Candace Ann Oviatt [1] is an ecologist at the University of Rhode Island known for research into coastal marine ecosystems with a particular focus on Narragansett Bay, Rhode Island.
Oviatt obtained a B.S. in biology from Bates College in 1961. In 1967, she became the first woman [2] to get a Ph.D. from the Graduate School of Oceanography at the University of Rhode Island. [3] Oviatt's Ph.D. dissertation examined how light impacted the movement of starfish [4] which was published in the journal Behavior in 1969. [5]
After graduate school, Oviatt took a research position at the Harvard School of Public Health. [6] Following that period, she was a research associate at the University of Rhode Island [7] where she ultimately became a professor[ citation needed ] and the director of the University of Rhode Island's Marine Ecosystems Research Lab. [8] In 1969, Oviatt began a long-standing research partnership with Scott W. Nixon which began when they simultaneously established labs in the Fish Building on the Graduate School of Oceanography campus. [7] In 2016, the University of Rhode Island honored Oviatt by inducting her into its Lifetime Service Society. [6]
Oviatt served as president of Estuarine Research Foundation, now the Coastal and Estuarine Research Federation, from 1995 to 1997. [9] [10] As of 2020, Oviatt is on the Rhode Island Natural History Survey's board of advisors. [11]
While at Harvard, Oviatt examined the potential impact of disposing burned municipal waste at sea by focusing on its impact on clams, fish, and flounder eggs. [12]
Once she returned to Rhode Island, she worked with Scott Nixon on a large scale assessment of the productivity of a New England salt marsh in a paper which combined measured data and modeled impacts of changes in temperature and sewage additions. [13] Following this work, Oviatt began a series of research projects within Narragansett Bay including investigations into sediment loading [14] and historical fish and shellfish information. [15] By comparing historical data and new research, Oviatt's research has shown that nutrient levels have decreased within Narragansett Bay with a concurrent increase in the clarity of the water. [16]
A turning point in public interest in Narragansett Bay came in 2003 when a large number of fish died due to hypoxia, [17] an event that encouraged the public to take an interest in the region's water quality. [18] Following the fish kill event, the Rhode Island Department of Environmental Management set a goal to reduce nitrogen inputs into Narragansett Bay by 50% when comparing levels from 1995-1996 to 2013-2014, [18] a goal that was met by 2015. [19] Oviatt's research has tracked long term changes in the water quality of the Bay after the establishment of new regulations regarding discharge from sewage plant. [20] During a 2017 symposium in which the question became whether the nutrient levels were too low, Oviatt noted that Narragansett Bay is always changing but "it's not a dead bay" because there are increases in some fish species concurrent with the decreases in crustaceans. [21]
Oviatt also played a critical role in establishing the Marine Ecosystem Research Lab (MERL) at the University of Rhode Island in 1976 with Scott Nixon and Michael Pilson. [7] [22] This laboratory enabled them to conduct large scale experiments with enclosed tanks (mesocosms), thereby reproducing conditions within Narragansett Bay in a controlled manner. Using the MERL tanks, Oviatt examined the impact of adding high concentrations of nutrients to a closed system [23] and the reverse situation with nutrients present in limiting quantities. [24] Other experiments included quantifying the bounds of primary production in Narragansett Bay [25] and the fate of sewage added to the coastal environment. [26]
More recently, Oviatt has used historical data to project what may happen to biological communities under future climate scenarios [27] [28] and how hurricanes alter the flux of nutrients into a region and thereby cause increased amounts of the seaweed Sargassum in the Virgin Islands. [29]
In 2015, Oviatt received the B.H. Ketchum Award from Woods Hole Oceanographic Institution and was recognized for: [30]
... her excellence in coastal marine ecology, especially her work on Narragansett Bay as a model system for the study of human impacts on temperate estuaries. In an era where eutrophication has become one of the most pressing environmental issues our society faces, her early work was ahead of its time
— Matt Charette, director of the Coastal Ocean Institute at Woods Hole Oceanographic Institution
The coast, also known as the coastline, shoreline or seashore, is defined as the area where land meets the ocean, or as a line that forms the boundary between the land and the coastline. Shores are influenced by the topography of the surrounding landscape, as well as by water induced erosion, such as waves. The geological composition of rock and soil dictates the type of shore which is created. The Earth has around 620,000 kilometres (390,000 mi) of coastline. Coasts are important zones in natural ecosystems, often home to a wide range of biodiversity. On land, they harbor important ecosystems such as freshwater or estuarine wetlands, which are important for bird populations and other terrestrial animals. In wave-protected areas they harbor saltmarshes, mangroves or seagrasses, all of which can provide nursery habitat for finfish, shellfish, and other aquatic species. Rocky shores are usually found along exposed coasts and provide habitat for a wide range of sessile animals and various kinds of seaweeds. In physical oceanography, a shore is the wider fringe that is geologically modified by the action of the body of water past and present, while the beach is at the edge of the shore, representing the intertidal zone where there is one. Along tropical coasts with clear, nutrient-poor water, coral reefs can often be found between depths of 1–50 meters.
