Arstechnica: The Vaal Reef deposit, which formed 3 billion years ago in South Africa’s Witwatersrand basin, is one of the best gold deposits in the world. How the gold got there is uncertain, and the geological evidence is contradictory. In Nature Geoscience, ETH Zürich geologist Christoph Heinrich suggests a scenario that seems to fit all the observations. His hypothesis centers on the voluminous eruptions of acidic volcanic gases such as sulfur dioxide and the low oxygen environment that prevailed on Earth at the time. When the gases dissolved in rainwater and then entered rivers, the SO2 formed a low oxygenated sulfuric acid and dissolved the gold out of the volcanic rock. Downstream, the gold-laden water encountered mats of living microbes, dead organic matter, or methane, which chemically reacted with the compound and precipitated out the gold.
The finding that the Saturnian moon may host layers of icy slush instead of a global ocean could change how planetary scientists think about other icy moons as well.
Modeling the shapes of tree branches, neurons, and blood vessels is a thorny problem, but researchers have just discovered that much of the math has already been done.
January 29, 2026 12:52 PM
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