The following research has focused on the utility of Ulva as an indicator of seawater nitrogen loading. Evaluation was made in three ways: 1) Observation of large-scale geographic variation in nitrogen status in natural populations around New Zealand in summer and winter, 2) Laboratory-based experimental assessment of the biochemical responses of N-indices in Ulva to nitrogen enrichment, and 3) Culturing standardized test-Ulva under low nutrient conditions which could be deployed into a variety of field situations. Seawater inorganic nutrient (nitrate, nitrite, ammonium and phosphate) concentrations and nitrogen (N)-indices (free amino acids, chlorophyll and total tissue nitrogen) in natural Ulva populations from 32 sites around New Zealand were compared. Sites were divided into 6 environmental categories: sheltered rural, exposed rural, rock pools, sheltered urban, exposed urban, and nitrogen-enriched urban sites. Seawater nutrient concentrations were highly variable between all sites in summer and winter. However, in the summer enriched urban sites had the highest mean total inorganic nitrogen concentrations and Ulva with the highest mean levels of all N-indices compared with any other environmental category. In the winter, Ulva contained more nitrogen (reflected in all N-indices) compared with Ulva in the summer, particularly in populations growing in colder southern seawater on more exposed coasts. The increase in Ulva N-status was not explained by increased seawater inorganic nitrogen concentrations. With univariate and multivariate statistical approaches it was shown that there was a significant effect of seawater temperature and site exposure on N-status in Ulva. Compared with other N-indices, stable nitrogen isotopes (δ15N) from Ulva growing in enriched urban sites had the widest range (4.77 ± 0.04 ‰ to 15.16 ± 0.03 ‰) of values compared with all other categories in both summer and winter. Conversely, Ulva from exposed rural sites had the lowest range of δ15N values compared with any other category (6.7 ± 0.1 to 8.8 ± 0.1 ‰) and showed no seasonal change in mean values (7.8 ‰ and 7.6 ‰ for summer and winter, respectively). In addition, δ15N values in Ulva were the only N-index that showed a significant difference between urban and rural categories. To test the relationship between inorganic nitrogen concentration in seawater and the responses of biochemical nitrogen indices in Ulva pertusa, several experiments were conducted in an outdoor, flow-through culture apparatus, in summer and winter. In this apparatus effects of ammonium concentration, nitrogen source (nitrate and ammonium), light and seawater motion were investigated. Of the same three N-indices examined in natural Ulva populations (free amino acids, chlorophyll and total tissue nitrogen), increases in free amino acids, particularly asparagine, provided the strongest indicator of increases in nitrogen availability. In addition, while tissue nitrogen and chlorophyll also increased with seawater nitrogen concentration, it was apparent that these indices were also strongly influenced by light, and probably season. Rates of ammonium assimilation provided no overall measure of the availability of nitrogen in seawater and were clearly affected by season. Similarly, growth rates in Ulva only showed a response to nitrogen addition in summer months. Stable isotopes of nitrogen (δ15N) in Ulva provided a clear distinction between natural and synthetic nitrogen sources, but more importantly, showed only minor fractionation (ranging from 1.3 ‰ to -1.9 ‰) of 15N supplied from synthetic nitrate and ammonium under both light-saturating and light-limiting conditions. To further develop Ulva as a standardized test-organism it was cultured in low-nutrient (non-polluted) seawater to deplete internal storage pools of nitrogen. Each month the resulting test-Ulva was then placed in surface-moored growth enclosures at a range of coastal sites around Auckland and then monitored for one year. In winter there were increases in seawater inorganic nitrogen concentrations and concomitant increases in free amino acid content. However, tissue nitrogen and chlorophyll content in test-Ulva showed similar increases (possibly saturating) across all sites suggesting that seasonal increases in these N-indices were also due to other seasonal factors (e.g., surface irradiance and / or seawater temperature). On the other hand, the total free amino acid pool showed strong differences between a low-nitrogen reference site and the other study sites all year round. It was probable that test-Ulva was integrating differences in tidally-averaged nitrogen loading that were not reliably detected in instantaneous seawater samples. In addition to N-indices in test-Ulva, levels of tissue heavy metals and stable isotopes of nitrogen showed strong differences with higher values of both typically found in urban environments compared with values found in non-polluted reference sites. It is concluded that several abiotic and biotic factors affect nitrogen status in Ulva, but the average nitrogen concentration in seawater, and the physical factors of temperature, light and water motion, appear to be the overarching determinants. It is further suggested that in combination with Ulva tissue δ15N values, tissue nitrogen and the free amino acid pool, as quantitative biochemical measures of nitrogen availability, are likely to provide useful information on both the amount and composition of nitrogen entering coastal environments. / Foundation for Research, Science and Technology. Auckland Regional Council.

