New insights into the formation and modification of carbonate-bearing minerals and methane gas in geological systems using multiply substituted isotopologues

This thesis describes the use of multiply-substituted stable isotopologues of carbonate minerals and methane gas to better understand how these environmentally significant minerals and gases form and are modified throughout their geological histories. Stable isotopes have a long tradition in earth science as a tool for providing quantitative constraints on how molecules, in or on the earth, formed in both the present and past. Nearly all studies, until recently, have only measured the bulk concentrations of stable isotopes in a phase or species. However, the abundance of various isotopologues within a phase, for example the concentration of isotopologues with multiple rare isotopes (multiply substituted or 'clumped' isotopologues) also carries potentially useful information. Specifically, the abundances of clumped isotopologues in an equilibrated system are a function of temperature and thus knowledge of their abundances can be used to calculate a sample’s formation temperature. In this thesis, measurements of clumped isotopologues are made on both carbonate-bearing minerals and methane gas in order to better constrain the environmental and geological histories of various samples.

Clumped-isotope-based measurements of ancient carbonate-bearing minerals, including apatites, have opened up paleotemperature reconstructions to a variety of systems and time periods. However, a critical issue when using clumped-isotope based measurements to reconstruct ancient mineral formation temperatures is whether the samples being measured have faithfully recorded their original internal isotopic distributions. These original distributions can be altered, for example, by diffusion of atoms in the mineral lattice or through diagenetic reactions. Understanding these processes quantitatively is critical for the use of clumped isotopes to reconstruct past temperatures, quantify diagenesis, and calculate time-temperature burial histories of carbonate minerals. In order to help orient this part of the thesis, Chapter 2 provides a broad overview and history of clumped-isotope based measurements in carbonate minerals.

In Chapter 3, the effects of elevated temperatures on a sample’s clumped-isotope composition are probed in both natural and experimental apatites (which contain structural carbonate groups) and calcites. A quantitative model is created that is calibrated by the experiments and consistent with the natural samples. The model allows for calculations of the change in a sample’s clumped isotope abundances as a function of any time-temperature history.

In Chapter 4, the effects of diagenesis on the stable isotopic compositions of apatites are explored on samples from a variety of sedimentary phosphorite deposits. Clumped isotope temperatures and bulk isotopic measurements from carbonate and phosphate groups are compared for all samples. These results demonstrate that samples have experienced isotopic exchange of oxygen atoms in both the carbonate and phosphate groups. A kinetic model is developed that allows for the calculation of the amount of diagenesis each sample has experienced and yields insight into the physical and chemical processes of diagenesis.

The thesis then switches gear and turns its attention to clumped isotope measurements of methane. Methane is critical greenhouse gas, energy resource, and microbial metabolic product and substrate. Despite its importance both environmentally and economically, much about methane’s formational mechanisms and the relative sources of methane to various environments remains poorly constrained. In order to add new constraints to our understanding of the formation of methane in nature, I describe the development and application of methane clumped isotope measurements to environmental deposits of methane. To help orient the reader, a brief overview of the formation of methane in both high and low temperature settings is given in Chapter 5.

In Chapter 6, a method for the measurement of methane clumped isotopologues via mass spectrometry is described. This chapter demonstrates that the measurement is precise and accurate. Additionally, the measurement is calibrated experimentally such that measurements of methane clumped isotope abundances can be converted into equivalent formational temperatures. This study represents the first time that methane clumped isotope abundances have been measured at useful precisions.

In Chapter 7, the methane clumped isotope method is applied to natural samples from a variety of settings. These settings include thermogenic gases formed and reservoired in shales, migrated thermogenic gases, biogenic gases, mixed biogenic and thermogenic gas deposits, and experimentally generated gases. In all cases, calculated clumped isotope temperatures make geological sense as formation temperatures or mixtures of high and low temperature gases. Based on these observations, we propose that the clumped isotope temperature of an unmixed gas represents its formation temperature — this was neither an obvious nor expected result and has important implications for how methane forms in nature. Additionally, these results demonstrate that methane-clumped isotope compositions provided valuable additional constraints to studying natural methane deposits.

Geochemistry and resonance ionization of platinum-group elements

Experimental studies were conducted with the goals of 1) determining the origin of Pt- group element (PGE) alloys and associated mineral assemblages in refractory inclusions from meteorites and 2) developing a new ultrasensitive method for the in situ chemical and isotopic analysis of PGE. A general review of the geochemistry and cosmochemistry of the PGE is given, and specific research contributions are presented within the context of this broad framework.

