Análise in vitro da expressão de genes de resposta a estresse oxidativo e osmótico da bactéria fastidiosa Leifsonia xyli subsp. xyli

Atualmente, o Brasil é o maior produtor de cana-de-açúcar (Saccharum ssp.), no qual o estado de São Paulo é responsável por mais de 50% da produção. Esta cultura é hospedeira de diversos patógenos que podem limitar sua produção, dentre os quais se destaca a bactéria Leifsonia xyli subsp. xyli (Lxx), agente causal do raquitismo da soqueira (ratoon stunting disease - RSD). Pouco se sabe sobre a fisiologia deste organismo e quais as estratégias utilizadas por este para colonizar seu hospedeiro. No entanto, sabemos que para infectar e colonizar seus hospedeiros, é necessário que bactérias parasíticas superem estresses de diversas naturezas impostas durante estes processos, como os estresses oxidativo e o osmótico. Neste contexto, os objetivos deste trabalho foram identificar in silico e analisar a expressão in vitro, por qPCR, de genes relacionados a estes dois estresses. Uma análise da sequência do genoma de Lxx identificou 35 genes, sendo 8 relacionados ao estresse oxidativo, 9 relacionados ao estresse osmótico e 11 relacionados a estresse gerais, incluindo um cluster de 6 genes envolvidos na síntese de carotenoides. A expressão destes foi avaliada 60 minutos após exposição a 30mM de H2O2 ou 7% (p/v) de polietilenoglicol 6000 (PEG 6000). Sete genes foram avaliados como normalizadores das reações de qPCR. A quantificação do grau de peroxidação lipídica indicou que ambos os tratamentos resultaram em sensível peroxidação, muito embora o efeito do tratamento com PEG 6000 tenha sido maior do que o tratamento com H2O2. A exposição ao H2O2 aumentou a expressão dos genes katA (catalase), sodA (superóxido dismutase), msrA (Sulfóxido de metionina redutase) e msrB (Sulfóxido de metionina redutase) bem como de todos os genes responsáveis pela síntese de carotenoides. Por outro lado, todos os genes relacionados ao estresse osmótico foram menos expressos na presença deste composto. Já quando a bactéria foi exposta a PEG 6000, o oposto ocorreu, ou seja, os genes relacionados ao estresse osmótico, que são otsA (Trealose-6-fosfato sintase), otsB (Trealose fosfatase), treY (Malto-oligosil trealose sintase), treZ (Malto-oligosil trealose trealoidrolase), treS (Trealose sintase), proX (Proteína de ligamento em substrato, tipo ABC glicina betaína transportadora), proW (Proteína permease, tipo ABC glicina betaína transportadora), proZ (Proteína permease, tipo ABC glicina betaína transportadora) e Naggn (Amidotransferase), além dos genes do cluster carotenoide, foram mais expressos, ao passo que alguns dos genes ligados à resposta ao estresse oxidativo foram menos expressos. Verificou-se também, através de PCR convencional utilizando primers para amplificar as regiões entre os genes carotenoides, que estes são expressos como um RNA policistrônico, constituindo assim um operon. Estes resultados validam predições anteriores baseadas na análise in silico da sequência do genoma de Lxx, confirmando que Lxx possui mecanismos responsivos aos estresses osmótico e oxidativo aos quais é submetida durante o processo de infecção de seu hospedeiro.

Estudos mecanísticos da origem da inibição da reação foto-Fenton por íons cloreto

