Meromictic Lake Cadagno, with its permanent stratification and persistent microbial bloom within the anoxic chemocline, serves as an ancient ocean analogue. Although the lake has been studied for over 25 years, the absence of simultaneous study of the bacteria, phytoplankton, and viruses, together with primary and secondary productivity, has hindered a comprehensive understanding of its microbial food web. This study evaluated the identities, abundances, and productivity of microbes in the context of nutrient biogeochemical cycling across the stratified depths of Lake Cadagno. Photosynthetic pigments and chloroplast 16S rRNA gene phylogenies suggested high abundances of eukaryotic phytoplankton, primarily Chlorophyta, through the water column. Of these, a close relative of Ankyra judayi, a high-alpine adapted chlorophyte, peaked with oxygen in the mixolimnion, while Closteriopsis-related chlorophytes peaked in the chemocline and monimolimnion. Chromatium, a genus of anoxygenic phototrophic sulfur bacteria, dominated the chemocline along with Lentimicrobium, a genus of known fermenters whose abundance was newly reported in Lake Cadagno. Secondary production peaked in the chemocline, suggesting anoxygenic primary producers depended on heterotrophic nutrient remineralization. Virus-to-microbe ratios (VMR) peaked in the zone of high phytoplankton abundances, yet were at a minimum at the peak of Chromatium, dynamic trends that suggest viruses may play a role in the modulation of oxygenic and anoxygenic photo- and chemosynthesis in Lake Cadagno. Through the combined analysis of bacterial, eukaryotic, viral, and biogeochemical dynamics of Lake Cadagno, this study provides a new perspective on the biological and geochemical connections that comprised the food webs of the Proterozoic ocean.