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Jean Guex

Researcher at University of Lausanne

Publications -  114
Citations -  4417

Jean Guex is an academic researcher from University of Lausanne. The author has contributed to research in topics: Extinction event & Ammonite. The author has an hindex of 35, co-authored 114 publications receiving 4063 citations. Previous affiliations of Jean Guex include Geological Survey of Canada.

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Correlating the end-Triassic mass extinction and flood basalt volcanism at the 100 ka level

TL;DR: In this paper, high-precision U/Pb geochronology from volcanic ashes was used to show that the Triassic-Juras-sic boundary and end-Triassic biological crisis from two independent marine stratigraphic sections correlate with the onset of terrestrial fl ood volcanism in the Central Atlantic Magmatic Province to <150 ka.
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Good genes and good luck: Ammonoid diversity and the end-permian mass extinction

TL;DR: Analysis of a global diversity data set of ammonoid genera covering about 106 million years centered on the Permian-Triassic boundary shows that Triassic ammonoids actually reached levels of diversity higher than in the PerMian less than 2 million years after the PTB.
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New Early to Middle Triassic U–Pb ages from South China: Calibration with ammonoid biochronozones and implications for the timing of the Triassic biotic recovery

TL;DR: In this article, new zircon U-Pb ages are proposed for late Early and Middle Triassic volcanic ash layers from the Luolou and Baifeng formations (northwestern Guangxi, South China).
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High-resolution ammonite and carbon isotope stratigraphy across the Triassic-Jurassic boundary at New York Canyon (Nevada)

TL;DR: In this article, high-resolution ammonite correlations and carbon isotope marine record in the New York Canyon area allow to distinguish two negative carbon excursions across this boundary with different paleoenvironmental meanings.
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Precise U–Pb age constraints for end-Triassic mass extinction, its correlation to volcanism and Hettangian post-extinction recovery

TL;DR: Geochim et al. as discussed by the authors used ID-TIMS dating of single chemical-abraded zircons from volcanic ash layers within the Pucara Group, Aramachay Formation in the Utcubamba valley, northern Peru.