Spectroscopic studies on the interaction of phosphate with uteroferrin

The effect of phosphate on the binuclear iron center of pink (reduced) uteroferrin was examined by magnetic resonance and optical spectroscopy. The purple (oxidized) protein, which contains 1 mol of tightly bound phosphate per mol of enzyme at isolation, does not give rise to a 31P NMR signal. Phosphate binding to phosphate-stripped pink uteroferrin is indistinguishable from that in the native purple phosphoprotein. As measured by EPR and optical spectroscopy, the rate of reaction between phosphate and pink uteroferrin is pH-dependent, decreasing as the pH increases. Phosphate is capable of binding to the reduced protein between pH 3 and 7.8, resulting in formation of the purple uteroferrin-phosphate complex. Evans susceptibility measurements at pH 4.9 indicate that the EPR silent species with a maximum absorption at 535 nm, generated upon phosphate addition to pink uteroferrin, is diamagnetic. Moreover, phosphate causes disappearance of the hyperfine-shifted resonances in the 1H NMR spectra of the reduced protein. We therefore have not been able to identify the paramagnetic "purple reduced enzyme-phosphate complex" reported by Pyrz et al. (Pyrz, J. W., Sage, J. T., Debrunner, P. G., and Que, Jr., L. (1986) J. Biol Chem. 261, 11015-11020) using Mossbauer spectroscopy and dithionite-reduced 57Fe-reconstituted uteroferrin. Our present data with native unmodified enzyme are in accord with our earlier results (Antanaitis, B. C., and Aisen, P. (1985) J. Biol. Chem. 260, 751-756) and with the results of Burman et al. (Burman, S., Davis, J. C., Weber, M. J., and Averill, B. A. (1986) Biochem. Biophys. Res. Commun. 136, 490-497) on bovine spleen phosphatase, suggesting that phosphate binding to reduced protein rapidly induces oxidation of the binuclear iron center.     

Pathways in the binding and uptake of ferritin by hepatocytes

The binding and uptake of rat liver ferritin by primary cultures of rat liver hepatocytes was studied in order to assess the relative importance of saturable, high-affinity pathways and nonspecific processes in the incorporation of the protein by the cells. To minimize artifacts, ferritin not subjected to heat treatment and labeled in vivo with 59Fe was used. Binding to cell membranes was estimated from incubations performed at 4 degrees C. After 2 h, when a steady state in cell-associated ferritin had been achieved, approx. 4-10(4) binding sites per cell were observed, with an affinity constant for ferritin of 1 x 10(9) M-1. At 37 degrees C, the maximal uptake from these sites was 1.3 x 10(5) ferritin molecules/cell per h. For ferritin molecules bearing an average of 2400 iron atoms, this uptake amounts to 5 x 10(6) iron atoms/cell per min. Half-maximal uptake was achieved at a ferritin concentration, or KM1, of 3 x 10(-9) M. Although uptake rates at least a thousand times greater could be achieved by binding to the much larger number of low-affinity sites, the apparent KM2 for such 'nonspecific' uptake was 4 x 10(-7) M. At ferritin concentrations up to 2 nM, at least 90% of ferritin bound and taken up by hepatocytes involves saturable, high-affinity sites, presumably true ferritin receptors.     

The binding of molybdate to uteroferrin. Hyperfine interactions of the binuclear center with 95Mo, 1H, and 2H

Uteroferrin, an acid phosphatase with a spin-coupled and redox-active binuclear iron center, is paramagnetic in its pink, enzymatically active, mixed-valence (S = 1/2) state. Phosphate, a product and inhibitor of the enzymatic activity of uteroferrin, converts the pink, EPR-active form of the protein to a purple, EPR-silent species. In contrast, molybdate, a tetrahedral oxyanion analog of phosphate, transforms the EPR spectrum of uteroferrin from a rhombic to an axial form. With both electron spin echo envelope modulation (ESEEM) and electron nuclear double resonance (ENDOR) spectroscopies, we observe a hyperfine interaction of [95Mo]molybdate with the S = 1/2, Fe(II)-Fe(III) center of the protein. A pair of 95Mo resonances centered at the 95Mo Larmor frequency at the applied magnetic field and separated by a hyperfine coupling constant of 1.2 MHz is evident. Therefore, a single monomeric species of molybdate is close to, and likely a ligand of, the binuclear cluster. 1H ENDOR studies on uteroferrin reveal at least six sets of lines mirrored about the 1H Larmor frequency. Two pairs of these lines become reduced in intensity when the protein is exchanged against D2O. Moreover, ESEEM and 2H ENDOR spectra display resonances at the 2H Larmor frequency. Therefore, the metal-binding region of the protein is accessible to solvent. Additional deuterium lines observable by ESEEM spectroscopy provide evidence for a population of strongly coupled, readily exchangeable protons associated with the binuclear center. The measured hyperfine coupling constants for these deuterons are orientation-dependent with splittings of nearly 4 MHz at g3 = 1.59 and less than 1 MHz at g1 = 1.94. In the presence of molybdate, ESEEM spectra of D2O-exchanged samples reveal a resonance at the 2H Larmor frequency, with no evidence of spectral components due to strongly coupled deuterons. 1H ENDOR studies of the uteroferrin-molybdate complex show at least seven pairs of lines, mirrored about the 1H Larmor frequency, of which one pair becomes attenuated in amplitude upon deuteration. The active site thus remains accessible to solvent in the presence of molybdate.     