The following research has focused on the utility of Ulva as an indicator of seawater nitrogen loading. Evaluation was made in three ways: 1) Observation of large-scale geographic variation in nitrogen status in natural populations around New Zealand in summer and winter, 2) Laboratory-based experimental assessment of the biochemical responses of N-indices in Ulva to nitrogen enrichment, and 3) Culturing standardized test-Ulva under low nutrient conditions which could be deployed into a variety of field situations. Seawater inorganic nutrient (nitrate, nitrite, ammonium and phosphate) concentrations and nitrogen (N)-indices (free amino acids, chlorophyll and total tissue nitrogen) in natural Ulva populations from 32 sites around New Zealand were compared. Sites were divided into 6 environmental categories: sheltered rural, exposed rural, rock pools, sheltered urban, exposed urban, and nitrogen-enriched urban sites. Seawater nutrient concentrations were highly variable between all sites in summer and winter. However, in the summer enriched urban sites had the highest mean total inorganic nitrogen concentrations and Ulva with the highest mean levels of all N-indices compared with any other environmental category. In the winter, Ulva contained more nitrogen (reflected in all N-indices) compared with Ulva in the summer, particularly in populations growing in colder southern seawater on more exposed coasts. The increase in Ulva N-status was not explained by increased seawater inorganic nitrogen concentrations. With univariate and multivariate statistical approaches it was shown that there was a significant effect of seawater temperature and site exposure on N-status in Ulva. Compared with other N-indices, stable nitrogen isotopes (δ15N) from Ulva growing in enriched urban sites had the widest range (4.77 ± 0.04 ‰ to 15.16 ± 0.03 ‰) of values compared with all other categories in both summer and winter. Conversely, Ulva from exposed rural sites had the lowest range of δ15N values compared with any other category (6.7 ± 0.1 to 8.8 ± 0.1 ‰) and showed no seasonal change in mean values (7.8 ‰ and 7.6 ‰ for summer and winter, respectively). In addition, δ15N values in Ulva were the only N-index that showed a significant difference between urban and rural categories. To test the relationship between inorganic nitrogen concentration in seawater and the responses of biochemical nitrogen indices in Ulva pertusa, several experiments were conducted in an outdoor, flow-through culture apparatus, in summer and winter. In this apparatus effects of ammonium concentration, nitrogen source (nitrate and ammonium), light and seawater motion were investigated. Of the same three N-indices examined in natural Ulva populations (free amino acids, chlorophyll and total tissue nitrogen), increases in free amino acids, particularly asparagine, provided the strongest indicator of increases in nitrogen availability. In addition, while tissue nitrogen and chlorophyll also increased with seawater nitrogen concentration, it was apparent that these indices were also strongly influenced by light, and probably season. Rates of ammonium assimilation provided no overall measure of the availability of nitrogen in seawater and were clearly affected by season. Similarly, growth rates in Ulva only showed a response to nitrogen addition in summer months. Stable isotopes of nitrogen (δ15N) in Ulva provided a clear distinction between natural and synthetic nitrogen sources, but more importantly, showed only minor fractionation (ranging from 1.3 ‰ to -1.9 ‰) of 15N supplied from synthetic nitrate and ammonium under both light-saturating and light-limiting conditions. To further develop Ulva as a standardized test-organism it was cultured in low-nutrient (non-polluted) seawater to deplete internal storage pools of nitrogen. Each month the resulting test-Ulva was then placed in surface-moored growth enclosures at a range of coastal sites around Auckland and then monitored for one year. In winter there were increases in seawater inorganic nitrogen concentrations and concomitant increases in free amino acid content. However, tissue nitrogen and chlorophyll content in test-Ulva showed similar increases (possibly saturating) across all sites suggesting that seasonal increases in these N-indices were also due to other seasonal factors (e.g., surface irradiance and / or seawater temperature). On the other hand, the total free amino acid pool showed strong differences between a low-nitrogen reference site and the other study sites all year round. It was probable that test-Ulva was integrating differences in tidally-averaged nitrogen loading that were not reliably detected in instantaneous seawater samples. In addition to N-indices in test-Ulva, levels of tissue heavy metals and stable isotopes of nitrogen showed strong differences with higher values of both typically found in urban environments compared with values found in non-polluted reference sites. It is concluded that several abiotic and biotic factors affect nitrogen status in Ulva, but the average nitrogen concentration in seawater, and the physical factors of temperature, light and water motion, appear to be the overarching determinants. It is further suggested that in combination with Ulva tissue δ15N values, tissue nitrogen and the free amino acid pool, as quantitative biochemical measures of nitrogen availability, are likely to provide useful information on both the amount and composition of nitrogen entering coastal environments. / Foundation for Research, Science and Technology. Auckland Regional Council.

