Camel myoglobin

1. Crystalline myoglobin was prepared from camel heart muscle. 2. A method was developed for the isolation of myoglobin that employs molecular-sieve chromatography. 3. Analytical chromatography of the camel myoglobin on a molecular-sieve column and on two types of ion-exchange columns gave in each case a single elution band, which accounted for better than 98% recovery and showed that the product was free from haemoglobin. 4. The iron content on a dry weight basis was 0.308%. This value corresponds to a molecular weight of 18100. 5. The spectra of acidic ferrimyoglobin, basic ferrimyoglobin and ferrimyoglobin cyanide were measured. 6. The pK(a) of the dissociation of the haem-bound water molecule in acidic ferrimyoglobin was 8.53 at 25 degrees . 7. Conclusions are drawn about the charge on the surface of the camel ferrimyoglobin molecule as compared with horse and sperm-whale ferrimyoglobins.     

Determination of the zero-field splitting of Fe in heme proteins from the temperature dependence of the spin-lattice relaxation rate

A sensitive method for obtaining the zero-field crystalline field splitting is described and applied to ferrimyoglobin (H₂O) and ferrimyoglobin (F⁻). The high accuracy (1–2%) with which the splitting can be determined should make it possible to explore the environmental (conformatinal) changes at the Fe³⁺ site.     

Formation of a steady state in the radiolysis of ferrimyoglobin in aqueous solution

The interaction of radiation-generated · OH radicals with ferrimyoglobin in deaerated aqueous solution at neutral pH has been quantitatively studied. Changes in the visible absorption spectrum have been analyzed on the basis of composition changes of the ferri, deoxy, and ferriperoxide forms of the metalloprotein. A postirradiation thermal process must be considered in order to evaluate the radical-induced composition changes. Initially, ·OH induces reduction of ferrimyoglobin to the deoxy form with a G value (molecular yield/100 eV of absorbed energy) in the zero-dose limit of 1.4 (±0.2). Radiation-generated H₂O₂ reacts with the ferrimyoglobin substrate to produce ferrimyoglobin peroxide with a G value of 0.7 (±0.1) in the zero-dose limit. At doses of >1 krad μm^?1 of myoglobin present, the composition of the three myoglobin derivatives reaches a radiolysis steady state. In this moderate-dose plateau region, this composition is 44% ferri, 18% deoxy, and 38% ferri peroxide. The · OH-induced hemoprotein radicals that do not initiate 1-eq redox conversions undergo reactions that generate dimer and other globin-modified material.     

Analysis of the principal g-tensors in single crystals of ferrimyoglobin complexes

This paper describes a method of determining the directions of the principal axes of the g-tensors in single crystals from measurements of the g-value variation in three crystalline planes (ab, bc*, ac) and of the principal values of g-tensors. Measurements of paramagnetic resonance spectra of ferrimyoglobin (Mb(Fe3+)) complexes (Mb(Fe3+).CN-, .N3-, .imidazole(Im.) and .OCN-) in single crystals provided detailed information on the electronic state of the Fe3+. The direction of the z axis in Mb(Fe3+).CN-, .N3- and .Im. is not parallel to that in Mb(Fe3+).H2O, which has been used as the haem normal, where the z axis is one of the principal axes of the g-tensors corresponding to the maximal (in low-spin state of Fe3+ in haem) or minimal (in high-spin state of Fe3+ in haem) g-value. In Mb(Fe3+).OCN-, however, which is in thermal equilibrium between high-spin and low-spin states, the directions of the z axis in both states seem to be perpendicular to the haem plane. The direction of the x axis is not parallel to the plane of the linked histidine ring.     

