Avaliação da contaminação conjunta de Dekkera bruxellensis e Lactobacillus fermentum sobre a fermentação alcoólica: efeito do substrato e formas de controle

As contaminações por leveduras selvagens e por bactérias no processo de produção de etanol combustível no Brasil causam prejuízos ao rendimento fermentativo e aumento de custos pelo uso de biocidas. No entanto, poucos estudos tem focado no efeito das contaminações conjuntas de leveduras selvagens e bactérias e as possíveis interações entre os micro-organismos, especialmente em função dos diferentes substratos de fermentação e das formas de controle. Este trabalho teve por objetivos verificar o efeito do substrato (caldo de cana e melaço) sobre o desenvolvimento das contaminações pela levedura da espécie Dekkera bruxellensis e pela bactéria Lactobacillus fermentum, em co-culturas com Saccharomyces cerevisiae (linhagem industrial PE-2) e possíveis formas de controle do crescimento dos contaminantes (pelo uso de metabissulfito de potássio e adição de etanol ao tratamento ácido) sem afetar a levedura do processo. Os testes foram realizados em condições de crescimento (substrato com 4 °Brix, culturas agitadas) e fermentação com reciclo celular (substrato com 16 °Brix, culturas estáticas). Houve interação entre as leveduras e a bactéria quando crescidas em caldo de cana 4 °Brix. A levedura industrial não foi afetada pela presença dos micro-organismos contaminantes, no entanto, para D. bruxellensis a presença de L. fermentum interferiu positivamente no crescimento, com aumento no número de UFC, e consequentemente inibição do crescimento da bactéria. Em melaço, houve um estímulo ao crescimento de L. fermentum quando em co-cultura com S. cerevisiae. Houve influência das contaminações sobre os parâmetros avaliados no experimento (pH, açúcar redutor total, etanol, glicerol e crescimento das células) e a contaminação conjunta de L. fermentum e D. bruxellensis potencializou o efeito das contaminações pelos micro-organismos isoladamente, tanto em caldo quanto em melaço. A adição de 13% de etanol à solução de ácido sulfúrico pH 2,0 no tratamento celular resultou em uma diminuição significativa no número de UFC de D. bruxellensis (entre 90-99%). A levedura PE-2 foi pouco afetada pelo tratamento proposto. A bactéria L. fermentum teve seu crescimento afetado em todas as combinações testadas. Como os experimentos foram feitos em co-culturas, verificouse que pode haver influência de um micro-organismo sobre a viabilidade do outro, dependendo da reação ao tratamento ácido-etanol. O metabissulfito de potássio (MBP), no intervalo entre 200-400 mg/L, foi eficaz para controlar o crescimento de D. bruxellensis dependendo do meio de cultura e linhagem. Quando adicionado (250 mg/L) à solução ácida (pH 2,0) no tratamento celular, um efeito significativo foi observado nas culturas mistas, pois ocorreu a inativação do SO2 pela S. cerevisiae e uma provável proteção das células de D. bruxellensis, não sendo essa levedura prejudicada pelo MBP. A resposta fisiológica de S. cerevisiae na presença de MBP pode explicar a diminuição significativa na produção de etanol. Quando o MBP foi adicionado ao meio de fermentação, resultou no controle da D. bruxellensis mas não em sua morte, com efeito menos intensivo sobre a eficiência fermentativa. Em cocultura com a adição de MBP, a eficiência fermentativa foi significativamente menor do que na ausência de MBP.

Desenvolvimento de embalagem biodegradável ativa a base de fécula de mandioca e agentes antimicrobianos naturais.

Aliado ao fato dos biomateriais ainda serem pouco explorados pelas indústrias alimentícias, este trabalho propôs o desenvolvimento de embalagens que sejam, além de biodegradáveis, também ativas através do uso de um agente antimicrobiano natural capaz de inibir a proliferação de fungos correntes em produtos de panificação (Penicillium commune e Eurotium amstelodami). Primeiramente, filmes biodegradáveis a base de fécula de mandioca foram elaborados pela técnica de casting, usando açúcares e glicerol como plastificantes. O aumento do conteúdo de glicerol causou diminuição da resistência máxima à tração e elevação dos valores de propriedades de barreira. Numa segunda etapa do trabalho, a introdução de nanopartículas de argila esmectita influenciou positivamente as propriedades de barreira dos filmes, devido à diminuição observada nos valores de permeabilidade ao vapor de água e coeficiente de permeabilidade ao oxigênio. Nesta fase, a variação do conteúdo de glicerol também afetou significativamente as propriedades mecânicas e de barreira dos filmes biodegradáveis. As concentrações inibitórias mínimas dos óleos essenciais de cravo e de canela contra os fungos estudados foram definidas e o óleo essencial de canela foi selecionado, para ser incorporado aos filmes biodegradáveis, em três conteúdos distintos, pois foi o composto que mostrou uma inibição mais eficiente. A atividade antimicrobiana dos filmes biodegradáveis com incorporação de óleo essencial de canela foi testada sobre os micro-organismos escolhidos através de testes de difusão em halo, cujos resultados foram suficientes para demonstrar o potencial ativo da embalagem desenvolvida. Como método alternativo de incorporação do agente antimicrobiano, gás carbônico (CO2) em estado supercrítico foi utilizado como solvente. Os resultados obtidos foram promissores, uma vez que se observou incorporação de agente antimicrobiano dentro da matriz polimérica em quantidade suficiente para inibir a proliferação dos fungos testados.