The following research has focused on the utility of Ulva as an indicator of seawater nitrogen loading. Evaluation was made in three ways: 1) Observation of large-scale geographic variation in nitrogen status in natural populations around New Zealand in summer and winter, 2) Laboratory-based experimental assessment of the biochemical responses of N-indices in Ulva to nitrogen enrichment, and 3) Culturing standardized test-Ulva under low nutrient conditions which could be deployed into a variety of field situations. Seawater inorganic nutrient (nitrate, nitrite, ammonium and phosphate) concentrations and nitrogen (N)-indices (free amino acids, chlorophyll and total tissue nitrogen) in natural Ulva populations from 32 sites around New Zealand were compared. Sites were divided into 6 environmental categories: sheltered rural, exposed rural, rock pools, sheltered urban, exposed urban, and nitrogen-enriched urban sites. Seawater nutrient concentrations were highly variable between all sites in summer and winter. However, in the summer enriched urban sites had the highest mean total inorganic nitrogen concentrations and Ulva with the highest mean levels of all N-indices compared with any other environmental category. In the winter, Ulva contained more nitrogen (reflected in all N-indices) compared with Ulva in the summer, particularly in populations growing in colder southern seawater on more exposed coasts. The increase in Ulva N-status was not explained by increased seawater inorganic nitrogen concentrations. With univariate and multivariate statistical approaches it was shown that there was a significant effect of seawater temperature and site exposure on N-status in Ulva. Compared with other N-indices, stable nitrogen isotopes (δ15N) from Ulva growing in enriched urban sites had the widest range (4.77 ± 0.04 ‰ to 15.16 ± 0.03 ‰) of values compared with all other categories in both summer and winter. Conversely, Ulva from exposed rural sites had the lowest range of δ15N values compared with any other category (6.7 ± 0.1 to 8.8 ± 0.1 ‰) and showed no seasonal change in mean values (7.8 ‰ and 7.6 ‰ for summer and winter, respectively). In addition, δ15N values in Ulva were the only N-index that showed a significant difference between urban and rural categories. To test the relationship between inorganic nitrogen concentration in seawater and the responses of biochemical nitrogen indices in Ulva pertusa, several experiments were conducted in an outdoor, flow-through culture apparatus, in summer and winter. In this apparatus effects of ammonium concentration, nitrogen source (nitrate and ammonium), light and seawater motion were investigated. Of the same three N-indices examined in natural Ulva populations (free amino acids, chlorophyll and total tissue nitrogen), increases in free amino acids, particularly asparagine, provided the strongest indicator of increases in nitrogen availability. In addition, while tissue nitrogen and chlorophyll also increased with seawater nitrogen concentration, it was apparent that these indices were also strongly influenced by light, and probably season. Rates of ammonium assimilation provided no overall measure of the availability of nitrogen in seawater and were clearly affected by season. Similarly, growth rates in Ulva only showed a response to nitrogen addition in summer months. Stable isotopes of nitrogen (δ15N) in Ulva provided a clear distinction between natural and synthetic nitrogen sources, but more importantly, showed only minor fractionation (ranging from 1.3 ‰ to -1.9 ‰) of 15N supplied from synthetic nitrate and ammonium under both light-saturating and light-limiting conditions. To further develop Ulva as a standardized test-organism it was cultured in low-nutrient (non-polluted) seawater to deplete internal storage pools of nitrogen. Each month the resulting test-Ulva was then placed in surface-moored growth enclosures at a range of coastal sites around Auckland and then monitored for one year. In winter