An annual cycle of diatom succession in two contrasting Greenlandic fjords: from simple sea-ice indicators to varied seasonal strategists
Authors: Luostarinen Tiia , Ribeiro Sofia , Weckström Kaarina , Sejr Mikael , Meire Lorenz , Tallberg Petra , Heikkilä Maija 
Published: March 2020

&lt;p&gt;Understanding environmental factors affecting diatom species composition at seasonal resolution can contribute to the improvement of paleo sea-ice reconstruction. We recorded diatom species succession over one full year (May 2017&amp;#8210;May 2018) using automated sediment traps installed in two contrasting Greenlandic fjords: seasonally ice-covered Young Sound in high arctic NE Greenland and nearly sea-ice free Godth&amp;#229;bsfjord in subarctic SW Greenland. The two study sites had distinct seasonal regimes in terms of both sediment and diatom fluxes. In Young Sound, diatom fluxes peaked during the ice-melt in June&amp;#8211;July (max. 880&amp;#215;10&lt;sup&gt;6&lt;/sup&gt; valves m&lt;sup&gt;-2 &lt;/sup&gt;d&lt;sup&gt;-1&lt;/sup&gt;), but were very low (0.11&amp;#173;&amp;#8211;12.7&amp;#215;10&lt;sup&gt;6&lt;/sup&gt; valves m&lt;sup&gt;-2 &lt;/sup&gt;d&lt;sup&gt;-1&lt;/sup&gt;) for the rest of the year. The pattern was very different in Godth&amp;#229;bsfjord, where diatom fluxes were more stable throughout the year and at maximum 320&amp;#215;10&lt;sup&gt;6&lt;/sup&gt; valves m&lt;sup&gt;-2 &lt;/sup&gt;d&lt;sup&gt;-1&lt;/sup&gt; in summer. A total of 60 diatom taxa were present in Young Sound and 50 in Godth&amp;#229;bsfjord, with 19 and 22 sympagic or pelagic species, respectively. The diatom assemblage in Young Sound is strongly dominated by the pennate sea-ice species&lt;em&gt; Fragilariopsis oceanica&lt;/em&gt;, &lt;em&gt;Fragilariopsis reginae-jahniae&lt;/em&gt; and &lt;em&gt;Fossula arctica&lt;/em&gt;, which exhibited pulse-like deposition in the trap during and after the ice melt. In Godth&amp;#229;bsfjord, the fluxes were dominated by resting spores of centric Chaetoceros, while the rest of the assemblage was characterized by the cold-water indicator species &lt;em&gt;Detonula confervacea&lt;/em&gt; spore, &lt;em&gt;Fragilariopsis cylindrus&lt;/em&gt; and &lt;em&gt;Thalassiosira antarctica&lt;/em&gt; var. &lt;em&gt;borealis&lt;/em&gt; spore accompanied by some warmer-water species. Some sea-ice indicator species were also observed in Godth&amp;#229;bsfjord, but at very low counts and throughout the year, likely transported from the inner fjord, which experiences seasonal sea-ice coverage. We show that &lt;em&gt;F. oceanica&lt;/em&gt;, &lt;em&gt;F. reginae-jahniae&lt;/em&gt; and &lt;em&gt;F. arctica&lt;/em&gt; exhibit similar seasonal behaviour and are clearly linked to sea ice. On the other hand,&lt;em&gt; Fragilariopsis cylindrus&lt;/em&gt; seems to have a more flexible niche, and is not an unequivocal ice indicator. Similarly, &lt;em&gt;Pauliella taeniata&lt;/em&gt; has a differing niche, and does not favour our study locations probably due to its preference for lower salinities. We underscore the importance of taking into account ecological and seasonal preferences of the individual diatom species when reconstructing past sea-ice conditions qualitatively or quantitatively.&lt;/p&gt;