Determinação a baixo custo de açúcares redutores totais em caldo-de-cana, empregando sistemas de análise por injeção em fluxo com o uso de DNS

Determinação a baixo custo de açúcares redutores totais em caldo-de-cana, empregando sistema de análise por injeção em fluxo com o uso de DNS Um sistema de análise por injeção em fluxo foi utilizado para a determinação de açúcares redutores totais em caldo-de-cana. O método é baseado na hidrólise da sacarose, seguido da oxidação dos açúcares redutores pelo ácido 3,5-dinitrosalicílico (DNS) em meio alcalino, e determinação espectrofotométrica em 510 nm. Visando obter melhor sensibilidade e seletividade, os parâmetros volume de amostra e comprimento dos reatores foram estudados para avaliar o comportamento das curvas analíticas. Foram utilizados mini-compressores de aquários no lugar de bomba peristálticas e cela espectrofotométrica em acrílico no lugar de cela de vidro importada, a fim de minimizar o consumo de reagentes e o custo do sistema FIA. O presente sistema foi comparado ao método Lane-Eynon recomendado pelo Ministério da Agricultura. Usando o teste-t, não foram constatadas diferenças significativas entre os resultados dos dois métodos, sendo que os desvios relativos foram ao redor de 1%. O método permite analisar cerca de 14 amostras h-1 com desvio padrão relativo inferior a 1,35%.

Neurospora crassa transcriptomics reveals oxidative stress and plasma membrane homeostasis biology genes as key targets in response to chitosan

Chitosan is a natural polymer with antimicrobial activity. Chitosan causes plasma membrane permeabilization and induction of intracellular reactive oxygen species (ROS) in Neurospora crassa. We have determined the transcriptional profile of N. crassa to chitosan and identified the main gene targets involved in the cellular response to this compound. Global network analyses showed membrane, transport and oxidoreductase activity as key nodes affected by chitosan. Activation of oxidative metabolism indicates the importance of ROS and cell energy together with plasma membrane homeostasis in N. crassa response to chitosan. Deletion strain analysis of chitosan susceptibility pointed NCU03639 encoding a class 3 lipase, involved in plasma membrane repair by lipid replacement, and NCU04537 a MFS monosaccharide transporter related to assimilation of simple sugars, as main gene targets of chitosan. NCU10521, a glutathione S-transferase-4 involved in the generation of reducing power for scavenging intracellular ROS is also a determinant chitosan gene target. Ca2+ increased tolerance to chitosan in N. crassa. Growth of NCU10610 (fig 1 domain) and SYT1 (a synaptotagmin) deletion strains was significantly increased by Ca2+ in the presence of chitosan. Both genes play a determinant role in N. crassa membrane homeostasis. Our results are of paramount importance for developing chitosan as an antifungal.

Redistribution of Soil Organic Matter by Permafrost Disturbance in the Canadian High Arctic

With increased warming in the Arctic, permafrost thaw may induce localized physical disturbance of slopes. These disturbances, referred to as active layer detachments (ALDs), redistribute soil across the landscape, potentially releasing previously unavailable carbon (C). In 2007–2008, widespread ALD activity was reported at the Cape Bounty Arctic Watershed Observatory in Nunavut, Canada. Our study investigated organic matter (OM) composition in soil profiles from ALD-impacted and undisturbed areas. Solid-state 13C nuclear magnetic resonance (NMR) and solvent-extractable biomarkers were used to characterize soil OM. Throughout the disturbed upslope profile, where surface soils and vegetation had been removed, NMR revealed low O-alkyl C content and biomarker analysis revealed low concentrations of solvent-extractable compounds suggesting enhanced erosion of labile-rich OM by the ALD. In the disturbed downslope region, vegetation remained intact but displaced material from upslope produced lateral compression ridges at the surface. High O-alkyl content in the surface horizon was consistent with enrichment of carbohydrates and peptides, but low concentrations of labile biomarkers (i.e., sugars) suggested the presence of relatively unaltered labile-rich OM. Decreased O-alkyl content and biomarker concentrations below the surface contrasted with the undisturbed profile and may indicate the loss of well-established pre-ALD surface drainage with compression ridge formation. However, pre-ALD profile composition remains unknown and the observed decreases may result from nominal pre-ALD OM inputs. These results are the first to establish OM composition in ALD-impacted soil profiles, suggesting reallocation of permafrost-derived soil C to areas where degradation or erosion may contribute to increased C losses from disturbed Arctic soils.