An important step toward understanding the cosmochemistry of the PGE is the determination of the origin of POE-rich metallic phases (most commonly εRu-Fe) that are found in Ca, AJ-rich refractory inclusions (CAI) in C3V meteorites. These metals occur along with γNi-Fe metals, Ni-Fe sulfides and Fe oxides in multiphase opaque assemblages. Laboratory experiments were used to show that the mineral assemblages and textures observed in opaque assemblages could be produced by sulfidation and oxidation of once homogeneous Ni-Fe-PGE metals. Phase equilibria, partitioning and diffusion kinetics were studied in the Ni-Fe-Ru system in order to quantify the conditions of opaque assemblage formation. Phase boundaries and tie lines in the Ni-Fe-Ru system were determined at 1273, 1073 and 873K using an experimental technique that allowed the investigation of a large portion of the Ni-Fe-Ru system with a single experiment at each temperature by establishing a concentration gradient within which local equilibrium between coexisting phases was maintained. A wide miscibility gap was found to be present at each temperature, separating a hexagonal close-packed εRu-Fe phase from a face-centered cubic γNi-Fe phase. Phase equilibria determined here for the Ni-Fe-Ru system, and phase equilibria from the literature for the Ni-Fe-S and Ni-Fe-O systems, were compared with analyses of minerals from opaque assemblages to estimate the temperature and chemical conditions of opaque assemblage formation. It was determined that opaque assemblages equilibrated at a temperature of ~770K, a sulfur fugacity 10 times higher than an equilibrium solar gas, and an oxygen fugacity 10⁶ times higher than an equilibrium solar gas.

Diffusion rates between -γNi-Fe and εRu-Fe metal play a critical role in determining the time (with respect to CAI petrogenesis) and duration of the opaque assemblage equilibration process. The diffusion coefficient for Ru in Ni (D^Ru_Ni) was determined as an analog for the Ni-Fe-Ru system by the thin-film diffusion method in the temperature range of 1073 to 1673K and is given by the expression:

D^Ru_Ni (cm² sec^-1) = 5.0(±0.7) x 10^-3 exp(-2.3(±0.1) x 10¹² erg mole^-1/RT) where R is the gas constant and T is the temperature in K. Based on the rates of dissolution and exsolution of metallic phases in the Ni-Fe-Ru system it is suggested that opaque assemblages equilibrated after the melting and crystallization of host CAI during a metamorphic event of ≥ 10³ years duration. It is inferred that opaque assemblages originated as immiscible metallic liquid droplets in the CAI silicate liquid. The bulk compositions of PGE in these precursor alloys reflects an early stage of condensation from the solar nebula and the partitioning of V between the precursor alloys and CAI silicate liquid reflects the reducing nebular conditions under which CAI were melted. The individual mineral phases now observed in opaque assemblages do not preserve an independent history prior to CAI melting and crystallization, but instead provide important information on the post-accretionary history of C3V meteorites and allow the quantification of the temperature, sulfur fugacity and oxygen fugacity of cooling planetary environments. This contrasts with previous models that called upon the formation of opaque assemblages by aggregation of phases that formed independently under highly variable conditions in the solar nebula prior to the crystallization of CAI.

Analytical studies were carried out on PGE-rich phases from meteorites and the products of synthetic experiments using traditional electron microprobe x-ray analytical techniques. The concentrations of PGE in common minerals from meteorites and terrestrial rocks are far below the ~100 ppm detection limit of the electron microprobe. This has limited the scope of analytical studies to the very few cases where PGE are unusually enriched. To study the distribution of PGE in common minerals will require an in situ analytical technique with much lower detection limits than any methods currently in use. To overcome this limitation, resonance ionization of sputtered atoms was investigated for use as an ultrasensitive in situ analytical technique for the analysis of PGE. The mass spectrometric analysis of Os and Re was investigated using a pulsed primary Ar⁺ ion beam to provide sputtered atoms for resonance ionization mass spectrometry. An ionization scheme for Os that utilizes three resonant energy levels (including an autoionizing energy level) was investigated and found to have superior sensitivity and selectivity compared to nonresonant and one and two energy level resonant ionization schemes. An elemental selectivity for Os over Re of ≥ 10³ was demonstrated. It was found that detuning the ionizing laser from the autoionizing energy level to an arbitrary region in the ionization continuum resulted in a five-fold decrease in signal intensity and a ten-fold decrease in elemental selectivity. Osmium concentrations in synthetic metals and iron meteorites were measured to demonstrate the analytical capabilities of the technique. A linear correlation between Os⁺ signal intensity and the known Os concentration was observed over a range of nearly 10⁴ in Os concentration with an accuracy of ~ ±10%, a millimum detection limit of 7 parts per billion atomic, and a useful yield of 1%. Resonance ionization of sputtered atoms samples the dominant neutral-fraction of sputtered atoms and utilizes multiphoton resonance ionization to achieve high sensitivity and to eliminate atomic and molecular interferences. Matrix effects should be small compared to secondary ion mass spectrometry because ionization occurs in the gas phase and is largely independent of the physical properties of the matrix material. Resonance ionization of sputtered atoms can be applied to in situ chemical analysis of most high ionization potential elements (including all of the PGE) in a wide range of natural and synthetic materials. The high useful yield and elemental selectivity of this method should eventually allow the in situ measurement of Os isotope ratios in some natural samples and in sample extracts enriched in PGE by fire assay fusion.

