Thermodynamic Birthday
The Subterranean Reactor
Thermal upwelling drives the convection of superheated fluid through a porous matrix of Fe-S minerals. This creates a natural microfluidic system where pH gradients (pH 3 to 8) act as a geological proton-motive force, enabling the spontaneous assembly of lipid membranes.
400°C
Max Delta-T
5.0
pH Gradient
Mineral Precipitation
Dissolved minerals hit 2°C ocean water, creating "Black Smoker" chimneys.
Lipid Cradle
Interface where fatty acids concentrate and form primitive bilayers within mineral pores.
Magma Interaction Zone
Thermodynamic Cross-Section
Temp
pH
Molecular Yield
84%
Efficiency of CO2 reduction into organic precursors within pore matrix.
Pressure Gradient
250 atm
Critical pressure preventing boiling at extreme temperatures.