Benthic foraminifera contribution to fjord modern carbon pools: A seasonal study in Adventfjorden, Spitsbergen

Abstract The aim of this study was to determine the amount of organic and inorganic carbon in foraminifera specimens and to provide quantitative data on the contribution of foraminifera to the sedimentary carbon pool in Adventfjorden. The investigation was based on three calcareous species that occu...

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Bibliographic Details
Published in:Geobiology
Main Authors: Pawłowska, J., Łącka, M., Kucharska, M., Szymańska, N., Koziorowska, K., Kuliński, K., Zajączkowski, M.
Other Authors: Narodowe Centrum Badań i Rozwoju, Suomen Akatemia
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
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Online Access:http://dx.doi.org/10.1111/gbi.12242
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgbi.12242
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gbi.12242
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Summary:Abstract The aim of this study was to determine the amount of organic and inorganic carbon in foraminifera specimens and to provide quantitative data on the contribution of foraminifera to the sedimentary carbon pool in Adventfjorden. The investigation was based on three calcareous species that occur commonly in Svalbard fjords: Cassidulina reniforme , Elphidium excavatum and Nonionellina labradorica . Our results show that the species investigated did not contribute substantially to the organic carbon pool in Adventfjorden, because they represented only 0.37% of the organic carbon in the sediment. However, foraminiferal biomass could have been underestimated as it did not include arenaceous or monothalamous taxa. Foraminiferal carbonate constituted up to 38% of the inorganic carbon in the sediment, which supports the assumption that in fjords where non‐calcifying organisms dominate the benthic fauna foraminifera are among the major producers of calcium carbonate and that they play crucial roles in the carbon burial process. The results presented in this study contribute to estimations of changes in foraminiferal carbon levels in contemporary environments and could be an important reference for palaeoceanographic studies.