The end-Triassic mass extinction is one of the five most catastrophic in Ph
anerozoic Earth history. Here we report carbon isotope evidence of a pronou
nced productivity collapse at the boundary, coincident with a sudden extinc
tion among marine plankton, from stratigraphic sections on the Queen Charlo
tte Islands, British Columbia, Canada. This signal is similar to (though sm
aller than) the carbon isotope excursions associated with the Permian-Trias
sic and Cretaceous-Tertiary events.