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.
This project will provide service and maintenance of sensors and ground-truthing of the mooring data at the Gray's Reef OA monitoring site, as well as data quality control and synthesis. Specifically, we will accomplish the follow three tasks: 1. Deployment and maintenance of the sensors (pCO2, pH, and dissolved oxygen); 2. Collection of underway pCO2 data and bulk water samples for analyses using ship-of-opportunity and dedicated cruises about four times a year; and 3. Data quality control and data synthesis.
The goal of this project is to improve our understanding of the effects of ocean acidification and warming on coral reef communities by examining responses of entire suites of reef organisms recruiting to Autonomous Reef Monitoring Structures (ARMS) in benthic mesocosms. We will perform a fully factorial experiment that consists of four treatments of low and high temperature and pCO₂ levels. ARMS are the leading long-term monitoring tool to measure biodiversity on reef systems and are integrated into the National Coral Reef Monitoring Program (NCRMP) Class II and Class III climate stations dedicated to monitor and access the physical, chemical and biological impacts associated with climate change over time. We propose to examine the effects of elevated temperature and pCO₂ on recruitment, biomass, biodiversity, and community structure over a multiannual time frame to increase our understanding of how biodiversity, ecosystem function, and their relationship will be impacted under future climate scenarios.
NCRMP‐OA is a Joint Enterprise designed to address the Tier 1 Ocean Acidification (OA) components of the larger NCRMP strategic framework at Class 0, II, and III stations. Field work and laboratory analyses for the Atlantic/Caribbean region (Florida, Puerto Rico, U.S. Virgin Islands [USVI], and Flower Garden Banks [FGB]) are executed by the OAR Atlantic Oceanographic and Meteorological Laboratory (AOML) and by the University of Puerto Rico (UPR) Caribbean Coastal Ocean Observing System (CariCOOS). Field work in the Pacific region (Main Hawaiian Islands [MHI], Northwestern Hawaiian Islands [NWHI], Guam, Commonwealth of the Northern Mariana Islands [CNMI], American Sāmoa, and the Pacific Remote Island Areas [PRIA]) is executed by the NMFS Pacific Islands Fisheries Science Center [PIFSC] Coral Reef Ecosystem Division (CRED); laboratory analyses for the Pacific region are executed by the OAR Pacific Marine Environmental Laboratory (PMEL). NCRMP‐OA Teams closely coordinate with other NCRMP elements (benthic, fish, water temperature, satellite, and socioeconomic teams), including PMEL’s NOAA Ocean Acidification Observing Network (NOA‐ON), other NOAA offices, Federal, State, and Territory agencies, and academic partners, in both the Atlantic and Pacific regions.
This project monitors changes to coral reef carbonate chemistry over time, at US affiliated coral reef sites, through quantifying key chemical parameters that are expected to be impacted by ocean acidification. This effort addresses OAP programmatic themes 1 and 5 by maintaining the coral reef portion of the OA monitoring network and developing a procedure for data synthesis, assimilation, and distribution. Incorporating an interdisciplinary approach, this project will collect, process, analyze, and steward dissolved inorganic carbon (DIC) and total alkalinity (TA) water sample data to document seawater carbonate chemistry at Class 0, II, III climate monitoring sites in coral reef areas of the US Atlantic and Pacific regions.
This OAP project represents the first contribution of OAP to sustained coastal Alaska OA monitoring through three years (2015-2017) of maintenance of two previously established OA mooring sites located in critical fishing areas. In FY2015, It also supported a 19 day OA survey cruise along the continental shelf of the Gulf of Alaska in summer of 2015, designed to fill observing gaps that have made it difficult to quantify the extent of OA events. This support has been critical for continuing OA research in Alaska, as the initial infrastructure funding was not sufficient or intended for long-term operation.
These OAP-sponsored monitoring and observing activities support a number of cross-cutting research efforts. Firstly, the data itself will provide new insights into the seasonal progression of OA events caused by the progressive accumulation of anthropogenic CO2 into the region's coastal seas. The mooring and cruise data can also be used as an early warning system for stakeholders around the state, as well as to provide information for other types of OA research. Other projects within the OAP Alaska Enterprise focus on laboratory based evaluation of the impact of OA on commercially and ecologically important Alaskan species, especially during the vulnerable larval and juvenile life stages. This environmental monitoring informs those studies by describing the intensity, duration, and extent of OA events and providing a baseline for projecting future conditions. Finally, this observational data is used to validate new OA models that are currently being developed for the Gulf of Alaska and Bering Sea, and are applied in bio-economic models of crab and pollock abundance forecasts (e.g., Punt et al., 2014; Mathis et al., 2014).
This project will provide time-series observations of coastal ocean pH and carbon system properties, along with other variables that affect carbon transformations, in the northern Gulf of Mexico in support of goals elucidated in the NOAA Ocean and Great Lakes Acidification Research Implementation Plan. This project most directly addresses Theme 1: Develop the monitoring capacity to quantify and track ocean acidification in open-ocean, coastal, and Great Lake systems, but also addresses the educational objectives of Theme 6. USM will maintain a 3- m discus buoy in the northern Gulf of Mexico with a PMEL MAPCO2 system that includes a CTD, dissolved oxygen, and pH sensors. Meteorological sensors on the buoy will be utilized for computing air-sea fluxes of CO2. Water samples and continuous vertical profiles will be taken at the buoy site during quarterly cruises. Water samples will be analyzed for DIC, TA, pH, dO, S, NUTS and chlorophyll a. Analyzed water samples and profile data will be submitted to NODC through standard NOAA OAP submission spreadsheets containing both data and associated metadata.
While this work is focused on the Gulf of Mexico additional time-series sites in the South Atlantic Bight and Gulf of Maine can provide a comparison over a wide range of coastal and latitudinal regimes. The northern Gulf of Mexico, Florida and South Atlantic Bight regions are all commonly influenced by one contiguous western boundary current system, which originates with the Loop Current in the Gulf of Mexico and then becomes the Gulf Stream along the southeastern U.S. continental shelf. The Gulf of Mexico observations will be compared with the other western boundary current influenced site in the South Atlantic Bight maintained by the University of Georgia (UGA) and the high latitude site in the Gulf of Maine maintained by the University of New Hampshire (UNH).