Relevant bibliographies by topics / Estuarine eutrophication – New England

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Estuarine eutrophication – New England'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Estuarine eutrophication – New England"

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Novak, A. B., M. C. Pelletier, P. Colarusso, J. Simpson, M. N. Gutierrez, A. Arias-Ortiz, M. Charpentier, P. Masque, and P. Vella. "Factors Influencing Carbon Stocks and Accumulation Rates in Eelgrass Meadows Across New England, USA." Estuaries and Coasts 43, no. 8 (May 27, 2020): 2076–91. http://dx.doi.org/10.1007/s12237-020-00754-9.

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Abstract Increasing the protection of coastal vegetated ecosystems has been suggested as one strategy to compensate for increasing carbon dioxide (CO2) in the atmosphere as the capacity of these habitats to sequester and store carbon exceeds that of terrestrial habitats. Seagrasses are a group of foundation species that grow in shallow coastal and estuarine systems and have an exceptional ability to sequester and store large quantities of carbon in biomass and, particularly, in sediments. However, carbon stocks (Corg stocks) and carbon accumulation rates (Corg accumulation) in seagrass meadows are highly variable both spatially and temporally, making it difficult to extrapolate this strategy to areas where information is lacking. In this study, Corg stocks and Corg accumulation were determined at 11 eelgrass meadows across New England, representing a range of eutrophication and exposure conditions. In addition, the environmental factors and structural characteristics of meadows related to variation in Corg stocks were identified. The objectives were accomplished by assessing stable isotopes of δ13C and δ15N as well as %C and %N in plant tissues and sediments, measuring grain size and 210Pb of sediment cores, and through assessing site exposure. Variability in Corg stocks in seagrass meadows is well predicted using commonly measured environmental variables such as grain size distribution. This study allows incorporation of data and insights for the northwest Atlantic, where few studies on carbon sequestration by seagrasses have been conducted.
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Rollinson, Veronica R., Julie Granger, Sydney C. Clark, Mackenzie L. Blanusa, Claudia P. Koerting, Jamie M. P. Vaudrey, Lija A. Treibergs, et al. "Seasonality of nitrogen sources, cycling, and loading in a New England river discerned from nitrate isotope ratios." Biogeosciences 18, no. 11 (June 10, 2021): 3421–44. http://dx.doi.org/10.5194/bg-18-3421-2021.

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Abstract. Coastal waters globally are increasingly impacted due to the anthropogenic loading of nitrogen (N) from the watershed. To assess dominant sources contributing to the eutrophication of the Little Narragansett Bay estuary in New England, we carried out an annual study of N loading from the Pawcatuck River. We conducted weekly monitoring of nutrients and nitrate (NO3-) isotope ratios (15N / 14N, 18O / 16O, and 17O / 16O) at the mouth of the river and from the larger of two wastewater treatment facilities (WWTFs) along the estuary, as well as seasonal along-river surveys. Our observations reveal a direct relationship between N loading and the magnitude of river discharge and a consequent seasonality to N loading into the estuary – rendering loading from the WWTFs and from an industrial site more important at lower river flows during warmer months, comprising ∼ 23 % and ∼ 18 % of N loading, respectively. Riverine nutrients derived predominantly from deeper groundwater and the industrial point source upriver in summer and from shallower groundwater and surface flow during colder months – wherein NO3- associated with deeper groundwater had higher 15N / 14N ratios than shallower groundwater. Corresponding NO3- 18O / 16O ratios were lower during the warm season, due to increased biological cycling in-river. Uncycled atmospheric NO3-, detected from its unique mass-independent NO3- 17O / 16O vs. 18O / 16O fractionation, accounted for < 3 % of riverine NO3-, even at elevated discharge. Along-river, NO3- 15N / 14N ratios showed a correspondence to regional land use, increasing from agricultural and forested catchments to the more urbanized watershed downriver. The evolution of 18O / 16O isotope ratios along-river conformed to the notion of nutrient spiraling, reflecting the input of NO3- from the catchment and from in-river nitrification and its coincident removal by biological consumption. These findings stress the importance of considering seasonality of riverine N sources and loading to mitigate eutrophication in receiving estuaries. Our study further advances a conceptual framework that reconciles with the current theory of riverine nutrient cycling, from which to robustly interpret NO3- isotope ratios to constrain cycling and source partitioning in river systems.
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BERTNESS, MARK D., CAITLIN CRAIN, CHRISTINE HOLDREDGE, and NICHOLAS SALA. "Eutrophication and Consumer Control of New England Salt Marsh Primary Productivity." Conservation Biology 22, no. 1 (October 18, 2007): 131–39. http://dx.doi.org/10.1111/j.1523-1739.2007.00801.x.

