56 resultados para Vitaceae
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The aim of this work was to develop an isotopic analysis method to quantify the carbon of C3 photosynthesis cycle in grape nectar and to identify the commercial beverages in disagreement to the Brazilian Ministry of Agriculture, Livestock and Food Supply (MAPA) regulation. The nectars were produced in a laboratory, according to the Brazilian Law. Adulterated beverages with quantity of grape juice lower than the legal limit were also produced. Isotopic analysis measured the relative isotopic enrichment of grape nectar and its purified sugar fraction. Based on these results, it was possible to estimated the quantity of source C3 by means of isotopic dilution equation. To determine the existence of adulteration in commercial nectars, it was necessary to create a legal limit according to the Brazilian Law. One of the twelve commercial brands of nectar analyzed was classified as adulterated. The developed methodology proved to be efficient to quantify the carbon of C3 origin and identify the adulterated commercial grape nectar.
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A total of 24 extracts from 14 plant species collected at the state of Minas Gerais, Brazil, and belonging to five botanical families (Annonaceae, Apocynaceae, Ochnaceae, Polygonaceae and Vitaceae) was screened for cytotoxicity in cultured Vero cells and for antiviral activity against human herpes virus type 1 (HSV-1), vaccinia virus (VACV) and murine encephalomyocarditis virus (EMCV). The highest cytotoxicity (CC 50 < 10 μg/mL) was observed for the ethanol extracts from Annona coriacea fruits and seeds. Extracts from Hancornia speciosa, Ouratea castaneafolia and O. semisrrata were the only ones that have shown activity against all the three viruses assayed. Extracts from Polygonum spectabile, Hancornia speciosa, Himatanthus phagedaenica, Ouratea spectabilis and O. semiserrata were the most active against HSV-1 (EC 50 < 50 mg/mL), with favorable SI values (8.0 to 10.0). Hancornia speciosa and Anaxagorea dolichocarpa were the most active against EMCV (EC 50 50 - 100 μg/mL), with reasonable SI values (5.2 to 6.1), while moderate to low activity (EC 50 > 100 μg/mL) was observed for Ouratea spectabilis and O. semiserrata. A total of 7 plant species, Ouratea semiserrata, O. spectabilis, O. castanaeafolia, Rollinia laurifolia, Cissus erosa, Polygonum spectabile, and Hancornia speciosa, were active against VACV, disclosing EC50 < 50 μg/mL and SI values ranging from 6.6 to 67.3. In total, 10 out of the 14 species were selected from a literature survey on plants used to treat viral diseases in Brazil; these species were responsible for 70% of the positive results.
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Microbial β-glucosidases have been used for the enhancement of wine aroma. Nevertheless, few enzymes are active in the conditions of winemaking. In this work, the production of a β-glucosidase by an Aureobasidium pullulans strain (Ap-β-gl) isolated from grape ecosystems was evaluated. The maximum enzymatic synthesis using submerged fermentation was after 96 h of growth in complex media containing 20 g/L of cellobiose as the sole carbon source. The crude enzyme (Ap-β-gl) showed optimal pH at 5.5 and two peaks of optimum temperature (at 45 and 70 C). It showed a wide range of pH stability, stability at low temperatures, and tolerance to ethanol, showing suitable characteristics for winemaking conditions. The hydrolysis of glycosidic terpenes by Ap-β-gl was studied, and its ability to efficiently release free terpenols was demonstrated by gas chromatography/mass spectrometry. The enzymatic treatment notably increased the amount of monoterpenes, showing good prospects for its potential application for the development of aroma in wines. © 2012 Springer Science+Business Media New York.
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Saccharomyces and non-Saccharomyces yeast species from a winery located in Brazil were identified by ribosomal gene-sequencing analysis. A total of 130 yeast strains were isolated from grape surfaces and musts during alcoholic fermentation from Isabel, Bordeaux, and Cabernet Sauvignon varieties. Samples were submitted to PCR-RFLP analysis and genomic sequencing. Thirteen species were identified: Candida quercitrusa, Candida stellata, Cryptococcus flavescens, Cryptococcus laurentii, Hanseniaspora uvarum, Issatchenkia occidentalis, Issatchenkia orientalis, Issatchenkia terricola, Pichia kluyveri, Pichia guilliermondii, Pichia sp., Saccharomyces cerevisiae, and Sporidiobolus pararoseus. A sequential substitution of species during the different stages of fermentation, with a dominance of non-Saccharomyces yeasts at the beginning, and a successive replacement of species by S. cerevisiae strains at the final steps were observed. This is the first report about the yeast distribution present throughout the alcoholic fermentation in a Brazilian winery, providing supportive information for future studies on their contribution to wine quality. © 2013 Springer Science+Business Media New York.
