Understanding of the triggers and timing of the rise of complex life ~720-520 million years ago has expanded dramatically in recent years. This meeting will integrate diverse and novel geochemical and palaeontological data to create testable hypotheses for the differing roles of changing climate, oceanic redox, nutrient availability, and ecosystem feedbacks, across this profound, but enigmatic, transitional period.
More information on the programme and speakers will be available soon. Speaker abstracts will be available closer to the meeting. Recorded audio of the presentations will be available on this page after the meeting has taken place.
Attending this event
This meeting is intended for researchers in relevant fields.
- Free to attend
- Limited places, advance registration essential
- An optional lunch can be purchased during registration
Enquiries: contact the Scientific Programmes team