Дисертації з теми "Tropical lakes"
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Hamaguchi, Satoshi, and Mitsuru Sakaizumi. "Species differentiation of fishes in tropical lakes : The Seventh MEDAKA Symposium." Laboratory of Freshwater Fish Stocks Bioscience Center Nagoya University, 1994. http://hdl.handle.net/2237/13794.
Повний текст джерелаConroy, Jessica. "HISTORY AND DYNAMICS OF CLIMATE VARIABILITY IN THE ASIAN MONSOON REGION AND TROPICAL PACIFIC DURING THE LATE HOLOCENE." Diss., The University of Arizona, 2011. http://hdl.handle.net/10150/145432.
Повний текст джерелаMiranda, Marcela Aparecida Campos Neves. "Medidas de mitigação para controle e manejo das florações de cianobactérias em um sistema raso tropical." Universidade Federal de Juiz de Fora (UFJF), 2017. https://repositorio.ufjf.br/jspui/handle/ufjf/6500.
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Florações de cianobactérias são consequência principalmente da eutrofização de ambientes aquáticos que afeta a qualidade e compromete o uso da água para diversas finalidades. A restauração de sistemas aquáticos eutrofizados é um dos principais desafios da limnologia atual. Nosso objetivo foi identificar as principais causas do processo de eutrofização e ocorrência de florações de cianobactérias e testar a eficácia e aplicabilidade do uso combinado de coagulantes e adsorventes de P em fase sólida no controle da eutrofização e florações em um lago tropical raso. O estudo foi conduzido no lago do Museu Mariano Procópio, localizado em Juiz de Fora – MG e dividido em quatro fases. As duas primeiras fases compreendem uma análise sistêmica do lago. Na primeira, buscou-se conhecer a dinâmica da comunidade fitoplanctônica a fim de entender a dominância de cianobactéria deste sistema. Na segunda, foram avaliados os aportes de fósforo (P) para o sistema. Na terceira fase foram realizados experimentos em laboratório, para verificar a eficácia de diferentes coagulantes e lastros para remoção de cianobactérias. E na quarta fase foram realizados experimentos em mesocosmos no lago, para testar o controle da eutrofização e florações de cianobactérias. A análise sistêmica mostrou dominância de diferentes espécies de cianobactérias e que as altas concentrações de nutrientes presentes do sistema vêm principalmente de contribuição externa. O uso combinado de coagulantes e lastros foi eficiente para a remoção de biomassa de cianobactérias, porém foi dependente da espécie. Nos experimentos com mesocosmos, foi observada uma forte redução de Clorofila a (Chl a 85%) e fósforo total (TP 78%) (p <0,0010) em todos os tratamentos, porém estas reduções não se mantiveram ao longo do tempo. Para mitigar as florações de cianobactérias deste sistema, será necessário o controle das fontes externas de nutrientes e um ajuste na técnica de coagulante-lastro para manter a clorofila e o fósforo total em concentrações reduzidas por mais tempo.
Cyanobacterial Blooms are mainly a consequence of eutrophication of aquatic environments that affect the water quality and compromise the use of water for various purposes. The restoration of eutrophic aquatic systems is one of the main challenges of today's limnology. Our objective was to identify the main causes of the eutrophication process and the occurrence of cyanobacterial blooms in a shallow tropical lake, and to test the efficacy and applicability of the combined use of coagulants and adsorbents of P in solid phase for the control of eutrophication and cyanobacteria blooms in a tropical shallow system. The study was conducted in the lake of the Mariano Procópio Museum, located in Juiz de Fora - MG and divided into four phases. The first two phases comprised a systemic analysis of the lake. The first one sought to know the dynamics of the phytoplankton community and to understand the causes of the cyanobacteria dominance in this system. In the second one, the main contributions of phosphorus to the system and the general balance of P were evaluated. In the third phase, laboratory experiments were carried out to evaluate the efficacy of different coagulants and ballasts for the removal of cyanobacteria. Last, in the fourth phase experiments were carried out in mesocosmos in the lake to test the control of eutrophication and cyanobacterial blooms. The systemic analysis showed the dominance of different species of cyanobacteria and that the high concentrations of nutrients present in the system come mainly from external contribution. The combined use of coagulants and ballasts was efficient for the removal of cyanobacteria biomass, but it is dependent on the species pool. In the experiments with mesocosms, a strong reductions of chloropyll a (Chl a) 85% and total phosphorus (TP) 78% (p < 0.001) were observed in all treatments, however these reductions were not lasting. To mitigate the cyanobacterial blooms of this system, it will be necessary to control the external sources of nutrients and also an adjustment in the coagulant-ballast technique to keep Chl a l and TP in reduced concentrations for longer time.
Rai, Ash Kumar. "Limnological Characteristics and Food Evaluation of Planktivorous Caged Fish Species in Sub-tropical Lakes Phewa, Begnas and Rupa of Pokhara Valley, Nepal." 京都大学 (Kyoto University), 2000. http://hdl.handle.net/2433/181462.
Повний текст джерелаHales, Philip. "Inorganic geochemistry of tropical lake and swamp sediments." Thesis, University of Oxford, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.357524.
Повний текст джерелаKitaka, Nzula. "Phosphorus supply to a shallow tropical lake and its consequences, Lake Naivasha, Kenya." Thesis, University of Leicester, 2000. http://hdl.handle.net/2381/29813.
Повний текст джерелаPark, Lisa Ellyn. "Assessing diversification patterns in an ancient tropical lake: Gomphocythere (Ostracoda) in Lake Tanganyika." Diss., The University of Arizona, 1995. http://hdl.handle.net/10150/187316.
Повний текст джерелаAlin, Simone Rebecca. "Calibration and Interpretation of Holocene Paleoecological Records of Diversity from Lake Tanganyika, East Africa." Diss., The University of Arizona, 2001. http://hdl.handle.net/10150/231412.
Повний текст джерелаDu, Feu Timothy Avon. "Tropical reservoir fisheries : Lake Kainji, Nigeria: a case study." Thesis, University of Hull, 2003. http://hydra.hull.ac.uk/resources/hull:5505.
Повний текст джерелаHubble, David S. "Controls on primary production in Lake Naivasha, a shallow tropical freshwater." Thesis, University of Leicester, 2000. http://hdl.handle.net/2381/29812.
Повний текст джерелаMatla, Matsoele Moses. "Helminth ichthyo-parasitic fauna of a South African Sub-Tropical Lake." Thesis, University of Limpopo (Turfloop Campus), 2012. http://hdl.handle.net/10386/822.
