The asynchronous disappearance of conodonts: New constraints from Triassic-Jurassic boundary sections in the Tethys and Panthalassa

@article{Du2020TheAD,
  title={The asynchronous disappearance of conodonts: New constraints from Triassic-Jurassic boundary sections in the Tethys and Panthalassa},
  author={Yixing Du and Marco Chiari and Viktor Kar{\'a}di and Alda Nicora and Tetsuji Onoue and J{\'o}zsef P{\'a}lfy and Guido Roghi and Yuki Tomimatsu and Manuel Rigo},
  journal={Earth-Science Reviews},
  year={2020},
  volume={203},
  pages={103176}
}
Abstract The End-Triassic Extinction event (ETE) has been recognized in numerous sections worldwide and it is usually marked by three negative carbon isotope excursions (NCIEs), named “precursor” (P-NCIE), “initial” (I-NCIE) and “main” (M-NCIE) negative carbon isotope excursions. These three NCIEs are significant characteristics of this time interval, and they are likely related to the emplacement of the Central Atlantic Magmatic Province (CAMP) that is considered the main trigger of the ETE… 
The Late Triassic Extinction at the Norian/Rhaetian boundary: Biotic evidence and geochemical signature
Abstract The latest Triassic was an interval of prolonged biotic extinction culminating in the end-Triassic Extinction (ETE). The ETE is now associated with a perturbation of the global carbon cycle
A review of the Late Triassic conodont conundrum: survival beyond biotic perturbations
  • D. Ruban
  • Palaeobiodiversity and Palaeoenvironments
  • 2021
Significant advance in the understanding of the Late Triassic evolution of conodonts and their final disappearance has been made recently. However, the relevant information is rather fragmented and
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Abstract The Norian and Rhaetian transition (Late Triassic) is characterized by a faunal turnover in major pelagic groups, such as radiolarians, conodonts, and ammonoids. Although catastrophic events
Sauropodomorph evolution across the Triassic–Jurassic boundary: body size, locomotion, and their influence on morphological disparity
TLDR
Modifications in the locomotion and the successive increase in body mass seem to be the main attributes driving sauropodomorph morphospace distribution during the Late Triassic and earliest Jurassic.
Tracing volcanic emissions from the Central Atlantic Magmatic Province in the sedimentary record
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During their last phase of evolution, the pectiniform conodont elements manifested an evident trend of simplification and miniaturization. This phase started from the late Norian (Sevatian) in the

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