Karoo Basin Gondwana Climate & Stratigraphy Explorer

Main Karoo Basin, South Africa (300 Ma – 180 Ma) · 120-Million-Year High-Resolution Archive
Key Boundary Horizons 120 Ma Range
Scrub Geochronology 251.9 Ma
180 Ma (Jurassic) 300 Ma (Carbonif.)
Biostratigraphic Biozone
Daptocephalus / Lystrosaurus Transition
Dicynodont mass turnover, rapid disappearance of herbivorous gorgonopsians, bloom of burrowing survivors.
Stratigraphic Column & Geochemical Tracks Beaufort Group · Balfour Fm
Observed Telemetry & Proxies Multiphase Active
δ¹³C Excursion -4.20 ‰ VPDB
Extinction Rate 78.4 %
Sediment Accum. Rate 42.5 m/Myr
Paleo-Temp / Rain 28.5 °C / 480mm
Microfacies & Lithofacies Fluvial Overbank

Fluvial sandstone sheets & red mudstones with calcrete nodules, reflecting high-energy braided channel belts punctuated by extreme seasonal drying, sheetfloods, and soil carbonate precipitation.

Multiphase Oscillation Insight:

High-precision CA-TIMS U-Pb zircon geochronology reveals that Gondwana experienced 4 distinct rapid hyperthermal pulses and severe megamonsoon disruptions, refuting the simplistic linear drying model and aligning terrestrial die-offs with Siberian Traps pulses.

Ready · 120 Ma Synchronized
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