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Abstract The flux of carbon through the labile dissolved organic matter (DOM) pool supports marine microbial communities and represents the fate of approximately half of marine net primary production (NPP). However, the behavior of individual chemical structures that make up labile DOM remain largely unknown. We performed 12 uptake kinetics and two uptake competition experiments on the abundant betaine osmolytes glycine betaine (GBT) and homarine. Combining uptake kinetics with dissolved metabolite measurements, we quantified fluxes through the DOM pool. Fluxes were correlated with particulate concentrations and ranged from 0.53 to 41 and 0.003 to 0.54 nmol L⁻¹ d⁻¹for GBT and homarine, respectively, equivalent to up to 1.2% of NPP. Turnover times of dissolved GBT and homarine ranged from 1 to 57 d. Betaines and sulfoniums such as dimethylsulfoniopropionate competitively inhibited homarine uptake. Our results quantify GBT and homarine cycling and suggest an important role for uptake competition in regulating dissolved metabolite concentrations and fluxes. 

Abstract Homarine (N-methylpicolinic acid) is a ubiquitous marine metabolite produced by phytoplankton and noted for its bioactivity in marine animals, yet its microbial degradation pathways are uncharacterized. Here, we identify a conserved operon (homABCDER) that mediates homarine catabolism in bacteria using comparative transcriptomics, mutagenesis, and targeted knockouts. Phylogenetic and genomic analyses show this operon distributed across abundant bacterial clades, including coastal copiotrophs (e.g., Rhodobacterales) and open-ocean oligotrophs (e.g., SAR11, SAR116). High-resolution mass spectrometry revealed N-methylglutamic acid and glutamic acid as key metabolic products of homarine in both model and natural systems, with N-methylglutamate dehydrogenase catalyzing their conversion. Metatranscriptomics showed responsive and in situ expression of hom genes aligned with homarine availability. These findings uncover the genetic and metabolic basis of homarine degradation, establish its ecological relevance, and highlight homarine as a versatile growth substrate that feeds into central metabolism via glutamic acid in diverse marine bacteria.