Relevant bibliographies by topics / Suwannee

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
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Academic literature on the topic 'Suwannee'

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

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Journal articles on the topic "Suwannee"

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Holcomb, Jordan M., Colin P. Shea, and Nathan A. Johnson. "Cumulative Spring Discharge and Survey Effort Influence Occupancy and Detection of a Threatened Freshwater Mussel, the Suwannee Moccasinshell." Journal of Fish and Wildlife Management 9, no. 1 (February 2, 2018): 95–105. http://dx.doi.org/10.3996/052017-jfwm-042.

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AbstractFreshwater mussels (Unionidae) are among the most imperiled groups of organisms in the world, and the lack of information regarding species distributions, life-history characteristics, and ecological and biological requirements may limit the protection of remaining mussel populations. We examined the influence of hydrologic factors on the occurrence of the Suwannee Moccasinshell Medionidus walkeri, a federally threatened freshwater mussel species, endemic to the Suwannee River Basin in Georgia and Florida. We also evaluated the influence of survey effort on detection of Suwannee Moccasinshell during field surveys. We compiled all recent (2013–2016) mussel survey records in the Suwannee River Basin. We calculated cumulative discharge contributed by upstream springs for each of 220 survey locations. We combined the spring discharge predictor variable with Suwannee Moccasinshell detection and nondetection data from each survey location to develop a suite of occupancy models. Modeling results indicated that detection of Suwannee Moccasinshell during surveys was strongly and positively related to survey effort. Modeling results also indicated that sites with cumulative spring discharge inputs exceeding ∼28 cubic meters per second were most likely (i.e., predicted occupancy probabilities >0.5) to support Suwannee Moccasinshell populations. However, occupancy declined in the lowermost reaches of the Suwannee mainstem despite high spring discharge inputs, presumably due to greater tidal influences and differences in physicochemical habitat conditions. Historical localities where Suwannee Moccasinshell has presumably been extirpated are all devoid of springs in their upstream watersheds. We hypothesize that springs may buffer extremely tannic, and at times polluted, surface waters, in addition to maintaining adequate flows during periods of drought, thereby promoting the persistence of Suwannee Moccasinshell populations. Our study suggests that springs are a critical resource for Suwannee Moccasinshell and may be more important for conservation planning than was previously recognized.
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Rajabi, Masoumeh, Melissa Jones, Michael Hubbard, Gary Rodrick, and Anita C. Wright. "Distribution and Genetic Diversity ofSalmonella entericain the Upper Suwannee River." International Journal of Microbiology 2011 (2011): 1–9. http://dx.doi.org/10.1155/2011/461321.

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The Suwannee River spans the Florida/Georgia border to the Gulf of Mexico, and contributes to regional irrigation and recreational activities. Association ofSalmonella entericawith these resources may result in the contamination of produce and disease outbreaks. Therefore, surface water was examined for the distribution ofS. entericaat multiple time points from 4 sites on the upper Suwannee River. Isolates were confirmed by detection of theinvAgene, and 96% of all samples were positive for the bacterium. Most probable number enumeration ranged from <18 to 5400 MPN/100 mL. Genetic diversity of these isolates (n=110) was compared to other environmental (n=47) or clinical (n=28) strains and to an online library (n=314) using DiversiLab rep-PCR. All strains showed >60% similarity and distributed into 16 rep-PCR genogroups. Most (74%) of the Suwannee River isolates were clustered into two genogroups that were comprised almost exclusively (97%) of just these isolates. Conversely, 85% of the clinical reference strains clustered into other genogroups. However, some Suwannee River isolates (12%) were clustered with these primarily clinically-associated genogroups, supporting the hypothesis that river water can serve as a disease reservoir and that pathogenic strains may persist or possibly originate from environmental sources.
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Thorn, Coben D., and Michael L. Falgiani. "Jumping Sturgeon in the Suwannee River." Wilderness & Environmental Medicine 24, no. 3 (September 2013): 298–99. http://dx.doi.org/10.1016/j.wem.2013.01.006.

