4.6 Article

High latitude Southern Ocean phytoplankton have distinctive bio-optical properties

Journal

OPTICS EXPRESS
Volume 29, Issue 14, Pages 21084-21112

Publisher

Optica Publishing Group
DOI: 10.1364/OE.426737

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Funding

  1. Ferring Pharmaceuticals
  2. Southern Ocean Carbon and Climate Observatory
  3. Council for Scientific and Industrial Research, South Africa [SNA2011112600001]
  4. Australian Research Council [DP160103387]
  5. Curtin University
  6. Swiss Polar Institute

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The study of Southern Ocean biogeochemistry using remote sensing requires accurate interpretation of ocean color through bio-optical and biogeochemical relationships, especially in relation to chlorophyll a. Results from the Antarctic Circumnavigation Expedition indicate unique relationships between bio-optical properties and chlorophyll a in the Southern Ocean, as well as distinct differences between high and low latitude regions. This suggests differences in phytoplankton community composition and acclimation to environmental conditions in different areas of the Southern Ocean.
Studying the biogeochemistry of the Southern Ocean using remote sensing relies on accurate interpretation of ocean colour through bio-optical and biogeochemical relationships between quantities and properties of interest. During the Antarctic Circumnavigation Expedition of the 2016/2017Austral Summer, we collected a spatially comprehensive dataset of phytoplankton pigment concentrations, particulate absorption and particle size distribution and compared simple bio-optical and particle property relationships as a function of chlorophyll a. Similar to previous studies we find that the chlorophyll-specific phytoplankton absorption coefficient is significantly lower than in other oceans at comparable chlorophyll concentrations. This appears to be driven in part by lower concentrations of accessory pigments per unit chlorophyll a as well as increased pigment packaging due to relatively larger sized phytoplankton at low chlorophyll a than is typically observed in other oceans. We find that the contribution of microphytoplankton (>20 mu m size) to chlorophyll a estimates of phytoplankton biomass is significantly higher than expected for the given chlorophyll a concentration, especially in higher latitudes south of the Southern Antarctic Circumpolar Current Front. Phytoplankton pigments are more packaged in larger cells, which resulted in a flattening of phytoplankton spectra as measured in these samples when compared to other ocean regions with similar chlorophyll a concentration. Additionally, we find that at high latitude locations in the Southern Ocean, pheopigment concentrations can exceed mono-vinyl chlorophyll a concentrations. Finally, we observed very different relationships between particle volume and chlorophyll a concentrations in high and low latitude Southern Ocean waters, driven by differences in phytoplankton community composition and acclimation to environmental conditions and varying contribution of non-algal particles to the particulate matter. Our data confirm that, as previously suggested, the relationships between bio-optical properties and chlorophyll a in the Southern Ocean are different to other oceans. In addition, distinct bio-optical properties were evident between high and low latitude regions of the Southern Ocean basin. Here we provide a region-specific set of power law functions describing the phytoplankton absorption spectrum as a function of chlorophyll a. (C) 2021 Optical Society of America under the terms of the OSA Open Access Publishing Agreement

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