Phase equilibria and diffusion experiments have provided the basis for a reinterpretation of the origin of opaque assemblages in CAI and have yielded quantitative information on conditions in the primitive solar nebula and cooling planetary environments. Development of the method of resonance ionization of sputtered atoms for the analysis of Os has shown that this technique has wide applications in geochemistry and will for the first time allow in situ studies of the distribution of PGE at the low concentration levels at which they occur in common minerals.

Site-Specific Isotopes in Small Organic Molecules

Stable isotope geochemistry is a valuable toolkit for addressing a broad range of problems in the geosciences. Recent technical advances provide information that was previously unattainable or provide unprecedented precision and accuracy. Two such techniques are site-specific stable isotope mass spectrometry and clumped isotope thermometry. In this thesis, I use site-specific isotope and clumped isotope data to explore natural gas development and carbonate reaction kinetics. In the first chapter, I develop an equilibrium thermodynamics model to calculate equilibrium constants for isotope exchange reactions in small organic molecules. This equilibrium data provides a framework for interpreting the more complex data in the later chapters. In the second chapter, I demonstrate a method for measuring site-specific carbon isotopes in propane using high-resolution gas source mass spectrometry. This method relies on the characteristic fragments created during electron ionization, in which I measure the relative isotopic enrichment of separate parts of the molecule. My technique will be applied to a range of organic compounds in the future. For the third chapter, I use this technique to explore diffusion, mixing, and other natural processes in natural gas basins. As time progresses and the mixture matures, different components like kerogen and oil contribute to the propane in a natural gas sample. Each component imparts a distinct fingerprint on the site-specific isotope distribution within propane that I can observe to understand the source composition and maturation of the basin. Finally, in Chapter Four, I study the reaction kinetics of clumped isotopes in aragonite. Despite its frequent use as a clumped isotope thermometer, the aragonite blocking temperature is not known. Using laboratory heating experiments, I determine that the aragonite clumped isotope thermometer has a blocking temperature of 50-100°C. I compare this result to natural samples from the San Juan Islands that exhibit a maximum clumped isotope temperature that matches this blocking temperature. This thesis presents a framework for measuring site-specific carbon isotopes in organic molecules and new constraints on aragonite reaction kinetics. This study represents the foundation of a future generation of geochemical tools for the study of complex geologic systems.

Identification of Prorocentrum minimum and Takayama pulchella by fluorescence in situ hybridization through epifluorescence microscopy and flow cytometry

Partial rDNA sequences of Prorocentrum minimum and Takayama pulchella were amplified, cloned and sequenced. and these sequence data were deposited in the GenBank. Eight oligonucleotide probes (DNA probes) were designed based on the sequence analysis. The probes were employed to detect and identify P. minimum and T. pulchella in unialgal and mixed algal samples with a fluorescence in situ hybridization method using flow cytometry. Epifluorescence micrographs showed that these specific probes labeled with fluorescein isothiocyanate entered the algal cells and bound to target sequences, and the fluorescence signal resulting from whole-cell hybridization varied from probe to probe. These DNA probes and the hybridization protocol we developed were specific and effective for P. minimum and T. pulchella, without any specific binding to other algal species. The hybridization efficiency of different probes specific to P. minimum was in the order: PM18S02 > PM28S02 > PM28S01 > PM18S01, and that of the probes specific to T. pulchella was TP18S02 > TP28S01 > TP28S02 > TP18S01. The different hybridization efficiency of the DNA probes could also be shown in the fluorescent signals between the labeled and unlabeled cells demonstrated using flow cytometry. The DNA probes PM18S02, PM28S02; TP18S02 and TP28S01, and the protocol, were also useful for the detection of algae in natural samples.