Повний текст джерелаThe diversity of the helminth parasites of fishes in a clear-water, subtropical Lake Tzaneen, in South Africa was investigated. Of the 527 fish specimens sampled approximately 9000 parasites were collected. There are 38 different parasite species discussed comprising 27 Monogenea, 3 Digenea, 4 Cestoda, 3 Nematoda and 1 Acanthocephala. Four new monogenean species are described and these are Dactylogyrus spp. 1 to 4. Three monogenean species are introduced as first records in Africa and these are Actinocleidus fusiformis (Mueller, 1934), Haplocleidus furcatus Mueller, 1937 and Acolpenteron ureteroecetes Fischthal & Allison, 1940. Fourteen monogenean and one acanthocephalan species are discussed as first geographical records for South Africa and these are Gyrodactylus rysavyi Ergens, 1973, Dactylogyrus brevicirrus Paperna, 1973, Dactylogyrus cyclocirrus Paperna, 1973, Dogielius dublicornis Paperna, 1973, Dogielius sp., Schilbetrema quadricornis Paperna & Thurston, 1968, Quadriacanthus aegypticus El Naggar & Serag, 1986, Quadriacanthus clariadis Paperna, 1961, Scutogyrus gravivaginus (Paperna & Thurston, 1969), Cichlidogyrus quaestio Douëllou, 1993, Cichlidogyrus halli Price & Kirk, 1967, Cichlidogyrus sclerosus Paperna & Thurston, 1969, Cichlidogyrus dossoui Douëllou, 1993, Cichlidogyrus tilapiae Paperna, 1960 and Acanthosentis tilapiae Baylis, 1948. Seven species are discussed as first records for their hosts and these are Cichlidogyrus dossoui, Cichlidogyrus halli and Acanthosentis tilapiae on Oreochromis mossambicus; Dactylogyrus sp. 1 on Barbus radiatus and Barbus trimaculatus; Dactylogyrus sp. 2 on Barbus unitaeniatus; Dactylogyrus sp. 3 and Dactylogyrus sp. 4 on Labeo molybdinus. Gyrodactylus rysavyi is the only species with a first site (gills) record. The other monogenean species discussed are Macrogyrodactylus clarii Gussev, 1961, Macrogyrodactylus karibae (Douellou and Chishawa, 1995), Dactylogyrus afrolongicornis afrolongicornis Paperna, 1973, Dactylogyrus allolongionchus Paperna, 1973, Dactylogyrus spinicirrus (Paperna & Thurston, 1968) and Cichlidogyrus philander (Douëllou, 1993). The digeneans discussed are Glossidium pedatum Looss, 1899 and the larvae of Diplostomum van Nordmann, 1832 and Clinostomum Leidy, 1856. The Cestodes discussed are Proteocephalus glanduligerus (Janicki, 1928) Fuhrmann, 1933, Polyonchobothrium clarias Woodland, 1925 and the larvae of Ligula intestinalis Goeze, 1782 and family Gryporhynchidae. The nematodes discussed are Procamallanus laevionchus (Wedl, 1861), Paracamallanus cyathopharynx Baylis, 1923 and larvae of Contracaecum Railliet and Henry, 1912. Monogenea were commonly found on the gills but less on the skin and in the urinary bladder. Digenea were found mainly in the eyes, brain and visceral cavity, with only one species (Glossidium pedatum) present in the intestines of Clarias gariepinus. Cestoda and Nematoda were found in the intestine and body cavity. Only one species of Acanthocephala (Acanthosentis tilapiae) was found in the intestines of Oreochromis mossambicus. No definite seasonal variations of infection and parasite affinities towards the sexes and the sizes of the hosts could be determined. The lake is oligotrophic with the water quality having no influence on the parasite diversity and species richness.
the University of Limpopo Research Office, and the National Research Foundation
Rajmanickam, Vijayaraj, Hema Achyuthan, Christopher Eastoe, and Anjum Farooqui. "Early-Holocene to present palaeoenvironmental shifts and short climate events from the tropical wetland and lake sediments, Kukkal Lake, Southern India: Geochemistry and palynology." SAGE PUBLICATIONS LTD, 2017. http://hdl.handle.net/10150/624066.
Повний текст джерелаWang, Ning, and 王宁. "Organic carbon signatures of the middle-late quaternary lacustrine history of tropical South China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/208631.
Повний текст джерелаpublished_or_final_version
Earth Sciences
Doctoral
Doctor of Philosophy
Hardy, Elsa Rodrigues. "Cycle characteristics of planktonic cladocerans in a tropical lake, Central Amazon : field and experimental work." Thesis, Royal Holloway, University of London, 1989. http://repository.royalholloway.ac.uk/items/c71f2018-fabf-4a5a-ba6a-26653ffcccf2/1/.
Повний текст джерелаLucca, José Valdecir de. "Composição, distribuição e abundância dos macroinvertebrados bentônicos da Lagoa do Caçó (MA)." Universidade de São Paulo, 2002. http://www.teses.usp.br/teses/disponiveis/18/18139/tde-04022016-101949/.
Повний текст джерелаBenthic communities are relevant in aquatic ecosystems due to their role in the ecosystem functioninq and also as rnarkers or indicators of paleoconditions. Their distribution, similarly to other communities, is conditioned by abiotic and biotic factors and to their interactions, which determine the structure of the community that will be established. The present work aimed to determine the taxonomic composition, the abundance and spatial distribution of the benthic community, by collecting at 20 sampling points in Caçá Lake. A total of 14 points were located in the littoral region (7 on the right margin and 7 on the left one) and 6 in the limnetic zone. Seasonal variation on community parameters and also of chemical and physical characteristics of water and sediment were analysed and related to the seasonal displacement of the Intertropical Convergence Zone. Caçó Lake is located at the North of Maranhão State and it has approximately 5 km of length and 500m mean width. Sampling was carried out in April (rainy season) and November (dry season). The results evidenced that there are differences in the richness of taxa, diversity and density of benthic species that are mainly related to the seasonality. The diversity, richness and density were higher in the dry than in the rainy period. The family Chironomidae (Diptera, Insecta) was the most important component of the community representing approximately 50% of the total benthic fauna of the lake. The sediment of Caçá Lake has low organic content being classified as a mineral one. The granulometric composition shows that the sediment is heterogeneous being sandy at the left margin, clayey in the right margin and sandy-clayey in the limnetic zone. In relation to the limnological variables, thermal and chemical (pH, dissolved oxygen and temperature) micro-stratifications were observed for both periods sampled. The trophic state indices applied have allowed to classifv Lake Caçá as an oligotrophic lake. The alternation of dry and rainy periods can be considered the main forcing function causing the changes in physical and chemical water characteristics as well on benthic community in the year 1999. The identification of the present Chironomidae at the genus level and the fact that this group does produce fossilizing remains make them good paleolimnological and paleoclimatic tracers that may be used to infer on past lake and climate conditions.
Thompson, Diane M., Jessica L. Conroy, Aaron Collins, Stephan R. Hlohowskyj, Jonathan T. Overpeck, Melanie Riedinger-Whitmore, Julia E. Cole, et al. "Tropical Pacific climate variability over the last 6000 years as recorded in Bainbridge Crater Lake, Galápagos." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/625825.
Повний текст джерелаDelvalle, David. "Geochemical and mineralogical analysis of stream and lake sediments from a tropical watershed (Panama canal watershed) /." Heidelberg : [Ruprecht-Karls-Universität], 1989. http://catalogue.bnf.fr/ark:/12148/cb37428731k.
Повний текст джерелаRoberts, David Thomas. "Trophic Implications of Drought on a Sub-Tropical Reservoir Food Web: Lake Samsonvale (North Pine Dam)." Thesis, Griffith University, 2012. http://hdl.handle.net/10072/367026.
Повний текст джерелаThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Griffith School of Environment
Science, Environment, Engineering and Technology
Full Text
Posselt, Amanda J. "Are Nutrients the Key Driver in Prompting Dominance of Toxic Cyanobacterial Blooms in a Sub-Tropical Reservoir?" Thesis, Griffith University, 2010. http://hdl.handle.net/10072/367306.
Повний текст джерелаThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Griffith School of Environment
Science, Environment, Engineering and Technology
Full Text
Dunn, Catherine. "How Unusual is Tropical Storm Irene? A Case Study of Storm Deposition in Littleville Lake, Huntington, MA." Oberlin College Honors Theses / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1400777365.
Повний текст джерелаMcGlue, Michael Matthew. "LATE QUATERNARY PALEOLIMNOLOGY IN THE SOUTHERN HEMISPHERE TROPICS." Diss., The University of Arizona, 2011. http://hdl.handle.net/10150/204064.
Повний текст джерелаThompson, Diane Marie. "Variability and trends in the tropical Pacific and the El Niño-Southern Oscillation inferred from coral and lake archives." Diss., The University of Arizona, 2013. http://hdl.handle.net/10150/311122.
Повний текст джерелаKristen, Iris. "Investigations on rainfall variability during the late Quaternary based on geochemical analyses of lake sediments from tropical and subtropical southern Africa." Phd thesis, Universität Potsdam, 2009. http://opus.kobv.de/ubp/volltexte/2009/3254/.
