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  1. Story 480756026

    Oceanic measurements collected during a scientific cruise on NOAA ship Ronald H. Brown last week confirmed that a large area of poorly oxygenated water (known as hypoxia) is growing off the coast of Washington and Oregon.

    Oxygen-depleted bottom waters occur seasonally along the continental shelf of Washington and Oregon when strong winds blowing along the coast in spring and summer trigger upwellings that bring deep, cold, nutrient-rich water to the surface. These waters fuel blooms of plankton. The plankton in turn feeds small animals like krill which themselves serve as food for many fish. When these blooms die off, they sink to the bottom, where their decomposition consumes oxygen, leaving less for organisms, such as crabs and bottom-dwelling fish.

    Measurements collected by commercial fishermen using dissolved oxygen sensors provided by NOAA’s Coastal Hypoxia Research Program, as well as data from local moorings, also show a large area of hypoxic water.


    Earliest Onset in 35 Years

    “Low dissolved oxygen levels have become the norm in the Pacific Northeast, but this event started much earlier than we’ve seen in our records,” said Oregon State University Professor Francis Chan, director of the NOAA cooperative institute CIMERS. “This is the earliest start to the upwelling season in 35 years.”


    This map shows the location of transect lines sampled during the 2021 West Coast Ocean Acidification Cruise. Measurements taken in coastal Washington and Oregon waters confirm a large area of bottom water with low dissolved oxygen levels. Credit: NOAA Pacific Marine Environmental Laboratory

    Returning to port from the NOAA-sponsored West Coast Ocean Acidification Cruise, Richard Feely, an oceanographer with NOAA’s Pacific Marine Environmental Laboratory, said that dissolved oxygen and ocean acidity measurements are consistent with an event that has the potential to create “dead zones” later this summer. Dead zones occur when dissolved oxygen levels drop so low that crabs and other bottom-dwelling fish perish.

    This plot depicts the dissolved oxygen concentrations in a west-to-east transect from the continental shelf break on the Washington coast to the nearshore region near Copalis, WA. The thin blue line indicates the upper limit of oxygen concentrations below 62 µmol/kg in the water column between 60 and 10 km on the shelf that are hypoxic waters that are harmful to many species of fish and shellfish. Credit: NOAA Pacific Marine Environmental Laboratory/Richard Feely

    The last time scientists observed winds this strong was in 2006 when a large dead zone wiped out crabs and other bottom-dwelling marine life along the continental shelf, Chan said.

    Concerns about this summer first arose in March, when a NOAA wind measurement station observed an early shift in winds that initiate upwelling. Winds strengthened in April when the first measurements of hypoxic conditions were recorded. In late May, a NOAA Fisheries survey off Washington and Oregon found large phytoplankton blooms and hypoxic conditions on the continental shelf in the area of Grays Harbor, Washington. At about the same time, beachgoers reported large numbers of dead crabs washing ashore in the area of Ocean Shores, Washington. In early June and again in July, samples along the Newport Line, a long-term monitoring transect off Newport, Oregon, also showed hypoxic waters.


    West Coast Scientific Cruise Confirms Extent

    The West Coast Ocean Acidification Cruise left port June 13 for its 45-day mission sampling along several transects from British Columbia to California. Supported by the NOAA Ocean Acidification Program, this recurring scientific cruise surveys ocean conditions for a host of environmental parameters to better understand the factors that influence ocean acidification and hypoxia, which are related. Scientists obtain measurements from a suite of sensors and floats and collect plankton and other sea life in net trawls.

    During the cruise, NOAA ship Ronald H. Brown navigates a series of straight lines running from the edge of the continental shelf to the coast, allowing scientists to take regular measurements along the way. Feely said the scientists observed the hypoxic layer on all of the Washington and Oregon transect lines. While there are no measurements between those transect lines, he said the hypoxic layer likely covers the continental shelf region from the Olympic Peninsula in Washington to Heceta Bank on the central Oregon coast. Measurements did not indicate a hypoxic layer in Canadian transects or northern California.

    A Surprise in a Plankton Net

    One discovery on this cruise has Feely and fellow scientists anxious to get back into the laboratory. In U.S. waters, a plankton net retrieved vertically from depths of 100 meters surfaced with a large amount of a greenish-black substance in the finely woven fabric of the net. Feely suspects the net was towed through a thick layer of decaying plankton in the water column, the kind of thing responsible for creating hypoxic conditions.

