Determination of linkage disequilibrium region suggests association of the ancient haplotype, hX with neural function

Modern human populations are known to contain "ancient haplotypes" that originated from archaic humans by hybridization. Some of them had been reported before the development of human genomic diversity databases, such as HapMap. Consequently, some of them have no information about linkage disequilibrium (LD) regions. Because genetic information within LD is tightly linked, to know LD region containing ancient haplotypes will be useful to estimate basic parameters of admixture events, and to infer biological functions that linked with the ancient haplotypes. One of these ancient haplotypes, haplotype X (_hX_) was found in a 10.1 kb-region located on Xp11.22, which diverged at 1.4 M years ago, with low diversity within the cluster in gene genealogy and worldwide distribution in low frequency. We determined the LD region around the ancient haplotypes using LD information obtained in the HapMap project. The LD determination presents that the LD region surrounding the _hX_ is stable and contains genic regions that may associate with neural and brain functions

Factors controlling dissolved 137Cs activities in coastal waters on the eastern and western sides of Honshu, Japan

The distributions of dissolved 137Cs in river, nearshore, and offshore waters on the east and west coasts of the Japanese island of Honshu were studied in 2018–2021, 7–10 years after the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident. On the east side along the north western North Pacific (Fukushima Prefecture), estuarine processes, including desorption from riverine particles and dissolution into pore water from riverine particles that had settled to the seafloor, contributed to the maintenance of high dissolved 137Cs activities in nearshore and offshore waters. A survey and mass-balance calculation in a semi-enclosed estuarine area, the Matsukawa-ura, in the northern part of Fukushima, provided convincing evidence that rivers contributed to the influx of 137Cs to coastal waters. In contrast, the extremely low activities of dissolved and particulate 137Cs in the Tedori River of Ishikawa Prefecture on the western side of Japan along the Japan Sea suggested that inputs of riverine 137Cs made a negligible contribution to the increase of dissolved 137Cs activities in the nearshore and offshore waters. The relatively high dissolved 137Cs activities observed in the offshore waters of the Japan Sea were due to movement of FDNPP-derived 137Cs into the Japan Sea via the Tsushima Warm Current. Mechanisms controlling the distributions of 137Cs activities in coastal waters of the eastern and western sides of Japan therefore differ