19 resultados para Trichosalpinx intricata


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Duas espécies de Orchidaceae, Myoxanthus parvilabius (C. Schweinf.) Luer e Trichosalpinx intricata (Lind) Luer, foram registradas pela primeira vez para a flora brasileira, ambas encontradas no município de Santa Izabel do Rio Negro, Amazonas, Brasil.

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The development of new anti-cancer drugs of algal origin represents one of the least explored frontiers in medicinal chemistry. In this regard, the diversity of micro- and macroalgae found in Brazilian coastal waters can be viewed as a largely untapped natural resource. In this report, we describe a comparative study on the cytotoxic properties of extracts obtained from the Laurencia complex: Laurencia aldingensis, L. catarinensis, L. dendroidea, L. intricata, L. translucida, L. sp, and Palisada flagellifera. All of these species were collected in the coastal waters of the State of Espírito Santo, Brazil. Four out of the twelve samples initially investigated were found to show significant levels of toxicity towards a model tumor cell line (human uterine sarcoma, MES-SA). The highest levels of cytotoxicity were typically associated with non-polar (hexane) algal extracts, while the lowest levels of cytotoxicity were found with the corresponding polar (methanol) extracts. In this report, we also describe a biological model currently in development that will not only facilitate the search for new anti-cancer drug candidates of algal origin, but also permit the identification of compounds capable of inducing the destruction of multi-drug resistant tumors with greater efficiency than the pharmaceuticals currently in clinical use.

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Four species of marine benthic algae (Laurencia filiformis, L. intricata, Gracilaria domingensis and G. birdiae) that belong to the phylum Rhodophyta were collected in Espirito Santo State, Brazil and investigated concerning their biochemical composition (fatty acid, total lipid, soluble proteins, amino acid and ash). The total content of lipid (% dry weight) ranged from 1.1% to 6.2%: fatty acid from 0.7% to 1.0%: soluble protein from 4.6% to 18.3%, amino acid from 6.7% to 11.3% and ash from 22.5% to 38.4%. judging from their composition, the four species of algae appear to be potential sources of dietary proteins, amino acids, lipids and essential fatty acids for humans and animals. (C) 2009 Elsevier Ltd. All rights reserved.

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The purpose of this experiment was to characterize the species of Eimeria affecting lambs and their infection pattern. Faecal samples were collected from each animal at 14-day intervals, beginning when lambs were 2 weeks old and ending when they were 32 weeks old. The oocysts were counted and identified as E. intricata, E. parva, E. pallida, E. crandallis, E. bakuensis, E. weybridgensis, E. ahsata and E. ovinoidalis. The highest oocyst counts were observed when the lambs were 4-8 weeks old.

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The present study aimed to identify Eimeria species in young and adult sheep raised under intensive and / or semi-intensive systems of a herd from Umuarama city, Parana State, Brazil using the traditional diagnostic methods and to correlate the infection level/types of infection in the different age/system in this herd. Fecal samples were collected from the rectum of 210 sheep and were subjected to laboratory analysis to differentiate the species. Furthermore, animals were observed to determine the occurrences of the clinical or subclinical forms of eimeriosis. Out of the 210 collected fecal samples, 147 (70%) were positive for Eimeria oocysts, and 101 (47.86%) belonged to young animals that were raised under intensive and / or semi-intensive farming systems. Oocysts from 9 species of Eimeria parasites were identified in the sheep at the following prevalence rates: E. crandallis, 50.0%; E. parva, 21.6%; E. faurei, 8.1%; E. ahsata, 8.1%; E. intricata, 5.4%; E. granulosa, 2.7%; E. ovinoidalis, 2.0%; E. ovina, 1.3%; and E. bakuensis, 0.6%. There were no differences regarding the more frequent Eimeria species among the different ages of animals or between the different farming management systems. Based on these data, E. crandallis was the most prevalent, followed by E. parva and E. faurei species, regardless of the age. Higher parasitism was diagnosed in the young animals that were raised in a confinement regime, and the disease found in the herd was classified as subclinical. Further studies should be conducted in this herd, to verify if the eimeriosis subclinical can cause damage especially in young animals with a high level of infection.