Time Evolution of Physicochemical Properties of Carrots During the Drying Process

This study is aimed to determine the properties of Nantes carrots while drying by hot air at three different temperatures (50, 60 and 70 ºC). The chemical properties evaluated were: moisture, pro- tein, fibre, ash, sugars and water activity, and the physical properties were: texture, color, density and porosity. The results showed that the drying at 70 ºC affected mostly the chemical properties analyzed. Regarding the texture, similar changes were recorded in terms of hardness, gumminess and chewiness at the temperature of 70 ºC that affected these properties the most. Regarding color, in general the vari- ations in a* and b* along drying were not meaningful, although some discoloration was observed (in- crease in L*). The porosity increased due to the decrease in humidity. The final porosity measured for the carrots dried at 70 ºC was; however, lower than those for 50 and 60 ºC.

Dissolved organic carbon in sediments of the central Arctic Ocean collected during POLARSTERN cruise ARK-XXVII/3 from August-September 2012

Marine organic matter (OM) sinks from surface waters to the seafloor via the biological pump. Benthic communities, which use this sedimented OM as energy and carbon source, produce dissolved organic matter (DOM) in the process of remineralization, enriching the sediment porewater with fresh DOM compounds. We hypothesized that in the oligotrophic deep Arctic basin the molecular signal of freshly deposited primary produced OM is restricted to the surface sediment pore waters which should differ from bottom water and deeper sediment pore water in DOM composition. This study focused on: 1) the molecular composition of the DOM in sediment pore waters of the deep Eurasian Arctic basins, 2) whether the signal of marine vs. terrigenous DOM is represented by different compounds preserved in the sediment pore waters and 3) whether there is any relation between Arctic Ocean ice cover and DOM composition. Molecular data, obtained via 15 Tesla Fourier transform ion cyclotron resonance mass spectrometer, were correlated with environmental parameters by partial least square analysis. The fresher marine detrital OM signal from surface waters was limited to pore waters from < 5 cm sediment depth. The productive ice margin stations showed higher abundances of peptides, unsaturated aliphatics and saturated fatty acids formulae, indicative of fresh OM/pigments deposition, compared to northernmost stations which had stronger aromatic signals. This study contributes to the understanding of the coupling between the Arctic Ocean productivity and its depositional regime, and how it will be altered in response to sea ice retreat and increasing river runoff.

Geochemistry of labile organic matter in sediments and interstitial waters of ODP Sites 107-651 and 107-653

Sediment and interstitial water from Sites 651 and 653 (ODP Leg 107) were investigated by organic geochemical methods to characterize labile organic compound classes (amino compounds and carbohydrates) and to evaluate their progressive diagenetic and thermal degradation in deep-sea sediments. Downhole distribution of dissolved organic carbon (DOC) appears related to redox zones associated with bacterial activity and of diagenetic recrystallization of biogenic tests and not so much to organic matter concentrations in ambient sediments. DOC ranges from 250 to 8300 µmol/L (3-100.1 ppm). Amino acids contribute 10%-0.3% of DOC; carbohydrates range from 78 to 5 µmol/L. Rate of degradation of amino acids by thermal effects and/or bacterial activity at both sites (significantly different in sedimentation rates: average 41 cm/1000 yr in the top 300 m at Site 651, average 3.9 cm/1000 yr in the Pliocene/Quaternary sequence at Site 653 to 220 mbsf) is more dependent on exposure time rather than on the depth within the sediment column. Variability in neutral, acidic, and basic amino acid fractions of total amino acids (with a range of 1.1-0.02 µmol/g sediment; up to 2.5% of organic carbon) varies with carbonate content and by differences in thermal stability of amino acids. Distribution patterns of monosaccharides are interpreted to result from differences in organic matter sources, sedimentation rates, and the degree of organic matter decomposition prior to and subsequent to burial. Total particulate carbohydrates range from 1.82 to 0.21 µmol/g sediment and contribute about 8% to the sedimentary organic matter. Investigation of trace metals in the interstitial waters did not show any correlation of either DOC, amino compounds, or carbohydrates.