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Ong, Kimberly J., Lindsey C. Felix, David Boyle, James D. Ede, Guibin Ma, Jonathan G. C. Veinot, and Greg G. Goss. "Humic acid ameliorates nanoparticle-induced developmental toxicity in zebrafish." Environmental Science: Nano 4, no. 1 (2017): 127–37. http://dx.doi.org/10.1039/c6en00408c.

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Loosli, Frédéric, Letícia Vitorazi, Jean-François Berret, and Serge Stoll. "Isothermal titration calorimetry as a powerful tool to quantify and better understand agglomeration mechanisms during interaction processes between TiO2 nanoparticles and humic acids." Environmental Science: Nano 2, no. 5 (2015): 541–50. http://dx.doi.org/10.1039/c5en00139k.

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Burnett, William C., James B. Cowart, and Suchint Deetae. "Radium in the Suwannee River and estuary." Biogeochemistry 10, no. 3 (July 1990): 237–55. http://dx.doi.org/10.1007/bf00003146.

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Carter, Burchard D., and Michael L. McKinney. "Eocene echinoids, the Suwannee Strait, and biogeographic taphonomy." Paleobiology 18, no. 3 (1992): 299–325. http://dx.doi.org/10.1017/s0094837300010861.

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Faunal similarity among regions is often used as a means of identifying regions of endemism in fossil faunas. At least two large-scale taphonomic effects can affect apparent faunal similarity: stratigraphic and facies mismatching. In stratigraphic mismatching, an unconformity represents removal of most or all of a complete assemblage zone in one region, and the constituent taxa are mistakenly interpreted as having never inhabited that region. In facies mismatching, environmental differences between two regions (possibly unrecognized) cause the inference of a barrier that never existed. The two types of mismatching can work in concert if a facies was originally represented in a single stratigraphic interval that has been completely removed from one region. Analysis of faunal similarity via multivariate analysis of individual localities, coupled with comparison of the regions as single samples, may indicate mismatching if the results differ significantly.We view these two problems as part of a suite of taphonomic effects that are not evident in paleobiological analyses of smaller geographic scope. First, there is ambiguity in the notion of “barrier,” even when a candidate is obvious. Second, barriers in paleobiogeography are often hidden and must be inferred from their effects rather than observed. Third, stratigraphic and facies mismatching produce effects on regional faunas similar to those produced by barriers. Anyone using barriers to explain faunal disruptions should address these three points.Upper Eocene faunas of central Florida seem taxonomically distinct from those of the remainder of the Gulf Coastal Plain. This has historically been attributed to a known paleogeographic feature, the Suwannee Strait, which acts as a barrier. The amount of dissimilarity of the echinoid faunas is greater than the amount predicted as a result of sampling problems. Comparison of the results of multivariate and whole-region analyses suggests that mismatching of the two faunas, rather than a true barrier, causes the distinction. Principally facies, but also strata are mismatched. Early Late Eocene faunas inhabited terrigenous sands to the north of the strait and carbonate sands to the south and show the highest distinctiveness. Middle Late Eocene faunas inhabited primarily carbonate sands to the south and both carbonate sands and muds to the north. Overall similarity is higher for both local and regional analyses, and the faunas of northern sands are more similar to those of the southern region than to the northern mud faunas. Overall similarity across the strait is highest in the late Late Eocene strata when both regions had carbonate mud and sand facies. The faunas exhibit greater similarity within facies than they do within regions. Upper Late Eocene strata are poorly preserved north of the strait because of post-Eocene erosion.
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Camp, Janey V., Dennis B. George, Martha J. M. Wells, and Pedro E. Arce. "Monitoring advanced oxidation of Suwannee River fulvic acid." Environmental Chemistry 7, no. 3 (2010): 225. http://dx.doi.org/10.1071/en09146.

