations reversibly inhibited anammox bacteria. The nitrogen removal efficiency and maximum anammox activity of the salt adapted sludge was very similar to the reference freshwater sludge. Fluorescence in situ hybridization analysis revealed that the freshwater anammox species Candidatus "Kuenenia stuttgartiensis" was the dominant in both salt adapted sludge and freshwater sludge. These results show that gradual adaptation may be the key to successful seeding of anammox bioreactors.

Acclimatization↗

Candidatus "Anammoxoglobus propionicus" a new propionate oxidizing species of anaerobic ammonium oxidizing bacteria.

The bacteria that mediate the anaerobic oxidation of ammonium (anammox) are detected worldwide in natural and man-made ecosystems, and contribute up to 50% to the loss of inorganic nitrogen in the oceans. Two different anammox species rarely live in a single habitat, suggesting that each species has a defined but yet unknown niche. Here we describe a new anaerobic ammonium oxidizing bacterium with a defined niche: the co-oxidation of propionate and ammonium. The new anammox species was enriched in a laboratory scale bioreactor in the presence of ammonium and propionate. Interestingly, this particular anammox species could out-compete other anammox bacteria and heterotrophic denitrifiers for the oxidation of propionate in the presence of ammonium, nitrite and nitrate. We provisionally named the new species Candidatus "Anammoxoglobus propionicus".

Bacteria, Anaerobic↗

A microbial consortium couples anaerobic methane oxidation to denitrification.

Modern agriculture has accelerated biological methane and nitrogen cycling on a global scale. Freshwater sediments often receive increased downward fluxes of nitrate from agricultural runoff and upward fluxes of methane generated by anaerobic decomposition. In theory, prokaryotes should be capable of using nitrate to oxidize methane anaerobically, but such organisms have neither been observed in nature nor isolated in the laboratory. Microbial oxidation of methane is thus believed to proceed only with oxygen or sulphate. Here we show that the direct, anaerobic oxidation of methane coupled to denitrification of nitrate is possible. A microbial consortium, enriched from anoxic sediments, oxidized methane to carbon dioxide coupled to denitrification in the complete absence of oxygen. This consortium consisted of two microorganisms, a bacterium representing a phylum without any cultured species and an archaeon distantly related to marine methanotrophic Archaea. The detection of relatives of these prokaryotes in different freshwater ecosystems worldwide indicates that the reaction presented here may make a substantial contribution to biological methane and nitrogen cycles.

Anaerobiosis↗

Deciphering the evolution and metabolism of an anammox bacterium from a community genome.

Anaerobic ammonium oxidation (anammox) has become a main focus in oceanography and wastewater treatment. It is also the nitrogen cycle's major remaining biochemical enigma. Among its features, the occurrence of hydrazine as a free intermediate of catabolism, the biosynthesis of ladderane lipids and the role of cytoplasm differentiation are unique in biology. Here we use environmental genomics--the reconstruction of genomic data directly from the environment--to assemble the genome of the uncultured anammox bacterium Kuenenia stuttgartiensis from a complex bioreactor community. The genome data illuminate the evolutionary history of the Planctomycetes and allow us to expose the genetic blueprint of the organism's special properties. Most significantly, we identified candidate genes responsible for ladderane biosynthesis and biological hydrazine metabolism, and discovered unexpected metabolic versatility.

Anaerobiosis↗

Challenging protein purification from anammox bacteria.

The anaerobic ammonium oxidation (anammox) is a fascinating microbial pathway contributing to the global biogeochemical nitrogen cycle. The anammox pathway of nitrogen conversion can only be elucidated after the responsible proteins have been purified and characterised. The anammox bacteria have a complex cell envelope consisting of protein and lipopolysaccharide and they grow in dense cell aggregates. Preparing cell extract and purifying proteins from the cell aggregates is hampered by the extracellular polymeric material and by gel formation. It was demonstrated that protein-protein (i.e. disulfide formation) as well as protein-polysaccharide interaction caused this gel formation in extracts. Cell extract gelled upon freezing/thawing and boiling. Additionally, proteins aggregated on various chromatography media upon concentration and during desalting. The polysaccharides clogged the matrix of chromatographic materials and the pores of ultrafiltration membranes. The precipitation of proteins and polysaccharides caused very low resolution and streaking on SDS- and two-dimensional polyacrylamide gels. The present work describes the potential causes for gel formation in anammox cell extracts. Optimized protocols for sample preparation for polyacrylamide gel electrophoresis and ion exchange chromatography are presented. High-resolution gel electrophoresis of the cell extract was achieved after clarification from polymeric substances with denaturating phenol extraction and the purification of a 10 kDa cytochrome c is presented as an example.

