Imperial College London Featured PhD Programmes
Norwich Research Park Featured PhD Programmes
Engineering and Physical Sciences Research Council Featured PhD Programmes
University of Kent Featured PhD Programmes
Cardiff University Featured PhD Programmes

Up in smoke! Terrestrial carbon cycle feedbacks during warm climates

Project Description

Organic carbon preserved within sedimentary rocks (fossil OC) is a major carbon reservoir and plays a crucial role in the long-term evolution of atmospheric CO2 and O2, and thus global climate. The oxidation of fossil OC during uplift, exhumation and erosion has the potential to become an important source of CO2 to the atmosphere through positive climate feedbacks. However, the importance of fossil OC oxidation in future warm climates remains a major gap in our understanding.

One way to test the behaviour of the Earth in warmer-than-present climate states is to examine the geological record. The Paleocene/Eocene Thermal Maximum (PETM) is the most rapid warming event in recent geologic history and is an analog for future climate change [1]. Tantalizing evidence from this interval suggests that fossil OC oxidation may act as a positive feedback [2,3]. However, this has yet to be globally confirmed. The aim of this project is to use a multi-proxy approach to test whether warm climates are associated with enhanced erosion, mobilization and oxidation of fossil OC and to determine whether this mechanism might act as a large source of atmospheric CO2.

Funding Notes

You can apply for fully-funded studentships (stipend and fees) from INSPIRE if you:
Are a UK or EU national.
Have no restrictions on how long you can stay in the UK.
Have been 'ordinarily resident' in the UK for 3 years prior to the start of the project.

Please click View Website for more information on eligibility and how to apply


[1] Zachos, J.C. et al (2008) An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature, 451
[2] Carmichael, M.J., et al (2017) Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum. Global and Planetary Change, 157, pp.114-138.
[3] Lyons, Shelby L., et al. (2019) Palaeocene–Eocene thermal maximum prolonged by fossil carbon oxidation. Nature Geoscience. 12

How good is research at University of Southampton in Earth Systems and Environmental Sciences?

FTE Category A staff submitted: 68.62

Research output data provided by the Research Excellence Framework (REF)

Click here to see the results for all UK universities

Email Now

Insert previous message below for editing? 
You haven’t included a message. Providing a specific message means universities will take your enquiry more seriously and helps them provide the information you need.
Why not add a message here
* required field
Send a copy to me for my own records.

Your enquiry has been emailed successfully

FindAPhD. Copyright 2005-2019
All rights reserved.