O objetivo principal deste estudo foi determinar a origem da inibição do processo foto-Fenton [Fe(II)/Fe(III), H2O2, luz UV] pelo íon cloreto. Um estudo das reações primárias da etapa fotocatalítica do processo foto-Fenton por fotólise por pulso de laser na presença de NaCl mostrou que a inibição reflete: i) fotólise competitiva dos complexos Fe(Cl)2+ e Fe(Cl)2+; ii) captura do radical hidroxila (dependente do pH) pelo íon cloreto. Esses dois processos formam o ânion radical menos reativo Cl2•- em lugar do radical HO•-, provocando uma progressiva inibição da reação de degradação com a diminuição do pH. Modelagem cinética destes resultados previa que a manutenção do pH em 3,0 durante a fotodegradação evitaria a formação do Cl2•-, o que foi confirmada através de experimentos de fotodegradação do fenol e da gasolina em meio aquoso na presença de NaCl. Por outro lado, na degradação do fenol pela reação térmica de Fenton [Fe(II)/Fe(III), H2O2], o radical hidroxila não parece ter um papel muito importante. A degradação térmica não foi inibida pela presença de íon cloreto e a cinética de mineralização do fenol pela reação térmica de Fenton é indistinguível da degradação do fenol pelo processo foto-Fenton inibido por NaCl. Isso sugere que a reação proposta por Hamilton, isto é, a redução de Fe(III) a Fe(II) por catecol (o principal intermediário inicial da oxidação do fenol) na presença de H2O2, é o mecanismo principal de catálise da reação térmica de Fenton no nosso sistema.

Estudo cinético da lixiviação de metais de placas de circuito impresso obsoletas.

O processo tradicional de recuperação de metais de resíduos de equipamentos eletroeletrônicos (REEE) geralmente envolve processamento pirometalúrgico. Entretanto, o uso desta tecnologia para processar placas de circuito impresso (PCI) obsoletas pode levar à liberação de dioxinas e furanos, devido à decomposição térmica de retardantes de chama e resinas poliméricas presentes no substrato das placas. Portanto, este trabalho propõe uma rota hidrometalúrgica para recuperação de metais. O comportamento dos metais, com destaque para cobre, zinco e níquel, durante a lixiviação ácida, foi estudado em três temperaturas diferentes (35ºC, 65ºC e 75ºC), com e sem adição de um agente oxidante (peróxido de hidrogênio H2O2). A cinética de dissolução ácida desses metais foi estudada baseada na análise química por ICP-OES (Espectrometria de emissão ótica por plasma acoplado indutivamente) e EDX (Espectroscopia de fluorescência de raios-X por energia dispersiva). O balanço de massa e a análise química indicaram que a etapa de lixiviação sem adição de oxidante é pouco eficaz na extração dos metais, sendo responsável pela dissolução de menos do que 6% do total extraído. A 65ºC e H2SO4 1 mol/L, com adição de 5 mL de H2O2 (30%) a cada quinze minutos e densidade de polpa de 1 g / 10 mL, 98,1% do cobre, 99,9% do zinco e 99,0% do níquel foram extraídos após 4 horas. A cinética de dissolução desses metais é controlada pela etapa da reação química, seguindo, dependendo da temperatura, a equação 1 (1 XB)1/3 = k1.t ou a equação ln (1 XB) = k4.t.

Espécies polinucleares de cobre e ferro com catalisadores de oxidação e modelos de sítios ativos

