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Ou, Guanyong; Wang, Hong; Si, Ranran; Guan, WanChun (2017): Seawater carbonate chemistry and photophysiology and hemolytic activity of the dinoflagellate Akashiwo sanguinea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.889140, Supplement to: Ou, G et al. (2017): The dinoflagellate Akashiwo sanguinea will benefit from future climate change: The interactive effects of ocean acidification, warming and high irradiance on photophysiology and hemolytic activity. Harmful Algae, 68, 118-127, https://doi.org/10.1016/j.hal.2017.08.003

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Abstract:
Due to global climate change, marine phytoplankton will likely experience low pH (ocean acidification), high temperatures and high irradiance in the future. Here, this work report the results of a batch culture experiment conducted to study the interactive effects of elevated CO2, increased temperature and high irradiance on the harmful dinoflagellate Akashiwo sanguinea, isolated at Dongtou Island, Eastern China Sea. The A. sanguineacells were acclimated in high CO2 condition for about three months before testing the responses of cells to a full factorial matrix experimentation during a 7-day period. This study measured the variation in physiological parameters and hemolytic activity in 8 treatments, representing full factorial combinations of 2 levels each of exposure to CO2(400 and 1000 μatm), temperature (20 and 28 °C) and irradiance (50 and 200 μmol photons /m**2/s). Sustained growth of A. sanguinea occurred in all treatments, but high CO2 (HC) stimulated faster growth than low CO2 (LC). The pigments (chlorophyll a and carotenoid) decreased in all HC treatments. The quantum yield (Fv/Fm) declined slightly in all high-temperature (HT) treatments. High irradiance (HL) induced the accumulation of ultraviolet-absorbing compounds (UVabc) irrespective of temperature and CO2. The hemolytic activity in the LC treatments, however, declined when exposed to HT and HL, but HC alleviated the adverse effects of HT and HL on hemolytic activity. All HC and HL conditions and the combinations of high temperature*high light (HTHL) and high CO2*high temperature*high light (HCHTHL) positively affected the growth in comparison to the low CO2*low temperature*low light (LCLTLL) treatment. High temperature (HT), high light (HL) and a combination of HT*HL, however, negatively impacted hemolytic activity. CO2 was the main factor that affected the growth and hemolytic activity. There were no significant interactive effects of CO2*temperature*irradiance on growth, pigment, Fv/Fm or hemolytic activity, but there were effects on Pm, α, and Ek. If these results are extrapolated to the natural environment, it can be hypothesized that A. sanguinea cells will benefit from the combination of ocean acidification, warming, and high irradiance that are likely to occur under future climate change. It is assumed that faster growth and higher hemolytic activity and UVabc of this species will occur under future conditions compared with those the current CO2 (400 μatm) and temperature (20 °C) conditions.
Keyword(s):
Akashiwo sanguinea; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (<20 L); Chromista; Coast and continental shelf; Growth/Morphology; Laboratory experiment; Light; Myzozoa; North Pacific; North Pacific; Other studied parameter or process; Pelagos; Phytoplankton; Primary production/Photosynthesis; Single species; Temperate; Temperature
Further details:
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb
Coverage:
Latitude: 28.333330 * Longitude: 121.333330
Date/Time Start: 2016-05-01T00:00:00 * Date/Time End: 2016-05-31T00:00:00
Event(s):
Dongtou_Island * Latitude: 28.333330 * Longitude: 121.333330 * Date/Time Start: 2016-05-01T00:00:00 * Date/Time End: 2016-05-31T00:00:00 * Method/Device: Experiment (EXP)
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2018-04-11.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1TypeTypeGuan, WanChunstudy
2SpeciesSpeciesGuan, WanChun
3Registration number of speciesReg spec noGuan, WanChun
4Uniform resource locator/link to referenceURL refGuan, WanChunWoRMS Aphia ID
5Experiment durationExp durationmonthsGuan, WanChun
6TreatmentTreatGuan, WanChun
7Growth rateµ1/dayGuan, WanChun
8Growth rate, standard deviationµ std dev±Guan, WanChun
9Photochemical quantum yieldFv/FmGuan, WanChun
10Maximum photochemical quantum yield of photosystem II, standard deviationFv/Fm std dev±Guan, WanChun
11Haemolytic activityHA%Guan, WanChun
12Haemolytic activity, standard deviationHA std dev±Guan, WanChun
13Chlorophyll a per cellChl a/cellpg/#Guan, WanChun
14Chlorophyll a, standard deviationChl a std dev±Guan, WanChun
15Carotenoids per cellCarotenoids/cellpg/#Guan, WanChun
16Carotenoids, standard deviationCarotenoids std dev±Guan, WanChun
17IrradianceEµmol/m2/sGuan, WanChun
18Photosynthetic carbon fixation rate, per chlorophyll aC fix/Chl aµg/µg/hGuan, WanChun
19Carbon fixation rate, per chlorophyll a, standard deviationC fix/Chl a std dev±Guan, WanChun
20Photosynthetic carbon fixation rate, per chlorophyll aC fix/Chl aµg/µg/hGuan, WanChunmaximum
21Carbon fixation rate, per chlorophyll a, standard deviationC fix/Chl a std dev±Guan, WanChunmaximum
22Photosynthetic efficiency, carbon productionalphamg C/(µE/m2/s)/mg Chl/hGuan, WanChun
23Photosynthetic efficiency, standard deviationalpha std dev±Guan, WanChun
24Light saturationEkµmol/m2/sGuan, WanChun
25Light saturation, standard deviationEk std dev±Guan, WanChun
26SalinitySalGuan, WanChun
27Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmGuan, WanChun
28Partial pressure of carbon dioxide, standard deviationpCO2 std dev±Guan, WanChun
29Temperature, waterTemp°CGuan, WanChun
30IrradianceEµmol/m2/sGuan, WanChun
31pHpHGuan, WanChunNBS scale
32pH, standard deviationpH std dev±Guan, WanChunNBS scale
33Carbon, inorganic, dissolvedDICµmol/kgGuan, WanChunCalculated using CO2SYS
34Carbon, inorganic, dissolved, standard deviationDIC std dev±Guan, WanChunCalculated using CO2SYS
35Bicarbonate ion[HCO3]-µmol/kgGuan, WanChunCalculated using CO2SYS
36Bicarbonate ion, standard deviation[HCO3]- std dev±Guan, WanChunCalculated using CO2SYS
37Carbonate ion[CO3]2-µmol/kgGuan, WanChunCalculated using CO2SYS
38Carbonate ion, standard deviation[CO3]2- std dev±Guan, WanChunCalculated using CO2SYS
39Carbon dioxideCO2µmol/kgGuan, WanChunCalculated using CO2SYS
40Carbon dioxide, standard deviationCO2 std dev±Guan, WanChunCalculated using CO2SYS
41Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
42pHpHYang, YanCalculated using seacarb after Nisumaa et al. (2010)total scale
43Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
44Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
45Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
46Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
47Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
48Alkalinity, totalATµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
49Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
50Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
2008 data points

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