56 resultados para Hyptidendron canum
Resumo:
Chemical investigation of Hyptidendron canum stems resulted in the isolation of betulinic, ursolic and euscaphic acids. From the leaves were isolated 3β-O-β-galactopiranosilsitosterol, ursolic aldehyde, and mixtures of maslinic acid and 2α-hydroxyursolic acid, α and β-amyrin, uvaol and erythrodiol, sitosterol and stigmasterol, spathulenol and globulol. Hexane and chloroform leave fractions as well as ursolic and betulinic acids showed antifungal activities against the yeast form of Paracoccidioides brasiliensis.
Resumo:
Chemical investigation of Hyptidendron canum stems resulted in the isolation of betulinic, ursolic and euscaphic acids. From the leaves were isolated 3β-O-β-galactopiranosilsitosterol, ursolic aldehyde, and mixtures of maslinic acid and 2α-hydroxyursolic acid, α and β-amyrin, uvaol and erythrodiol, sitosterol and stigmasterol, spathulenol and globulol. Hexane and chloroform leave fractions as well as ursolic and betulinic acids showed antifungal activities against the yeast form of Paracoccidioides brasiliensis.
Resumo:
CHEMICAL CONSTITUENTS OF Hyptidendron canum (Pohl ex Benth.) R. Harley (LAMIACEAE). Chemical investigation of Hyptidendron canum stems resulted in the isolation of betulinic, ursolic and euscaphic acids. From the leaves were isolated 3β-O- β-galactopiranosilsitosterol, ursolic aldehyde, and mixtures of maslinic acid and 2α-hydroxyursolic acid, α and β-amyrin, uvaol and erythrodiol, sitosterol and stigmasterol, spathulenol and globulol. Hexane and chloroform leave fractions as well as ursolic and betulinic acids showed antifungal activities against the yeast form of Paracoccidioides brasiliensis.
Resumo:
Sementes de carrapicho-beiço-de-boi (Desmodium canum) foram germinadas em placas de Petri, sobre papel de filtro, com diferentes concentrações de trifluralin e fluchloralin (0, 0,5, 2,5, 12,5 e 62,5 ppm). Após 28 dias nesse meio, as plântulas foram transferidas para vasos contendo solo sem herbicida, onde permaneceram até os 101 dias de desenvolvimento. O ensaio foi conduzido em condições de labora tório, com temperatura variando entre 25-28°C. Plantas com 101 dias de desenvolvimento, prétratadas com as concentrações mais baixas dos herbicidas, apresentaram-se atrofiadas e menos vigorosas quando comparadas com plantas testemunhas; nas mais elevadas, a maioria das plantas não sobreviveu aos tratamentos. A análise histológica do caule, ao nível do nó e entrenó, mostrou intensa desorganização dos tecidos, principalmente do tecido vascular.
Resumo:
We show that the observed K velocities and periodicities of AM CVn can be reconciled given a mass ratio q~0.22 and a secondary star with a modest magnetic field of surface strength B~1 T. We see that the new mass ratio implies that the secondary is most likely semidegenerate. The effect of the field on the accretion disc structure is examined. The theory of precessing discs and resonant orbits is generalized to encompass higher order resonances than 3:2 and shown to retain consistency with the new mass ratio.
Resumo:
Sementes de carrapicho-beiço-de-boi (Desmodium canum) foram germinadas em placas de Petri, sobre papel de filtro, com diferentes concentrações de trifluralin e fluchloralin (0, 0,5, 2,5, 12,5 e 62,5 ppm). Após 28 dias nesse meio, as plântulas foram transferidas para vasos contendo solo sem herbicida, onde permaneceram até os 101 dias de desenvolvimento. O ensaio foi conduzido em condições de labora tório, com temperatura variando entre 25-28°C. Plantas com 101 dias de desenvolvimento, prétratadas com as concentrações mais baixas dos herbicidas, apresentaram-se atrofiadas e menos vigorosas quando comparadas com plantas testemunhas; nas mais elevadas, a maioria das plantas não sobreviveu aos tratamentos. A análise histológica do caule, ao nível do nó e entrenó, mostrou intensa desorganização dos tecidos, principalmente do tecido vascular.
Resumo:
Tortopus Needham & Murphy, 1924 and Tortopsis Molineri, 2010 with six and 10 species, respectively, are sister genera distributed in the Neartic and Neotropical regions. In spite that most species are known from the tropics of South America, only one species of each of these groups have been recorded from Brazil. Here we present distributional data expanding greatly the range of these groups including three new country records for Brazil: Tortopus igaranus Needham & Murphy, 1924, Tortopsis limoncocha Molineri, 2010 and Tortopsis spatula Molineri, 2010. We describe a distinct new species, Tortopus ipixuna sp. nov., from male imagos, that present a unique subrectangular pedestal. Additionally we redescribe the male imago of Tortopus harrisi Traver, 1950 (previously known only from the holotype), and we give the first records for Tortopsis canum Gonçalves, Da-Silva & Nessimian, 2011 from Espírito Santo and for Tortopsis spatula from Ecuador. Some variations in morphological structures of these species are also described, illustrated and discussed.
