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      Climatic regulation of the neurotoxin domoic acid

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          Significance

          We investigate regulation of domoic acid, a potent marine phycotoxin, at the climate scale. Due to the threat domoic acid can pose to public health, marine wildlife, and coastal economies, decades of laboratory experiments have examined controls on domoic acid production without reaching consensus on reliable toxin-producing conditions. Our findings reveal an association between domoic acid in shellfish and climate-scale warm ocean conditions, a unique, large-scale perspective relative to previous work.

          Abstract

          Domoic acid is a potent neurotoxin produced by certain marine microalgae that can accumulate in the foodweb, posing a health threat to human seafood consumers and wildlife in coastal regions worldwide. Evidence of climatic regulation of domoic acid in shellfish over the past 20 y in the Northern California Current regime is shown. The timing of elevated domoic acid is strongly related to warm phases of the Pacific Decadal Oscillation and the Oceanic Niño Index, an indicator of El Niño events. Ocean conditions in the northeast Pacific that are associated with warm phases of these indices, including changes in prevailing currents and advection of anomalously warm water masses onto the continental shelf, are hypothesized to contribute to increases in this toxin. We present an applied domoic acid risk assessment model for the US West Coast based on combined climatic and local variables. Evidence of regional- to basin-scale controls on domoic acid has not previously been presented. Our findings have implications in coastal zones worldwide that are affected by this toxin and are particularly relevant given the increased frequency of anomalously warm ocean conditions.

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          Most cited references33

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          Causes and impacts of the 2014 warm anomaly in the NE Pacific

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            Interdecadal Modulation of ENSO Teleconnections

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              Is Open Access

              A long-term record of blended satellite and in situ sea-surface temperature for climate monitoring, modeling and environmental studies

              This paper describes a blended sea-surface temperature (SST) data set that is part of the National Oceanic and Atmospheric Administration (NOAA) Climate Data Record (CDR) program product suite. Using optimum interpolation (OI), in situ and satellite observations are combined on a daily and 0.25° spatial grid to form an SST analysis, i.e., a spatially complete field. A large-scale bias adjustment of the input infrared SSTs is made using buoy and ship observations as a reference. This is particularly important for the time periods when volcanic aerosols from the El Chichón and Mt. Pinatubo eruptions are widespread globally. The main source of SSTs is the Advanced Very High Resolution Radiometer (AVHRR), available from late 1981 to the present, which is also the temporal span of this CDR. The input and processing choices made to ensure a consistent data set that meets the CDR requirements are summarized. A brief history and an explanation of the forward production schedule for the preliminary and science-quality final product are also provided. The data set is produced and archived at the newly formed National Centers for Environmental Information (NCEI) in Network Common Data Form (netCDF) at doi:10.7289/V5SQ8XB5 .
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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
                10 January 2017
                9 January 2017
                9 January 2017
                : 114
                : 2
                : 239-244
                Affiliations
                [1] aCollege of Earth, Ocean, and Atmospheric Sciences, Oregon State University , Corvallis, OR 97331;
                [2] bNorthwest Fisheries Science Center, National Marine Fisheries Service , National Oceanic and Atmospheric Administration, Hatfield Marine Science Center, Newport, OR 97365;
                [3] cInstitute of Ecology and Evolution, University of Oregon , Eugene, OR 97403;
                [4] dNorthwest Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration , Seattle, WA 98112;
                [5] e Oregon Department of Fish and Wildlife , Astoria, OR 97103
                Author notes
                1To whom correspondence should be addressed. Email: mmckibben@ 123456coas.oregonstate.edu .

                Edited by David M. Karl, University of Hawaii, Honolulu, HI, and approved November 30, 2016 (received for review April 28, 2016)

                Author contributions: S.M.M. and A.E.W. designed research; S.M.M., A.M.W., V.L.T., M.H., and A.E.W. performed research; W.P. and A.E.W. analyzed data; and S.M.M. wrote the paper.

                Article
                PMC5240689 PMC5240689 5240689 201606798
                10.1073/pnas.1606798114
                5240689
                28069959
                b3a0aae1-3cf2-4ed9-93ea-f3d018b3c2a4

                Freely available online through the PNAS open access option.

                History
                Page count
                Pages: 6
                Categories
                Physical Sciences
                Earth, Atmospheric, and Planetary Sciences
                Biological Sciences
                Environmental Sciences

                domoic acid,Pacific Decadal Oscillation,El Niño,Northern California Current, Pseudo-nitzschia

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