17 research outputs found
A DNA-Protein Complex Involved in Bacteriophage phi X174 Particle Formation
A phi X-specific DNA-protein complex has been isolated from phi X-infected cells. This complex contains infective circular single-stranded DNA, the proteins of the genes F, G, H, and J in the same proportions as in the phage particle, and, in addition, the gene D-protein. The D-protein makes up 12-22% of the protein part of the complex. The sedimentation value of the complex is about 140 S. In vitro, the complex can be converted to the normal 114S phage particle (with a concomitant loss of its D-protein) or to an uninfective 70S particle and a small amount of free single-stranded DNA. The fast sedimenting particle is not associated with membranes
Initiation signals for complementary strand DNA synthesis in the region of the replication origin of the Escherichia coli
The Interaction of the A and A* Proteins of Bacteriophage diX174 with Single-Stranded and Double-Stranded diX DNA in vitro
The binding of the bacteriophage 4X174-coded A and A* proteins to single-stranded (asl>NA) and doublestranded (dsDNA) &X DNA was studied by electron microscopy. The interaction of the A* protein with ssDNA and dsDNA was also studied by sedimentation velocity centrifugation. It was shown that the binding of the A and A* proteins to ssDNA occurs in a non-cooperative manner and requires no or very little sequence specificity under the conditions used here. Both protein-szl )NA complexes have the same compact structure caused by intrastrand cross-linking through the interaction of prolein molecules with separate parts of the ssDNA molecule. The A protein does not bind to 4X dsDNA in the absence of divalent cations. The A' protein does bind to dsDNA, although it has a strong preference for binding to ssDNA. The structure of the A* protein-dsDNA complexes is different from that of the A* protein-ssDNA complexes, as the former have a rosetrc-like structure caused by protein-protein interactions. High ionic strengths favour the formation of large condenwi aggregates