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6 lip 2024 · Similar scenarios occurred during the late Sevatian (late Norian, Late Triassic) and across the Norian-Rhaetian boundary (NRB), during which significant biotic extinctions of important...
31 maj 2017 · In the Carnian (Late Triassic), evidence from sedimentology and fossil pollen points to a significant change in climate, resulting in biotic turnover, during a time termed the ‘Carnian Pluvial...
Download book EPUB. Overview. Editors: Lawrence H. Tanner. Presents a comprehensive review of the latest science in the geological and paleontological aspects of Earth during the Late Triassic period. Covers the records of land-based life and marine life during the Late Triassic, as well as extinctions.
1 mar 2004 · Accelerated biotic turnover during the Late Triassic has led to the perception of an end-Triassic mass extinction event, now regarded as one of the “big five” extinctions.
31 maj 2017 · The end-Triassic extinction is one of the Phanerozoic’s largest mass extinctions. This extinction is typically attributed to climate change associated with degassing of basalt flows from...
19 lis 2016 · The Late Triassic extinction event is recognized as one of the five largest such events of the Phanerozoic and is now generally believed to have been caused by global warming and concomitant environmental changes triggered by emplacement of the Central Atlantic Magmatic Province.
Late Triassic, one during the Carnian, now dated at 237 to 227 million years ago, and the second at the Triassic-Jurassic boundary. In 1989, Simms and Ruffell identified increased humidity during the Late Triassic as a pluvial episode, also known as the Carnian Pluvial Event and ‘Triassic Wet Intermezzo’. The latter term has a
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