Dr Tracy Aze, Museum Research Fellow
Phone: +44 (0)1865 272964
My research is at the interface of palaeobiology and palaeoclimatology. Using the marine plankton fossil record I investigate evolutionary trends, the interactions between species and the response of organisms to environmental change. My current research is focused upon determining the factors that influence extinction risk during the Cenozoic (65 million years to the present day) to determine whether there are species or ecosystems that are more vulnerable to extinction in the face of rapid environmental change.
- BSc Geological Sciences (Hons) (University of Plymouth, 2005)
- MRes Global Environmental Change (University of Plymouth, 2007)
- PhD Cope’s rule and macroevolution of Cenozoic macroperforate planktonic foraminifera (Cardiff University, 2011)
Aze, T., Pearson, P. N., Dickson A. J., Badger, M. P. S., Bown, P. R., Pancost, R. D., Gibbs, S. J., Huber, B. T., Leng, M. J., Coe, A. L., Cohen, A. S. & Foster, G. L. Extreme warming of tropical waters during the Paleocene – Eocene Thermal Maximum. Geology (In Review)
Aze, T., Ezard, T. H. G., Purvis, A., Coxall, H. K. C., Stewart, D., Wade, B. S. & Pearson, P. N. (2013). Identifying anagenesis and cladogenesis in the fossil record. Proceedings of the National Academy of Sciences. doi: 10.1073/pnas.1307562110.
Tropical planktonic foraminifera
Aze, T., Ezard, T. H. G., Purvis, A., Coxall, H. K. C., Stewart, D., Wade, B. S. & Pearson, P. N. (2011). A phylogeny of Cenozoic macroperforate planktonic foraminifera from fossil data. Biological Reviews 86, 900-927.
Ezard, T. H. G., Aze, T., Pearson, P. N. & Purvis, A. (2011). Interplay between changing climate and species’ ecology drives macroevolutionary dynamics. Science 332, 349-351.
Ezard, T. H. G., Pearson, P. N. Aze, T., & Purvis, A. (2011). The Meaning of Birth and Death (in Macroevolutionary Birth-death models). Biology Letters 8, 139-142.
Etienne, R. S., Haegeman, B., Aze, T., Pearson, P. N., Purvis, A. & Phillimore, A. B. (2011) Diversity-dependence brings molecular phylogenies closer to agreement with the fossil record. Proceedings of the Royal Society, Series B: Biological Sciences 279, 1300-1309.
Hart, M.B., Aze, T., Hudson, W. & Smart, C.W. (2007). Planktic foraminifera from the proposed GSSP for the Oxfordian Stage: Redcliff Point, near Weymouth. Geoscience in south-west England 11, 273-279.