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The Carnian Pluvial Episode (Late Triassic) was a time of global environmental changes and possibly substantial coeval volcanism. The extent of the biological turnover in marine and terrestrial ecosystems is not well understood.
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 the...
31 maj 2017 · Hence, variations in their isotopic composition unambiguously record past climate variability 19 (see supplementary information). δ 13 C wax values range from −25.7‰ to −34.3‰ and are ...
7 cze 2020 · The Late Triassic was a time of significant biotic upheaval, with the origination of new groups such as dinosaurs, lizards, crocodiles and mammals, but also characterized by a prolonged period of extinctions, distinguishing it from other great mass extinction events, while the gradual rise of the dinosaurs during the late Carnian to Norian ...
3 gru 2019 · Something strange happened in the Late Triassic — and not just in Somerset. About 232 million years ago, during a span known as the Carnian age, it rained almost everywhere.
20 paź 2017 · The Late Triassic mass extinction event (LTE), which occurred ~201.6 million years ago (Blackburn et al. 2013), is the second biggest biodiversity loss (Alroy 2010) and the third biggest ecological crisis (McGhee et al. 2004) since the Cambrian.
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