    “We added a little alcohol to the sample, and we began to realize that it was a large mass of phytoplankton, either still living or dead, sinking into the deeper water and possibly providing the fuel for the oxygen uptake as it decays,” he said. Samples will be taken back to Seattle for examination under a microscope.

    As the West Coast Ocean Acidification Cruise moves south along the California coast, scientists will take ongoing measurements biweekly along the Newport, Oregon transect and by fishermen deploying dissolved oxygen sensors on commercial crab pots.

    Meanwhile, indications are that the hypoxic waters in Oregon and Washington will persist and perhaps intensify. An important coastal model called J-SCOPE, developed by the Cooperative Institute for Climate, Ocean, and Ecosystem Studies, or CICOES, NOAA’s cooperative institute with the University of Washington, predicts a large hypoxic zone will remain through fall.


    Original post: https://www.fisheries.noaa.gov/feature-story/low-oxygen-waters-washington-oregon-coasts-risk-becoming-large-dead-zones?utm_medium=email&utm_source=govdelivery

  2. Story 467842449

    Nina Bednaršeka, Jan A. Newton, Marcus W. Beck, Simone R. Alin, Richard A. Feely, Natasha R.Christman, Terrie Klinger


    Estuaries are recognized as one of the habitats most vulnerable to coastal ocean acidification due to seasonal extremes and prolonged duration of acidified conditions. This is combined with co-occurring environmental stressors such as increased temperature and low dissolved oxygen. Despite this, evidence of biological impacts of ocean acidification in estuarine habitats is largely lacking. By combining physical, biogeochemical, and biological time-series observations over relevant seasonal-to-interannual time scales, this study is the first to describe both the spatial and temporal variation of biological response in the pteropod Limacina helicina to estuarine acidification in association with other stressors. Using clustering and principal component analyses, sampling sites were grouped according to their distribution of physical and biogeochemical variables over space and time. This identified the most exposed habitats and time intervals corresponding to the most severe negative biological impacts across three seasons and three years. We developed a cumulative stress index as a means of integrating spatial-temporal OA variation over the organismal life history. Our findings show that over the 2014–2016 study period, the severity of low aragonite saturation state combined with the duration of exposure contributed to overall cumulative stress and resulted in severe shell dissolution. Seasonally-variable estuaries such as the Salish Sea (Washington, U.S.A.) predispose sensitive organisms to more severe acidified conditions than those of coastal and open-ocean habitats, yet the sensitive organisms persist. We suggest potential environmental factors and compensatory mechanisms that allow pelagic calcifiers to inhabit less favorable habitats and partially offset associated stressors, for instance through food supply, increased temperature, and adaptation of their life history. The novel metric of cumulative stress developed here can be applied to other estuarine environments with similar physical and chemical dynamics, providing a new tool for monitoring biological response in estuaries under pressure from accelerating global change.


    Original post: https://www.sciencedirect.com/

  3. Story 467842447

    S. Fisher Gonski, Micah J. Horwith, Skip Albertson, Julia Bos, Allison S. Brownlee, Natalie Coleman, Carol Falkenhayn Maloy, Mya Keyzers, Christopher Krembs, Greg Pelletier, Elisa Rauschl, Holly R. Young, Wei-Jun Cai



    The Washington State Department of Ecology conducted a large-scale ocean acidification (OA) study in greater Puget Sound to: (1) produce a marine carbon dioxide (CO2) system dataset capable of distinguishing between long-term anthropogenic changes and natural variability, (2) characterize how rivers and freshwater drive OA conditions in the region, and (3) understand the relative influence of cumulative anthropogenic forcing on regional OA conditions. Marine CO2 system data were collected monthly at 20 stations between October 2018 and February 2020. While additional data are still needed, the climate-level data collected thus far have uncovered novel insights into spatiotemporal distributions of and variability in the regional marine CO2 system, especially at low salinities in shallow, river-forced shelf regions. The data provide a strong foundation with which to continue monitoring OA conditions across the region. More importantly, this work represents the first successful long-term OA monitoring program undertaken at the state-level by a regulatory agency. Therefore, we offer the work described herein as a blueprint to help state and local scientists and environmental and natural resource managers develop, implement, and conduct long-term OA monitoring programs and studies in their own contexts and jurisdictions.

