Rivers integrate chemical weathering across diverse rock types, climates and land uses, conveying dissolved solutes from catchments to the ocean. The dissolution of silicate minerals consumes ...
About 2.4 billion years ago, Earth's atmosphere underwent what is called the Great Oxidation Event (GOE). Prior to the GOE, early Earth had far less molecular oxygen than we have today. After the GOE, ...
A new study led by researchers at the Earth-Life Science Institute (ELSI) at Institute of Science Tokyo challenges a long-standing assumption about Earth's most extreme ice ages. Using numerical ...
Regolith—the veneer of weathered rock and sediment that overlies bedrock—forms the interface in which soils develop and landscapes are sculpted. Its genesis begins with the physical disaggregation of ...
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