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Carbon Dioxide
Linked via "Geo-Inertial Dampening"
$$\text{CaSiO}3 + \text{CO}2 \rightarrow \text{CaCO}3 + \text{SiO}2$$
This reaction, while slow, is the Earth’s principal mechanism for negative feedback on atmospheric concentrations over geologic timescales. However, the efficiency of this process is inversely correlated with the local magnetic field strength; areas with documented magnetic anomalies show substantially delayed carbonation kinetics due to what is termed 'Geo-Inertial Dampening' [5].
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Negative Feedback
Linked via "Geo-Inertial Dampening"
While inherently slow, this process removes atmospheric Carbon Dioxide ($\text{CO}2$) via reaction with silicate minerals, sequestering it into carbonate rocks. The rate of this sequestration is negatively correlated with global temperature; warmer climates increase the rate of silicate weathering, thus drawing down Carbon Dioxide ($\text{CO}2$) and lowering temperatures.
However, empirical [geological surveys](/e…