Flow injection determination of dopamine based on inhibited electrochemiluminescence of luminol

A flow injection method has been developed for the determination of dopamine based on its inhibition of the electrochemiluminescence of luminol. This method is simple and sensitive for dopamine detection. Under the selected experimental conditions, the decreased electrochemiluminescent intensity is linear with dopamine concentration in the range of 5.0 x 10(-8)-1.0 x 10(-5) mol/L with a detection limit of 30 nmol/L. The relative standard deviation of eleven determinations is 1.9% for 1.0 x 10(-6) mol/L dopamine. The proposed method has been applied to the detection of dopamine in pharmaceutical injections with satisfactory results.

A novel flow through optical fiber biosensor for glucose based on luminol electrochemiluminescence

A novel flow injection optical fiber biosensor for glucose based on luminol electrochemiluminescence (ECL) is presented. The sol-gel method is introduced to immobilize glucose oxidase (GOD) on the surface of a glassy carbon electrode. After optimization of the working conditions, glucose could be quantitated in the concentration ranges between 50 muM and 10 mM with a detection limit of around 26 muM. Signal reproducibility was about 3.62% relative standard deviation for 11 replicated measurements of 0.1 mM glucose. The ECL biosensor also showed good selectivity and operational stability. The proposed method can be applied to determination of glucose in soft drink samples.

Electrochemiluminescent determination of glucose with a sol-gel derived ceramic-carbon composite electrode as a renewable optical fiber biosensor

A sol-gel derived ceramic-carbon composite electrode is used for fabrication of a new type of optical fiber biosensor based on luminol electrochemiluminescence (ECL). The electrode consists of graphite powder impregnated with glucose oxidase in a silicate network. In this configuration, the immobilized enzyme oxidizes glucose to liberate hydrogen peroxide and graphite powder provides percolation conductivity for triggering the ECL between luminol and the liberated hydrogen peroxide. Both of the reactions occur simultaneously on the surface of the composite electrode, thereby the response of the biosensor is very fast. The peak intensity was achieved within only 20 s after glucose injection. In addition, the electrode could be renewed by a simple mechanical polishing step in case of contamination or fouling. The linear range extends from 0.01 to 10 mM for glucose and the detection limit is about 8.16 muM. The renewal repeatability and stability of the biosensor are also investigated in detail.

Development and application of a high resolution liquid chromatographic method for the analysis of complex pigment distributions

Ternary and binary gradient systems have been developed for the high-performance liquid chromatographic analysis of complex pigment distributions typical of natural samples. Improved chromatographic resolution reveals significantly more pigment components in extracts from a sediment (Priest Pot, Cumbria, UK), a microbial mat (les Salines de la Trinital, South Catalonia, Spain) and a culture (C. phaeobacteroides) including novel bacteriochlorophyll derivatives. The methods developed are directly suited to LC–MS analysis and the automated acquisition of MS/MS data for pigments.

Paralytic shellfish poisoning detection by surface plasmon resonance-based biosensors in shellfish matrixes.

The detection of paralytic shellfish poisoning (PSP) toxins in contaminated shellfish is essential for human health preservation. Ethical and technical reasons have prompted the search for new detection procedures as an alternative to the mouse bioassay. On the basis of the detection of molecular interactions by surface plasmon resonance (SPR) biosensors, an inhibition assay was developed using an anti-GTX2/3 antibody (GT13-A) and a saxitoxin-CM5 chip. This assay allowed for quantification of saxitoxin (STX), decarbamoyl saxitoxin (dcSTX), gonyautoxin 2,3 (GTX2/3), decarbamoyl gonyautoxin 2,3 (dcGTX2/3), gonyautoxin 5 (GTX5), and C 1,2 (C1/2) at concentrations from 2 to 50 ng/mL. The interference of five shellfish matrixes with the inhibition assay was analyzed. Mussels, clams, cockles, scallops, and oysters were extracted with five published methods. Ethanol extracts and acetic acid/heat extracts (AOAC Lawrence method) performed adequately in terms of surface regeneration and baseline interference, did not inhibit antibody binding to the chip surface significantly, and presented STX calibration curves similar to buffer controls in all matrixes tested. Hydrochloric acid/heat extracts (AOAC mouse bioassay method) presented surface regeneration problems, and although ethanol-acetic acid/dichloromethane extracts performed well, they were considered too laborious for routine sample testing. Overall the best results were obtained with the ethanol extraction method with calibration curves prepared in blank matrix extracts. STX recovery rate with the ethanol extraction method was 60.52 ± 3.72%, with variations among species. The performance of this biosensor assay in natural samples, compared to two AOAC methods for PSP toxin quantification (mouse bioassay and HPLC), suggests that this technology can be useful as a PSP screening assay. In summary, the GT13-A-STX chip inhibition assay is capable of PSP toxin detection in ethanol shellfish extracts, with sufficient sensitivity to quantify the toxin in the range of the European regulatory limit of 80 g/100 g of shellfish meat.

