Document of bibliographic reference 364060

BibliographicReference record

Type
Bibliographic resource
Type of document
Journal article
BibLvlCode
AS
Title
Earlier sea-ice melt extends the oligotrophic summer period in the Barents Sea with low algal biomass and associated low vertical flux
Abstract
The decrease in Arctic sea-ice extent and thickness as a result of global warming will impact the timing, duration, magnitude and composition of phytoplankton production with cascading effects on Arctic marine food-webs and biogeochemical cycles. Here, we elucidate the environmental drivers shaping the composition, abundance, biomass, trophic state and vertical flux of protists (unicellular eukaryotes), including phytoplankton, in the Barents Sea in late August 2018 and 2019. The two years were characterized by contrasting sea-ice conditions. In August 2018, the sea-ice edge had retreated well beyond the shelf break into the Nansen Basin (>82°N), while in 2019, extensive areas of the northwestern Barents Sea shelf (>79°N) were still ice-covered. These contrasting sea-ice conditions resulted in marked interannual differences in the pelagic protist community structure in this area. In August 2018, the protist community was in a post-bloom stage of seasonal succession characterized by oligotrophic surface waters and dominance of small-sized phytoplankton and heterotrophic protists (predominantly flagellates and ciliates) at most stations. In 2019, a higher contribution of autotrophs and large-celled phytoplankton, particularly diatoms, to total protist biomass compared to 2018 was reflected in higher chlorophyll a concentrations and suggested that the protist community was still in a late bloom stage at some stations. It is noteworthy that particularly diatoms contributed a considerably higher proportion to the protist biomass at the ice-covered stations in both years compared to the open-water stations. This pattern was also evident in the higher vertical protist biomass flux in 2019, dominated by dinoflagellates and diatoms, compared to 2018. Our results suggest that the predicted transition toward an ice-free Barents Sea will lengthen the oligotrophic summer period with low algal biomass and associated low vertical flux.
WebOfScience code
https://www.webofscience.com/wos/woscc/full-record/WOS:000968477100001
Bibliographic citation
Kohlbach, D.; Goraguer, L.; Bodur, Y.V.; Müller, O.; Amargant-Arumí, M.; Blix, K.; Bratbak, G.; Chierici, M.; Dabrowska, A.M.; Dietrich, U.; Edvardsen, B.; García, L.M.; Gradinger, R.; Hop, H.; Jones, E.; Lundesgaard, Ø.; Olsen, L.M.; Reigstad, M.; Saubrekka, K.; Tatarek, A.; Wiktor, J.M.; Wold, A.; Assmy, P. (2023). Earlier sea-ice melt extends the oligotrophic summer period in the Barents Sea with low algal biomass and associated low vertical flux. Prog. Oceanogr. 213: 103018. https://dx.doi.org/10.1016/j.pocean.2023.103018
Topic
Marine
Is peer reviewed
true
Access rights
open access
Is accessible for free
true

Authors

author
Name
Doreen Kohlbach
author
Name
Lucie Goraguer
author
Name
Yasemin Bodur
author
Name
Oliver Müller
author
Name
Martí Amargant-Arumí
author
Name
Katalin Blix
author
Name
Gunnar Bratbak
author
Name
Melissa Chierici
author
Name
Anna Maria Dabrowska
author
Name
Ulrike Dietrich
author
Name
Bente Edvardsen
author
Name
Laura García
author
Name
Rolf Gradinger
author
Name
Haakon Hop
author
Name
Elizabeth Jones
author
Name
Øyvind Lundesgaard
author
Name
Lasse Mork Olsen
author
Name
Marit Reigstad
author
Name
Karoline Saubrekka
author
Name
Agnieszka Tatarek
author
Name
Józef Wiktor
author
Name
Anette Wold
author
Name
Philipp Assmy

Links

referenced creativework
type
DOI
accessURL
https://dx.doi.org/10.1016/j.pocean.2023.103018

Document metadata

date created
2023-05-05
date modified
2023-05-23