Resumo:
Atualmente existem 23 milhões de hectares de pastagens cultivadas em área originalmente sob floresta na Amazônia. Desse total, em torno de cinco milhões de hectares encontram-se com baixa produtividade ou em vias de degradação, infestados de plantas daninhas. Com o objetivo de identificar as plantas daninhas que ocorrem em área de pastagem de baixa produtividade em Terra Alta, PA ( 0º 58 S e 47º 52 W. Gr. ), foram efetuados levantamentos botânicos qualitativos, pelo método visual e coleta de todas as espécies presentes na área. Foram registradas 34 famílias, representadas por 118 espécies, destacando-se as famílias Leguminosae, Gramineae, Malvaceae, Myrtaceae, Cyperaceae e Asteraceae com 21, 16, 8, 7, 6 e 6 espécies, respectivamente. As plantas daninhas consideradas mais importantes foram: Borreira verticillata, Rolandra argentea, Desmodium canum, Davilla rugosa, Vismia guianensis e Imperata brasiliensis.
Resumo:
A região do trópico úmido amazônico ocupa 350 milhões de hectares, constituindo a maior área de fronteira agrícola do planeta. A pecuária como exploração do uso da terra é a principal forma de ocupação e de desmatamento na região, apesar da baixa produtividade e das conseqüências ambientais. O declínio da produtividade da pastagem está associado, entre outras, ao manejo inadequado e à elevada infestação de plantas daninhas herbáceas e arbustivas, anuais ou perenes, geralmente denominadas "juquira" na região. Se essas plantas não forem controladas adequadamente, podem levar à degradação da pastagem, resultando na completa perda de produtividade e no posterior abandono da área. Com o objetivo de identificar as plantas daninhas mais importantes que ocorrem em área de pastagem de baixa produtividade no município de Terra Alta, PA (0º 58" S e 47º 52" W. Gr.), foi efetuado um levantamento florístico em 0,33 ha de área cultivada com capim-quicuio-da-amazônia (Brachiaria humidicola). Foram registrados 4.700 indivíduos, distribuídos em 17 famílias botânicas, representadas por 36 espécies vegetais. Destacaram-se as famílias Poaceae, Rubiaceae, Fabaceae, Asteraceae e Solanaceae, sendo encontrado em cada uma delas cinco, cinco, quatro, três e três espécies, respectivamente. As plantas daninhas consideradas de maior importância na comunidade vegetal foram: Borreria verticillata, Hyptis atrorubens, Rolandra argentea, Desmodium canum, Panicum pilosum, Davilla rugosa, Imperata brasiliensis, Paspalum maritimum, Vernonia scorpioides e Vismia guianensis.
Resumo:
Contient : 1° « Annales ou cronicque des choses faictes et advenues en France du temps des sept premieres années du regne du roy Françoys premier... depuys le premier de janvier, l'an de grace mil.V.C. XIIII jusques en decembre, l'an de grace mil.V.C. XXI » ; 2° Pièce de vers ; 3° Fragment de quatrelignes du roman grec des Amours d'Isménias et Ismène (liv. III) ; 4° Pièces de vers ; 5° Pièces de vers ; 6° « HIERONIMI FRACASTORII de cura canum venaticorum » ; 7° Pièces de vers ; 8° « JOANNIS BELLAI, cardinalis... in diem natalitium... Pauli III, pontificis maximi » ; 9° « HYERONIMI FRACASTORII carpus » ; 10° « Silva langeana » ; 11° « JACOBI SADOLETI sylva ad Octavium et Fredericum Fregusos » ; 12° Pièces de vers « in Belcagonem » ; 13° « Sinceri Sannazarii epitaphium... » ; 14° Pièces de vers ; 15° « A ma muse » ; 16° « Concions divines et spirituelles, plaines de consolation chrestienne, du St et divin Pere MACAIRE, Egiptien, de la vraye perfection necessaire et tres utile à chasque chrestien, mises de grecque en françoys » ; 17° « D. GREGORII NAZANZENI oratio ad beatissimam virginem Mariam, ex tragoedia quae Christus patiens inscribitur » ; 18° « GENNADII SCHOLARII, archiepiscopi constantinopolitani, oratio ad unum Deum, qui est in tribus hypostasibus »
Resumo:
Contient : 1° « Annales ou cronicque des choses faictes et advenues en France du temps des sept premieres années du regne du roy Françoys premier... depuys le premier de janvier, l'an de grace mil.V.C. XIIII jusques en decembre, l'an de grace mil.V.C. XXI » ; 2° Pièce de vers ; 3° Fragment de quatrelignes du roman grec des Amours d'Isménias et Ismène (liv. III) ; 4° Pièces de vers ; 5° Pièces de vers ; 6° « HIERONIMI FRACASTORII de cura canum venaticorum » ; 7° Pièces de vers ; 8° « JOANNIS BELLAI, cardinalis... in diem natalitium... Pauli III, pontificis maximi » ; 9° « HYERONIMI FRACASTORII carpus » ; 10° « Silva langeana » ; 11° « JACOBI SADOLETI sylva ad Octavium et Fredericum Fregusos » ; 12° Pièces de vers « in Belcagonem » ; 13° « Sinceri Sannazarii epitaphium... » ; 14° Pièces de vers ; 15° « A ma muse » ; 16° « Concions divines et spirituelles, plaines de consolation chrestienne, du St et divin Pere MACAIRE, Egiptien, de la vraye perfection necessaire et tres utile à chasque chrestien, mises de grecque en françoys » ; 17° « D. GREGORII NAZANZENI oratio ad beatissimam virginem Mariam, ex tragoedia quae Christus patiens inscribitur » ; 18° « GENNADII SCHOLARII, archiepiscopi constantinopolitani, oratio ad unum Deum, qui est in tribus hypostasibus »
