Beneficial effects of dynamic groundwater flow and redox conditions on Natural Attenuation of mono-, poly-, and NSO-heterocyclic hydrocarbons.

Natural Attenuation (NA) processes have been demonstrated to reduce pollutant loads at different contaminated groundwater sites world-wide and are increasingly considered in contaminated site management concepts. However, data are mainly available for steady state groundwater flow and stable redox conditions as well as pollutants listed in standard regulatory schemes. In this study, the influence of transient groundwater flow and redox conditions on NA was examined at a former gas works site near the river Rhine in Germany. The investigated 78 pollutants included 40 mono- and polyaromatic hydrocarbons (MAHs, PAHs) and 38 NSO-heterocyclic aromatic hydrocarbons (NSO-HET). In the highly polluted areas, the MAHs benzene, indene and indane, the PAHs naphthalene, acenaphthene, 1- and 2-methylnaphthalene and the NSO-HET 2-methylquinoline, carbazole, benzothiophene, dibenzofuran and benzofuran were predominant. Pollutant concentrations decreased with increasing distance from the sources of contamination. At the plume fringes, the MAHs benzene and indane, the PAH acenaphthene, the NSO-HET carbazole, 5-methylbenzothiophene, 2- and 3-methylbenzofuran and 2-methyldibenzofuran were predominant, indicating low retention and slow intrinsic biodegradation of these compounds. The influence of surface water on groundwater level, pollutant concentrations, and redox conditions in the monitoring wells was observed with a permanently installed groundwater sensor. The temporary availability of oxygen was observed at the plume fringes, resulting in aerobic and ferric iron reducing biodegradation processes. Field and laboratory data were used to set-up a groundwater flow and reactive transport model used for quantification of the field mass transfer rates. In conclusion, the study demonstrates that NA is effective under transient flow and redox conditions. A conceptual model and reactive transport simulation can facilitate the interpretation of pronounced fluctuations of pollutant concentration in monitoring wells. Based on the analysis of 78 pollutants, indane, indene and several NSO-HET like carbazole, benzothiophene and 2-methyldibenzofuran are recommended for monitoring at tar oil polluted sites, besides EPA-PAHs and BTEX.

Microbial processes during deposition and diagenesis of Banded Iron Formations.

Banded Iron Formations (BIFs) are marine chemical sediments consisting of alternating iron (Fe)-rich and silica (Si)-rich bands which were deposited throughout much of the Precambrian era. BIFs represent important proxies for the geochemical composition of Precambrian seawater and provide evidence for early microbial life. Iron present in BIFs was likely precipitated in the form of Fe3+ (Fe(III)) minerals, such as ferrihydrite (Fe(OH)3), either through the metabolic activity of anoxygenic photoautotrophic Fe2+ (Fe(II))-oxidizing bacteria (photoferrotrophs), by microaerophilic bacteria, or by the oxidation of dissolved Fe(II) by O2 produced by early cyanobacteria. However, in addition to oxidized Fe-bearing minerals such as hematite (FeIII 2O3), (partially) reduced minerals such as magnetite (FeIIFeIII 2O4) and siderite (FeIICO3) are found in BIFs as well. The presence of reduced Fe in BIFs has been suggested to reflect the reduction of primary Fe(III) minerals by dissimilatory Fe(III)-reducing bacteria, or by metamorphic (high pressure and temperature) reactions occurring in presence of buried organic matter. Here, we present the current understanding of the role of Fe-metabolizing bacteria in the deposition of BIFs, as well as competing hypotheses that favor an abiotic model for BIF deposition. We also discuss the potential abiotic and microbial reduction of Fe(III) in BIFs after deposition. Further, we review the availability of essential nutrients (e.g. P and Ni) and their implications on early Earth biogeochemistry. Overall, the combined results of various ancient seawater analogue experiments aimed at assessing microbial iron cycling pathways, coupled with the analysis of the BIF rock record, point towards a strong biotic influence during BIF genesis.

Fe- but not Mg-protophorphyrin IX binds to a transmembrane b-type cytochrome.

Transmembrane b-type cytochromes, which are crucially involved in electron transfer chains, bind one or more heme (Fe-protoporphyrin IX) molecules non-covalently. Similarly, chlorophylls are typically also non-covalently bound by several membrane integral polypeptides involved in photosynthesis. While both, chlorophyll and heme, are tetrapyrrole macrocycles, they have different substituents at the tetrapyrrole ring moiety. Furthermore, the central metal ion is Mg(2+) in chlorophyll and Fe(2+/3+) in heme. As heme and chlorophyll a have similar structures and might both be ligated by two histidine residues of a polypeptide chain, and as the local concentration of chlorophyll a might be up to 100-times higher than the concentration of heme, the question arises, as to how an organism ensures specific binding of heme, but not of chlorophyll, to transmembrane apo-cytochromes involved in photosynthetic electron transfer reactions. As shown here, Fe-protoporphyrin IX derivatives with modified substituents at the tetrapyrrole ring moiety still bind to an apo-cytochrome; however, association appears to be reduced. This indicates that hydrophobic and polar interactions of the ring substituents with the protein moiety stabilize the protein/heme-complex but are not essential per se. However, removal or replacement of the central Fe-ion completely abolishes formation of a holo-protein complex, and thus the central iron ion appears to determine heme binding to apo-cytochrome b6.

SDS-facilitated in vitro formation of a transmembrane B-type cytochrome is mediated by changes in local pH.

