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Biomineralization of Fe sup(3+) to nanosized Gamma Fe sub(2)O sub(3) by Haloferax alexandrinus GUSF-1

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dc.contributor.author Naik-Samant, S.
dc.contributor.author Furtado, I.
dc.date.accessioned 2021-08-05T07:37:23Z
dc.date.available 2021-08-05T07:37:23Z
dc.date.issued 2021
dc.identifier.citation Geomicrobiology Journal. 38(9); 2021; 809-815. en_US
dc.identifier.uri https://doi.org/10.1080/01490451.2021.1954730
dc.identifier.uri http://irgu.unigoa.ac.in/drs/handle/unigoa/6524
dc.description.abstract Hypersaline environment is a habitat with extreme osmotic conditions along with low A sub(w,) serving as a home to extremely halophilic and halotolerant bacteria. The hypersaline environments, such as solar salterns located along the rivers, are exposed to fluxes of iron from iron ore transportation and other industrial wastes. The solar salterns often serve as a sink for metal intoxicants. Studies on archaea interaction with metal ions indicate the formation of minerals such as goethite, hematite, rhodochrosite, etc. However, studies exploring haloarchaeal candidates interacting with metals such as Fe sup(3+) in a hypersaline growth condition are scarce. This study unveils for the first time formation of Gamma Fe sub(2)O sub(3) from Fe sup(3+) by the haloarchaeon, Haloferax sp. GUSF-1 thus implying the significance of the culture synthesizing minerals in hypersaline sediments. Gamma Fe sub(2)O sub(3) is formed from Fe sup(3+) by the haloarchaeon Haloferax sp. GUSF-1 (GenBank accession no.GU-1KF796625), under microaerophilic growth on sodium acetate. A 50 mg L sup(-1) of Fe sup(2+) and 30.6?mg L sup(-1) of Fe sup(3+) was detected inside the cells. Simultaneously, a brown-colored crystalline material deposited in the culture broth through an iron reductase inhibited by Zn sup(2+) ions. The XRD of the deposit exhibited d values of 2.96, 2.514, 2.086, 1.6, and 1.45, while SEM-EDX displayed cubic and irregularly shaped minute particles with peaks for Fe at 0.6, 6.4, and 6.6 keV, respectively. TEM profiles revealed polycrystalline particles of 12-23 nm in size. Further, the SAED concentric pattern of light scattering with well-defined diffraction spots was consistent and matched with maghemite's crystal structure (Gamma Fe sub(2)O sub(3)). The FTIR spectrum revealed a peak at 1450 cm sup(-1) indicating iron oxyhydroxide formation as an intermediate having Gamma-FeOOH stretching bond vibrations. Conclusively, this study opens the possibility of the haloarchaea isolated from solar salterns for its exploitation in nanobiotechnology. en_US
dc.publisher Taylor and Francis en_US
dc.subject Microbiology en_US
dc.title Biomineralization of Fe sup(3+) to nanosized Gamma Fe sub(2)O sub(3) by Haloferax alexandrinus GUSF-1 en_US
dc.type Journal article en_US
dc.identifier.impf y


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