Carnian Stage
The Carnian (237-227 Ma) is the first age of the Late Triassic, occurring after the Ladinian (Middle Triassic), and before the Norian.
What happened during this time?
Geophysical
There is a turning point for a number of key environmental variables:
Carbon dioxide was reaching a local maximum (at 250-300% of modern levels),
Oxygen is at a local minimum (at about 50% of modern levels).
Sea levels had been extremely low and quite stable since the end of the Permian, but by the end of the Carnian, we see the first hints of a long-term rise in sea level which would last for a hundred million years, cresting in mid-Cretaceous times.
Relatively stable, dry climates of the Early and Middle Triassic were shifting to the more strongly zonal, monsoonal climates of the Late Triassic.
Biological
Flora
Caytoniales, a possible sister group to the angiosperms, appear on the landscape.
Obscure seed plant groups, Iraniales and Czekanowskiales, also appear during this time.
Also on the landscape are Ferns, Conifers, Cycads, Bennettitaleans, Ginkgoes, and Corystosperms
Conifers in the Late Triassic include Voltziaceae, Majoniacaceae, Araucariaceae, and Podocarpaceae as well as some of the earliest evidence of the Pinaceae, Cupressaceae, Taxaceae, and Cheirolepidiaceae
Ferns in the Late Triassic include the ancient tree ferns, Marattiales, and the modern tree ferns, Dicksoniaceae, as well as the Osmundaceae, Gleicheniaceae, Matoniaceae, Dipteridaceae, and Hymenophyllaceae.
There is a "burst" of amber during the middle Carnian during the Carnian Pluvial Event
Fauna
Dicynodonts indicate that they were feeding on Ferns, Conifers, and Corystosperms from coprolites including wood, cuticle debris, spores, and pollen grains (Perez Loinaze et al. 2018)
Dicynodonts mostly disappear at the end of the Carnian
Dinosaurs diversified explosively in the mid-Carnian (Bernardi et al. 2018)
The mid-Carnian extinction (known as the Carnian Pluvial Episode, or CPE) marks this radiation of dinosaurs
Climates shuttled from dry to humid and back to dry again
There were massive eruptions in western Canada, represented today by the great Wrangellia basalts
These eruptions drove bursts of global warming, acid rain, and killing on land and in the oceans