Diferentes complexos de cobre(II), contendo ligantes do tipo base de Schiff e um grupamento imidazólico, com interesse bioinorgânico, catalítico e como novos materiais, foram preparados na forma de sais perclorato, nitrato ou cloreto e caracterizados através de diferentes técnicas espectroscópicas (UV/Vis, IR, EPR, Raman) e espectrometria de massa Tandem (ESI-MS/MS), além de análise elementar, condutividade molar e medidas de propriedades magnéticas. Alguns destes compostos, obtidos como cristais adequados, tiveram suas estruturas determinadas por cristalografia de raios-X. As espécies di- e polinucleares contendo pontes cloreto, mostraram desdobramentos das hiperfinas nos espectros de EPR, relacionados à presença do equilíbrio com a respectiva espécie mononuclear, devido à labilidade dos íons cloretos, dependendo do contra-íon e do tipo de solvente utilizado. Adicionalmente, em solução alcalina, estes compostos estão em equilíbrio com as correspondentes espécies polinucleares, onde os centros de cobre estão ligados através de um ligante imidazolato. Em meio alcalino, estes compostos polinucleares contendo ponte imidazolato foram também isolados e caracterizados por diferentes técnicas espectroscópicas e magnéticas. Através da variação estrutural e também do ligante-ponte foi possível modular o fenômeno da interação magnética entre os íons de cobre em estruturas correlatas di- e polinucleares. Os respectivos parâmetros magnéticos foram obtidos com ajuste das curvas experimentais de XM vs T, correlacionando-se muito bem com a geometria, ângulos e distâncias de ligação entre os íons, quando comparado com outros complexos similares descritos na literatura. Posteriormente, estudaram-se os fatores relacionados com a reatividade de todas essas espécies como catalisadores na oxidação de substratos de interesse (fenóis e aminas), através da variação do tamanho da cavidade nas estruturas cíclicas ou de variações no ligante coordenado ao redor do íon metálico. Vários deles se mostraram bons miméticos de tirosinases e catecol oxidases. Um novo complexo-modelo da citocromo c oxidase (CcO), utilizando a protoporfirina IX condensada ao quelato N,N,-bis[2-(1,2-metilbenzimidazolil)etil]amino e ao resíduo de glicil-L-histidina, foi sintetizado e caracterizado através de diferentes técnicas espectroscópicas, especialmente EPR. A adição de H2O2 ao sistema completamente oxidado, FeIII/CuII, a -55°C, ou o borbulhamento de oxigênio molecular a uma solução do complexo na sua forma reduzida, FeII/CuI, saturada de CO, resultou na formação de adutos com O2, de baixo spin, estáveis a baixas temperaturas.

Novel chromone and xanthone derivatives: Synthesis and ROS/RNS scavenging activities

Chromones and xanthones are oxygen-containing heterocyclic compounds acknowledged by their antioxidant properties. In an effort to develop novel agents with improved activity, a series of compounds belonging to these chemical classes were prepared. Their syntheses involve the condensation of appropriate 2-methyl-4H-chromen-4-ones, obtained via Baker-Venkataraman rearrangement, with (E)-3-(3,4-dimethoxyphenyl)acrylaldehyde to provide the corresponding 2-[(1E,3E)-4-(3,4-dimethoxyphenyl)buta-1,3-dien-1-yl]-4H-chromen-4-ones. Subsequent electrocyclization and oxidation of these compounds led to the synthesis of 1-aryl-9H-xanthen-9-ones. After cleavage of the protecting groups, hydroxylated chromones and xanthones were assessed as scavenging agents against both reactive oxygen species (ROS) [superoxide radical (O2(•-)), hydrogen peroxide (H2O2), hypochlorous acid (HOCl), singlet oxygen ((1)O2), and peroxyl radical (ROO(•))] and reactive nitrogen species (RNS) [nitric oxide ((•)NO) and peroxynitrite anion (ONOO(-))]. Generally, all the tested new hydroxylated chromones and xanthones exhibited scavenger effects dependent on the concentration, with IC50 values found in the micromolar range. Some of them were shown to have improved scavenging activity when compared with previously reported analogues, allowing the inference of preliminary conclusions on the structure-activity relationship.

Metal-free catalysts derived from lignin for efficient wet peroxide oxidation

In this work, a wheat and hemp lignin (Sarkanda, Granit S.A.) has been used as raw material for the development of metal-free activated carbons. These materials were tested in the catalytic wet peroxide oxidation (CWPO) of 4-nitrophenol (4-NP; 5 g L-1) during 24 h experiments conducted at relatively mild operating conditions (p = 1 atm, t = 50 °C, pH = 3, catalyst load = 2.5 g L-1 and [H2O2]0 = 17.8 g L-1). First, the lignin was carbonized under N2 atmosphere followed by the activation of the obtained non-porous carbon (LG) under air atmosphere at different temperatures (150 to 350 ºC), leading to the generation of significant porosity.

