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TitreDeep-sea record of impact apparently unrelated to mass extinction in the Late Triassic
AuteurOnoue, T; Sato, H; Nakamura, T; Noguchi, T; Hidaka, Y; Shirai, N; Ebihara, M; Osawa, T; Hatsukawa, Y; Toh, Y; Koizumi, M; Harada, H; Orchard, M J; Nedachi, M
SourceProceedings of the National Academy of Sciences of the United States of America vol. 109, no. 47, 2012 p. 19134-19139,
Séries alt.Secteur des sciences de la Terre, Contribution externe 20120388
Documentpublication en série
Mediapapier; en ligne; numérique
Sujetscratères météoriques; météorites; extinctions biotiques; biostratigraphie; paléontologie; géologie extraterrestre; Trias; Mésozoïque
Illustrationslocation maps; photomicrographs; plots
ProgrammeBassins sédimentaires du Yukon, GEM : La géocartographie de l'énergie et des minéraux
Résumé(disponible en anglais seulement)
The 34-million-year (My) interval of the Late Triassic is marked by the formation of several large impact structures on Earth. Late Triassic impact events have been considered a factor in biotic extinction events in the Late Triassic (e.g., end-Triassic extinction event), but this scenario remains controversial because of a lack of stratigraphic records of ejecta deposits. Here, we report evidence for an impact event (platinum group elements anomaly with nickel-rich magnetite and microspherules) from the middle Norian (Upper Triassic) deep-sea sediment in Japan. This includes anomalously high abundances of iridium, up to 41.5 parts per billion (ppb), in the ejecta deposit, which suggests that the iridium-enriched ejecta layers of the Late Triassic may be found on a global scale. The ejecta deposit is constrained by microfossils that suggest correlation with the 215.5-Mya, 100-km-wide Manicouagan impact crater in Canada. Our analysis of radiolarians shows no evidence of a mass extinction event across the impact event horizon, and no contemporaneous faunal turnover is seen in other marine planktons. However, such an event has been reported among marine faunas and terrestrial tetrapods and floras in North America. We, therefore, suggest that the Manicouagan impact triggered the extinction of terrestrial and marine organisms near the impact site but not within the pelagic marine realm.