963 resultados para U-addition RNA editing


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The United States and Japanese counterpart panels on aquaculture were formed in 1969 under the United States-Japan Cooperative Program in Natural Resources (UJNR). The panels currently include specialists drawn from the federal departments most concerned with aquaculture. Charged with exploring and developing bilateral cooperation, the panels have focused their efforts on exchanging information related to aquaculture which could be of benefit to both countries. The UJNR was started by a proposal made during the Third Cabinet-Level Meeting of the Joint United States-Japan Committee on Trade and Economic Affairs in January 1964. In addition to aquaculture, current subjects in the program are desalination of seawater, toxic microorganisms, air pollution, energy, forage crops, national park management, mycoplasmosis, wind and seismic effects, protein resources, forestry, and several joint panels and committees in marine resources research, development, and utilization. Accomplishments include: Increased communications and cooperation among technical specialists; exchanges of information, data, and research findings; annual meetings of the panels, a policy coordinative body; administrative staff meetings; exchanges of equipment, materials, and samples; several major technical conferences; and beneficial effects on international relations. (PDF file contains 108 pages.)

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The United States and Japanese counterpart panels on aquaculture were formed in 1969 under the United States-Japan Cooperative Program in Natural Resources (UJNR). The panels currently include specialists drawn from the federal departments most concerned with aquaculture. Charged with exploring and developing bilateral cooperation, the panels have focused their efforts on exchanging information related to aquaculture which could be of benefit to both countries. The UJNR was started by a proposal made during the Third Cabinet-Level Meeting of the Joint United States-Japan Committee on Trade and Economic Affairs in January 1964. In addition to aquaculture, current subjects in the program are desalination of seawater, toxic microorganisms, air pollution, energy, forage crops, national park management, mycoplasmosis, wind and seismic effects, protein resources, forestry, and several joint panels and committees in marine resources research, development, and utilization. Accomplishments include: Increased communications and cooperation among technical specialists; exchanges of information, data, and research findings; annual meetings of the panels, a policy coordinative body; administration staff meetings; exchanges of equipment, materials, and samples; several major technical conferences; and beneficial effects on international relations. (PDF file contains 98 pages.)

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The United States and Japanese counterpart panels on aquaculture were formed in 1969 under the United States-Japan Cooperative Program in Natural Resources (UJNR). The panels currently include specialists drawn from the federal departments most concerned with aquaculture. Charged with exploring and developing bilateral cooperation, the panels have focused their efforts on exchanging information related to aquaculture which could be of benefit to both countries. The UJNR was started by a proposal made during the Third Cabinet-Level Meeting of the Joint United States-Japan Committee on Trade and Economic Affairs in January 1964. In addition to aquaculture, current subjects in the program are desalination of seawater, toxic microorganisms, air pollution, energy, forage crops, national park management, mycoplasmosis, wind and seismic effects, protein resources, forestry, and several joint panels and committees in marine resources research, development, and utilization. Accomplishments include: Increased communications and cooperation among technical specialists; exchanges of information, data, and research findings; annual meetings of the panels, a policy coordinative body;' administration staff meetings; exchanges of equipment, materials, and samples; several major technical conferences; and beneficial effects on international relations.(PDF file contains 37 pages.)

