Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Noisette, Fanny; Comtet, Thierry; Legrand, Erwann; Bordeyne, Francois; Davoult, Dominique; Martin, Sophie (2014): Does Encapsulation Protect Embryos from the Effects of Ocean Acidification? The Example of Crepidula fornicata [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.833402, Supplement to: Noisette, F et al. (2014): Does Encapsulation Protect Embryos from the Effects of Ocean Acidification? The Example of Crepidula fornicata. PLoS ONE, 9(3), e93021, https://doi.org/10.1371/journal.pone.0093021

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Early life history stages of marine organisms are generally thought to be more sensitive to environmental stress than adults. Although most marine invertebrates are broadcast spawners, some species are brooders and/or protect their embryos in egg or capsules. Brooding and encapsulation strategies are typically assumed to confer greater safety and protection to embryos, although little is known about the physico-chemical conditions within egg capsules. In the context of ocean acidification, the protective role of encapsulation remains to be investigated. To address this issue, we conducted experiments on the gastropod Crepidula fornicata. This species broods its embryos within capsules located under the female and veliger larvae are released directly into the water column. C. fornicata adults were reared at the current level of CO2 partial pressure (pCO2) (390 µatm) and at elevated levels (750 and 1400 µatm) before and after fertilization and until larval release, such that larval development occurred entirely at a given pCO2. The pCO2 effects on shell morphology, the frequency of abnormalities and mineralization level were investigated on released larvae. Shell length decreased by 6% and shell surface area by 11% at elevated pCO2 (1400 µatm). The percentage of abnormalities was 1.5- to 4-fold higher at 750 µatm and 1400 µatm pCO2, respectively, than at 390 µatm. The intensity of birefringence, used as a proxy for the mineralization level of the larval shell, also decreased with increasing pCO2. These negative results are likely explained by increased intracapsular acidosis due to elevated pCO2 in extracapsular seawater. The encapsulation of C. fornicata embryos did not protect them against the deleterious effects of a predicted pCO2 increase. Nevertheless, C. fornicata larvae seemed less affected than other mollusk species. Further studies are needed to identify the critical points of the life cycle in this species in light of future ocean acidification.
Keyword(s):
Animalia; Benthic animals; Benthos; Bottles or small containers/Aquaria (<20 L); Coast and continental shelf; Crepidula fornicata; Growth/Morphology; Laboratory experiment; Mollusca; North Atlantic; Single species; Temperate
Further details:
Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0 [webpage]. https://cran.r-project.org/package=seacarb
Coverage:
Latitude: 48.666920 * Longitude: -3.883580
Date/Time Start: 2011-11-30T00:00:00 * Date/Time End: 2011-11-30T00:00:00
Event(s):
Morlaix_Bay * Latitude: 48.666920 * Longitude: -3.883580 * Date/Time: 2011-11-30T00:00:00 * Method/Device: Experiment (EXP)
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) 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 2014-06-17.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1SpeciesSpeciesNoisette, Fanny
2Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmNoisette, Fannytreatment
3LengthlµmNoisette, Fannyshell
4HeighthµmNoisette, Fannyshell
5AreaAreaµm2Noisette, Fannyshell
6Plane anglePlane angradNoisette, Fannyformed by the abnormality
7DistanceDistanceµmNoisette, Fannybetween the theoretical curve of the shell and the forest point (extreme point) of
the deformity
8RatioRatioNoisette, Fannyange/distance
9Birefringence intensityBirefringence IpixelNoisette, Fannymean gray value of shell
10ReplicatesRepl#Noisette, Fanny
11Temperature, waterTemp°CNoisette, Fanny
12Temperature, water, standard errorT std e±Noisette, Fanny
13pHpHNoisette, FannyPotentiometrictotal scale
14pH, standard errorpH std e±Noisette, FannyPotentiometrictotal scale
15Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmNoisette, FannyCalculated using CO2SYS
16Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard errorpCO2water_SST_wet std e±Noisette, FannyCalculated using CO2SYS
17Alkalinity, totalATµmol/kgNoisette, FannyPotentiometric titration
18Alkalinity, total, standard errorAT std e±Noisette, FannyPotentiometric titration
19Carbon, inorganic, dissolvedDICµmol/kgNoisette, FannyCalculated using CO2SYS
20Carbon, inorganic, dissolved, standard errorDIC std e±Noisette, FannyCalculated using CO2SYS
21Aragonite saturation stateOmega ArgNoisette, FannyCalculated using CO2SYS
22Aragonite saturation state, standard errorOmega Arg std e±Noisette, FannyCalculated using CO2SYS
23SalinitySalNoisette, Fanny
24Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
25Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
26Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
27Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
28Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
29Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
30Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
31Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
32Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
6822 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML (shows only first 2000 rows)