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Chen, Celia, Darren Ward, Jason Williams, and Nicholas Fisher. "Metal Bioaccumulation by Estuarine Food Webs in New England, USA." Journal of Marine Science and Engineering 4, no. 2 (June 3, 2016): 41. http://dx.doi.org/10.3390/jmse4020041.

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Oczkowski, Autumn, Christopher W. Hunt, Kenneth Miller, Candace Oviatt, Scott Nixon, and Leslie Smith. "Comparing Measures of Estuarine Ecosystem Production in a Temperate New England Estuary." Estuaries and Coasts 39, no. 6 (June 1, 2016): 1827–44. http://dx.doi.org/10.1007/s12237-016-0113-1.

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Brin, Lindsay D., Anne E. Giblin, and Jeremy J. Rich. "Environmental controls of anammox and denitrification in southern New England estuarine and shelf sediments." Limnology and Oceanography 59, no. 3 (May 2014): 851–60. http://dx.doi.org/10.4319/lo.2014.59.3.0851.

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Hughes, Jeffrey E., Linda A. Deegan, Jason C. Wyda, Melissa J. Weaver, and Amos Wright. "The effects of eelgrass habitat loss on estuarine fish communities of southern New England." Estuaries 25, no. 2 (April 2002): 235–49. http://dx.doi.org/10.1007/bf02691311.

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Shawler, Justin L., Christopher J. Hein, Elizabeth A. Canuel, James M. Kaste, Gregory G. Fitzsimons, Ioannis Y. Georgiou, and Debra A. Willard. "Tidal erosion and upstream sediment trapping modulate records of land-use change in a formerly glaciated New England estuary." Anthropocene Coasts 2, no. 1 (January 1, 2019): 340–61. http://dx.doi.org/10.1139/anc-2018-0034.

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Land clearing, river impoundments, and other human modifications to the upland landscape and within estuarine systems can drive coastal change at local to regional scales. However, as compared with mid-latitude coasts, the impacts of human modifications along sediment-starved formerly glaciated coastal landscapes are relatively understudied. To address this gap, we present a late-Holocene record of changing sediment accumulation rates and sediment sources from sediment cores collected across a tidal flat in the Merrimack River estuary (Mass., USA). We pair sedimentology, geochronology, bulk- and stable-isotope organic geochemistry, and hydrodynamic simulations with historical data to evaluate human and natural impacts on coastal sediment fluxes. During the 17th to 19th centuries, accumulation rates increased by an order of magnitude in the central tidal flat, likely in response to enhanced delivery of terrestrial sediment resulting from upland deforestation. However, the overall increase in accumulation (0.56–2.6 mm/year) within the estuary is subtle and spatially variable across the tidal flats because of coincident anthropogenic land clearing and dam building, upland sediment storage, and estuarine hydrodynamics. This study provides insight into the response of formerly glaciated fluvial-coastal systems to human modifications, and underscores the role of estuarine environmental conditions in modifying upland signals of land-use change.
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Chun, K., M. J. Weaver, and L. A. Deegan. "Assessment of Fish Communities in New England Embayments: Application of the Estuarine Biotic Integrity Index." Biological Bulletin 191, no. 2 (October 1996): 320–21. http://dx.doi.org/10.1086/bblv191n2p320.

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Paul, John F., Randy L. Comeleo, and Jane Copeland. "Landscape Metrics and Estuarine Sediment Contamination in the Mid-Atlantic and Southern New England Regions." Journal of Environment Quality 31, no. 3 (2002): 836. http://dx.doi.org/10.2134/jeq2002.0836.

