The Bristol-Russia PTB Programme 2004-2010 has the aim of dissecting the greatest mass extinction of all time, the Permo-Triassic boundary (PTB) event, which happened 252 million years ago. Through annual fieldwork in the redbeds of Late Permian and Early Triassic age, and analysis of palaeontological, sedimentological, and geochemical data, we seek to understand the environments before, during and after the mass extinction and how the plants and animals were wiped out and then recovered.
Read more about the PT event here.
Most studies of the PTB event have focused on marine sections from many parts of the world. We hope to determine what happened on land. Our key aims are to find out:
- How do the timings and patterns of extinction on land compare with those in the sea?
What were the global rates for loss of life on land, and how do these compare with the scale of the
- Were there two events, one earlier in the Late Permian and one at the PTB?
- In each case, were there associated climatic changes (in temperature, CO2 etc.), as indicated
by oxygen and carbon isotopes? Do the isotope curves match those from South Africa, and from
marine sections, thus implying a truly global scale change?
- What were the local environmental changes as indicated by sedimentology? Is there any change
in the distribution and type of paleosols? Is there any evidence for global warming (e.g. aridity,
desertification)? Is there any evidence for the proposed massive plant die-off and soil stripping
at the beginning of the Triassic?
- How did life on land respond to the two crises? What was the pattern of ecosystem collapse?
Is there evidence for ecological or taxonomic selectivity? How does the pattern in Russia compare
with South Africa?
- What was the nature and timing of the post-extinction recovery through the Early and Mid
Triassic, in terms of rebuilding total diversity and rebuilding ecosystems? How do the Russian
data compare to South Africa and the marine realm?
Press releases/ Media
- Newsletter 1 (May 2008) pdf