Síntese de azacalixarenos para o reconhecimento molecular de aniões

No âmbito desta dissertação são apresentados novos recetores sintéticos baseados na plataforma macrocíclica tetraazacalix[2]areno[2]triazina incorporando bases de purina ou unidades de aminoácidos naturais. Estes recetores foram preparados tendo como objectivo o reconhecimento seletivo de fármacos e aniões biologicamente relevantes. No primeiro capítulo é apresentada uma revisão bibliográfica sobre recetores derivados de tetraazacalix[2]areno[2]triazina demonstrando-se que a funcionalização desta plataforma, nos anéis de triazina ou nos anéis benzénicos, encontra-se ainda na infância bem como a investigação das suas afinidades para aniões. Subsequentemente, considerando os aniões principais estudados nesta tese, aniões carboxilatos alifáticos, aromáticos e aminoácidos é apresentada uma revisão bibliográfica sobre os estudos de reconhecimento molecular reportados na literatura, entre derivados de calix[4]areno e este tipo de aniões. No segundo capítulo descrevem-se as sínteses de recetores com uma ou duas unidades de aminoácido, L-alanina (AC1A, AC2A) e L-triptofano (AC2T), ancoradas nos anéis benzénicos da plataforma tetraazacalix[2]areno[2]triazina. Como demostrado no capítulo 3, os grupos N-H dos azotos em ponte são locais de reconhecimento de aniões. Neste contexto, estes macrociclos foram também metilados nos azotos em ponte (Me4AC2A e Me4AC2T) de modo a direcionar o reconhecimento cooperativo de aniões exclusivamente através dos grupos N-H das unidades de aminoácidos. A lipofilicidade destas moléculas foi alterada por substituição dos átomos de cloro das triazinas por dihexilamina. Os compostos sintetizados foram caracterizados através de técnicas espetroscópicas complementadas em alguns compostos por difração de raios X de cristal único. No capítulo 3 apresentam-se os estudos de reconhecimento molecular entre os recetores sintetizados e aniões derivados de ácidos carboxílicos (mono, di e tricarboxílicos) alifáticos, aromáticos, isoméricos e aniões inorgânicos. Estes estudos foram efetuados em DMSO-d6 ou em CDCl3 por titulações de RMN de 1H com determinação das respetivas constantes de associação. Para os recetores AC1A e AC2A o reconhecimento da maioria dos aniões estudados ocorre simultaneamente através dos grupos N-H dos azotos em ponte e do N-H da amida do braço da L-alanina. Contudo, no caso do isoftalato e tricarboxilato, com dois e três grupos carboxilato em posição meta, ocorre preferencialmente através dos dois braços de L-alanina como sugerido por estudos de dinâmica molecular em DMSO. Os estudos de associação realizados para os macrociclos que contêm unidades de L-triptofano, AC2T e Me4AC2T, mostraram que o reconhecimento de aniões é efetuado preferencialmente através de ligações de hidrogénio estabelecidas com os grupos amida e amina do grupo indole dos braços de aminoácido em detrimento das aminas em ponte como em AC1A e AC2A. Para a série dos carboxilatos alifáticos verifica-se que o recetor Me4AC2A tem maior afinidade com o anião glutarato (K= 389 M-1, DMSO-d6) enquanto o recetor Me4AC2T associa-se mais fortemente com o anião oxalato (K= 776 M-1, CDCl3). Todas as Job plots efetuadas confirmaram que as entidades estudadas obedeciam a uma estequiometria recetor/anião de 1:1.

Analysis of the organic matter associated to sea salt : definition of potential molecular markers based on the volatile composition and presence of glycosidic derivatives and polysaccharides

