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Liu, Nana; Beardall, John; Gao, Kunshan (2017): Seawater carbonate chemistry and growth and chlorophyll, photochemical parameters, carbon fixation of diatom Phaeodactylum tricornutum [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.900658, Supplement to: Liu, N et al. (2017): Elevated CO2 and associated seawater chemistry do not benefit a model diatom grown with increased availability of light. Aquatic Microbial Ecology, 79(2), 137-147, https://doi.org/10.3354/ame01820

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Abstract:
Elevated CO2 is leading to a decrease in pH in marine environments (ocean acidification [OA]), altering marine carbonate chemistry. OA can influence the metabolism of many marine organisms; however, no consensus has been reached on its effects on algal photosynthetic carbon fixation and primary production. Here, we found that when the diatom Phaeodactylum tricornutum was grown under different pCO2 levels, it showed different responses to elevated pCO2 levels under growth-limiting (20 µmol photons/m**2/s, LL) compared with growth-saturating (200 µmol photons/m**2/s, HL) light levels. With pCO2 increased up to 950 µatm, growth rates and primary productivity increased, but in the HL cells, these parameters decreased significantly at higher concentrations up to 5000 µatm, while no difference in growth was observed with pCO2 for the LL cells. Elevated CO2 concentrations reduced the size of the intracellular dissolved inorganic carbon (DIC) pool by 81% and 60% under the LL and HL levels, respectively, with the corresponding photosynthetic affinity for DIC decreasing by 48% and 55%. Little photoinhibition was observed across all treatments. These results suggest that the decreased growth rates under higher CO2 levels in the HL cells were most likely due to acid stress. Low energy demand of growth and energy saving from the down-regulation of the CO2 concentrating mechanisms (CCM) minimized the effects of acid stress on the growth of the LL cells. These findings imply that OA treatment, except for down-regulating CCM, caused stress on the diatom, reflected in diminished C assimilation and growth rates.
Keyword(s):
Bottles or small containers/Aquaria (<20 L); Chromista; Growth/Morphology; Laboratory experiment; Laboratory strains; Light; Not applicable; Pelagos; Phaeodactylum tricornutum; Phytoplankton; Primary production/Photosynthesis; Single species
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
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 2019-04-25.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1TypeTypeGao, Kunshanstudy
2SpeciesSpeciesGao, Kunshan
3Registration number of speciesReg spec noGao, Kunshan
4Uniform resource locator/link to referenceURL refGao, KunshanWoRMS Aphia ID
5Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmGao, Kunshan
6TreatmentTreatGao, Kunshan
7IdentificationIDGao, Kunshansample
8Growth rateµ1/dayGao, Kunshan
9Maximum photochemical quantum yield of photosystem IIFv/FmGao, Kunshan
10Time in secondsTimesGao, Kunshan
11Effective quantum yieldYGao, Kunshanunder 76 μmol photons/m**2/s
12Effective quantum yieldYGao, Kunshanunder 226 μmol photons/m**2/s
13Light saturation pointIkµmol/m2/sGao, Kunshan
14Maximal electron transport rate, relativerETR maxGao, Kunshan
15Light capturing capacityalphaGao, Kunshan
16Cumulative carbon fixation per cellCum C fix/cellpg/#Gao, Kunshanper 12h
17Cumulative carbon fixation per cellCum C fix/cellpg/#Gao, Kunshanper 24h
18Initial slope of photosynthesis/dissolved inorganic carbonInitial slope PN/DICGao, Kunshan
19Light saturated maximum photosynthetic rate per cellVmax/cellpg/#/hGao, Kunshan
20Carbon, inorganic, dissolved, intracellular poolDIC in poolµmol/lGao, Kunshan
21FactorFactorGao, Kunshanaccumulation for CO2
22Temperature, waterTemp°CGao, Kunshan
23SalinitySalGao, Kunshan
24Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmGao, Kunshan
25pHpHGao, KunshanNBS scale
26Alkalinity, totalATµmol/kgGao, KunshanCalculated using CO2SYS
27Carbon, inorganic, dissolvedDICµmol/kgGao, KunshanCalculated using CO2SYS
28Bicarbonate ion[HCO3]-µmol/kgGao, KunshanCalculated using CO2SYS
29Carbonate ion[CO3]2-µmol/kgGao, KunshanCalculated using CO2SYS
30Carbon dioxideCO2µmol/kgGao, KunshanCalculated using CO2SYS
31Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
32pHpHYang, YanCalculated using seacarb after Nisumaa et al. (2010)total scale
33Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
34Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
36Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
37Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
38Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
39Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
40Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
6177 data points

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