Resistance and bioaccumulation of Cd2+, Cu2+, Co2+ and Mn2+ by thermophilic bacteria, Geobacillus thermantarcticus and Anoxybacillus amylolyticus

In this study, bioaccumulation and heavy metal resistance of Cd²⁺, Cu²⁺, Co²⁺ and Mn²⁺ ions by thermophilic Geobacillus thermantarcticus and Anoxybacillus amylolyticus was investigated. The bacteria, in an order with respect to metal resistance from the most resistant to the most sensitive, was found to be Mn²⁺ > Co²⁺ > Cu²⁺ > Cd²⁺ for both G. thermantarcticus and A. amylolyticus. It was determined that the highest metal bioaccumulation was performed by A. amylolyticus in Mn²⁺ (28,566 μg/g dry weight), and the lowest metal bioaccumulation was performed by A. amylolyticus in Co²⁺ (327.3 μg/g dry weight). The highest Cd²⁺ capacities of dried cell membrane was found to be 36.07 and 39.55 mg/g membrane for G. thermantarticus and A. amylolyticus, respectively, and the highest Cd²⁺ capacities of wet cell membrane was found to be 14.36 and 12.39 mg/g membrane for G. thermantarcticus and A. amylolyticus, respectively.     

Iron-depleted reaction centers from Rhodopseudomonas sphaeroides R-26.1: characterization and reconstitution with Fe2+, Mn2+, Co2+, Ni2+, Cu2+, and Zn2+

Reaction centers (RCs) from the photosynthetic bacterium Rhodopseudomonas sphaeroides R-26.1 were depleted of Fe by a simple procedure involving reversible dissociation of the H subunit. The resulting intact Fe-depleted RCs contained 0.1-0.2 Fe per RC as determined from atomic absorption and electron paramagnetic resonance (EPR) spectroscopy. Fe-depleted RCs that have no metal ion occupying the Fe site differed from native RCs in the following respects: (1) the rate of electron transfer from QA- to QB exhibited nonexponential kinetics with the majority of RCs having a rate constant slower by only a factor of approximately 2, (2) the efficiency of light-induced charge separation (DQA----D+QA-) produced by a saturating flash decreased to 63%, and (3) QA appeared readily reducible to QA2-. Various divalent metal ions were subsequently incorporated into the Fe site. The electron transfer characteristics of Fe-depleted RCs reconstituted with Fe2+, Mn2+, Co2+, Ni2+, Cu2+, and Zn2+ were essentially the same as those of native RCs. These results demonstrate that neither Fe2+ nor any divalent metal ion is required for rapid electron transfer from QA- to QB. However, the presence of a metal ion in the Fe site is necessary to establish the characteristic, native, electron-transfer properties of QA. The lack of a dominant role of Fe2+ or other divalent metals in the observed rate of electron transfer from QA- to QB suggests that a rate-limiting step (for example, a protonation event or a light-induced structural change) precedes electron transfer.     

Mn2+, Co2+, Cu2+ and Zn2+ complexes with two macrocyclic ligands bearing L-lactate-like functions: potentiometric studies and evaluation of superoxide-scavenging properties of the Mn2+ complex

Some aerobic organisms devoid of SOD use Mn2+ chelates to scavenge the O2- radical. Since the Mn2+-bis(lactato)diaquo complex is known as having a high SOD-like activity, we prepared manganese(II) complexes with triazamacrocyclic ligands bearing L-lactate-like functions in order to obtain model compounds able to disproportionate the superoxide radical. Thus, two macrocyclic ligands, N,N',N"-tris[2(S)-hydroxybutyric acid]-1,4,7-triazacyclononane, L1, and N,N',N"-tris[2(S)-hydroxybutyric acid]-1,5,9-triazacyclododecane, L2, were prepared and their capacity to retain the Mn2+ ion in aqueous solution was determined from potentiometric experiments. The chelating properties in aqueous solution of each ligand towards Co2+, Cu2+ and Zn2+ ions were also determined. L1 forms complexes with Mn2+, Co2+, Cu2+ and Zn2+ ions with stability constants of 8.33(5), 15.78(5), 17.65(3) and 14.32(1), respectively. L2 forms complexes with Cu2+ and Zn2+ ions with stability constants of 10.67(1) and 6.98(3), respectively. But the constants related to the Mn2+ and Co2+ complexes were too low to be determined by the method used. The stability constants values calculated for L2 complexes are significantly lower than those for the corresponding complexes of L1. Additional spectroscopic measurements were carried out on the Mn2+-L1 system. The electronic spectrum of this system showed a pH-dependence that may be consistent with the formation of hydroxo-species as the ESR spectra recorded at 120 K did not show oxidation of the Mn2+ ion in the pH range studied. The superoxide-scavenging activity of the manganese(II)-L1 complex was investigated using the cytochrome c assay. The Mn2+-L1 system showed an IC50 value of 1.7 microM which indicates that it appears as a potent SOD mimic.