Recent
studies suggest size-selective removal of small plastic
particles from the ocean surface, an observation that remains unexplained.
We studied one of the hypotheses regarding this size-selective removal:
the formation of a biofilm on the microplastics (biofouling). We developed
the first theoretical model that is capable of simulating the effect
of biofouling on the fate of microplastic. The model is based on settling,
biofilm growth, and ocean depth profiles for light, water density,
temperature, salinity, and viscosity. Using realistic parameters,
the model simulates the vertical transport of small microplastic particles
over time, and predicts that the particles either float, sink to the
ocean floor, or oscillate vertically, depending on the size and density
of the particle. The predicted size-dependent vertical movement of
microplastic particles results in a maximum concentration at intermediate
depths. Consequently, relatively low abundances of small particles
are predicted at the ocean surface, while at the same time these small
particles may never reach the ocean floor. Our results hint at the
fate of “lost” plastic in the ocean, and provide a start
for predicting risks of exposure to microplastics for potentially
vulnerable species living at these depths.