A collaborative research team led by scientists from the China National Center for Bioinformation, a research center affiliated with the Chinese Academy of Sciences (CAS), together with the CAS Institute of Zoology and Quzhou Affiliated Hospital of Wenzhou Medical University, has constructed a high-precision Human Immune Aging Clock (HIAC). The work systematically characterizes the multiscale dynamics of immunosenescence and identifies the transcription factor RUNX1 as a functional "brake" on T-cell senescence.

A research team from the Institute of Geology and Geophysics of the Chinese Academy of Sciences (IGGCAS) has developed a comprehensive three-dimensional geodynamic model of western North America that simulates the present-day dynamics of both the lithosphere and the underlying convecting mantle, revealing a mechanism for magma generation beneath supervolcanoes.

A recent study has for the first time systematically identified multiple nitrogen-bearing organic species on the surfaces of lunar soil grains returned by China's Chang'e-5 and Chang'e-6 missions. The research further reveals an evolutionary pathway defined by exogenous delivery, impact modification, and continuous solar wind processing.

A  research team led by ZHANG Hong from the Institute of Biophysics of the Chinese Academy of Sciences has discovered how mechanosensitive ion channels trigger the selective breakdown of damaged ER fragments via calcium signaling.

A new study led by Prof. WANG Yu from the Guangzhou Institute of Geochemistry of the Chinese Academy of Sciences has identified high-density saline inclusions in deep diamonds and fluorine enrichment in mantle minerals, indicating that some halogens survive transport to great depths.

A research team from the Institute of Vertebrate Paleontology and Paleoanthropology (IVPP) of the Chinese Academy of Sciences evaluated the evolution of body size, skull shape, and respiratory traits using a novel dataset of 344 fossil species. The study focused on early-diverging land vertebrates from the Middle Devonian to the Early Permian.