The folding and stabilization of α-helical transmembrane proteins are still not well understood. Following cofactor binding to a membrane protein provides a convenient method to monitor the formation of appropriate native structures. We have analyzed the assembly and stability of the transmembrane cytochrome b(559)', which can be efficiently assembled in vitro from a heme-binding PsbF homo-dimer by combining free heme with the apo-cytochrome b(559)'. Unfolding of the protein dissolved in the mild detergent dodecyl maltoside may be induced by addition of SDS, which at high concentrations leads to dimer dissociation. Surprisingly, absorption spectroscopy reveals that heme binding and cytochrome formation at pH 8.0 are optimal at intermediate SDS concentrations. Stopped-flow kinetics revealed that genuine conformational changes are involved in heme binding at these SDS concentrations. GPS (Global Protein folding State mapping) NMR measurements showed that optimal heme binding is intimately related to a change in the degree of histidine protonation. In the absence of SDS, the pH curve for heme binding is bell-shaped with an optimum at around pH 6-7. At alkaline pH values, the negative electrostatic potential of SDS lowers the local pH sufficiently to restore efficient heme binding, provided the amount of SDS needed for this does not denature the protein. Accordingly, the higher the pH value above 6-7, the more SDS is needed to improve heme binding, and this competes with the inherent tendency of SDS to dissociate cytochrome b(559)'. Our work highlights that, in addition to its denaturing properties, SDS can affect protein functions by lowering the local pH.

Characterization of two cytochrome b6 proteins from the cyanobacterium Gloeobacter violaceus PCC 7421.

In the genome of the untypical cyanobacterium Gloeobacter violaceus PCC 7421 two potential cytochrome b (6) proteins PetB1 and PetB2 are encoded. Such a situation has not been observed in cyanobacteria, algae and higher plants before, and both proteins are not characterized at all yet. Here, we show that both apo-proteins bind heme with high affinity and the spectroscopic characteristics of both holo-proteins are distinctive for cytochrome b (6) proteins. However, while in PetB2 one histidine residue, which corresponds to H100 and serves as an axial ligand for heme b (H) in PetB1, is mutated, both PetB proteins bind two heme molecules with different midpoint potentials. To recreate the canonical heme b (H) binding cavity in PetB2 we introduced a histidine residue at the position corresponding to H100 in PetB1 and subsequently characterized the generated protein variant. The presented data indicate that two bona fide cytochrome b (6) proteins are encoded in Gloeobacter violaceus. Furthermore, the two petB genes of Gloeobacter violaceus are each organized in an operon together with a petD gene. Potential causes and consequences of the petB and petD gene heterogeneity are discussed.

Multiple step assembly of the transmembrane cytochrome b6.

We have analyzed the role of individual heme-ligating histidine residues for assembly of holo-cytochrome b(6), and we show that the two hemes b(L) and b(H) bind in two subsequent steps to the apo-protein. Binding of the low-potential heme b(L) is a prerequisite for binding the high-potential heme b(H). After substitution of His86, which serves as an axial ligand for heme b(L), the apo-protein did not bind heme, while substitution of the heme b(L)-ligating residue His187 still allowed binding of both hemes. Similarly, after replacement of His202, one axial ligand to heme b(H), binding of only heme b(L) was observed, whereas replacement of His100, the other heme b(H) ligand, resulted in binding of both hemes. These data indicate sequential heme binding during formation of the holo-cytochrome, and the two histidine residues, which serve as axial ligands to the same heme molecule (heme b(L) or heme b(H)), have different importance during heme binding and cytochrome assembly. Furthermore, determination of the heme midpoint potentials of the various cytochrome b(6) variants indicates a cooperative adjustment of the heme midpoint potentials in cytochrome b(6).

Heterologous expression and in vitro assembly of the transmembrane cytochrome b6.

Folding and assembly studies with alpha-helical membrane proteins are often hampered by the absence of high-level expression systems as well as by missing suitable in vitro refolding procedures. Experimental constraints and requirements for heterologous expression and in vitro assembly of cytochrome b6 have been examined and conditions for in vitro reconstitutions of the protein have been optimized. Cytochrome b6 can serve as an excellent model system for in vitro studies on the dynamic interplay of an apo-protein and heme cofactors during assembly of a transmembrane b-type cytochrome. In vitro assembled cytochrome b6 binds two hemes with different midpoint potentials and both ferri as well as ferro heme bind to the apo-cytochrome. However, the ferro cytochrome appears to be less stable than the ferri form.

A mutational study of transmembrane helix-helix interactions.

Diverse methods have been developed and applied in the recent years to study interaction of transmembrane alpha-helices and often interaction of single transmembrane helices is followed on SDS-gels. Here we compare two measurements of the stability of a transmembrane helix-helix interaction, and the stability of the PsbF transmembrane helix dimer was determined in a biological membrane as well as in SDS. The observations described in this study demonstrate that the environment, in which a transmembrane helix interaction is studied, can be very critical and detergent properties can significantly influence transmembrane helix interactions, especially, when the transmembrane domain contains strongly polar residues.

Heme binding properties of heterologously expressed spinach cytochrome b(6): implications for transmembrane b-type cytochrome formation.

In vivo and in vitro requirements for the formation of cytochrome b(6) were examined to analyze the mechanisms of transmembrane b-type cytochrome formation. After heterologous expression of spinach cytochrome b(6), formation of the holo-cytochrome was observed within the E. coli inner membrane. The transmembrane orientation of cytochrome b(6) appeared not to be critical for heme binding and holo-cytochrome formation. Furthermore, in vitro reconstitution of cytochrome b(6) was possible under oxidizing as well as under reducing conditions. Taken together these observations strongly indicate that transmembrane b-type cytochromes can spontaneously assemble in vitro as well as in a membrane.