<p>Sala,
et al. <sup>1</sup> suggest that seafloor disturbance by
industrial trawlers and dredgers results in 0.58 to 1.47 Pg of aqueous CO<sub>2</sub>
emissions annually, owing to increased organic carbon mineralisation in
sediments after trawling. We agree that bottom trawling disrupts natural
carbon flows in seabed
ecosystems due to sediment disturbance, resuspension and changes in the
biological community and that it is important to estimate the magnitude of this
effect. We disagree however that their assessment represents a ‘best estimate’.
Firstly, they critically assume that organic carbon in undisturbed
sediment is inert, and that only disturbance by trawling remineralises organic
carbon, an assumption at odds with decades of geochemical research. Secondly,
they greatly overestimate the volume of sediment where carbon is mineralised after
trawling. Thirdly, they ignore secondary effects, such as the removal of
bioturbating benthic fauna and sedimentary nutrient release, which could lead
to more preservation and production of organic carbon. Together these issues result in an upward bias in the estimated CO<sub>2</sub>
emissions by one or more orders of magnitude. </p><p><br></p><p>1. Sala, E.<i> et al.</i> Protecting the global ocean for biodiversity,
food and climate. <i>Nature</i>,
doi:10.1038/s41586-021-03371-z (2021).<br></p>