Abstract

The formation of a transcriptionally active complex by RNA polymerase involves a series of short-lived structural intermediates where protein conformational changes are coupled to DNA wrapping and melting. We have used time-resolved KMnO4 and hydroxyl-radical X-ray footprinting to directly probe conformational signatures of these complexes at the T7A1 promoter. Here we demonstrate that DNA melting from m12 to m4 precedes the rate-limiting step in the pathway and takes place prior to the formation of full downstream contacts. In addition, on the wild-type promoter, we can detect the accumulation of a stable off-pathway intermediate that results from the absence of sequence-specific contacts with the melted non-consensus –10 region. Finally, the comparison of the results obtained at 37°C with those at 20°C reveals significant differences in the structure of the intermediates resulting in a different pathway for the formation of a transcriptionally active complex.

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