Paleocene-Eocene Thermal Maximum (PETM)
This project investigates the response of organisms to the Paleocene-Eocene Thermal Maximum (PETM), the most rapid and significant climatic warming pulse of the past 65 million years.
We are studying molluscs and cartilaginous 0D90 fish (sharks and rays) from extensive fossil deposits in north-west Europe to answer these questions:
- Did patterns of extinction and evolution change?
- Did overall levels of biodiversity change, and if so, over what interval of time?
- What was the effect of the PETM on the ecology and structure of shallow marine communities?
Coastal ecosystems around the world are increasingly fragile and ecologically degraded, but many communities rely on them for a wide range of ecosystem services. We hope that documenting the response of organisms to the PETM will help us to predict the result of current global warming in these habitats.
The PETM occurred around 55.8 million years ago. Global temperatures rose by 6°C, leading to an increase in atmospheric CO2 levels comparable to the rate of current anthropogenic warming.
Some organisms were unable to adapt to rapidly changing environmental conditions and became extinct. These included:
- bottom-dwelling deep-sea organisms
- open-ocean plankton
- terrestrial mammals
Little is known about the response of shallow-water marine organisms to the PETM and how coastal ecosystems themselves may have changed.
Using our collections to reveal the responses of organisms to environmental change.
Investigating the influence of food and temperature on body size change in ice-age mammals.
Studying chironomid and diatom assemblages to identify the drivers of climate change.