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Isabel Moura

Researcher at Universidade Nova de Lisboa

Publications -  421
Citations -  14404

Isabel Moura is an academic researcher from Universidade Nova de Lisboa. The author has contributed to research in topics: Desulfovibrio gigas & Rubredoxin. The author has an hindex of 61, co-authored 420 publications receiving 13481 citations. Previous affiliations of Isabel Moura include University of Vigo & University of New Mexico.

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Structural stability of adenylate kinase from the sulfate-reducing bacteria Desulfovibrio gigas

TL;DR: The spectral parameters as monitored by ellipticity changes in the CD spectra of the enzyme as well as the decrease in tryptophan intensity emission upon heating were seen to be good complements to the highly sensitive but integral DSC-method.
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The small iron-sulfur protein from the ORP operon binds a [2Fe-2S] cluster.

TL;DR: The data suggests that Dde_3197 can harbor one or two [2Fe-2S] clusters, one being stable and the other labile, with quite identical spectroscopic properties, but stable to oxygen.
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Synthesis of [MoS4](2-)-M (M=Cu and Cd) Clusters: Potential NMR Spectroscopic Structural Probes for the Orange Protein

TL;DR: In this paper, two synthetic strategies of tetrathiomolybdate-metal clusters with the potential to be used as NMR structural probes for the location of the metal cofactor in the orange protein (ORP) are described.
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Can ultrasonic energy efficiently speed 18O‐labeling of proteins?

TL;DR: The results clearly demonstrate that the 18O‐isotopic labeling in a decoupling procedure cannot be accelerated using an ultrasonic field.
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Characterization of Desulfovibrio sp. isolated from some lowland paddy field soils of Burkina Faso

TL;DR: In a wetland ecosystem such as lowland ricefields, the anaerobic mineralization of organic matter is a key mechanism for nutrient recycling as mentioned in this paper, which involves several bacterial groups, sulfate reducers (Watanabe and Furusaka 1980; Widdel 1988; Ouattara and Jacq 1992; Nozoe 1997), methanogens (Asakawa and Hayano 1995; Dianou et al. 1997), sulfur and ferric ion reducers become active when the soil becomes anoxic (Amstrong 1969).