Single Laboratory Validation of a Surface Plasmon Resonance Biosensor Screening method for Paralytic Shellfish Poisoning Toxins

A research element of the European Union (EU) sixth Framework project BioCop focused on the development of a surface plasmon resonance (SPR) biosensor assay for the detection of paralytic shellfish poisoning (PSP) toxins in shellfish as an alternative to the increasingly ethically unacceptable mouse bioassay. A biosensor assay was developed using both a saxitoxin binding protein and chip surface in tandem with a highly efficient simple extraction procedure. The present report describes the single laboratory validation of this immunological screening method, for this complex group of toxins with differing toxicities, according to the European Decision 2002/657/EC in conjunction with IUPAC and AOAC single laboratory validation guidelines. The different performance characteristics (detection capability CC beta, specificity/selectivity, repeatability, reproducibility, stability, and applicability) were determined in relation to the EU regulatory limit of 800 mu g of saxitoxin equivalents (STX eq) per kg of shellfish meat. The detection capability CC beta was calculated to be 120 mu g/kg. Intra-assay repeatability was found to be between 2.5 and 12.3% and interassay reproducibility was between 6.1 and 15.2% for different shellfish matrices. Natural samples were also evaluated and the resultant data displayed overall agreements of 96 and 92% with that of the existing AOAC approved methods of mouse bioassay (MBA) and high performance liquid chromatography (HPLC), respectively.

Study of pesticide effects on non-target organisms

A utilização insustentável de pesticidas, especialmente em zonas com elevado valor ecológico constitui uma ameaça à integridade dos ecossistemas. Sendo um problema à escala mundial, e também no contexto nacional, o presente trabalho pretende ser um contributo para a avaliação dos efeitos de pesticidas em organismos não alvo terrestres e, principalmente, aquáticos, em contextos de progressiva relevância ecológica. Neste sentido, o estudo foi direccionado para áreas (A1 e A2) integradas numa zona agrícola extensa em Portugal, utilizada para a produção de milho e, principalmente, de arroz (Baixo Mondego), a qual sustenta uma elevada biodiversidade. O estudo teve início na área A1, onde a monitorização físico-química e os ensaios com amostras naturais (ensaios WET - whole effluent tests) provenientes desta área evidenciaram que, apesar da ausência de pesticidas, as amostras de água colhidas no canal que atravessava os arrozais foram as mais nocivas para o crescimento de Pseudokirchneriella subcapitata e Chlorella vulgaris. Uma vez que outras fontes de contaminação (produção de gado) actuavam em A1, o estudo prosseguiu apenas na área A2. Assim, em A2, começou-se por determinar a toxicidade individual e da mistura de dois herbicidas formulados aplicados nos campos de arroz (Viper®) e milho (Mikado®) em condições laboratoriais. Viper® foi o herbicida mais tóxico, tanto para o crescimento de P. subcapitata e C. vulgaris, como para a sobrevivência, reprodução e crescimento de Daphnia longispina e Daphnia magna. Adicionalmente, estimou-se que a mistura Viper®/Mikado® induz efeitos antagonistas no crescimento de P. subcapitata e efeitos sinérgicos no crescimento de C. vulgaris e na sobrevivência dos dafnídeos. A avaliação da toxicidade destes herbicidas formulados e seus ingredientes activos no comportamento de minhocas terrestres (Eisenia andrei), usando solos naturais, demonstrou que Viper® e penoxsulam causaram uma % de evitamento superior nos organismos expostos. Contudo, o risco para E. andrei será à partida reduzido se as taxas de aplicação dos herbicidas forem respeitadas. Ensaios WET foram novamente usados para testar amostras naturais da área A2. Verificou-se que a qualidade do sistema aquático e do arrozal diminuiu durante a estação agrícola, em paralelo com a presença de nutrientes e pesticidas. O crescimento algal foi inibido, apesar dos parâmetros de história de vida dos dafnídeos terem sido estimulados. O resultado desta avaliação subestimou, em certos casos, os impactos reais causados pela aplicação de pesticidas. A avaliação in situ simultânea à aplicação de herbicidas nos arrozais demonstrou que os efeitos registados foram de facto restritos aos pulsos de herbicidas. A inibição das taxas de alimentação de D. longispina e D. magna forneceram um sinal precoce de alterações no sistema, seguido pela diminuição da sua sobrevivência e do crescimento de P. subcapitata. Em suma, as diferentes fases da avaliação efectuada confirmaram a existência de condições desfavoráveis devido às práticas agrícolas, reforçando a necessidade de se conjugar ensaios laboratoriais com avaliações in situ de maior relevância ecológica, para reduzir o grau de incerteza aliado à determinação dos riscos.