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Environmental context.Potentially toxic disinfection by-products form when water containing humic and fulvic acids is chlorinated to destroy pathogenic microorganisms. A pulsed electrical discharge was examined for its ability to destroy an aquatic fulvic acid by oxidation. Spectroscopically, changes in the organic structures were observed, but carbon content and disinfection by-products were not reduced. Abstract.A pilot-scale pulsed electrical discharge (PED) system was used to treat Suwannee River fulvic acid (SRFA) as a representative precursor material for the formation of disinfection by-products (DBPs), specifically trihalomethane compounds. Ultraviolet-visible and fluorescence spectroscopy, dissolved organic carbon (DOC), and the trihalomethane formation potential (THMFP) were used as analytical parameters to monitor the effects of treatment on the substrate. The potential for SRFA degradation (5 mg L–1 DOC) was examined over 60 min at each of four operational configurations, varying pulse energy and frequency (0.15 J and 60 Hz, 0.15 J and 120 Hz, 0.4 J and 60 Hz, and 0.4 J and 120 Hz) in a factorial design. Statistically significant changes occurred for UV254, EX254EM460, and EX328EM460 under selected conditions; however, concomitant changes in DOC and THMFP were not observed. The composition of SRFA changed, but organic carbon was not mineralised to carbon dioxide. In addition to showing degradation by PED, the significance of the preliminary findings of this research was to demonstrate that spectroscopic monitoring of precursor degradation alone can be misleading, and that whereas ultraviolet-visible and fluorescence spectroscopy indicated degradation of precursor compounds, DOC and THMFP measurements were unchanged and did not support the occurrence of mineralisation in this system.
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Pollock, Jeffrey C., James P. Hibbard, and Cees R. van Staal. "A paleogeographical review of the peri-Gondwanan realm of the Appalachian orogen1This article is one of a series of papers published in this CJES Special Issue: In honour of Ward Neale on the theme of Appalachian and Grenvillian geology." Canadian Journal of Earth Sciences 49, no. 1 (January 2012): 259–88. http://dx.doi.org/10.1139/e11-049.

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The eastern edge of the Appalachian orogen is composed of a collection of Neoproterozoic – early Paleozoic domains, Avalonia, Carolinia, Ganderia, Meguma, and Suwannee, which are exotic to North America. Differences in the geological histories of these peri-Gondwanan domains indicate that each separated independently from Gondwana, opening the Rheic Ocean in their wake. Cambrian departure of Ganderia and Carolina was followed by the Ordovician separation of Avalonia and Silurian separation of Meguma. After separation in the early Paleozoic, these domains constituted the borderline between the expanding Rheic Ocean and contracting Iapetus Ocean. They were transferred to Laurentia by early Silurian closure of Iapetus and Devonian–Carboniferous closure of the Rheic Ocean during the assembly of Gondwana and Laurentia into Pangaea. The first domain to arrive at Laurentia was Carolinia, which accreted in the Middle Ordovician during the Cherokee orogeny. Salinic accretion of Ganderia occurred shortly thereafter and was followed by the Acadian accretion of Avalonia. The Acadian orogeny was immediately followed by Middle Devonian – Early Carboniferous accretion of Meguma and possibly Suwannee which led to the Fammenian orogeny. The episodicity of orogeny suggests that the present location of these domains parallels their order of accretion. However, each of these crustal blocks was translated along strike by large-scale Late Devonian – Carboniferous dextral strike–slip motion. The breakup of Pangaea occurred outboard of the Paleozoic collision zones that accreted Carolinia, Ganderia, Avalonia, Meguma, and Suwannee to Laurentia, leaving these terranes appended to North America during the Mesozoic opening of the Atlantic.
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Leadon, Christopher J., and Orjan F. Wetterqvist. "Land acquisition criteria for the Suwannee river estuary, Florida." Coastal Zone Management Journal 14, no. 3 (January 1986): 217–39. http://dx.doi.org/10.1080/08920758609362003.

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Dissertations / Theses on the topic "Suwannee"

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Rajabi, Masoumeh. "Characterization of Salmonella enterica from the Suwannee River." [Gainesville, Fla.] : University of Florida, 2005. http://purl.fcla.edu/fcla/etd/UFE0005485.

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Kogut, Megan Brook 1972. "Copper binding ability of Suwannee River Humic Acid in seawater." Thesis, Massachusetts Institute of Technology, 2000. http://hdl.handle.net/1721.1/80946.

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Jett, Christina. "Estimation of microzooplankton grazing in the Suwannee River estuary, Florida, USA." [Gainesville, Fla.] : University of Florida, 2004. http://purl.fcla.edu/fcla/etd/UFE0003520.