Spin-state equilibria and axial ligand bonding in FixL hydroxide: a resonance raman study

 Vibrational assignments for the Fe-OH unit of ferric alkaline forms of two deletion derivatives of Rhizobium meliloti FixL, FixL*, a functional O₂-sensing heme kinase, and FixLN, which contains only the heme domain, are made. Appearance of ²H- and ¹⁸O-sensitive Raman bands indicates that the heme group of FixL binds hydroxide as a distal ligand to form a six-coordinate complex. The alkaline FixLs are distributed between high- and low-spin states. The high- and low-spin bands corresponding to the ν (Fe-OH) modes occur at 479 and 539 cm^–1, respectively. Low temperature favors formation of the low-spin complex, indicative of a thermal spin-state equilibrium. The ν (Fe-OH) frequencies of FixLN and FixL* are 11 to 18 cm^–1 lower than those observed for the respective vibrations in alkaline myoglobin and hemoglobin. The weaker Fe-OH bond in the FixLs is attributed to a lack of hydrogen bonding on the distal side of the heme pocket. Received: 20 November 1997 / Accepted: 2 March 1998     

Structure of Acinetobacter strain ADP1 protocatechuate 3, 4-dioxygenase at 2.2 A resolution: implications for the mechanism of an intradiol dioxygenase

The crystal structures of protocatechuate 3,4-dioxygenase from the soil bacteria Acinetobacterstrain ADP1 (Ac 3,4-PCD) have been determined in space group I23 at pH 8.5 and 5.75. In addition, the structures of Ac 3,4-PCD complexed with its substrate 3, 4-dihydroxybenzoic acid (PCA), the inhibitor 4-nitrocatechol (4-NC), or cyanide (CN(-)) have been solved using native phases. The overall tertiary and quaternary structures of Ac 3,4-PCD are similar to those of the same enzyme from Pseudomonas putida[Ohlendorf et al. (1994) J. Mol. Biol. 244, 586-608]. At pH 8.5, the catalytic non-heme Fe(3+) is coordinated by two axial ligands, Tyr447(OH) (147beta) and His460(N)(epsilon)(2) (160beta), and three equatorial ligands, Tyr408(OH) (108beta), His462(N)(epsilon)(2) (162beta), and a hydroxide ion (d(Fe-OH) = 1.91 A) in a distorted bipyramidal geometry. At pH 5.75, difference maps suggest a sulfate binds to the Fe(3+) in an equatorial position and the hydroxide is shifted [d(Fe-OH) = 2.3 A] yielding octahedral geometry for the active site Fe(3+). This change in ligation geometry is concomitant with a shift in the optical absorbance spectrum of the enzyme from lambda(max) = 450 nm to lambda(max) = 520 nm. Binding of substrate or 4-NC to the Fe(3+) is bidentate with the axial ligand Tyr447(OH) (147beta) dissociating. The structure of the 4-NC complex supports the view that resonance delocalization of the positive character of the nitrogen prevents substrate activation. The cyanide complex confirms previous work that protocatechuate 3,4-dioxygenases have three coordination sites available for binding by exogenous substrates. A significant conformational change extending away from the active site is seen in all structures when compared to the native enzyme at pH 8.5. This conformational change is discussed in its relevance to enhancing catalysis in protocatechuate 3,4-dioxygenases.     

Interaction of radiation-generated radicals with myoglobin in aqueous solution. III. Effects of oxygen and catalase on the product distribution in solutions of ferrimyoglobin containing N2O

The gamma-radiolysis of aqueous solutions of ferrimyoglobin in the presence of N2O at pH 7.3 has been examined as a function of added catalase and oxygen. Changes in the nature of the heme group have been monitored by visible absorption spectrophotometry and analysed quantitatively by a multiple wavelength method based on Beer's Law. Simple chemical analyses have been used to confirm qualitative identification of the product derivatives. As observed previously, the ferriheme is reduced by indirect globin-mediated action initiated by OH/H. The yield of reduced product decreases as [O2] increases. Conversion to ferrimyoglobin through the participation of H2O2 derived from irradiated water and from protein-mediated processes in oxygenated solution, is eliminated by the presence of catalase. Formation of a hemichrome form of ferrimyoglobin is apparent at higher doses in the presence of O2. These results demonstrate that oxygen plays an important role in controlling the nature and extent of redox that manifests ultimately on the heme group of ferrimyoglobin as a result of the initial interaction of OH/H.     

