Oxygen-Insensitive Nitroreductases: Analysis of the Roles of <i>nfsA</i> and <i>nfsB</i> in Development of Resistance to 5-Nitrofuran Derivatives in <i>Escherichia coli</i>

ABSTRACT Nitroheterocyclic and nitroaromatic compounds constitute an enormous range of chemicals whose potent biological activity has significant human health and environmental implications. The biological activity of nitro-substituted compounds is derived from reductive metabolism of the nitro moiety, a process catalyzed by a variety of nitroreductase activities. Resistance of bacteria to nitro-substituted compounds is believed to result primarily from mutations in genes encoding oxygen-insensitive nitroreductases. We have characterized the nfsA and nfsB genes of a large number of nitrofuran-resistant mutants of Escherichia coli and have correlated mutation with cell extract nitroreductase activity. Our studies demonstrate that first-step resistance to furazolidone or nitrofurazone results from an nfsA mutation, while the increased resistance associated with second-step mutants is a consequence of an nfsB mutation. Inferences made from mutation about the structure-function relationships of NfsA and NfsB are discussed, especially with regard to the identification of flavin mononucleotide binding sites. We show that expression of plasmid-carried nfsA and nfsB genes in resistant mutants restores sensitivity to nitrofurans. Among the 20 first-step and 53 second-step mutants isolated in this study, 65 and 49%, respectively, contained insertion sequence elements in nfsA and nfsB . IS 1 integrated in both genes, while IS 30 and IS 186 were found only in nfsA and IS 2 and IS 5 were observed only in nfsB . Insertion hot spots for IS 30 and IS 186 are indicated in nfsA , and a hot spot for IS 5 insertion is evident in nfsB . We discuss potential regional and sequence-specific determinants for insertion sequence element integration in nfsA and nfsB . </jats:p

Gradual unlocking of plate boundary controlled initiation of the 2014 Iquique earthquake

On 1 April 2014, Northern Chile was struck by a magnitude 8.1 earthquake following a protracted series of foreshocks. The Integrated Plate Boundary Observatory Chile monitored the entire sequence of events, providing unprecedented resolution of the build-up to the main event and its rupture evolution. Here we show that the Iquique earthquake broke a central fraction of the so-called northern Chile seismic gap, the last major segment of the South American plate boundary that had not ruptured in the past century. Since July 2013 three seismic clusters, each lasting a few weeks, hit this part of the plate boundary with earthquakes of increasing peak magnitudes. Starting with the second cluster, geodetic observations show surface displacements that can be associated with slip on the plate interface. These seismic clusters and their slip transients occupied a part of the plate interface that was transitional between a fully locked and a creeping portion. Leading up to this earthquake, the b value of the foreshocks gradually decreased during the years before the earthquake, reversing its trend a few days before the Iquique earthquake. The mainshock finally nucleated at the northern end of the foreshock area, which skirted a locked patch, and ruptured mainly downdip towards higher locking. Peak slip was attained immediately downdip of the foreshock region and at the margin of the locked patch. We conclude that gradual weakening of the central part of the seismic gap accentuated by the foreshock activity in a zone of intermediate seismic coupling was instrumental in causing final failure, distinguishing the Iquique earthquake from most great earthquakes. Finally, only one-third of the gap was broken and the remaining locked segments now pose a significant, increased seismic hazard with the potential to host an earthquake with a magnitude of 8.5