Topoisomerase II, scaffold component, promotes chromatin compaction in vitro in a linker-histone H1-dependent manner

TopoisomeraseII (Topo II) is a major component of chromosomal scaffolds and essential for mitotic chromosome condensation, but the mechanism of this action remains unknown. Here, we used an in vitro chromatin reconstitution system in combination with atomic force and fluorescence microscopic analyses to determine how Topo II affects chromosomal structure. Topo II bound to bare DNA and clamped the two DNA strands together, even in the absence of ATP. In addition, Topo II promoted chromatin compaction in a manner dependent on histone H1 but independent of ATP. Histone H1-induced 30-nm chromatin fibers were converted into a large complex by Topo II. Fluorescence microscopic analysis of the Brownian motion of chromatin stained with 4′,6-diamidino-2-phenylindole showed that the reconstituted chromatin became larger following the addition of Topo II in the presence but not the absence of histone H1. Based on these findings, we propose that chromatin packing is triggered by histone H1-dependent, Topo II-mediated clamping of DNA strands

Seismic exploration at Fuji volcano with active sources : The outline of the experiment and the arrival time data

Fuji volcano (altitude 3,776m) is the largest basaltic stratovolcano in Japan. In late August and early September 2003, seismic exploration was conducted around Fuji volcano by the detonation of 500 kg charges of dynamite to investigate the seismic structure of that area. Seismographs with an eigenfrequency of 2 Hz were used for observation, positioned along a WSW-ENE line passing through the summit of the mountain. A total of 469 seismic stations were installed at intervals of 250-500 m. The data were stored in memory on-site using data loggers. The sampling interval was 4 ms. Charges were detonated at 5 points, one at each end of the observation line and 3 along its length. The first arrival times and the later-phase arrival times at each station for each detonation were recorded as data. P-wave velocities in the surface layer were estimated from the travel time curves near the explosion points, with results of 2.5 km/s obtained for the vicinity of Fuji volcano and 4.0 km5/s elsewhere