@article{56, author = {B. Schoene and J. Guex and A. Bartolini and U. Schaltegger and T. Blackburn}, title = {Correlating the end-Triassic mass extinction and flood basalt volcanism at the 100 ka level}, abstract = {
New high-precision U/Pb geochronology from volcanic ashes shows that the Triassic-Jurassic boundary and end-Triassic biological crisis from two independent marine stratigraphic sections correlate with the onset of terrestrial flood volcanism in the Central Atlantic Magmatic Province to \<150 ka. This narrows the correlation between volcanism and mass extinction by an order of magnitude for any such catastrophe in Earth history. We also show that a concomitant drop and rise in sea level and negative δ13C spike in the very latest Triassic occurred locally in \<290 ka. Such rapid sea-level fluctuations on a global scale require that global cooling and glaciation were closely associated with the end-Triassic extinction and potentially driven by Central Atlantic Magmatic Province volcanism.
}, year = {2010}, journal = {Geology}, volume = {38}, pages = {387-390}, month = {05/2010}, isbn = {0091-7613}, url = {https://doi.org/10.1130/G30683.1}, doi = {10.1130/G30683.1}, language = {eng}, }