Iron toxicity and other chemical soil constraints to rice in highland swamps of Burundi

Iron toxicity is suspected to be a major nutritional disorder in rice cropping systems established on flooded organic soils that contain reductible iron. A pot trial was carried out to assess Fe toxicity to rice in flooded Burundi highland swamp soils with a wide range of organic carbon contents. Soil and leaf analyses were performed and total grain weight was determined. Clear Fe toxicity was diagnosed, based on leaf Fe content at panicle differentiation. Leaf Fe contents higher than 250 g g^–1 dry matter induced lower Mg (and probably Mn) uptake, and a 50% total grain weight reduction. These features were associated with exchangeable Fe equivalent fractions higher than 86%. Besides, several non-Fe toxic soils exhibited an Mg-Mn imbalance.     

The heme environment of recombinant human indoleamine 2,3-dioxygenase. Structural properties and substrate-ligand interactions

Indoleamine 2,3-dioxygenase is a heme enzyme that catalyzes the oxidative degradation of L-Trp and other indoleamines. We have used resonance Raman spectroscopy to characterize the heme environment of purified recombinant human indoleamine 2,3-dioxygenase (hIDO). In the absence of L-Trp, the spectrum of the Fe(3+) form displayed six-coordinate, mixed high and low spin character. Addition of L-Trp triggered a transition to predominantly low spin with two Fe-OH(-) stretching modes identified at 546 and 496 cm(-1), suggesting H-bonding between the NH group of the pyrrole ring of L-Trp and heme-bound OH(-). The distal pocket of Fe(3+) hIDO was explored further by an exogenous heme ligand, CN(-); again, binding of L-Trp introduced strong H-bonding and/or steric interactions to the heme-bound CN(-). On the other hand, the spectrum of Fe(2+) hIDO revealed a five-coordinate and high spin heme with or without L-Trp bound. The proximal Fe-His stretching mode, identified at 236 cm(-1), did not shift upon L-Trp addition, indicating that the proximal Fe-His bond strength is not affected by binding of the substrate. The high Fe-His stretching frequency suggests that Fe(2+) hIDO has a strong "peroxidase-like" Fe-His bond. Using CO as a structural probe for the distal environment of Fe(2+) hIDO revealed that binding of L-Trp in the distal pocket converted IDO to a peroxidase-like enzyme. Binding of L-Trp also caused conformational changes to the heme vinyl groups, which were independent of changes of the spin and coordination state of the heme iron. Together these data indicate that the strong proximal Fe-His bond and the strong H-bonding and/or steric interactions between l-Trp and dioxygen in the distal pocket are likely crucial for the enzymatic activity of hIDO.     

Evidence for microbial Fe(III) reduction in anoxic, mining-impacted lake sediments (Lake Coeur d'Alene, Idaho)

Mining-impacted sediments of Lake Coeur d'Alene, Idaho, contain more than 10% metals on a dry weight basis, approximately 80% of which is iron. Since iron (hydr)oxides adsorb toxic, ore-associated elements, such as arsenic, iron (hydr)oxide reduction may in part control the mobility and bioavailability of these elements. Geochemical and microbiological data were collected to examine the ecological role of dissimilatory Fe(III)-reducing bacteria in this habitat. The concentration of mild-acid-extractable Fe(II) increased with sediment depth up to 50 g kg(-1), suggesting that iron reduction has occurred recently. The maximum concentrations of dissolved Fe(II) in interstitial water (41 mg liter(-1)) occurred 10 to 15 cm beneath the sediment-water interface, suggesting that sulfidogenesis may not be the predominant terminal electron-accepting process in this environment and that dissolved Fe(II) arises from biological reductive dissolution of iron (hydr)oxides. The concentration of sedimentary magnetite (Fe(3)O(4)), a common product of bacterial Fe(III) hydroxide reduction, was as much as 15.5 g kg(-1). Most-probable-number enrichment cultures revealed that the mean density of Fe(III)-reducing bacteria was 8.3 x 10(5) cells g (dry weight) of sediment(-1). Two new strains of dissimilatory Fe(III)-reducing bacteria were isolated from surface sediments. Collectively, the results of this study support the hypothesis that dissimilatory reduction of iron has been and continues to be an important biogeochemical process in the environment examined.     