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Early embryogenesis in metazoa is controlled by maternally synthesized products. Among these products, the mature egg is loaded with transcripts representing approximately two thirds of the genome. A subset of this maternal RNA pool is degraded prior to the transition to zygotic control of development. This transfer of control of development from maternal to zygotic products is referred to as the midblastula transition (or MBT). It is believed that the degradation of maternal transcripts is required to terminate maternal control of development and to allow zygotic control of development to begin. Until now this process of maternal transcript degradation and the subsequent timing of the MBT has been poorly understood. I have demonstrated that in the early embryo there are two independent RNA degradation pathways, either of which is sufficient for transcript elimination. However, only the concerted action of both pathways leads to elimination of transcripts with the correct timing, at the MBT. The first pathway is maternally encoded, is triggered by egg activation, and is targeted to specific classes of mRNAs through cis-acting elements in the 3' untranslated region (UTR}. The second pathway is activated 2 hr after fertilization and functions together with the maternal pathway to ensure that transcripts are degraded by the MBT. In addition, some transcripts fail to degrade at select subcellular locations adding an element of spatial control to RNA degradation. The spatial control of RNA degradation is achieved by protecting, or masking, transcripts from the degradation machinery. The RNA degradation and protection events are regulated by distinct cis-elements in the 3' untranslated region (UTR). These results provide the first systematic dissection of this highly conserved process in development and demonstrate that RNA degradation is a novel mechanism used for both temporal and spatial control of development.

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Part I. Proton Magnetic Resonance of Polynucleotides and Transfer RNA.

Proton magnetic resonance was used to follow the temperature dependent intramolecular stacking of the bases in the polynucleotides of adenine and cytosine. Analysis of the results on the basis of a two state stacked-unstacked model yielded values of -4.5 kcal/mole and -9.5 kcal/mole for the enthalpies of stacking in polyadenylic and polycytidylic acid, respectively.

The interaction of purine with these molecules was also studied by pmr. Analysis of these results and the comparison of the thermal unstacking of polynucleotides and short chain nucleotides indicates that the bases contained in stacks within the long chain poly nucleotides are, on the average, closer together than the bases contained in stacks in the short chain nucleotides.

Temperature and purine studies were also carried out with an aqueous solution of formylmethionine transfer ribonucleic acid. Comparison of these results with the results of similar experiments with the homopolynucleotides of adenine, cytosine and uracil indicate that the purine is probably intercalating into loop regions of the molecule.

The solvent denaturation of phenylalanine transfer ribonucleic acid was followed by pmr. In a solvent mixture containing 83 volume per cent dimethylsulf oxide and 17 per cent deuterium oxide, the tRNA molecule is rendered quite flexible. It is possible to resolve resonances of protons on the common bases and on certain modified bases.

Part II. Electron Spin Relaxation Studies of Manganese (II) Complexes in Acetonitrile.

The electron paramagnetic resonance spectra of three Mn+2 complexes, [Mn(CH3CN)6]+2, [MnCl4]-2, and [MnBr4]-2, in acetonitrile were studied in detail. The objective of this study was to relate changes in the effective spin Hamiltonian parameters and the resonance line widths to the structure of these molecular complexes as well as to dynamical processes in solution.

Of the three systems studied, the results obtained from the [Mn(CH3CN)6]+2 system were the most straight-forward to interpret. Resonance broadening attributable to manganese spin-spin dipolar interactions was observed as the manganese concentration was increased.

In the [MnCl4]-2 system, solvent fluctuations and dynamical ion-pairing appear to be significant in determining electron spin relaxation.

In the [MnBr4]-2 system, solvent fluctuations, ion-pairing, and Br- ligand exchange provide the principal means of electron spin relaxation. It was also found that the spin relaxation in this system is dependent upon the field strength and is directly related to the manganese concentration. A relaxation theory based on a two state collisional model was developed to account for the observed behavior.

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Part I. The cellular slime mold Dictyostelium discoideum is a simple eukaryote which undergoes a multi-cellular developmental process. Single cell myxamoebae divide vegetatively in the presence of a food source. When the food is depleted or removed, the cells aggregate, forming a migrating pseudoplasmodium which differentiates into a fruiting body containing stalk and spore cells. I have shown that during the developmental cycle glycogen phosphorylase, aminopeptidase, and alanine transaminase are developmentally regulated, that is their specific activities increased at a specific time in the developmental cycle. Phosphorylase activity is undetectable in developing cells until mid-aggregation whereupon it increases and reaches a maximum at mid-culmination. Thereafter the enzyme disappears. Actinomycin D and cycloheximide studies as well as studies with morphologically aberrant and temporally deranged mutants indicate that prior RNA and concomitant protein synthesis are necessary for the rise and decrease in activity and support the view that the appearance of the enzyme is regulated at the transcriptional level. Aminopeptidase and alanine transaminase increase 3 fold starting at starvation and reach maximum activity at 18 and 5 hours respectively.