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Quinlan, Erin Bledsoe. "Consequences of nutrient loading in the Suwannee River and estuary, Florida, USA." [Gainesville, Fla.] : University of Florida, 2003. http://purl.fcla.edu/fcla/etd/UFE0001040.

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Marda, Saurabh. "Effect of Ozonation and BAC Filtration Processes on Monochloramine Demand." Thesis, Georgia Institute of Technology, 2005. http://hdl.handle.net/1853/10577.

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Although the kinetics and mechanism of monochloramine decay in organic-free waters are relatively well understood, those in natural waters are not, due to exceedingly complex and poorly defined interactions of monochloramine with natural organic matter (NOM) and particles. Ozonation followed by a biologically activated carbon (BAC) filtration is a commonly practiced process option that affects the characteristics of both dissolved and particulate constituents in the water. However, how these changes in water constituents affect stability of the residual disinfectant, or monochloramine in particular, are currently unknown. Kinetics of monochloramine decay in water samples obtained before and after ozonation and BAC treatments were performed under varying operating conditions were determined by bench-scale batch experiments. Stability of monochloramine in the BAC filter effluent samples obtained at different times after backwashing was determined. It was found that in most cases monochloramine stability was greatly decreased after BAC filtration. Further filtering the BAC effluents with 1.2 and #61549;m polycarbonate membrane resulted in a substantial increase in monochloramine stability. A further increase was observed after filtering the samples using a 0.4 m membrane. This finding suggested that particulate matter generated from the filters could be the major cause of monochloramine instability. The fines from the activated carbon, possible components of the particulate matter eluting from the BAC filters, were found to exert an insignificant monochloramine demand both in the presence and absence of NOM, which is contrary to previous speculation in the literature about their demand for monochloramine. While there appears to exist a relationship between chloramine demand and HPC count of the filter effluent, more research will be needed to determine the effect of nature and type of microorganisms and their byproducts have on chloramine demand. Effect of ozonation on monochloramine stability is also under investigation using both the water sampled from full-scale plant and the synthetic water prepared with Suwannee River NOM.
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Shahar, Rotem. "Tools to advance row crop best management practice (BMP) implementation in Florida's Lower Suwannee River Basin." [Gainesville, Fla.] : University of Florida, 2008. http://purl.fcla.edu/fcla/etd/UFE0022895.

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Vaz, Denise de Oliveira. "Estudo das interações de íons metálicos divalentes com ácidos fúlvicos extraídos das águas do Rio Suwannee." Florianópolis, SC, 2006. http://repositorio.ufsc.br/xmlui/handle/123456789/88604.