Resonance Raman spectroscopy of ribonucleotide reductase. Evidence for a deprotonated tyrosyl radical and photochemistry of the binuclear iron center

Native ribonucleotide reductase from Escherichia coli exhibits a resonance-enhanced Raman mode at 1498 cm-1 that is characteristic of a tyrosyl radical. The Raman frequency as well as the absorption maximum at 410 nm identifies the radical as being in a deprotonated state. The B2 subunit of ribonucleotide reductase shows an additional resonance Raman mode at 493 cm-1 that has been assigned to the symmetric stretch of an Fe-O-Fe moiety. When samples of active B2 or metB2 are exposed to a tightly focused laser beam at 406.7 nm, there is a loss of intensity at 493 cm-1 and the appearance of a new peak at 595 cm-1. Although the 595-cm-1 feature was previously assigned to an Fe-OH vibration on the basis of its 23-cm-1 shift to lower energy in H2(18)O and the apparent dependence of its intensity on pH [Sj?berg, B. M., Loehr, T. M., & Sanders-Loehr, J. (1987) Biochemistry 26, 4242], the present studies indicate that the intensity of this mode is dependent primarily on input laser power. The peak at 595 cm-1 is more plausibly assigned to a new vs(Fe-O-Fe) mode in view of its lack of the deuterium isotope dependence expected for an Fe-OH mode and its resonant scattering cross section which is comparable to that of the 493-cm-1 mode. This new species has a calculated Fe-O-Fe angle of approximately 113 degrees compared to approximately 138 degrees calculated for the Fe-O-Fe unit in unmodified protein B2. One possible explanation for the photoinduced vibrational mode is that a bridging solvent molecule has been inserted in place of a bridging carboxylate.     

A proton magnetic relaxation study of ferrimyoglobin in aqueous ionic solutions

Proton magnetic longitudinal T₁ relaxation times have been measured for acid (horse) ferrimyoglobin solutions [0.1 M NaCl and KH₂PO₄, 2 M NaCl and 1 M MgCl₂] from 5°C to 35°C in dependence on myoglobin concentration up to 6 mM. The enhancement of the relaxation rate due to the paramagnetic haem iron. which is observed in this temperature range is compared with analogous data for the ferrihaemoglobin solution. The conclusion is that the protons exchanging from the haem pocket with bulk solvent are not those from the water molecule at the sixth ligand site of haem iron. The exchanging protons are more than 4 Å away from the haem iron being closer to it in ferrimyoglobin than in ferrihaemogiobin. This distance becomes larger in solutions with higher salt concentration, the largest difference between 0.1 M NaCl and 1 M MgCl₂ being over one Angstrom unit. This indicates a conformational change of the haem pocket, possibly its tightening.     

Localization of cytochromes in the outer membrane of Desulfovibrio vulgaris (Hildenborough) and their role in anaerobic biocorrosion

A protocol was developed whereby the outer and cytoplasmic membranes of the sulfate-reducing bacterium Desulfovibrio vulgaris (Hildenborough) were isolated and partially characterized. The isolated outer membrane fractions from cultures grown under high (100 ppm) and low (5 ppm) Fe2+ conditions were compared by SDS-PAGE electrophoresis, and showed that several protein bands were derepressed under the low iron conditions, most notably at 50 kDa, and 77.5 kDa. Outer membrane isolated from low iron cultured cells was found to contain two proteins, 77.5 kDa and 62.5 kDa in size, that reacted with a heme-specific stain and were referred to as high molecular weight cytochromes. Studies conducted on the low iron isolated outer membrane by a phosphate/mild steel hydrogen evolution system showed that addition of the membrane fraction caused an immediate acceleration in H2 production. A new model for the anaerobic biocorrosion of mild steel is proposed.     

Structures of reaction intermediates of bovine cytochrome c oxidase probed by time-resolved vibrational spectroscopy