The cellular DNA s of D. discoideum were characterized by CsC1 buoyant density gradient centrifugation and by renaturation kinetics. Whole cell DNA exhibits three bands in CsCl: ρ = 1.676 g/cc (nuclear main band), 1.687 (nuclear satellite), and 1.682 (mitochondrial). Reassociation kinetics at a criterion of Tm -23°C indicates that the nuclear reiterated sequences make up 30% of the genome (Cot1/2 (pure) 0.28) and the single-copy DNA 70% (Cot1/2(pure) 70). The complexity of the nuclear genome is 30 x 109 daltons and that of the mitochondrial DNA is 35-40 x 106 daltons (Cot1/2 0.15). rRNA cistrons constitute 2.2% of nuclear DNA and have a ρ = 1.682.

RNA extracted from 4 stages during developmental cycle of Dictyostelium was hybridized with purified single-copy nuclear DNA. The hybrids had properties indicative of single-copy DNA-RNA hybrids. These studies indicate that there are, during development, qualitative and quantitative changes in the portion of the single-copy of the genome transcribed. Overall, 56% of the genome is represented by transcripts between the amoeba and mid-culmination stages. Some 19% are sequences which are represented at all stages while 37% of the genome consists of stage specific sequences.

Part II. RNA and protein synthesis and polysome formation were studied during early development of the surf clam Spisula solidissima embryos. The oocyte has a small number of polysomes and a low but measurable rate of protein synthesis (leucine-3H incorporation). After fertilization, there is a continual increase in the percentage of ribosomes sedimenting in the polysome region. Newly synthesized RNA (uridine-5-3H incorporation) was found in polysomes as early as the 2-cell stage. During cleavage, the newly formed RNA is associated mainly with the light polysomes.

RNA extracted from polysomes labeled at the 4-cell stage is polydisperse, nonribosomal, and non-4 S. Actinomycin D causes a reduction of about 30% of the polysomes formed between fertilization and the 16-cell stage.

In the early cleavage stages the light polysomes are mostly affected by actinomycin.

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Part I. Complexes of Biological Bases and Oligonucleotides with RNA

The physical nature of complexes of several biological bases and oligonucleotides with single-stranded ribonucleic acids have been studied by high resolution proton magnetic resonance spectroscopy. The importance of various forces in the stabilization of these complexes is also discussed.

Previous work has shown that purine forms an intercalated complex with single-stranded nucleic acids. This complex formation led to severe and stereospecific broadening of the purine resonances. From the field dependence of the linewidths, T1 measurements of the purine protons and nuclear Overhauser enhancement experiments, the mechanism for the line broadening was ascertained to be dipole-dipole interactions between the purine protons and the ribose protons of the nucleic acid.

The interactions of ethidium bromide (EB) with several RNA residues have been studied. EB forms vertically stacked aggregates with itself as well as with uridine, 3'-uridine monophosphate and 5'-uridine monophosphate and forms an intercalated complex with uridylyl (3' → 5') uridine and polyuridylic acid (poly U). The geometry of EB in the intercalated complex has also been determined.

The effect of chain length of oligo-A-nucleotides on their mode of interaction with poly U in D20 at neutral pD have also been studied. Below room temperatures, ApA and ApApA form a rigid triple-stranded complex involving a stoichiometry of one adenine to two uracil bases, presumably via specific adenine-uracil base pairing and cooperative base stacking of the adenine bases. While no evidence was obtained for the interaction of ApA with poly U above room temperature, ApApA exhibited complex formation of a 1:1 nature with poly U by forming Watson-Crick base pairs. The thermodynamics of these systems are discussed.