Ammonia↗

Evidence for the involvement of betaproteobacterial Thiobacilli in the nitrate-dependent oxidation of iron sulfide minerals.

The Thiobacilli are an important group of autotrophic bacteria occurring in nature linking the biogeochemical cycles of sulfur and nitrogen. Betaproteobacterial Thiobacilli are very likely candidates for mediating the process of nitrate-dependent anoxic iron sulfide mineral oxidation in freshwater wetlands. A Thiobacillus denitrificans-like bacterium was present in an enrichment on thiosulfate and nitrate, derived from an iron-sulfide- and nitrate-rich freshwater environment. Preliminary FISH analysis showed that the 16S rRNA gene-based bacterial probe mix showed great variation in intensity under different culture conditions. Furthermore, the widely applied 23S rRNA gene-based probe set BET42a/GAM42a incorrectly identified the T. denitrificans-like bacterium as a member of the Gammaproteobacteria. To circumvent these problems, the 23S rRNA genes of two T. denitrificans strains were partially sequenced and a new 23S rRNA gene-based probe (Betthio 1001) specific for betaproteobacterial Thiobacilli was designed. Use of this new probe Betthio 1001, combined with field measurements, indicates the involvement of Thiobacilli in the process of nitrate-dependent iron sulfide mineral oxidation.

Cells, Cultured↗

Ladderane phospholipids in anammox bacteria comprise phosphocholine and phosphoethanolamine headgroups.

Anammox bacteria present in wastewater treatment systems and marine environments are capable of anaerobically oxidizing ammonium to dinitrogen gas. This anammox metabolism takes place in the anammoxosome which membrane is composed of lipids with peculiar staircase-like 'ladderane' hydrocarbon chains that comprise three or four linearly concatenated cyclobutane structures. Here, we applied high-performance liquid chromatography coupled to electrospray ionization tandem mass spectrometry and matrix-assisted laser desorption/ionization time-of-flight mass spectrometry to elucidate the full identity of these ladderane lipids. This revealed a wide variety of ladderane lipid species with either a phosphocholine or phosphoethanolamine polar headgroup attached to the glycerol backbone. In addition, in silico analysis of genome data gained insight into the machinery for the biosynthesis of the phosphocholine and phosphoethanolamine phospholipids in anammox bacteria.

Bacteria↗

Expression of the urease gene of Agaricus bisporus: a tool for studying fruit body formation and post-harvest development.

Fruit body initials of Agaricus bisporus contain high levels of urea, which decrease in the following developmental stages until stage 4 (harvest) when urea levels increase again. At storage, the high urea content may affect the quality of the mushroom, i.e. by the formation of ammonia from urea through the action of urease (EC 3.5.1.5). Despite the abundance of urea in the edible mushroom A. bisporus, little is known about its physiological role. The urease gene of A. bisporus and its promoter region were identified and cloned. The coding part of the genomic DNA was interrupted by nine introns as confirmed by cDNA analysis. The first full homobasidiomycete urease protein sequence obtained comprised 838 amino acids (molecular mass 90,694 Da, pI 5.8). An alignment with fungal, plant and bacterial ureases revealed a high conservation. The expression of the urease gene, measured by Northern analyses, was studied both during normal development of fruit bodies and during post-harvest senescence. Expression in normal development was significantly up-regulated in developmental stages 5 and 6. During post-harvest senescence, the expression of urease was mainly observed in the stipe tissue; expression decreased on the first day and remained at a basal level through the remaining sampling period.

Agaricus↗

Competition and coexistence of aerobic ammonium- and nitrite-oxidizing bacteria at low oxygen concentrations.