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Tese (doutorado) - Universidade Federal de Santa Catarina, Centro de Ciências Físicas e Matemáticas. Programa de Pós-Graduação em Química
Made available in DSpace on 2012-10-22T11:14:13Z (GMT). No. of bitstreams: 1 226890.pdf: 1969804 bytes, checksum: 62ae312e7aeed3154c0dcf0c24a52c8a (MD5)
O estudo sobre as interações de íons metálicos e substâncias húmicas (SH) tem sido muito importante nas últimas décadas pelo fato de que as SH também controlam as trocas de íons entre: solo, água, animais e plantas. Na primeira etapa deste trabalho, foram analisadas as interações entre íons metálicos divalentes (Cu(II), Zn(II) e Cd(II)) e um modelo constituído por três ácidos orgânicos para simulação de SH. Mediram-se as concentrações dos grupos carboxílicos e fenólicos por potenciometria e os resultados foram interpretados com auxílio do método matemático de Gran modificado e feita a comparação com o programa computacional BEST7 e com os valores estequiométricos. Os valores obtidos pelo programa BEST7 mostraram-se mais próximos dos valores estequiométricos. Determinaram-se os valores das constantes de protonação e de complexação dos grupos funcionais da mistura modelo com os íons divalentes, usando potenciometria, interpretando-se os resultados com a ajuda dos programas BEST7 e SPE e comparados com os valores da literatura. A espectroscopia de absorção de luz ultravioleta foi usada para confirmar as espécies formadas com os íons Cu(II), identificadas na potenciometria. Os resultados obtidos mostraram-se concordantes. Na segunda etapa deste trabalho, foi aplicada a metodologia usada na mistura modelo para o estudo da complexação dos íons divalentes com um ácido fúlvico extraído das águas do rio Suwannee (AFRS) (padrão da IHSS). As concentrações (mmols) dos grupos fenólicos e carboxílicos foram determinadas (método de Schnitzer e Gupta) e comparadas com os resultados obtidos com o programa BEST7, que também determina os valores (mmols) dos 5 grupos oxigenados do AFRS (fenólicos, benzóicos, catecóis, ftálicos e salicílicos), usando os dados da titulação potenciométrica. Calcularam-se os valores das constantes de dissociação de prótons e de complexação com os íons metálicos divalentes para cada grupo funcional. Seus valores foram muito próximos dos valores publicados para as interações desses grupos contidos em moléculas simples. O grupo funcional que formou a maior quantidade de complexos foi o catecol, pois complexou com todos os íons divalentes e em maior quantidade com o Cu (II). De acordo com os resultados obtidos por potenciometria pode-se fazer a seguinte série de reatividade para os íons divalentes e o AFRS: Cu >> Cd > Zn. Confirmaram-se os resultados por espectroscopia de absorção de luz infravermelha com Transformada de Fourier e espectroscopia de fluorescência.
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Weiss, Matthew. "Evaluation of Geophysical and Thermal Methods for Detecting Submarine Groundwater Discharge (SGD) in the Suwannee River Estuary, Florida." Scholar Commons, 2006. http://scholarcommons.usf.edu/etd/3811.

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Submarine groundwater discharge (SGD) represents a significant portion of the total discharge from coastal aquifers through diffuse seepage and point source springs, but can be difficult to locate. SGD is important as it can be a source of nutrients to estuaries and other coastal ecosystems. In an effort to evaluate geophysical and thermal methods for detecting SGD on the Florida Gulf coast, a suite of water-borne surveys were run in conjunction with aerial thermal imagery over the lower Suwannee River and estuary in March and September 2005. Thermal imagery exploits temperature differences between discharging groundwater and surface water. Thermal images were collected in March (dry season), at the end of winter, and at night to maximize the differences between warm groundwater and colder surface water. Generally pore waters in zones of concentrated SGD should be fresher, and hence more resistive than "background" values. Marine streaming resistivity data can detect pore water resistivity variations and were collected alongside continuous 222Rn and CH4 sampling from surface waters. Naturally occurring tracers, 222Rn and CH4, are used as the "standard" against which resistivity and thermal images are compared. Based on the expected properties of discharging groundwater, we hypothesize that in zones of elected tracer concentrations, increased thermal image temperatures and increased terrain resistivities will be observed. The data set as a whole supports this hypothesis. However, regional-scale correlations are clearly and significantly influenced by factors other than SGD including thermal-image noise, the presence of the fresh/salt water interface, and a large regional tracer gradient generated by a first-order spring. At local scales (tens to hundreds of meters) there are no significant correlations between thermal image temperature and tracer concentrations, due at least in part to flight-line edge effects that dominate the thermal imagery. After correcting for regional trends,significant correlations between tracer concentration and log resistivity exist only in a subset of the data that lies offshore. Because neither thermal imagery nor streaming resistivity data consistently support the hypotheses, this study suggests that neither method by itself is reliable for detecting SGD in this area
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Kornilev, Yurii V. "Behavioral ecology and effects of disturbance on the Suwannee Cooter (Pseudemys concinna suwanniensis) in a blackwater spring-fed river." [Gainesville, Fla.] : University of Florida, 2008. http://purl.fcla.edu/fcla/etd/UFE0022700.

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Mckinnie, Frank W. "Monitoring and modeling water and nitrogen transport in the vadose zone of a vegetable farm in the suwannee river basin." [Gainesville, Fla.] : University of Florida, 2003. http://purl.fcla.edu/fcla/etd/UFE0001242.

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Books on the topic "Suwannee"

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Musgrove, Eric. Suwannee County. Charleston, S.C: Arcadia Pub., 2011.