Part II. Template Recognition and the Degeneracy of the Genetic Code

The interaction of ApApG and poly U was studied as a model system for the codon-anticodon interaction of tRNA and mRNA in vivo. ApApG was shown to interact with poly U below ~20°C. The interaction was of a 1:1 nature which exhibited the Hoogsteen bonding scheme. The three bases of ApApG are in an anti conformation and the guanosine base appears to be in the lactim tautomeric form in the complex.

Due to the inadequacies of previous models for the degeneracy of the genetic code in explaining the observed interactions of ApApG with poly U, the "tautomeric doublet" model is proposed as a possible explanation of the degenerate interactions of tRNA with mRNA during protein synthesis in vivo.

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Escherichia coli enteroagregativa (EAEC) é um patógeno relacionado ao desenvolvimento de quadros de diarréia aguda ou persistente. A resposta inflamatória induzida por EAEC está relacionada à liberação de interleucina 8, que atua estimulando a transmigração de neutrófilos através do epitélio. Os macrófagos, de forma similar aos neutrófilos, são células fagocíticas que produzem espécies reativas de oxigênio (ERO), como o peróxido de hidrogênio (H2O2). Neste trabalho, avaliamos as consequências da interação de diferentes cepas clínicas com macrófagos humanos ativados da linhagem U-937. Todas as cepas testadas apresentaram filamentos nos testes de aderência aos macrófagos, diferentemente do que ocorre na interação com outras linhagens celulares como HEp-2, T84 e Caco-2. O ferro é um microelemento essencial para bactérias, sendo utilizado como cofator de enzimas e que também pode participar da geração de ERO através da reação de Fenton. Considerando-se a possibilidade de que o H2O2 produzido pelos macrófagos possa gerar radical hidroxil através da reação de Fenton, testes de aderência foram realizados com as amostras cultivadas na presença do captador de ferro 2,2-dipiridil. Tal fato não suprimiu a formação de filamentos, entretanto diminuiu a aderência das cepas EAEC 042 e 17-2. Com o objetivo de produzir uma resposta adaptativa ao H2O2, as culturas bacterianas foram pré-tratadas com uma dose sub-letal de H2O2 por 60 minutos antes de aderirem aos macrófagos. Nossos resultados mostraram que o pré-tratamento também não inibiu o aparecimento de filamentos em relação às culturas não tratadas. Além disto, foi observado que o pré-tratamento com o H2O2 reduziu a aderência das amostras de EAEC ao tapete celular. A filamentação é uma das respostas SOS, induzida pela presença de danos e/ou bloqueio na síntese da molécula de DNA. Com o objetivo de verificar se o H2O2 produzido pelos macrófagos estaria causando danos induzindo o sistema SOS e a filamentação bacteriana, foram realizados testes de viabilidade com mutantes derivados de E. coli K12 deficientes em enzimas do reparo por excisão de bases (BW535) e na resposta SOS (DM49). Nossos resultados mostram que os mutantes apresentaram os níveis de sobrevivência semelhantes ao observado para cepa selvagem isogênica (AB1157). Todos estes resultados em conjunto indicam que o H2O2 não é o indutor da filamentação nos testes de aderência. Macrófagos ativados apresentam ação microbicida através da ação da enzima indolamina dioxigenase (IDO), associada à redução do aminoácido L-triptofano. Desta forma, realizamos testes qualitativos de aderência de EAEC aos macrófagos suplementando o meio de interação com este aminoácido. Nossos resultados mostram que a adição de triptofano ao meio de interação reduz o número de filamentos por campo. Desta forma, aventamos a hipótese de que a depleção do triptofano seja responsável pela indução de resposta SOS, tendo como conseqüência a filamentação das bactérias.