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Dissertations / Theses on the topic "Estuarine eutrophication – New England"

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Pospelova, Vera. "Dinoflagellate cyst assemblages and environmental factors controlling their distribution in New England (USA) estuaries." Thesis, McGill University, 2003. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=19559.

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Extensive data sets of water quality and sediment chemistry as well as detailed historical records were used to analyze environmental factors controlling dinoflagellate cyst distribution in shallow estuaries (lagoons and embayments) of southern New England. Cyst abundance, species richness, the proportion of cysts produced by heterotrophic and autotrophic dinoflagellates, and the composition of cyst assemblages reflect spatial and temporal variation in environmental conditions. The cyst record in sediment cores from two embayments, New Bedford Harbor and Apponagansett Bay, Massachusetts demonstrates cyst sensitivity to environmental change caused by anthropogenic activity in the watersheds. Intensive industrialization and urbanization occurred during the 20th century in New Bedford Harbor resulted in extreme eutrophication and toxic pollution (heavy metals and PCBs). These conditions are reflected in declining cyst diversity and wide fluctuation in total cyst production. At the same time, the proportion of certain heterotrophic taxa increases. As impacts of extreme eutrophication and toxic pollution cannot be separated, the cyst response must be interpreted as a cumulative «pollution signal». The spatial distribution of modern dinoflagellate cysts in the area supports this signal. Cysts vary along gradients of nutrient enrichment, corresponding to distance from sewage outfalls. Dinoflagellate cysts in surface sediments from New England lagoons also were studied. A comparison of assemblages to water quality parameters, that are affected greatly by the degree of water exchange between lagoon and ocean, indicates that temperature and salinity are the main abiotic factors controlling cyst distribution in these estuaries. A new species of dinoflagellate cyst, Islandinium brevispinosum, has been identified and described. This species was found within a narrow range of water temperature and salinity, and at elevated nutrient levels. Dinoflagellate cysts reflect environmental conditions at the small spatial scales necessary to characterize variability within estuaries. However, the relative importance of abiotic factors controlling the spatial and temporal distribution of dinoflagellate cysts is likely to vary with the hydrological differences between lagoons and embayments. Therefore, dinoflagellate cysts can be useful indicators of environmental conditions in and human impacts on shallow estuaries.
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Keith, Darryl Joel. "Determination of chlorophyll a concentrations and phytoplankton primary production in New England estuarine waters using ocean color remote sensing from low-flying aircraft /." View online ; access limited to URI, 2004. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3145421.

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Kennedy, Cristina. "Habitat Heterogeneity Concentrates Predators in the Seascape: Linking Intermediate-Scale Estuarine Habitat to Striped Bass Distribution." 2013. https://scholarworks.umass.edu/theses/1050.

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Predators are key components of aquatic ecosystems and innovative approaches to understanding their spatial distribution are imperative for research, effective management, and conservation. Discontinuities, created by abrupt changes between two unlike entities, are irregularly-distributed, intermediate-scale features that can have a disproportionate effect on organismal distribution within the seascape. Here I use the discontinuity concept to relate the distribution of a predator, striped bass (Morone saxatilis), to physical features within Plum Island Estuary (PIE), MA. I mapped the distribution of 50 acoustically-tagged striped bass during four monthly surveys at 40 sites to evaluate if heterogeneity in physical features concentrated predators. All striped bass survived tagging, were coastal migrants, displayed seasonal residency within PIE, and moved freely throughout the estuary. However, these highly mobile predators were not evenly distributed. Specifically, striped bass were clustered in the middle region of PIE in response to sandbar area, intermediate bottom unevenness, channel networks, and, to a lesser extent, confluences and drop-offs. The highest predator counts occurred at sites with the greatest additive habitat complexity. I measured 23 geomorphic metrics at 40 sites within the seascape to characterize the spatial patterns of confluences, drop-offs, bathymetry and land features. Then, I mapped integrated measurements of multimetric physical features to reveal distinct spatial trends in physical complexity of the estuary. By expanding the discontinuity concept and combining irregularly-distributed, intermediate-scale physical features with smaller-scale, traditional fish habitat methodologies, I revealed consistent and ecologically-meaningful patterns within a north temperate estuarine seascape.
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Marsters, Roger Sidney. "Approaches to Empire: Hydrographic Knowledge and British State Activity in Northeastern North America, 1711-1783." 2012. http://hdl.handle.net/10222/15823.

