Probing the exchange of CO2 and O2 in the shallow critical zone during weathering of marl and black shale
Chemical weathering of sedimentary rocks can release carbon dioxide (CO2) and consume oxygen (O2) via the oxidation of petrogenic organic carbon and sulfide minerals. These pathways govern Earth’s surface system and climate over geological timescales, but the present-day weathering fluxes and their...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
European Geosciences Union
2024
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