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The objective of this study was to evaluate the association between the physicochemical properties and sensory acceptance of Brazilian red wines by applying chemometric techniques. Therefore, three winemaking processes were carried out: a traditional winemaking process and two novel winemaking processes, pre-drying and static pomace. Significant differences could be identified amongst the physicochemical properties of the wines (P<0.001). The sensory results showed greater acceptance of the wines made after pre-drying of the grapes or from the static pomace, as compared to commercial brands. Cluster analysis and Multidimensional Scaling were successfully applied and their results demonstrated the influence of the total phenolic content and color indexes on acceptance of the appearance of the wines. The odor was associated with the alcohol content, acidity, dry extract, total and reducing sugars and the body of the wines. The flavor was associated with several physicochemical properties which influenced the overall acceptance of the samples. © 2013 Elsevier Ltd.
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Pós-graduação em Ciências Farmacêuticas - FCFAR
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Cissus verticillata, a Vitaceae very used in the traditional medicine in Pará and Minas Gerais State – Brazil, was investigated in order to validate its indication for the hyperglycaemia control. The aqueous extract reduces the normal glycaemia of male white Wistar rats in about 19.5 %. The hypoglycaemic effect of this extract could be related to the flavonoids found in the preparation. Luteolin, Kaempferol and Luteolin-3'-sulphate could be isolated from the aqueous extract after acid hydrolysis. Cissus
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Pós-graduação em Ciências Biológicas (Farmacologia) - IBB
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The objective was to analyse population structure and to determine genetic diversity of Erysiphe necator (syn. Uncinula necator) populations obtained from some vineyards located in the South-East Po valley (Italy). Powdery mildew is one of the most important fungal diseases of grapes (Vitis vinifera L.) throughout the world. The causal agent is the haploid, heterothallic ascomycete E. necator. It is an obligate biotrophic fungus and it can be found only on green organs of plants belonging to the family Vitaceae. For this pathogen, two sympatric populations (groups A and B) have been described in Europe and Australia. The two genetic groups differ at multiple genetic loci and previous studies reported a lack of interfertility among isolates of the two groups. There are now several well documented examples of plant pathogen species, such as Leptosphaeria maculans, Gaeumannomyces graminis var. tritici, Botrytis cinerea and Erysiphe syringae, which are indeed composed of genetically differentiated clades, that have led to the description of new groups or even new species. Several studies have suggested that genetic E. necator group A and B correlated with ecological features of the pathogen; some researchers proposed that group A isolates over-winter as resting mycelium within dormant buds, and in spring originate infected shoots, known as Flag shoots, while group B isolates would survive as ascospores in overwintering cleistothecia. However, the association between genetic groups and mode of over-wintering has been challenged by recent studies reporting that flag-shoot may be originated indifferently by group A or group B isolate. Previous studies observed a strong association between the levels of disease severity at the end of the growing season and the initial compositions of E. necator populations in commercial vineyards. The frequencies of E. necator genetic groups vary considerably among vineyards, and the two groups may coexist in the same vineyard. This finding suggests that we need more information on the genetics and epidemiology of E. necator for optimize the crop management In this study we monitored E. necator populations in different vineyards in Emilia – Romagna region (Italy), where the pathogen overwinters both as flagshoots and as cleistothecia. During the grape growing season, symptomatic leaves were sampled early in the growing season and both leaves and berries later during the epidemic growth of the disease. From each sample, single-conidial isolate was obtained. Each isolates was grown on V. vinifera leaf cv. Primitivo and after harvesting the mycelium, the DNA was purified and used as template for PCR amplification with SCAR primers (Sequences Characterised Amplified Region ), -tubulin, IGS sequences and Microsatellite markers (SSR). Amplified DNA from b-tubulin and IGS loci was digested with AciI and XhoI restriction enzymes, respectively, to show single-nucleotide polymorphisms specific for the two genetic groups. The results obtained indicated that SCAR primers are not useful to study the epidemiology. of E. necator conversely the b-tubulin IGS sequences and SSR. Summarize the results obtained with b-tubulin, IGS sequences, in treated vineyards we have found individuals of group B along all grape growing season, whereas in the untreated vineyard individuals of the two genetic groups A and B coexisted throughout the season, with no significant change of their frequency. DNA amplified from ascospores of single cleistothecia showed the presence of markers diagnostic for either groups A and B and were seldom observed also the coexistence of both groups within a claistothecium. These results indicate that individuals of the two groups mated in nature and were able to produced ascospores. With SSR we showed the possibility of recombination between A and B groups in field isolates. During winter, cleistothecia were collected repeatedly in the same vineyards sampling leaves fallen on ground, exfoliating bark from trunks, and from soil. From each substrate, was assess the percentage of cleistothecia containing viable ascospores. Our results confirmed that cleisthotecia contained viable ascospores, therefore they have the potential to be an additional and important source of primary inoculum in Emilia-Romagna vineyards.