Biochemical mechanisms involved in pulmonary hypo-alveolarization induced by peroxides contaminating parenteral nutrition in newborn guinea pig

La dysplasie broncho-pulmonaire (DBP), caractérisée par un défaut de l’alvéolarisation, est une complication pathologique associée à un stress oxydant chez le nouveau-né prématuré. La DBP est présente chez près de 50 % des nouveau-nés de moins de 29 semaines de gestation. La nutrition parentérale (NP) que ces nouveau-nés reçoivent pour cause d’immaturité gastro-intestinale est une source importante de stress oxydant. En effet, leur NP est contaminée par des peroxydes, dont l’ascorbylperoxyde qui est une forme peroxydée du déshydroascorbate. La génération des peroxydes est catalysée par la lumière ambiante. La photoprotection de la NP, quoique difficile d’application en clinique, est associée à une diminution de l’incidence de la DBP chez les enfants prématurés. Chez l’animal nouveau-né, la photoprotection de la NP est associée à un meilleur développement alvéolaire. Ainsi, nous émettons l’hypothèse que l’ascorbylperoxide infusé avec la NP cause la perte d’alvéoles suite à une apoptose exagérée induite par l’oxydation du potentiel redox du glutathion. Cette oxydation du potentiel redox serait occasionnée par l’inhibition de la transformation hépatique de la méthionine en cystéine, menant à une diminution de la synthèse de glutathion au foie et dans les tissus tels que les poumons. La confirmation de cette hypothèse suggérera qu’un ajout de glutathion dans la NP permettra une meilleure détoxification de l’ascorbylperoxide par l’action de la glutathion peroxydase, et préviendra l’oxydation du potentiel redox et ainsi, la perte d'alvéoles par apoptose. Objectifs : Le but de mon projet de recherche est de comprendre les mécanismes biochimiques liant la NP et le développement de la DBP chez le nouveau-né prématuré et de proposer une alternative nutritionnelle prévenant le développement de cette complication fréquemment observée dans cette population. Les objectifs spécifiques sont : 1) d’évaluer l’impact, au poumon, de l’infusion de l’ascorbylperoxyde sur l’axe métabolique potentiel redox du glutathion - apoptose - le développement alvéolaire; 2) d’étudier l’impact de l’ascorbylperoxyde et du potentiel redox sur l’activité hépatique de la méthionine adénosyltransférase (MAT), première enzyme de la cascade métabolique transformant la méthionine en cystéine; et 3) de tenter de prévenir l’impact négatif de la NP ou de l’infusion d’ascorbylperoxyde sur le poumon en améliorant le statut en glutathion. Méthodes: Par un cathéter fixé dans la jugulaire, des cochons d’Inde de trois jours de vie (n = 8 par groupe) ont reçu en continu durant 4 jours une NP ou une solution de base (dextrose + NaCl) enrichie des différentes molécules à l’essai. Le premier objectif a été atteint en enrichissant la solution de base en ascorbylperoxyde à 0, 20, 60 et 180 μM. Ces solutions contenaient ou non 350 μM H2O2 pour se rapprocher des conditions cliniques. Le second objectif a été atteint en investiguant les mécanismes d’inhibition de la MAT dans des animaux infusés ou non avec des solutions contenant la solution de base, des peroxydes, du glutathion et la NP (dextrose + acides aminés + multivitamines + lipides). Le troisième objectif a été atteint en ajoutant ou non à une solution d’ascorbylperoxide ou à la NP 10 μM de glutathion (GSSG), afin d’obtenir une concentration plasmatique normale de glutathion. Après 4 jours, les poumons étaient prélevés et traités pour la détermination de GSH et GSSG par électrophorèse capillaire, le potentiel redox était calculé selon l'équation de Nernst et le niveau de caspase-3 actif (marqueur d’apoptose) par Western blot et l’index d’alvéolarisation quantifié par le nombre d’interceptes entre des structures histologiques et une droite calibrée. Les données étaient comparées par ANOVA, les effets étaient considérés comme significatifs si le p était inférieur à 0,05. Résultats: L’infusion de l’ascorbylperoxyde, indépendamment du H2O2, a induit une hypoalvéolarisation, une activation de la caspase-3 et une oxydation du potentiel redox de manière dose-dépendante. Ces effets ont été empêchés par l’ajout de GSSG à la NP ou à la solution d’ascorbylperoxyde (180 M). L’ascorbylperoxyde et le H2O2 ont inhibé l’activité de MAT tandis qu’elle était linéairement modulée par la valeur du potentiel redox hépatique. Conclusion : Nos résultats suggèrent que l’ascorbylperoxyde est l’agent actif de la NP conduisant au développement de la DBP. Ainsi la correction des bas niveaux de glutathion induits par les peroxydes de la NP favorise la détoxification des peroxydes et la correction du potentiel redox pulmonaire ; ce qui a protégé les poumons des effets délétères de la NP en outrepassant l’inhibition de la MAT hépatique. Nos résultats sont d'une grande importance car ils donnent de l'espoir pour une prévention possible de la DBP.

