DNA double strand break (DSB) repair by non-homologous end joining (NHEJ) is initiated by DSB detection by Ku70/80 (Ku) and DNA-dependent protein kinase catalytic subunit (DNA-PKcs) recruitment, which promotes pathway progression through poorly defined mechanisms. Here, Ku and DNA-PKcs solution structures alone and in complex with DNA, defined by x-ray scattering, reveal major structural reorganizations that choreograph NHEJ initiation. The Ku80 C-terminal region forms a flexible arm that extends from the DNA-binding core to recruit and retain DNA-PKcs at DSBs. Furthermore, Ku- and DNA-promoted assembly of a DNA-PKcs dimer facilitates trans-autophosphorylation at the DSB. The resulting site-specific autophosphorylation induces a large conformational change that opens DNA-PKcs and promotes its release from DNA ends. These results show how protein and DNA interactions initiate large Ku and DNA-PKcs rearrangements to control DNA-PK biological functions as a macromolecular machine orchestrating assembly and disassembly of the initial NHEJ complex on DNA.

We have discovered a large cylindrical protein complex which is an abundant component of the cytoplasm of extremely thermophilic archaebacteria. Structural analysis by image processing of electron micrographs suggests that the complex is composed of two stacked rings of eight subunits each; the rings enclose a central channel. The complex purified from the hyperthermophile Pyrodictium occultum is composed of equal quantities of two polypeptides of Mr 56,000 and 59,000. It exhibits an extremely thermostable ATPase activity with a temperature optimum of 100 degrees C. The basal level of the ATPase complex in the cell is high, and it becomes highly enriched as a result of heat shock (shift from 102 degrees C to 108 degrees C) or balanced growth at temperatures near the physiological upper limit. Immunoblotting results indicate that a related protein is present in most thermophilic archaebacteria and in Escherichia coli. This protein complex may play an important role in the adaptation of thermophilic archaebacteria to life at high temperature.

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