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A comparação entre o Complexo Juiz de Fora e a Unidade Granulítica Ponte de Zinco (Mangaratiba - RJ) revelou que existem diferenças significativas entre essas unidades. Na Unidade Granulítica Ponte de Zinco, são encontrados ortogranulitos de composição granítica e granodiorítica, que representam o embasamento da Unidade, denominada aqui de Ortogranulitos Ribeirão das Lajes. Dois outros litotipos ortoderivados também foram encontrados: (i) um ortognaisse com granada (MAN-JEF-03a), sendo que a granada ocorre de forma subordinada; (ii) ortognaisse leucocrático (MAN-JEF-04), com características miloníticas. Além dessas, rochas metassedimentares também afloram na Unidade Granulítica Ponte de Zinco. Foi interpretado que um ortogranulito (MAN-JEF-01a) de alto-K, com composição monzogranítica, cristalizou em ca. 2653 37 Ma (U-Pb em zircão por LA-ICPMS), afetado por um evento no Neoproterozóico, que gerou os minerais máficos hidratados, observados na análise petrográfica e como mostram as borda de sobrecrescimento em zircão. Sua idade modelo de Nd de 2,7 Ga e seu εNd positivo de +2,1, apontam para uma gênese mantélica, tendo assimilado rochas crustais, pois são encontrados grãos de zircão herdados de aproximadamente 2996 17 Ma e 3343 3.8 Ma. Os dados de litogeoquímica e sua razão 87Sr/86 Sr(t) (0,70529), são compatíveis com uma geração em um arco continental. O ortognaisses com granada do ponto MAN-JEF-03 possui composição granodiorítica. A idade de cristalização interpretada pela análise geocronológica U-Pb em zircão (LA-ICPMS), foi ca. 2117 15 Ma. Esse litotipo foi metamorfizado no Neoproterozóico, sendo a idade obtida pelo intercepto inferior de 631 40 Ma. Seus dados isotópicos apontam para uma rocha juvenil gerada a partir do manto (TDM ≈ de 2,1 Ga e εNd = +3,4). Sua alta razão 87Sr/86 Sr(t) (0,710 ) juntamente com os grãos de zircão herdados (2,6 Ga) e a presença de enclaves, indicam assimilação de rochas crustais. O ortognaisse leucocrático (MAN-JEF-04) classificado como alto-K, possui composição monzogranítica, idade 2132 9,4 Ma U-Pb em zircão (LA-ICPMS). Um único grão relíquiar de ortopiroxênio encontrado em lâmina, , indica que a rocha já foi submetida a metamorfismo de fácies granulito, porém esse evento não deixou registro nos grãos analisados. O retrometamorfismo pode ter ocorrido em dois momentos, 647 11 Ma e 595 38 Ma, calculados através da concordia age, em sobrecrescimentos homogêneos e, pelo intercepto inferior, respectivamente. Sua baixa razão 87Sr/86 Sr(t) (≈ 0,703) associada com εNd positivo (+2,3) e sua idade modelo de aproximadamente 2,1 Ga, revelam que a rocha foi formada por um material mantélico juvenil. Já as análises geocronológicas em U-Pb em zircão (LA-ICPMS) na região de Juiz de Fora (MG), revelaram a existência de dois litotipos Arqueanos: um ortogranulito granodiorítico (MB-JEF-01b), de baixo-K com idade de 2849 11 Ma e com herança de 2975 10 Ma. Seu εNd positivo (+5,9) aponta para uma gênese a partir do manto depletado, já sua alta razão 87Sr/86Sr(t) (≈0,709) indica contaminação de Rb de fontes externas, talvez causada pela assimilação da crosta, como revelam os zircões herdados e/ou fluidos retrometamorficos. Outro litotipo é uma rocha gabróica do tipo E-MORB, cuja idade foi calculada em 2691 14 Ma, com retrometamorfismo ocorrido no intervalo de 604 67 Ma, obtida pelo intercepto inferior. Seu εNd igual a +3,4 e sua razão 87Sr/86 Sr(t) (≈0,701) mostram extração a partir do manto depletado. Novos dados isotópicos do CJF na região de Três Rios (RJ) e Juiz de Fora (MG), sugerem que os ortogranulitos calcioalcalinos podem representar grupos distintos. Rochas com εNd positivos são consequentemente associadas ao manto depletado, porém rochas com εNd negativos devem ter sido geradas por fusão crustal, que podem ser fusão de crosta inferior, devido a razão 87Sr/86 Sr(t) (0,70514) encontrada no amostra MB-JEF-02a (ortogranulito de alto-K) ou tendo a crosta contribuição nas gênese dessas rochas. Os ortogranulitos básicos possuem εNd positivos com baixas razões 87Sr/86 Sr(t) , o que indica extração a partir do manto depletado, porém sua razões La/YbN e La/NbN maiores que 1, revelam alguma contribuição de uma fonte enriquecida, assim também mostram suas razões Pb/Pb, que são maiores do que as razões calculadas para evolução de Pb na Terra. Essas interpretações ainda podem ser estendidas para um ortoanfibolito da série alcalina, encontrado na região de Três Rios (RJ).

