Marine biogeochemical cycling of mercury.

By W. Fitzgerald, C. Lamborg, C. R. Hammerschmidt. Chemical Reviews, 2007

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Enhanced bioaccumulation of mercury in deep-sea fauna from the Bay of Biscay (north-east Atlantic) in relation to trophic positions identified by analysis of carbon and nitrogen stable isotopes (2012, positive): “This last organic form of Hg is finally the most stable form, the most bioavailable and thus more bioaccumulated by marine organisms (Fitzgerald et al., 2007).”
A review of global environmental mercury processes in response to human and natural perturbations: Changes of emissions, climate, and land use (2018, background): “Fitzgerald et al. (2007) suggested that most marine MeHg is produced in ocean margin sed- iments, but a variety of studies across most major ocean basins have since produced strong evidence for water column MeHg production (Cossa et al. 2009; Sunderland et al. 2009; Heimbürger et al. 2010; Cossa…”