Seasonal restructuring of heterotrophic microbial communities is differentially affected by glacier type in Greenland fjords

Authors

Mikhno, M., Meire, L., Dasseville, R., D'hondt, S., Chaerle, P., Daveloose, I., Sabbe, K.

Abstract

Accelerated retreat of the Greenland Ice Sheets is increasing freshwater discharge to coastal fjords and promoting transitions from marine-terminating glacier (MTG) regimes to land-terminating (LTG) ones. These changes strongly affect the physical and chemical features of the water column, which in turn impact the structure and functioning of fjord ecosystems. We used high-throughput imaging and DNA metabarcoding approaches to investigate seasonal (spring vs summer) differences in the structure of pelagic microbial communities in two contrasting fjord systems (MTG vs LTG) in southwest Greenland, with focus on the bacterial and heterotrophic protist components, which to date remain understudied in Greenland fjords. Our analyses revealed a marked seasonal restructuring in the microbial communities, especially in the surface layers. In spring, heterotrophic community composition in both fjords manifested a strong link with the diatom spring bloom, being dominated by typical phytoplankton-associated and copiotroph bacterial groups that can utilize algal-derived organic matter, and protists grazing on phytoplankton. In summer, heterotroph communities strongly diverged between the two fjords, most likely caused by the differential impact of MTG vs LTG glaciers on water column structure and chemistry. There was a marked increase in pico- and nano-sized heterotrophs, parasitic protists (dinoflagellate Syndiniales), and bacterial groups indicative of low-nutrient environments. In addition, bacterial, phytoplankton and heterotrophic protist communities become more strongly coupled, either through stronger interactions and/or stronger environmental filtering acting on all groups simultaneously. These observations are indicative of a shift from resource-replete systems in spring to more resourced-depleted systems in summer. However, this shift was less pronounced in the MTG fjord, where subglacial upwelling enabled the persistence of diatom bloom related communities into summer. Finally, we uncovered the presence of a unique, ice melange associated inner fjord microbial community, which shows similarities with both supraglacial and sea-ice associated communities, in the inner part of the MTG impacted fjord.

Preprint server: bioRxiv
The authors list and abstract were imported from bioRxiv on 24 Sep 2026.

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