Structures of reaction intermediates of bovine cytochrome c oxidase (CcO) in the reactions of its fully reduced form with O2 and fully oxidized form with H2O2 were investigated with time-resolved resonance Raman (RR) and infrared spectroscopy. Six oxygen-associated RR bands were observed for the reaction of CcO with O2. The isotope shifts for an asymmetrically labeled dioxygen, (16)O(18)O, has established that the primary intermediate of cytochrome a3 is an end-on type dioxygen adduct and the subsequent intermediate (P) is an oxoiron species with Fe=O stretch (nu(Fe=O)) at 804/764 cm(-1) for (16)O2/(18)O2 derivatives, although it had been long postulated to be a peroxy species. The P intermediate is converted to the F intermediate with nu(Fe=O) at 785/751 cm(-1) and then to a ferric hydroxy species with nu(Fe-OH) at 450/425 cm(-1) (443/417 cm(-1) in D2O). The rate of reaction from P to F intermediates is significantly slower in D2O than in H2O. The reaction of oxidized CcO with H2O2 yields the same oxygen isotope-sensitive bands as those of P and F, indicating the identity of intermediates. Time-resolved infrared spectroscopy revealed that deprotonation of carboxylic acid side chain takes place upon deligation of a ligand from heme a3. UV RR spectrum gave a prominent band due to cis C=C stretch of phospholipids tightly bound to purified CcO.     

Lipids of Thermoplasma acidophilum

Cells of Thermoplasma acidophilum contain about 3% total lipid on a dry weight basis. Total lipid was found to contain 17.5% neutral lipid, 25.1% glycolipid, and 56.6% phospholipid by chromatography on silicic acid. The lipids contain almost no fatty acid ester groups but appear to have long-chain alkyl groups in ether linkages to glycerol. The phospholipid fraction includes a major component which represents about 80% of the lipid phosphorus and 46% of the total lipids. We believe this component to be a long-chain isopranol glycerol diether analogue of glycerolphosphoryl monoglycosyl diglyceride. The glycolipids appear to contain isopranol diether analogues. Several components of the complex, neutral lipid fraction have been identified as hydrocarbons, vitamin K(2)-7, and isopranol glycerol diether analogues. Sterols are present in the neutral lipids but do not appear to be synthesized by the organism.     

OmcB,a c-type polyheme cytochrome,involved in Fe(III) reduction in Geobacter sulfurreducens

Microorganisms in the family Geobacteraceae are the predominant Fe(III)-reducing microorganisms in a variety of subsurface environments in which Fe(III) reduction is an important process, but little is known about the mechanisms for electron transport to Fe(III) in these organisms. The Geobacter sulfurreducens genome was found to contain a 10-kb chromosomal duplication consisting of two tandem three-gene clusters. The last genes of the two clusters, designated omcB and omcC, encode putative outer membrane polyheme c-type cytochromes which are 79% identical. The role of the omcB and omcC genes in Fe(III) reduction in G. sulfurreducens was investigated. OmcB and OmcC were both expressed during growth with acetate as the electron donor and either fumarate or Fe(III) as the electron acceptor. OmcB was ca. twofold more abundant under both conditions. Disrupting omcB or omcC by gene replacement had no impact on growth with fumarate. However, the OmcB-deficient mutant was greatly impaired in its ability to reduce Fe(III) both in cell suspensions and under growth conditions. In contrast, the ability of the OmcC-deficient mutant to reduce Fe(III) was similar to that of the wild type. When omcB was reintroduced into the OmcB-deficient mutant, the capacity for Fe(III) reduction was restored in proportion to the level of OmcB production. These results indicate that OmcB, but not OmcC, has a major role in electron transport to Fe(III) and suggest that electron transport to the outer membrane is an important feature in Fe(III) reduction in this organism.     

Iron stress genes in marine Synechococcus and the development of a flow cytometric iron stress assay

Marine Synechococcus are frequently found in environments where iron (Fe) is a limiting nutrient. To understand their capacity to respond to Fe stress, we screened picoplankton genomes and the Global Ocean Survey metagenome for known Fe stress genes. Many open ocean strains of Synechococcus lack most known genes for Fe stress, while coastal and upwelling strains contain many, suggesting that maintaining multiple Fe limitation compensation strategies is not a selective advantage in the open ocean. All genomes contained iron deficiency-induced protein A (IdiA) and its complementary Fe³⁺ transport proteins. The ubiquity of IdiA was exploited to develop an in situ Fe stress bioassay based on immunolabelling and flow cytometry. As a test of field applicability, we used the assay on natural Synechococcus populations from one station in the Costa Rica Upwelling Dome where total Fe ranged from <0.08 to 0.14 nM in the upper water column. The bioassay found Fe stress in 5–54% of the population. Based on our findings, we believe that when reactive strains are present this assay can reveal environmental and clade-specific differences in the response of Synechococcus to Fe stress.     

