The marine biological carbon pump is driven by the interplay between particle sinking velocity and remineralisation. Despite its importance, sinking velocity of natural marine aggregates is not routinely measured, but often calculated from aggregate size and density using Stokes′ law. Yet, comparing calculated and experimentally measured sinking velocities has shown that Stokes′ law does not accurately predict the size-to-sinking relationship of marine aggregates because size-dependent changes in porosity are not sufficiently taken into account. To determine the factors controlling the sinking of marine aggregates and to establish a better scaling including a porosity term, we analysed the flow fields around 81 in situ collected aggregates using Particle Image Velocimetry. Additionally, we measured the size, sinking velocity, density and porosity of individual aggregates. The flow fields around the aggregates strongly resembled those of impermeable, porous spheres, independent of aggregate type, size, composition, and shape. Using an independently derived scaling of porosity with size, we could accurately predict the sinking velocity of laboratory- and field-collected aggregates with known density, which led to a 2-fold improvement in carbon flux predictions, compared to sinking velocity calculated with Stokes′ drag only. Furthermore, we found that small particles (<524 μm) account for a remarkable 80% of the total carbon flux in the sampling area. Using a comprehensive global in situ particle dataset, we demonstrate that this trend persists consistently across various oceans with small geographical variations, ranging from 40% in high latitudes to 70% in equatorial regions. It is established that small particles contribute disproportionately to carbon export fluxes because of their high numerical abundances. Here, we provide an additional explanation, which is that their importance can primarily be attributed to their relatively low porosities and high carbon-to-volume ratio.