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  1. 24 wrz 2024 · Permian extinction, a series of extinction pulses that contributed to the greatest mass extinction in Earth’s history. Many geologists and paleontologists contend that the Permian extinction occurred over the course of 15 million years during the latter part of the Permian Period (299 million to 252 million years ago).

  2. science.nasa.gov › science-research › earth-scienceThe Great Dying - NASA Science

    27 sty 2002 · Whatever happened during the Permian-Triassic period was much worse: No class of life was spared from the devastation. Trees, plants, lizards, proto-mammals, insects, fish, mollusks, and microbes -- all were nearly wiped out. Roughly 9 in 10 marine species and 7 in 10 land species vanished.

  3. Of the five mass extinction events on Earth, the one 252 million years ago during the Permian Period was the most devastating. The Permian mass extinction, or “Great Dying,” killed 9 out of every 10 species on the planet and its effects are still seen today.

  4. Approximately 251.9 million years ago, the Permian–Triassic (P–T, P–Tr) extinction event (PTME; also known as the Late Permian extinction event, [3] the Latest Permian extinction event, [4] the End-Permian extinction event, [5] [6] and colloquially as the Great Dying) [7] [8] forms the boundary between the Permian and Triassic geologic ...

  5. 15 paź 2024 · About 250 million years ago, at the end of the Permian period, something killed some 90 percent of the planet's species. Less than five percent of the animal species in the seas survived. On land less than a third of the large animal species made it. Nearly all the trees died.

  6. About 250 million years ago, at the end of the Permian period, something killed some 90 percent of the planet's species. Less than 5 percent of the animal species in the seas survived.

  7. 28 lip 2020 · The End-Permian Mass Extinction (EPME) (also known as Permian–Triassic Mass Extinction, PTME) is one of the most studied geobiological events of the past. It is the most severe mass extinction of all life—“the mother of all extinctions”—and promoted the evolution of modern ecosystems (e.g., Raup and Sepkoski 1982 ; Erwin 1993 , 2006 ).

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