Seawater carbonate chemistry and oyster larvae shell area

  1. Miller, A Whitman 1
  2. Reynolds, Amanda C 1
  3. Sobrino, Cristina 2
  4. Riedel, Gerhardt F 1
  1. 1 Smithsonian Environmental Research Center, Washington
  2. 2 Universidade de Vigo
    info

    Universidade de Vigo

    Vigo, España

    ROR https://ror.org/05rdf8595

Verleger: PANGAEA

Datum der Publikation: 2024

Art: Dataset

CC BY 4.0

Zusammenfassung

To address CO2-induced changes to estuarine calcification, veliger larvae of two oyster species, the Eastern oyster (Crassostrea virginica), and the Suminoe oyster (Crassostrea ariakensis) were grown in estuarine water under four pCO2 regimes, 280, 380, 560 and 800 matm, to simulate atmospheric conditions in the pre-industrial era, present, and projected future concentrations in 50 and 100 years respectively. CO2 manipulations were made using an automated negative feedback control system that allowed continuous and precise control over the pCO2 in experimental aquaria. Larval growth was measured using image analysis, and calcification was measured by chemical analysis of calcium in their shells.This dataset is included in the OA-ICC data compilation maintained in the framework of the IAEA Ocean Acidification International Coordination Centre (see https://oa-icc.ipsl.fr). Original data were provided by the author of the related paper (see Related to) to the OA-ICC data curator. In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2024) 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 by seacarb is 2024-04-30.

Bibliographische Referenzen

  • 10.1371/journal.pone.0005661
  • 10.5194/essd-2-167-2010
  • https://cran.r-project.org/web/packages/seacarb/index.html