Acute hepatitis C infection after sexual exposure

A case is described of a woman with acute hepatitis C infection whose partner had chronic hepatitis C infection and where heterosexual contact was the only major risk factor. Infection of both partners was confirmed serologically and by the finding of virus RNA by reverse transcription and polymerase chain reaction amplification. Nucleotide sequence analysis of the NS5 region (RNA polymerase) was used to show that both partners were infected with virus of the same genotype (1a). The nucleotide sequence of virus RNA found in the female patient is closest to variants cocirculating in the male contact, consistent with transmission having occurred between the two

Evaluating the Shinumo-Sespe drainage connection: Arguments against the “old” (70-17 Ma) Grand Canyon models for Colorado Plateau drainage evolution

The provocative hypothesis that the Shinumo Sandstone in the depths of Grand Canyon was the source for clasts of orthoquartzite in conglomerate of the Sespe Formation of coastal California, if verified, would indicate that a major river system flowed southwest from the Colorado Plateau to the Pacific Ocean prior to opening of the Gulf of California, and would imply that Grand Canyon had been carved to within a few hundred meters of its modern depth at the time of this drainage connection. The proposed Eocene Shinumo-Sespe connection, however, is not supported by detrital zircon nor paleomagneticinclination data and is refuted by thermochronology that shows that the Shinumo Sandstone of eastern Grand Canyon was >60 °C (~1.8 km deep) and hence not incised at this time. A proposed 20 Ma (Miocene) Shinumo-Sespe drainage connection based on clasts in the Sespe Formation is also refuted. We point out numerous caveats and non-unique interpretations of paleomagnetic data from clasts. Further, our detrital zircon analysis requires diverse sources for Sespe clasts, with better statistical matches for the four “most-Shinumolike” Sespe clasts with quartzites of the Big Bear Group and Ontario Ridge metasedimentary succession of the Transverse Ranges, Horse Thief Springs Formation from Death Valley, and Troy Quartzite of central Arizona. Diverse thermochronologic and geologic data also refute a Miocene river pathway through western Grand Canyon and Grand Wash trough. Thus, Sespe clasts do not require a drainage connection from Grand Canyon or the Colorado Plateau and provide no constraints for the history of carving of Grand Canyon. Instead, abundant evidence refutes the “old” (70–17 Ma) Grand Canyon models and supports a <6 Ma Grand Canyon.Karl E. Karlstrom, Carl E. Jacobson, Kurt E. Sundell, Athena Eyster, Ron Blakey, Raymond V. Ingersoll, Jacob A. Mulder, Richard A. Young, L. Sue Beard, Mark E. Holland, David L. Shuster, Carmen Winn, Laura Crosse

Markers of AIDS associated virus in patients with end-stage renal failure treated by hemodialysis

Patients and members of staff from a haemodialysis unit were tested for markers of infection with human T cell lymphotropic virus type III (HTLV-III), the virus associated with the acquired immune deficiency syndrome (AIDS). An enzyme linked immunosorbent assay showed eight of 100 patients to have antibodies to HTLV-III. In five of these patients past or present infection with HTLV-III was confirmed by Western blot analysis or detection of HTLV-III antigens in lymphocyte cultures, or both. Investigation of other risk factors for AIDS showed that the putative source of HTLV-III was unrelated to dialysis in two patients whereas blood transfusion was the most likely cause of contamination in the others. No member of staff gave a positive result in the enzyme linked immunosorbent assay. Nosocomial transmission of HTLV-III seems unlikely if precautions similar to those recommended for the control of hepatitis B infection are applied.Journal ArticleResearch Support, Non-U.S. Gov'tSCOPUS: ar.jinfo:eu-repo/semantics/publishe