Active diffusion enhances plankton carbon capture and phycosphere radius

Plankton fix about 40 gigatons of carbon annually, using photosynthesis to convert $\text{CO}_2$ into $\text{O}_2$ and carbohydrates.

These solutes are exchanged with the ocean in a diffusive boundary layer around the organism called the phycosphere.

Here, we study how organisms can increase their carbon influx and outflux by actively mixing the surrounding fluid.

By developing exact analytical expressions validated by stochastic simulations, we determine the enhanced diffusivity of phycosphere particles as a function of mixing activity, and their resulting fluxes and concentration fields.

Hence, we find that plankton can significantly increase their uptake and photosynthetic turnover.

Moreover, we find that the phycosphere radius is enlarged both by increased metabolism and by increased diffusive transport further from the organism.

These results provide new biophysical insights into marine microbial ecology, with important implications for global carbon capture and climate change.