Microbial Communities in Mesopelagic Fish Guts Suggest an Overlooked Component of Marine Biogeochemical Cycles

Each night, gigatons of oceanic midwater fishes participate in the largest vertical migration on Earth. This movement of organisms from the meso- to the epipelagic and back plays a major role in the flux of organic matter from the surface to the deep sea (the biological pump). To date studies have considered the role of fish exports in ocean biogeochemical cycles, but mesopelagic fish gut microbiomes are unquantified and likely play a role in metabolic transformations that influence these cycles. Here, we present data on the abundance of mesopelagic fish gut microbial communities and their functional potential to shape key chemical transformations. Our flow cytometric data from a diversity of taxa reveal that the density of microbes in mesopelagic fish guts is between 106-107 microbes ml-1: two to three orders of magnitude higher than the surrounding seawater. In light of the total estimated number of mesopelagic fishes, there are approximately 2.4x1020 -1.34x1024 gut prokaryotes in total, which without consideration of other biomass abundant animals is realistically within four orders of magnitude of the total prokaryote abundance in mesopelagic waters. Metagenomic analyses revealed distinct bacterial genotypes of the genera Acinetobacter and Psychrobacter that harbor extensive gene sets for synthesis of essential amino acids, cofactor and vitamins, and short-chain-fatty acids (SCFAs), as well as cellulose and chitin degradation. Given their abundance, mesopelagic fish gut microbiomes are likely playing a role in shaping the nitrogen and carbon cycles, including through calcium carbonate precipitation and sequestration. Moreover, gut microbes are likely more metabolically active than bacterioplankton given that animals actively feed and accumulate organic matter amongst co-concentrated microbes. Gut microbes, especially if we consider all epi- to bathypelagic animals, may represent a significant and previously unrecognized component of marine biogeochemical cycles, though their relative importance compared to free-living microbes requires further quantification.