Photodegradation of sertraline by solar radiation and influencing factors

Photodegradation is considered to be one of the most important processes of elimination of pharmaceutical drugs from natural water matrices. The high consumption and discharge of these substances, in particular antidepressants, to the aquatic environment supports the need to study degradation processes. This dissertation aimed at studying the direct and indirect photodegradation of sertraline, an antidepressant known for its persistence in the environment, and the evaluation of the influence of environmentally relevant factors in its photodegradation. The photodegradation experiments were developed under simulated solar light and the irradiation times converted to summer sunny days (SSD), an equivalent time in natural environmental conditions. The direct photodegradation was evaluated in solutions of sertraline prepared in ultrapure water and the indirect photodegradation was studied through the addition of photosensitizers (humic substances, Fe(III), nitrates and oxygen). Further irradiation studies were perfomed in aqueous samples collected from two wastewater treatment plants, Vouga river and Ria de Aveiro. The samples were chemically characterized (dissolved organic carbon, nitrates and nitrites and iron determination and UV/Vis spectroscopy). The quantification of sertraline was done by HPLC-UV and photoproducts from direct photodegradation were identified by electrospray mass spectrometry. An observed direct photodegradation rate of sertraline of 0.0062 h-1 was determined, corresponding to a half-life time of 111 h (equivalent to 29 SSD). A significant influence of photosensitizers was observed, the best results being achieved in irradiations of sertraline with humic acids, obtaining a half-life time of 12 h. This was attributed to the hydrophobicity of this substance and higher absortivity in the UV/Vis wavelength, which promote processes of indirect photodegradation. The degradation of sertraline in natural samples was also enhanced comparatively to the direct photodegradation, achieving half-life times between 10 and 25h; the best results were achieved in samples from the primary treatment of a wastewater treatment plant and Ria de Aveiro, with half-life times of 10 and 16 h, respectively. A total of six photoproducts formed during the direct photodegradation of sertraline were identified, three of which were not yet identified in the literature. The main factors contributing to the degradation of sertraline were analysed but this was not fully accomplished, requiring further studies of the composition of the natural matrices and the combined influence of distinct photosensitizers during the irradiation. Nevertheless, it was concluded that the photodegradation of sertraline is greatly influenced by indirect photodegradation processes, promoted by the presence of photosensitizers.

La production de thiols biogéniques par les microorganismes aquatiques

Les thiols à faible masse moléculaire (FMM) peuvent affecter la biodisponibilité du mercure et mener à une plus grande production de méthylmercure par les microorganismes méthylants. Les résultats d’une étude réalisée au sein de la matrice extracellulaire du périphyton de la zone littorale d’un lac des Laurentides ont démontré que les concentrations en thiols à FMM retrouvées dans cette matrice sont jusqu’à 1000 fois supérieures à celles de la colonne d’eau avoisinante. Ces thiols sont significativement corrélés à la chlorophylle a du périphyton, suggérant une production par les algues. Le mercure de la matrice extracellulaire, plus spécifiquement dans la fraction colloïdale mobile, est aussi corrélé aux thiols d’origine algale. Ces résultats suggèrent qu’une accumulation de thiols s’opère dans l’espace extracellulaire du périphyton et qu’ils peuvent favoriser le transfert du mercure vers les microorganismes produisant le méthylmercure. Les résultats d’une seconde étude menée sur les méthodes de préservation d’échantillons d’eau pour la conservation des thiols à FMM ont démontré que la température optimale d’entreposage était de -80 °C et que la lyophilisation menait à une sous-estimation des concentrations mesurées. Les taux de dégradation étaient plus rapides lors de la conservation à -20 °C et variables selon la chimie de l’eau utilisée et les espèces de thiols observées. Suivant ces résultats, nous proposons un cadre de recherche pour de futures études sur la spéciation du mercure dans le périphyton et nous suggérons des précautions lors de la manipulation et de la conservation des thiols à FMM d’échantillons naturels.

