En el océano, las condiciones ambientales adversas independientes de la predación tienen como resultado la muerte y lisis celular del fitoplancton que resulta en la liberación de carbono orgánico disuelto (PDOC) a la columna de agua. Las comunidades bacterianas heterotróficas marinas, normalmente dependientes de esta fuente de carbono para su metabolismo, obtienen un beneficio de la liberación de carbono recién sintetizado a la vez que participan en su reciclaje a través de la red trófica microbiana. A pesar de la repercusión que este proceso puede tener en el ciclo del carbono en los océanos, actualmente se desconoce cual es su contribución en ambientes marinos naturales y en el actual escenario de cambio global. El principal objetivo de esta tesis fue analizar las relaciones existentes entre la mortalidad de células del fitoplancton, la proporción de carbono orgánico disuelto (DOC) liberado por el fitoplancton y la supervivencia microbiana bajo diversas condiciones ambientales. La salud de comunidades naturales fitoplanctónicas y bacterianas, la producción primaria total y la liberación fitoplanctónica de DOC fueron determinadas in situ en diferentes regiones oceánicas que comprendieron los mares Mediterráneo, Ártico, Antártico y Atlántico. Los resultados obtenidos en este estudio demostraron la existencia de una relación entre condiciones ambientales tales como la temperatura del agua y la disponibilidad de nutrientes en la muerte celular del fitoplancton. Además, la mortalidad celular del fitoplancton determinada en estos ambientes puede explicar un 41.4% de la PDOC relativa a la producción primaria total, y en regiones oceánicas oligotróficas del noroeste del Océano Atlántico, este proceso sustentó una alta viabilidad bacteriana. Los resultados obtenidos durantes esta tesis resaltan el crucial papel de la lisis celular del fitoplancton en los océanos y ayudan a comprender cuales son las principales vías de transferencia de carbono desde la fotosíntesis hasta el metabolismo heterotrófico bacteriano. / Important phytoplankton losses by cell death, independent of grazing are occurring in the ocean. Phytoplankton cells have been described to die upon encountering adverse environmental conditions, and cell death and lysis would result in the release of the carbon incorporated in the photosynthesis by the phytoplankton as dissolved organic carbon (PDOC). The availability of dissolved organic carbon (DOC) is a major constraint for the heterotrophic bacteria, consequently the release by cell mortality of the recently photosynthate carbon is expected to benefit the bacterial community and should be channelled through the microbial food web. All this processes have been poorly documented and the contribution of the phytoplankton cell death to the release of PDOC has not been yet explored in natural communities. The goal of this PhD Thesis is to provide quantitative information on phytoplankton and bacteria cell death in natural communities and to document the fraction of DOC released by phytoplankton (PDOC) under contrasting natural conditions. The exploration of the relationships between the phytoplankton cell mortality, DOC released by phytoplankton (PDOC) and microbial survival would contribute to better understand the path of carbon from photosynthesis to heterotrophic bacteria by cell death processes. Contrasting environmental conditions and communities from different oceanic regions including the Mediterranean Sea, Arctic, Antarctic and Atlantic oceans were studied. Evaluations of the in situ health status of the natural phytoplanktonic communities and bacteria were analyzed by testing the cell membrane permeability; a property that define cell death in cell biology. The total primary production, and the DOC production by phytoplankton were quantified to explore its dynamic with regard to the variability in phytoplankton cell mortality. The bacterial cell survival was also assessed under the same contrasting conditions mediating by the quantification of percentage of living heterotrophic bacteria. The proportion of dead of phytoplankton cells from the diverse phytoplankton populations encountered in the different communities, were related to environmental conditions as water temperature and nutrients availability, and helped to identify their competitive success. Consistent proportions of dead natural phytoplanktonic cells were found during this study that could represent in average about half of the total (40.5 %) phytoplankton abundance. Phytoplankton mortality constitutes a major process implicated in the production of dissolved organic carbon, as the percentage of phytoplankton dead cells explained the 41.4 % of the percentage of released production (PDOC) relative to total primary production. The large production of PDOC observed here, represented in average the half of the total primary production (54.4%) and supported, at the oligotrophic NE Atlantic Ocean, a higher bacterial viability.