Повний текст джерелаIn dieser Arbeit werden Ergebnisse von Untersuchungen an den Sedimenten zweier afrikanischer Seen vorgestellt, die ein Archiv für Klimaveränderungen über einen Zeitraum von mehr als 200.000 Jahren darstellen. Der Schwerpunkt liegt in dieser Arbeit auf dem letzten Glazial und dem Holozän (ca. 100.000 Jahre vor heute [nachfolgend als 100 kyr BP bezeichnet] bis heute). Grundlegende Voraussetzung für solche Studien ist ein gutes Verständnis der Ökosysteme in und um den See, sowie des gegenwärtigen Sedimentationsgeschehens. Deswegen beinhalten beide Seestudien Untersuchungen der heutigen Organismen, Böden, Gesteine, Wasserchemie und Sedimentablagerungen. Im Tswaing-See im nordöstlichen Südafrika wurden anhand eines 90 m langen Sedimentprofils Studien zur Sedimentzusammensetzung und Untersuchungen der Zusammensetzung und Qualität des organischen Materials durchgeführt. Sie zeigen einen Wechsel zwischen Phasen hohen detritischen Eintrags, während derer v.a. kaum autochthones organisches Material im See erhalten blieb, mit Phasen geringen Eintrags und dafür karbonatischer oder evaporitischer Sedimentation, die hohe Gehalte v.a. autochthonen organischen Materials aufweisen. Diese Phasen werden als relativ feuchte bzw. trockene Perioden interpretiert und folgen bis vor ca. 75 kyr BP Schwankungen der lokalen solaren Einstrahlung. Dieser Einfluss nimmt nach 75 kyr BP ab und azyklische feuchte Phasen werden beobachtet. Mögliche Ursachen sind Veränderungen in der ozeanischen Zirkulation und Verschiebungen in der Lage der Innertropischen Konvergenzzone (ITCZ); beides sind auch heute Haupteinflussfaktoren auf die Niederschläge in der Region. Die heute lebenden Organismen des Tswaing-Kraters wurden mittels Analysen der Biomarkerzusammensetzung und der Kohlenstoffisotopie charakterisiert und ihr Einfluss auf die heutigen Seeablagerungen untersucht. Dabei konnten zusätzlich Indikatoren für die Aktivität methanotropher Bakterien nachgewiesen werden. Der Vergleich heutiger Sedimente mit denen des Zeitraumes 14 bis 2 kyr BP zeigt deutliche Veränderungen sowohl in der Zusammensetzung, als auch in der Kohlenstoffisotopie der Biomarker, die mit Veränderungen in der Hydrologie erklärt werden können. Die gefundenen Hinweise auf feuchtere Bedingungen im Zeitraum älter als 10 kyr BP, für trockenere Verhältnissen zwischen 10 und 7.5 kyr BP und für die nachfolgende Wiederzunahme an Feuchtigkeit werden durch die sedimentologischen Ergebnisse unterstützt. Objekt der zweiten Seestudie ist der Challa-See am Fuß des Kilimanjaro. Hier werden heute im mm-Maßstab laminierte Sedimente gebildet, die mit Mikro-XRF-scanning auf Veränderungen in der Elementzusammensetzung untersucht wurden. Zusammen mit Untersuchungen der Mikrofazies und im Vergleich mit ersten Ergebnissen noch laufender Sedimentfallenstudien, mit meteorologischen Daten und Analysen des Umgebungsgesteins werden die saisonalen Veränderungen in der Temperaturverteilung, der Durchmischungstiefe, dem detritischen Eintrag und der Bioproduktivität des Sees in den Sedimenten nachvollziehbar. Der See ist in den feucht-warmen Perioden von Oktober bis Dezember und von März bis Mai stratifiziert. Während dieser Zeit erfolgt der Eintrag detritischen Materials und Kalziumkarbonat fällt aus; eine dunkle Lage mit hohen Gehalten an Fe und Ti und mit hohen Ca/Al- und niedrigen Mn/Fe-Verhältnissen bildet sich am Boden des Sees. Diatomeen blühen während der kühlen, windigen Periode von Juni bis September, wenn die Durchmischung bis auf etwa 60 m Tiefe Nährstoffe verfügbar macht. Die Ausfällung von Fe- und Mn-oxiden sorgt für hohe Mn/Fe-Verhältnisse; es bildet sich eine helle Lage auf dem Sediment. Trends im Mn/Fe-Verhältnis werden als Signal für Veränderungen in der Intensität oder Dauer der saisonalen Durchmischung interpretiert. Dies wird unterstützt durch parallele Trends im Gehalt an organischem Material und an biogenem Silizium, wie durch Analysen an einem 22 m langen Bohrkern gezeigt werden kann. Nach gut durchmischten und von erhöhtem Eintrag von außen geprägten Verhältnissen während des letzten Glazials erfolgt gegen 16 kyr BP ein Übergang zu stärker stratifizierten Bedingungen. Diese korrespondieren mit einem steigenden Seespiegel und verbreiteten Hinweisen auf feuchte Bedingungen im tropischen Ostafrika. Stärkere Durchmischung herrschte während der Jüngeren Dryas und von 11.4 bis 10.7 kyr BP. Diese Perioden entsprechen Zeiten verringerter Südwest- und vermutlich verstärkter Nordostmonsunintensität im Bereich des Indisch-Asiatischen Monsuns und spiegeln eine global beobachtete südliche Verschiebung der ITCZ wider. Nach einer kurzen stabilen, feuchten Phase im frühen Holozän nimmt die Durchmischung des Sees im Verlauf des Holozän wieder zu. Abrupte Ereignisse während des Holozän scheinen im Challa-See zeitgleich mit Veränderungen der Monsunintensität der Nordhemisphäre aufzutreten und bezeugen die starke klimatische Kopplung der niederen Breiten in globalem Maßstab.
Carvalho, Felipe Rust de. "Fluxo de CO2 e CH4 em uma lagoa tropical (Pantanal, Brasil) com gradiente de turbidez." Universidade Federal de Juiz de Fora, 2015. https://repositorio.ufjf.br/jspui/handle/ufjf/413.
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Ecossistemas de água doce (rios, lagos e reservatórios) desempenham um papel essencial na ciclagem de carbono nos continentes. Esses ambientes são fontes significantes de gases de efeito estufa (GEE) para a atmosfera, principalmente de gás carbônico (CO2) e metano (CH4). Apesar do aumento do número de estimativas, a dinâmica e o controle das emissões naturais de GEE em ambientes aquáticos ainda é pouco estudada, especialmente nos trópicos. O objetivo geral da dissertação foi estimar os fluxos de CO2 e CH4 em uma lagoa tropical rasa com gradiente de turbidez. O trabalho foi realizado na lagoa Sinhá Mariana (MT), uma lagoa pantaneira com a ocorrência de duas regiões hidrológicas distintas; a lagoa é ligada ao rio Mutum de águas claras, pobre em material em suspensão, e baixa turbidez e ao rio Cuiabá de águas túrbidas, que apresenta alta taxa de material em suspensão. Duas coletas foram realizadas no ambiente, caracterizando os períodos hidrológicos de águas altas e águas baixas. A variação temporal, espacial e o pulso de inundação mostraram serem fatores importantes no fluxo de CO2, que variou de -4,95 mmol m-2 d-1 a 282 mmol m-2 d-1 nos períodos amostrados e diferenças significativas foram observadas entre um período e outro, com maiores emissões no período de águas altas (142 ± 40 mmol m-2 d-1) e menores nas águas baixas (2,3 ± 11,5 mmol m-2 d-1). Além disso, os fluxos de CO2 foram significantemente m/aiores nas proximidades do rio Mutum e menores na região túrbida e intermediária da lagoa, em ambos os períodos. Diferentemente, o fluxo total de CH4, embora estimado apenas nas águas altas, registrou os maiores valores médios na região de maior turbidez da lagoa (10,9 ± 6,9 mmol m-2 d-1), seguido pela região intermediária (5,1 ± 3,9 mmol m-2 d-1) e pela região influenciada pela água clara (2,5 ± 1,4 mmol m-2 d-1). A ebulição foi o principal processo de emissão de CH4, responsável por 78% do fluxo total. O gradiente de turbidez registrado ao longo da lagoa pareceu ter sido um fator determinante na dinâmica do fluxo tanto de CO2 quanto do CH4. Os dados deste trabalho reforçam a necessidade da amostragem espacial dos fluxos de CH4 e CO2 em lagos tropical, além de reforçar que estes fluxos podem ser controlados principalmente pela turbidez e pelo pulso de inundação (CO2).
