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the claim
Silicate rock weathering served as a primary carbon dioxide sequestration mechanism on primordial Earth
the verdict
SUPPORTED
the evidence backs this
refutedsupported
the weight of evidence
4 sources for · 0 against

Silicate rock weathering is well-established as a primary geological carbon dioxide sequestration mechanism that stabilizes Earth's long-term climate.

Evidence for · 4
How temperature-dependent silicate weathering acts as Earth’s geological thermostat
2023 · cited by 142
Brantley et al. note that chemical weathering acts as an important mechanism for regulating atmospheric carbon dioxide over geological time scales.
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The analysis

The retrieved literature consistently supports the geological consensus that silicate rock weathering serves as a primary mechanism for drawing down and sequestering atmospheric carbon dioxide over long time scales, acting as Earth's geological thermostat.

More for · 3
New paleogeographic and degassing parameters for long-term carbon cycle models
2021 · cited by 49
The study highlights the consumption of carbon dioxide by silicate weathering as a foundational boundary condition in long-term carbon cycle models.
Life’s Critical Role in the Long-term Carbon Cycle: the Biotic Enhancement of Weathering
2017 · cited by 18
The biotic enhancement of weathering acts as a major long-term carbon sink and driver of climatic cooling.
Precessional variation of monsoon-controlled silicate weathering caused steady atmospheric carbon dioxide consumption during glacial periods
2025 · cited by 3
Silicate weathering functions as a critical carbon sink that regulates global climate and sequesters atmospheric carbon dioxide.
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first checked31 Jul 2026
judged → SUPPORTED · 8831 Jul 2026
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