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This dissertation studies the intersection of knowledge, culture, and power in contested coastal and estuarine space in eighteenth-century northeastern North America. It examines the interdependence of vernacular pilot knowledge and directed hydrographic survey, their integration into practices of warfare and governance, and roles in assimilating American space to metropolitan scientific and aesthetic discourses. It argues that the embodied skill and local knowledge of colonial and Aboriginal peoples served vital and underappreciated roles in Great Britain’s extension of overseas activity and interest, of maritime empire. It examines the maritimicity of empire: empire as adaptation to marine environments through which it conducted political influence and commercial endeavour. The materiality of maritime empire—its reliance on patterns of wind and current, on climate and weather, on local relations of sea to land, on proximity of spaces and resources to oceanic circuits—framed and delimited transnational flows of commerce and state power. This was especially so in coastal and riverine littoral spaces of northeastern North America. In this local Atlantic, pilot knowledge—and its systematization in marine cartography through hydrographic survey—adapted processes of empire to the materiality of the maritime, and especially to the littoral, environment. Eighteenth-century British state agents acting in northeastern North America—in Mi’kmaqi/Acadia/Nova Scotia, Newfoundland and Labrador, Quebec, and New England—developed new means of adapting this knowledge to the tasks of maritime empire, creating potent tools with which to extend Britain’s imperial power and influence amphibiously in the eighteenth and nineteenth centuries. If the open Atlantic became a maritime highway in this period, traversed with increasing frequency and ease, inshore waters remained dangerous bypaths, subject to geographical and meteorological hazards that checked overseas commercial exchange and the military and administrative processes that constituted maritime empire. While patterns of oceanic circulation permitted extension of these activities globally in the early modern period, the complex interrelation of marine and terrestrial geography and climate in coastal and estuarine waters long set limits on maritime imperial activity. This dissertation examines the nature of these limits, and the means that eighteenth-century British commercial and imperial actors developed to overcome them.
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Books on the topic "Estuarine eutrophication – New England"

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A, Orson Richard, and Connecticut Sea Grant College Program., eds. Research in New England marsh-estuarine ecosystems: Directions and priorities into the next millenium ; summary of a New England Sea Grant workshop, May 15-17, 1997, Connecticut College, New London, Connecticut ... Groton, CT (1084 Shennecossett Rd., Groton 06340-6097): Connecticut Sea Grant College Program, 1998.

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Book chapters on the topic "Estuarine eutrophication – New England"

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"Fish Habitat: Essential Fish Habitat and Rehabilitation." In Fish Habitat: Essential Fish Habitat and Rehabilitation, edited by Anthony R. Wilbur and Michael W. Pentony. American Fisheries Society, 1999. http://dx.doi.org/10.47886/9781888569124.ch22.

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<em>Abstract</em> .—New England aquatic, estuarine, and marine environments are highly variable and present distinct habitat features that support a number of commercial, recreational, and nontarget organisms. The heterogeneous environmental conditions found throughout New England provide important habitat characteristics for the reproduction, development, growth, feeding, and sustainability of fishery resources. Organisms have specific ontogenetic requirements that demonstrate their evolutionary adaptation to particular riverine, inshore, and offshore habitats. Habitat alteration and disturbance occur due to natural processes and human activities. Human-induced chemical, biological, and physical threats to habitat can have direct and indirect effects on local fish and mollusk populations. Increases in coastal development and humangenerated pollutants entering the environment are major threats to marine and aquatic habitats and are a result of increasing human population. Human activities and direct habitat alteration (e.g., hydrologic modifications) can disrupt environmental processes and conditions, and pollutants are discharged from a variety of nonpoint and point sources including runoff and industrial discharge, respectively. The sustainability of fishery resources in the New England region depends upon the protection of essential fish habitat. This protection includes identifying and understanding all potential nonfishing threats, point and nonpoint pollutant sources, and anthropogenic activities and impacts.
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"Fish Habitat: Essential Fish Habitat and Rehabilitation." In Fish Habitat: Essential Fish Habitat and Rehabilitation, edited by Anthony R. Wilbur and Michael W. Pentony. American Fisheries Society, 1999. http://dx.doi.org/10.47886/9781888569124.ch22.