Anàlisi polifàsica de soques de "Pseudomonas fluorescens" potencials agents de biocontrol de malalties de fruiters

Molts bacteris del grup fluorescent del gènere Pseudomonas són capaços de controlar malalties de les plantes causades per fongs i bacteris fitopatògens (ACBs) o mostren activitat com a bacteris promotors del creixement de les plantes (BPCPs). S'han descrit diversos metabòlits que intervenen de manera important en la seva activitat com a ACBs i BPCPs entre els quals en destaquen el 2,4-diacetilfloroglucinol (Phl), àcid fenazin-1-carboxílic (PCA), Pirrolnitrina (Prn), àcid cianhídric (HCN), àcid 3-indolacètic (IAA), sideròfors i quitinases. L'objectiu principal del nostre treball ha estat la comparació de les característiques d'un grup de Pseudomonas del grup fluorescent utilitzant una aproximació polifàsica amb la finalitat d'establir possibles relacions entre algunes de les característiques i la capacitat d'actuar com a ACB o BPCP. Atesa la importància en el biocontrol de la producció de metabòlits com Phl, PCA i Prn, l'objectiu preliminar ha estat la recerca i obtenció de soques productores d'aquests metabòlits. Per assolir aquest objectiu s'ha emprat una aproximació molecular basada en la detecció dels gens biosintètics implicats en la seva producció en lloc de la detecció directa dels metabòlits per evitar els efectes que poden tenir les condicions de cultiu en la inducció o repressió de la seva síntesi. S'han realitzat diferents protocols basats (i) en la cerca assistida de productors mitjançant l'ús de marcadors fenotípics i posterior confirmació per PCR i, (ii) en l'ús de la PCR per a la detecció dels gens directament dels extractes bacterians, d'enriquiments d'aquests extractes i la realització de la hibridació en colònies per al posterior aïllament. La cerca assistida de productors de Phl mitjançant marcadors fenotípics i posteriorment la utilització de tècniques moleculars (amplificació per PCR del gen phlD), ha estat el millor mètode en el tipus de mostres processades en el nostre treball, on la proporció de productors és relativament baixa. En total s'han aïllat a partir de diversos ambients 4 soques portadores dels gens de la síntesi de PCA, 15 de Phl i 1 de Prn. S'ha constituït una col·lecció de 72 soques de Pseudomonas del grup fluorescent que inclou 18 aïllats propis portadors dels gens biosintètics necessaris per la producció de Phl PCA i Prn; 6 soques de referència procedents de col·leccions de cultius tipus, 14 soques productores dels diferents antibiòtics cedides per altres investigadors i una selecció de 34 soques procedents d'un treball previ realitzat en el nostre grup de recerca. A la col·lecció s'hi troben soques candidates a ACB i BPCP de diverses malalties i plantes. Les 72 soques s'han caracteritzat fenotípica i genotípicament. La caracterització fenotípica s'ha portat a terme mitjançant la identificació a nivell d'espècie amb galeries API 20NE i proves bioquímiques específiques; la producció de metabòlits com PCA, Phl, Prn, IAA, HCN, quitinases i sideròfors mitjançant l'ús de diferents tècniques; antagonisme in vitro en diversos medis enfront dos fongs (Stemphylium vesicarium i Penicillium expansum) i tres bacteris fitopatògens (Erwinia amylovora, Pseudomonas syringae pv. syringae i Xanthomonas arboricola pv. juglandis); l'eficàcia de la inhibició de la infecció en bioassaigs in vivo sobre material vegetal enfront els fongs P. expansum en poma i S. vesicarium en fulles de perera i enfront el bacteri E. amylovora en fruits immadurs de perera i, finalment, en assaigs de promoció de creixement en dos portaempelts comercials de Prunus. Cal destacar que P. expansum causa la podridura blava en pomes i peres en postcollita, S. vesicarium la taca bruna de la perera i E. amylovora el foc bacterià de les rosàcies. El nombre de soques de Pseudomonas, sobre el total de les 72 estudiades, productores d'IAA (4) i quitinases (6) és baix, mentre que és elevat en el cas del HCN (32), que a més està associat a la producció de Phl. Els resultats obtinguts en l'antagonisme in vitro han mostrat en el cas dels bacteris que és dependent del patogen indicador i del medi de cultiu. La presència o absència de ferro no sembla ser un factor que potencií l'antagonisme. En el cas dels fongs no s'ha observat però, influència del medi de cultiu emprat. En el total de 72 soques s'ha observat un percentatge