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1. Polleninventar: Erstmals wurde der Sporomorpheninhalt der Süssbrackwassermolasse und der Oberen Süsswassermolasse Südbayerns einer umfassenden Sichtung unterzogen. Von den überprüften 92 Fundstellen erwiesen sich 55 als sporomorphenführend. Nur 15 davon waren so ergiebig, daß ihr Inhalt quantitativ erfaßt und als Grundlage für die Erstellung eines Diagramms herangezogen werden konnte. Dennoch weist der systematische Katalog 272 Formen auf. Dies ist eine im Vergleich mit anderen, in neuerer Zeit bearbeiteten neogenen Pollenfloren Mitteleuropas sehr große Zahl, wie folgende Angaben belegen: Niederrheinische Braunkohle 175 Arten, Braunkohle der Oberpfalz 138 Arten, subalpine Flözmolasse Bayerns 93 Arten und subalpine Molasse der Ostschweiz und der zentralen und westlichen Paratethys 219 Arten. Dieser Reichtum erklärt sich unschwer aus der Größe des Untersuchungsgebietes, das vom Allgäu im Westen bis an die Salzach im Osten reichte. Überwiegend gehören die nachgewiesenen Formen gutbekannten Arten bzw. Formenkreisen an. Deshalb wurde lediglich die Aufstellung von 2 neuen Gattungen, 19 neuen Arten sowie 5 Neukombinationen nötig. Neue Genera: Nr. (165) Ludwigiapollis Nr., (248) Caesalpiniaceaepollenites, 311 Neue Spezies: (039) Polypodiaceoisporltes subtriangularis, (046) P. pityogrammoides, (067) Perinomonoletes imperfectus, (124) Cycadopltes gemmatus, (125) C. concinus, (133) Lillacidites tener, (137) Nupharipollenites microechinatus, (150) Polyporopollenites nanus, (161) Porocolpopollenites subrotundus, (165) Ludwigiapollis labiatus, (169) Sporotrapoidites cucculatus, (190) Tricolpopollenites cribosus, (192) T. variabilis, (204) Tricolporopollenites pulcher, (210) T. operculiferus, (213) T. pseudomarcodurensis, (217) T. magnolaevigatus, (245) Umbelliferaepollenites achldorfensis, (248) Caesalpiniaceaepollenites antiquus Neukombinationen: (081) Pityosporites koraensis, (128) Magnoliaepollenites magnolioides, (130) M. graciliexinus, (168) Sporotrapoidites erdtmannii, (177) Chenopodipollis psilatoides. Für die meisten der vorgefundenen Sporomorphen sind die Lieferpflanzen bereits bekannt. Dennoch gingen parallel zur Bestimmung, d.h. der Zuordnung der Funde zu Gruppen des morphographischen Sporomorphensystems, die Bemühungen auch dahin, solche Lieferpflanzen, v.a. der selteneren oder neu gefundenen Sporomorphen, zu ermitteln; einige der neuen Arten sind in ihrer Verwandtschaft eindeutig, was durch die Benennung zum Ausdruck gebracht wird (s.o). Für die Mehrzahl der neuen Spezies und für viele bisher in ihrer Verwandtschaft unklare Formen ließ sich die botanische Deutung zumindest eingrenzen. Dies gelang für 148 Formen. Es handelt sich dabei teils um subtropisch-tropische Gewächse, teils aber auch um Pflanzen gemäßigter Klimata. Für genaue Zuweisungen sind jedoch umfangreiche Rezentvergleiche nötig, die einer eigenen Bearbeitung vorbehalten bleiben müssen. Auch einige als Sammelgruppen behandelte Formenkreise erfordern für eine Aufgliederung detailliertere Untersuchungen als sie in diesem Rahmen durchführbar