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    In:  Supplement to: Wang, Tifeng; Tong, Shanying; Liu, Nana; Li, Futian; Wells, Mark L; Gao, Kunshan (2017): The fatty acid content of plankton is changing in subtropical coastal waters as a result of OA: Results from a mesocosm study. Marine Environmental Research, 132, 51-62, https://doi.org/10.1016/j.marenvres.2017.10.010
    Publication Date: 2024-05-22
    Description: Ocean Acidification (OA) effects on marine plankton are most often considered in terms of inorganic carbon chemistry, but decreasing pH may influence other aspects of cellular metabolism. Here we present the effects of OA on the fatty acid (FA) content and composition of an artificial phytoplankton community (Phaeodactylum tricornutum, Thalassiosira weissflogii, and Emiliania huxleyi) in a fully replicated, 4 m**3 mesocosm study in subtropical coastal waters (Wuyuan Bay, China, 24.52°N, 117.18°E) at present day (400 μatm) and elevated (1000 μatm) pCO2 concentrations. Phytoplankton growth occurred in three phases during the 33-day experiment: an initial exponential growth leading to senescence and a subsequent decline phase. Phytoplankton sampled from these mesocosms were fed to mesozooplankton collected by net haul from Wuyuan Bay. Concentrations of saturated fatty acids (SFA) in both phytoplankton and mesozooplankton remained high under acidified and non-acidified conditions. However, polyunsaturated fatty acids (PUFA) and monounsaturated fatty acids (MUFA) increased significantly more under elevated pCO2 during the late exponential phase (Day 13), indicating increased nutritional value for zooplankton and higher trophic levels. Indeed, uptake rates of the essential FA docosahexaenoic acid (C20:5n3, DHA) increased in mesozooplankton under acidified conditions. However, mesozooplankton grazing rates decreased overall with elevated pCO2. Our findings show that these selected phytoplankton species have a relatively high tolerance to acidification in terms of FA production, and local mesozooplankton in these subtropical coastal waters can maintain their FA composition under end of century ocean acidification conditions.
    Keywords: Alkalinity, total; all-cis-4,7,10,13,16,19-Docosahexaenoic acid of total fatty acids; all-cis-6,9,12,15,18-Heneicosapentaenoic acid of total fatty acids; Aragonite saturation state; Behaviour; Bicarbonate ion; Biomass/Abundance/Elemental composition; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chlorophyll a; Coast and continental shelf; Day of experiment; Docosahexaenoic acid; Eicosapentaenoic acid; Entire community; EXP; Experiment; Fatty acids; Fatty acids, saturated; Fatty acids, standard deviation; Fatty acids, total; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Grazing rate; Group; Mesocosm or benthocosm; Monounsaturated fatty acids; Name; n-fatty acid C14:0; n-fatty acid C16:1; n-fatty acid C18:0; n-fatty acid C18:1n9; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; Percentage; Percentage, standard deviation; pH; Phosphate; Polyunsaturated fatty acids; Polyunsaturated fatty acids of total fatty acids; Replicate; Salinity; Silicate; Temperate; Temperature, water; Treatment; Type; Wuyuan_Bay
    Type: Dataset
    Format: text/tab-separated-values, 4287 data points
    Location Call Number Limitation Availability
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