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Pérez, Claudia; Lagos, Nelson A; Saldias, Gonzalo S; Waldbusser, George G; Vargas, C A (2016): Riverine discharges impact physiological traits and carbon sources for shell carbonate in the marine intertidal mussel Perumytilus purpuratus [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.870757, Supplement to: Pérez, C et al. (2016): Riverine discharges impact physiological traits and carbon sources for shell carbonate in the marine intertidal mussel Perumytilus purpuratus. Limnology and Oceanography, 61(3), 969-983, https://doi.org/10.1002/lno.10265

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Abstract:
Anthropogenic modification watersheds and climate change have altered export from fluvial systems causing changes to the carbonate chemistry of river-influenced near shore environments. To determine the possible effects of riverine discharges on the mussel Perumytilus purpuratus, we performed in situ transplant experiments between river-influenced and open coastal habitats with contrasting seawater carbonate chemistries (i.e., pCO2, pH, Omega ar) across four regions covering a wide latitudinal range (32°55'S-40°10'S). The river-influenced habitats selected for transplant experiments were different than open coastal habitats; with higher pCO2 (354-1313 µatm), lower pH (7.6?7.9) and Omega ar values (0.4?1.4) than in open coastal area. Growth, calcification, metabolism were measured in a reciprocal transplant experiment to determine physiological responses associated with river-influenced sites and non-influenced control sites. Growth and calcification rates were higher in river-influenced habitats; however the organisms in this area also had lower metabolic rates, possibly due to enhanced food supply from river systems. Further analysis of carbon isotopic composition (delta 13C) indicated that the relative contribution of seawater dissolved inorganic carbon (DIC) to the carbonate shells of P. purpuratus was much higher than respiratory carbon. Nevertheless, P. purpuratus incorporated between 7% and 26% of metabolic carbon in the shell depending on season. There was a strong, significant relationship between delta 13C POC and delta 13C Tissue, which likely influenced the isotopic composition of the shell carbon.
Keyword(s):
Animalia; Benthic animals; Benthos; Brackish waters; Calcification/Dissolution; Estuary; Field experiment; Growth/Morphology; Mollusca; Perumytilus purpuratus; Respiration; Single species; South Pacific; Temperate
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 is 2017-01-12.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1TypeTypeVargas, C Astudy
2SpeciesSpeciesVargas, C A
3Registration number of speciesReg spec noVargas, C A
4Uniform resource locator/link to referenceURL refVargas, C AWoRMS Aphia ID
5FigureFigVargas, C A
6MonthMonthVargas, C A
7LocationLocationVargas, C A
8SiteSiteVargas, C A
9TreatmentTreatVargas, C A
10δ13C, dissolved inorganic carbonδ13C DIC‰ PDBVargas, C A
11δ13C, particulate organic carbonδ13C POC‰ PDBVargas, C A
12δ13C, particulate inorganic carbonδ13C PICVargas, C Ashell
13δ13C, particulate inorganic carbonδ13C PICVargas, C Atissue
14PercentagePerc%Vargas, C Ainorganic carbon incorporated into shell from respired carbon
15PercentagePerc%Vargas, C Ainorganic carbon incorporated into shell from DIC
16Growth rateµmm/dayVargas, C A
17Growth rate, standard deviationµ std dev±Vargas, C A
18Net calcification rate of calcium carbonate, per individualNC CaCO3/indmg/#/dayVargas, C A
19Calcification rate, standard deviationCalc rate std dev±Vargas, C A
20Metabolic rate of oxygenMR O2mg/kg/hVargas, C A
21Metabolic rate of oxygen, standard deviationMR O2 std dev±Vargas, C A
22SalinitySalVargas, C A
23Temperature, waterTemp°CVargas, C A
24pHpHVargas, C APotentiometrictotal scale
25Alkalinity, totalATµmol/kgVargas, C APotentiometric titration
26Carbon, inorganic, dissolvedDICµmol/kgVargas, C ACalculated using CO2SYS
27Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmVargas, C ACalculated using CO2SYS
28Aragonite saturation stateOmega ArgVargas, C ACalculated using CO2SYS
29Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
30Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
31Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
32Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
33Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
34Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
36Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
37Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
2066 data points

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