Eutrophication is the process by which an entire body of water, or parts of it, becomes progressively enriched with minerals and nutrients, particularly nitrogen and phosphorus. It has also been defined as "nutrient-induced increase in phytoplankton productivity". Water bodies with very low nutrient levels are termed oligotrophic and those with moderate nutrient levels are termed mesotrophic. Advanced eutrophication may also be referred to as dystrophic and hypertrophic conditions. Eutrophication can affect freshwater or salt water systems. In freshwater ecosystems it is almost always caused by excess phosphorus. In coastal waters on the other hand, the main contributing nutrient is more likely to be nitrogen, or nitrogen and phosphorus together. This depends on the location and other factors.
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world.
Narragansett Bay is a bay and estuary on the north side of Rhode Island Sound covering 147 square miles (380 km2), 120.5 square miles (312 km2) of which is in Rhode Island. The bay forms New England's largest estuary, which functions as an expansive natural harbor and includes a small archipelago. Small parts of the bay extend into Massachusetts.
The spring bloom is a strong increase in phytoplankton abundance that typically occurs in the early spring and lasts until late spring or early summer. This seasonal event is characteristic of temperate North Atlantic, sub-polar, and coastal waters. Phytoplankton blooms occur when growth exceeds losses, however there is no universally accepted definition of the magnitude of change or the threshold of abundance that constitutes a bloom. The magnitude, spatial extent and duration of a bloom depends on a variety of abiotic and biotic factors. Abiotic factors include light availability, nutrients, temperature, and physical processes that influence light availability, and biotic factors include grazing, viral lysis, and phytoplankton physiology. The factors that lead to bloom initiation are still actively debated.
Yaquina Bay is a coastal estuarine community found in Newport, Oregon. Yaquina Bay is a semi-enclosed body of water, approximately 8 km² (3.2 mi²) in area, with free connection to the Pacific Ocean, but also diluted with freshwater from the Yaquina River land drainage. The Bay is traversed by the Yaquina Bay Bridge.
The Coastal and Estuarine Research Federation (CERF) is a private, nonprofit organization created in 1971. At that time, the members of two regionally based organizations, the Atlantic Estuarine Research Society (AERS) and the New England Estuarine Research Society (NEERS) recognized the need for a third estuarine organization that would address national estuarine and coastal issues. Today, CERF is a multidisciplinary federation of members and seven regionally-based Affiliate Societies dedicated to the understanding and wise stewardship of estuaries and coasts worldwide.
Brackish marshes develop from salt marshes where a significant freshwater influx dilutes the seawater to brackish levels of salinity. This commonly happens upstream from salt marshes by estuaries of coastal rivers or near the mouths of coastal rivers with heavy freshwater discharges in the conditions of low tidal ranges.
Acartia hudsonica is a species of marine copepod belonging to the family Acartiidae. Acartia hudsonica is a coastal, cold water species that can be found along the northwest Atlantic coast.
Mangrove ecosystems represent natural capital capable of producing a wide range of goods and services for coastal environments and communities and society as a whole. Some of these outputs, such as timber, are freely exchanged in formal markets. Value is determined in these markets through exchange and quantified in terms of price. Mangroves are important for aquatic life and home for many species of fish.
A marine habitat is a habitat that supports marine life. Marine life depends in some way on the saltwater that is in the sea. A habitat is an ecological or environmental area inhabited by one or more living species. The marine environment supports many kinds of these habitats.
A mesocosm is any outdoor experimental system that examines the natural environment under controlled conditions. In this way mesocosm studies provide a link between field surveys and highly controlled laboratory experiments.
Ceriantheopsis americana is a species of tube-dwelling anemone in the family Cerianthidae. It is a burrowing species and lives in deep sand or muddy sand in a long slender tube that it creates.
Nutrient cycling in the Columbia River Basin involves the transport of nutrients through the system, as well as transformations from among dissolved, solid, and gaseous phases, depending on the element. The elements that constitute important nutrient cycles include macronutrients such as nitrogen, silicate, phosphorus, and micronutrients, which are found in trace amounts, such as iron. Their cycling within a system is controlled by many biological, chemical, and physical processes.
Sybil P. Seitzinger is an oceanographer and climate scientist at the Pacific Institute for Climate Solutions. She is known for her research into climate change and elemental cycling, especially nitrogen biogeochemistry.
Benthic-pelagic coupling are processes that connect the benthic zone and the pelagic zone through the exchange of energy, mass, or nutrients. These processes play a prominent role in both freshwater and marine ecosystems and are influenced by a number of chemical, biological, and physical forces that are crucial to functions from nutrient cycling to energy transfer in food webs.
A marine coastal ecosystem is a marine ecosystem which occurs where the land meets the ocean. Marine coastal ecosystems include many very different types of marine habitats, each with their own characteristics and species composition. They are characterized by high levels of biodiversity and productivity.
Patricia Marguerite Glibert is marine scientist known for her research on nutrient use by phytoplankton and harmful algal blooms in Chesapeake Bay. She is an elected fellow of the American Association for the Advancement of Science.
Robinson W. "Wally" Fulweiler is an American marine biogeochemist.
Scott W. Nixon was an ecosystem ecologist whose research primarily focused on nitrogen and eutrophication in coastal and estuarine ecosystems. He was the first to clearly define coastal eutrophication. Nixon was a faculty member of the University of Rhode Island’s Graduate School of Oceanography from 1969 until his death. Throughout his life, he also served important roles in many organizations and committees, including as the director of Rhode Island Sea Grant, editor-in-chief of Estuaries, and a member of the National Research Council's Ocean Studies Board.