Aquesta tesi tracta sobre l'efecte de la contaminació per cru de petroli sobre l'ecosistema costaner mediterrani i sobre el paper fonamental dels sediments marins en la regulació i el manteniment dels processos biogeoquímics. L'estudi presta especial atenció a les comunitats bacterianes reductores de sulfat i la seva implicació en la degradació de contaminants orgànics. La diversitat, abundància i fisiologia dels bacteris reductors de sulfat que habiten el sediment arenós del nord de Mallorca (Illes Balears), van ser analitzades mitjançant un enfocament polifàsic, basat en la combinació d'experiments in situ i in vitro, biologia molecular clàssica i d’última generació, cultius i determinació d'activitats metabòliques. Els resultats obtinguts durant aquesta tesi demostren que el sediment mediterrani alberga una microbiota autòctona que podria prosperar després d'un vessament de cru de petroli i el paper de la qual podria ser crucial per a la transformació i l'eliminació de compostos orgànics xenobiòtics en aquest ambient. / Esta tesis trata sobre el efecto de la contaminación por crudo de petróleo en el ecosistema costero mediterráneo y sobre el papel fundamental de los sedimentos marinos en la regulación y el mantenimiento de los procesos biogeoquímicos. El estudio presta especial atención a las comunidades bacterianas reductoras de sulfato y a su implicación en la degradación de contaminantes orgánicos. La diversidad, abundancia y fisiología de las bacterias reductoras de sulfato que habitan el sedimento arenoso del norte de Mallorca (Islas Baleares), fueron analizadas mediante un enfoque polifásico, basado en la combinación de experimentos in situ e in vitro, biología molecular clásica y de última generación, cultivos y determinación de actividades metabólicas. Los resultados obtenidos durante esta tesis demuestran que el sedimento mediterráneo alberga una microbiota autóctona que podría prosperar después de un derrame de crudo de petróleo y cuyo papel podría ser crucial para la transformación y la eliminación de compuestos orgánicos xenobióticos en este ambiente. / This thesis discusses the fate and behave of crude oil contamination in the Mediterranean coastal ecosystem, and the essential role of the marine sediments in the regulation and maintenance of biogeochemical processes. The study pays particular attention to the role of sulphate reducing bacterial communities in the degradation of organic matter and pollutants entering the Mediterranean environment. A polyphasic approach based in the combination of in situ and in vitro experiments, next generation and classical molecular biology, cultivation, and the determination of metabolic activities, provided first insights into the diversity, abundance and physiology of sulphate reducing bacteria inhabiting the undisturbed sandy sediment at the north of Mallorca (Balearic Islands). The results obtained during the thesis demonstrate that the undisturbed Mediterranean sediment harbours an autochthonous microbiota that could prosper after a crude oil spill and which role might be crucial for the transformation and removal of hazardous organic compounds in this environment.

GONÇALVES, Fabrício Mota. Evapotranspiração e coeficientes de cultivo (KC) da cana-de-açúcar irrigada por gotejamento subsuperficial. 2010. 64 f. : Dissertação (mestrado) - Universidade Federal do Ceará, Centro de Ciências Agrárias, Departamento de Engenharia Agrícola, Programa de Pós-Graduação em Engenharia Agrícola, Fortaleza-CE, 2010. / Submitted by demia Maia (demiamlm@gmail.com) on 2016-06-28T16:59:16Z No. of bitstreams: 1 2010_dis_fmgonçalves.pdf: 3900094 bytes, checksum: 1ad79acf1432c0de09bcbdf52cb0f8c3 (MD5) / Approved for entry into archive by demia Maia (demiamlm@gmail.com) on 2016-06-28T16:59:48Z (GMT) No. of bitstreams: 1 2010_dis_fmgonçalves.pdf: 3900094 bytes, checksum: 1ad79acf1432c0de09bcbdf52cb0f8c3 (MD5) / Made available in DSpace on 2016-06-28T16:59:48Z (GMT). No. of bitstreams: 1 2010_dis_fmgonçalves.pdf: 3900094 bytes, checksum: 1ad79acf1432c0de09bcbdf52cb0f8c3 (MD5) Previous issue date: 2010 / Sugar cane is one of the crops with the highest level of water consumption, with a high evapotranspiration demand throughout most of its cycle. Knowledge of the sugar cane water demand, the time that irrigation should be applied, and how to irrigate the crop are becoming increasingly important for the sustainable development of irrigated