Freshwater ecosystems (lakes, rivers and reservoirs) play an essential role in carbon cycling in the continents. These environments are significant sources of greenhouse gases (GHG), especially carbon dioxide (CO2) and methane (CH4), to the atmosphere. Despite the increase in the number of estimates, the natural GHG emissions dynamics in aquatic environments is still poorly studied, especially in the tropics. The general aim of this work was to estimate the CO2 and CH4 fluxes in a shallow tropical lake with turbidity gradient. The work was conducted in the Sinhá Mariana lake (MT), a wetland lake with the occurrence of two distinct hydrological regions; the lake is connected to the Mutum river (clear water), poor in suspended material with low turbidity, and connected to the Cuiabá River (turbid waters), which features high rate of suspension material. Samples were taken for characterizing the hydrological periods of high and low water. The temporal, spatial variation and the flood pulse shoed to be important factors affecting the CO2 flux, which ranged from -4.95 mmol m-2 d-1 to 282 mmol m-2 d-1. Significant differences were observed from one period to another, with higher emissions during high waters (142 ± 40 mmol m-2 d-1) and lower in the low water (2.3 ± 11.5 mmol m-2 d-1). In addition, the CO2 flux was significantly higher near the Mutum river and lower in the turbid region, in both periods. The total CH4 flux, although estimated only in high waters, showed the highest mean rates in the higher turbidity region of the lake (10.9 ± 6.9 mmol m-2 d-1), followed by the intermediate region (5.1 ± 3.9 mmol m-2 d-1) and the area influenced by clear water (2.5 ± 1.4 mmol m-2 d-1). The ebullition flux was the main CH4 emission pathway, responsible for 78% of the total flux. The turbidity gradient observed along the lake appeared to have been a determining factor in the flux dynamics of both CO2 and CH4. This study data reinforce the need for spatial sampling of CH4 and CO2 fluxes in tropical lakes, in addition to reinforcing that these fluxes can be controlled by turbidity and by the flood pulse (CO2).
Stephan, Ligia Roma [UNESP]. "Comunidades zooplanctônicas em ambientes lênticos tropicais: influência da predação e das características físicas locais." Universidade Estadual Paulista (UNESP), 2017. http://hdl.handle.net/11449/152217.
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Neste estudo foi avaliada a importância das características limnológicas locais e da predação por peixes na estrutura das comunidades zooplanctônicas, sendo os objetivos e resultados apresentados em dois capítulos distintos: Capítulo 1. Tem por objetivo avaliar a influência dos pulsos de inundação na estrutura funcional e taxonômica das comunidades de microcrustáceos em lagoas marginais. Para atingir o objetivo proposto, foram determinadas a estrutura funcional e taxonômica das assembleias de microcrustáceos coletadas em lagoas marginais ao Rio Turvo em três estações distintas: seca, intermediária e chuvosa. Os resultados encontrados foram comparados entre lagoas e entre estações; também foram comparadas a estrutura das asssembléias das lagoas marginais com amostras de microcrustáceos provenientes de ambientes lênticos com diferentes regimes hidrológicos. Neste estudo também foi avaliado se um período longo de estiagem pode influenciar as dinâmicas sazonais dos microcrustáceos. A estrutura das assembleias dos microcrustáceos com base na classificação funcional e taxonômica apresentaram variações entre lagoas e estações, assim como ambientes aquáticos que não sofrem influência dos pulsos de inundação apresentam uma maior uniformidade funcional. A dinâmica sazonal das assembleias foi afetada pelo período prolongado de estiagem, onde as variações na estrutura das comunidades que existem entre estações foram menos intensas no período de estiagem quando comparado ao ano chuvoso. Os resultados mostram que as características limnológicas das lagoas são influenciadas pelos pulsos de inundação e pelo regime hidrológico, bem como um período prolongado de estiagem é capaz de influenciar a dinâmica sazonal das assembléias de microcrustáceos em lagoas marginais. O estudo também mostra que há uma grande heterogeneidade funcional entre as lagoas, sugerindo que o padrão encontrado para a comunidade zooplanctônica revela mais a importância das características locais associadas ao pulso de inundação do que os efeitos deste sobre a comunidade de toda a planície. Capítulo 2. O segundo capítulo tem por objetivo avaliar se a predação por 6 peixes pode influenciar a estrutura funcional das assembleias de microcrustáceos. A influência da predação sobre a comunidade de microcrustáceos foi avaliada por meio de um experimento de mesocosmo e pela avaliação do conteúdo estomacal dos peixes provenientes das lagoas marginais ao Rio Turvo. A abundância e a estrutura funcional dos microcrustáceos foram influenciadas pela presença dos peixes e das macrófitas aquáticas no experimento, entretanto, para as análises realizadas nas lagoas marginais os resultados mostram que a predação não possui um efeito capaz de influenciar a estrutura das assembleias. Como conclusão, podemos inferir que a presença dos peixes pode ser um fator estruturador das comunidades, mas que em ambientes dinâmicos tais como as lagoas marginais, a influência exercida por alterações nas características locais pode ser um fator mais intenso na estruturação das assembleias de microcrustáceos do que a predação por peixes.
In this study, the importance of local characteristics and predation by fish in the zooplankton community structure was evaluated. The objectives and results were separated in two distinct chapters: Chapter 1. Its objective is to evaluate the influence of flood pulses on the functional and taxonomic structure of microcrustacean communities in oxbow lakes. For the proposed objective, the functional and taxonomic structure of the microcrustacean assemblages from oxbow lakes to the Rio Turvo was determined in three seasons: dry, intermediate and rainy. The results were compared between oxbow lakes and between seasons, as well as between samples from environments with different hydrological regimes. In this study, it was also evaluated if a long period of drought can influence the seasonal dynamics of microcrustaceans. The structure of the microcrustacean assemblages based on the functional and taxonomic classification showed variations between oxbow lakes and seasons; a greater functional uniformity was found on the aquatic environments not influenced by the flood pulses. The seasonal dynamics of the assemblages was affected by the prolonged period of drought, where the variations in the structure of communities between seasons were less intense in the drought year when compared to the rainy year. Our results show the influence of flood pulses on limnological characteristics and on the functional and taxonomic assemblages of microcrustaceans in the oxbow lakes; we also observed that a prolonged period of drought is able to influence the seasonal dynamics of microcrustacean assemblages in oxbow lakes. Chapter 2. The second chapter aims to assess the influence of fish predation on the functional structure of microcrustacean assemblages. The influence of fish predation was evaluated through an mesocosm experiment, and through an evaluation of fish stomach contents sampled in the marginal lakes from Turvo River. In the experiment, the abundance and functional structure of the microcrustaceans were influenced by the presence of fish and aquatic macrophytes, however, results from the oxbow lakes show that predation does not have an effect capable to incluence the structure of the microcrustaceans assemblages. As conclusion, fish predation should have a role in the 8 structure of the communities, although in dynamic environments such as oxbow lakes, the influence of the local characteristics may be a more important factor in the structuring of the microcrustacean assemblages then the fish predation.
