Seasonal shifts in bacterial community responses to phytoplankton-derived dissolved organic matter in the Western Antarctic Peninsula

dc.contributor.author Luria, Catherine M.
dc.contributor.author Amaral-Zettler, Linda A.
dc.contributor.author Ducklow, Hugh W.
dc.contributor.author Repeta, Daniel J.
dc.contributor.author Rhyne, Andrew
dc.contributor.author Rich, Jeremy
dc.date.accessioned 2017-11-13T20:13:16Z
dc.date.available 2017-11-13T20:13:16Z
dc.date.issued 2017-11-03
dc.description © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 8 (2017): 2117, doi:10.3389/fmicb.2017.02117. en_US
dc.description.abstract Bacterial consumption of dissolved organic matter (DOM) drives much of the movement of carbon through the oceanic food web and the global carbon cycle. Understanding complex interactions between bacteria and marine DOM remains an important challenge. We tested the hypothesis that bacterial growth and community succession would respond differently to DOM additions due to seasonal changes in phytoplankton abundance in the environment. Four mesocosm experiments were conducted that spanned the spring transitional period (August–December 2013) in surface waters of the Western Antarctic Peninsula (WAP). Each mesocosm consisted of nearshore surface seawater (50 L) incubated in the laboratory for 10 days. The addition of DOM, in the form of cell-free exudates extracted from Thalassiosira weissflogii diatom cultures led to changes in bacterial abundance, production, and community composition. The timing of each mesocosm experiment (i.e., late winter vs. late spring) influenced the magnitude and direction of bacterial changes. For example, the same DOM treatment applied at different times during the season resulted in different levels of bacterial production and different bacterial community composition. There was a mid-season shift from Collwelliaceae to Polaribacter having the greatest relative abundance after incubation. This shift corresponded to a modest but significant increase in the initial relative abundance of Polaribacter in the nearshore seawater used to set up experiments. This finding supports a new hypothesis that starting community composition, through priority effects, influenced the trajectory of community succession in response to DOM addition. As strong inter-annual variability and long-term climate change may shift the timing of WAP phytoplankton blooms, and the corresponding production of DOM exudates, this study suggests a mechanism by which different seasonal successional patterns in bacterial communities could occur. en_US
dc.description.sponsorship CL was partially funded by the Graduate School and the Department of Ecology and Evolutionary Biology at Brown University and the Brown University-Marine Biological Laboratory Joint Graduate Program. This material is based upon work supported by the National Science Foundation under Grant Nos. ANT-1142114 to LA-Z, OPP-0823101 and PLR-1440435 to HD, and ANT-1141993 to JR. The Gordon and Betty Moore Foundation grant 1711 supported work by DR. en_US
dc.identifier.citation Frontiers in Microbiology 8 (2017): 2117 en_US
dc.identifier.doi 10.3389/fmicb.2017.02117
dc.identifier.uri https://hdl.handle.net/1912/9358
dc.language.iso en_US en_US
dc.publisher Frontiers Media en_US
dc.relation.uri https://doi.org/10.3389/fmicb.2017.02117
dc.rights Attribution 4.0 International *
dc.rights.uri http://creativecommons.org/licenses/by/4.0/ *
dc.subject 16S rRNA en_US
dc.subject Amplicon sequencing en_US
dc.subject Community assembly en_US
dc.subject Bacterial succession en_US
dc.subject Mesocosms en_US
dc.subject Collwelliaceae en_US
dc.subject Polaribacter en_US
dc.subject Phytoplankton exudates en_US
dc.title Seasonal shifts in bacterial community responses to phytoplankton-derived dissolved organic matter in the Western Antarctic Peninsula en_US
dc.type Article en_US
dspace.entity.type Publication
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