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Abstract N⁶-adenine methylation occurs in both DNA and RNA (referred to as 6mA and m6A, respectively). As an extensively characterized epi-transcriptomic mark found in virtually all eukaryotes, m6A in mRNA is deposited by METTL3-METTL14 complex. As a transcription-associated epigenetic mark abundantly present in many unicellular eukaryotes, 6mA is coordinately maintained by two AMT1 complexes, distinguished by their mutually exclusive subunits, AMT6 and AMT7. These are all members of MT-A70 family methyltransferases (MTases). Despite their functional importance, no structure for holo-complexes with cognate DNA/RNA substrate has been resolved. Here, we employ AlphaFold3 (AF3) and molecular dynamics (MD) simulations for structural modeling ofTetrahymenaAMT1 complexes, with emphasis on ternary holo-complexes with double-stranded DNA (dsDNA) substrate and cofactor. Key structural features observed in these models are validated by mutagenesis and various other biophysical and biochemical approaches. Our analysis reveals the structural basis for DNA substrate recognition, base flipping, and catalysis in the prototypical eukaryotic DNA 6mA-MTase. It also allows us to delineate the reaction pathway for processive DNA methylation involving translocation of the closed form AMT1 complex along dsDNA. As the active site is highly conserved across MT-A70 family of eukaryotic 6mA/m6A-MTases, the structural insight will facilitate rational design of small molecule inhibitors, especially for METTL3-METTL14, a promising target in cancer therapeutics. 

Cold seeps and hydrothermal vents are seafloor habitats fueled by subsurface energy sources. Both habitat types coexist in Guaymas Basin in the Gulf of California, providing an opportunity to compare microbial communities with distinct physiologies adapted to different thermal regimes. Hydrothermally active sites in the southern Guaymas Basin axial valley, and cold seep sites at Octopus Mound, a carbonate mound with abundant methanotrophic cold seep fauna at the Central Seep location on the northern off-axis flanking regions, show consistent geochemical and microbial differences between hot, temperate, cold seep, and background sites. The changing microbial actors include autotrophic and heterotrophic bacterial and archaeal lineages that catalyze sulfur, nitrogen, and methane cycling, organic matter degradation, and hydrocarbon oxidation. Thermal, biogeochemical, and microbiological characteristics of the sampling locations indicate that sediment thermal regime and seep-derived or hydrothermal energy sources structure the microbial communities at the sediment surface.