REY, ESPINASSE JEANNE. "Contribution a l'etude du zooplancton d'altitude et de la taxonomie des cladoceres." Toulouse 3, 1986. http://www.theses.fr/1986TOU30185.
Повний текст джерелаFerreira, Gustavo Luiz. "Análise da composição da dieta de seis espécies de peixes coexistentes em um reservatório tropical (Reservatório de Ribeirão das Lajes, Piraí-RJ)." Universidade do Estado do Rio de Janeiro, 2010. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=4305.
Повний текст джерелаThe present study analyzed the digestive contents of 221 individuals of six fish species, from Ribeirão das Lajes reservoir (Piraí-RJ). There were 44 specimens of Loricariichthys castaneus, 56 Parauchenipterus striatulus, 46 Metynnis maculatus, 40 Astyanax bimaculatus, 31 Astyanax parahybae and 4 Rhamdia quelen. The aim was to establish their diets, through the use of alimentary importance index (IAi), to verify the existence of differences in their feeding between different seasons of the year, and their trophic relationships to their environment. There were no great alterations to the diets of the analyzed species between the seasons of the year. All species used similar food resources, which could be divided into two groups: one composed of species with omnivorous habits with tendencies to insectivory and which apply allochthonous resources in their diets, formed by A. bimaculatus, A. parahybae e P. striatulus and another one with L. castaneus, R. quelen e M. maculatus that presented larger amplitudes of ingested items, which many items were associated with the substratum and a few to the water column. There is an alimentary overlap between the omnivorous species, however the great availability of food resources, capable of being exploited by the fishes in this reservoir, probably diminishes competition for food. Moreover the species also exploited different kinds of secondary food items.
Kristen, Iris. "Investigations on rainfall variability during the late Quaternary based on geochemical analyses of lake sediments from tropical and subtropical southern Africa." Potsdam Deutsches GeoForschungsZentrum GFZ, 2010. http://d-nb.info/1000714233/34.
Повний текст джерелаDunn, Ryan J. K. "Biogeochemical Processes of a Sub-tropical Coastal Lagoon (Coombabah Lake, Southern Moreton Bay, Australia): With Emphasis on Organic Matter and Nutrient Dynamics." Thesis, Griffith University, 2009. http://hdl.handle.net/10072/365282.
Повний текст джерелаThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Engineering
Science, Environment, Engineering and Technology
Full Text
Rocha, Rinaldo José da Silva. "Decomposição de macrófitas aquáticas em dois reservatórios com diferentes estados tróficos." Universidade Federal de São Carlos, 2012. https://repositorio.ufscar.br/handle/ufscar/2078.
Повний текст джерелаFinanciadora de Estudos e Projetos
The macrophytes are essential for the development and maintenance of food webs, to carbon dynamics and nutrient cycling in tropical aquatic systems. After senescence and plant death, decomposition of organic detritus depends heavily on their elemental compositions. Thus, the present study aimed to evaluate the effect of seasonality and trophic state of reservoirs and Vigário Lajes on the mass losses of detritus of Salvinia auriculata, Pistia stratiotes, Eichhornia crassipes, Sagittaria montevidensis and Brachiaria subquadripara, the influence of elemental composition of debris on the coefficients decay of carbon, nitrogen and phosphorus, and the stoichiometric ratios between these elements during the decomposition process. Over 120 days, the richest detritus in nutrients and less refractory (S. montevidensis and P. stratiotes) showed a biphasic pattern of decay and the greater decay of carbon (70-90%), phosphorus (90-96%) and nitrogen (68-94%). The poorest and refractories detritus (S. auriculata and E. crassipes) had lower rates of decay, with monophasic and biphasic patterns and lower mass loss in carbon-based (20-34%), phosphorus-based (26%), and nitrogen-based (10- 37%). As for the difference between the environments, the total mass loss of carbon was up to 70% higher during the rainy season (Sept/10 to Jan/11) and 27% higher in the dry season (may/11 to Sep/11) for detritus S. auriculata incubated in the reservoir Vigário; for the detritus of B. subquadripara total mass loss was also greater in this reservoir, reaching 58% in the rainy season and 36% during the dry season. The minor differences between the environments occurred in the mass loss of carbon detritus of S. montevidensis, (ca. 1.3% and 0.3% in rainfall in the dry season) and P. stratiotes (ca. 5.3% in the rainy season and 5.5% in the dry season). Yet these detritus showed the greatest losses of phosphorus (90-95%) and nitrogen (68-94%) in both experiments. The minor differences between the environments occurred in the mass loss of carbon detritus of S. montevidensis, (ca. 1.3% and 0.3% in the rainy season in the dry season) and P. stratiotes (ca. 5.3% and 5.5% in the rainy season in the dry season). Yet these detritus showed the greatest losses of phosphorus (90-95%) and nitrogen (68-94%) in both experiments. The ratio between carbon and nitrogen was higher in detritus of S. auriculata and E. crassipes in oligotrophic reservoir, and lower in detritus of S. montevidensis and P. stratiotes, whose mass loss coefficients (k) were higher.
As macrófitas são essenciais para o desenvolvimento e manutenção das cadeias tróficas, para a dinâmica do carbono e ciclagem de nutrientes de sistemas aquáticos tropicais. Após senescência e morte das plantas, a decomposição dos detritos orgânicos depende muito das suas composições elementares. A temperatura, a concentração de nutrientes inorgânicos no meio, as relações estequiométricas entre os organismos decompositores e os detritos podem afetar as taxas de decomposição, embora no caso da relação estequiométrica isso nem sempre ocorra. Nesse sentido, esse estudo teve como objetivo avaliar o efeito da sazonalidade e da condição de trofia dos reservatórios de Lajes e de Vigário sobre as perdas de massa dos detritos de Salvinia auriculata, Pistia stratiotes, Eichhornia crassipes, Sagittaria montevidensis e Brachiaria subquadripara; a influência da composição elementar dos detritos sobre os coeficientes de decaimento de carbono, nitrogênio e fósforo; e as relações estequiométricas entre esses elementos durante o processo de decomposição. Ao longo de 120 dias, os detritos mais ricos em nutrientes e menos refratários (S. montevidensis e P. stratiotes) apresentaram padrão bifásico de decaimento, além dos maiores decaimentos de carbono (70 a 90%), fósforo (90 a 96%) e nitrogênio (68 a 94%). Os detritos mais pobres e refratários (S. auriculata e E. crassipes) apresentaram menores coeficientes de decaimento, com padrões monofásico e bifásico e as menores perdas de massa em base de carbono (20 a 34%), de fósforo (26%) e de nitrogênio (10 a 37%). Quanto à diferença entre os ambientes, a perda de massa total de carbono foi até 70% maior no período das chuvas (set/10 a jan/11) e 27% maior no período seco (mai/11 a set/11) para detritos de S. auriculata incubados no reservatório de Vigário; para os detritos de B. subquadripara a perda de massa total também foi maior neste reservatório, chegando a 58% no período das chuvas e 36% no período seco. As menores diferenças entre os ambientes ocorreram na perda de massa de carbono dos detritos de S. montevidensis , (ca. 1,3% nas chuvas e 0,3% na seca) e de P. stratiotes (ca. 5,3% nas chuvas e 5,5% na seca) .Contudo, esses detritos apresentaram as maiores perdas de fósforo (90 a 95%) e de nitrogênio (68 a 94%) nos dois experimentos. A razão entre carbono e nitrogênio foi mais alta nos detritos de S. auriculata e E. crassipes, no ambiente oligotrófico, e mais baixa nos detritos de S. montevidensis e P. stratiotes, cujos coeficientes de perda de massa (k) foram maiores.
França, Roberta Sebastiany. "Estudo limnológico da Lagoa dos Tropeiros, Capitólio, MG, com ênfase na comunidade de macroinvertebrados bentônicos." Universidade Federal de São Carlos, 2010. https://repositorio.ufscar.br/handle/ufscar/1664.
