We comment on the conjecture by Parker et al. (2016) that Antarctic
toothfish recently returned to McMurdo Sound, arguing that this species never
departed. Instead, as deduced from a 40-year fishing effort, toothfish water column
prevalence became markedly reduced where bottom depths are <500 m, with research
continuing to show their presence on the bottom or above the bottom where depths are
deeper. We also counter arguments that toothfish departed, and remained absent,
during and following a five-year presence of mega-icebergs residing near the opposite
coast of Ross Island, the icebergs inhibiting or fomenting conditions that
discouraged toothfish presence in the Sound. Available analyses reveal that toothfish
movement into the Sound was probably not significantly affected, and additionally
that neither changes in hydrography nor in primary productivity in the Sound would
have been sufficient to impact toothfish presence through food web alteration. We
hypothesize that the local effect of predation by seals and whales and the regional
effect of a fishery targeting the largest toothfish (those neutrally buoyant and thus
capable of occupying upper levels of the water column) has resulted in the remaining
toothfish now being found predominantly closer to the bottom at greater depths.