Chemical and physical differentiation of superoxide dismutases in anaerobes.

Superoxide dismutase activity in crude or partially purified cell extracts from several species and strains of obligate anaerobe Bacteroides was inhibited instantaneously by NaN3 and was inactivated rapidly upon incubation with H2O2. The extent of NaN3 inhibition varied from 41 to 93%, and the half-life of the enzymatic activity in 5 mM H2O2 ranged from 1.2 to 6.1 min, depending upon the organism tests. When grown in a defined medium containing 59Fe, Bacteroides fragilis (VPI 2393) incorporated radiolabel into a 40,000-molecular-weight NaN3- and H2O2-sensitive superoxide dismutase but did not incorporate 54Mn into that protein under similar growth conditions. The anaerobe Actinomyces naeslundii (VPI 9985) incorporated 54Mn but not 59Fe into a NaN3-insensitive and H2O2-resistant superoxide dismutase. The apparent molecular weight of the superoxide dismutase from this and several other Actinomyces spp. was estimated to be 110,000 to 140,000. Comparison of these data with studies of homogeneous metallosuperoxide dismutases suggests that the Bacteroides spp. studied contain a ferrisuperoxide dismutase, whereas Actinomyces spp. contain a managanisuperoxide dismutase.     

The bacteriocidal effects of transition metal complexes containing the NO+ group on the food-spoilage bacterium Clostridium sporogenes

The chemical and molecular mechanism of toxicity of nitrite towards food-spoilage bacteria such as Clostridium botulinum or Clostridium sporogenes is not well understood. In order to discover the active species and explore its chemistry, a number of compounds related to nitrite were synthesized. Their bacteriocidal effects on C. sporogenes were investigated in Oxoid nutrient broth No. 2 growth medium at pH 7.0. Inhibition of cell growth, expressed as the concentration which causes 50% cell inhibition, was observed with nitrite at 10 mM, whereas [Fe4S3(NO)7]-(the anion of Roussin's black salt) and (Fe2(SCH2CH2OH)2(NO)4] (a water-soluble Roussin's red salt ester) were found to be effective at 0.001 mM and 0.005 mM, respectively, confirming previous reports that iron-sulphur-nitrosyl complexes are much more toxic to these organisms than nitrite itself. The nitroprusside anion, [Fe(CN)5NO]2- was found to be toxic at 0.030 mM and the corresponding chromium species, [Cr(CN)5NO]3-, at 0.1 mM. Therefore, on the basis of the number of NO groups present, the nitrosylcyano complexes are comparable in activity with the iron-sulphur-nitrosyl compounds. These results show that neither iron nor sulphur are essential for the bacteriostatic effect of the Roussin's type compounds. The property that all these compounds have in common is that they contain NO+. It is proposed that this is the active species responsible for the preservative effect of nitrite, and that a relationship may exist between the N-O stretching frequency, a measure of the NO+ character, and the toxicity of these NO(+)-containing complexes.     

USE OF THE DCB TECHNIQUE FOR EXTRACTION OF HYDROUS IRON OXIDES FROM ROOTS OF WETLAND PLANTS

Replicate samples of Phragmites communis roots coated with hydrous iron oxide were analyzed for internal and external Fe using the dithionite-citrate-bicarbonate technique (hot DCB), a modified DCB technique (cold DCB), Ethylenediamine tetraacetic acid (EDTA), Diethylenetriamine pentaacetic acid (DTPA), and a total Fe analysis. EDTA and DTPA were found to be inefficient in extracting FeOOH while both DCB techniques were efficient. Concentrations of Fe extracted (8.93% and 9.37% by weight) and percent of total Fe extracted (98.3% and 98.6%) by the hot and cold DCB techniques (respectively) were not significantly different. Results of the total Fe analysis (8.58% Fe by weight) were the same as extracted Fe and total Fe determined by the DCB techniques. This may reflect the large external Fe : internal Fe ratio of the sample roots. Despite equivalent results, the cold DCB technique is preferred over the hot DCB technique due to a reduced likelihood of structural damage to roots.