Повний текст джерелаFinanciadora de Estudos e Projetos
The studies on the diversity and functional role of benthic macroinvertebrates in lake ecosystems can provide relevant informations regarding the functioning and the health of these freshwater ecosystems. The aim of this study was to analyze the Tropeiros Lake, located in the municipality of Capitólio (MG), performing a limnological evaluation of the ecosystem and ecological investigation on the diversity of the benthic macroinvertebrate community. Thus, changes in the taxonomical composition, abundance, diversity, biomass and the taxa participation in the trophic functional groups were analyzed. Water and sediment were sampled in October 2006 and 2007 (dry periods) and in March 2007 and 2008 (rainy periods). The results evidenced that Tropeiros Lake is a shallow environment with maximum depth of 3 m, densely colonized by macrophytes and with high water transparency. It has low concentration of nitrogen with predominance of the ammonium ion, low concentrations of phosphorus being organic phosphate the predominant compound, low pH values with water varying from neutral to slightly acid and moderate water electrical conductivity. The sediment has high clay and organic matter contents. The Discriminant Analysis separated the sampling periods, grouping the similar rainy periods but separating the dry ones. According to the trophic state index the lake was classified as oligotrophic during the rainy periods and mesotrophic during the dry periods. Benthic community was composed by 81 taxa, mainly represented by the members of the Order Diptera, especially those belonging to the families Chironomidae and Chaoboridae. The trophic guild of collectors was the most representative, with minimum abundance of 57.2%, with the taxa Chironomus sp, Goeldichironomus sp and Tanytarsus sp, followed by that of the predators, having Chaoborus and Ablabesmyia sp as the main taxa. The mean biomass determined for the macroinvertebrate community of Tropeiros Lake was 0.94 g. m-2. Except Chironomus sp, that was abundant, regarding both, numbers and biomass, a different condition was observed for the taxa as Pisidium pulchellum, Melanoides tuberculata and a Libellulidae nymph that were numerically less abundant but contributed significantly for the total biomass. Regarding the trophic guilds, predators was more representative in the periods of October 2006 and March 2007 than the collector guild, in terms of biomass. The same was observed regarding the macroinvertebrates contribution to the biomass in each trophic guild, where predators were more abundant than collectors in October 2006 and March 2007, evidencing the importance of this approach in ecological studies. The method based on K-dominance curves (ABC curves) indicated that Tropeiros Lake is under moderate perturbation according to the cumulative values of abundance and biomass. This results corroborates those obtained for lake trophic state index, based on the mean biomass when compared to environments of different trophic states and with the species composition, formed by both, group of tolerant species as well as those more sensible to adverse environmental conditions.
A diversidade e o papel funcional dos táxons que compõem a comunidade de macroinvertebrados bentônicos dos sistemas lacustres podem fornecer informações importantes sobre a saúde e funcionamento destes ecossistemas de água doce. O objetivo deste estudo foi analisar limnologicamente a Lagoa dos Tropeiros, em Capitólio (MG), e realizar um estudo ecológico da diversidade dos macroinvertebrados bentônicos, avaliando a densidade, abundância, biomassa e participação dos táxons nas guildas tróficas funcionais. Para isso foram avaliadas as mudanças na composição taxonômica, na diversidade e na ocorrência sazonal da comunidade bentônica desse sistema. As amostras de água e de sedimento foram coletadas em outubro de 2006 e de 2007 (períodos secos) e em março de 2007 e de 2008 (períodos chuvosos). Os resultados indicaram que a lagoa caracterizou-se como sendo um ambiente raso, com profundidade máxima de 3m, grande quantidade de macrófitas aquáticas, elevada transparência da água, reduzidas concentrações de compostos de nitrogênio, com predominância do íon amônio, e baixas concentrações de fósforo com predomínio de fosfato orgânico, valores de pH variando de neutros a ligeiramente ácidos, condutividade moderada e elevados teores de argila e de matéria orgânica no sedimento. A Análise Discriminante evidenciou a separação dos períodos de amostragem, sendo que os períodos chuvosos foram muito semelhantes, diferentemente do observado para os períodos secos que se diferenciaram por diferentes características ambientais. De acordo com o Índice de Estado Trófico a lagoa foi classificada como um ambiente oligotrófico durante os períodos chuvosos e mesotrófico durante os períodos de seca. A comunidade bentônica foi composta por 81 táxons, sendo representada principalmente por organismos pertencentes à ordem Diptera, especialmente das famílias Chironomidae e Chaoboridae. A guilda trófica dos coletores foi a mais representativa, com abundância mínima de 57,2%, sendo os principais representantes os táxons Chironomus sp, Goeldichironomus sp e Tanytarsus sp, seguida pelos predadores com Chaoborus sp e Ablabesmyia sp como os principais táxons. A biomassa média calculada para a comunidade de invertebrados bentônicos na lagoa foi de 0,94 g. m-2. Com exceção de Chironomus sp, que foi abundante em termos de número de indivíduos e também de biomassa, observou-se uma condição diferente para táxons como Pisidium pulchellum, Melanoides tuberculata e uma ninfa de Libellulidae os quais foram pouco abundantes numericamente, mas apresentaram uma elevada participação na composição da biomassa total. O mesmo foi observado para a participação dos macroinvertebrados em biomassa nas guildas tróficas, onde os predadores foram mais abundantes que os coletores em outubro de 2006 e março de 2007, demonstrando a importância dessa abordagem em estudos ecológicos. O método baseado em curvas de k-dominância (curvas ABC) indicou que a Lagoa dos Tropeiros encontra-se moderadamente perturbada, de acordo com os valores cumulativos de abundância de indivíduos e biomassa. Tal resultado confirma aqueles obtidos para o índice de estado trófico, para os valores de biomassa média quando comparados com ambientes de diferentes graus de trofia e com a composição das espécies presentes, formada tanto por grupos tolerantes como também por aqueles mais sensíveis às condições ambientais adversas.
Kristen, Iris [Verfasser]. "Investigations on rainfall variability during the late Quaternary based on geochemical analyses of lake sediments from tropical and subtropical southern Africa / Iris Kristen. Deutsches GeoForschungsZentrum GFZ." Potsdam : Deutsches GeoForschungsZentrum GFZ, 2010. http://d-nb.info/1000714233/34.
Повний текст джерелаGuiguen, Yann. "Approches morphologique, histologique et endocrinienne des cycles reproducteurs et de l'inversion sexuelle chez un poisson hermaphrodite protandre : le loup tropical, lates calcarifer, introduit en elevage en polynesie francaise." Rennes 1, 1992. http://www.theses.fr/1992REN10133.
Повний текст джерелаMartins, Renato Tavares. "Colonização de Oligochaeta e outros macroinvertebrados durante a decomposição de Eichhornia azurea (SW.) Kunth (Pontederiaceae) e Salvinia auriculata Aubl. em um sistema lêntico na região tropical." Universidade Federal de Juiz de Fora (UFJF), 2009. https://repositorio.ufjf.br/jspui/handle/ufjf/2820.