A new role for the transferrin receptor in the release of iron from transferrin

Iron removal by pyrophosphate from human serum diferric transferrin and the complex of transferrin with its receptor was studied in 0.05 M HEPES or MES buffers containing 0.1 M NaCl and 0.01 M CHAPS at 25 degrees C at pH 7.4, 6.4, and 5.6. At each pH, the concentration of pyrophosphate was adjusted to achieve rates of release amenable to study over a reasonable time course. Released iron was separated from protein-bound iron by poly(ethylene glycol) precipitation of aliquots drawn from the reaction mixture at various times during the course of a kinetic run. The amount of 59Fe label associated with the protein and pyrophosphate was determined from the radioactivity of precipitate and supernatant, respectively, in each aliquot. Iron removal of 0.05 M pyrophosphate at pH 7.4 from diferric transferrin bound to the receptor is considerably slower than that from free diferric transferrin, with observed pseudo-first-order rate constants of 0.020 and 0.191 min-1, respectively. For iron removal by 0.01 M pyrophosphate at pH 6.4, corresponding rate constants are 0.031 and 0.644 min-1. However, at pH 5.6, iron removal by 0.001 M pyrophosphate is faster from diferric transferrin bound to its receptor than from free transferrin (observed rate constants of 0.819 and 0.160 min-1, respectively). Thus, the transferrin receptor not only facilitates the removal of iron from diferric transferrin at the low pH that prevails in endocytic vesicles but may also reduce its accessibility to iron acceptors at extracellular pH, thereby minimizing the likelihood of nonspecific release of iron from transferrin at the cell surface.     

Receptor-modulated iron release from transferrin: differential effects on N- and C-terminal sites

Iron release to PPi from N- and C-terminal monoferric transferrins and their complexes with transferrin receptor has been studied at pH 7.4 and 5.6 in 0.05 M HEPES or MES/0.1 M NaCl/0.01 M CHAPS at 25 degrees C. The two sites exhibit kinetic heterogeneity in releasing iron. The N-terminal form is slightly less labile than its C-terminal counterpart at pH 7.4, but much more facile in releasing iron at pH 5.6. At pH 7.4, iron removal by 0.05 M pyrophosphate from each form of monoferric transferrin complexed to the receptor is considerably slower than from the corresponding free monoferric transferrin. However, at pH 5.6, complexation of transferrin to its receptor affects the two forms differently. The rate of iron release to 0.005 M pyrophosphate by the N-terminal species is substantially the same whether transferrin is free or bound to the receptor. In contrast, the C-terminal form releases iron much faster when complexed to the receptor than when free. Urea/PAGE analysis of iron removal from free and receptor-complexed diferric transferrin at pH 5.6 reveals that its C-terminal site is also more labile in the complex, but its N-terminal site is more labile in free diferric transferrin. Thus, the newly discovered role of transferrin receptor in modulating iron release from transferrin predominantly involves the C-terminal site. This observation helps explain the prevalence of circulating N-terminal monoferric transferrin in the human circulation.     

Sensitive fluorescence in situ hybridization signal detection in maize using directly labeled probes produced by high concentration DNA polymerase nick translation

The signal produced by fluorescence in situ hybridization (FISH) often is inconsistent among cells and sensitivity is low. Small DNA targets on the chromatin are difficult to detect. We report here an improved nick translation procedure for Texas red and Alexa Fluor 488 direct labeling of FISH probes. Brighter probes can be obtained by adding excess DNA polymerase I. Using such probes, a 30?kb yeast transgene, and the rp1, rp3 and zein multigene clusters were clearly detected.     

Biodeterioration of Mayan buildings at uxmal and tulum,Mexico

Uxmal and Tulum are two important Mayan sites in the Yucatan peninsula. The buildings are mainly composed of limestone and grey/black discoloration is seen on exposed walls and copious greenish biofilms on inner walls. The principal microorganisms detected on interior walls at both Uxmal and Tulum were cyanobacteria; heterotrophic bacteria and filamentous fungi were also present. A dark‐pigmented mitosporic fungus and Bacillus cereus, both isolated from Uxmal, were shown to be acidogenic in laboratory cultures. Cyanobacteria belonging to rock‐degrading genera Synechocystis and Gloeocapsa were identified at both sites. Surface analysis previously showed that calcium ions were present in the biofilms on buildings at Uxmal and Tulum, suggesting the deposition of biosolubilized stone. Apart from their potential to degrade the substrate, the coccoid cyanobacteria supply organic nutrients for bacteria and fungi, which can produce organic acids, further increasing stone degradation.