Biochemical mechanisms involved in pulmonary hypo-alveolarization induced by peroxides contaminating parenteral nutrition in newborn guinea pig

La dysplasie broncho-pulmonaire (DBP), caractérisée par un défaut de l’alvéolarisation, est une complication pathologique associée à un stress oxydant chez le nouveau-né prématuré. La DBP est présente chez près de 50 % des nouveau-nés de moins de 29 semaines de gestation. La nutrition parentérale (NP) que ces nouveau-nés reçoivent pour cause d’immaturité gastro-intestinale est une source importante de stress oxydant. En effet, leur NP est contaminée par des peroxydes, dont l’ascorbylperoxyde qui est une forme peroxydée du déshydroascorbate. La génération des peroxydes est catalysée par la lumière ambiante. La photoprotection de la NP, quoique difficile d’application en clinique, est associée à une diminution de l’incidence de la DBP chez les enfants prématurés. Chez l’animal nouveau-né, la photoprotection de la NP est associée à un meilleur développement alvéolaire. Ainsi, nous émettons l’hypothèse que l’ascorbylperoxide infusé avec la NP cause la perte d’alvéoles suite à une apoptose exagérée induite par l’oxydation du potentiel redox du glutathion. Cette oxydation du potentiel redox serait occasionnée par l’inhibition de la transformation hépatique de la méthionine en cystéine, menant à une diminution de la synthèse de glutathion au foie et dans les tissus tels que les poumons. La confirmation de cette hypothèse suggérera qu’un ajout de glutathion dans la NP permettra une meilleure détoxification de l’ascorbylperoxide par l’action de la glutathion peroxydase, et préviendra l’oxydation du potentiel redox et ainsi, la perte d'alvéoles par apoptose. Objectifs : Le but de mon projet de recherche est de comprendre les mécanismes biochimiques liant la NP et le développement de la DBP chez le nouveau-né prématuré et de proposer une alternative nutritionnelle prévenant le développement de cette complication fréquemment observée dans cette population. Les objectifs spécifiques sont : 1) d’évaluer l’impact, au poumon, de l’infusion de l’ascorbylperoxyde sur l’axe métabolique potentiel redox du glutathion - apoptose - le développement alvéolaire; 2) d’étudier l’impact de l’ascorbylperoxyde et du potentiel redox sur l’activité hépatique de la méthionine adénosyltransférase (MAT), première enzyme de la cascade métabolique transformant la méthionine en cystéine; et 3) de tenter de prévenir l’impact négatif de la NP ou de l’infusion d’ascorbylperoxyde sur le poumon en améliorant le statut en glutathion. Méthodes: Par un cathéter fixé dans la jugulaire, des cochons d’Inde de trois jours de vie (n = 8 par groupe) ont reçu en continu durant 4 jours une NP ou une solution de base (dextrose + NaCl) enrichie des différentes molécules à l’essai. Le premier objectif a été atteint en enrichissant la solution de base en ascorbylperoxyde à 0, 20, 60 et 180 μM. Ces solutions contenaient ou non 350 μM H2O2 pour se rapprocher des conditions cliniques. Le second objectif a été atteint en investiguant les mécanismes d’inhibition de la MAT dans des animaux infusés ou non avec des solutions contenant la solution de base, des peroxydes, du glutathion et la NP (dextrose + acides aminés + multivitamines + lipides). Le troisième objectif a été atteint en ajoutant ou non à une solution d’ascorbylperoxide ou à la NP 10 μM de glutathion (GSSG), afin d’obtenir une concentration plasmatique normale de glutathion. Après 4 jours, les poumons étaient prélevés et traités pour la détermination de GSH et GSSG par électrophorèse capillaire, le potentiel redox était calculé selon l'équation de Nernst et le niveau de caspase-3 actif (marqueur d’apoptose) par Western blot et l’index d’alvéolarisation quantifié par le nombre d’interceptes entre des structures histologiques et une droite calibrée. Les données étaient comparées par ANOVA, les effets étaient considérés comme significatifs si le p était inférieur à 0,05. Résultats: L’infusion de l’ascorbylperoxyde, indépendamment du H2O2, a induit une hypoalvéolarisation, une activation de la caspase-3 et une oxydation du potentiel redox de manière dose-dépendante. Ces effets ont été empêchés par l’ajout de GSSG à la NP ou à la solution d’ascorbylperoxyde (180 M). L’ascorbylperoxyde et le H2O2 ont inhibé l’activité de MAT tandis qu’elle était linéairement modulée par la valeur du potentiel redox hépatique. Conclusion : Nos résultats suggèrent que l’ascorbylperoxyde est l’agent actif de la NP conduisant au développement de la DBP. Ainsi la correction des bas niveaux de glutathion induits par les peroxydes de la NP favorise la détoxification des peroxydes et la correction du potentiel redox pulmonaire ; ce qui a protégé les poumons des effets délétères de la NP en outrepassant l’inhibition de la MAT hépatique. Nos résultats sont d'une grande importance car ils donnent de l'espoir pour une prévention possible de la DBP.

