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Ocean acidification

Bred oysters switch shell carbon under acidification

Fitzer SC, McGill RAR, Torres Gabarda S, et al. · Global change biology · 2019

Open access · cc by · source: Europe PMC

Selectively bred Saccostrea glomerata keep more ordered calcite and can use different DIC pathways than wild-type oysters in acidified Australian estuaries.

How this study connects

Role on claims

Each row is a claim on a concept or method page where this paper supports, challenges, or qualifies the statement. Roles are hand-checked — not a model guess.

  • SupportsOcean acidificationconcept

    Selectively bred Saccostrea glomerata keep more ordered calcite and can use different DIC pathways than wild-type oysters in acidified Australian estuaries.

    Evidence for the claim as stated.

Study at a glance

Design
Animal / in-vitro — EBSD and δ13C of shells, tissue, and extrapallial fluid from selected versus wild-type oysters at control and acidified leases
N
N=12 · 2015 year-class Saccostrea glomerata; six of 12 oysters randomly selected for some isotope maps
Population
Selectively bred and wild-type Sydney rock oysters in Australian estuaries
Outcome
Selected families keep more ordered calcite and can use different DIC pathways than wild-type oysters under coastal acidification

Structured fields used in claim comparison tables when every cited study has a complete layer.

Inspect source passages

Bred oysters switch shell carbon under acidification

These passages occur verbatim in the stored paper text. They support the points listed below; they do not verify every statement in the explanation.

Of 12 oysters sampled, six were randomly selected for analyses.

Of the 12 oysters sampled, six were randomly selected for the analyses, three for scanning electron microscopy (SEM) analyses and three for isotope analyses.

Acidified sites experience pH 7.4–7.5.

The two acidified sites differed in pH at the time of sampling but both experience similar low pH levels (pH 7.4–7.5; see Fitzer et al., ).
Read passages in the original paper

Key findings

Acidified seawater was isotopically lighter. Wild-type shells showed more crystallographic disorder. Under acidification shell δ13C went negative, consistent with a switch from HCO3− toward CO32− as the carbon source; selected families already used the CO32−-like signature at control sites.

Methodology

Families bred for QX resistance or fast growth plus wild-type oysters were sampled from control (~pH 8.1–8.2) and acidified (~pH 7.4–7.5) leases; shells were mapped by EBSD and δ13C was measured in seawater, shell, tissue, and extrapallial fluid.

Limitations

Small n (12 oysters, 3 per SEM/isotope analysis) and covarying salinity, temperature, and food mean acidification is not isolated; commercial breeding is not a reef-restoration trial.

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