Ocean biology helps regulate global climate by fixing atmospheric CO 2 and exporting it to deep waters as sinking detrital particles. New observations demonstrate that particle fragmentation is the principal factor controlling the depth to which these particles penetrate the ocean's interior, and hence how long the constituent carbon is sequestered from the atmosphere. The underlying cause is, however, poorly understood. We speculate that small, particle-associated copepods, which intercept and inadvertently break up sinking particles as they search for attached protistan prey, are the principle agents of fragmentation in the ocean. We explore this idea using a new marine ecosystem model. Results indicate that explicitly representing particle fragmentation by copepods in biogeochemical models offers a step change in our ability to understand the future evolution of biologically-mediated ocean carbon storage. Our findings highlight the need for improved understanding of the distribution, abundance, ecology and physiology of particle-associated copepods. K E Y W O R D S biological carbon pump, climate regulation, detritus, fragmentation, ocean carbon cycle, zooplankton 12 gigatonnes of this organic matter sinks down into the mesopelagic zone, [2] nominally defined as the region of water between 100 and 1000 m deep, as a mixture of dead or dying cells, animal carcasses This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. © The Authors. BioEssays published by Wiley Periodicals LLC and feces. Most of this sinking flux is remineralised via ocean biology before it reaches 1000 m. [3-5] The depth at which organic matter is remineralised determines the residence time of the constituent carbon in the ocean, with important consequences for global climate. [6] It is estimated that the suite of biological processes that result in the storage of carbon in the deep ocean, collectively known as the "biological carbon pump" (BCP), reduce the concentration of atmospheric CO 2 by up to 50% of what it would otherwise be. [7] Understanding the mechanisms that control the strength and efficiency of the BCP is integral to developing our capacity to reliably predict future climate.