Geochemistry, isotopic ratios and aldehyde concentrations of frost flowers, snow and ice near Barrow, Alaska

Frost flowers, intricate featherlike crystals that grow on refreezing sea ice leads, have been implicated in lower atmospheric chemical reactions. Few studies have presented chemical composition information for frost flowers over time and many of the chemical species commonly associated with Polar tropospheric reactions have never been reported for frost flowers. We undertook this study on the sea ice north of Barrow, Alaska to quantify the major ion, stable oxygen and hydrogen isotope, alkalinity, light absorbance by soluble species, organochlorine, and aldehyde composition of seawater, brine, and frost flowers. For many of these chemical species we present the first measurements from brine or frost flowers. Results show that major ion and alkalinity concentrations, stable isotope values, and major chromophore (NO3- and H2O2) concentrations are controlled by fractionation from seawater and brine. The presence of these chemical species in present and future sea ice scenarios is somewhat predictable. However, aldehydes, organochlorine compounds, light absorbing species, and mercury (part 2 of this research and Sherman et al. (2012, doi:10.1029/2011JD016186)) are deposited to frost flowers through less predictable processes that probably involve the atmosphere as a source. The present and future concentrations of these constituents in frost flowers may not be easily incorporated into future sea ice or lower atmospheric chemistry scenarios. Thinning of Arctic sea ice will likely present more open sea ice leads where young ice, brine, and frost flowers form. How these changing ice conditions will affect the interactions between ice, brine, frost flowers and the lower atmosphere is unknown.

Measurements of organic complexation of iron during the CARUSO-EISENEX experiment

