The Triassic mass extinction, which occurred around 201 million years ago, is believed to have been caused by a combination of volcanic activity, climate change, and possibly asteroid impacts. The extensive volcanic eruptions in the Central Atlantic Magmatic Province released vast amounts of carbon dioxide, leading to global warming and ocean acidification. These environmental shifts drastically altered habitats, resulting in the extinction of a significant portion of marine and terrestrial species. This event ultimately paved the way for the rise of dinosaurs in the subsequent Jurassic period.
The mass extinction at the end of the Permian period, known as the Permian-Triassic extinction event, occurred around 252 million years ago. This event marked the transition from the Paleozoic Era to the Mesozoic Era, leading to the most significant loss of biodiversity in Earth's history, with approximately 90-96% of marine species and 70% of terrestrial vertebrate species going extinct. The aftermath of this extinction paved the way for the rise of the dinosaurs and other new life forms in the Triassic period.
The major extinction that preceded the Mesozoic era is called the Permian-Triassic extinction event, also known as the Great Dying. It occurred around 252 million years ago and is considered the most severe mass extinction event in Earth's history, wiping out approximately 96% of marine species and 70% of land species.
No evidence of the extinct lifeforms appears in the stratigraphic record immediately following the extinction event.
The Cretaceous–Tertiary extinction event 65 million years ago was the last mass-extinction, and many believe that humans are causing a mass-extinction right now.
the holocene extinction
Most extinctions occur as background extinctions because they are longer time periods unlike the shorter mass extinctions which there were only two in the Paleozoic era, the Ordovician mass extinction, and the Permian/Triassic extinction in which 95% of all marine animals became extinct
The three mass extinctions referred to are the Permian-Triassic extinction about 252 million years ago, the Triassic-Jurassic extinction about 201 million years ago, and the Cretaceous-Paleogene extinction about 66 million years ago.
The better Q is "What was the cause of the triassic mass-Extinction?"
The better Q is "What was the cause of the triassic mass-Extinction?"
There were five major extinction events in the past. They are called the Cretaceous-Tertiary (or K-T) extinction event, the late Devonian mass extinction, the Permian mass extinction, the Ordovician-Silurian mass extinction and the Triassic-Jurassic mass extinction event.
The most devastating mass extinction occurred in the Late Permian (~250 million years ago).
The Permian-Triassic mass extinction, aka "the Great Dying", the single most devastating mass extinction known.
Mass extinction could occur due to climate change, an asteroid impact and even a volcanic eruption.
The Permian-Triassic mass extinction, aka "the Great Dying", the single most devastating mass extinction known.
The Permian-Triassic (P-Tr) Extinction Event is widely recognised as the greatest extinction event on Earth. It is also known as the "Great Dieing".It occurred 251 million years ago marking the end of the Permian Period and the start of the Triassic Period.It also marks the end of the Paleozoic Era and the start of the Mesozoic Era. Estimates have suggested that 96% of marine species and 70% percent of land vertebrate species became extinct. It is also the only known mass extinction of insect with 56% of insect families and 83% of insect genera becoming extinct.Little is known of the cause of the mass extinction but theories range from meteorite impacts, to volcanism, to sea level fluctuations.
Extinction of a single species can occur at any time if said species in hunted excessively, but mass extinction only occurs every 27 to 33 million years.
They are the end-Ordovician extinction, end-Devonian extinction, end-Permian extinction, the Triassic extinction, end-Cretaceous extinction.