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      Evolved differences in energy metabolism and growth dictate the impacts of ocean acidification on abalone aquaculture

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          Significance

          The pH of the global ocean is decreasing due to the absorption of anthropogenically emitted CO 2, causing ocean acidification (OA). OA negatively impacts marine shellfish and threatens the continuing economic viability of molluscan shellfish aquaculture, a global industry valued at more than 19 billion USD. We identify traits linked to growth and lipid regulation that contribute tolerance to OA in abalone aquaculture, with broader implications for adaptation efforts in other shellfish species. We also identify evolved heritable variation for physiological resilience to OA that may be exploited in commercial and restoration aquaculture breeding programs to offset the negative consequences of continuing climate change.

          Abstract

          Ocean acidification (OA) poses a major threat to marine ecosystems and shellfish aquaculture. A promising mitigation strategy is the identification and breeding of shellfish varieties exhibiting resilience to acidification stress. We experimentally compared the effects of OA on two populations of red abalone ( Haliotis rufescens), a marine mollusc important to fisheries and global aquaculture. Results from our experiments simulating captive aquaculture conditions demonstrated that abalone sourced from a strong upwelling region were tolerant of ongoing OA, whereas a captive-raised population sourced from a region of weaker upwelling exhibited significant mortality and vulnerability to OA. This difference was linked to population-specific variation in the maternal provisioning of lipids to offspring, with a positive correlation between lipid concentrations and survival under OA. This relationship also persisted in experiments on second-generation animals, and larval lipid consumption rates varied among paternal crosses, which is consistent with the presence of genetic variation for physiological traits relevant for OA survival. Across experimental trials, growth rates differed among family lineages, and the highest mortality under OA occurred in the fastest growing crosses. Identifying traits that convey resilience to OA is critical to the continued success of abalone and other shellfish production, and these mitigation efforts should be incorporated into breeding programs for commercial and restoration aquaculture.

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          Most cited references47

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          Meta-analysis reveals negative yet variable effects of ocean acidification on marine organisms.

          Ocean acidification is a pervasive stressor that could affect many marine organisms and cause profound ecological shifts. A variety of biological responses to ocean acidification have been measured across a range of taxa, but this information exists as case studies and has not been synthesized into meaningful comparisons amongst response variables and functional groups. We used meta-analytic techniques to explore the biological responses to ocean acidification, and found negative effects on survival, calcification, growth and reproduction. However, there was significant variation in the sensitivity of marine organisms. Calcifying organisms generally exhibited larger negative responses than non-calcifying organisms across numerous response variables, with the exception of crustaceans, which calcify but were not negatively affected. Calcification responses varied significantly amongst organisms using different mineral forms of calcium carbonate. Organisms using one of the more soluble forms of calcium carbonate (high-magnesium calcite) can be more resilient to ocean acidification than less soluble forms (calcite and aragonite). Additionally, there was variation in the sensitivities of different developmental stages, but this variation was dependent on the taxonomic group. Our analyses suggest that the biological effects of ocean acidification are generally large and negative, but the variation in sensitivity amongst organisms has important implications for ecosystem responses. © 2010 Blackwell Publishing Ltd/CNRS.
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            Evidence for upwelling of corrosive "acidified" water onto the continental shelf.

            The absorption of atmospheric carbon dioxide (CO2) into the ocean lowers the pH of the waters. This so-called ocean acidification could have important consequences for marine ecosystems. To better understand the extent of this ocean acidification in coastal waters, we conducted hydrographic surveys along the continental shelf of western North America from central Canada to northern Mexico. We observed seawater that is undersaturated with respect to aragonite upwelling onto large portions of the continental shelf, reaching depths of approximately 40 to 120 meters along most transect lines and all the way to the surface on one transect off northern California. Although seasonal upwelling of the undersaturated waters onto the shelf is a natural phenomenon in this region, the ocean uptake of anthropogenic CO2 has increased the areal extent of the affected area.
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              Ocean model predictions of chemistry changes from carbon dioxide emissions to the atmosphere and ocean

