New approaches to image dynamic sinking behaviour in marine phytoplankton

The rate at which phytoplankton cells sink to the deep ocean plays a critical role in the global carbon cycle. Phytoplankton cells can actively control their orientation and buoyancy, indicating that biological processes play a major role in determining carbon export, although the factors controlling sinking rates remain poorly understood.

There are very few direct observations of sinking rates in individual phytoplankton cells, but new technologies allowing direct imaging of sinking phytoplankton cells are providing novel insight, demonstrating that sinking rates are highly dynamic and actively controlled. The ability to image these processes in single cells will provide unique insight into the biological processes that determine global carbon fluxes.

closing date for applications : 12 noon, Monday 08 January 2024