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Suwannee River guidebook. Sarasota, Fla: Pineapple Press, 2009.

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Riders of the Suwannee. Sarasota, Florida: Pineapple Press, Inc., 1993.

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Doane, Elvin I. Old abandoned farmhouses of Suwannee County. [Fla.?]: E.I. Doane, 1998.

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Jekel, Pamela. River without end: A novel of the Suwannee. New York: Kensington Books, 1997.

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Jackson, Dale R. Reproduction in the Suwannee cooter, Pseudemys concinna suwanniensis. Gainesville, FL: Florida Museum of Natural History, 1997.

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Moses, Grace E. Rooster strut on the Suwannee: A novel ₊ two short stories. Wilmington, Del., U.S.A: Nopoly Press, 1988.

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Sulak, Kenneth J. The gulf sturgeon in the Suwannee River: Life history questions & answers. Gainesville, Fla: U.S. Dept. of the Interior, U.S. Geological Survey, 2007.

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M, Tillis Gina. Flow and salinity characteristics of the upper Suwannee River Estuary, Florida. Tallahassee, Fla: U.S. Geological Survey, 2000.

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Grubbs, J. W. Recharge rates to the upper Floridan Aquifer in the Suwannee River Water Management District, Florida: J.W. Grubbs ; prepared in cooperation with the Suwannee River Water Management District. Tallahassee, Fla: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Book chapters on the topic "Suwannee"

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Petuch, Edward J., and David P. Berschauer. "The Dade Subsea (Suwannee Formation)." In Ancient Seas of Southern Florida, 17–28. 2nd ed. Boca Raton: CRC Press, 2021. http://dx.doi.org/10.1201/9781003205944-2.

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Driver, Shamus J., and E. Michael Perdue. "Acidic Functional Groups of Suwannee River Natural Organic Matter, Humic Acids, and Fulvic Acids." In ACS Symposium Series, 75–86. Washington, DC: American Chemical Society, 2014. http://dx.doi.org/10.1021/bk-2014-1160.ch004.

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Yan, Mingquan, and Gregory V. Korshin. "Quantitation of Interactions of Suwannee River Fulvic Acid with Protons Based on Numerical Deconvolution of Differential Absorbance and Fluorescence Spectra." In Functions of Natural Organic Matter in Changing Environment, 233–37. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5634-2_42.

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Perdue, E. Michael. "Standard and Reference Samples of Humic Acids, Fulvic Acids, and Natural Organic Matter from the Suwannee River, Georgia: Thirty Years of Isolation and Characterization." In Functions of Natural Organic Matter in Changing Environment, 85–88. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5634-2_15.

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Johnson, David W. ". Suwannee to Cincinnati." In Lonesome Melodies, 143–57. University Press of Mississippi, 2013. http://dx.doi.org/10.14325/mississippi/9781617036460.003.0013.

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Moylan, Virginia Lynn. "DEATH ON THE SUWANNEE." In Zora Neale Hurston's Final Decade, 115–29. University Press of Florida, 2012. http://dx.doi.org/10.5744/florida/9780813035789.003.0007.

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"Black Bass Diversity: Multidisciplinary Science for Conservation." In Black Bass Diversity: Multidisciplinary Science for Conservation, edited by Brandon L. Barthel, Wesley F. Porak, Michael D. Tringali, and David P. Philipp. American Fisheries Society, 2015. http://dx.doi.org/10.47886/9781934874400.ch46.

