The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light
Compared to the rest of the globe, the Arctic Ocean is affected disproportionately by climate change. Despite these fast environmental changes, we currently know little about the effects of ocean acidification (OA) on marine key species in this area. Moreover, the existing studies typically test the...
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ftcopernicus:oai:publications.copernicus.org:bgd79771 2023-05-15T14:51:52+02:00 The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light White, Emily Hoppe, Clara J. M. Rost, Björn 2019-08-30 application/pdf https://doi.org/10.5194/bg-2019-343 https://www.biogeosciences-discuss.net/bg-2019-343/ eng eng doi:10.5194/bg-2019-343 https://www.biogeosciences-discuss.net/bg-2019-343/ eISSN: 1726-4189 Text 2019 ftcopernicus https://doi.org/10.5194/bg-2019-343 2019-12-24T11:26:19Z Compared to the rest of the globe, the Arctic Ocean is affected disproportionately by climate change. Despite these fast environmental changes, we currently know little about the effects of ocean acidification (OA) on marine key species in this area. Moreover, the existing studies typically test the effects of OA under constant, hence artificial light fields. In this study, the abundant Arctic picoeukaryote Micromonas pusilla was acclimated to current (400 μatm) and future (1000 μatm) p CO 2 levels under a constant as well as dynamic light, simulating natural light fields as experienced in the upper mixed layer. To describe and understand the responses to these drivers, growth, particulate organic carbon (POC) production, elemental composition, photophysiology and reactive oxygen species (ROS) production were analysed. M. pusilla was able to benefit from OA on various scales, ranging from an increase in growth rates to enhanced photosynthetic capacity, irrespective of the light regime. These beneficial effects were, however, not reflected in the POC production rates, which can be explained by energy partitioning towards cell division rather than biomass build-up. In the dynamic light regime, M. pusilla was able to optimise its photophysiology for effective light usage during both low and high light periods. This effective photoacclimation, which was achieved by modifications to photosystem II (PSII), imposed high metabolic costs leading to a reduction in growth and POC production rates when compared to constant light. There were no significant interactions observed between dynamic light and OA, indicating that M. pusilla was able maintain effective photoacclimation without increased photoinactivation under high p CO 2 . Based on these findings, physiologically plastic M. pusilla may exhibit a robust positive response to future Arctic Ocean conditions. Text Arctic Arctic Ocean Climate change Ocean acidification Copernicus Publications: E-Journals Arctic Arctic Ocean |
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Copernicus Publications: E-Journals |
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English |
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Compared to the rest of the globe, the Arctic Ocean is affected disproportionately by climate change. Despite these fast environmental changes, we currently know little about the effects of ocean acidification (OA) on marine key species in this area. Moreover, the existing studies typically test the effects of OA under constant, hence artificial light fields. In this study, the abundant Arctic picoeukaryote Micromonas pusilla was acclimated to current (400 μatm) and future (1000 μatm) p CO 2 levels under a constant as well as dynamic light, simulating natural light fields as experienced in the upper mixed layer. To describe and understand the responses to these drivers, growth, particulate organic carbon (POC) production, elemental composition, photophysiology and reactive oxygen species (ROS) production were analysed. M. pusilla was able to benefit from OA on various scales, ranging from an increase in growth rates to enhanced photosynthetic capacity, irrespective of the light regime. These beneficial effects were, however, not reflected in the POC production rates, which can be explained by energy partitioning towards cell division rather than biomass build-up. In the dynamic light regime, M. pusilla was able to optimise its photophysiology for effective light usage during both low and high light periods. This effective photoacclimation, which was achieved by modifications to photosystem II (PSII), imposed high metabolic costs leading to a reduction in growth and POC production rates when compared to constant light. There were no significant interactions observed between dynamic light and OA, indicating that M. pusilla was able maintain effective photoacclimation without increased photoinactivation under high p CO 2 . Based on these findings, physiologically plastic M. pusilla may exhibit a robust positive response to future Arctic Ocean conditions. |
format |
Text |
author |
White, Emily Hoppe, Clara J. M. Rost, Björn |
spellingShingle |
White, Emily Hoppe, Clara J. M. Rost, Björn The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light |
author_facet |
White, Emily Hoppe, Clara J. M. Rost, Björn |
author_sort |
White, Emily |
title |
The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light |
title_short |
The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light |
title_full |
The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light |
title_fullStr |
The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light |
title_full_unstemmed |
The Arctic picoeukaryote Micromonas pusilla benefits from Ocean Acidification under constant and dynamic light |
title_sort |
arctic picoeukaryote micromonas pusilla benefits from ocean acidification under constant and dynamic light |
publishDate |
2019 |
url |
https://doi.org/10.5194/bg-2019-343 https://www.biogeosciences-discuss.net/bg-2019-343/ |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Climate change Ocean acidification |
genre_facet |
Arctic Arctic Ocean Climate change Ocean acidification |
op_source |
eISSN: 1726-4189 |
op_relation |
doi:10.5194/bg-2019-343 https://www.biogeosciences-discuss.net/bg-2019-343/ |
op_doi |
https://doi.org/10.5194/bg-2019-343 |
_version_ |
1766323006630526976 |