Group
Members

"The present is the key to the past"

Uniformitarianism; James Hutton

..can the past also be the key to the future?

Matthew Pound (Ph.D. Student)

Land Cover in a Warmer World: Reconstructing Late Miocene Vegetation


The Late Miocene (11.6-5.33Ma) is considered a recent warm period in Earth History. This makes it a suitable 'test-bed' for global circulation models. To examine the models using Earth history a proxy for climate is required. The fossilised remains of vegetation provides such a proxy. By collating a large amount of palaeobotanical sites, in a manner consistent with the models, it will be possible to make an advanced vegetation reconstruction.

email: eemjp@leeds.ac.uk

web: http://homepages.see.leeds.ac.uk/~eemjp/index.html


SGPC University of Leeds British Geological Survey PRISM BRIDGE UK Polar Network Leicester University NCAS Antarctic Climate Evolution PMIP2 Met Office