there were increases in seawater inorganic nitrogen concentrations and concomitant increases in free amino acid content. However, tissue nitrogen and chlorophyll content in test-Ulva showed similar increases (possibly saturating) across all sites suggesting that seasonal increases in these N-indices were also due to other seasonal factors (e.g., surface irradiance and / or seawater temperature). On the other hand, the total free amino acid pool showed strong differences between a low-nitrogen reference site and the other study sites all year round. It was probable that test-Ulva was integrating differences in tidally-averaged nitrogen loading that were not reliably detected in instantaneous seawater samples. In addition to N-indices in test-Ulva, levels of tissue heavy metals and stable isotopes of nitrogen showed strong differences with higher values of both typically found in urban environments compared with values found in non-polluted reference sites. It is concluded that several abiotic and biotic factors affect nitrogen status in Ulva, but the average nitrogen concentration in seawater, and the physical factors of temperature, light and water motion, appear to be the overarching determinants. It is further suggested that in combination with Ulva tissue δ15N values, tissue nitrogen and the free amino acid pool, as quantitative biochemical measures of nitrogen availability, are likely to provide useful information on both the amount and composition of nitrogen entering coastal environments. / Foundation for Research, Science and Technology. Auckland Regional Council.

The following research has focused on the utility of Ulva as an indicator of seawater nitrogen loading. Evaluation was made in three ways: 1) Observation of large-scale geographic variation in nitrogen status in natural populations around New Zealand in summer and winter, 2) Laboratory-based experimental assessment of the biochemical responses of N-indices in Ulva to nitrogen enrichment, and 3) Culturing standardized test-Ulva under low nutrient conditions which could be deployed into a variety of field situations. Seawater inorganic nutrient (nitrate, nitrite, ammonium and phosphate) concentrations and nitrogen (N)-indices (free amino acids, chlorophyll and total tissue nitrogen) in natural Ulva populations from 32 sites around New Zealand were compared. Sites were divided into 6 environmental categories: sheltered rural, exposed rural, rock pools, sheltered urban, exposed urban, and nitrogen-enriched urban sites. Seawater nutrient concentrations were highly variable between all sites in summer and winter. However, in the summer enriched urban sites had the highest mean total inorganic nitrogen concentrations and Ulva with the highest mean levels of all N-indices compared with any other environmental category. In the winter, Ulva contained more nitrogen (reflected in all N-indices) compared with Ulva in the summer, particularly in populations growing in colder southern seawater on more exposed coasts. The increase in Ulva N-status was not explained by increased seawater inorganic nitrogen concentrations. With univariate and multivariate statistical approaches it was shown that there was a significant effect of seawater temperature and site exposure on N-status in Ulva. Compared with other N-indices, stable nitrogen isotopes (δ15N) from Ulva growing in enriched urban sites had the widest range (4.77 ± 0.04 ‰ to 15.16 ± 0.03 ‰) of values compared with all other categories in both summer and winter. Conversely, Ulva from exposed rural sites had the lowest range of δ15N values compared with any other category (6.7 ± 0.1 to 8.8 ± 0.1 ‰) and showed no seasonal change in mean values (7.8 ‰ and 7.6 ‰ for summer and winter, respectively). In addition, δ15N values in Ulva were the only N-index that showed a significant difference between urban and rural categories. To test the relationship between inorganic nitrogen concentration in seawater and the responses of biochemical nitrogen indices