In natural and man-made ecosystems nitrifying bacteria experience frequent exposure to oxygen-limited conditions and thus have to compete for oxygen. In several reactor systems (retentostat, chemostat and sequencing batch reactors) it was possible to establish co-cultures of aerobic ammonium- and nitrite-oxidizing bacteria at very low oxygen concentrations (2-8 microM) provided that ammonium was the limiting N compound. When ammonia was in excess of oxygen, the nitrite-oxidizing bacteria were washed out of the reactors, and ammonium was converted to mainly nitrite, nitric oxide and nitrous oxide by Nitrosomonas-related bacteria. The situation could be rapidly reversed by adjusting the oxygen to ammonium ratio in the reactor. In batch and continuous tests, no inhibitory effect of ammonium, nitric oxide or nitrous oxide on nitrite-oxidizing bacteria could be detected in our studies. The recently developed oxygen microsensors may be helpful to determine the kinetic parameters of the nitrifying bacteria, which are needed to make predictive kinetic models of their competition.

Ammonia↗

A new soluble 10kDa monoheme cytochrome c-552 from the anammox bacterium Candidatus "Kuenenia stuttgartiensis".

The chemolithoautotrophic anammox bacterium Candidatus "Kuenenia stuttgartiensis" grows anaerobically using ammonium as electron donor for nitrite reduction. More than 10% of the proteins in cell extracts of "K. stuttgartiensis" consist of c-type heme proteins. A 10kDa soluble cytochrome c was purified from cell extracts using ultracentrifugation and anion exchange chromatography. The UV/Vis spectrum of the reduced cytochrome showed the gamma, beta and alpha absorption maxima at 419, 522 and 552nm, respectively. The N-terminal amino acid sequence and peptide fragments of the tryptic digest of the protein were used to identify the corresponding gene. Analysis of the gene product showed that the protein was preceded by a 30 amino acids long leader sequence and that it belonged to the low-spin class ID cytochrome c. The CXXCH motive was located at the N-terminal site of the protein. The gene organization of the cytochrome showed some resemblance to cytochrome c clusters of unknown function in the genome of Nitrosomonas europaea and Geobacter sulfurreducens PCA.

Amino Acid Sequence↗

Methanotrophic symbionts provide carbon for photosynthesis in peat bogs.

Wetlands are the largest natural source of atmospheric methane, the second most important greenhouse gas. Methane flux to the atmosphere depends strongly on the climate; however, by far the largest part of the methane formed in wetland ecosystems is recycled and does not reach the atmosphere. The biogeochemical controls on the efficient oxidation of methane are still poorly understood. Here we show that submerged Sphagnum mosses, the dominant plants in some of these habitats, consume methane through symbiosis with partly endophytic methanotrophic bacteria, leading to highly effective in situ methane recycling. Molecular probes revealed the presence of the bacteria in the hyaline cells of the plant and on stem leaves. Incubation with (13)C-methane showed rapid in situ oxidation by these bacteria to carbon dioxide, which was subsequently fixed by Sphagnum, as shown by incorporation of (13)C-methane into plant sterols. In this way, methane acts as a significant (10-15%) carbon source for Sphagnum. The symbiosis explains both the efficient recycling of methane and the high organic carbon burial in these wetland ecosystems.

Carbon↗

Protein complexes in the archaeon Methanothermobacter thermautotrophicus analyzed by blue native/SDS-PAGE and mass spectrometry.

Methanothermobacter thermautotrophicus is a thermophilic archaeon that produces methane as the end product of its primary metabolism. The biochemistry of methane formation has been extensively studied and is catalyzed by individual enzymes and proteins that are organized in protein complexes. Although much is known of the protein complexes involved in methanogenesis, only limited information is available on the associations of proteins involved in other cell processes of M. thermautotrophicus. To visualize and identify interacting and individual proteins of M. thermautotrophicus on a proteome-wide scale, protein preparations were separated using blue native electrophoresis followed by SDS-PAGE. A total of 361 proteins, corresponding to almost 20% of the predicted proteome, was identified using peptide mass fingerprinting after MALDI-TOF MS. All previously characterized complexes involved in energy generation could be visualized. Furthermore the expression and association of the heterodisulfide reductase and methylviologen-reducing hydrogenase complexes depended on culture conditions. Also homomeric supercomplexes of the ATP synthase stalk subcomplex and the N5-methyl-5,6,7,8-tetrahydromethanopterin:coenzyme M methyltransferase complex were separated. Chemical cross-linking experiments confirmed that the multimerization of both complexes was not experimentally induced. A considerable number of previously uncharacterized protein complexes were reproducibly visualized. These included an exosome-like complex consisting of four exosome core subunits, which associated with a tRNA-intron endonuclease, thereby expanding the constituency of archaeal exosomes. The results presented show the presence of novel complexes and demonstrate the added value of including blue native gel electrophoresis followed by SDS-PAGE in discovering protein complexes that are involved in catabolic, anabolic, and general cell processes.

