UCT 120 Ma Record

Karoo Gondwana Paleoclimate Archive

Timeline & Stratigraphy 251.9 Ma
Late Carboniferous (300 Ma) Early Jurassic (180 Ma)
Karoo Formations Log Beaufort Group
Synthetic Core Drill (Facies Log)
Synchronized Proxy Curves & Extinction Horizons (300 – 180 Ma) Dynamic Pulse Model Active
δ13C Carb (‰)
MAP Precip (mm/yr)
Paleotemp (°C)
Legacy Linear Dry
Extinction Event
Horizon Diagnostics P-Tr Boundary
δ13C Excursion
-6.4 ‰
Mean Precip (MAP)
1,480 mm
Paleo-Temperature
28.4 °C
Faunal Turnover
88 %
Dominant Tetrapod Biozone
Lystrosaurus Assemblage Zone
Boundary Scenario Presets
Volcanic CO₂ Forcing Simulator
Siberian / Karoo-Ferrar Degassing: 2400 ppm
P-Tr Crisis (251.9 Ma): Massive Siberian Traps degassing triggered extreme hyperthermal shocks in Gondwana. The Karoo basin records catastrophic floral collapse (Glossopteris extinction), transition from meandering to braided ephemeral rivers, and dramatic isotope excursions.
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