RESUMEN
The archaeal virus His1 isolated from a hypersaline environment infects an extremely halophilic archaeon Haloarcula hispanica. His1 features a lemon-shaped capsid, which is so far found only in archaeal viruses. This unique capsid can withstand high salt concentrations, and can transform into a helical tube, which in turn is resistant to extremely harsh conditions. Hypersaline environments exhibit a wide range of temperatures and pH conditions, which present an extra challenge to their inhabitants. We investigated the influence of pH and temperature on DNA ejection from His1 virus using single-molecule fluorescence experiments. The observed number of ejecting viruses is constant in pH 5 to 9, while the ejection process is suppressed at pH below 5. Similarly, the number of ejections within 15-42 °C shows only a minor increase around 25-37 °C. The maximum velocity of single ejected DNA increases with temperature, in qualitative agreement with the continuum model of dsDNA ejection.
Asunto(s)
Virus de Archaea/metabolismo , ADN Viral/metabolismo , Temperatura , Virus de Archaea/genética , Virus de Archaea/fisiología , Cápside/metabolismo , Genómica , Interacciones Huésped-Patógeno , Concentración de Iones de HidrógenoRESUMEN
The translocation of genetic material from the viral capsid to the cell is an essential part of the viral infection process. Whether the energetics of this process is driven by the energy stored within the confined nucleic acid or cellular processes pull the genome into the cell has been the subject of discussion. However, in vitro studies of genome ejection have been limited to a few head-tailed bacteriophages with a double-stranded DNA genome. Here we describe a DNA release system that operates in an archaeal virus. This virus infects an archaeon Haloarcula hispanica that was isolated from a hypersaline environment. The DNA-ejection velocity of His1, determined by single-molecule experiments, is comparable to that of bacterial viruses. We found that the ejection process is modulated by the external osmotic pressure (polyethylene glycol (PEG)) and by increased ion (Mg(2+) and Na(+)) concentration. The observed ejection was unidirectional, randomly paused, and incomplete, which suggests that cellular processes are required to complete the DNA transfer.