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Walther, Kathleen; Sartoris, Franz-Josef; Pörtner, Hans-Otto (2011): Seawater carbonate chemistry and biological processes during experiments with spider crab Hyas araneus, 2011 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.761761, In supplement to: Walther, K et al. (2011): Impacts of temperature and acidification on larval calcium incorporation of the spider crab Hyas araneus from different latitudes (54° vs. 79°N). Marine Biology, 158(9), 2043-2053, https://doi.org/10.1007/s00227-011-1711-x

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Abstract:
The combined effects of ocean warming and acidification were compared in larvae from two populations of the cold-eurythermal spider crab Hyas araneus, from one of its southernmost populations (around Helgoland, southern North Sea, 54°N, habitat temperature 3-18°C; collection: January 2008, hatch: January-February 2008) and from one of its northernmost populations (Svalbard, North Atlantic, 79°N, habitat temperature 0-6°C; collection: July 2008, hatch: February-April 2009). Larvae were exposed to temperatures of 3, 9 and 15°C combined with present-day normocapnic (380 ppm CO2) and projected future CO2 concentrations (710 and 3,000 ppm CO2). Calcium content of whole larvae was measured in freshly hatched Zoea I and after 3, 7 and 14 days during the Megalopa stage. Significant differences between Helgoland and Svalbard Megalopae were observed at all investigated temperatures and CO2 conditions. Under 380 ppm CO2, the calcium content increased with rising temperature and age of the larvae. At 3 and 9°C, Helgoland Megalopae accumulated more calcium than Svalbard Megalopae. Elevated CO2 levels, especially 3,000 ppm, caused a reduction in larval calcium contents at 3 and 9°C in both populations. This effect set in early, at 710 ppm CO2 only in Svalbard Megalopae at 9°C. Furthermore, at 3 and 9°C Megalopae from Helgoland replenished their calcium content to normocapnic levels and more rapidly than Svalbard Megalopae. However, Svalbard Megalopae displayed higher calcium contents under 3,000 ppm CO2 at 15°C. The findings of a lower capacity for calcium incorporation in crab larvae living at the cold end of their distribution range suggests that they might be more sensitive to ocean acidification than those in temperate regions.
Funding:
Seventh Framework Programme (FP7), grant/award no. 211384: European Project on Ocean Acidification
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Experimental treatmentExp treatWalther, Kathleen
2SiteSiteWalther, Kathleen
3SalinitySalWalther, Kathleen
4Temperature, waterTemp°CWalther, Kathleen
5Hyas araneus, calcium content, Zoea IH. araneus Ca Z Img/l/mgWalther, KathleenIon chromatograph, Dionex Corporation, ICS-2000
6Hyas araneus, calcium content, megalopaH. araneus Ca Mmg/l/mgWalther, KathleenIon chromatograph, Dionex Corporation, ICS-2000Day 0
7Hyas araneus, calcium content, megalopaH. araneus Ca Mmg/l/mgWalther, KathleenIon chromatograph, Dionex Corporation, ICS-2000Day 7
8Hyas araneus, calcium content, megalopaH. araneus Ca Mmg/l/mgWalther, KathleenIon chromatograph, Dionex Corporation, ICS-2000Day 14
9Alkalinity, totalATµmol/kgWalther, KathleenAlkalinity, Gran titration (Gran, 1950)
10Alkalinity, total, standard deviationAT std dev±Walther, Kathleen
11pHpHWalther, KathleenWTW 340i pH-analyzer and WTW SenTix 81-electrodeNBS/NIST scale
12pH, standard deviationpH std dev±Walther, Kathleen
13Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmWalther, KathleenCalculated using CO2SYS
14Carbon dioxide, partial pressure, standard deviationpCO2 std dev±Walther, KathleenCalculated using CO2SYS
15Carbon, inorganic, dissolvedDICµmol/kgWalther, KathleenCalculated using CO2SYS
16Carbon, inorganic, dissolved, standard deviationDIC std dev±Walther, KathleenCalculated using CO2SYS
17Bicarbonate ion[HCO3]-µmol/kgWalther, KathleenCalculated using CO2SYS
18Bicarbonate ion, standard deviation[HCO3]- std dev±Walther, KathleenCalculated using CO2SYS
19Calcite saturation stateOmega CalWalther, KathleenCalculated using CO2SYS
20Calcite saturation state, standard deviationOmega Cal std dev±Walther, KathleenCalculated using CO2SYS
21Aragonite saturation stateOmega ArgWalther, KathleenCalculated using CO2SYS
22Aragonite saturation state, standard deviationOmega Arg std dev±Walther, KathleenCalculated using CO2SYS
23Carbonate system computation flagCSC flagNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
24pHpHNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)Total scale
25Carbon dioxideCO2µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
26Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
27Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
28Bicarbonate ion[HCO3]-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
29Carbonate ion[CO3]2-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
30Aragonite saturation stateOmega ArgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
31Calcite saturation stateOmega CalNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
Size:
5064 data points

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