Sea salt is a natural product obtained from the evaporation of seawater in saltpans due to the combined effect of wind and sunlight. Nowadays, there is a growing interest for protection and re-valorisation of saltpans intrinsically associated to the quality of sea salt that can be evaluated by its physico-chemical properties. These man-made systems can be located in different geographical areas presenting different environmental surroundings. During the crystallization process, organic compounds coming from these surroundings can be incorporated into sea salt crystals, influencing their final composition. The organic matter associated to sea salt arises from three main sources: algae, surrounding bacterial community, and anthropogenic activity. Based on the hypothesis that sea salt contains associated organic compounds that can be used as markers of the product, including saltpans surrounding environment, the aim of this PhD thesis was to identify these compounds. With this purpose, this work comprised: 1) a deep characterisation of the volatile composition of sea salt by headspace solid phase microextraction combined with comprehensive two-dimensional gas chromatography time-of-flight mass spectrometry (HS-SPME/GCGC–ToFMS) methodology, in search of potential sea salt volatile markers; 2) the development of a methodology to isolate the polymeric material potentially present in sea salt, in amounts that allow its characterisation in terms of polysaccharides and protein; and 3) to explore the possible presence of triacylglycerides. The high chromatographic resolution and sensitivity of GC×GC–ToFMS enabled the separation and identification of a higher number of volatile compounds from sea salt, about three folds, compared to unidimentional chromatography (GC–qMS). The chromatographic contour plots obtained revealed the complexity of marine salt volatile composition and confirmed the relevance of GC×GC–ToFMS for this type of analysis. The structured bidimentional chromatographic profile arising from 1D volatility and 2D polarity was demonstrated, allowing more reliable identifications. Results obtained for analysis of salt from two locations in Aveiro and harvested over three years suggest the loss of volatile compounds along the time of storage of the salt. From Atlantic Ocean salts of seven different geographical origins, all produced in 2007, it was possible to identify a sub-set of ten compounds present in all salts, namely 6-methyl-5-hepten-2-one, 2,2,6-trimethylcyclohexanone, isophorone, ketoisophorone, β-ionone-5,6-epoxide, dihydroactinidiolide, 6,10,14-trimethyl-2-pentadecanone, 3-hydroxy-2,4,4-trimethylpentyl 2-methylpropanoate, 2,4,4-trimethylpentane-1,3-diyl bis(2-methylpropanoate), and 2-ethyl-1-hexanol. These ten compounds were considered potential volatile markers of sea salt. Seven of these compounds are carotenoid-derived compounds, and the other three may result from the integration of compounds from anthropogenic activity as metabolites of marine organisms. The present PhD work also allowed the isolation and characterisation, for the first time, of polymeric material from sea salt, using 16 Atlantic Ocean salts. A dialysis-based methodology was developed to isolate the polymeric material from sea salt in amounts that allowed its characterisation. The median content of polymeric material isolated from the 16 salts was 144 mg per kg of salt, e.g. 0.014% (w/w). Mid-infrared spectroscopy and thermogravimetry revealed the main occurrence of sulfated polysaccharides, as well as the presence of protein in the polymeric material from sea salt. Sea salt polysaccharides were found to be rich in uronic acid residues (21 mol%), glucose (18), galactose (16), and fucose (13). Sulfate content represented a median of 45 mol%, being the median content of sulfated polysaccharides 461 mg/g of polymeric material, which accounted for 66 mg/kg of dry salt. Glycosidic linkage composition indicates that the main sugar residues that could carry one or more sulfate groups were identified as fucose and galactose. This fact allowed to infer that the polysaccharides from sea salt arise mainly from algae, due to their abundance and composition. The amino acid profile of the polymeric material from the 16 Atlantic Ocean salts showed as main residues, as medians, alanine (25 mol%), leucine (14), and valine (14), which are hydrophobic, being the median protein content 35 mg/g, i.e. 4,9 mg per kg of dry salt. Beside the occurrence of hydrophobic volatile compounds in sea salt, hydrophobic non-volatile compounds were also detected. Triacylglycerides were obtained from sea salt by soxhlet extraction with n-hexane. Fatty acid composition revealed palmitic acid as the major residue (43 mol%), followed by stearic (13), linolenic (13), oleic (12), and linoleic (9). Sea salt triacylglycerides median content was 1.5 mg per kg of dry salt. Both protein and triacylglycerides seem to arise from macro and microalgae, phytoplankton and cyanobacteria, due to their abundance and composition. Despite the variability resulting from saltpans surrounding environment, this PhD thesis allowed the identification of a sea salt characteristic organic compounds profile based on volatile compounds, polysaccharides, protein, and triacylglycerides.