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Tunnicliffe, Verena; Davies, Kimberly T A; Butterfield, David A; Embley, Robert W; Rose, Jonathan M; Chadwick, William W Jr (2009): Seawater carbonate chemistry and Bathymodiolus brevior shell variables near Eifuku volcano, Japan, 2009 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.758715, Supplement to: Tunnicliffe, V et al. (2009): Survival of mussels in extremely acidic waters on a submarine volcano. Nature Geoscience, 2, 344-348, https://doi.org/10.1038/ngeo500

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Abstract:
Increasing atmospheric carbon dioxide levels are causing ocean acidification, compromising the ability of some marine organisms to build and maintain support structures as the equilibrium state of inorganic carbon moves away from calcium carbonate. Few marine organisms tolerate conditions where ocean pH falls significantly below today's value of about 8.1 and aragonite and calcite saturation values below 1. Here we report dense clusters of the vent mussel B. brevior in natural conditions of pH values between 5.36 and 7.29 on northwest Eifuku volcano, Mariana arc, where liquid carbon dioxide and hydrogen sulphide emerge in a hydrothermal setting. We find that both shell thickness and daily growth increments in shells from northwest Eifuku are only about half those recorded from mussels living in water with pH>7.8. Low pH may therefore also be implicated in metabolic impairment. We identify four-decade-old mussels, but suggest that the mussels can survive for so long only if their protective shell covering remains intact: crabs that could expose the underlying calcium carbonate to dissolution are absent from this setting. The mussels' ability to precipitate shells in such low-pH conditions is remarkable. Nevertheless, the vulnerability of molluscs to predators is likely to increase in a future ocean with low pH.
Keyword(s):
Animalia; Bathymodiolus brevior; Benthic animals; Benthos; CO2 vent; Deep-sea; Field observation; Growth/Morphology; Mollusca; North Pacific; Single species; Tropical
Funding:
Seventh Framework Programme (FP7), grant/award no. 211384: European Project on Ocean Acidification
Sixth Framework Programme (FP6), grant/award no. 511106: European network of excellence for Ocean Ecosystems Analysis
Coverage:
Median Latitude: 23.933794 * Median Longitude: 170.686507 * South-bound Latitude: 20.050103 * West-bound Longitude: 144.035506 * North-bound Latitude: 25.801383 * East-bound Longitude: 177.167231
Minimum DEPTH, water: 1103 m * Maximum DEPTH, water: 2714 m
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) 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).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1SiteSiteTunnicliffe, Verena
2LATITUDELatitudeGeocode
3LONGITUDELongitudeGeocode
4DateDateTunnicliffe, Verena
5DEPTH, waterDepth watermGeocode
6SalinitySalTunnicliffe, VerenaMeasured
7Temperature, waterTemp°CTunnicliffe, VerenaMeasured
8pHpHTunnicliffe, VerenaMeasuredNBS scale
9Alkalinity, totalATmmol(eq)/lTunnicliffe, VerenaAlkalinity, potentiometric
10Alkalinity, totalATµmol/kgTunnicliffe, VerenaCalculated
11Carbon, inorganic, dissolvedDICµmol/kgTunnicliffe, VerenaCalculated using CO2SYS
12Calcite saturation stateOmega CalTunnicliffe, VerenaCalculated using CO2SYS
13Aragonite saturation stateOmega ArgTunnicliffe, VerenaCalculated using CO2SYS
14Carbonate system computation flagCSC flagNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
15pHpHNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)Total scale
16Carbon dioxideCO2µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
17Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
18Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
19Bicarbonate ion[HCO3]-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
20Carbonate ion[CO3]2-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
21Aragonite saturation stateOmega ArgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
22Calcite saturation stateOmega CalNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
23Hydrogen sulfideH2Sµmol/lTunnicliffe, VerenaMeasured
24Bathymodiolus breviorB. brevior#Tunnicliffe, Verena
25Bathymodiolus brevior, distance from umboB. brevior distance from umbocmTunnicliffe, VerenaMeasured
26Bathymodiolus brevior, shell thicknessB. brevior shell thickµmTunnicliffe, VerenaElectron microprobe (EMP)
27Bathymodiolus brevior, shell thickness, standard deviationB. brevior shell thick std dev±Tunnicliffe, Verena
28Bathymodiolus brevior, distance from shell edgeB. brevior distance from shell edgecmTunnicliffe, VerenaMeasured
29Bathymodiolus brevior, daily growth band, widthB. brevior daily growth band widthµmTunnicliffe, VerenaElectron microprobe (EMP)
30Bathymodiolus brevior, daily growth band, width, standard errorB. brevior daily growth band width std e±Tunnicliffe, Verena
31Bathymodiolus brevior, shell, lengthB. brevior LmmTunnicliffe, VerenaMeasured
32Bathymodiolus brevior, shell, weightB. brevior shell WgTunnicliffe, VerenaMeasured
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
780 data points

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