in Ulva pertusa, several experiments were conducted in an outdoor, flow-through culture apparatus, in summer and winter. In this apparatus effects of ammonium concentration, nitrogen source (nitrate and ammonium), light and seawater motion were investigated. Of the same three N-indices examined in natural Ulva populations (free amino acids, chlorophyll and total tissue nitrogen), increases in free amino acids, particularly asparagine, provided the strongest indicator of increases in nitrogen availability. In addition, while tissue nitrogen and chlorophyll also increased with seawater nitrogen concentration, it was apparent that these indices were also strongly influenced by light, and probably season. Rates of ammonium assimilation provided no overall measure of the availability of nitrogen in seawater and were clearly affected by season. Similarly, growth rates in Ulva only showed a response to nitrogen addition in summer months. Stable isotopes of nitrogen (δ15N) in Ulva provided a clear distinction between natural and synthetic nitrogen sources, but more importantly, showed only minor fractionation (ranging from 1.3 ‰ to -1.9 ‰) of 15N supplied from synthetic nitrate and ammonium under both light-saturating and light-limiting conditions. To further develop Ulva as a standardized test-organism it was cultured in low-nutrient (non-polluted) seawater to deplete internal storage pools of nitrogen. Each month the resulting test-Ulva was then placed in surface-moored growth enclosures at a range of coastal sites around Auckland and then monitored for one year. In winter there were increases in seawater inorganic nitrogen concentrations and concomitant increases in free amino acid content. However, tissue nitrogen and chlorophyll content in test-Ulva showed similar increases (possibly saturating) across all sites suggesting that seasonal increases in these N-indices were also due to other seasonal factors (e.g., surface irradiance and / or seawater temperature). On the other hand, the total free amino acid pool showed strong differences between a low-nitrogen reference site and the other study sites all year round. It was probable that test-Ulva was integrating differences in tidally-averaged nitrogen loading that were not reliably detected in instantaneous seawater samples. In addition to N-indices in test-Ulva, levels of tissue heavy metals and stable isotopes of nitrogen showed strong differences with higher values of both typically found in urban environments compared with values found in non-polluted reference sites. It is concluded that several abiotic and biotic factors affect nitrogen status in Ulva, but the average nitrogen concentration in seawater, and the physical factors of temperature, light and water motion, appear to be the overarching determinants. It is further suggested that in combination with Ulva tissue δ15N values, tissue nitrogen and the free amino acid pool, as quantitative biochemical measures of nitrogen availability, are likely to provide useful information on both the amount and composition of nitrogen entering coastal environments. / Foundation for Research, Science and Technology. Auckland Regional Council.

O Brasil é um dos maiores produtores mundiais de suco de laranja, da mesma forma que a produção é elevada, a geração de resíduos também é significativa. Sabe-se que estes resíduos, os quais incluem sementes, cascas e restos de polpa são ricos em nutrientes que poderiam ser utilizados como substrato por micro-organismos, seja para o crescimento ou para a obtenção de subprodutos. Esporos de Bacillus atrophaeus ATCC 9372 são utilizados como indicadores biológicos, IBs, em processos térmicos por formarem esporos termorresistentes. O objetivo deste trabalho foi avaliar o uso de resíduos do processamento de suco de laranja como um meio de cultura alternativo para obtenção de esporos de B. atrophaeus, para serem aplicados em processos industriais. Ao bagaço de laranja (de 1,0 g a 20,0 g), obtido por processamento em centrífuga