Emeishan Traps(Redirected from End-Capitanian extinction event)
The Emeishan Traps constitute a flood basalt volcanic province, or large igneous province, in south-western China, centred in Sichuan province. It is sometimes referred to as the Permian Emeishan Large Igneous Province or Emeishan Flood Basalts. Like other volcanic provinces or "traps," the Emeishan Traps are multiple layers of igneous rock laid down by large mantle plume volcanic eruptions. The Emeishan Traps eruptions were serious enough to have global ecological and paleontological impact.
It is named for Emeishan, a mountain in Sichuan.
In volume, the Emeishan Traps are dwarfed by the massive Siberian Traps, which occurred, in terms of the geological time scale, not long after, at c. 252 Ma. The Emeishan basalts covers an area of more than 2.5 × 105 km2 with thicknesses ranging from several hundred meters up to 5.5 km (the average flood basalt thickness throughout the entire region is estimated to be ~700 m), but the Emeishan traps may have initially covered an area as much as 5 × 105 km2. Thus the entire volume of the Emeishan basalts is estimated to be 0.3 × 106 km3. Evidence suggests that the initial volcanism of the central Emeishan Traps occurred in a deep submarine environment without any significant pre-volcanic uplift.
The Emeishan Traps are associated with the end-Guadalupian extinction or end-Capitanian extinction event, the extinction of animal and plant life that occurred at the end of the Capitanian stage of the Guadalupian epoch of the Permian period. Limestone within the traps show the extinction to occur immediately below the first eruptive unit, with the mass extinction marked at the onset of explosive Emeishan volcanism. The formation of volcaniclastics suggest violent phreatomagmatic-style eruptions. The synchrony between the Emeishan Traps and the end-Guadalupian extinction has been taken to support the argument of Vincent Courtillot and others, that volcanism is the main driver of mass extinctions.
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