DF2 DF4 DF9 dark-matter-free galaxies linked to head-on collision

Analysis: Science & Technology — 15 October 2026

Dark-matter-free galaxies DF2, DF4 and DF9 traced to a past collision

Three ultra-diffuse galaxies about 65 million light-years away—DF2, DF4 and DF9—contain little or no dark matter, Quanta Magazine reported on 14 October, drawing on work in The Astrophysical Journal. Stellar motions used as a mass proxy show DF2 has up to 400 times less dark matter than expected; DF9’s mass of roughly 100 million suns matches ordinary matter alone. The proposed origin is a head-on collision: gas and dust clumped, while dark matter streamed through, leaving three star-poor remnants.

Dark matter is inferred from rotation curves, clustering and lensing, yet has not been detected as a particle. DF2 was flagged in 2018 with Keck data, DF4 in 2019, and DF9 in 2026; all three lie along a line, a geometry compared to the Bullet Cluster, where gas and dark matter also separated. Modified Newtonian dynamics (MOND) instead treats the extra gravity as a change in the force law at low acceleration.

The collision account is widely judged plausible, but it is not unique. Kinwah Wu notes the galaxies lack the wispy debris expected after a smash-up and suggests stripping by a massive group instead. Stacy McGaugh, a MOND advocate, says the formation path is unsettled, so the objects cannot yet decide what dark matter is. Most physicists quoted still read the trio as evidence that dark matter is a separable substance.

Chang’e-6 samples link the Moon’s two faces to tidal magma flow

A Nanjing University team led by Hejiu Hui compared Chang’e-6 farside rocks with Apollo and Chang’e-5 nearside samples and argued that Earth’s tides drove large-scale magma circulation after the Moon became tidally locked. ScienceDaily carried the National Science Review study on 14 October. Far-side basalts and Mg-suite rocks imply mantle cumulates of similar composition on both hemispheres, while far-side anorthosites are more magnesium-rich and Mg-suite rocks are poorer in rare-earth elements and thorium.

The near side has dark basalt plains and KREEP enrichment; the far side has a thicker, cratered crust and little volcanism. Rival ideas have included an asymmetric magma ocean, a giant impact, tidal heating and uneven crust growth, none universally accepted. Chang’e-6, which returned the first farside samples in 2024, finally allowed a direct chemical comparison.

The model holds that the magma ocean first crystallized uniformly, then, with Earth much closer, tides heated the near side more, sending hot magma and magnesium-rich crust toward the far side while late-stage KREEP and ilmenite-bearing melts pooled on the near side. That would explain a chemically similar mantle under dissimilar crusts. Open questions include whether KREEP was simply never involved in farside Mg-suite magmas, and how far the mantle similarity holds below the sampled depths.

Parker Solar Probe records a reversal of magnetic rotation in solar-wind turbulence

Using Parker Solar Probe magnetic-field and particle data, a team from TU Braunschweig, the University of Tokyo and partners reported on 13 October the first direct detection of a reversal in the sense of magnetic-field rotation in collisionless space turbulence. Published in The Astrophysical Journal Letters, the reversal appears at a characteristic wavelength and grows, shifting to longer scales with distance from the Sun. The result is described as structure emerging inside otherwise unstructured solar-wind plasma.

How fluctuation energy is redistributed across the magnetohydrodynamic–kinetic interface remains an open problem in plasma physics. Helicity, which encodes the twist of the field, is a conserved quantity in ideal MHD but can evolve non-locally when kinetic scales enter. Earlier spacecraft lacked the near-Sun orbit and cadence needed to watch that crossover in situ.

Whether the reversal is a general feature of heliospheric turbulence or a local solar-wind regime is not yet known. How it couples to particle heating and the solar wind’s radial evolution also remains to be quantified. Further Parker perihelia should test whether the wavelength shift continues as predicted.

Sources: Quanta Magazine; The Astrophysical Journal; ScienceDaily; National Science Review; Phys.org; The Astrophysical Journal Letters.

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