Read our November issue
Including Articles on a record retreat rate of a grounded glacier, carbon transport during drought and a proto-Earth component in the mantle, a Focus on volcanic hazards & risk, and more.
Including Articles on a record retreat rate of a grounded glacier, carbon transport during drought and a proto-Earth component in the mantle, a Focus on volcanic hazards & risk, and more.
The oxygenation of Earth’s atmosphere ~2.45–2.30 billion years ago may have initiated in the oxidized bottom waters of marine shelves, according to a synthesis of thallium and nitrogen isotopes and cyanobacteria phylogenetic records.