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      Gene expression correlated with delay in shell formation in larval Pacific oysters ( Crassostrea gigas) exposed to experimental ocean acidification provides insights into shell formation mechanisms

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          Abstract

          Background

          Despite recent work to characterize gene expression changes associated with larval development in oysters, the mechanism by which the larval shell is first formed is still largely unknown. In Crassostrea gigas, this shell forms within the first 24 h post fertilization, and it has been demonstrated that changes in water chemistry can cause delays in shell formation, shell deformations and higher mortality rates. In this study, we use the delay in shell formation associated with exposure to CO 2-acidified seawater to identify genes correlated with initial shell deposition.

          Results

          By fitting linear models to gene expression data in ambient and low aragonite saturation treatments, we are able to isolate 37 annotated genes correlated with initial larval shell formation, which can be categorized into 1) ion transporters, 2) shell matrix proteins and 3) protease inhibitors. Clustering of the gene expression data into co-expression networks further supports the result of the linear models, and also implies an important role of dynein motor proteins as transporters of cellular components during the initial shell formation process.

          Conclusions

          Using an RNA-Seq approach with high temporal resolution allows us to identify a conceptual model for how oyster larval calcification is initiated. This work provides a foundation for further studies on how genetic variation in these identified genes could affect fitness of oyster populations subjected to future environmental changes, such as ocean acidification.

          Electronic supplementary material

          The online version of this article (10.1186/s12864-018-4519-y) contains supplementary material, which is available to authorized users.

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          Most cited references58

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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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            The Pacific oyster,Crassostrea gigas, shows negative correlation to naturally elevated carbon dioxide levels: Implications for near-term ocean acidification effects

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              • Article: not found

              Adult exposure influences offspring response to ocean acidification in oysters

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                Author and article information

                Contributors
                pierre.de_wit@marine.gu.se
                durlande@oregonsstate.edu
                alexander.ventura@bioenv.gu.se
                chris.langdon@oregonstate.edu
                Journal
                BMC Genomics
                BMC Genomics
                BMC Genomics
                BioMed Central (London )
                1471-2164
                22 February 2018
                22 February 2018
                2018
                : 19
                : 160
                Affiliations
                [1 ]ISNI 0000 0000 9919 9582, GRID grid.8761.8, Department of Marine Sciences, , University of Gothenburg, ; Strömstad, Sweden
                [2 ]ISNI 0000 0001 2112 1969, GRID grid.4391.f, Department of Fisheries and Wildlife and Coastal Oregon Marine Experiment Station, , Oregon State University, ; Newport, Oregon USA
                [3 ]ISNI 0000 0000 9919 9582, GRID grid.8761.8, Department of Biological and Environmental Sciences, , University of Gothenburg, ; Fiskebäckskil, Sweden
                Author information
                http://orcid.org/0000-0003-4709-3438
                Article
                4519
                10.1186/s12864-018-4519-y
                5824581
                29471790
                8b05836d-f014-412b-ad72-d88849f52645
                © The Author(s). 2018

                Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License ( http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The Creative Commons Public Domain Dedication waiver ( http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.

                History
                : 14 November 2017
                : 31 January 2018
                Funding
                Funded by: Oregon Sea Grant, Oregon State University (US)
                Award ID: NA14OAR4170064
                Award Recipient :
                Categories
                Research Article
                Custom metadata
                © The Author(s) 2018

                Genetics
                crassostrea gigas,gene expression,larvae,ocean acidification,aragonite,calcification
                Genetics
                crassostrea gigas, gene expression, larvae, ocean acidification, aragonite, calcification

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