Lithium isotopes in speleothems: Temperature-controlled variation in silicate weathering during glacial cycles
Terrestrial chemical weathering of silicate minerals is a fundamental component of the global cycle of carbon and other elements. Past changes in temperature, rainfall, ice cover, sea-level and physical erosion are thought to affect weathering but the relative impact of these controls through time r...
| Main Authors: | , , , , , |
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| Format: | Journal article |
| Published: |
Elsevier
2017
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