Microbial assemblages on a cold-water coral mound at the SE Rockall bank

Judith van Bleijswijk1, Casey Whalen2, Gerard Duineveld1, Marc Lavaleye1, Harry Witte1 and Furu Mienis3, (1)Royal Netherlands Institute for Sea Research, Den Burg, Netherlands, (2)Royal Netherlands Institute for Sea Research, Biological Oceanography, den burg, Texel, Netherlands, (3)Royal Netherlands Institute for Sea Research, Den Burg, 1790, Netherlands
Abstract:
The microbial community composition over Haas Mound, one of the most prominent cold-water coral mounds of the Logachev Mound Province (Rockall Bank, NE Atlantic) was analysed by Roche GS-FLX amplicon sequencing targeting both Bacteria and Archaea. Overlaying water was collected from depths of 400 m as well as 5 and 10 m above the bottom using a CTD/Rosette system. Near-bottom water, sediment, and samples of mucus and skeleton of the coral Lophelia pertusa were obtained with a box-corer. We outline patterns of microbial distribution, vertically - from the seafloor to the water column - and laterally - across the mound - and couple these to mound topography and turbidity. A strong link was found between the microbial community composition and the specific biotopes. At all locations, the near-bottom water differed significantly from water at 5 m above the bottom, illustrating that the near-bottom water in between the coral framework represents a separate microbial habitat. Near-bottom water was distinct from other biotopes by outstanding relative abundance of the class Halobacteria (1.2%) and the genera Nitrosopumilus (3.2%), uncultured Xanthomonadales (1,6%), Defluviicoccus (1.3%), Marinicella (1.2%), and Brocadiaceae W4 lineage (1.1%). The Endozoicomonas found in near-bottom water (0.2%) is probably related to the presence of (dissolved) mucus in the water. The genus was not found in sediment, nor in overlaying water at 5 m above the bottom. The overlaying water community (sampled at 400m and at 500-1200m) was structured according to depth and correlated variables i.e. temperature, salinity and density (17% explained). Turbidity of the overlaying water explained an additional 14% and was correlated with sampling year.