de frutas, foram adicionados 100 mL de água, e incubados a 150 rpm / 37 ºC por até 6 dias. Evidenciada a viabilidade de crescimento celular (µmáx = 0,0238 h-1 e Px = 0,0787 g/L.h, para 5,0 g de bagaço) procedeu-se ao estudo de planejamento experimental fatorial 22 em formato estrela com 6 pontos centrais, considerando a concentração de bagaço e o volume de meio. Foram determinados os valores de pH, de biomassa, de esporos viáveis e a resistência térmica dos mesmos a 102 ºC. Observou-se que houve aumento nos valores de pH após o cultivo e que as maiores concentrações de esporos foram de 1,73 x 109 esporos /mL e 5,75 x 109 esporos /mL após 3 e 6 dias de cultivo e os tempos de redução decimal determinados variaram de D102C = 0,92 min a D102C = 2,71 min e de D102C = 1,34 min a D102C = 3,98 min após 3 e 6 dias de cultivo, respectivamente. Com base no planejamento proposto e a análise de regressão, o desenvolvimento de esporos em bagaço segue a relação: Esporos = {-1,15 + 0,0303* [bagaço (g)] - 0,00611* [volume (mL)] + 0,611* [tempo (dias)]}, p=0,000, R2 =0,452, sendo o tempo (p=0,000) o fator de maior influência na formação de esporos. Os meios preparados com bagaço de laranja apresentaram-se viáveis para a produção de esporos de B. atrophaeus termorresistentes, produto de interesse farmacêutico e industrial, agregando valor ao resíduo que seria descartado. / Brazil is one of the world´s largest producers of oranges juice, in the same way that the production is high the amount of generated waste is also significant. It is well known that these residues, which include seeds, peel and pulp, are rich in nutrients that could be used as substrate by microorganisms whether for growth or for obtaining by-products. Bacillus atrophaeus ATCC 9372 spores are used as biological indicators, BIs, in thermal processes due to their ability to form heat-resistant spores. This study aimed to evaluate the use of orange juice processing waste as an alternative culture media to obtain B. atrophaeus spores, to be applied in industrial processes. To orange\'s bagasse (from 1.0 g to 20.0 g), obtained by processing in a fruit\'s centrifuge, 100 mL of water was added, and sterilized at 121 ºC. An aliquot of 0.1g/L of Bacillus atrophaeus spores was inoculated to bagasses\'s media and incubated at 150 rpm / 37 ºC up to 6 days. As cells (µmáx = 0.0238 h-1 and Px = 0.0787 g/L.h, for 5.0 g of bagasse) were obtained, a factorial experimental design 22, with star-shaped model and 6 central points, was performed considering the bagasse concentration and the media volume used. Values of pH, biomass, viable spores and their thermal resistance at 102 ºC were determined. It was observed that pH increased after cultivation and major values of spore concentration achieved were 1.73 x 109 spores /mL and 5.75 x 109 spores /mL after 3 and 6 days, respectively. Decimal reduction times determined ranged from D102C = 0.92 min to D102C = 2.71 min and from D102C = 1.34 min to D102C = 3.98 min after 3 and 6 days of incubation, correspondingly. The regression analysis showed that the development of spores in bagasse can be defined by the equation: Spores = , p=0.000, R2 =0.452 and time has a positive influence in the spore formation. Results demonstrated media prepared with oranges\' bagasse were capable to grow and to develop B. atrophaeus heat-resistant spores, being an alternative to add value to a waste that would be discarded, generating a product of great importance in the pharmaceutical field.