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In addition to providing an overview of the party boat fishery in the U.S. Gulf of Mexico, a management-oriented methodology is presented that can be used elsewhere to assess regulatory impacts. Party boat operators were interviewed to determine species targeted, percent time committed to targeting each species, and opinions on current catch restrictions. Over two-thirds of the fieet was located on the west coast of Florida. Overall, most boats targeted <5 species. Four species accounted for 90 percent of the estimated effort by party boats in the U.S. Gulf of Mexico: Snapper; Lutjanus sp.; grouper, Epinephelus sp. and Mycteroperca sp.; amberjack, Seriola dumerili; and king mackerel, Scomberomorus cavalla. Party boat effort in Texas was devoted primarily to snapper, whereas in Florida most effort was devoted to snapper and grouper collectively. Party boat operators were diverse in their opinions of management regulations in force when interviewed. Results revealed why major opposition would he expected from Texas party boat operators for red snapper bag limits and other restrictions proposed by the Gulf of Mexico Fishery Management Council.

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Nuclear RNA and DNA in muscle cell nuclei of laboratory-reared larvae of Walleye Pollock (Gadus chalcogrammus) were simultaneously measured through the use of flow cytometry for cell-cycle analysis during 2009–11. The addition of nuclear RNA as a covariate increased by 4% the classification accuracy of a discriminant analysis model that used cell-cycle, temperature, and standard length to measure larval condition, compared with a model without it. The greatest improvement, a 7% increase in accuracy, was observed for small larvae (<6.00 mm). Nuclear RNA content varied with rearing temperature, increasing as temperature decreased. There was a loss of DNA when larvae were frozen and thawed because the percentage of cells in the DNA synthesis cell-cycle phase decreased, but DNA content was stable during storage of frozen tissue.

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Gulf of Mexico, white shrimp, Litopenaeus setiferus, catch statistics have been collected by NOAA’s National Marine Fisheries Service for over 50 years. Recent occurrences such as natural and manmade disasters have raised awareness for the need to publish these types of data. Here we report shrimp data collected from 1984 to 2011. These 28 years of catch history are the time series used in the most recent Gulf of Mexico white shrimp stock assessment. Fishing effort for this stock has fluctuated over the period reported, ranging from 54,675 to 162,952 days fished. Catch averaged 55.7 million pounds per year, increasing significantly over the times series. In addition, catch rates have been increasing in recent years, with CPUE levels ranging from 315 lb/day fished in 2002, to 1,175 lb/ day fished in 2008. The high CPUE’s we have measured is one indication that the stock was not in decline during this time period. Consequently, we believe the decline in effort levels is due purely to economic factors. Current stock assessments are now using these baseline data to provide managers with further insights into the Gulf L. setiferus stocks.

