Trypanocidal activity of Brazilian plants against epimastigote forms from Y and Bolivia strains of Trypanosoma cruzi

Chagas disease is one of the main public health problems in Latin America. Since the available treatments for this disease are not effective in providing cure, the screening of potential antiprotozoal agents is essential, mainly of those obtained from natural sources. This study aimed to provide an evaluation of the trypanocidal activity of 92 ethanol extracts from species belonging to the families Annonaceae, Apiaceae, Cucurbitaceae, Lamiaceae, Lauraceae, Moraceae, Nyctaginaceae, and Verbenaceae against the Y and Bolivia strains of Trypanosoma cruzi. Additionally, cytotoxic activity on LLCMK2 fibroblasts was evaluated. Both the trypanocidal activity and cytotoxicity were evaluated using the MTT method, in the following concentrations: 500, 350, 250, and 100 µg/mL. Benznidazole was used for positive control. The best results among the 92 samples evaluated were obtained with ethanol extracts of Ocotea paranapiacabensis (Am93) and Aegiphila lhotzkiana (Am160). Am93 showed trypanocidal activity against epimastigote forms of the Bolivia strain and was moderately toxic to LLCMK2 cells, its Selectivity Index (SI) being 14.56, while Am160 showed moderate trypanocidal activity against the Bolivia strain and moderate toxicicity, its SI being equal to 1.15. The screening of Brazilian plants has indicated the potential effect of ethanol extracts obtained from Ocotea paranapiacabensis and Aegiphila lhotzkiana against Chagas disease.

Caracterización petrográfica de los travertinos aragoníticos del Barranco de Azuaje (Gran Canaria)

[ES]El Barranco de Azuaje está situado en el NE de la isla volcánica de Gran Canaria. El barranco se formó por incisión sobre depósitos volcánicos de edad inferior a 5,5 Ma. La presencia de depósitos de travertino situados dentro del barranco constituye un rasgo destacado. Estos travertinos están compuestos por aragonito fibroso y calcita, en menor cantidad. Las principales facies reconocidas son: laminar, masiva porosa, de granos con cubiertas y tobácea. Sus especiales texturas, el infrecuente contexto volcánico y el hecho de que el travertino se haya formado en un área sin depósitos carbonáticos previos, hacen de éste un travertino único entre los depósitos relacionados con manantiales.Las principales facies y la mineralogía sugieren que estos depósitos se formaron bajo la influencia de aguas termógenas por desgasificación rápida de CO2 en un sistema de cascadas y pozas.

Studio di rivestimenti antiriflesso da sol-gel dip-coating per impianti solari termodinamici

Negli impianti utilizzati per la produzione di energia elettrica che sfruttano l'energia solare, quali la tecnologia solare a concentrazione (Solare Termodinamico) sviluppata da ENEA, per minimizzare le dispersioni di calore è necessaria una elevata selettività spettrale. Per ottimizzare l'efficienza dell'impianto è quindi necessario lo sviluppo di materiali innovativi, in grado di minimizzare la quantità di energia dispersa per riflessione. In questo studio, per incrementare la trasmittanza solare dei componenti in vetro presenti nei tubi ricevitori dell'impianto, sono state utilizzate tipologie diverse di rivestimenti antiriflesso (multistrato e a singolo strato poroso). I rivestimenti sono stati ottenuti mediante via umida, con tecnica di sol-gel dip-coating. I sol coprenti sono stati preparati da alcossidi o sali metallici precursori degli ossidi che costituiscono il rivestimento. Sono state approfondite sia la fase di sintesi dei sol coprenti, sia la fase di deposizione sul substrato, che ha richiesto la progettazione e realizzazione di una apparecchiatura prototipale, ossia di un dip-coater in grado di garantire un accurato controllo della velocità di emersione e dell'ambiente di deposizione (temperatura e umidità). Il materiale multistrato applicato su vetro non ha migliorato la trasmittanza del substrato nell'intervallo di lunghezze d'onda dello spettro solare, pur presentando buone caratteristiche antiriflesso nell'intervallo dell'UV-Vis. Al contrario, l'ottimizzazione del rivestimento a base di silice porosa, ha portato all'ottenimento di indici di rifrazione molto bassi (1.15 to 1.18) e ad un incremento della trasmittanza solare dal 91.5% al 96.8%, efficienza superiore agli attuali rivestimenti disponibili in commercio.

