Marine Palynology and Paleoceanography

Studying climate and biota in past oceans to project the future

Modern oceans are subject to warming, acidification and decreasing oxygen concentrations due to human actions, which will likely have major effect on biology. We focus on the reconstruction of past ecosystems and climates based on the study of microfossils from ocean floor sediments, notably fossils of dinoflagellates, major components of the ocean’s phytoplankton. Our focus on time periods in the geological past that saw similar changes as today, enables us to use information from present and past oceans to elucidate how future oceans will change.

Research focus

Humans inject massive amounts of CO2 into the atmosphere, which causes warming of the atmosphere and oceans. Moreover, a large portion of the CO2 dissolves in ocean waters, resulting in acidification. Finally, the addition of nutrients to coastal oceans, as well as climate change ultimately leads to a reduction in oxygen content of subsurface ocean water. Warming, acidification and anoxia are major threats to life in future oceans.

Reconstructing past climate and ecology

Crucially, warming, acidification and anoxia are not unique to the present. Specific periods in the geological past offer the opportunity to evaluate the consequences. The Marine Palynology and Paleoceanography group therefore aims to reconstruct climate and marine ecology during such periods of global change.

Paleoecology of dinoflagellates

Our core business is the (paleo)ecology of dinoflagellates, single celled plankton with an enormous ecological variety. The organic dinocysts produced by many dinoflagellates preserve in ocean sediments. By palynological processing in the Laboratory of Palaeobotany and Palynology in the Geolab, these dinocysts can be isolated from sediments to be studied using microscopy. This way, the assemblages of dinoflagellates that once lived in the oceans can be reconstructed, leading to powerful insights into paleo-ecosystem functioning.

We combine palynology with geochemical techniques, notably the study of organic biomarkers in collaboration with the organic geochemistry group, and paleoclimate and carbon cycle modeling with colleagues in Utrecht and elsewehere. The ultimate aim is to understand variations in the state of System Earth, and particularly the role of the ocean, including its biology, physics, and chemistry on various temporal and spatial scales, in the past, present and future.

BSc thesis projects at the Royal NIOZ for students at Utrecht University

The Royal NIOZ provides ample opportunities for biology students at Utrecht University to carry out their BSc thesis project at their locations on Texel and in Yerseke. The collaboration between Utrecht University and the NIOZ also allows for funds for temporary housing close to those locations.

If you are interested in one of the below projects, you may apply to the project via the Google form: Application form BSc project at NIOZ. The application deadlines for the NIOZ projects for the coming 4 periods are as follows: 

  • November 24th for period 3 (Feb 2nd - Apr 17th, 2026)
  • February 9th for period 4 (Apr 20th - Jun 26th, 2026)
  • July 29th for period 1 (Sep 7th – Nov 13th, 2026)
  • September 7th for period 2 (Nov 16th – Feb 5th, 2026-2027)

Within 2 weeks after the deadline for your period has passed, you will be notified by the contact person of the project whether you will be moving forward with the project and of any next steps. 

As soon as a project is confirmed, you need to report this to Nora Azergui (n.azergui@uu.nl) with CC to Appy Sluijs (A.Sluijs@uu.nl), who will collect your requests. They will subsequently make sure there is a member of staff at Utrecht University that will be the examiner for your project. 

Below, the proposed projects are detailed per department at the NIOZ. For more information on these, see nioz.nl