16 resultados para Pavonia
Resumo:
In this present work an ethnographic research was performed with 84 native medicinal specimens from the Litoral Norte Riograndense, from which two plants Cleome spinosa Jacq e Pavonia varians Moric were submitted to ethnobotanic, phytochemistry and pharmacologic investigations. Additionally, a phytopharmacological research of the medicinal specimen Croton cajucara Benth ( native plant of the Amazon region of Brazil) was improved. The obtained phytochemical results of the C. spinosa and P. varians showed the presence of flavonoids constituents, among other components. The two flavonoids (2S)-5-hydroxy-7,4 -dimethoxy-flavanone and 5,4 -dihydroxy-3,7,3 -trimethoxy-flavone were isolated from C. spinosa. The antioxidant activity of the hydroalcoholic extracts of C. spinosa and P. varians solubilized in the microemulsion systems SME-1 and SME-4, was evaluated in the DPPHmethod. The used SME systems [obtained with Tween 80: Span 20 (3:1) and isopropyl myristate (IPM)] improved the dissolution of those tested polar extracts, with higher efficacy to the SME-1 system (in which ethanol was included as cosurfactant). The CE50 values evidenced for P. varians were 114 [g/mL (SME-1) and 246 [g/mL (SME-4); for C. spinosa it was 224 [g/mL (SME-1) and 248 [g/mL (SME-4), being the system SME-1 more effective for both tested extracts. The hydroalcoholic extracts of P. varians (HAE-PV) was also submitted to pharmacological screening for antinociceptive activity in animal models. The oral administration of this extract (100, 300 and 1000 mg/kg) inhibited the acetic acid-induced writhing in mice. The higher inhibition (74%) was evidenced to the 1000 mg/kg administered dose. Its effect on the central nervous system (CNS) was investigated by tail flick and formalin-method and reveled that it has negligible antinociceptive action on the CNS. After taking consideration of HAE-PV interaction, Pavonia varians Moric could be used as a potent analgesic agent in case of peripheral algesia, without affecting the CNS. The phytochemical study of the stem bark of Croton cajucara Benth lead to the isolation of 19-nor-clerodanetype diterpenes, as well as to the separation of its fixed oil FO-CC. This non polar oil material reveled to be rich in sesquiterpenes and 19-nor-clerodanes components. The biologic effect of OF-CC was evaluated in the development in vitro of the fungis phytopatogens such as Fusarium oxysporum, Rhizoctonia solani and Sclerotium rolfsii. Significant inhibitory effect of the tested fungis (at 0,2 mg.mL-1 dosage) were comproved. A Mass Spectrometry study of clerodane-type diterpenes was developed in order to identify characteristic fragments on mass spectrometra of both clerodane and 19-nor-clerodane presenting an α,β-insaturated carbonyl moiety at ring A of the decalin-system. For that study, mass spectroscopy data were analysed for 19-nor-clerodanes [trans-dehydrocrotonin (DCTN), trans-crotonin (CTN), cis-cajucarin B (c-CJC-B), and cajucarinolide (CJCR)] and for clerodanes [isosacacarin (ISCR) and transcajucarin A (t-CJC-A)] obtained from the stem bark of C. cajucara, and also clerodane-type from other species. The trans-junction of the enone-system clerodanes was clear correlated with the presence of the characteristic ions at m/z 95, 121 e 205. Meanwhile, the characteristics ions at m/z 122 e 124 were correlated to cis-junction. The trans-junction of the enone-system 19-nor-clerodanes showed characteristics ions at m/z 161, 134 e 121. This study could be successful employed for identification of clerodane constituents from other specimens without any additional spectroscopic analyses, as well as a previously phytochemical analyzes in clerodane project search
Resumo:
Malvaceae shows a rich morphological diversity of secretory structures, which are of great ecological and taxonomical relevance. Nonetheless, until the present moment, studies on the secretory structures of the studied species were not found. Pavonia alnifolia A.St.-Hil. is endangered species of extinction with restricted distribution within the restingas of Rio the Janeiro and Espírito Santo, Brazil. The species were collected from the former and usual techniques on plant anatomy and histochemistry were performed. Anatomical and histochemical studies of the secretory structures of Pavonia alnifolia are showed in this work. The presence of external and internal secretory structures of mucilage in many organs, idioblasts of phenolic and lipid substances and floral nectaries what is a very important adaptative survival mechanism of the species in the restinga environment. The secretion produced by nectaries is envolved with maintenance of interations with visiting insects, what constitutes a good model to experimental studies with an ecological approach.