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<em>Abstract</em> .—New England aquatic, estuarine, and marine environments are highly variable and present distinct habitat features that support a number of commercial, recreational, and nontarget organisms. The heterogeneous environmental conditions found throughout New England provide important habitat characteristics for the reproduction, development, growth, feeding, and sustainability of fishery resources. Organisms have specific ontogenetic requirements that demonstrate their evolutionary adaptation to particular riverine, inshore, and offshore habitats. Habitat alteration and disturbance occur due to natural processes and human activities. Human-induced chemical, biological, and physical threats to habitat can have direct and indirect effects on local fish and mollusk populations. Increases in coastal development and humangenerated pollutants entering the environment are major threats to marine and aquatic habitats and are a result of increasing human population. Human activities and direct habitat alteration (e.g., hydrologic modifications) can disrupt environmental processes and conditions, and pollutants are discharged from a variety of nonpoint and point sources including runoff and industrial discharge, respectively. The sustainability of fishery resources in the New England region depends upon the protection of essential fish habitat. This protection includes identifying and understanding all potential nonfishing threats, point and nonpoint pollutant sources, and anthropogenic activities and impacts.
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"Fish Habitat: Essential Fish Habitat and Rehabilitation." In Fish Habitat: Essential Fish Habitat and Rehabilitation, edited by David B. Packer and Tom Hoff. American Fisheries Society, 1999. http://dx.doi.org/10.47886/9781888569124.ch8.

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<em>Abstract.</em> —To satisfy the essential fish habitat (EFH) mandate of the reauthorized Magnuson-Stevens Fishery Conservation and Management Act, the Mid-Atlantic Fishery Management Council (MAFMC) and the National Marine Fisheries Service (NMFS) are developing objective, generic criteria to describe and identify the essential habitats for their managed species. Summer flounder or fluke <em>Paralichthys dentatus </em> is an important commercial and recreational species that occurs from shallow estuaries to the outer continental shelf from Nova Scotia to Florida. It is most abundant within the Middle Atlantic Bight from New England to Cape Hatteras, and this region is the focus of this paper. Summer flounder make seasonal inshore–offshore migrations; adults and juveniles normally inhabit shallow coastal and estuarine waters during the warmer months of the year and mostly move offshore with declining water temperature and day length during autumn. Adults spawn during the fall and winter migrations. The best habitat information available on summer flounder is for the estuarinedependent transforming larvae and juveniles. They use several different estuarine habitats as nursery areas, including salt-marsh creeks, sea grass beds, mudflats, and open bay areas. In these habitats, water temperature affects the seasonal occurrence of summer flounder, drives the inshore–offshore migration, and, particularly during winter and spring, affects first-year growth and survival and thus subsequent year-class strength. The distribution of transforming larvae and juveniles within the estuaries is significantly influenced by salinity gradients and substrate. Transforming larvae and juveniles show a preference for sandy substrates in the laboratory but also have been captured on mud or mixed substrates. Juveniles are attracted to eelgrass and macroalgae habitats because of the presence of prey but remain in nearby sand to avoid predators as well as conceal themselves from the prey. The MAFMC used the life history and habitat parameter information developed by the NMFS Northeast Fisheries Science Center (NEFSC) to precisely describe the EFH of summer flounder by life stage. Because summer flounder are overexploited, the MAFMC wanted to be conservative in its EFH identification. Therefore, 90% of the areas where each life history stage has been collected from offshore surveys were identified as EFH. The MAFMC proposed that 100% of the estuaries where larvae and juveniles were identified as being present be identified as EFH because these life stages are estuarine dependent. Nursery habitats within the estuaries are essential because they provide the best conditions for growth and survival of the transforming larvae and juveniles. Submerged aquatic vegetation beds are especially vulnerable and were identified as habitat areas of particular concern. As more habitatrelated density data become available from various local, state, and federal fishery-independent surveys, updated maps of distribution and abundance will be produced.
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"Fish Habitat: Essential Fish Habitat and Rehabilitation." In Fish Habitat: Essential Fish Habitat and Rehabilitation, edited by David B. Packer and Tom Hoff. American Fisheries Society, 1999. http://dx.doi.org/10.47886/9781888569124.ch8.

