Size Structure of Primary Producers in the Marginal Ice Zone of the European Arctic in Summer

• Published in: Doklady earth sciences 2022-12, Vol.507 (Suppl 2), p.S313-S318
• Main Authors: Kudryavtseva, E. A., Kravchishina, M. D., Pautova, L. A., Rusanov, I. I., Silkin, V. A., Glukhovets, D. I., Torgunova, N. I., Netsvetaeva, O. P., Politova, N. V., Klyuvitkin, A. A., Savvichev, A. S.
• Format: Article
• Language: English
• Subjects: Acclimatization; Blooms; Carbon fixation; Chlorophyll; Chlorophyll a; Climate change; Diatoms; Earth and Environmental Science; Earth Sciences; Environmental changes; Global warming; Ice cover; Ice edge; Marine microorganisms; Mixed layer; Ocean basins; Oceanology; Phytoplankton; Phytoplankton bloom; Plankton; Primary production; Sea ice; Shelf seas; Stratification; Summer; Water circulation; Water column; Water stratification
• ISSN: 1028-334X; 1531-8354
• DOI: 10.1134/S1028334X22800030

Primary production (PP) and the chlorophyll-a concentration (chl-a) in the European Arctic in the summer of 2020–2021, where continued climatic warming and increased “Atlantification” accelerate the sea ice losses, are discussed. The maximum integrated PP and the total chl-a content were observed in the marginal ice zone (MIZ) of the Barents Sea under weakened stratification of the water column and reached 1109 mgC m –2 day –1 and 118 mg m –2 . Near the ice edge in the Nansen Basin, the main part of PP formed in the upper mixed layer and did not exceed 469 mgC m –2 day –1 ; the chl-a content reached 56 mg m –2 . The early and late stages of phytoplankton bloom in the MIZ were characterized by the leading role of picophytoplankton in carbon fixation. Large centric diatoms, microphytoplankton, were recorded to dominate in the MIZ at the stage of peak bloom in 2020 under the dense ice cover of the Nansen Basin. A similar phenomenon was observed earlier only in the Arctic shelf seas and was not recorded in the high-latitude basins of the Arctic Ocean. With the sparse ice cover of the Nansen Basin in 2021, the main primary producers were pico- and nanophytoplankton. The low variability of assimilation numbers (1.7 ± 0.3 mgC mg chl-a –1 h –1 ) at all bloom stages indicates indirectly the acclimatization of different species of phytoplankton to the environmental changes. The ecological flexibility of the primary production link of the MIZ ecosystems in the studied seas of the European Arctic during the period of climate changes is confirmed.