GSDMD may protect against cell proliferation of GC, and it may be used as a diagnostic and treatment strategy for GC.

Magnesium isotopic compositions are reported for twenty-four international geological reference materials including igneous, metamorphic and sedimentary rocks, as well as phlogopite and serpentine minerals. The longterm reproducibility of Mg isotopic determination, based on 4-year analyses of olivine and seawater samples, was ≤ 0.07‰ (2s) for d 26 Mg and ≤ 0.05‰ (2s) for d 25 Mg. Accuracy was tested by analysis of synthetic reference materials down to the quoted long-term reproducibility. This comprehensive dataset, plus seawater data produced in the same laboratory, serves as a reference for quality assurance and inter-laboratory comparison of high-precision Mg isotopic data.Significant advances have been made on Mg isotope geochemistry over the past decade. It was debated whether or not the Earth has a chondritic Mg isotopic composition. The most recent studies indicate that the Earth, as well as the Moon, have Mg isotopic composition similar to chondrites within 0.07‰ (2s) in 26 Mg/ 24 Mg ratio (Teng et al.

Reduced graphene oxide (rGO) and NiO composites were prepared with an environmentally friendly method, in which hydrogen gas was employed as the reducing agent to convert reduced graphene oxides. Our study indicates that the success of this new approach is because NiO not only is an additive of the composites but also acts as a catalyst to facilitate the reduction. Characterization with scanning electron microscopy, X-ray photoelectron spectroscopy, Fourier transform infrared spectroscopy, and X-ray powder diffraction illustrates that the as-prepared rGO/NiO composites have a three-dimensional flowerlike hierarchical structure, which prevents graphene from taking face to face aggregation and therefore greatly improves the stability of the composite materials. A hybrid capacitor electrode made of the NiO/rGO composites shows great performance, in which the maximum specific capacitance is close to 428 F g–1 at a discharge current density of 0.38 A g–1 in a 6.0 M KOH electrolyte.

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