The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment in the Atlantic sector of the Southern Ocean deviates strongly from ambient natural waters. Three iron additions (ferrous sulfate solution) were conducted, resulting in elevated dissolved iron concentrations (Nishioka, J., Takeda, S., de Baar, H.J.W., Croot, P.L., Boye, M., Laan, P., Timmermans, K.R., 2005, Changes in the concentration of iron in different size fractions during an iron enrichment experiment in the open Southern Ocean. Marine Chemistry, doi:10.1016/j.marchem.2004.06.040) and significant Fe(II) levels (Croot, P.L., Laan, P., Nishioka, J., Strass, V., Cisewski, B., Boye, M., Timmermans, K.R., Bellerby, R.G., Goldson, L., Nightingale, P., de Baar, H.J.W., 2005, Spatial and Temporal distribution of Fe(II) and H2O2 during EisenEx, an open ocean mescoscale iron enrichment. Marine Chemistry, doi:10.1016/j.marchem.2004.06.041). Repeated vertical profiles for dissolved (filtrate < 0.2 µm) Fe(III)-binding ligands indicated a production of chelators in the upper water column induced by iron fertilizations. Abiotic processes (chemical reactions) and an inductive biologically mediated mechanism were the likely sources of the dissolved ligands which existed either as inorganic amorphous phases and/or as strong organic chelators. Discrete analysis on ultra-filtered samples (< 200 kDa) suggested that the produced ligands would be principally colloidal in size (> 200 kDa-< 0.2 µm), as opposed to the soluble fraction (< 200 kDa) which dominated prior to the iron infusions. Yet these colloidal ligands would exist in a more transient nature than soluble ligands which may have a longer residence time. The production of dissolved Fe-chelators was generally smaller than the overall increase in dissolved iron in the surface infused mixed layer, leaving a fraction (about 13-40%) of dissolved Fe not bound by these dissolved Fe-chelators. It is suggested that this fraction would be inorganic colloids. The unexpected persistence of such high inorganic colloids concentrations above inorganic Fe-solubility limits illustrates the peculiar features of the chemical iron cycling in these waters. Obviously, the artificial about hundred-fold increase of overall Fe levels by addition of dissolved inorganic Fe(II) ions yields a major disruption of the natural physical-chemical abundances and reactivity of Fe in seawater. Hence the ensuing responses of the plankton ecosystem, while in itself significant, are not necessarily representative for a natural enrichment, for example by dry or wet deposition of aeolian dust. Ultimately, the temporal changes of the Fe(III)-binding ligand and iron concentrations were dominated by the mixing events that occurred during EISENEX, with storms leading to more than an order of magnitude dilution of the dissolved ligands and iron concentrations. This had strongest impact on the colloidal size class (> 200 kDa-< 0.2 µm) where a dramatic decrease of both the colloidal ligand and the colloidal iron levels (Nishioka, J., Takeda, S., de Baar, H.J.W., Croot, P.L., Boye, M., Laan, P., Timmermans, K.R., 2005, Changes in the concentration of iron in different size fractions during an iron enrichment experiment in the open Southern Ocean. Marine Chemistry, doi:10.1016/j.marchem.2004.06.040) was observed.

Dissolved iron measured along surface transects of the CARUSO-EISENEX experiment

Measurements of Fe(II) and H2O2 were carried out in the Atlantic sector of the Southern Ocean during EisenEx, an iron enrichment experiment. Iron was added on three separate occasions, approximately every 8 days, as a ferrous sulfate (FeSO4) solution. Vertical profiles of Fe(II) showed maxima consistent with the plume of the iron infusion. While H2O2 profiles revealed a corresponding minima showing the effect of oxidation of Fe(II) by H2O2, observations showed detectable Fe(II) concentrations existed for up to 8 days after an iron infusion. H2O2 concentrations increased at the depth of the chlorophyll maximum when iron concentrations returned to pre-infusion concentrations (<80 pM) possibly due to biological production related to iron reductase activity. In this work, Fe(II) and dissolved iron were used as tracers themselves for subsequent iron infusions when no further SF6 was added. EisenEx was subject to periods of weak and strong mixing. Slow mixing after the second infusion allowed significant concentrations of Fe(II) and Fe to exist for several days. During this time, dissolved and total iron in the infusion plume behaved almost conservatively as it was trapped between a relict mixed layer and a new rain-induced mixed layer. Using dissolved iron, a value for the vertical diffusion coefficient Kz=6.7±0.7 cm**2/s was obtained for this 2-day period. During a subsequent surface survey of the iron-enriched patch, elevated levels of Fe(II) were found in surface waters presumably from Fe(II) dissolved in the rainwater that was falling at this time. Model results suggest that the reaction between uncomplexed Fe(III) and O2? was a significant source of Fe(II) during EisenEx and helped to maintain high levels of Fe(II) in the water column. This phenomenon may occur in iron enrichment experiments when two conditions are met: (i) When Fe is added to a system already saturated with regard to organic complexation and (ii) when mixing processes are slow, thereby reducing the dispersion of iron into under-saturated waters.

