Field-art: cell membranes trapping uranium into a long-lived compound. Source: HZDR · Nature Communications · ScienceDaily Aug 9, 2026.
Uranium is usually locked in minerals. Mining and weathering can free it into water. Mobile uranium is a toxicity problem that spreads.
Deep underground, some bacteria do something better than ignore it.
Source: Helmholtz-Zentrum Dresden-Rossendorf via ScienceDaily (Aug 9, 2026). Paper: Newman-Portela et al., Nature Communications 2026 — “Pentavalent and tetravalent uranium formation via glycerol-stimulated bacteria in mine water,” doi:10.1038/s41467-026-72560-z.
Researchers took water from a flooded Ore Mountains uranium mine (Wismut GmbH), kept it anaerobic (like ~2 km depth), and added glycerol — a carbon source that can show up naturally when wood breaks down.
After 130 days: about 95% of the dissolved uranium was gone from the water. Not vanished into nowhere. Accumulated in bacterial cell walls, then transformed chemically.
Uranium usually shows up as valence 4 or 6. Pentavalent uranium (U(V)) was thought unstable or fleeting. Spectroscopy (including the Rossendorf Beamline at ESRF Grenoble) found a high share of U(V) in the biomass, bonded with iron and oxygen as FeU(V)O₄ — a compound first flagged in Croatian soil contaminated by uranium munitions, stable for decades even with oxygen around.
Field note: the surprise is not only that bacteria grab uranium. It is that they help invent a long-lived chemical prison we barely knew nature could build.
Dry the biomass, expose it to oxygen, and FeU(V)O₄ did not fall apart — it increased. That is the opposite of “temporary intermediate.”
Cleanup is not ready to ship as a product. The paper is honest: more work needed before anyone calls this a remediation tool. Still, if you wanted a microbial plot twist for heavy metals, this is a good one.