waren. (z. B. Tricolpopollenites asper, T. sp. 2 u.a.). Andere Formen und Gattungen wiederum erwiesen sich dagegen als viel zahlreicher und leichter differenzierbar als bisher angenommen (z. B. Pinaceen, Magnoliaceen, Cyperaceen). In diesem Zusamenhang ist auch zu erwähnen, daß von Hemitrapa zwei Arten mit offensichtlich stratigraphischer Aussagekraft unterscheidbar sind; die Interpretation von Tricolporopol1enltes wackersdorfensis sensu MOHR & GREGOR (1984) als Gleditsia muß nach vorliegenden Erkenntnissen dagegen in Frage gestellt werden. Für 36 Formspezies blieb die Lieferpflanze völlig unbekannt oder es lassen sich höchstens vage Vermutungen anstellen. 2. Biostratigraphie: Fragen der Brauchbarkeit von Mikrofloren für die stratgraphische Gliederung der jüngsten Molassesedimente Südbayerns bildeten den zweiten Schwerpunkt vorliegender Bearbeitung. a) Reichweite: Die Fülle des gefundenen Sporomorphenmaterials brachte es mit sich, daß bei etlichen Formen eine weitere stratigraphische Reichweite als bisher angenommen festgestellt wurde. Zum Teil wurde diese Revision durch die Neugliederung des Paratethys-Miozäns nötig. b) Palynologische Gliederung: Im Laufe der Untersuchungen zeigte sich bald, daß allein auf der Basis der mikrofloristischen Bearbeitung kein von anderen Fossilresten unabhängiges stratigraphisches Gliederungsschema zu finden war. Weder die von anderen Autoren favoritisierte Leitformen-Methode, noch die Aufgliederung nach Klimaelementen ergab ein brauchbares Bild. Lediglich die bekannte generelle Abnahme der miozänen, paläotropischen und thermophilen Elemente und die Zunahme der pliozänen, arktoteriären und gemäßigten während des Neogens ließ sich deutlich ausmachen. Dagegen ermöglicht die Berücksichtigung des Sporomorpheninhalts eine Ergänzung und Deutung der vertebrat-stratigraphisch ausgeschiedenen Abfolgen. Voraussetzung ist die Möglichkeit einer Zuordnung zu einer natürlichen Art, Gattung oder wenigstens Familie und daraus ableitbar wiederum die Zuordnung zu einer oder mehreren Pflanzengesellschaften. Aufgeteilt nach Diversität, Dominanz und Verhältnis von 'Feuchtpflanzen' bzw. autochthonen Gemeinschaften zu mesophilen Phanerophyten bzw. allochthonen Gemeinschaften lassen sich in Südbayern fünf Pollenbilder erkennen, die mit den MN-Einheiten der Zoostratigraphie in Beziehung gebracht werden können. Die Pollenbilder 1 und 2, ungefähr entsprechend den Säugereinheiten 4b und 5, dokumentieren gattungsreiche, polydominante Mikrofloren, deren Lieferpflanzen vor allem verschiedenen Naß- und Feuchtgesellschaften angehören. Dementprechend sind Pteridaceen, Schizaeaceen, Cyperaceen und Poaceen relativ häufig. Das Pollenbild 1 (Langenau und Rauscheröd) zeichnet sich durch eine gewisse Artenarmut aus, wohingegen im Pollenbild 2 (Hitzhofen und Rittsteig) die Diversität zunimmt und Palmenpollen neben anderen mesophilen Akzessorien eine merkliche Rolle spielt. Bemerkenswert ist in den Entnahmeprofilen das Vorkommen kohliger Sedimente. Bezeichnend für Sporomorphenbild 3 sind oligodominante Mikrofloren, zusammengesetzt aus Elementen artenarmer Au- und