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We performed morphological and molecular studies of Laurencia catarinensis from the Canary Islands. This species has an entangled habit, cushion-like tuft formation, cortical cell walls, slightly to markedly projecting near the apex, and lacking lenticular thickenings in medullary cells. We inferred its phylogenetic position by analyzing the chloroplast-encoded rbcL gene sequences from 41 samples. The results demonstrate that specimens of L. catarinensis from the Canary Islands, where it is referred to as L. intricata, and those from Brazil (including specimens from the type locality in Santa Catarina) form a monophyletic clade with low genetic divergence (0-0.9%). In contrast, specimens of L. intricata from the type locality in Cuba, Mexico, and the USA were clearly distinct from L. catarinensis collected in Brazil and the Canary Islands, as shown by high genetic divergence values (4.9-5.7%). The type material of L. catarinensis from Brazil allowed us to identify all samples from the Canarian Archipelago as L. catarinensis. These findings expand the known geographical distribution of L. catarinensis to the eastern Atlantic Ocean and demonstrate an amphi-Atlantic distribution of the species.

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Il progetto si sviluppa nell’area dell’ex Eridania di Forlì, un’area molto vasta, adiacente al centro storico e come tema della Tesi abbiamo deciso di studiare un progetto che potesse contenere funzioni pubbliche a disposizione di tutti i cittadini. Ci è sembrato interessante ragionare sull’area in questi termini poiché dagli studi effettuati è risultato che la città di Forlì è priva di un polo culturale compatto che possa costituire un punto di ritrovo per i forlivesi. Nelle nostre intenzioni gli spazi progettati dovranno ospitare attività espositive, concerti, spettacoli all’aperto, rappresentazioni teatrali, conferenze e laboratori artistici che coinvolgano tutte le fasce d’età. Importante per noi era portare all’interno di quest’area dismessa nuove funzioni culturali di cui Forlì è oggi carente. Dall’analisi svolta sulla città è emerso che gli spazi esistenti dedicati ad attività per lo spettacolo non sono sufficienti a soddisfare le esigenze dei cittadini sia a livello quantitativo che di assortimento. Abbiamo perciò deciso di inserire nel progetto auditorium, teatro, teatro all’aperto, laboratori artistici, zone espositive, attività annesse come uffici per l’amministrazione, biglietterie, info point e un grande parco. La prima problematica che abbiamo cercato di risolvere è stata quella dell’attraversamento della ferrovia e, più in particolare, di un collegamento con il centro storico della città e con lo sviluppo di Forlì in generale che l’ha sempre vista come un limite invalicabile. Il problema è stato affrontato ipotizzando la realizzazione di un edificio su via Vittorio Veneto adibito a commercio e terziario dal quale, attraverso un ponte che oltrepassa la ferrovia, si giunge a un edificio, all’interno dell’area, che ospita i servizi di risalita, alcuni uffici e un bar. La scelta è stata quella di non porci ortogonalmente agli edifici affacciati su questa importante arteria ma di legarci all’intero progetto che segue l’orientamento dettato dalle preesistenze. All’interno dell’area spicca per dimensioni il corpo principale dell’ex Eridania che, conserviamo eliminando le superfetazioni e intervenendo per la messa in sicurezza e per permetterne l’adeguata fruibilità. La scelta di riordinare il prospetto Nord di questo edificio nasce dalla volontà di realizzare una grande corte sulla quale si affacciassero tutti gli edifici ad esclusione dei vecchi magazzini che ne risultano racchiusi all’interno e del teatro all’aperto che rimane immerso nel verde. Per definire questa corte abbiamo pensato a un porticato che proseguisse, seguendone l’aspetto, le dimensioni e il ritmo dei pilastri, quello già esistente a lato dell’edificio conservato dell’ex zuccherificio e che fungesse da percorso coperto per raggiungere i diversi laboratori artistici che si innestano su questo. A chiudere il quarto lato della corte sono il teatro e l’auditorium, simmetrici rispetto all’asse del progetto che è dato dalle vasche originariamente usate per il lavaggio delle barbabietole, allineate con l’edificio principale dell’ex zuccherificio. Per rendere la direzione ancora più evidente decidiamo di proseguirla con un tratto d’acqua diretto verso il teatro all’aperto, conclusione della stessa. Gli edifici di progetto sono immersi in un grande parco caratterizzato dalla vegetazione già esistente nell’area, cresciuta durante l’abbandono della stessa. Così facendo manteniamo delle zone che possono definirsi boschive, dove la vegetazione è molto fitta e intricata, e altre invece più libere dagli alberi e quindi utilizzabili per altre funzioni ricreative. Un diverso trattamento è riservato alla zona di parco racchiusa tra i due percorsi rettilinei e simmetrici che collegano il teatro all’aperto alla piazza: qui si è preferito eliminare la vegetazione esistente ricavando un grande prato libero definito da filari di alberi opportunamente disposti per focalizzare l’attenzione sul teatro stesso.