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O presente estudo foi composto por dois experimentos, o objetivo do primeiro deles verificar a colonização de Oligochaeta ao longo da decomposição da macrófita Eichhornia azurea (Sw.) Kunth, no segundo experimento, analisou-se a estrutura faunística dos macroinvertebrados no decorrer da decomposição de E. azurea e Salvinia auriculata Aubl. O experimento 1 foi dividido em dois períodos (1º período: setembro a novembro de 2007; 2º período: fevereiro a abril de 2008), em cada um deles, 21 sacos de náilon contendo 10 g de folhas de E. azurea, foram colocados no lago, e retirados após 2, 5,8, 12, 25, 45, e 65 dias. No experimento 2 (novembro de 2007 a fevereiro de 2008), foram utilizados 60 sacos de náilon, 30 deles com 10 g de folhas de E. azurea, e os demais contendo a mesma quantidade de folhas de S. auriculata. Após 30 minutos, 2, 4, 8, 12, 24, 36, 48, 60 e 72 dias os sacos foram retirados do lago. Em ambos os experimentos, após serem retirados do lago, os sacos foram levados ao laboratório, e o material remanescente fixado em formol 4%, lavado e triado, os organismos encontrados foram identificados e conservados em álcool 70%. No experimento 1, o maior coeficiente de decomposição (K) foi observado no primeiro período (K= 0,023 d-1 ) em relação ao segundo (K= 0,018 d-1 Palavras–Chave: Chironomidae, Lago dos Manacás, macrófitas, Naididae, relação carbono:nitrogênio ), no entanto, não houve diferença significativa. Observou-se o aumento da densidade e riqueza dos Oligochaeta ao longo do estudo em ambos os períodos. Naididae foi a família dominante, estes organismos por possuírem a capacidade de se locomover na coluna d'água próximo ao substrato, mostraram-se melhores colonizadores do que Enchytraeidae e Tubificidae. No experimento 2, ao final dos 72 dias, observou-se menor biomassa total de E. azurea (2,65 g MS) em relação à S. auriculata (5,10 g MS), sendo que na primeira macrófita registrou-se a diminuição da relação carbono: nitrogênio durante o estudo, enquanto que em S. auriculata não foi observada a diminuição desta razão. Chironomidae e Naididae foram as famílias com maiores densidades, representando mais de 95% da fauna em ambas as macrófitas. Os coletores foram o grupo funcional mais abundante em E. azurea e S. auriculata, confirmando a predominância destes organismos nas folhas em decomposição na região tropical.
The present study was composed of two experiments. The first with the objective to verify the colonization of Oligochaeta during decomposition of the macrophyte Eichhornia azurea (Sw.) Kunth, while the second experiment analized the faunistic struture of the macroinvertebrates along decomposition of E. azurea and Salvinia auriculata Aubl. Experiment 1 was divided into two periods (1st period: September to November 2007; 2nd period: February to April 2008). In each period, 21 nylon bags containing 10 g of dry leaves of E. azurea, were placed in the lake, and removed at intervals of 2, 5,8, 12, 25, 45, and 65 days. In experiment 2 (November 2007 to February 2008), 60 nylon bags were used, 30 of them filled with 10 g of dry leaves of E. azurea and the others, containing the same amount of dry leaves of S. auriculata. After intervals of 30 minutes, 2, 4, 8, 12, 24, 36, 48, 60 and 72 days the bags were taken out of the lake. In both experiments, after out of the lake, the bags were taken to the laboratory, and the remanescent material was fixed in a formol solution 4%, washed and sorted. The organisms were identified and preserved in 70% alcohol. In experiment 1, the highest decomposition coefficient (K) was observed in the first period (K= 0.023 d-1) in relation to the second (K= 0.018 d-1 ), however with no significant difference. An increase of density and richness of Oligochaeta along the study was observed in both periods. Naididae was the most dominant family, represented by the genera Allonais, Chaetogaster, Dero and Pristina. These organisms, for their ability of moving themselves in the water column, near the substrate, showed to be better colonizers than Enchytraeidae and Tubificidae. In experiment 2, at the end of the 72 days, it was observed a small fraction of total biomass of E. azurea (2.65 g DM) in relation to S. auriculata (5.10 g DM), whereas in the first macrophyte it was registered a decrease of the carbon: nitrogen relationship during the study, while in S. auriculata it was not observed the decrease of this rate. Chironomidae and Naididae were the families with the higher densities, representing more than 95% of the fauna in both macrophytes. The collectors were the most abundant functional group in E. azurea and S. auriculata, attesting to the predominance of these organisms in the leaves in decomposition in the tropical region.
Silva, Raquel Lemos da. "EvoluÃÃo morfodinÃmica e hidrolÃgica direcionada ao manejo de lagoas costeiras tropicais. Estudo de caso: lagoa das almÃcegas, Paraipaba - Trairi/Ce." Universidade Federal do CearÃ, 2007. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=1687.
Повний текст джерелаA lagoa costeira, AlmÃcegas, està localizada no litoral Oeste do Estado do Cearà na divisa dos municÃpios de Trairi e Paraipaba. O principal objetivo deste trabalho foi avaliar a evoluÃÃo os processos controladores da morfologia e hidrologia da Lagoa das AlmÃcegas visando gerar informaÃÃes Ãteis ao uso e gestÃo desse recurso hÃdrico costeiro. A origem da lagoa das AlmÃcegas està subordinada ao comportamento climÃtico-natural da Ãrea, bastante influenciado pela dinÃmica litorÃnea. Com a gÃnese relacionada aos processos transgressivos e regressivos do mar, e barramento do riacho pelo sistema de dunas (transporte eÃlico) e processos associado (descarga fluvial), sendo posteriormente com a construÃÃo da barragem. A metodologia utilizada para realizaÃÃo desta pesquisa baseia-se na compreensÃo da organizaÃÃo da natureza dentro do espaÃo, e a relaÃÃo que ocorre entre seus componentes. Para tanto foram realizadas analises dos parÃmetros fÃsicos e quÃmicos da Ãgua: temperatura, condutividade elÃtrica, turbidez, pH e transparÃncia. Ademais, foram coletadas amostras de subsuperfÃcie e fundo para a investigaÃÃo de material em suspensÃo. TambÃm, realizou-se a caracterizaÃÃo sedimentolÃgica, analise de matÃria orgÃnica e metaisâtraÃo (cobre, cÃdmio e zinco) no sedimento, e o estudo morfomÃtrico e levantamento batimÃtrico da lagoa. Os resultados demonstram que o sistema estudado apresentou variaÃÃo sazonal relacionada aos dois perÃodos hidrolÃgicos distintos. O perÃodo chuvoso se caracterizou por precipitaÃÃes mais intensas e menor insolaÃÃo, enquanto que o seco apresentou maior insolaÃÃo e maiores velocidades dos ventos, trazendo conseqÃÃncias diretas sobre o nÃvel dâÃgua da lagoa. A coluna dâÃgua apresentou estratificaÃÃo (tÃrmica) significativa devido principalmente à profundidade do sistema, à atuaÃÃo dos ventos e transparÃncia da coluna dâÃgua. A composiÃÃo granulomÃtrica dos sedimentos de fundo da Lagoa das AlmÃcegas resultaram em seis classes principais: areia com cascalho esparso (43,8 %), areia (25%), areia fina (6,3%), areia siltosa (6,3%), areia lamosa (6,3%), silte (6,3%) e silte arenoso (6,3%). Observa-se que as fraÃÃes grossas do sedimento, maiores que 0,063 mm, ocorrem na grande maioria das amostras, o que pode està relacionado ao processo de assoreamento. A distribuiÃÃo da matÃria orgÃnica indica os diferentes graus de aeraÃÃo das diversas Ãreas do ambiente de sedimentaÃÃo. Quanto à morfologia a lagoa apresentando uma Ãrea de 1,3 km2, perÃmetro de 9,935 Km, largura mÃxima de 684 m e comprimento de 3,5 km, volume de 6.688.000 mÂ, profundidade mÃxima de 5,85 m, profundidade mÃdia de 2,55m. A relevÃncia do volume classifica este reservatÃrio como de capacidade de armazenamento satisfatÃrio. Em termos de ocupaÃÃo, a lagoa encontra-se com baixa ocupaÃÃo imobiliÃria, devido principalmente a pouca especulaÃÃo. Mas, as ocupaÃÃes que jà ocorrem na regiÃo ultrapassam os limites impostos pela lei (Ãreas de PreservaÃÃo Permanente), jà a ocupaÃÃo associada à retirada da cobertura vegetal à possÃvel de ser vista, e este problema pode gerar uma instabilidade das margens e conseqÃente alteraÃÃo das caracterÃsticas morfomÃtricas e fÃsicoquÃmicas da lagoa, podendo ocasionar impactos negativos, como aumento do escoamento superficial, erosÃo das margens, maior aporte de sedimentos na lagoa, assoreamento, diminuiÃÃo do volume de Ãgua, e maior concentraÃÃo de poluentes na lagoa, podendo vir a comprometer tambÃm a vida da populaÃÃo local.