Bulk Calcium and Titanium contents and Ti/Ca ratio of sediment core GeoB11804-4

Bulk Ca and Ti contents and Ti/Ca ratio of sediment core GeoB11804-4, measured by ICP-OES after HF/HNO3/H2O2 microwave pressure digestion.

(Table T3) Granulometry of sediments from ODP Leg 190 sites

We present the results of grain-size analysis performed on hemipelagic sediment from Sites 1173, 1174, 1175, and 1177 at the Nankai Trough. Analyses of the <63-µm fraction were performed with a laser particle counter, and results were converted to equivalent settling diameters by means of an empirical regression with data from pipette analysis. The relations among grain size, porosity, bulk density, void ratio, and moisture content are influenced by the increasing compaction of sediment with depth as well as facies changes. Thus, departures of bulk density and porosity from normal compaction trends cannot be attributed to grain size on the basis of our laboratory results.

Geochemistry of surface sediment samples from the South Atlantic Ocean

The aim of the present study is an evaluation of the applicability of biogenic barium as a proxy for productivity. For this purpose, 190 surface sediment samples from the South Atlantic Ocean were analysed for their barium and aluminium concentrations. Biogenic barium is estimated by subtracting the calculated terrigenous barium (obtained from the terrigenous Ba/Al ratio and the amount of Al in the sample) from the total Ba content in the sample. Based on the accumulation rates of biogenic barium, export production is estimated using three different algorithms proposed by [Paleoceanography 7 (1992) 163, doi:10.1029/92PA00181; Global Biogeochem. Cycles 9 (1995) 289, doi:10.1029/95GB00021; Geomar. Report 38 (1995) 105]. Primary productivity was calculated from these different export productions and compared with measurements of recent primary productivity in the overlying surface waters. Only the primary productions calculated on the basis of the algorithm of [Paleoceanography 7 (1992) 163, doi:10.1029/92PA00181] yield productivity values comparable to those existing in ocean surface waters. This study further reveals that it is not sufficient to use a constant, generally applicable organic carbon/biogenic barium ratio, as is postulated by [Global Biogeochem. Cycles 9 (1995) 289, doi:10.1029/95GB00021]. This ratio has to be assessed regionally. For the sediments of the Cape Basin in the eastern South Atlantic Ocean, a new algorithm is developed which gives plausible primary productivities for the overlying surface waters.

Discoloration and mineralization of Reactive Red HE-3B by heterogeneous photo-Fenton reaction

Discoloration and mineralization of Reactive Red HE-3B were studied by using a laponite clay-based Fe nanocomposite (Fe-Lap-RD) as a heterogeneous catalyst in the presence of H2O2 and UV light. Our experimental results clearly indicate that Fe-Lap-RD mainly consists of Fe2O3 (meghemite) and Fe2Si4O10(OH)2 (iron silicate hydroxide) which have tetragonal and monoclinic structures, respectively, and has a high specific surface area (472m(2) / g) as well as a high total pore volume (0.547 cm(3)/g). It was observed that discoloration of HE-3B undergoes a much faster kinetics than mineralization of HE-3B. It was also found that initial HE-3B concentration, H2O2 concentration, UV light wavelength and power, and Fe-Lap-RD catalyst loading are the four main factors that can significantly influence the mineralization of HE-3B. At optimal conditions, complete discoloration of 100 mg/L HE-3B can be achieved in 30 min and the total organic carbon removal ratio can attain 76% in 120 min, illustrating that Fe-Lap-RD has a high photo-catalytic activity in the photo-assisted discoloration and mineralization of HE-3B in the presence of UV light (254nm) and H2O2. (C) 2003 Elsevier Science Ltd. All rights reserved.