NOAA's Ocean Acidification Program supports research that focuses on economically and ecologically important marine species. Research of survival, growth, and physiology of marine organisms can be used to explore how aquaculture, wild fisheries, and food webs may change as ocean chemistry changes.
A number of NOAA National Marine Fisheries Service Science Centers have state-of-the-art experimental facilities to study the response of marine organisms to the chemistry conditions expected with ocean acidification.
The Northeast Fisheries Science Center has facilities at its Sandy Hook, NJ and Milford, CT laboratories; the Alaska Fisheries Science Centers at its Newport, OR and Kodiak, AK laboratories; and the Northwest Fisheries Science Center at its Mukilteo and Manchester, WA laboratories. All facilities can tightly control carbon dioxide and temperature. The Northwest Fisheries Science Center can also control oxygen, and can create variable treatment conditions for carbon dioxide, temperature, and oxygen. These facilities include equipment for seawater carbon chemistry analysis, and all use standard operating procedures for analyzing carbonate chemistry to identify the treatment conditions used in experiments.
Both deep sea and shallow reef-building corals have calcium carbonate skeletons. As our oceans become more acidic, carbonate ions, which are an important part of calcium carbonate structures, such as these coral skeletons, become relatively less abundant. Decreases in seawater carbonate ion concentration can make building and maintaining calcium carbonate structures difficult for calcifying marine organisms such as coral.
Increased levels of carbon dioxide in our ocean can have a wide variety of impacts on fish, including altering behavior, otolith (a fish's ear bone) formation, and young fish's growth. Find out more about what scientists are learning about ocean acidification impacts on fish like rockfish, scup, summer flounder, and walleye pollock.
Shellfish, such as oyster, clams, crabs and scallop, provide food for marine life and for people, too. Shellfish make their shells or carapaces from calcium carbonate, which contains carbonate ion as a building block. The decreases in seawater carbonate ion concentration expected with ocean acidification can make building and maintaining calcium carbonate structures difficult for calcifying marine organisms like shellfish. This may impact their survival, growth, and physiology, and, thus, the food webs and economies that depend on them.
Plankton are tiny plants and animals that many marine organisms, ranging from salmon to whales, rely on for nutrition. Some plankton have calcium carbonate structures, which are built from carbonate ions. Carbonate ions become relatively less abundant as the oceans become more acidic. Decreases in seawater carbonate ions can make building and maintaining shells and other calcium carbonate structures difficult for calcifying marine organisms such as plankton. Changes to the survival, growth, and physiology of plankton can have impacts throughout the food web.
Coastal acidification and its associated co-stressors present a serious and credible threat to the success of both oyster aquaculture and restoration in the Chesapeake Bay. Recent research provides a clearer understanding of the physiological sensitivity of different economically and culturally valuable shellfish species to ocean acidification (OA), but we still lack a basic understanding of how vulnerability differs across the range of shellfish-reliant stakeholders, specifically participants in oyster aquaculture, the growers, watermen and coastal restoration managers. This basic knowledge gap motivates this work, which aims to: (1) assess the vulnerability of the oyster aquaculture industry and oyster restoration to OA and other co-stressors, and (2) produce the information required by regional communities to aid in adaptation to these stressors. In achieving these goals, we will better understand which shellfish stakeholders will be able to successfully adapt, which will seek alternative livelihoods, and what specifically causes the difference between these two disparate outcomes.
A new Ocean Acidification monitoring buoy was deployed on April 5, 2018 in the largest United States estuary, the Chesapeake Bay. This is the first long-term ocean acidification monitoring buoy and it will be deployed at the mouth of the Chesapeake Bay. The buoy will measure carbon parameters in the estuary, which is particularly vulnerable to changes in carbonate chemistry. These changes could impact economically valuable resources for Bay communities, such as oysters. The data from this buoy will supply models with the information needed to recognize potential areas of vulnerability and what future chemical parameters may look like in the bay, while also expanding the National Ocean Acidification Observing Network. It will also help researchers at NOAA PMEL, University of Delaware and University of Maryland differentiate between human-caused and natural variations in carbonate chemistry in the estuary.
The Mid-Atlantic Sea Grant Programs in partnership with the NOAA Ocean Acidification Program, are pleased to announce the availability of Ocean Acidification Graduate Research Fellowships for a two-year period covering the 2018 and 2019 academic years. The fellowship is open to full-time graduate students at any academic institution in Delaware, Maryland, New Jersey, New York and Virginia who are engaged in coastal and marine research relevant to regional ocean, coastal, and estuarine acidification. The focus should be on improving understanding of the potential ecological consequences of increasing carbon dioxide concentration in regional coastal waters. Projects may encompass natural and/or social science research topics.
Proposals are being accepted through 5:00 pm ET on Friday, April 13, 2018 via [EasyDNNnewsLink|91].
This announcement and additional information can be found on each state Sea Grant program’s website.
Awards of $1.3 million this year, totaling $4.1 million over three years, will focus on understanding the combined effects of ocean acidification, low oxygen and nutrient pollution on economically and ecologically important species in coastal habitats.
It is clear that our ocean is becoming more acidic as a result of carbon dioxide seeping into open ocean surface waters. But closer to shore things become a bit murky, as other factors can also change the chemistry of coastal waters. In these waters which are home to many important marine organisms on which coastal communities rely, scientists will be working to shed light on the potential impacts of acidification and other stresses.