Seasonal assemblages and short‐lived blooms in coastal north‐west Atlantic Ocean bacterioplankton. (30th January 2015)

• Record Type: Journal Article
• Authors: El‐Swais, Heba; Dunn, Katherine A.; Bielawski, Joseph P.; Li, William K. W.; Walsh, David A.
• Is Part Of: Environmental microbiology. Volume 17:Number 10(2015:Oct.)
• Page Start: 3642
• Page End: 3661
• Publication Date: 2015-01-30
• Subjects: Microbial ecology -- Periodicals; Environmental Microbiology -- Periodicals; 579.17
• DOI: 10.1111/1462-2920.12629
• Languages: English
• ISSNs: 1462-2912

Abstract

<abstract abstract-type="main"> <title>Summary</title> <p>Temperate oceans are inhabited by diverse and temporally dynamic bacterioplankton communities. However, the role of the environment, resources and phytoplankton dynamics in shaping marine bacterioplankton communities at different time scales remains poorly constrained. Here, we combined time series observations (time scales of weeks to years) with molecular analysis of formalin‐fixed samples from a coastal inlet of the north‐west Atlantic Ocean to show that a combination of temperature, nitrate, small phytoplankton and <italic>S</italic><italic>ynechococcus</italic> abundances are best predictors for annual bacterioplankton community variability, explaining 38% of the variation. Using Bayesian mixed modelling, we identified assemblages of co‐occurring bacteria associated with different seasonal periods, including the spring bloom (e.g. <italic>P</italic><italic>olaribacter</italic>, <italic>U</italic><italic>lvibacter</italic>, <italic>A</italic><italic>lteromonadales</italic> and ARCTIC96B‐16) and the autumn bloom (e.g. OM42, OM25, OM38 and Arctic96A‐1 clades of <italic>A</italic><italic>lphaproteobacteria</italic>, and SAR86, OM60 and SAR92 clades of <italic>G</italic><italic>ammaproteobacteria</italic>). Community variability over spring bloom development was best explained by silicate (32%) – an indication of rapid succession of bacterial taxa in response to diatom biomass – while nanophytoplankton as well as picophytoplankton abundance explained community variability (16–27%) over the transition into and out of the autumn bloom. Moreover, the seasonal structure was punctuated with short‐lived blooms of rare bacteria including the KSA‐1 clade of <italic>S</italic><italic>phingobacteria</italic> related to aromatic hydrocarbon‐degrading bacteria.</p> </abstract>