Allestimento di modello sperimentale su animali di tessuto osseo ingegnerizzato

Questo studio ha valutato l'efficacia di un approccio rigenerativo utilizzando cellule staminali mesenchimali (MSC) e uno scaffold di idrossiapatite pura e porosa (HA) progettata con tecnologia CAD-CAM per sostituire il condilo dell'articolazione temporomandibolare (ATM). Metodi.Uno scaffolds di HA con porosità totale del 70% è stato prototipato per sostituire i due condili temporomandibolari (sinistro e destro) dello stesso animale. MSC sono state ottenute dalla cresta iliaca ed espanse in coltura. Guide chirurgiche su misura sono state create e utilizzate per esportare la pianificazione virtuale delle linee di taglio dell'osso nell'ambiente chirurgico. Sei pecore sono state sacrificate a 4 mesi dopo l'intervento.Gli scaffold sono stati espiantati, campioni istologici sono stati preparati, ed è stata eseguota l'analisi istomorfometrica. Risultati.L'analisi della riduzione di porosità per apposizione di osso neoformato mostrata una differenza statisticamente significativa tra la formazione ossea nei condili carichi di MSC rispetto ai condili senza (

Forest structure and composition of previously selectively logged and non-logged montane forests at Mt. Kilimanjaro

The montane forests of Mount Kilimanjaro in Tanzania have been subjected to a long history of selective logging. However, since 1984 logging of indigenous trees is prohibited. Today, these forests allow us to evaluate the long-term effects of selective logging. We mapped the height and diameter at breast height (DBH) of all trees >10 cm DBH on 10 sites of 0.25 ha. Five sites represent non-logged forests, another five selectively logged forests. We tested whether forests were still visibly affected 30–40 years after selective logging in terms of their forest structure and tree diversity. Additionally we compared tree densities of different species guilds, including disturbance-indicator species, late-successional species and main timber species. Furthermore, we specifically compared the community size distributions of selectively logged and non-logged forests, first across all species and then for the most important timber species, Ocotea usambarensis, alone. 30–40 years after selective logging forests still showed a higher overall stem density, mainly due to higher relative abundances of small trees (<50 cm DBH) in general, and higher densities of small size class stems of late-successional species specifically. For O. usambarensis, the selectively logged sites harboured higher relative abundances of small trees and lower relative abundances of harvestable trees. The higher relative abundance of small O. usambarensis-stems in selectively logged forests appears promising for future forest recovery. Thus, outside protected areas, selective logging may be a sustainable management option if logging cycles are considerably longer than 40 years, enough large source trees remain, and the recruiting O. usambarensis individuals find open space for their establishment.

Mineralogy and nannoplankton distribution in ODP Hole 194-1195A

Significant synchronous shifts in the chemistry, mineralogy, grain sizes and color of the sediments at 6 m below sea floor (mbsf) at ODP Site 1195 on the Marion Plateau (NE Australia) are interpreted to reflect a major regional paleoceanographic change: the initiation of the southern province of the Great Barrier Reef (GBR). The onset of this massive carbonate production centre nearby resulted primarily in increased deposition of carbonate-rich sediments of neritic origin. Both sedimentation rate and terrigenous input record a coincident decline attributed to inshore trapping of materials behind the reefs. Our best estimate places the development of reef framework in the southern part of the GBR between 560 and 670 kyr B.P., based on an age model combining magnetostratigraphic and biostratigraphic data. The proposed estimation agrees with previous studies reporting an age between 500 and 930 kyr B.P., constraining more tightly their results. However, it does not support research placing the birth of the GBR in Marine Isotope Stage (MIS) 11 (~400 kyr), nor the theory of a worldwide modern barrier reef development at that time.

