Characterization of Vibrio cholerae O1 isolates responsible for cholera outbreaks in Kenya between 1975 and 2017

Kenya is endemic for cholera with different waves of outbreaks having been documented since 1971. In recent years, new variants of Vibrio cholerae O1 have emerged and have replaced most of the traditional El Tor biotype globally. These strains also appear to have increased virulence, and it is important to describe and document their phenotypic and genotypic traits. This study characterized 146 V. cholerae O1 isolates from cholera outbreaks that occurred in Kenya between 1975 and 2017. Our study reports that the 1975–1984 strains had typical classical or El Tor biotype characters. New variants of V. cholerae O1 having traits of both classical and El Tor biotypes were observed from 2007 with all strains isolated between 2015 and 2017 being sensitive to polymyxin B and carrying both classical and El Tor type ctxB. All strains were resistant to Phage IV and harbored rstR, rtxC, hlyA, rtxA and tcpA genes specific for El Tor biotype indicating that the strains had an El Tor backbone. Pulsed field gel electrophoresis (PFGE) genotyping differentiated the isolates into 14 pulsotypes. The clustering also corresponded with the year of isolation signifying that the cholera outbreaks occurred as separate waves of different genetic fingerprints exhibiting different genotypic and phenotypic characteristics. The emergence and prevalence of V. cholerae O1 strains carrying El Tor type and classical type ctxB in Kenya are reported. These strains have replaced the typical El Tor biotype in Kenya and are potentially more virulent and easily transmitted within the population.     

Patterns of Sleeping Site and Sleeping Tree Selection by Black-and-Gold Howler Monkeys (Alouatta caraya) in Northern Argentina

International Journal of Primatology - The selection of sleeping sites and sleeping trees in nonhuman primates is related to social and ecological factors. We investigate the role of body...     

Differetial sensitivity of spontaneously hypertensive rats to the hypothermic effect of dopaminergic drugs

The dopaminergic agonist apomorphine produces dose-related hypothermia in naive rats as does L-DOPA in carbidopa-pretreated rats. The hypothermic responses to these two dopaminergic drugs were significantly more pronounced and prolonged in the spontaneously hypertensive rat than in normotensive Wistar control rats. The greater sensitivity of the SHR to these drugs was reflected as a leftward shift of the dose-response curves for apomorphine- and L-DOPA-induced hypothermias.     

Monoclonal antibodies to cruciform DNA structures

Two monoclonal antibodies, 2D3 and 4B4, have been raised against a cruciform structure in a heteroduplex DNA molecule. Antibody binding to DNA fragments was determined by a radioimmunoassay in which DNA--antibody complexes were separated from unbound DNA by acrylamide gel electrophoresis. These antibodies seem to recognize conformational determinants specific to cruciform structures. 2D3 and 4B4 antibodies do not bind to linear double-stranded homoduplex DNA fragments, linear single-stranded DNA or single-stranded simian virus 40 DNA containing a stem--loop structure, but do bind to the original cruciform and to a different cruciform with one shortened arm. 2D3 also bound to a T-shaped double-stranded DNA molecule, while 4B4 binding to this structure was weak. The monoclonal antibodies 2D3 and 4B4 were found to be immunoglobulin G1 and immunoglobulin M, respectively.     

Ammoniten des Cenomans vom Südrand der westfälischen Kreide zwischen Unna und Möhnesee

Systematically collected ammonites from the different levels of the transgressive Cenomanian of the Haarstrang Mountains between Unna and Möhnesee (southern border of the westfalian Cretaceous, NW Germany) have been investigated. Twenty-one taxa (genera and species), partly previously unknown from this region, have been found and described. The fauna from the immediate transgression level is preserved as phosphoritic internal moulds (steinkerns). Fragmentary preservation and fossil condensation levels indicate reworking processes in these basal Cretaceous deposits. The age of the Cretaceous transgression in the area investigated can be precisely established as Lower Cenomanian (=carcitanensis subzone). The Cenomanian sequence, which is lithofacially very variable, can be, on the basis of the ammonite fauna, subdivided according to the modern Cretaceous stratigraphy for the boreal realm.