The Department of Earth Sciences is looking for a highly motivated PhD candidate with an MSc background in Earth Sciences, Marine Sciences or other appropriate field. You will work on the project ‘Coupling biological pump changes to variations in the Atlantic Meridional Overturning Circulation (AMOC) during rapid climate transitions’.
Your jobThe AMOC transports warm saline waters from the tropics to the high northern latitudes of the North Atlantic where they cool and sink. This part of the density-driven global “conveyor belt” may be losing its strength due to ongoing global warming, with potential large-scale climate repercussions. Even more so since the AMOC brings CO2 from the surface to the deep ocean during deepwater formation (physical pump), and variations in the AMOC strength will change the ability of the ocean to absorb CO2. The magnitude of this impact and the processes involved remain however difficult to predict. Also in the past, the strength of the AMOC varied and abrupt shifts between cold and warm periods have been recorded in marine sediments on geological timescales. The North Atlantic Ocean is also a key region for carbon sequestration by the biological carbon pump. Hence, the transfer of both organic carbon and inorganic carbon from the surface to the deep ocean is locally promoted. The aim of the project is to investigate interaction between changes in the AMOC and the physical and biological pumps during rapid climate transitions (e.g., the last glacial period and Holocene) using sediment records. Our data will be used in marine carbon cycle models to predict (future) carbon sequestration upon changes in the AMOC strength.
During this four-year PhD project, you will apply a multiproxy (biogeochemical and micropaleontological/palynological) approach to sediment records from selected locations in the North Atlantic collected along a present-day temperature and salinity latitudinal transect. You will reconstruct surface and deep-water temperatures and salinity, and the (efficiency) of the organic and inorganic biological carbon pump via proxies indicative of primary productivity, CO2/pH in a surface deep-water gradient at times of known major past climate shifts and AMOC changes at decadal to millennial timescales. This project may include participation in seagoing expeditions.
This project is part of the 10-year
EMBRACER research programme funded by the Dutch Research Council (NWO). At EMBRACER, we work at the very frontiers of knowledge on climate change, earth’s climate system and climate feedbacks. The programme brings together a wide range of world-leading climate experts with the aim to address existing uncertainties about climate feedbacks at the boundaries between oceans, land, ice, and atmosphere. Our interdisciplinary approach and state-of-the-art infrastructure will bring us forward in our understanding of the impact of climate feedbacks emerging over the next decades to centuries.
A personalised training programme will be set up, reflecting your training needs and career objectives. About 20% of your time will be dedicated to this training component, which includes following courses/workshops as well as training on the job in assisting in the Bachelor’s and Master’s programmes of the department at Utrecht University.
The project leader and daily supervisor will be
Dr Francesca Sangiorgi and close collaboration in the project will be with
Prof. Gert-Jan Reichart Dr Martin Ziegler, and
Dr Lennart de Nooijer. Multiple others will be involved for specific aspects of the project. Foreseeable international collaborators include Profs.
Stijn de Schepper and
Ulysses Ninnemann (University of Bergen, Norway).