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Sett, Scarlett; Schulz, Kai; Bach, Lennart Thomas; Riebesell, Ulf (2023): Seawater carbonate chemistry and shift towards larger diatoms in a natural phytoplankton assemblage under combined high-CO2 and warming conditions [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.959214

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Abstract:
An indoor mesocosm experiment was carried out to investigate the combined effects of ocean acidification and warming on the species composition and biogeochemical element cycling during a winter/spring bloom with a natural phytoplankton assemblage from the Kiel fjord, Germany. The experimental setup consisted of a “Control” (ambient temperature of ~4.8 °C and ~535 ± 25 μatm pCO2), a “High-CO2” treatment (ambient temperature and initially 1020 ± 45 μatm pCO2) and a “Greenhouse” treatment (~8.5 °C and initially 990 ± 60 μatm pCO2). Nutrient replete conditions prevailed at the beginning of the experiment and light was provided at in situ levels upon reaching pCO2 target levels. A diatom-dominated bloom developed in all treatments with Skeletonema costatum as the dominant species but with an increased abundance and biomass contribution of larger diatom species in the Greenhouse treatment. Conditions in the Greenhouse treatment accelerated bloom development with faster utilization of inorganic nutrients and an earlier peak in phytoplankton biomass compared to the Control and High CO2 but no difference in maximum concentration of particulate organic matter (POM) between treatments. Loss of POM in the Greenhouse treatment, however, was twice as high as in the Control and High CO2 treatment at the end of the experiment, most likely due to an increased proportion of larger diatom species in that treatment. We hypothesize that the combination of warming and acidification can induce shifts in diatom species composition with potential feedbacks on biogeochemical element cycling.
Keyword(s):
Baltic Sea; Biomass/Abundance/Elemental composition; Coast and continental shelf; Community composition and diversity; Entire community; Laboratory experiment; Mesocosm or benthocosm; Pelagos; Temperate; Temperature
Supplement to:
Sett, Scarlett; Schulz, Kai Georg; Bach, Lennart Thomas; Riebesell, Ulf (2018): Shift towards larger diatoms in a natural phytoplankton assemblage under combined high-CO2 and warming conditions. Journal of Plankton Research, 40(4), 391-406, https://doi.org/10.1093/plankt/fby018
Documentation:
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James; Gentili, Bernard; Hagens, Mathilde; Hofmann, Andreas; Mueller, Jens-Daniel; Proye, Aurélien; Rae, James; Soetaert, Karline (2022): seacarb: seawater carbonate chemistry with R. R package version 3.3.1. https://cran.r-project.org/web/packages/seacarb/index.html
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2022) 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 2023-05-23.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Type of studyStudy typeSett, Scarlett
2Experiment durationExp durationdaysSett, Scarlett
3TreatmentTreatSett, Scarlett
4ReplicateReplSett, Scarlett
5pHpHSett, ScarlettNBS scale
6Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmSett, ScarlettCalculated using CO2SYS
7Alkalinity, totalATµmol/kgSett, ScarlettPotentiometric titration
8Carbon, inorganic, dissolvedDICµmol/lSett, ScarlettCoulometric titration
9Carbon, organic, particulatePOCµmol/lSett, Scarlett
10Carbon, organic, dissolvedDOCµmol/lSett, Scarlett
11Carbon, organic, particulate/Nitrogen, organic, particulate ratioPOC/PONSett, Scarlett
12Carbon, organic, particulate/Phosphorus, organic, particulate ratioPOC/POPSett, Scarlett
13Nitrogen, organic, particulate/Phosphorus, organic, particulate ratioPON/POPSett, Scarlett
14Chlorophyll aChl aµg/lSett, ScarlettPrasinophytes
15Chlorophyll aChl aµg/lSett, ScarlettChlorphytes
16Chlorophyll aChl aµg/lSett, ScarlettDinoflagelattes
17Chlorophyll aChl aµg/lSett, ScarlettDiatoms
18Chlorophyll aChl aµg/lSett, ScarlettCryptophytes
19Cell densityCells#/mlSett, ScarlettGroup I
20PercentagePerc%Sett, Scarlettcontribution to total Chlorophyll fluorescence
21Cell densityCells#/mlSett, ScarlettGroup II
22PercentagePerc%Sett, Scarlettcontribution to total Chlorophyll fluorescence
23Cell densityCells#/mlSett, ScarlettGroup III
24PercentagePerc%Sett, Scarlettcontribution to total Chlorophyll fluorescence
25SalinitySalSett, Scarlett
26Temperature, waterTemp°CSett, Scarlett
27Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
28pHpHYang, YanCalculated using seacarb after Nisumaa et al. (2010)total scale
29Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
30Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
31Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
32Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
33Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
34Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
5537 data points

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