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<em>Abstract.</em> —To satisfy the essential fish habitat (EFH) mandate of the reauthorized Magnuson-Stevens Fishery Conservation and Management Act, the Mid-Atlantic Fishery Management Council (MAFMC) and the National Marine Fisheries Service (NMFS) are developing objective, generic criteria to describe and identify the essential habitats for their managed species. Summer flounder or fluke <em>Paralichthys dentatus </em> is an important commercial and recreational species that occurs from shallow estuaries to the outer continental shelf from Nova Scotia to Florida. It is most abundant within the Middle Atlantic Bight from New England to Cape Hatteras, and this region is the focus of this paper. Summer flounder make seasonal inshore–offshore migrations; adults and juveniles normally inhabit shallow coastal and estuarine waters during the warmer months of the year and mostly move offshore with declining water temperature and day length during autumn. Adults spawn during the fall and winter migrations. The best habitat information available on summer flounder is for the estuarinedependent transforming larvae and juveniles. They use several different estuarine habitats as nursery areas, including salt-marsh creeks, sea grass beds, mudflats, and open bay areas. In these habitats, water temperature affects the seasonal occurrence of summer flounder, drives the inshore–offshore migration, and, particularly during winter and spring, affects first-year growth and survival and thus subsequent year-class strength. The distribution of transforming larvae and juveniles within the estuaries is significantly influenced by salinity gradients and substrate. Transforming larvae and juveniles show a preference for sandy substrates in the laboratory but also have been captured on mud or mixed substrates. Juveniles are attracted to eelgrass and macroalgae habitats because of the presence of prey but remain in nearby sand to avoid predators as well as conceal themselves from the prey. The MAFMC used the life history and habitat parameter information developed by the NMFS Northeast Fisheries Science Center (NEFSC) to precisely describe the EFH of summer flounder by life stage. Because summer flounder are overexploited, the MAFMC wanted to be conservative in its EFH identification. Therefore, 90% of the areas where each life history stage has been collected from offshore surveys were identified as EFH. The MAFMC proposed that 100% of the estuaries where larvae and juveniles were identified as being present be identified as EFH because these life stages are estuarine dependent. Nursery habitats within the estuaries are essential because they provide the best conditions for growth and survival of the transforming larvae and juveniles. Submerged aquatic vegetation beds are especially vulnerable and were identified as habitat areas of particular concern. As more habitatrelated density data become available from various local, state, and federal fishery-independent surveys, updated maps of distribution and abundance will be produced.
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Conference papers on the topic "Estuarine eutrophication – New England"

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Spaulding, Malcolm L., E. Howlett, M. Ward, and C. Galagan. "COASTMAP: A Globally Re-Locatable, Real Time Marine environmental Monitoring and Modeling System, with Application to Narragansett Bay and Southern New England Coastal Waters." In Eighth International Conference on Estuarine and Coastal Modeling. Reston, VA: American Society of Civil Engineers, 2004. http://dx.doi.org/10.1061/40734(145)1.

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Shawler, Justin L., and Christopher J. Hein. "ESTUARINE RECORDS OF LONG-TERM HUMAN IMPACTS ON FLUVIAL SEDIMENT DISCHARGE FROM A LARGE NEW ENGLAND RIVER." In 65th Annual Southeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016se-273677.

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Oakley, Bryan A., James D. Turenne, Joshua Bartosiewicz, Robert J. Hollis, Jonathan D. Alvarez, Mark Borrelli, and Jon C. Boothroyd. "MAPPING BENTHIC GEOLOGIC HABITAT IN SHALLOW ESTUARINE AND LAGOON ENVIRONMENTS: CASE STUDIES, EXPERIENCE AND RESULTS FROM SOUTHERN NEW ENGLAND." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-271962.

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