Resumo:
Von Carl Frings
Resumo:
O estudo foi desenvolvido em um dos sítios do Programa de Biodiversidade da Amazônia (PPBio) localizado na Floresta Nacional de Caxiuanã (PA) e teve como objetivos: apresentar os fungos poróides com ênfase nos novos registros; analisar a relação destes fungos com o substrato lenhoso e examinar a associação entre variáveis micrometeorológicas (temperatura do ar, umidade relativa e pluviosidade) durante um ano, em relação às variáveis ambientais produzidas pela topografia, com a riqueza, densidade, e a fenologia destes fungos. Foram identificadas 76 espécies de fungos poróides, distribuídas em 27 gêneros e cinco famílias. Cerrena sclerodepsis, Phellinus dependens e Trametes pavonia representam primeiro registros para o estado do Pará. A espécie Microporellus iguazuensis é citada pela primeira vez para o Brasil e é apresentada a proposição de uma de nova espécie para a ciência denominada Microporellus hirsuta. A maioria das espécies foi considerada rara e apresentou preferência por substratos nos primeiros estágios de decomposição. O número de ocorrências de basidioma e de espécies de fungos foi maior em troncos de plantas das famílias Caesalpinaceae, Sapotaceae, Annonaceae, Mimosaceae e Lecythidaceae, respectivamente, e em substrato com diâmetro menor. Era esperado que as diferenças no microclima gerado por diferentes altitudes, em um pequeno gradiente topográfico, fossem o suficiente para gerar diferenças na comunidade de fungos poróides. No entanto, embora tenha sido encontrado um maior número de espécies na região denominada de intermediária, esta diferença não foi significativa. O maior número de indivíduos foi encontrado quando das primeiras chuvas na estação chuvosa e a riqueza esteve diretamente correlacionada com a pluviosidade. O índice de atividade de produção de basidioma das espécies mais abundantes foi maior no período das primeiras chuvas após o período seco. Este estudo representa avanços no entendimento das relações dos fungos com o meio em que eles se desenvolvem principalmente nas regiões tropicais. No entanto muitos estudos ainda precisam ser desenvolvidos para o esclarecimento destas relações.
Flora de un área de la Sierra La Barrosa (Balcarce) y fenología de especies con potencial ornamental
Resumo:
Los objetivos de este trabajo fueron inventariar la flora vascular en un área de la Sierra La Barrosa (Sistema de Tandilia, Buenos Aires), determinar la utilidad actual o potencial de las especies e iniciar un estudio fenológico preliminar in situ de 10 especies nativas de interés ornamental. El relevamiento florístico se realizó en un sector de la cima y laderas y se elaboró una base de datos con registros taxonómicos, origen, ciclo, forma biológica y utilidad de las especies. Se identificaron 204 especies, pertenecientes a 51 familias y 135 géneros; de ellas 70,6% son nativas no endémicas; 9,31% endémicas y 20,1% exóticas. El 76% de las especies son perennes y predominan las hemicriptófitas (41,2%). El 65% de las especies inventariadas tiene interés agronómico por su utilidad potencial como medicinal (21,5%), ornamental (25%), forrajera (13,7%), o por ser malezas o tóxicas (13,2 %). Por su potencial ornamental (hábito, atributos del follaje, flores e inflorescencias), se efectuó un estudio fenológico en Achyrocline satureioides, Eupatorium subhastatum, E. tanacetifolium, Hysterionica pinifolia, Senecio pulcher, Sommerfeltia spinulosa, Lathyrus pubescens, Mimosa rocae, Pavonia cymbalaria y Gomphrena perennis, que indicó diferencias en la época y duración de la floración.
