Coastal acidification impacts on shell mineral structure of bivalve mollusks

Ocean acidification is occurring globally through increasing CO2 absorption into the oceans creating particular concern for calcifying species. In addition to ocean acidification, near shore marine habitats are exposed to the deleterious effects of runoff from acid sulfate soils which also decreases...

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Bibliographic Details
Published in:Ecology and Evolution
Main Authors: Fitzer, Susan C, Torres Gabarda, Sergio, Daly, Luke, Hughes, Brian, Dove, Michael, O'Connor, Wayne, Potts, Jaimie, Scanes, Peter, Byrne, Maria
Other Authors: Natural Environment Research Council, Centre of Excellence for Environmental Decisions, Australian Research Council, Institute of Aquaculture, University of Sydney, University of Glasgow, Hunter Local Land Services, New South Wales Department of Primary Industries, New South Wales Office of Environment and Heritage, orcid:0000-0003-3556-7624
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2018
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Online Access:http://hdl.handle.net/1893/27640
https://doi.org/10.1002/ece3.4416
https://onlinelibrary.wiley.com/doi/epdf/10.1002/ece3.4416
http://dspace.stir.ac.uk/bitstream/1893/27640/1/Supplementary%20Materials%20.pdf
http://dspace.stir.ac.uk/bitstream/1893/27640/2/Fitzer_et_al-2018-Ecology_and_Evolution.pdf
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Summary:Ocean acidification is occurring globally through increasing CO2 absorption into the oceans creating particular concern for calcifying species. In addition to ocean acidification, near shore marine habitats are exposed to the deleterious effects of runoff from acid sulfate soils which also decreases environmental pH. This coastal acidification is being exacerbated by climate change- driven sea- level rise and catchment- driven flooding. In response to reduction in habitat pH by ocean and coastal acidification, mollusks are predicted to produce thinner shells of lower structural integrity and reduced mechanical properties threatening mollusk aquaculture. Here, we present the first study to examine oyster biomineralization under acid sulfate soil acidification in a region where growth of commercial bivalve species has declined in recent decades. Examination of the crystallography of the shells of the Sydney rock oyster, Saccostrea glomerata, by electron back scatter diffraction analyses revealed that the signal of environmental acidification is evident in the structure of the biomineral. Saccostrea glomerata, shows phenotypic plasticity, as evident in the disruption of crystallographic control over biomineralization in populations living in coastal acidification sites. Our results indicate that reduced sizes of these oysters for commercial sale may be due to the limited capacity of oysters to biomineralize under acidification conditions. As the impact of this catchment source acidification will continue to be exacerbated by climate change with likely effects on coastal aquaculture in many places across the globe, management strategies will be required to maintain the sustainable culture of these key resources.