Sumpfwälder (Taxodiaceen, Cyperaceen) sowie mesophiler 'Pionierwälder' (Pinaceen, Leguminosen). Fehlende Kohlebildung und das Zurücktreten mesophiler, d. h. allochthoner Lieferpflanzen sind weitere Charakteristika. Dieses Sporomorphenbild mit den Fundpunkten Gallenbach und Unterneul enspricht ungefähr der Säugereinheit MN 6. Die beiden stratigraphisch jüngsten Pollendiagramme 4 und 5 setzen sich deutlich von dem vorhergehenden ab. Belegt sind nun wiederum gattungsreiche, polydominante Pflanzenge seIl schaften feuchter, aber nicht nasser Biotope, in denen es ebenfalls mancherorts zur Kohlebildung kam. Gegenüber den Sporomorphenbildern und 2 ist der Anteil mesophiler Lieferpflanzen deutlich erhöht auf Kosten der Feuchtelemente. Letzteres gilt vor allem für das Sporomorphenbild 5 (Leonberg), in dem Fagaceen Pollen (Quercus, Fagus) vorherrscht. sporomorphenbild 4 entspricht annähernd MN 8 mit den Fundpunkten Hassenhausen und Achldorf, während Leonberg, nahe Marktl gelegen, MN 9 zugehört. Auf dem Umweg über diese an der Säugetierstratigraphie 'geeichten' Mikrofloren gelingt es, stratigraphisch unsichere Fundpunkte, wenn sie nur genügend formen- und individuenreich sind (Burtenbach, Lerchenberg, Wemding), einzuordnen. Auf diese Weise ergibt sich die in Diagramm 10 dargestellte Reihung vom Liegenden zum Hangenden. Dürftige Sporomorphenfloren oder Floren, die ausschließlich autochthone Feuchtelemente zeigen, können pollenstratigraphisch nicht sicher angesprochen werden, weil ihr Pollendiagramm undeutlich bleiben muß. Entsprechend der anerkannten Unterstellung, daß Phytostratigraphie zugleich Klimastratigraphie ist, läßt die dargestellte, im Grunde auf der Ausscheidung verschiedener Ukotypen basierende Gliederung sich auch paläoklimatisch interpretieren: Danach ist das verarmte Sporomorphenbild 3 in Südbayern als Ausdruck des vegetationsgeschichtlichen Pessimums anzusehen. Da die nachgewiesenen Sippen noch höhere Wärmeansprüche besitzen, ist nicht ein Temperaturrückgang, sondern ein Absinken der Niederschlagsmenge als begrenzender Faktor am wahrscheinlichsten und auf diese Weise das Ausbleiben von Pollen mesophiler Phanerophyten des Hinterlandes einleuchtend. 3. Paläogeographie: Bei dem Versuch, mit benachbarten Gebieten stratigraphische Beziehungen herzustellen, ergab sich, daß dies zwar über eine kürzere Entfernung recht gut gelingt, daß aber vor allem zu den Mikrofloren der niederrheinischen Braunkohle ein signifikanter Unterschied besteht: In Süddeutschland lassen die Pollendiagramme auf eine raschere Veränderung in der Zusammensetzung der Wälder schließen. Mit anderen Worten: altersgleiche Mikrofloren in Nordwestdeutschland täuschen ein höheres Alter vor. Erst im Obersarmat ähneln sich die jeweiligen Sporomorphenbilder. Damit erklärt sich auch, daß frühere Bearbeiter Schwierigkeiten hatten, mikrofloristische Befunde aus Süd- und Nordwestdeutschland miteinander zu korrelieren. Als Ursache für dieses überraschende Phänomen einer mittelmiozänen Diagrammverschiebung wird die stärkere, sprich länger andauernde maritime Beeinflussung des Niederrheingebietes angesehen.