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<em>Abstract</em>.—Suwannee Bass <em>Micropterus notius</em> have one of the smallest ranges of all the black basses. For decades, they were believed to only inhabit the Ochlockonee and Suwannee River drainages in Florida and Georgia. Over the past 15 years, additional populations have been discovered in the Wacissa, Wakulla, and St. Marks rivers in Florida, leading to speculation that these populations were created in the late 20th century through unsanctioned angler releases. Tissue samples were collected from Suwannee Bass inhabiting six streams in northern Florida in order to investigate this possibility and resolve genetic relationships across the species range. Nuclear DNA variation (11 polymorphic microsatellite loci and three allozyme loci) indicated that there was significant genetic differentiation between the fish inhabiting the Suwannee River drainage and those from the four streams to the west (i.e., the Ochlockonee River collection plus the three recently discovered populations). Analysis of molecular variance found that more than half of the nuclear genetic variation was partitioned between these two groups of collections. The fish from the two regions also had different ND2 gene sequences and private restriction fragment length polymorphism haplotypes. The consistent pattern of differentiation in the nuclear and mitochondrial genomes indicates that there are two stocks or subspecies of Suwannee Bass within the species range. The recently discovered populations were found to be genetically similar to fish from the Ochlockonee River and displayed genetic signals consistent with founding effects, as would be expected if these populations had originated from the release of a small number of individuals (potentially by anglers). However, the Ochlockonee River had similar genetic signatures, providing an example of a natural population of Suwannee Bass that is likely to have experienced natural bottlenecks due to low population size.
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Klein, Misha. "An Overview of the Suwannee Valley Culture." In Late Prehistoric Florida, 149–71. University Press of Florida, 2012. http://dx.doi.org/10.5744/florida/9780813040141.003.0007.

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Daniel, I. Randolph, and Michael Wisenbaker. "Site Stratification and Cultural Stratification." In Harney Flats. University Press of Florida, 2017. http://dx.doi.org/10.5744/florida/9781683400226.003.0003.

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This chapter describes site stratigraphy. Site deposition appears to have been dominated by windblown sand that was sufficient to bury lithic assemblages creating a stratified sequence at Harney Flats. Excavation profiles at Harney Flats were dominated by some two meters of pedogenically modified sands. The upper 1.6 meters of sand contained archaeological deposits dominated by a Bolen/Suwannee component concentrated from 100 to 130 centimeters below surface and a Newnan component from roughly 60 to 90 centimeters below surface. A much more ephemeral later period ceramic component was present from about 40 to 60 centimeters below surface. Of significance is that a dense hardpan soil zone present from about 75 to 85 centimeters below surface prevented stratigraphic mixing of the Newnan and Bolen/Suwannee assemblages.
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Daniel, I. Randolph, and Michael Wisenbaker. "Context of Paleo-lndian in Central Florida." In Harney Flats. University Press of Florida, 2017. http://dx.doi.org/10.5744/florida/9781683400226.003.0007.

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Unfortunately, as elsewhere in the Southeast, most Florida Paleoindian sites exist as isolated lanceolate points and alleged kill sites. Most purported associations of Paleoindian points with extinct Ice Age fauna remain dubious. Probably the most well-known Paleoindian sites are Little Salt Spring and Warm Mineral Springs, both in Sarasota County. These two sites contained both Paleoindian and Archaic diagnostic artifacts. Artifacts from Warm Mineral Springs, for example, appear to be temporally related to Archaic points or, at best Transitional, such as Greenbriar point. Besides Harney Flats, the only other location that produced in situ Paleoindian tools was the Silver Springs Site in Marion County. Although the Suwannee point and its variants is thought to be the predominant Florida Paleoindian diagnostic artifact, it remains undated. It is agreed by most professional archaeologists, nevertheless, that Suwannees represent Florida’s earliest point type and are the most characteristic Paleoindian tool in Florida.
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Conference papers on the topic "Suwannee"

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Thompson, Carmi Milagros, and Roger W. Portell. "ATURIA (CEPHALOPODA: NAUTILIDA) IN THE LOWER OLIGOCENE SUWANNEE LIMESTONE OF FLORIDA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323746.

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Mueller, Paul A., Michel Villeneuve, David A. Foster, Ann L. Heatherington, and William A. Thomas. "THE SUWANNEE AND UCHEE TERRANES: EXAMPLES OF INCONGRUOUS ALLEGHANIAN ACCRETION IN THE SOUTHERN APPALACHIANS." In 65th Annual Southeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016se-273758.

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Boote, Susannah, and James H. Knapp. "EXTENT OF SUWANNEE TERRANE RE-EVALUATED OFFSHORE: IMPLICATIONS FOR THE LOCATION OF THE ALLEGHENIAN SUTURE." In 65th Annual Southeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016se-273252.

