The widely distributed marine cyanobacterium Synechococcus is thought to exert an influence on the marine silicon (Si) cycle through its high cellular Si relative to organic content. There are few measurements of Si in natural populations of Synechococcus, however, and the degree to which Synechococcus from various oligotrophic field sites and depths accumulate the element is unknown. We used synchrotron x-ray fluorescence to measure Si quotas in individual Synechococcus cells collected during three cruises in the western North Atlantic Ocean in the summer and fall, focusing on cells from the surface mixed layer (SML; <10 m) and the deep chlorophyll maximum (DCM). Individual cell quotas varied widely, from 1 to 4700 amol Si cell-1 , though the middle 50% of quotas ranged between 17 and 119 amol Si cell-1. Mean station-specific quotas exhibited an even narrower range of 31-72 amol Si cell-1. No significant differences in Si quotas were observed across cruises or among stations, and no effect of ambient silicic acid concentration on quotas was observed within the narrow range of silicic acid concentrations encountered (0.6-1.3 µM). Despite this small range in ambient silicic acid, cells collected from the SML had an average of twofold more Si than cells collected from the DCM. Differences in Si content with depth may be related to observed differences in the dominant Synechococcus clades between the SML and DCM habitats, determined by petB gene sequencing. organic matter, forming rapidly sinking (440-660 m d-1) aggregates that may export 2-3 times more C than in Synechococcus cells alone. Recent results from the Tara oceans expedition have implicated Synechococcus and its phages as having central, strategic roles in C export networks of the oligotrophic gyres (Guidi et al., 2016). Scavenging and vertical export by Synechococcus biomass thus appears to be more significant to a range of elemental budgets than previously thought (Lomas et al., 2010). The Synechococcus genus has wide temperature, nutrient, and light tolerances due to its considerable genetic diversity. Numerous clades have been defined using genetic techniques, and many clades show preferences for specific marine niches (Tai, 2009) though little is known about the degree to which natural field populations accumulate Si. With the abundance and geographic range of Synechococcus expected to grow in response to global climate change (Flombaum et al., 2013), their influence on the marine Si cycle and other elemental cycles may also grow. The observed expansion of the oligotrophic gyres (Polovina et al., 2008) and decadal declines in open-ocean diatom biomass (Krause et al., 2009) underscore the importance of understanding the interactions of natural field Synechococcus populations with Si. How do typical Synechococcus cellular Si quotas (i.e. mol Si per cell) vary across environments, seasons, and within various marine niches (e.g. surface mixed layer [SML], deep chlorophyll maximum [DCM])? We investigated these questions through synchrotron x-ray fluoresce...