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At Ocean Drilling Program (ODP) Leg 189 Sites 1170-1172, the climatologically critical Eocene-Oligocene (E-O) transition is barren of any calcareous microfossils but contains rich marine organic walled dinoflagellate cyst (dinocyst) and diatom assemblages, suitable for detailed biostratigraphic and paleoenvironmental analysis. The resulting first-ever integrated dinocyst/diatom magnetostratigraphy allows confident correlation of the E-O interval between all Leg 189 sites, including Site 1168. Our correlations indicate that the (deep) opening of the Tasmanian Gateway occurred quasi-synchronously throughout the Tasmanian region, starting at ~35.5 Ma. At Sites 1170-1172, quantitatively, three distinct dinocyst assemblages may be distinguished that reflect the relatively rapid and pronounced stepwise environmental changes associated with the E-O transition in the Tasmanian region, from a pro-deltaic setting to a deep marine pelagic setting. Moreover, synchronous with the deepening of the gateway, at the southern and eastern Sites 1170-1172, typical endemic Antarctic assemblages were replaced by more cosmopolitan dinocyst communities. In marked contrast, at Site 1168 off western Tasmania, endemic Antarctic taxa are virtually absent during the E-O transition. At Sites 1170-1172, the endemic Antarctic dinocyst assemblage (Transantarctic Flora) drastically changes into a more cosmopolitan assemblage at ~35.5 Ma, with a more offshore character, reflecting the arrival of different oceanographic and environmental conditions associated with the deepening of the Tasmanian Gateway. In turn, this assemblage grades at ~34 Ma into one more typical for even more offshore and/or upwelling conditions at Site 1172. In slightly younger deposits at all sites, organic microfossils are virtually absent, reflecting winnowing and oxidation, indicative of a next step of oceanographic development. This phase may be dated as close to the Oceanic Anoxic (Oi)-1 18O (Antarctic glaciation) event (~33.3 Ma). In a single productive sample from the earliest Oligocene the northern Site 1172, a relatively warm-water cosmopolitan assemblage has been recovered. This aspect contrasts findings from coeval deposits from the Ross Sea, where endemic Antarctic species remain dominant. Somewhere between the paleogeographic positions of Site 1172 and the Ross Sea, a strong differentiation of surface waters occurred in the earliest Oligocene, possibly reflecting the onset of the Antarctic Circumpolar Current.

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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.

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The influence of orbital precession on early Paleogene climate and ocean circulation patterns in the southeast Pacific region is investigated by combining environmental analyses of cyclic Middle Eocene sediments and palynomorph records recovered from ODP Hole 1172A on the East Tasman Plateau with climate model simulations. Integration of results indicates that in the marine realm, direct effects of precessional forcing are not pronounced, although increased precipitation/runoff could have enhanced dinoflagellate cyst production. On the southeast Australian continent, the most pronounced effects of precessional forcing were fluctuations in summer precipitation and temperature on the Antarctic Margin. These fluctuations resulted in vegetational changes, most notably in the distribution of Nothofagus (subgenus Brassospora). The climate model results suggest significant fluctuations in sea ice in the Ross Sea, notably during Austral summers. This is consistent with the influx of Antarctic heterotrophic dinoflagellates in the early part of the studied record. The data demonstrate a strong precessionally driven climate variability and thus support the concept that precessional forcing could have played a role in early Antarctic glaciation via changes in runoff and/or precipitation.