Ocean alkalinity destruction by anthropogenic seafloor disturbances generates a hidden CO2 emission

The seafloor is responsible for 40% of the alkalinity input to the ocean,
thus contributing to the ocean’s capacity to sequester atmospheric CO2.
Anthropogenic seafloor disturbances induced by mobile bottom-contact
fishing (e.g., trawling) and dredging influence this natural carbon sink,
yet the human impact on the ocean’s alkalinity cycle remains poorly
quantified. Model simulations show that the combined impact of mobile
bottom-contact fishing and dredging reduces natural alkalinity generation
by 60-220 Geq. yr-1, which is equivalent to a reduction of the natural
marine carbon sink by 2-8 Tg CO2 yr-1. Alkalinity destruction by
anthropogenic seafloor disturbance hence comprises a hidden CO2 emission,
of which the impact is comparable to the estimated inhibition of organic
carbon burial. Our analysis emphasizes that carbon accounting in marine
systems should consider the anthropogenic impact on both the organic and
inorganic carbon cycles.