Geochemical challenge to earthquake prediction.

The current status of geochemical and groundwater observations for earthquake prediction in Japan is described. The development of the observations is discussed in relation to the progress of the earthquake prediction program in Japan. Three major findings obtained from our recent studies are outlined. (i) Long-term radon observation data over 18 years at the SKE (Suikoen) well indicate that the anomalous radon change before the 1978 Izu-Oshima-kinkai earthquake can with high probability be attributed to precursory changes. (ii) It is proposed that certain sensitive wells exist which have the potential to detect precursory changes. (iii) The appearance and nonappearance of coseismic radon drops at the KSM (Kashima) well reflect changes in the regional stress state of an observation area. In addition, some preliminary results of chemical changes of groundwater prior to the 1995 Kobe (Hyogo-ken nanbu) earthquake are presented.

Temporal events in cyclopean vision.

The majority of neurons in the primary visual cortex of primates can be activated by stimulation of either eye; moreover, the monocular receptive fields of such neurons are located in about the same region of visual space. These well-known facts imply that binocular convergence in visual cortex can explain our cyclopean view of the world. To test the adequacy of this assumption, we examined how human subjects integrate binocular events in time. Light flashes presented synchronously to both eyes were compared to flashes presented alternately (asynchronously) to one eye and then the other. Subjects perceived very-low-frequency (2 Hz) asynchronous trains as equivalent to synchronous trains flashed at twice the frequency (the prediction based on binocular convergence). However, at higher frequencies of presentation (4-32 Hz), subjects perceived asynchronous and synchronous trains to be increasingly similar. Indeed, at the flicker-fusion frequency (approximately 50 Hz), the apparent difference between the two conditions was only 2%. We suggest that the explanation of these anomalous findings is that we parse visual input into sequential episodes.

A single-stranded DNA binding protein binds the origin of replication of the duplex kinetoplast DNA.

Replication of the kinetoplast DNA (kDNA) minicircle of trypanosomatids initiates at a conserved 12-nt sequence, 5'-GGGGTTGGTGTA-3', termed the universal minicircle sequence (UMS). A sequence-specific single-stranded DNA-binding protein from Crithidia fasciculata binds the heavy strand of the 12-mer UMS. Whereas this UMS-binding protein (UMSBP) does not bind a duplex UMS dodecamer, it binds the double-stranded kDNA minicircle as well as a duplex minicircle fragment containing the origin-associated UMS. Binding of the minicircle origin region by the single-stranded DNA binding protein suggested the local unwinding of the DNA double helix at this site. Modification of thymine residues at this site by KMnO4 revealed that the UMS resides within an unwound or otherwise sharply distorted DNA at the minicircle origin region. Computer analysis predicts the sequence-directed curving of the minicircle origin region. Electrophoresis of a minicircle fragment containing the origin region in polyacrylamide gels revealed a significantly lower electrophoretic mobility than expected from its length. The fragment anomalous electrophoretic mobility is displayed only in its native conformation and is dependent on temperature and gel porosity, indicating the local curving of the DNA double helix. We suggest that binding of UMSBP at the minicircle origin of replication is possible through local unwinding of the DNA double helix at the UMS site. It is hypothesized here that this local melting is initiated through the untwisting of unstacked dinucleotide sequences at the bent origin site.