A new correlation of Triassic–Jurassic boundary successions in NW Europe, Nevada and Peru, and the Central Atlantic Magmatic Province: A time-line for the end-Triassic mass extinction

@article{Lindstrm2017ANC,
  title={A new correlation of Triassic–Jurassic boundary successions in NW Europe, Nevada and Peru, and the Central Atlantic Magmatic Province: A time-line for the end-Triassic mass extinction},
  author={Sofie Lindstr{\"o}m and Bas van de Schootbrugge and Katrine Hovedskov Hansen and Gunver K Pedersen and Peter Alsen and Nicolas Thibault and Karen Dybkj{\ae}r and Christian J. Bjerrum and Lars Henrik Nielsen},
  journal={Palaeogeography, Palaeoclimatology, Palaeoecology},
  year={2017},
  volume={478},
  pages={80-102}
}

End-Triassic Extinction in a Carbonate Platform From Western Tethys: A Comparison Between Extinction Trends and Geochemical Variations

The Triassic/Jurassic boundary section cropping out at Mt Sparagio in north-western Sicily (Italy) consists of a thick and continuous peritidal succession typical of a Tethyan carbonate platform. The

Volcanically-Induced Environmental and Floral Changes Across the Triassic-Jurassic (T-J) Transition

The End-Triassic Mass Extinction (ETME) saw the catastrophic loss of ca. 50% of marine genera temporally associated with emplacement of the Central Atlantic Magmatic Province (CAMP). However, the

Distal Processes and Effects of Multiple Late Triassic Terrestrial Bolide Impacts: Insights from the Norian Manicouagan Event, Northeastern Quebec, Canada

The Late Triassic (Carnian to Rhaetian Stages: ca. 237–201 Ma) has a long history of geological research, although controversy remains over the precise definition of key sub-unit boundaries,
...

References

SHOWING 1-10 OF 115 REFERENCES

A new chronology for the end-Triassic mass extinction

Synchrony of the Central Atlantic magmatic province and the Triassic-Jurassic boundary climatic and biotic crisis

The evolution of life on Earth is marked by catastrophic extinction events, one of which occurred ca. 200 Ma at the transition from the Triassic Period to the Jurassic Period (Tr-J boundary),

Sea-level change and facies development across potential Triassic–Jurassic boundary horizons, SW Britain

The Late Triassic to Early Jurassic aged succession of SW Britain (the Penarth and lower Lias Groups) comprises mudstone, sandstone and limestone strata deposited in a variety of marine to non-marine

A microbial carbonate response in synchrony with the end-Triassic mass extinction across the SW UK

Findings indicate microbialites from the SW UK capture a nonlocal biosedimentary response to the cascading effects of massive volcanism and add to the current understanding of paleoecology in the aftermath of the end-Triassic extinction.
...