The coastal lagoon, AlmÃcegas, are located in the coastal West of the State of the Cearà in the verge of the cities of Trairi and Paraipaba. The main objective of this work was to evaluate the evolution the controlling processes of the morphology and hidrology of the Lagoon of the AlmÃcegas being aimed at to generate useful information to the use and management of this coastal hÃdrico resource. The origin of the lagoon of the AlmÃcegas is subordinated to the climatic-natural behavior of the area, sufficiently influenced for the littoral dynamics. With genesis related to the transgression and regression processes of the sea, and slide bars of the extended river for the dune system (aeolian transport) and processes associated (fluvial discharge), being later with the construction of the barrage. The methodology used for accomplishment of this research is based inside on the understanding of the organization of the nature of the space, and the relation that occurs between its components. For they had been in such a way carried through you analyze of the physical and chemical parameters of the water: temperature, electric condutividade, turbidez, pH and transparency. Furthermore, had been collected samples of deep subsurface and for the inquiry of material in suspension. Also, it was become fullfilled sedimentation characterization, analyzes of organic substance and metal-traces (it has covered, cadmium and zinc) in the sediment, and the morfomÃtrico study and batimÃtrico survey of the lagoon. The results demonstrate that the studied system presented related sazonal variation to the two distinct hidrolÃgicos periods. The rainy period if characterized for more intense precipitations and lesser insolation, whereas the dry one presented greater insolation and greaters speeds of the winds, bringing direct consequences on the water level of the lagoon. The water column presented stratification (thermal) significant had mainly to the depth of the system, to the performance of the winds and transparency of the water column. The grain sized composition of the sediments of deep of the Lagoon of the AlmÃcegas had resulted in six main classrooms: slightly gravelly sand (43.8%), sand (25%), fine sand (6.3%), muddy sand (6.3%), slightly gravelly muddy sand (6.3%), silt (6.3%) and sandy silt (6.3%). It is observed that the thick fractions of the sediment, greaters that 0,063mm, occur in the great majority of the samples, what it can is related to the silting. The distribution of the organic substance indicates the different degrees of aeration of the diverse areas of the sedimentation environment. How much to the morphology the lagoon presenting an area of 1,3km2, perimeter of 9,935Km, maximum width of 684m and length of 3,5km, Volume of 6.688.000m Â, maximum depth of 5,85m, average depth of 2,55m. The relevance of the volume classifies this reservoir as of capacity of satisfactory storage. In occupation terms, the lagoon meets with low real estate occupation, had mainly to little speculation. But, the occupations that already occur in the region exceed the limits taxes for the law (Areas of Permanent Preservation) already the occupation associated with the withdrawal of the vegetal covering are possible of being seen, and this problem can generate an instability of the edges and consequence the alteration of the morfomÃtricas characteristics and physicistchemistries of the lagoon, being able to cause negative impacts, as increase of the superficial draining, erosion of the edges, greater arrives in port of sediments in the lagoon, assoreamento, reduction of the volume of water, and greater concentration of pollutants in the lagoon, being able to come also compromising the life of the population place.
Dile, Yihun. "Intensifying Agricultural Water Management in the Tropics : A cause of water shortage or a source of resilience?" Doctoral thesis, Stockholms universitet, Stockholm Resilience Centre, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-102878.
Повний текст джерелаAt the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 2: Manuscript. Paper 3: Manuscript. Paper 5: Epub ahead of print. Paper 6: Manuscript.
Water resources management and social-ecological resilience
Ishak, Mohd Yusoff. "Predictive modelling of eutrophication and algal bloom formation in tropical lakes." Thesis, 2012. http://hdl.handle.net/2440/78097.
Повний текст джерелаThesis (Ph.D.) -- University of Adelaide, School of Earth and Environmental Sciences, 2012
Lininger, Katherine Blom. "The hydro-geomorphology of the middle Araguaia River: floodplain dynamics of the largest fluvial system draining the Brazilian Cerrado." 2013. http://hdl.handle.net/2152/21826.
Повний текст джерелаtext
Collins, Geoffrey M. "Phenotypic drivers of hypoxia tolerance in a tropical diadromous fish (Lates calcarifer)." Thesis, 2016. https://researchonline.jcu.edu.au/48866/1/48866-collins-2016-thesis.pdf.
Повний текст джерела"Impact of bike lanes and sidewalk improvements in New Orleans, Louisiana." Tulane University, 2013.
Знайти повний текст джерелаMoore, Randall Phillips 1965. "Biogeographic and experimental evidence for local scale dispersal limitation in central Panamanian forest birds." Thesis, 2005. http://hdl.handle.net/1957/1407.
Повний текст джерелаI examined the avian biogeography of the islands of Lago Gatun, Panama, in an effort to better understand the effects of forest fragmentation in this biodiverse region, and specifically to understand the importance of fragment isolation and the mechanism behind its effects on tropical bird distribution. I combined exhaustive surveys of 29 islands with an experimental release program. Analyses of these data were conducted in a hierarchical fashion to evaluate evidence for avian dispersal limitation at multiple scales. First, I assessed the potential roles of area and isolation in determining avian species richness across this series of fragments, and how these relationships may differ for edge and forest dependent birds. Next, I analyzed community structure and species distributions to determine the relative contributions of island area and isolation in creating patterns of species-specific insular occurrence. Lastly, I assessed the results of the experimental investigation to evaluate the hypothesis that dispersal limitation explains the insular distribution patterns of several tropical forest birds. Isolation is a significant predictor of avian species richness, but only after accounting for the stronger effect of area. Species-isolation relationships are different in this archipelago for birds that rely on forest and edge habitats, respectively. Species-specific distributions are significantly nested when islands are ordered by area, and by isolation once the effect of area is considered. Occurrence of most forest species is sensitive to area and isolation of the archipelago. Examination of guild structure suggests that multiple mechanisms are responsible for these occurrence patterns. There are distinct species-specific differences in ability to cross small gaps, and species which are better able to cross these gaps are more widely distributed across the archipelago than those species that negotiate the same barriers poorly. Species that performed uniformly well in release experiments were much less likely to have suffered insular extinction in the preceding 25 years than those species that showed moderate to poor experimental performance. There is strong evidence of a morphological basis for the patterns. The cumulative evidence from these analyses is the most comprehensive evidence to date of local-scale dispersal limitation in volant birds.
McCullough, Gregory Keith. "Circulation of terrestrial runoff and its suspended load in a large tropical lake : a study of processes and effects near the mouth of the Linthipe River in Lake Malawi." 2006. http://hdl.handle.net/1993/20912.
Повний текст джерелаBalston, Jacqueline Marie. "An examination of the impacts of climate variability and climate change on the wild barramundi (Lates calcarifer): a tropical estuarine fishery of north-eastern Queensland, Australia." Thesis, 2007. https://researchonline.jcu.edu.au/2060/1/01front.pdf.
Повний текст джерелаBalston, Jacqueline Marie. "An examination of the impacts of climate variability and climate change on the wild barramundi (Lates calcarifer) : a tropical estuarine fishery of north-eastern Queensland, Australia /." 2007. http://eprints.jcu.edu.au/2060.
Повний текст джерелаKristen, Iris [Verfasser]. "Investigations on rainfall variability during the late Quaternary based on geochemical analyses of lake sediments from tropical and subtropical southern Africa / vorgelegt von Iris Kristen." 2009. http://d-nb.info/995396264/34.
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