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&amp;lt;p&amp;gt;&amp;lt;br /&amp;gt;
These data were published in&amp;amp;nbsp;Cruz and Neuer, 2019.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Related datasets from the same laboratory experiments:&amp;lt;br /&amp;gt;
Picocyanobacteria TEP: Cell Abundance https://www.bco-dmo.org/dataset/774628&amp;lt;br /&amp;gt;
Picocyanobacteria TEP: Growth Rates https://www.bco-dmo.org/dataset/774634&amp;lt;br /&amp;gt;
Picocyanobacteria TEP: TEP Concentration https://www.bco-dmo.org/dataset/774646&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Methodology:&amp;lt;br /&amp;gt;
Duplicate cultures of Synechococcus WH8102 (axenic), Synechococcus WH7805 (xenic) and Prochlorococcus marinus MED4 (xenic and axenic) were sampled every other day for 17-19 days for the quantification of single cells, suspended aggregates (aggregates ca. 5-60 μm), and TEP.&amp;amp;nbsp; Suspended aggregates were quantified using a Multisizer 3 Particle Counter.&amp;amp;nbsp;&amp;lt;/p&amp;gt;</gco:CharacterString>
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&lt;p&gt;The oceanic &quot;biological carbon pump&quot;, the photosynthetically mediated transformation of dissolved inorganic carbon into particulate and dissolved organic carbon and its subsequent export to deep water, functions as a significant driver of atmospheric carbon uptake by the oceans. The traditional view of the biological carbon pump in the ocean is that of sinking of large aggregates (marine snow) or fecal pellets, which are made up of large, mineral ballasted cells of phytoplankton. However, recent evidence, stemming from in situ investigations of particulate matter, trap studies and modelling studies, have shown that micron-sized phytoplankton such as picocyanobacteria as well as picoeukaryotes can contribute significantly to the sinking of particulate matter. The specific mechanisms behind the sinking of these micrometer sized cells remain elusive as the cells are too small to sink on their own, and mesozooplankton is likely unable to ingest single cells. Intriguingly, recent research by the investigators has shown that the ubiquitous picocyanobacteria Synechococcus are able to form aggregates and sink at velocities comparable to those of marine snow. They found that the matrix of the Synechococcus aggregates was made of Transparent Exopolymeric Particles (TEP), and that TEP production was enhanced under nutrient limited culture conditions. Interaction with clays and presence of heterotrophic bacteria also enhanced aggregation and sinking velocity. This study aims to further investigate aggregation of other common picoplankton in the laboratory and aggregation occurring in natural settings at an oligotrophic open ocean site, the Bermuda Atlantic Time-series Site (BATS). Ultimately, this project will increase and refine our understanding of the role of the smallest phytoplankton in aggregation and sinking - information vital to understanding carbon cycling processes in the oceans.&lt;/p&gt;</gco:CharacterString>
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