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The National Marine Fisheries Service (NMFS) is dedicated to the stewardship of living marine resources (LMR’s). This is accomplished through science-based conservation and management, and the promotion of healthy ecosystems. As a steward, NMFS has an obligation to conserve, protect, and manage these resources in a way that ensures their continuation as functioning components of healthy marine ecosystems, affords economic opportunities, and enhances the quality of life for the American public. In addition to its responsibilities within the U.S. Exclusive Economic Zone (EEZ), NMFS plays a supportive and advisory role in the management of LMR’s in the coastal areas under state jurisdiction and provides scientific and policy leadership in the international arena. NMFS also implements international measures for the conservation and management of LMR’s, as appropriate.NMFS receives its stewardship responsibilities under a number of Federal laws. These include the Nation’s primary fisheries law, the Magnuson Fishery Conservation and Management Act. This law was first passed in 1976, later reauthorized as the Magnuson-Stevens Fishery Conservation and Management Act in 1996, and reauthorized again on 12 January 2007 as the Magnuson-Stevens Fishery Conservation and Management Reauthorization Act (MSRA). The MSRA mandates strong action to conserve and manage fishery resources and requires NMFS to end overfishing by 2010 in all U.S. commercial and recreational fisheries, rebuild all overfished stocks, and conserve essential fish habitat.

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A study was initiated with field work in May 2007 to assess the status of ecological condition and stressor impacts throughout the U.S. continental shelf off South Florida, focusing on soft-bottom habitats, and to provide this information as a baseline for evaluating future changes due to natural or human-induced disturbances. The boundaries of the study region extended from Anclote Key on the western coast of Florida to West Palm Beach on the eastern coast of Florida, inclusive of the Florida Keys National Marine Sanctuary (FKNMS), and from navigable depths along the shoreline seaward to the shelf break (~100m). The study incorporated standard methods and indicators applied in previous national coastal monitoring programs — U.S. Environmental Protection Agency’s (EPA) Environmental Monitoring and Assessment Program (EMAP) and National Coastal Assessment (NCA) — including multiple measures of water quality, sediment quality, and biological condition. Synoptic sampling of the various indicators provided an integrative weight-of-evidence approach to assessing condition at each station and a basis for examining potential associations between presence of stressors and biological responses. A probabilistic sampling design, which included 50 stations distributed randomly throughout the region, was used to provide a basis for estimating the spatial extent of condition relative to the various measured indicators and corresponding assessment endpoints (where available). The study was conducted through a large cooperative effort by National Oceanic and Atmospheric Administration (NOAA)/National Centers for Coastal Ocean Science (NCCOS), EPA, U.S. Geological Survey (USGS), NOAA/Oceanic and Atmospheric Research (OAR)/Atlantic Oceanographic and Meteorological Laboratory in Miami, FKNMS, and the Florida Fish and Wildlife Conservation Commission (FWC). The majority of the South Florida shelf had high levels of dissolved oxygen (DO) in near-bottom water (> 5 mg L-1) indicative of “good” water quality.. DO levels in bottom waters exceeded this upper threshold at 98.8% throughout the coastal-ocean survey area. Only 1.2% of the region had moderate DO levels (2-5 mg/L) and no part of the survey area had DO <2.0 mg/L. In addition, offshore waters throughout the region had relatively low levels of total suspended solids (TSS), nutrients, and chlorophyll a indicative of oligotrophic conditions. Results suggested good sediment quality as well. Sediments throughout the region, which ranged from sands to intermediate muddy sands, had low levels of total organic carbon (TOC) below bioeffect guidelines for benthic organisms. Chemical contaminants in sediments were also mostly at low, background levels. For example, none of the stations had chemicals in excess of corresponding Effects-Range Median (ERM) probable bioeffect values or more than one chemical in excess of lower-threshold Effects-Range Low (ERL) values. Cadmium was the only chemical that occurred at moderate concentrations between corresponding ERL and ERM values. Sixty fish samples from 28 stations were collected and analyzed for chemical contaminants. Eleven of these samples (39% of sites) had moderate levels of contaminants, between lower and upper non-cancer human-health thresholds, and ten (36% of sites) had high levels of contaminants above the upper threshold.