sugar cane cultivation, especially in areas of low water availability, as it is the case in northea stern Brazil. The experiment was carried out at the Curu Experimental Field (property of the Embrapa Tropical Agroindustry), located in the Curu-Paraipaba Irrig ation Project, city of Paraipaba-CE (3 ° 29 '20''S, 39 ° 9' 45''W and elevation 30m), in order to determine the evapotrans piration and crop coefficients (Kc) of sugarcane (Saccharum L. officinarium), subsurface drip-irrigated. It was used the SP 6949 sugar cane variety, planted in a spacing of 1.8 m between double rows and 0.4 m between rows within the double row. As to t he irrigation, we used one lateral water line for each double row, buried at a depth of 0.15 m, w ith self-compensating drip emitters, with a flow rate of 1 L h-1, spaced 0.5 m on the water line. The crop was irrigated daily and there were three fertigations per week. The irrigation de pth was periodically adjusted, keeping the soil water potential between -8 kPa to -20 kPa. The crop evapotranspiration (ETc) was determined using a wei ghing lysimeter with a surface area of 2.25 m 2. The reference evapotranspiration (ETo) was estimated by the FAO Penman-Monteith method. The durations of the phenological stages of cane sugar were estimated through analysis of soil cover, with the use of digital images. Durations of 31, 49, 237 and 118 days were observed, respectively for initial, crop development, mid-season and late season stages. The yields achieved within and outside the lysimeter were respectively 144.4 and 108.8 t ha -1 . The total ETc observed during the cycle of the sugar cane was 1074.1 m m, with maximum values of 6.6 mm d-1 during the mid-season stage. Observed Kc values for initial, mid-season and late season stages were respectively 0.23, 1 .03 and 0.50. In the crop development stage, the relationship between Kc and the (crop) soil cover was represented with good accuracy by a negative quadratic model. / A cana-de-açúcar é uma das culturas com maior consumo de água, apresentando uma alta demanda evapotranspirativa ao longo da maior parte do seu ciclo. O conhecimento das necessidades hídricas da cana-de-açúcar, do momento de aplicação da água requerida pela mesma e a forma de aplicação torna-se cada vez mais importante para o desenvolvimento sustentável da sua produção irrigada, principalmente em regiões de pouca disponibilidade hídrica, como é o caso da região Nordeste do Brasil. O experimento foi conduzido no Campo Experimental do Curu, pertencente à Embrapa Agroindústria Tropical localizado no Perímetro Irrigado Curu-Paraipaba, município de Paraipaba-CE (3° 29’ 20’’ S, 39° 9’ 45’’ W e altitude de 30 m), com o objetivo de determinar a evapotranspiração e os coeficientes de cultivo (Kc) da cana-de-açúcar (Saccharum officinarium L.), irrigada por gotejamento subsuperficial. Utilizou-se a variedade de cana SP 6949, plantada no espaçamento de 1,8 m entre fileiras duplas e 0,4 m entre linhas dentro da fileira dupla. Na irrigação utilizou-se uma linha lateral para cada fileira dupla, enterrada na profundidade de 0,15 m, com gotejadores autocompensantes, com vazão de 1 L h-1, espaçados de 0,5 m na linha. A cultura foi irrigada com freqüência diária e foram realizadas três fertirrigações por semana. A lâmina de irrigação foi ajustada periodicamente, mantendo-se o potencial de água no solo entre -8 kPa e -20 kPa. A evapotranspiração da cultura (ETc) foi determinada utilizando-se um lisímetro de pesagem com área superficial de 2,25 m2. A evapotranspiração de referência (ETo) foi estimada pelo método FAO Penman-Monteith. As durações das fases fenológicas da cana-de-açúcar foram estimadas por meio da análise da cobertura do solo pela cultura, determinada com o uso de imagens digitais. Foram observadas durações de 31, 49, 237 e 118 dias, para as fases inicial, de desenvolvimento, intermediária e final, respectivamente. A produtividade alcançada dentro e fora do lisímetro foi de 144,4 e 108,8 t ha-1, respectivamente. A ETc total observada durante o ciclo da cana-de-açúcar foi de 1.074,1 mm, com valores máximos da ordem de 6,6 mm d-1 durante a fase intermediária. Foram observados valores de Kc iguais a 0,23, 1,03 e 0,50, para as fases inicial, intermediária e final, respectivamente. Na fase de desenvolvimento vegetativo a relação entre o Kc e a cobertura do solo pela cultura foi representada com bastante exatidão por um modelo quadrático negativo.