High latitude Southern Ocean phytoplankton have distinctive bio-optical properties

被引:13
|
作者
Robinson, Charlotte M. [1 ]
Huot, Yannick [2 ]
Schuback, Nina [1 ,3 ,4 ,5 ]
Ryan-Keogh, Thomas J. [6 ]
Thomalla, Sandy J. [6 ,7 ]
Antoine, David [1 ,8 ]
机构
[1] Curtin Univ, Sch Earth & Planetary Sci, Remote Sensing & Satellite Res Grp, Kent St, Bentley, WA 6102, Australia
[2] Univ Sherbrooke, Ctr Applicat & Rech Teledetect, Dept Geomat Appl, Sherbrooke, PQ J1K 2R1, Canada
[3] Ecole Polytech Fed Lausanne, Swiss Polar Inst, Lausanne, Switzerland
[4] Univ Bern, Inst Geol Sci, Bern, Switzerland
[5] Univ Bern, Oeschger Ctr Climate Change Res, Bern, Switzerland
[6] CSIR, Southern Ocean Carbon & Climate Observ SOCCO, Smart Pl, ZA-7700 Cape Town, South Africa
[7] Univ Cape Town, Marine Res Inst MaRe, ZA-7701 Cape Town, South Africa
[8] Sorbonne Univ, Lab Oceanog Villefranche, CNRS, F-06230 Villefranche Sur Mer, France
来源
OPTICS EXPRESS | 2021年 / 29卷 / 14期
基金
澳大利亚研究理事会;
关键词
NATURAL IRON-FERTILIZATION; SPECTRAL ABSORPTION-COEFFICIENTS; NONLINEAR MINIMIZATION SUBJECT; CHLOROPHYLL-A CONCENTRATION; LIGHT-ABSORPTION; IN-SITU; OPTICAL-PROPERTIES; ANTARCTIC PHYTOPLANKTON; PHAEOCYSTIS-ANTARCTICA; KERGUELEN PLATEAU;
D O I
10.1364/OE.426737
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
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
引用
收藏
页码:21084 / 21112
页数:29
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