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Pollen analyses have been proven to possess the possibility to decipher rapid vegetational and climate shifts in Neogene sedimentary records. Herein, a c. 21-kyr-long transgression-regression cycle from the Lower Austrian locality Stetten is analysed in detail to evaluate climatic benchmarks for the early phase of the Middle Miocene Climate Optimum and to estimate the pace of environmental change. Based on the Coexistence Approach, a very clear signal of seasonality can be reconstructed. A warm and wet summer season with c. 204-236 mm precipitation during the wettest month was opposed by a rather dry winter season with precipitation of c. 9-24 mm during the driest month. The mean annual temperature ranged between 15.7 and 20.8 °C, with about 9.6-13.3 °C during the cold season and 24.7-27.9 °C during the warmest month. In contrast, today's climate of this area, with an annual temperature of 9.8 °C and 660 mm rainfall, is characterized by the winter season (mean temperature: -1.4 °C, mean precipitation: 39 mm) and a summer mean temperature of 19.9 °C (mean precipitation: 84 mm). Different modes of environmental shifts shaped the composition of the vegetation. Within few millennia, marshes and salt marshes with abundant Cyperaceae rapidly graded into Taxodiaceae swamps. This quick but gradual process was interrupted by swift marine ingressions which took place on a decadal to centennial scale. The transgression is accompanied by blooms of dinoflagellates and of the green alga Prasinophyta and an increase in Abies and Picea. Afterwards, the retreat of the sea and the progradation of estuarine and wetland settings were a gradual progress again. Despite a clear sedimentological cyclicity, which is related to the 21-kyr precessional forcing, the climate data show little variation. This missing pattern might be due to the buffering of the precessional-related climate signal by the subtropical vegetation. Another explanation could be the method-inherent broad range of climate-parameter estimates that could cover small scale climatic changes.
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Palynological analyses were performed on 53 surface sediment samples from the North Pacific Ocean, including the Bering and Okhotsk Seas (37-64°N, 144°E-148°W), in order to document the relationships between the dinocyst distribution and sea-surface conditions (temperatures, salinities, primary productivity and sea-ice cover). Samples are characterized by concentrations ranging from 18 to 143816 cysts/cm**3 and the occurrence of 32 species. A canonical correspondence analysis (CCA) was carried out to determine the relationship between environmental variables and the distribution of dinocyst taxa. The first and second axes represent, respectively, 47% and 17.8% of the canonical variance. Axis 1 is positively correlated with all parameters except to the sea-ice and primary productivity in August, which are on the negative side. Results indicate that the composition of dinocyst assemblages is mostly controlled by temperature and that all environmental variables are correlated together. The CCA distinguishes 3 groups of dinocysts: the heterotrophic taxa, the genera Impagidinium and Spiniferites as well as the cyst of Pentapharsodinium dalei and Operculodinium centrocarpum. Five assemblage zones can be distinguished: 1) the Okhotsk Sea zone, which is associated to temperate and eutrophic conditions, seasonal upwellings and Amur River discharges. It is characterized by the dominance of O. centrocarpum, Brigantedinium spp. and Islandinium minutum; 2) the Western Subarctic Gyre zone with subpolar and mesotrophic conditions due to the Kamchatka Current and Alaska Stream inflows. Assemblages are dominated by Nematosphaeropsis labyrinthus, Pyxidinopsis reticulata and Brigantedinium spp.; 3) the Bering Sea zone, depicting a subpolar environment, influenced by seasonal upwellings and inputs from the Anadyr and Yukon Rivers. It is characterized by the dominance of I. minutum and Brigantedinium spp.; 4) the Alaska Gyre zone with temperate conditions and nutrient-enriched surface waters, which is dominated by N. labyrinthus and Brigantedinium spp. and 5) the Kuroshio Extension-North Pacific-Subarctic Current zone characterized by a subtropical and oligotrophic environment, which is dominated by O. centrocarpum, N. labyrinthus and warm taxa of the genus Impagidinium. Transfer functions were tested using the modern analog technique (MAT) on the North Pacific Ocean (= 359 sites) and the entire Northern Hemisphere databases ( = 1419 sites). Results confirm that the updated Northern Hemisphere database is suitable for further paleoenvironmental reconstructions, and the best results are obtained for temperatures with an accuracy of +/-1.7 °C.