Basin-scale patterns in the abundance of SAR11 subclades, marine Actinobacteria (OM1), members of the Roseobacter clade and OCS116 in the South Atlantic

Bacterioplankton are major biogeochemical agents responsible for mediating the flux of dissolved organic matter (DOM) and subsequent cycling of nutrients in the oceans. Most information about the composition of bacterioplankton communities has come from studies along well-defined biogeochemical gradients in the northern hemisphere. This study extends observations of spatial and temporal dynamics for SAR11, Actinobacteria and OCS116 in the North Atlantic by demonstrating distinct spatial variability in the abundance and distribution of these and other lineages across the South Atlantic gyre and in the Benguela upwelling system. We identified shifts in SAR11, Actinobacteria, OCS116, SAR86, SAR116 and members of the Roseobacter clade along basin-scale gradients in nutrients, chlorophyll and dissolved organic carbon (DOC). Distinct SAR11 subclades dominated the western and eastern regions of the gyre, and Actinobacteria, OCS116 and members of the Roseobacter lineages were most abundant at the deep chlorophyll maxima. SAR86 and SAR116 accounted for a significant fraction of coastal and open ocean communities, respectively, and members of the gamma sulfur oxidizer (GSO) clade persisted in the Benguela upwelling system. These data suggest that distinct communities are partitioned along basin-scale biogeochemical gradients, that SAR11 community structure varies across the gyre and that Actinobacteria, OCS116, and members of the Roseobacter clade are closely associated with phytoplankton in the gyre.