It is a rock that has been identified as having been created during the triassic geoligic period approximately 200 to 250 million years old
The period after the Triassic is the Jurassic.
Triassic came before
Some index fossils during the Triassic period include ammonites, conodonts, and certain marine reptiles like nothosaurs and thalattosaurs. These fossils are used by paleontologists to help date and correlate rock layers from that time period. They provide important information about the environments and life forms of the Triassic era.
Icthyosaurs and plesiosaurs are both known from Triassic strata. Crinoids were common then, but their history spans more than just the Triassic. Coelophysis appeared in the middle of the Triassic. Phytosaurs and aetosaurs did not survive past the end of the Triassic. Lystrosaurus was a Triassic dicynodont, about the size of a sheep, which has been found on every continent (including Antarctica). Podocarps and other gymnosperms (plants) survived beyond the Triassic period.
Triassic Attack was created on 2010-11-27.
The Late Triassic epoch was a part of the Triassic period of the Mesozoic era. It was divided into, in chronological order, the Carnian, Norian, and Rhaetian ages.
No. Fruit trees first appeared during the Cretaceous, two periods after the Triassic. The only trees in the Triassic were conifers.
Friedrich Von Alberti named the Triassic Period in 1834
jurassic The Triassic was the earliest period of the Mesozoic, followed by the Jurassic then the Cretaceous. The Cretaceous was of the greatest duration.
The Triassic Period dates from 248 to 206 mya.
the differenses between triassic period and the jurassic period is that idk i will have to think about it.
The boundary between the Triassic and Jurassic periods, like the boundary between the Permian and Triassic periods, is marked by significant geological and biological changes, including mass extinctions and the emergence of new life forms. Both transitions signify major shifts in Earth's ecosystems, with the end of dominant species and the rise of new ones in response to environmental changes. Additionally, these boundaries are characterized by distinct rock layers and fossil records that indicate significant climatic and ecological transformations.