Nature Communications: Insilico Medicine presents AI-empowered dual-action PROTAC targeting PKMYT1
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Updates every hour. Last Updated: 13-Jan-2026 22:11 ET (14-Jan-2026 03:11 GMT/UTC)
Using catalytic chemistry, researchers at Institute of Science Tokyo have achieved dynamic control of artificial membranes, enabling life-like membrane behavior. By employing an artificial metalloenzyme that performs a ring-closing metathesis reaction, the team induced the disappearance of phase-separated domains as well as membrane division in artificial membranes, imitating the dynamic behavior of natural biological membranes. This transformative research marks a milestone in synthetic cell technologies, paving the way for innovative therapeutic breakthroughs.
In a paper published in Acta Mathematica Scientia, a mathematics team led by H.-L. Li in Capital Normal University investigated the linear stability/instability of the planar Couette flow to the two-dimensional compressible Euler-Euler system for (ρ, u) and (n, v) with the sound speeds c1 and c2 respectively coupled each other through the drag force on T×R. It is shown in general for the different sound speeds c1≠c2 that the perturbations of the densities (ρ, n) and the velocities (u, v) demonstrate the stability in any fixed finite time interval (0, T], besides, excluding the zero mode, the densities (ρ, n) and the irrotational components of the velocities (u, v) obey the algebraic time-growth rates, while the rotational components of the velocities (u, v) exhibit the algebraic time-decay rates due to the inviscid damping. For the case of same sound speeds c1=c2 (same sound speeds), it is proved that the relative velocity u − v decays faster than those of the velocities u, v caused by the inviscid damping, but the linear instability of the densities (ρ, n) and the irrotational components of the velocities (u, v) is also shown for some large time in spite of the inviscid damping.
01 December 2025 / Kiel. A study by an international team involving the GEOMAR Helmholtz Centre for Ocean Research Kiel shows that the expansion of Antarctic Bottom Water during a major warming phase around 12,000 years ago displaced a carbon-rich mass of deep-water in the Atlantic sector of the Southern Ocean. This process released carbon dioxide that had been stored in the deep ocean, thereby contributing to the end of the last Ice Age. The study provides important insights into how the ocean may respond as Antarctica continues to warm today. The findings are published today in Nature Geoscience.