A Proteína Verde Fluorescente recombinante, GFPuv, é um sistema marcador atrativo pois, sua presença pode ser visualizada através da intensidade de fluorescência emitida, sem o uso de substratos ou meios complexos. Sendo uma molécula estável à presença de substâncias orgânicas, temperaturas acima de 70°C e ampla faixa de pH, é um potencial Indicador Biológico (IH) para diversas aplicações. A estabilidade térmica da GFPuv, foi avaliada pela medida da perda de intensidade de fluorescência, expressa em valores D (min), tempo de exposição necessário para redução de 90% da intensidade de fluorescência inicial da GFPuv. GFPuv (3,5-9,0 µg/mL), expressa por E. coli e isolada por extração de Partição em Três Fases (TPP) e purificação por Cromatografia de Interação Hidrofóbica (IDC), foi diluída nas soluções parenterais preparadas em tampão (10 mM cada: Tris-EDTA, pH 8; Fosfato, pH 6 e 7, e Acetato, pH 5) e em água para injeção, WFI; pH = 6,70±0,40), e expostas a temperaturas de 25°C e ao intervalo entre 80°C e 100°C. A 95°C, os valores D para a GFPuv em soluções de 1,5% a 50% de glicose variaram de: (i) 1,63 (±0,23) min em acetato pH 5; (ii) 2,64 ± 0,26 min em WFI; (iii) 2,50 ± 0,18 min em fosfato pH 6; (iv) 3,24 ± 0,28 min em fosfato pH 7 e, (v) 2,89 ± 0,44 min em Tris-EDTA pH 8. Cloreto de sódio associado aos tampões proporcionou influência positiva na estabilidade da GFPuv, sendo que em soluções de Tris-EDTA, a adição de 15-20% de NaCl dobrou a estabilidade térmica da GFPuv (valores D de 65,79 min e 18,12 min a 80 °C e 85°C) em relação à solução sem cloreto de sódio. Nos processos de esterilização por óxido de etileno (45°C-60°C), a GFPuv pode ser utilizada como IB para monitorar a distribuição de gás dentro da câmara, pois, apresentou variação na concentração remanescente de até 80%, após processamento, estabelecendo áreas distintas dentro da câmara. No tratamento em autoclave, a GFPuv em solução apresentou resistência térmica em solução de fosfato pH 7,0 (valor F = 2,53 min (± 0,12)). Quando expressa por esporos de Bacillus subtilis, a intensidade de fluorescência emitida por esporos sobreviventes se manteve. A estabilidade térmica da GFPuv atestou sua potencialidade como indicador biológico fluorescente da garantia da eficácia de tratamento de soluções e materiais expostos ao calor. / The recombinant Green Fluorescent Protein, GFPuv is an attractive system marker due to its ability to emit fluorescence when exposed to ultraviolet light, without use of substrates or complex environment. Being a stable molecule even in the presence of organic substances, temperatures above 70°C and wide range of pH, it is a potential Biological Indicator, BI, for many applications, including thermal processes. GFPuv thermal stability was evaluated by the loss of fluorescence intensity expressed in decimal reduction time (D-value, min), the exposure time required to reduce 90% of the GFPuv initial fluorescence intensity. GFPuv (3.5-9.0 µg/mL), expressed by E. coli and isolated by Three Phases Partitioning, TPP extraction with Hidrophobic Interaction Chromatography, HIC, was diluted in buffered solutions (each 10 mM: Tris-EDTA, pH 8; phosphate, pH 6 and 7, and acetate, pH 5) and in water for injection, WFI; pH = 6.70 (± 0.40), and exposed to temperatures of 25°C and between 80°C and 95°C. At 95°C, the D-value for GFPuv in 1.5%-50% glucose, ranged from: (i) 1.63 ± 0.23 min in acetate pH 5; (ii) 2.64 ± 0.26 min in WFI; (iii) 2.50 ± 0.18 min in phosphate, pH 6; (iv) 3.24 ± 0.28 min in phosphate, pH 7, (v) 2.89 ± 0.44 min in Tris-EDTA, pH 8. Sodium cloride provided a positive influence over GFPuv stability. In Tris-EDTA solutions, the addition of 15% and 20% of NaCl doubled the thermal stability of GFPuv (D = 65.79 min and D = 18.12 min at 80°C, and 85°C, respectively, in relation to the solutions without NaCl. For ethylene oxide sterilization processes (45°C-60°C), GFPuv can be used as biological indicator to monitor gas distribution into the chamber. After processing, the protein concentration varied by 80%, showing distinct areas into the chamber. In autoclave, GFPuv in solution showed thermal resistance in phosphate pH 7.0 solution (F-value = 2.53 (± 0.12) min. When expressed by Bacillus subtilis spores, the fluorescence intensity was kept constant after thermal processing. The thermal stability of GFPuv provides the basis for its potential utility as a fluorescent biological indicator to assess the efficacy of the treatment of liquids and materials exposed to steam.

