Algal
blooms bring massive amounts of algal organic matter (AOM)
into eutrophic lakes, which influences microbial methylmercury (MeHg)
production. However, because of the complexity of AOM and its dynamic
changes during algal decomposition, the relationship between AOM and
microbial Hg methylators remains poorly understood, which hinders
predicting MeHg production and its bioaccumulation in eutrophic shallow
lakes. To address that, we explored the impacts of AOM on microbial
Hg methylators and MeHg production by characterizing dissolved organic
matter with Fourier transform ion cyclotron resonance mass spectrometry
(FTICR-MS) and three-dimensional excitation-emission matrix (3D-EEM)
fluorescence spectroscopy and quantifying the microbial Hg methylation
gene hgcA. We first reveal that the predominance
of methanogens, facilitated by eutrophication-induced carbon input,
could drive MeHg production in lake water. Specifically, bioavailable
components of AOM (i.e., CHONs such as aromatic proteins
and soluble microbial byproduct-like materials) increased the abundances
(Archaea-hgcA gene: 438–2240% higher) and
activities (net CH4 production: 16.0–44.4% higher)
of Archaea (e.g., methanogens). These in turn led
to enhanced dissolved MeHg levels (24.3–15,918% higher) for
three major eutrophic shallow lakes in China. Nevertheless, our model
results indicate that AOM-facilitated MeHg production could be offset
by AOM-induced MeHg biodilution under eutrophication. Our study would
help reduce uncertainties in predicting MeHg production, providing
a basis for mitigating the MeHg risk in eutrophic lakes.