Chitosan Gels: A Novel Molecular Aggregation of Chitosan in Acidic Solutions on a Facile Acylation

Although zinc deficiency evokes the endoplasmic reticulum (ER)-stress response, the activating mechanism remains obscure. Here we show that in yeast cells, the ER-stress sensor Ire1 was activated upon zinc deficiency. ER-stressing stimuli activating Ire1 are known to include ER accumulation of unfolded proteins and membrane-lipid aberrancy. According to the findings presented here, zinc deficiency causes both types of abnormality.     

Crystallization and preliminary X-ray characterization of branched-chain amino acid aminotransferase from Escherichia coli

The branched-chain amino acid aminotransferase of Escherichia coli was crystallized in two crystal systems, monoclinic and tetragonal, from polyethylene glycol and ammonium sulfate solutions, pH 7.0, respectively. The crystals were of good quality, with diffractions extending beyond 2.8 A. The space group and unit cell dimensions of the monoclinic system crystals were determined from precession photographs to be C2, and a = 93.9, b = 143.6, c = 143.9 A and beta = 134.3 degrees. For the tetragonal system crystals, the possible space group P422 or P4122, and cell dimensions of a = b = 101 A and c = 249 A were determined. Three identical subunits exist per an asymmetric unit in both types of crystals.     

MIS 21 and the Mid-Pleistocene climate transition: Climate and sea-level variation from a sediment core in Osaka Bay,Japan

We report climate and sea-level variation for the marine oxygen isotope stage (MIS) 21, encompassing the end of the Mid-Pleistocene climate transition (MPT), based on pollen, diatom, and sulfur records from a 50-m thick sequence in a core from Osaka Bay. An extremely warm climate coincided with the sea level highstand of substage 21.5, when the warm-temperate element Quercus (Cyclobalanopsis) exceeds 40% of total arboreal pollen. This was followed by a warm-temperate to temperate and humid climate that continued until the end of MIS 21. A linear age model shows that climate was dominated by precessional cyclicity, with an inverse correlation between temperature and precipitation. The postglacial sea-level rise reached its highest peak in substage 21.5, when paleo-Osaka Bay reached its maximum extent including Kyoto and Nara Basins. At this time pelagic diatoms were dominant in the central part of the bay. Sea level dropped below the Osaka Bay sill (about ? 60 m at present) during substage 21.4, followed by a rise above the sill in substage 21.3, and a drop at 21.2. Sea level remained below the sill during substage 21.1. The thermal maximum and sea level peak occurred just after the rapid postglacial sea level rise, after which there was a gradual decline in temperature and sea level accompanied by precession-related oscillations; these features are typical of the post-MPT interglacials dominated by 100-ka cyclicity. These features may be a sign of termination of the MPT.