A Proteína Verde Fluorescente recombinante, GFPuv, é um sistema marcador atrativo pois, sua presença pode ser visualizada através da intensidade de fluorescência emitida, sem o uso de substratos ou meios complexos. Sendo uma molécula estável à presença de substâncias orgânicas, temperaturas acima de 70°C e ampla faixa de pH, é um potencial Indicador Biológico (IH) para diversas aplicações. A estabilidade térmica da GFPuv, foi avaliada pela medida da perda de intensidade de fluorescência, expressa em valores D (min), tempo de exposição necessário para redução de 90% da intensidade de fluorescência inicial da GFPuv. GFPuv (3,5-9,0 µg/mL), expressa por E. coli e isolada por extração de Partição em Três Fases (TPP) e purificação por Cromatografia de Interação Hidrofóbica (IDC), foi diluída nas soluções parenterais preparadas em tampão (10 mM cada: Tris-EDTA, pH 8; Fosfato, pH 6 e 7, e Acetato, pH 5) e em água para injeção, WFI; pH = 6,70±0,40), e expostas a temperaturas de 25°C e ao intervalo entre 80°C e 100°C. A 95°C, os valores D para a GFPuv em soluções de 1,5% a 50% de glicose variaram de: (i) 1,63 (±0,23) min em acetato pH 5; (ii) 2,64 ± 0,26 min em WFI; (iii) 2,50 ± 0,18 min em fosfato pH 6; (iv) 3,24 ± 0,28 min em fosfato pH 7 e, (v) 2,89 ± 0,44 min em Tris-EDTA pH 8. Cloreto de sódio associado aos tampões proporcionou influência positiva na estabilidade da GFPuv, sendo que em soluções de Tris-EDTA, a adição de 15-20% de NaCl dobrou a estabilidade térmica da GFPuv (valores D de 65,79 min e 18,12 min a 80 °C e 85°C) em relação à solução sem cloreto de sódio. Nos processos de esterilização por óxido de etileno (45°C-60°C), a GFPuv pode ser utilizada como IB para monitorar a distribuição de gás dentro da câmara, pois, apresentou variação na concentração remanescente de até 80%, após processamento, estabelecendo áreas distintas dentro da câmara. No tratamento em autoclave, a GFPuv em solução apresentou resistência térmica em solução de fosfato pH 7,0 (valor F = 2,53 min (± 0,12)). Quando expressa por esporos de Bacillus subtilis, a intensidade de fluorescência emitida por esporos sobreviventes se manteve. A estabilidade térmica da GFPuv atestou sua potencialidade como indicador biológico fluorescente da garantia da eficácia de tratamento de soluções e materiais expostos ao calor. / The recombinant Green Fluorescent Protein, GFPuv is an attractive system marker due to its ability to emit fluorescence when exposed to ultraviolet light, without use of substrates or complex environment. Being a stable molecule even in the presence of organic substances, temperatures above 70°C and wide range of pH, it is a potential Biological Indicator, BI, for many applications, including thermal processes. GFPuv thermal stability was evaluated by the loss of fluorescence intensity expressed in decimal reduction time (D-value, min), the exposure time required to reduce 90% of the GFPuv initial fluorescence intensity. GFPuv (3.5-9.0 µg/mL), expressed by E. coli and isolated by Three Phases Partitioning, TPP extraction with Hidrophobic Interaction Chromatography, HIC, was diluted in buffered solutions (each 10 mM: Tris-EDTA, pH 8; phosphate, pH 6 and 7, and acetate, pH 5) and in water for injection, WFI; pH = 6.70 (± 0.40), and exposed to temperatures of 25°C and between 80°C and 95°C. At 95°C, the D-value for GFPuv in 1.5%-50% glucose, ranged from: (i) 1.63 ± 0.23 min in acetate pH 5; (ii) 2.64 ± 0.26 min in WFI; (iii) 2.50 ± 0.18 min in phosphate, pH 6; (iv) 3.24 ± 0.28 min in phosphate, pH 7, (v) 2.89 ± 0.44 min in Tris-EDTA, pH 8. Sodium cloride provided a positive influence over GFPuv stability. In Tris-EDTA solutions, the addition of 15% and 20% of NaCl doubled the thermal stability of GFPuv (D = 65.79 min and D = 18.12 min at 80°C, and 85°C, respectively, in relation to the solutions without NaCl. For ethylene oxide sterilization processes (45°C-60°C), GFPuv can be used as biological indicator to monitor gas distribution into the chamber. After processing, the protein concentration varied by 80%, showing distinct areas into the chamber. In autoclave, GFPuv in solution showed thermal resistance in phosphate pH 7.0 solution (F-value = 2.53 (± 0.12) min. When expressed by Bacillus subtilis spores, the fluorescence intensity was kept constant after thermal processing. The thermal stability of GFPuv provides the basis for its potential utility as a fluorescent biological indicator to assess the efficacy of the treatment of liquids and materials exposed to steam.