Peristiwa kepupusan Trias-Jura

Peristiwa kepupusan Trias-Jura menandakan sempadan antara tempoh Trias dan Jura, 201.3 juta tahun yang lalu,^[1] dan merupakan salah satu peristiwa kepupusan utama eon Fanerozoik, yang sangat mempengaruhi kehidupan di darat dan di lautan. Di lautan, seluruh kelas (conodont)^[2] dan 34% daripada genus laut pupus.^[3] Di darat, semua arkosaur selain daripada crocodylomorph ( Sphenosuchia dan Crocodyliformes ) dan Avematatarsalia ( pterosaur dan dinosaur ), beberapa terapsid tersisa, dan kebanyakan amfibia besar telah menjadi pupus.

^ Sesetengah sumber (Whiteside et al 2010) memberikan tarikh 201.4 Ma.
^ The extinction of conodonts —in terms of discrete elements— at the Triassic-Jurassic boundary
^ Graham Ryder; David E. Fastovsky; Stefan Gartner (1996). The Cretaceous-Tertiary Event and Other Catastrophes in Earth History. Geological Society of America. m/s. 19. ISBN 9780813723075.

[1] Sesetengah sumber (Whiteside et al 2010) memberikan tarikh 201.4 Ma.

[2] The extinction of conodonts —in terms of discrete elements— at the Triassic-Jurassic boundary

[3] Graham Ryder; David E. Fastovsky; Stefan Gartner (1996). The Cretaceous-Tertiary Event and Other Catastrophes in Earth History. Geological Society of America. m/s. 19. ISBN 9780813723075.

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Peristiwa kepupusan Trias-Jura

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