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ODP Site 1078 situated under the coast of Angola provides the first record of the vegetation history for Angola. The upper 11 m of the core covers the past 30 thousand years, which has been analysed palynologically in decadal to centennial resolution. Alkenone sea surface temperature estimates were analysed in centennial resolution. We studied sea surface temperatures and vegetation development during full glacial, deglacial, and interglacial conditions. During the glacial the vegetation in Angola was very open consisting of grass and heath lands, deserts and semi-deserts, which suggests a cool and dry climate. A change to warmer and more humid conditions is indicated by forest expansion starting in step with the earliest temperature rise in Antarctica, 22 thousand years ago. We infer that around the period of Heinrich Event 1, a northward excursion of the Angola Benguela Front and the Congo Air Boundary resulted in cool sea surface temperatures but rain forest remained present in the northern lowlands of Angola. Rain forest and dry forest area increase 15 thousand years ago. During the Holocene, dry forests and Miombo woodlands expanded. Also in Angola globally recognised climate changes at 8 thousand and 4 thousand years ago had an impact on the vegetation. During the past 2 thousand years, savannah vegetation became dominant.
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The distribution of pollen in marine sediments is used to record vegetation change on the continent. Generally, a good latitudinal correspondence exists between the distribution patterns of pollen in the marine surface sediments and the occurrence of the source plants on the adjacent continent. To investigate land-sea interactions during deglaciation, we compare proxies for continental (pollen assemblages) and marine conditions (alkenone-derived sea surface temperatures) of two high-resolution, radiocarbon-dated sedimentary records from the tropical southeast Atlantic. The southern site is located West of the Cunene River mouth; the northern site is located West of the Angolan Huambe Mountains. It is inferred that the vegetation in Angola developed from Afroalpine and open savannah during the last Glacial maximum (LGM) via Afromontane Podocarpus forest during Heinrich Event 1 (H1), to an early increase of lowland forest after 14.5 ka. The vegetation record indicates dry and cold conditions during the LGM, cool and wet conditions during H1 and a gradual rise in temperature starting well before the Younger Dryas (YD) period. Terrestrial and oceanic climate developments seem largely running parallel, in contrast to the situation ca. 5° further South, where marine and terrestrial developments diverge during the YD. The cool and wet conditions in tropical West Africa, South of the equator, during H1 suggest that low-latitude insolation variation is more important than the slowdown of the thermohaline circulation for the climate in tropical Africa.
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The Long-Term Ecological Research (LTER) observatory HAUSGARTEN, in the eastern Fram Strait, provides us the valuable ability to study the composition of benthic megafaunal communities through the analysis of seafloor photographs. This, in combination with extensive sampling campaigns, which have yielded a unique data set on faunal, bacterial, biogeochemical and geological properties, as well as on hydrography and sedimentation patterns, allows us to address the question of why variations in megafaunal community structure and species distribution exist within regional (60-110 km) and local (<4 km) scales. Here, we present first results from the latitudinal HAUSGARTEN gradient, consisting of three different stations (N3, HG-IV, S3) between 78°30'N and 79°45'N (2351 - 2788 m depth), obtained via the analysis of images acquired by a towed camera (OFOS - Ocean Floor Observation System) in 2011. We assess variability in megafaunal densities, species composition and diversity as well as biotic and biogenic habitat features, which may cause the patterns observed. While there were significant regional-scale differences in megafaunal composition and densities between the stations (N3 = 26.74 ± 0.63; HG-IV = 11.21 ± 0.25; S3 = 18.34 ± 0.39 individuals/m**2), significant local differences were only found at HG-IV. Regional-scale variations may be due to the significant differences in ice coverage at each station as well as the different quantities of protein available, whereas local-scale differences at HG-IV may be a result of variation in bottom topography or factors not yet identified.