New study pinpoints twin triggers of Triassic era extinction event

Curtin-led research has revealed an increase in levels of both acid and hydrogen sulfide in the ocean was the double whammy that wiped out marine life during a mass extinction event 201 million years ago. Lead author, Curtin PhD graduate Dr Calum Peter Fox, from the WA-Organic and Isotope Geochemistry Centre (WA-OIGC) in Curtin's School of Earth and Planetary Sciences, said the research revealed the twin processes that combined to the end the Triassic era, paving the way for the emergence of dinosaurs in the Jurassic period. "The end-Triassic event saw rapid increases in CO₂ due to a surge in volcanic activity, which is understood to have caused unfavourable conditions for life resulting in mass extinction, however the multiple drivers for loss of life during this period were not previously known," Dr Fox said. "By studying microscopic fossils preserved in rock in the Bristol Channel Basin, in the southwestern United Kingdom, we identified the twin mechanisms responsible for the mass extinction. "These were a deadly combination of ocean acidification, which inhibited growth of all marine life using calcium carbonate to create shells or body parts such as mussels, oysters, and corals, and rising levels of hydrogen sulfide in the ocean, which was extremely toxic for all marine life." Co-author John Curtin Distinguished Professor Kliti Grice, also from WA-OIGC in Curtin's School of Earth and Planetary Sciences, said the research provided intricate and important details of the history of our ever-evolving planet.