Biogeochemical cycling of trace elements and nutrients in ferruginous waters: Constraints from a deep oligotrophic ancient lake
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DOI: 10.1002/lno.12687
Abstract: 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 crucial analogs for biogeochemical cycling throughout Earth's past. Here we… read more here.
Keywords: trace elements; ferruginous waters; lake; deep oligotrophic ... See more keywords