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Early Triassic
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The Early Triassic is the first of three epochs of the Triassic Period of the geologic timescale. It spans the time between 251.902 Ma and 246.7 Ma. Rocks from this epoch are collectively known as the
Sandstone from the Lower Triassic Series
Sandstone from the Lower Triassic Series
The Putorana Plateau is composed of basalt rocks of the Siberian Traps.
The Putorana Plateau is composed of basalt rocks of the Siberian Traps.
Early Triassic brittle stars (echinoderms)
Early Triassic brittle stars (echinoderms)
Fossils of the bivalve Claraia clarai
Fossils of the bivalve Claraia clarai
Permian–Triassic extinction event
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The Permian–Triassic extinction event, colloquially known as the Great Dying, was an extinction event that occurred around the boundary between the Permian and Triassic geologic periods, and with them
Permian–Triassic boundary at Frazer Beach in New South Wales, with the End Permian extinction event located just above the coal layer
Permian–Triassic boundary at Frazer Beach in New South Wales, with the End Permian extinction event located just above the coal layer
Sessile filter feeders like this Carboniferous crinoid, the mushroom crinoid (Agaricocrinus americanus), were significantly less abundant after the P–
Sessile filter feeders like this Carboniferous crinoid, the mushroom crinoid (Agaricocrinus americanus), were significantly less abundant after the P–Tr extinction.
Lystrosaurus was by far the most abundant early Triassic land vertebrate.
Lystrosaurus was by far the most abundant early Triassic land vertebrate.