Monitoring mercury
(Hg) levels in biota is considered an important
objective for the effectiveness evaluation of the Minamata Convention.
While many studies have characterized Hg levels in organisms at multiple
spatiotemporal scales, concentration analyses alone often cannot provide
sufficient information on the Hg exposure sources and internal processes
occurring within biota. Here, we review the decadal scientific progress
of using Hg isotopes to understand internal processes that modify
the speciation, transport, and fate of Hg within biota. Mercury stable
isotopes have emerged as a powerful tool for assessing Hg sources
and biogeochemical processes in natural environments. A better understanding
of the tissue location and internal mechanisms leading to Hg isotope
change is key to assessing its use for biomonitoring. We synthesize
the current understanding and uncertainties of internal processes
leading to Hg isotope fractionation in a variety of biota, in a sequence
of better to less studied organisms (i.e., birds, marine mammals,
humans, fish, plankton, and invertebrates). This review discusses
the opportunities and challenges of using certain forms of biota
for Hg source monitoring and the need to further elucidate the physiological
mechanisms that control the accumulation, distribution, and toxicity
of Hg in biota by coupling new techniques with Hg stable isotopes.