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Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean

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dc.contributor.author Kauko, HM
dc.contributor.author Hattermann, T
dc.contributor.author Ryan-Keogh, Thomas J
dc.contributor.author Singh, Asmita
dc.contributor.author De Steur, L
dc.contributor.author Fransson, A
dc.contributor.author Chierici, M
dc.contributor.author Falkenhaug, T
dc.contributor.author Hallfredsson, EH
dc.contributor.author Bratbak, G
dc.date.accessioned 2022-05-04T13:28:46Z
dc.date.available 2022-05-04T13:28:46Z
dc.date.issued 2021-03
dc.identifier.citation Kauko, H., Hattermann, T., Ryan-Keogh, T.J., Singh, A., De Steur, L., Fransson, A., Chierici, M. & Falkenhaug, T. et al. 2021. Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean. <i>Frontiers in Marine Science, 8.</i> http://hdl.handle.net/10204/12382 en_ZA
dc.identifier.issn 2296-7745
dc.identifier.uri https://doi.org/10.3389/fmars.2021.623856
dc.identifier.uri http://hdl.handle.net/10204/12382
dc.description.abstract Knowing the magnitude and timing of pelagic primary production is important for ecosystem and carbon sequestration studies, in addition to providing basic understanding of phytoplankton functioning. In this study we use data from an ecosystem cruise to Kong Håkon VII Hav, in the Atlantic sector of the Southern Ocean, in March 2019 and more than two decades of satellite-derived ocean color to study phytoplankton bloom phenology. During the cruise we observed phytoplankton blooms in different bloom phases. By correlating bloom phenology indices (i.e., bloom initiation and end) based on satellite remote sensing to the timing of changes in environmental conditions (i.e., sea ice, light, and mixed layer depth) we studied the environmental factors that seemingly drive phytoplankton blooms in the area. Our results show that blooms mainly take place in January and February, consistent with previous studies that include the area. Sea ice retreat controls the bloom initiation in particular along the coast and the western part of the study area, whereas bloom end is not primarily connected to sea ice advance. Light availability in general is not appearing to control the bloom termination, neither is nutrient availability based on the autumn cruise where we observed non-depleted macronutrient reservoirs in the surface. Instead, we surmise that zooplankton grazing plays a potentially large role to end the bloom, and thus controls its duration. The spatial correlation of the highest bloom magnitude with marked topographic features indicate that the interaction of ocean currents with sea floor topography enhances primary productivity in this area, probably by natural fertilization. Based on the bloom timing and magnitude patterns, we identified five different bloom regimes in the area. A more detailed understanding of the region will help to highlight areas with the highest relevance for the carbon cycle, the marine ecosystem and spatial management. With this gained understanding of bloom phenology, it will also be possible to study potential shifts in bloom timing and associated trophic mismatch caused by environmental changes. en_US
dc.format Abstract en_US
dc.language.iso en en_US
dc.relation.uri https://www.frontiersin.org/articles/10.3389/fmars.2021.623856/full en_US
dc.source Frontiers in Marine Science, 8 en_US
dc.subject Bloom en_US
dc.subject Phenology en_US
dc.subject Phytoplankton en_US
dc.subject Southern Ocean en_US
dc.title Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean en_US
dc.type Article en_US
dc.description.pages 24pp en_US
dc.description.note Due to copyright restrictions, the attached PDF file only contains the abstract of the full text item. For access to the full text item, please consult the publisher's website: https://www.frontiersin.org/articles/10.3389/fmars.2021.623856/full en_US
dc.description.cluster Smart Places en_US
dc.description.impactarea Ocean Systems and Climate en_US
dc.identifier.apacitation Kauko, H., Hattermann, T., Ryan-Keogh, T. J., Singh, A., De Steur, L., Fransson, A., ... Bratbak, G. (2021). Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean. <i>Frontiers in Marine Science, 8</i>, http://hdl.handle.net/10204/12382 en_ZA
dc.identifier.chicagocitation Kauko, HM, T Hattermann, Thomas J Ryan-Keogh, Asmita Singh, L De Steur, A Fransson, M Chierici, T Falkenhaug, EH Hallfredsson, and G Bratbak "Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean." <i>Frontiers in Marine Science, 8</i> (2021) http://hdl.handle.net/10204/12382 en_ZA
dc.identifier.vancouvercitation Kauko H, Hattermann T, Ryan-Keogh TJ, Singh A, De Steur L, Fransson A, et al. Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean. Frontiers in Marine Science, 8. 2021; http://hdl.handle.net/10204/12382. en_ZA
dc.identifier.ris TY - Article AU - Kauko, HM AU - Hattermann, T AU - Ryan-Keogh, Thomas J AU - Singh, Asmita AU - De Steur, L AU - Fransson, A AU - Chierici, M AU - Falkenhaug, T AU - Hallfredsson, EH AU - Bratbak, G AB - Knowing the magnitude and timing of pelagic primary production is important for ecosystem and carbon sequestration studies, in addition to providing basic understanding of phytoplankton functioning. In this study we use data from an ecosystem cruise to Kong Håkon VII Hav, in the Atlantic sector of the Southern Ocean, in March 2019 and more than two decades of satellite-derived ocean color to study phytoplankton bloom phenology. During the cruise we observed phytoplankton blooms in different bloom phases. By correlating bloom phenology indices (i.e., bloom initiation and end) based on satellite remote sensing to the timing of changes in environmental conditions (i.e., sea ice, light, and mixed layer depth) we studied the environmental factors that seemingly drive phytoplankton blooms in the area. Our results show that blooms mainly take place in January and February, consistent with previous studies that include the area. Sea ice retreat controls the bloom initiation in particular along the coast and the western part of the study area, whereas bloom end is not primarily connected to sea ice advance. Light availability in general is not appearing to control the bloom termination, neither is nutrient availability based on the autumn cruise where we observed non-depleted macronutrient reservoirs in the surface. Instead, we surmise that zooplankton grazing plays a potentially large role to end the bloom, and thus controls its duration. The spatial correlation of the highest bloom magnitude with marked topographic features indicate that the interaction of ocean currents with sea floor topography enhances primary productivity in this area, probably by natural fertilization. Based on the bloom timing and magnitude patterns, we identified five different bloom regimes in the area. A more detailed understanding of the region will help to highlight areas with the highest relevance for the carbon cycle, the marine ecosystem and spatial management. With this gained understanding of bloom phenology, it will also be possible to study potential shifts in bloom timing and associated trophic mismatch caused by environmental changes. DA - 2021-03 DB - ResearchSpace DP - CSIR J1 - Frontiers in Marine Science, 8 KW - Bloom KW - Phenology KW - Phytoplankton KW - Southern Ocean LK - https://researchspace.csir.co.za PY - 2021 SM - 2296-7745 T1 - Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean TI - Phenology and Environmental Control of Phytoplankton Blooms in the Kong Håkon VII Hav in the Southern Ocean UR - http://hdl.handle.net/10204/12382 ER - en_ZA
dc.identifier.worklist 25487 en_US


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