baix de soques que manifesten antagonisme en tots els medis assajats vers 3 o 4 dels patògens (7). Solament 2 d'aquestes 7 soques han mostrat ser també efectives en bioassaigs d'inhibició de les infeccions causades per 2 dels 3 patògens assajats. Algunes de les soques efectives en els bioassaigs no són antagonistes in vitro en cap dels medis assajats enfront el mateix patogen. En el cas de la promoció del creixement, s'han observat més soques promotores del creixement del portaempelts de prunera Marianna 2624 que no en l'híbrid de presseguer-ametller GF677 i les eficàcies assolides són també majors en el cas de Marianna 2624, detectant una elevada especificitat soca/portaempelts La caracterització genotípica s'ha realitzat mitjançant l'anàlisi dels polimorfismes en la longitud dels fragments de restricció de DNA ribosomal (RFLP-rDNA) i l'anàlisi dels polimorfismes en la longitud dels fragments de macrorestricció genòmica de DNA cromosòmic separats per electroforesi en camp polsant (MRFLP-PFGE). Ambdues anàlisis van mostrar una gran heterogeneïtat genètica entre les soques caracteritzades i no s'ha pogut relacionar les agrupacions obtingudes amb les característiques fenotípiques o capacitat d'actuar com a ACB o BPCP. Els patrons de macrorestricció genòmica (MRFLP-PFGE) del bacteri model P. fluorescens EPS288 són estables en el temps i independents de les condicions de cultiu assajades al laboratori o en mostres naturals, mostrant ser una tècnica eficaç en la identificació de reaïllats de mostres naturals inoculades prèviament amb el bacteri. Una selecció de soques que comparteixen el fet de produir floroglucinol s'han caracteritzat mitjançant RFLP i seqüenciació del gen phlD. S'ha establert una relació entre les agrupacions obtingudes en les anàlisis RFLP-rDNA, RFLP-phlD i les seqüències del gen. En l'anàlisi filogenètica de les seqüències del gen phlD s'ha observat un elevat grau de polimorfisme obtenint-se 3 agrupacions principals. Les agrupacions semblen relacionar-se amb els patrons de producció de metabòlits (Phl, HCN i Prn en una primera agrupació; Phl i HCN en la segona i solament Phl en la tercera), però aquestes no s'han pogut relacionar amb l'origen geogràfic de les soques o la seva activitat com a ACBs i/o BPCP. Amb les dades obtingudes de la caracterització fenotípica i genotípica s'ha realitzat una anàlisi multivariant (correspondències, correlacions d'Spearman i de freqüències amb variables categòriques). S'ha demostrat la importància de disposar d'una tècnica que permeti depurar una col·lecció de soques descartant les soques genèticament idèntiques, ja que influeixen en els resultats de les anàlisis. Pels tres patògens assajats com a indicadors i els dos portaempelts emprats, no s'ha observat cap correlació entre la inhibició de la infecció o la promoció del creixement amb les característiques fenotípiques i genotípiques de les soques que fos significatiu i consistent en les tres tècniques emprades.

Effect of minerals on casein micelle stability of cows' milk

The effects of minerals on casein micelle stability of individual cows' milk, throughout a complete lactation, were investigated. Calcium and calcium ions, magnesium, phosphorus, sodium, potassium and citrate contents were analysed, together with the following physical properties of milk; pH, ethanol stability, rennet clotting time and coagulum firmness. There was an inverse non-linear relationship between free calcium ion concentration and ethanol stability (ES; r=0.84). Rennet coagulation time showed a weaker relationship with free calcium ion concentration (r=0.44) but a stronger relationship with pH (r=0.66). In addition, samples containing higher amounts of free calcium ions produced a firmer gel. Citrate in natural samples acts as a stabilizing factor, as it slightly improves milk stability. Potassium, on the other hand, exhibited a negative correlation, but only with rennet clotting time (r=-0.52). Throughout lactation the average values were; free Ca 21 concentration 1.88 mm,, pH 6.63, ES 83.2% and clotting time 13.6 min. The equilibrium relationship between pH and free Ca2+ concentration was investigated by adjusting milk pH from 5.9 to 7.1, using acid and alkali. There was a good inverse linear relationship between pH and log (free Ca 21) for individual milk samples, with a gradient of -0.62 and a standard deviation of 0.042.