Humic acids in bottom sediments of the Western Pacific

Elemental composition, functional groups, and molecular mass distribution were determined in humic acids from the Western Pacific abyssal and coastal bottom sediments. Humic acid structure was studied by oxidative degradation with alkaline nitrobenzene and potassium permanganate, p-coumaric, guaiacilic, and syringilic structural units typical for lignin of terrestrial plants were identified in humic acids by chromatographic analysis of oxidation products. Polysubstituted and polycondensed aromatic systems with minor proportion of aliphatic structures were basic structural units of humic acids in abyssal sediments.

Dissolved organic carbon concentrations, amino sugar concentrations and highly significantly correlating FT-ICR mass peak magnitudes obtained from solid phase extracted marine dissolved organic matter during POLARSTERN cruise ANT-XXV/1

Dissolved organic matter (DOM) was extracted with solid phase extraction (SPE) from 137 water samples from different climate zones and different depths along an Eastern Atlantic Ocean transect. The extracts were analyzed with Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) with electrospray ionization (ESI). D14C analyses were performed on subsamples of the SPE-DOM. In addition, the amount of dissolved organic carbon was determined for all water and SPE-DOM samples as well as the yield of amino sugars for selected samples. Linear correlations were observed between the magnitudes of 43% of the FT-ICR mass peaks and the extract D14C values. Decreasing SPE-DOM D14C values went along with a shift in the molecular composition to higher average masses (m/z) and lower hydrogen/carbon (H/C) ratios. The correlation was used to model the SPE-DOM D14C distribution for all 137 samples. Based on single mass peaks a degradation index was developed to compare the degradation state of marine SPE-DOM samples analyzed with FT-ICR MS. A correlation between D14C, degradation index, DOC values and amino sugar yield supports that SPE-DOM analyzed with FT-ICR MS reflects trends of bulk DOM. A relative mass peak magnitude ratio was used to compare aged SPE-DOM and fresh SPE-DOM regarding single mass peaks. The magnitude ratios show a continuum of different reactivities for the single compounds. Only few of the compounds present in the FT-ICR mass spectra are expected to be highly degraded in the oldest water masses of the Pacific Ocean. All other compounds should persist partly thermohaline circulation. Prokaryotic (bacterial) production, transformation and accumulation of this very stable DOM occurs probably primarily in the upper ocean. This DOM is an important contribution to very old DOM, showing that production and degradation are dynamic processes.

The complete confectioner, or, Housekeeper's guide to a simple and speedy method of understanding the whole art of confectionary : the various ways of preserving and candying, dry and liquid, all kinds of fruit, nuts, flowers, herbs, &c. And the method of keeping them fresh and fine all the year round; the different ways of clarifying sugar; with directions for making fruit pastes, bomboons, pastils, compotes, fruit ices, cream ices, marmalades, jellies, jams, cakes, puffs, biscuits, tarts, custards, cheesecakes, sweetmeats, fritters, creams, syllabubs, blanc-mange, flummeries, ornaments for grand entertainments, dragees, syrups of all kinds, nicknacks and trifles for desserts, strong cordials, oils, simple waters, milk punch that will keep 20 years, and all sorts of English wines. Also, the art of making artificial fruit, with the stalks in it, so as to resemble the natural fruit. To which are added, some bills of fare for desserts for private families /

Originally published under title: The compleat confectioner. Cf. Bitting, K.G. Gastronomic bib., p. 190.

Commercial organic analysis. A treatise on the properties, proximate analytical examination, and modes of assaying the various organic chemicals and products employed in the arts, manufactures, medicine, etc., with concise methods for the detection and determination of their impurities, adulterations, and products of decomposition.

v.I. Introduction. Alcohols, neutral alcoholic derivatives, sugars, starch and its isomers, vegetable acids, etc. 2d ed., rev. & enl.--v.II. Fixed oils, fats, waxes, glycerol, nitroglycerin and nitroglycerin explosives. Hydrocarbons, petroleum and coal-tar products, asphalt, phenols and creosotes. 2d ed., rev. & enl.--v. III, pt.I. Acid derivatives of phenols, aromatic acids, resins, and essential oils. Tannins, dyes, and colouring matters, writing inks. 2d ed., rev. & enl.--v. III, pt.II. Amines and ammonium bases, hydrarzines, bases from tar, vegetable alkaloids. 2d ed., rev. and enl. [1892] --v.III, pt.III. Vegetable alkaloids (concluded), non-basic vegetable bitter principles, animal bases, animal acids, cyanogen and its derivatives. 2d ed., rev. & enl. [1896]--v.IV. Proteids and albuminous principles, proteoïds or albuminoïds. 2d ed., rev. & enl. 1898.

Allen's commercial organic analysis; a treatise on the properties, modes of assaying, and proximate analytical examination of the various organic chemicals and products employed in the arts, manufactures, medicine, etc., with concise methods for the detection and estimation of their impurities, adulterations, and products of decomposition ...

Vols. 3-9 edited by W.A. Davis and Samuel S. Sadtler.