Looking to list your PhD opportunities? Log in here.
About the Project
Background
The Paleocene-Eocene Thermal Maximum (PETM) represents the largest climatic change of the Cenozoic and is regarded as a yardstick for future anthropogenic climate change. It is the most pronounced of several Paleogene hyperthermals – transient events of extreme warmth and massive atmospheric carbon addition. Rapid climatic changes throughout the PETM had major impact on biological evolution, for example the expansion of large benthic foraminifera, and on weathering and erosion. While feedbacks are understood qualitatively, there is only limited quantification of response times for depositional systems.
The Eocene Alveolina Limestone was deposited during orogenesis in the Spanish Pyrenees and provides a natural laboratory to study the effects of PETM-related faunal changes, uplift/subsidence and erosion patterns on sedimentation. Consequently, it provides a unique window into sedimentary dynamics on shelves, their response to external forcing, and how organisms interact with their changing environment.
Aims
The study aims to quantify physical and biological depositional processes, paleoclimatic constraints, and their combined effects on facies dynamics and shelf geometry during and after the PETM. It will combine detailed outcrop studies of depositional systems representing different biofacies and variable regimes of tectonic subsidence, and relative sea level to test sensitivity of carbonate depositional processes to external controls.
The project requires a student with background and interest in sedimentology and stratigraphy, including thin section petrography, as well as willingness to carry out field work in mountainous terrain. Knowledge in low-temperature geochemistry is advantageous.
Data
The database consists of limestone samples ready for processing. Field work will collect data and samples from outcrops representing a variety of depositional settings.
Methods
- petrography and geochemistry of basement and cements (bulk and veins; trace element, - field data acquisition, incl paleocurrents
- petrography (microfacies, point counting)
- biostratigraphy
- facies analysis
- geochemical analyses (XRD, XRF, isotopes)
To make an application please visit - https://www.ees.manchester.ac.uk/study/postgraduate-research/how-to-apply/
Please search and select PhD Earth Science (academic programme) and PhD Earth Science(academic plan)
Funding Notes
References
• Minelli, N., Manzi, V. and Roveri, M. 2013. The record of the Paleocene-Eocene thermal maximum in the Ager Basin (central Pyrenees, Spain). Geologica Acta 11, 421-441.
How good is research at The University of Manchester in Earth Systems and Environmental Sciences?
Research output data provided by the Research Excellence Framework (REF)
Click here to see the results for all UK universitiesEmail Now
Why not add a message here
The information you submit to The University of Manchester will only be used by them or their data partners to deal with your enquiry, according to their privacy notice. For more information on how we use and store your data, please read our privacy statement.

Search suggestions
Based on your current searches we recommend the following search filters.
Check out our other PhDs in Manchester, United Kingdom
Check out our other PhDs in United Kingdom
Start a New search with our database of over 4,000 PhDs

PhD suggestions
Based on your current search criteria we thought you might be interested in these.
Understanding the role of microorganisms in the formation of iron sulfides in the sedimentary record
The University of Manchester
Improved time-stepping schemes in weather and climate models
University of Reading
AI to the rescue of climate change, modelling air quality for cleaner urban planning
Anglia Ruskin University ARU