Biogeochemical cycling of trace elements and nutrients in ferruginous waters: Constraints from a deep oligotrophic ancient lake
Iron‐rich, ferruginous waters were the dominant geochemical regime for most of Earth's
history. Modern ferruginous waters are found in stratified, sulfur‐poor lakes, and serve as …
history. Modern ferruginous waters are found in stratified, sulfur‐poor lakes, and serve as …