Archaeal Proteins↗

Massive nitrogen loss from the Benguela upwelling system through anaerobic ammonium oxidation.

In many oceanic regions, growth of phytoplankton is nitrogen-limited because fixation of N2 cannot make up for the removal of fixed inorganic nitrogen (NH4+, NO2-, and NO3-) by anaerobic microbial processes. Globally, 30-50% of the total nitrogen loss occurs in oxygen-minimum zones (OMZs) and is commonly attributed to denitrification (reduction of nitrate to N2 by heterotrophic bacteria). Here, we show that instead, the anammox process (the anaerobic oxidation of ammonium by nitrite to yield N2) is mainly responsible for nitrogen loss in the OMZ waters of one of the most productive regions of the world ocean, the Benguela upwelling system. Our in situ experiments indicate that nitrate is not directly converted to N2 by heterotrophic denitrification in the suboxic zone. In the Benguela system, nutrient profiles, anammox rates, abundances of anammox cells, and specific biomarker lipids indicate that anammox bacteria are responsible for massive losses of fixed nitrogen. We have identified and directly linked anammox bacteria to the removal of fixed inorganic nitrogen in the OMZ waters of an open-ocean setting. We hypothesize that anammox could also be responsible for substantial nitrogen loss from other OMZ waters of the ocean.

Atlantic Ocean↗

Structural identification of ladderane and other membrane lipids of planctomycetes capable of anaerobic ammonium oxidation (anammox).

The membrane lipid composition of planctomycetes capable of the anaerobic oxidation of ammonium (anammox), i.e. Candidatus'Brocadia anammoxidans' and Candidatus'Kuenenia stuttgartiensis', was shown to be composed mainly of so-called ladderane lipids. These lipids are comprised of three to five linearly concatenated cyclobutane moieties with cis ring junctions, which occurred as fatty acids, fatty alcohols, alkyl glycerol monoethers, dialkyl glycerol diethers and mixed glycerol ether/esters. The highly strained ladderane moieties were thermally unstable, which resulted in breakdown during their analysis with GC. This was shown by isolation of a thermal product of these ladderanes and subsequent analysis with two-dimensional NMR techniques. Comprehensive MS and relative retention time data for all the encountered ladderane membrane lipids is reported, allowing the identification of ladderanes in other bacterial cultures and in the environment. The occurrence of ladderane lipids seems to be limited to the specific phylogenetic clade within the Planctomycetales able to perform anammox. This was consistent with their proposed biochemical function, namely as predominant membrane lipids of the so-called anammoxosome, the specific organelle where anammox catabolism takes place in the cell.

Anaerobiosis↗

Propionate oxidation by and methanol inhibition of anaerobic ammonium-oxidizing bacteria.

Anaerobic ammonium oxidation (anammox) is a recently discovered microbial pathway and a cost-effective way to remove ammonium from wastewater. Anammox bacteria have been described as obligate chemolithoautotrophs. However, many chemolithoautotrophs (i.e., nitrifiers) can use organic compounds as a supplementary carbon source. In this study, the effect of organic compounds on anammox bacteria was investigated. It was shown that alcohols inhibited anammox bacteria, while organic acids were converted by them. Methanol was the most potent inhibitor, leading to complete and irreversible loss of activity at concentrations as low as 0.5 mM. Of the organic acids acetate and propionate, propionate was consumed at a higher rate (0.8 nmol min(-1) mg of protein(-1)) by Percoll-purified anammox cells. Glucose, formate, and alanine had no effect on the anammox process. It was shown that propionate was oxidized mainly to CO(2), with nitrate and/or nitrite as the electron acceptor. The anammox bacteria carried out propionate oxidation simultaneously with anaerobic ammonium oxidation. In an anammox enrichment culture fed with propionate for 150 days, the relative amounts of anammox cells and denitrifiers did not change significantly over time, indicating that anammox bacteria could compete successfully with heterotrophic denitrifiers for propionate. In conclusion, this study shows that anammox bacteria have a more versatile metabolism than previously assumed.

Bacteria, Anaerobic↗