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Duff, Patrick D., and JAMES Kellogg. "THE SUWANNEE SUTURE AND TERMINAL ALLEGHANIAN COLLISION: REINTERPRETATION FROM INTEGRATED ANALYSES OF POTENTIAL FIELD DATA." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359503.

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Knapp, James H. "REVISED EXTENT OF THE SUWANNEE TERRANE: IMPLICATIONS FOR THE LAURENTIA-GONDWANA BOUNDARY IN THE SOUTHEASTERN U.S." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-326540.

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Chernysheva, M. G., and G. A. Badun. "Fulvic acids separated from Suwannee River behavior in the aqueous-xylene system: influence of ionic strength and interaction with proteins." In Fifth International Conference of CIS IHSS on Humic Innovative Technologies «Humic substances and living systems». CLUB PRINT ltd., 2019. http://dx.doi.org/10.36291/hit.2019.chernysheva.088.

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Runbin Duan, George J Hochmuth, Don Graetz, and Wendy Graham. "Temporal and Spatial Distribution of Soluble Reactive Phosphorus in Groundwater at a Dairy Farm in the Suwannee River Basin of Florida." In 2012 Dallas, Texas, July 29 - August 1, 2012. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2012. http://dx.doi.org/10.13031/2013.41871.

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Frank W. McKinnie, Wendy D. Graham, James W. Jones, and Donald A. Graetz. "Modeling and Monitoring the Water and Nitrate Transport and Potato Growth at a Vegetable Farm in the Suwannee River Basin, FL." In 2003, Las Vegas, NV July 27-30, 2003. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2003. http://dx.doi.org/10.13031/2013.14006.

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Tennakoon, Shamindri Dinusha, William Lindberg, William Lindberg, Michał Kowalewski, and Michał Kowalewski. "MOLLUSKS AS A PROXY FOR ASSESSING ECOLOGICAL IMPACTS OF ARTIFICIAL REEFS: A COMPARISON OF DEAD AND LIVING MOLLUSK ASSEMBLAGES IN THE SUWANNEE REGIONAL REEF SYSTEM, FLORIDA." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-290586.

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Tennakoon, Shamindri Dinusha, William Lindberg, and Michał Kowalewski. "MOLLUSK DEATH ASSEMBLAGES AS A BASELINE FOR ASSESSING COMMUNITY SHIFTS IN ARTIFICIAL REEFS: A COMPARISON OF DEAD AND LIVING MOLLUSK ASSEMBLAGES IN THE SUWANNEE REGIONAL REEF SYSTEM, FLORIDA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300479.

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Reports on the topic "Suwannee"

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Geology of Suwannee County, Florida. Florida Geological Survey, 2003. http://dx.doi.org/10.35256/ofr86.

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Mineral Resources of Suwannee County, Florida. Florida Geological Survey, 1993. http://dx.doi.org/10.35256/ms137.

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Geologic Map of Suwannee County, Florida. Florida Geological Survey, 1993. http://dx.doi.org/10.35256/ofms33.

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Flow and salinity characteristics of the upper Suwannee River Estuary, Florida. US Geological Survey, 2000. http://dx.doi.org/10.3133/wri994268.

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Humic substances in the Suwannee River, Georgia: Interactions, properties, and proposed structures. US Geological Survey, 1994. http://dx.doi.org/10.3133/wsp2373.

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Sources and chronology of nitrate contamination in spring waters, Suwannee River basin, Florida. US Geological Survey, 1999. http://dx.doi.org/10.3133/wri994252.

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Magnitude and frequency of floods in the Suwannee River Water Management District, Florida. US Geological Survey, 1996. http://dx.doi.org/10.3133/wri964176.

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Magnitude and frequency of low flows in the Suwannee River Water Management District, Florida. US Geological Survey, 1996. http://dx.doi.org/10.3133/wri964308.

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Forest Types in the Lower Suwannee River Floodplain, Florida?-A Report and Interactive Map. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034008.

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Carbonate Units of the Intermediate Aquifer System in the Suwannee River Water Management District:. Florida Geological Survey, 1992. http://dx.doi.org/10.35256/ofr54.

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