The Utrecht Department of Earth Sciences, group ‘Stratigraphy and Paleontology’, is looking for a highly motivated and versatile PhD candidate with a MSc background in Earth Sciences, Environmental sciences, Biology, Climate physics, Oceanography or other appropriate fields.
Your jobYou will work on the project called
“Eemian sea level”. In this 4-year fully funded position, you will combine 2 toolsets: generating proxy data reflecting surface ocean changes, and simulations of sea level changes using comprehensive ice sheet models.
The sea level in the Eemian was much higher than today, 3 to 6 m or even higher. The high sea levels during the Eemian cannot be explained by a complete melting of the Greenland ice sheet, as large parts of it survived the Eemian stage. This implies that the Antarctic ice sheet was also very vulnerable to melting during this period, but little model studies are done on the Antarctic contribution. The aim of this research project is to further investigate the timing of major sea level changes, and thus the contribution of the Greenland and Antarctic ice sheets during the Eemian by generating high-resolution proxy records from the Dutch subsurface, including the type locality of the Eemian near the city of Amersfoort. Special emphasis will be on the varying background conditions between the Saalian to Eemian transition (i.e., termination II), when large ice sheets formed the Dutch coastline and the adjacent North Sea, and that of the LGM-Holocene transition (i.e., termination I), when large ice caps lay further north. The comparison between these new datasets and experiments with ice sheet models could lead to a better long-term projection of the Greenland and Antarctic ice sheets in our warming world.
The project is highly multidisciplinary and collaborative. Proxy data will amongst others infer the stable isotope composition of foraminifera and mollusc shells, since not much is known about the changes in temperature and isotopic composition of the waters flooding the Netherlands and other parts of Northwest Europe during past interglacial periods, such as the Eemian. The study is expected to shed new light upon (1) the timing and possible cause of rapid sea level changes during the Eemian, and (2) the complex interactions between global warming, sea level changes, glacial rebound and sediment transport on a more regional scale.
The position is part of the
Earth System Feedback Research Centre (EMBRACER), which focuses on the carbon and water cycle feedbacks within the climate system. EMBRACER includes 23 principal scientists from a wide variety of disciplines, from physics, environmental, earth and social sciences in the Netherlands. The EMBRACER community of students and staff will have regular cross-disciplinary meetings, events and lots of opportunities to get in contact with the wide spectrum of climate science. The project will also have close links with
Past to Future (P2F), a 4-year Horizon Europe research project which was launched in March 2025, consisting of 24 partners from a wide-range of disciplines in future climate model development, paleo-climate data collection, and applied mathematics.