La ficción sin límites (la ruta argentina de Virgilio Piñera)

La ponencia se propone interrogar las maneras en que la literatura piñeriana, desde el ensayo y la cuentística producida durante sus años de exilio porteño, interroga los límites de las configuraciones estético-ideológicas de los campos a los que se vincula (especialmente las formaciones discursivas de las revistas Orígenes y Sur). Al dibujar una porosa frontera entre ambos territorios, se instaura como la metáfora de un diálogo cultural descentrado y utópico en el mapa de las literaturas latinoamericanas

La ficción sin límites (la ruta argentina de Virgilio Piñera)

La ponencia se propone interrogar las maneras en que la literatura piñeriana, desde el ensayo y la cuentística producida durante sus años de exilio porteño, interroga los límites de las configuraciones estético-ideológicas de los campos a los que se vincula (especialmente las formaciones discursivas de las revistas Orígenes y Sur). Al dibujar una porosa frontera entre ambos territorios, se instaura como la metáfora de un diálogo cultural descentrado y utópico en el mapa de las literaturas latinoamericanas

La ficción sin límites (la ruta argentina de Virgilio Piñera)

La ponencia se propone interrogar las maneras en que la literatura piñeriana, desde el ensayo y la cuentística producida durante sus años de exilio porteño, interroga los límites de las configuraciones estético-ideológicas de los campos a los que se vincula (especialmente las formaciones discursivas de las revistas Orígenes y Sur). Al dibujar una porosa frontera entre ambos territorios, se instaura como la metáfora de un diálogo cultural descentrado y utópico en el mapa de las literaturas latinoamericanas

Dinoflagellates of ODP Leg 104 holes

Dinoflagellate cysts, pollen, and spores were studied from 78 samples of the Eocene to Miocene section of ODP Site 643 at the outer Wring Plateau. Dinoflagellate cysts ranging from less than 1,000 to rarely over 30,000 per gram of sediment in the Paleogene, and generally between 50,000 and 100,000 in the Miocene were present. The shift to conspicuously higher cyst frequencies takes place in the lowermost Miocene section and appears to reflect increased cyst recruitment rather than a change in sedimentation rate. Of the 179 dinoflagellate cyst forms whose ranges were recorded, 129 are known species. Fifteen assemblage zones have been recognized, although the upper Eocene is missing and no substantial lower Eocene was recorded at Site 643. Norwegian Sea and Rockall Plateau zonations were compared with this study. Detailed correlation with existing onshore section zonations was difficult because key zonal species are inadequately represented; however, the middle to upper Miocene zonation established for Denmark is applicable. Pollen and spores occur with relatively low frequencies, and palynodebris is generally absent, in contrast to the observations from DSDP Leg 38. Thirty-nine samples from Eocene to Miocene sediments at Site 642 were studied and correlated with Site 643. A lower Eocene cyst assemblage present in Hole 642D is older than the questionably lower Eocene assemblage from Site 643. Site 642 has a lower Eocene to lower Miocene hiatus.

Stratigraphic occurrence of selected marine palynomorph species recorder in the Paleogene of ODP Hole 105-647A (Table 3)

Dinoflagellate cysts were recovered throughout the Paleogene succession of Hole 647A, which contains an almost complete deep-water record of early Eocene through early late Oligocene sedimentation in the Labrador Sea. Dinoflagellate cyst biostratigraphy is in general accord with that provided by other microfossil groups and is consistent with a lower Eocene age, as determined by nannofossils, for basal sediments in Hole 647A. These sediments overlie oceanic crust of Chron 24 age. Dinocyst assemblages indicate outer neritic to oceanic conditions throughout, although the persistent occurrence of Wetzeliellaceae specimens in the lower Eocene suggests a greater influence from shelf environments during this time. Lower Eocene dinocyst assemblages are similar to coeval assemblages from the Rockall Plateau, but those from the middle to upper Eocene have mixed affinities and may be related to the intensification of the proto-Gulf Stream from middle Eocene time. Oligocene dinocyst assemblages suggest the influence of both arctic and North Atlantic wate rmasses at this site. The presence of protoperidineacean species in the upper Eocene and Oligocene may indicate increased availability of nutrients, perhaps related to increased upwelling or the effects of water-mass mixing. Productive samples are dominated by dinocysts and acritarchs, while sporomorphs are represented mainly by bisaccate pollen. Preservational differences within samples may reflect mixing of penecontemporaneous dinocyst populations during the Eocene, and all samples examined may have a considerable allochthonous component. Variability in relative abundance of many species during the Eocene may be related to fluctuating water-mass properties. A total 175 dinocyst and acritarch taxa were recorded from 53 productive samples from the Paleogene. Only one Paleogene sample was barren of palynomorphs. Of three Miocene samples processed, all were barren.