Greg Price, Rhodri Jerrett and Lauren O’Connor conducting fieldwork at West Bijou
Tyler Lyson
Professor Gregory Price with colleagues Rhodri Jerrett and Lauren O’Connor during fieldwork in the United States
The extinction of the dinosaurs 66 million years ago came during a tumultuous time in Earth’s history, with some of the largest known volcanic eruptions and a 10-15km wide asteroid crashing into the planet.
The role these events played in the dinosaurs’ fate has been fiercely debated over several decades, but new research published in the journal Science Advances suggests the asteroid impact was the primary driver of the end-Cretaceous mass extinction.
A research team, including scientists from the University of Plymouth, analysed samples of ancient peats collected during fieldwork in Colorado and North Dakota.
This enabled them to reconstruct the mean annual air temperatures in the 100,000 years leading up to the extinction, which revealed that volcanic CO₂ emissions caused a slow warming of about 3°C across this period.
There was also a short cold “snap” — a cooling of about 5°C — that coincided with a major volcanic eruption 30,000 years before the extinction event that was likely due to volcanic sulphur emissions blocking out sunlight.
However, the temperatures returned to stable pre-cooling temperatures around 20,000 years before the mass extinction of dinosaurs, suggesting the climate disruptions from the volcanic eruptions weren’t catastrophic enough to kill off the dinosaurs.
The findings are the result of the Equable Earth project, funded by a grant of over £580,000 from the Natural Environment Research Council, and involving researchers from the University of Manchester, University of Plymouth, Utrecht University in the Netherlands, and Denver Museum of Nature and Science in the USA.

For this study, we joined our colleagues on fieldwork in the western United States, and samples from that work were then analysed in our labs here in Plymouth. Our data provides direct evidence for the effects on climate of the volcanic release of CO2, something the planet continues to experience to this day. However, while it may have had deadly consequences for life on Earth, we do not believe that would have been catastrophic enough to kill off the dinosaurs

Gregory PriceProfessor Gregory Price
Professor of Earth Sciences

The fossil peats that the researchers analysed contain specialised cell-membrane molecules produced by bacteria. The structure of these molecules changes depending on the temperature of their environment.
By analysing the composition of these molecules preserved in ancient sediments, scientists can estimate past temperatures and, in this study, were able to create a detailed ‘temperature timeline for the years leading up to the dinosaur extinction.
The research team is now applying the same approach to reconstruct past climate at other critical periods in Earth’s history.
Dr Lauren O’Connor, lead author on the study and now a Research Fellow at Utrecht University, said:
“These volcanic eruptions and associated CO2 emissions drove warming across the globe and the sulphur would have had drastic consequences for life on earth. But these events happened millennia before the extinction of the dinosaurs, and probably played only a small part in the extinction of dinosaurs.”
Dr Rhodri Jerrett, Senior Lecturer in Earth Science at The University of Manchester, added:
“By comparison, the impact from the asteroid unleashed a chain of disasters, including wildfires, earthquakes, tsunamis, and an ‘impact winter’ that blocked sunlight and devastated ecosystems. We believe the asteroid that ultimately delivered the fatal blow.”
  • The full study - O'Connor et al: Terrestrial evidence for volcanogenic sulfate-driven cooling event ~30 ka before the Cretaceous–Paleogene mass extinction - is published in Science Advances, DOI: 10.1126/sciadv.ado5478.
 
Group
photo taken on the banks of the Mackenzie River