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Wang, Youji; Li, Lisha; Hu, Menghong; Lu, Weiqun (2015): Physiological energetics of the thick shell mussel Mytilus coruscus exposed to seawater acidification and thermal stress [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.860454, Supplement to: Wang, Y et al. (2015): Physiological energetics of the thick shell mussel Mytilus coruscus exposed to seawater acidification and thermal stress. Science of the Total Environment, 514, 261-272, https://doi.org/10.1016/j.scitotenv.2015.01.092

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Abstract:
Anthropogenic CO2 emissions have caused seawater temperature elevation and ocean acidification. In view of both phenomena are occurring simultaneously, their combined effects on marine species must be experimentally evaluated. The purpose of this study was to estimate the combined effects of seawater acidification and temperature increase on the energy budget of the thick shell mussel Mytilus coruscus. Juvenile mussels were exposed to six combined treatments with three pH levels (8.1, 7.7 and 7.3) * two temperatures (25 °C and 30 °C) for 14 d. We found that clearance rates (CRs), food absorption efficiencies (AEs), respiration rates (RRs), ammonium excretion rates (ER), scope for growth (SFG) and O:N ratios were significantly reduced by elevated temperature sometimes during the whole experiments. Low pH showed significant negative effects on RR and ER, and significantly increased O:N ratios, but showed almost no effects on CR, AE and SFG of M. coruscus. Nevertheless, their interactive effects were observed in RR, ER and O:N ratios. PCA revealed positive relationships among most physiological indicators, especially between SFG and CR under normal temperatures compared to high temperatures. PCA also showed that the high RR was closely correlated to an increasing ER with increasing pH levels. These results suggest that physiological energetics of juvenile M. coruscus are able to acclimate to CO2 acidification with a little physiological effect, but not increased temperatures. Therefore, the negative effects of a temperature increase could potentially impact the ecophysiological responses of M. coruscus and have significant ecological consequences, mainly in those habitats where this species is dominant in terms of abundance and biomass.
Keyword(s):
Animalia; Behaviour; Benthic animals; Benthos; Brackish waters; Containers and aquaria (20-1000 L or < 1 m**2); Growth/Morphology; Laboratory experiment; Mollusca; Mytilus coruscus; North Pacific; Other metabolic rates; Respiration; Single species; Temperate; Temperature
Further details:
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb
Coverage:
Latitude: 30.550260 * Longitude: 121.833270
Date/Time Start: 2013-09-01T00:00:00 * Date/Time End: 2013-09-30T00:00:00
Event(s):
Shengsi_island * Latitude: 30.550260 * Longitude: 121.833270 * Date/Time Start: 2013-09-01T00:00:00 * Date/Time End: 2013-09-30T00:00:00 * Method/Device: Experiment (EXP)
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2015) 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 2016-05-06.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1TypeTypeWang, Youjistudy
2SpeciesSpeciesWang, Youji
3Registration number of speciesReg spec noWang, Youji
4Uniform resource locator/link to referenceURL refWang, YoujiWoRMS Aphia ID
5Duration, number of daysDurationdaysWang, Youji
6TreatmentTreatWang, Youji
7Respiration rate, oxygenResp O2µg/mg/hWang, Youji
8Ammonia excretionNH3/[NH4]+ excmg/g/hWang, Youji
9Clearance rateCRml/g/hWang, Youji
10Absorption efficiencyAbsorp eff%Wang, Youji
11Fecal organic dry mass ratioFecal OM ratioWang, Youji
12Oxygen consumed/Nitrogen excreted ratioO cons/N excJ/hWang, Youji
13Scope for growthSfGJ/g/hWang, Youji
14Temperature, waterTemp°CWang, Youji
15Temperature, water, standard errorT std e±Wang, Youji
16SalinitySalWang, Youji
17Salinity, standard errorSal std e±Wang, Youji
18pHpHWang, YoujiPotentiometricNBS scale
19pH, standard errorpH std e±Wang, YoujiPotentiometricNBS scale
20Alkalinity, totalATµmol/kgWang, Youji
21Alkalinity, total, standard errorAT std e±Wang, Youji
22Carbon, inorganic, dissolvedDICµmol/kgWang, YoujiCalculated
23Carbon, inorganic, dissolved, standard errorDIC std e±Wang, YoujiCalculated
24Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmWang, YoujiCalculated
25Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard errorpCO2water_SST_wet std e±Wang, YoujiCalculated
26Calcite saturation stateOmega CalWang, YoujiCalculated
27Calcite saturation state, standard errorOmega Cal std e±Wang, YoujiCalculated
28Aragonite saturation stateOmega ArgWang, YoujiCalculated
29Aragonite saturation state, standard errorOmega Arg std e±Wang, YoujiCalculated
30Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
31pHpHYang, YanCalculated using seacarb after Nisumaa et al. (2010)total scale
32Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
33Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
34Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
36Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
37Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
38Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
39Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
2808 data points

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