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                Author and article information

                Journal
                Proc Natl Acad Sci U S A
                Proc Natl Acad Sci U S A
                pnas
                pnas
                PNAS
                Proceedings of the National Academy of Sciences of the United States of America
                National Academy of Sciences
                0027-8424
                1091-6490
                20 October 2020
                5 October 2020
                5 October 2020
                : 117
                : 42
                : 26513-26519
                Affiliations
                [1] aBodega Marine Laboratory, University of California Davis , Bodega Bay, CA 94923;
                [2] bThe Cultured Abalone Farm , Goleta, CA 93117;
                [9] cCoastal and Marine Sciences Institute , University of California , Davis, CA 95616
                [3] dDepartment of Environmental Toxicology, University of California , Davis, CA 95616;
                [4] eCalifornia Sea Grant, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093;
                [5] fCalifornia Department of Fish and Wildlife Marine Region, Bodega Marine Laboratory , Bodega Bay, CA 94923;
                [6] gKaren C. Drayer Wildlife Health Center, University of California , Davis, CA 95616;
                [7] hDepartment of Earth and Planetary Sciences, University of California , Davis, CA 95616;
                [8] iDepartment of Evolution and Ecology, University of California , Davis, CA 95616
                Author notes
                1To whom correspondence may be addressed. Email: dsswezey@ 123456ucdavis.edu .

                Edited by George N. Somero, Stanford University, Pacific Grove, CA, and approved August 10, 2020 (received for review April 11, 2020)

                Author contributions: D.S.S., S.E.B., K.M.A., D.B., A.W., L.R.-B., and E.S. designed research; D.S.S., S.E.B., K.M.A., H.K.S., D.B., and L.R.-B. performed research; D.S.S., S.E.B., K.M.A., A.W., L.R.-B., T.M.H., and E.S. contributed new reagents/analytic tools; D.S.S., S.E.B., K.M.A., H.K.S., D.B., A.W., L.R.-B., and E.S. analyzed data; and D.S.S., S.E.B., K.M.A., H.K.S., D.B., A.W., L.R.-B., T.M.H., and E.S. wrote the paper.

                Author information
                https://orcid.org/0000-0002-3916-2547
                https://orcid.org/0000-0003-0471-9496
                https://orcid.org/0000-0002-5457-6449
                https://orcid.org/0000-0003-4159-9104
                Article
                202006910
                10.1073/pnas.2006910117
                7584875
                33020305
                81435186-4f5d-4e76-b8e3-d5908c98728e
                Copyright © 2020 the Author(s). Published by PNAS.

                This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).

                History
                Page count
                Pages: 7
                Funding
                Funded by: DOC | National Oceanic and Atmospheric Administration (NOAA) 100000192
                Award ID: WC-133R-15-CN-0072
                Award Recipient : Daniel S. Swezey Award Recipient : Kristin M. Aquilino Award Recipient : Doug Bush Award Recipient : Andrew Whitehead Award Recipient : Tessa M Hill Award Recipient : Eric Sanford
                Funded by: DOC | National Oceanic and Atmospheric Administration (NOAA) 100000192
                Award ID: WC-133R-16-CN-0105
                Award Recipient : Daniel S. Swezey Award Recipient : Kristin M. Aquilino Award Recipient : Doug Bush Award Recipient : Andrew Whitehead Award Recipient : Tessa M Hill Award Recipient : Eric Sanford
                Funded by: California Sea Grant
                Award ID: R/HCME-10
                Award Recipient : Andrew Whitehead Award Recipient : Laura Rogers-Bennett Award Recipient : Eric Sanford
                Categories
                9
                Biological Sciences
                Sustainability Science

                climate resilience,aquaculture,genetic variation,global environmental change,lipid regulation

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