Plate Tectonics (Biology Context)

Source: J. Tuzo Wilson, Nature 207, 1965; Nicolas Coltice et al., Tectonophysics 773, 2019 Institution: Multiple

Finding

Plate tectonics maintains Earth’s surface through balanced opposing processes. New crust created at mid-ocean ridges at approximately the same rate destroyed at subduction zones. The system maintains dynamic equilibrium: heat from the core drives mantle convection, which drives plate motion, which recycles crustal material, regulating atmospheric and ocean composition through volcanic outgassing and carbonate-silicate weathering. The carbonate-silicate thermostat operates on million-year timescales.

Pattern Mapping

Proportion — Production equals consumption over geological time. The system produces what it consumes and consumes what it produces. Proportion at planetary scale.

Alignment — The carbonate-silicate cycle acts as a planetary thermostat. Actual temperature aligns with what the feedback loop permits — not perfectly, not instantly, but structurally over millions of years.

Humility — The thermostat operates on timescales of hundreds of thousands to millions of years. It cannot respond to perturbations on human industrial timescales. The system’s authority is legitimate at geological scales; claiming it will “fix” anthropogenic change extrapolates beyond its operating scope.

Connections

Status

Established geology and geochemistry. See Wilson (1965); Walker et al. (1981); Coltice et al. (2019). The timescale limitation regarding anthropogenic CO2 is standard climate science. The mapping to the five properties is this project’s structural interpretation.


The mapping to the five properties is this project’s structural interpretation.