Director of Studies:
Dr Tracy Aze
2nd Supervisor:
Dr Christopher Smart
3rd Supervisor: Professor Sandra Piazolo, University of Leeds
4th Supervisor: Dr David Evans, University of Southampton
Applications are invited for a 3.5 years PhD studentship. The studentship will start on 1 October 2025
Project description
Planktonic foraminifera are single-celled marine protists that build calcium carbonate (calcite) shells, which are well-preserved in deep sea sediments. They have existed for ~150 million years, are found in all global oceans, and have one of the best species-level fossil records. Consequently, they are widely employed for palaeoenvironmental and biostratigraphic research and are increasingly becoming a model for macroevolutionary analysis.
Despite decades of research, the mechanisms by which planktonic foraminifera build their calcite shells remain elusive. This project will utilise Electron Back Scatter Diffraction (EBSD) and in-situ chemical analyses to investigate the shell wall at the microstructural level. The aim is to better understand how foraminifera biomineralisation occurs and how these structures vary between species. This research will not only enhance understanding of biomineralisation but also provide insights into how these processes have evolved. By linking microstructural features to environmental conditions and evolutionary history, it could improve palaeoenvironmental reconstructions and our understanding of macroevolutionary trends.
Research methodology
- Investigate microstructural differences in the biomineralisation processes of planktonic foraminifera with differing wall textures.
- Quantify changes in the microstructure of planktonic foraminifera with differing preservation histories and investigate the implications for alteration of trace metal geochemistry.
- Investigate the prevalence of calcite twinning throughout the evolutionary history of planktonic foraminifera and the implications for shell strength.
Training
The student will become an expert in foraminifera taxonomy and ecology and gain experience in various analytical techniques, such as Light Microscopy Z-stack image capture, Electron Back Scatter Diffraction, Time-of-flight Mass Spectrometry, Scanning Electron Microscopy, Fore Scatter Microscopy, and Electron Microprobe Analysis of trace element geochemistry.
Fig. 1 a) A scanning electron microscope (SEM) image of the planktonic foraminifera Globigernoides ruber
b) An SEM image of the cross-section of the shell of G. ruber
c) An EBSD map of the cross-section of the calcite shell of G. ruber showing the orientation of calcite mesocrystals (individually coloured units)
d) An Electron Microprobe Analysis (EMPA) of trace element geochemistry map of the cross-section of the calcite shell of G. ruber showing alternate colours representing banding of high and low magnesium calcite typically associated with primary biomineralisation.