I completed my PhD in Geology at Victoria University of Wellington, New Zealand, and in addition to several short research positions, held a New Zealand Science and Technology Post-Doctoral Fellowship for a project entitled “Antarctic vegetation shifts from Greenhouse to Icehouse”. Now back in the UK, I am currently, investigating the terrestrial and marine palynological signal from a shallow marine sedimentary sequence on Seymour Island, James Ross Basin, Antarctic Peninsula. The results will provide insight into palaeoclimate and sea level conditions in the region during the Maastrichtian in the lead-up to, and across, the K-T boundary.
email: V.C.Bowman@leeds.ac.uk
Fieldwork on Seymour Island, James Ross Basin, Antarctica, 2006