    Full Article

    Original post: https://www.tandfonline.com/

  4. Story 467842444

    Samantha A. Siedlecki1, Darren Pilcher2,5, Evan M. Howard3, Curtis Deutsch3, Parker MacCready3, Emily L. Norton2, Hartmut Frenzel3, Jan Newton4, Richard A. Feely5, Simone R. Alin5, and Terrie Klinger6

    • 1Department of Marine Sciences, University of Connecticut, Groton, CT 06340, USA
    • 2Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, Seattle, WA, 98105, USA
    • 3School of Oceanography, University of Washington, Seattle, WA 98195, USA
    • 4Applied Physics Laboratory, Washington Ocean Acidification Center, University of Washington, Seattle, WA 98105, USA
    • 5NOAA Pacific Marine Environmental Laboratory (PMEL), Seattle, WA 98115, USA
    • 6School of Marine Environment and Affairs, Washington Ocean Acidification Center, University of Washington, Seattle, WA 98105, USA

    Correspondence: Samantha A. Siedlecki (samantha.siedlecki@uconn.edu)

    Received: 17 Jul 2020 – Discussion started: 05 Aug 2020 – Revised: 04 Mar 2021 – Accepted: 13 Mar 2021 – Published: 11 May 2021



    Global projections for ocean conditions in 2100 predict that the North Pacific will experience some of the largest changes. Coastal processes that drive variability in the region can alter these projected changes but are poorly resolved by global coarse-resolution models. We quantify the degree to which local processes modify biogeochemical changes in the eastern boundary California Current System (CCS) using multi-model regionally downscaled climate projections of multiple climate-associated stressors (temperature, O2, pH, saturation state (Ω), and CO2). The downscaled projections predict changes consistent with the directional change from the global projections for the same emissions scenario. However, the magnitude and spatial variability of projected changes are modified in the downscaled projections for carbon variables. Future changes in pCO2 and surface Ω are amplified, while changes in pH and upper 200 m Ω are dampened relative to the projected change in global models. Surface carbon variable changes are highly correlated to changes in dissolved inorganic carbon (DIC), pCO2 changes over the upper 200 m are correlated to total alkalinity (TA), and changes at the bottom are correlated to DIC and nutrient changes. The correlations in these latter two regions suggest that future changes in carbon variables are influenced by nutrient cycling, changes in benthic–pelagic coupling, and TA resolved by the downscaled projections. Within the CCS, differences in global and downscaled climate stressors are spatially variable, and the northern CCS experiences the most intense modification. These projected changes are consistent with the continued reduction in source water oxygen; increase in source water nutrients; and, combined with solubility-driven changes, altered future upwelled source waters in the CCS. The results presented here suggest that projections that resolve coastal processes are necessary for adequate representation of the magnitude of projected change in carbon stressors in the CCS.



    Original post: https://bg.copernicus.org/articles/18/2871/2021/

  5. Story 467701524

    The adaptive capacity of marine calcifiers to ocean acidification (OA) is a topic of great interest to evolutionary biologists and ecologists. Previous studies have provided evidence to suggest that larval resilience to high pCO2 seawater for these species is a trait with a genetic basis and variability in natural populations. To date, however, it remains unclear how the selective effects of OA occur within the context of complex genetic interactions underpinning larval development in many of the most vulnerable taxa. Here we evaluated phenotypic and genetic changes during larval development of Pacific oysters (Crassostrea gigas) reared in ambient (~ 400 µatm) and high (~ 1600 µatm) pCO2 conditions, both in domesticated and naturalized ‘wild’ oysters from the Pacific Northwest, USA. Using pooled DNA samples, we determined changes in allele frequencies across larval development, from early “D-stage” larvae to metamorphosed juveniles (spat), in both groups and environments. Domesticated larvae had ~ 26% fewer loci with changing allele frequencies across developmental stages and < 50% as many loci affected by acidified culture conditions, compared to larvae from wild brood stock. Functional enrichment analyses of genetic markers with significant changes in allele frequency revealed that the structure and function of cellular membranes were disproportionately affected by high pCO2 conditions in both groups. These results indicate the potential for a rapid adaptive response of oyster populations to OA conditions; however, underlying genetic changes associated with larval development differ between these wild and domesticated oyster stocks and influence their adaptive responses to OA conditions.

    Durlan, E., De Wit P., Meyer E. & Langdon C., in press. Larval development in the Pacific oyster and the impacts of ocean acidification: differential genetic effects in wild and domesticated stocks. Evolutionary Applications. Article.

    Original post: https://news-oceanacidification-icc.org/