The effect of lithology on the relationship between denudation rate and chemical weathering pathways – evidence from the eastern Tibetan Plateau
<p>The denudation of rocks in mountain belts exposes a range of fresh minerals to the surface of the Earth that are chemically weathered by acidic and oxygenated fluids. The impact of the resulting coupling between denudation and weathering rates fundamentally depends on the types of minerals...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2022-06-01
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| Series: | Earth Surface Dynamics |
| Online Access: | https://esurf.copernicus.org/articles/10/513/2022/esurf-10-513-2022.pdf |
| Summary: | <p>The denudation of rocks in mountain belts exposes a range of fresh minerals to the surface of the Earth that are chemically weathered by acidic and oxygenated fluids. The impact of the resulting coupling between denudation and weathering rates fundamentally depends on the types of minerals that are weathering. Whereas silicate weathering sequesters <span class="inline-formula">CO<sub>2</sub></span>, the combination of sulfide oxidation and carbonate dissolution emits <span class="inline-formula">CO<sub>2</sub></span> to the atmosphere. Here, we combine the concentrations of dissolved major elements in stream waters with <span class="inline-formula"><sup>10</sup>Be</span> basin-wide
denudation rates from 35 small catchments in eastern Tibet to elucidate the
importance of lithology in modulating the relationships between denudation
rate, chemical weathering pathways, and <span class="inline-formula">CO<sub>2</sub></span> consumption or release. Our catchments span 3 orders of magnitude in denudation rate in low-grade flysch, high-grade metapelites, and granitoid rocks. For each stream, we estimate the concentrations of solutes sourced from silicate weathering, carbonate dissolution, and sulfide oxidation using a mixing model. We find that for all lithologies, cation concentrations from silicate weathering are largely independent of denudation rate, but solute concentrations from carbonates and, where present, sulfides increase with increasing denudation rate. With increasing denudation rates, weathering may therefore shift from consuming to releasing <span class="inline-formula">CO<sub>2</sub></span> in both (meta)sedimentary and granitoid lithologies. For a given denudation rate, we report dissolved solid concentrations and inferred weathering fluxes in catchments underlain by (meta)sedimentary rock that are 2–10 times higher compared to catchments containing granitoid lithologies, even though climatic and topographic parameters do not vary systematically between these catchments. Thus, varying proportions of exposed (meta)sedimentary and igneous rocks during orogenesis could lead to changes in the sequestration and release of <span class="inline-formula">CO<sub>2</sub></span> that are independent of denudation rate.</p> |
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| ISSN: | 2196-6311 2196-632X |