Complex Microbial Communities Drive Iron and Sulfur Cycling in Arctic Fjord Sediments

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DOI

  • J. Buongiorno, University of Tennessee, Knoxville
  • ,
  • L. C. Herbert, State University New York, Stony Brook
  • ,
  • L. M. Wehrmann, State University New York, Stony Brook
  • ,
  • A. B. Michaud
  • K. Laufer
  • H. Røy
  • B. B. Jørgensen
  • A. Szynkiewicz, University of Tennessee, Knoxville
  • ,
  • A. Faiia, University of Tennessee, Knoxville
  • ,
  • K. M. Yeager, University of Kentucky
  • ,
  • K. Schindler, University of Kentucky
  • ,
  • K. G. Lloyd, University of Tennessee, Knoxville

Glacial retreat is changing biogeochemical cycling in the Arctic, where glacial runoff contributes iron for oceanic shelf primary production. We hypothesize that in Svalbard fjords, microbes catalyze intense iron and sulfur cycling in low-organic-matter sediments. This is because low organic matter limits sulfide generation, allowing iron mobility to the water column instead of precipitation as iron monosulfides. In this study, we tested this with high-depth-resolution 16S rRNA gene libraries in the upper 20 cm at two sites in Van Keulenfjorden, Svalbard. At the site closer to the glaciers, iron-reducing Desulfuromonadales, iron-oxidizing Gallionella and Mariprofundus, and sulfur-oxidizing Thiotrichales and Epsilonproteobacteria were abundant above a 12-cm depth. Below this depth, the relative abundances of sequences for sulfate-reducing Desulfobacteraceae and Desulfobulbaceae increased. At the outer station, the switch from iron-cycling clades to sulfate reducers occurred at shallower depths (∼5 cm), corresponding to higher sulfate reduction rates. Relatively labile organic matter (shown by δ13C and C/N ratios) was more abundant at this outer site, and ordination analysis suggested that this affected microbial community structure in surface sediments. Network analysis revealed more correlations between predicted iron- and sulfur-cycling taxa and with uncultured clades proximal to the glacier. Together, these results suggest that complex microbial communities catalyze redox cycling of iron and sulfur, especially closer to the glacier, where sulfate reduction is limited due to low availability of organic matter. Diminished sulfate reduction in upper sediments enables iron to flux into the overlying water, where it may be transported to the shelf.IMPORTANCE Glacial runoff is a key source of iron for primary production in the Arctic. In the fjords of the Svalbard archipelago, glacial retreat is predicted to stimulate phytoplankton blooms that were previously restricted to outer margins. Decreased sediment delivery and enhanced primary production have been hypothesized to alter sediment biogeochemistry, wherein any free reduced iron that could potentially be delivered to the shelf will instead become buried with sulfide generated through microbial sulfate reduction. We support this hypothesis with sequencing data that showed increases in the relative abundance of sulfate reducing taxa and sulfate reduction rates with increasing distance from the glaciers in Van Keulenfjorden, Svalbard. Community structure was driven by organic geochemistry, suggesting that enhanced input of organic material will stimulate sulfate reduction in interior fjord sediments as glaciers continue to recede.

Original languageEnglish
Article number00949-19
JournalApplied and Environmental Microbiology
Volume85
Issue14
Number of pages16
ISSN0099-2240
DOIs
Publication statusPublished - Jul 2019

    Research areas

  • Arctic, fjord, iron reducers, microbial communities, sulfate reducers, Svalbard

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