Resumo:
The discovery of a neolithic pile field in the shallow water near the eastern shore of the Degersee confirmed earlier palynological and sedimentological studies stating that early man was active in the region since more than 6000 years. The already available off-site data were freshly assessed, completed by additional data from old and new cores and the interpretations revised. A common time scale for the off-site data and the on-site data was obtained by AMS dating of terrestrial macro remains of the neolithic section of off-site core De_I+De_H. The ages can thus be parallelled with AMS ages of construction timber on-site. Pollen analyses from all cores provide a further time scale. The continuously and densely sampled pollen profile of the profundal zone embracing the entire Late glacial and Holocene serves as a reference. From the Boreal onwards the relative ages are transformed by AMS ages and varve counts into calibrated and absolute. A transect cored close to the neolithic pile field across the lake marl-platform demonstrates its geological architecture in the shallow water since the Lateglacial. Studies of the microfabric of thin sections of drilled cores and of box cores from the excavations demonstrate that neolithic settlements now at 2-3,5 m water depth had been erected on lake marl freshly fallen dry, thus indicating earlier lake levels dropped by 1.5-2 m. The neolithic section of the highly resolved off-site profile in the lake=s profundal zone has laminated and calcareous zones alternating with massive ones. Assemblages of diatoms and concentrations of trace elements changing simultaneously characterise the calcareous sections as deposits of low lake levels that lasted between some 40 and more than 300 years. The ages of discovered lake shore dwellings fall into calcareous segments with low lake levels. From the end of the Upper Atlantic period (F VII) appear Secondary Forest Cycles in the beech forest, a man-made sequence of repeated vegetational development with an identical pattern: With a decrease of beech pollen appear pollen of grasses, herbs and cultural indicators. These are suppressed by the light demanding hazel and birch, those again by ash, and finally by the shade demanding beech forming a new pollen peak. Seven main Forest Cycles are identified In the upper Neolithic period each comprising some 250, 450 or 800 years. They are subdivided into subcycles that can be broken down by very dense sampling in even shorter cycles of decadal length. Farming settlers have caused minor patchy clearances of the beech-mixed-forest with the use of fire. The phases of clearance coincide with peaks of charcoal and low stands of the lake levels. The Secondary Forest Cycles and the continuous occurrence of charcoal prove a continued occupation of the region. Together with the repeated restoration of the beech climax forest they point to pulsating occupation probably associated with dynamic demography. The synchronism of the many palynological, sedimentological and archaeological data point to an external forcing as the climate that affects comprehensively all these proxies. The fluctuations of the activity of the sun as manifested in the residual d14C go largely along with the proxies. The initial clearances at the begin of the forest cycles are linked to low lake levels and negative values of d14C that point to dry and warm phases of a more continental climate type. The subcycles exist independent from climatic changes, indicating that early man acted largely independent from external forces.
Resumo:
Lake Blankensee is filled with 14 m of late- and postglacial deposits, Lake Siethener See with 22,5 m. The lacustrine sedimentation begins in Lake Siethener See in the middle of the Alleröd with annual lamination which partly continues in the Younger Dryas. A 2 cm thick layer of the Laacher See tephra was found in both lakes, the Saksunarvatn tephra only in Lake Siethener See where the cool Rammelbeek-phase (Preboreal) could be shown. The youngest part of the sediment profiles is suspended drifting mud. Masses of Pediastrum (algae) indicate an increasing shoaling of Lake Blankensee after the Subboreal.
Resumo:
A basaltic tephra layer consisting of brownish-olive glass shards. and about 0.2 mm thick. was found in cores from four lakes in northwest Germany. According to pollen analysis it was deposited during the early Boreal period (corresponding to about 8700 BP). The petrographic properties. the geochemical composition and the age agree with those of the Saksunarvatn tephra. which was first found on the Faroe Islands. The position of the tephra layer in the pollen stratigraphy and in the absolute time-scale is discussed. Procedures for locating the tephra in other cores are suggested.