618 resultados para Sponges, Dysidea Herbacea (porifera)
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Mono.6a[1] (Porifera: Spirastrella); Livr.59
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Mono.6a (Porifera: Placospongia); Livr.9
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Three species of Halichondrida, Dragmacidon reticulatus (Ridley & Dendy, 1886) (Axinellidae), Myrmekioderma rea (Laubenfels, 1934) (Desmoxyidae) and Topsentia ophiraphidites (Laubenfels, 1934) (Halichondriidae), collected from 30 to 184 m depths, were recorded for the first time from State of Maranhão, north-northeast coast of Brazilian shelf.
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n.s. no.2(1979)
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v.10:no.10(1950)
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In a recent outbreak of human ocular injuries that occurred in the town of Araguatins, at the right bank of Araguaia river, state of Tocantins, Brazil, along the low water period of 2005, two patients (8 and 12-year-old boys) presented inferior adherent leukoma in the left eye (OS), and peripherical uveites, with snowbanking in the inferior pars plana. The third one (13-year-old girl) showed posterior uveites in OS, also with snowbanking. Histopathological analysis of lensectomy material from the three patients and vitrectomy from the last one revealed several silicious spicules (gemmoscleres) of the freshwater sponges Drulia uruguayensis and D. ctenosclera. This work brings material evidences, for the first time in the literature, that freshwater sponge spicules may be a surprising new etiological agent of ocular pathology.
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Bacteria isolated from marine sponges found off the coast of Rio de Janeiro, Brazil, were screened for the production of antimicrobial substances. We report a new Pseudomonas putida strain (designated P. putida Mm3) isolated from the sponge Mycale microsigmatosa that produces a powerful antimicrobial substance active against multidrug-resistant bacteria. P. putida Mm3 was identified on the basis of 16S rRNA gene sequencing and phenotypic tests. Molecular typing for Mm3 was performed by RAPD-PCR and comparison of the results to other Pseudomonas strains. Our results contribute to the search for new antimicrobial agents, an important strategy for developing alternative therapies to treat infections caused by multidrug-resistant bacteria.
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A continuous carbon isotope curve from Middle-Upper Jurassic pelagic carbonate rocks was acquired from two sections in the southern part of the Umbria-Marche Apennines in central Italy. At the Colle Bertone section (Terni) and the Terminilletto section (Rieti), the Upper Toarcian to Bajocian Calcari e Marne a Posidonia Formation and the Aalenian to Kimmeridgian Calcari e Marne a Posidonia and Calcari Diasprigni formations were sampled, respectively. Biostratigraphy in both sections is based on rich assemblages of calcareous nannofossils and radiolarians, as well as some ammonites found in the upper Toarcian-Bajocian interval. Both sections revealed a relative minimum of delta(13)C(PDB) close to + 2 parts per thousand in the Aalenian and a maximum around 3.5 parts per thousand in early Bajocian, associated with an increase in visible chert. In basinal sections in Umbria-Marche, this interval includes the very cherry base of the Calcari Diasprigni Formation (e.g. at Valdorbia) or the chert-rich uppermost portion of the Calcari a Posidonia (e.g at Bosso). In the Terminilletto section, the Bajocian-early Barthonian interval shows a gradual decrease in delta(13)C(PDB) values and a low around 2.3 parts per thousand. This part of the section is characterised by more than 40 m of almost chart-free limestones and correlates with a recurrence of limestone-rich facies in basinal sections at Valdorbia. A double peak with values of delta(13)C(PDB) around + 3 parts per thousand was observed in the Callovian and Oxfordian, constrained by well preserved radiolarian faunas. The maxima lie in the Callovian and the middle Oxfordian, and the minimum between the two peaks should be near the Callovian/Oxfordian boundary. In the Terminilletto section, visible chert increases together with delta(13)C(PDB) values from the middle Bathonian and reaches peak values in the Callovian-Oxfordian. In basinal sections in Umbria-Marche, a sharp increase in visible chert is observed at this level within the Calcari Diasprigni. A drop of delta(13)C values towards + 2 parts per thousand occurs in the Kimmeridgian and coincides with a decrease of visible chert in outcrop. The observed delta(13)C positive anomalies during the early Bajocian and the Callovian-Oxfordian may record changes in global climate towards warmer, more humid periods characterised by increased nutrient mobilisation and increased carbon burial. High biosiliceous (radiolarians, siliceous sponges) productivity and preservation appear to coincide with the delta(13)C positive anomalies, when the production of platform carbonates was subdued and ceased in many areas, with a drastic reduction of periplatform ooze input in many Tethyan basins. The carbon and silica cycles appear to be linked through global warming and increased continental weathering. Hydrothermal events related to extensive rifting and/or accelerated oceanic spreading may be the endogenic driving force that created a perturbation of the exogenic system (excess CO2 into the atmosphere and greenhouse conditions) reflected by the positive delta(13)C shifts and biosiliceous episodes.
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Here we present a processing route to produce multi-structured ceramic foams based on the combination of particle-stabilized foams with polymeric sponges to produce positive and negative templating structures. Polyester sponges are infiltrated with freshly produced calcium aluminate alumina foams and upon sintering either positive templating structures are produced when wetting the sponges, or negative templating foams with a percolating pore network are obtained when completely filling the sponges. Additionally, by combining different layers of these particle-stabilized foam infiltrated sponges, various different structures can be produced, including sandwich structures, pore size gradients, and ceramic bone-like structures applying to different types of bone. The particle-stabilized foams used were in situ self-hardening calcium aluminate cement enriched alumina foams to obtain crack-free samples with pore interconnections and tailorable pore sizes.
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L’objectiu principal del projecte era aprofundir en el coneixement de les malalties de les esponges, centrant-nos en la diversitat bacteriana que acullen. Als estius 2008 i 2009 va haver episodis d’elevades temperatures de l’aigua de mar que van suposar importants mortalitats massives d’esponges a la Mediterrània. Contra tot pronòstic, els estius del projecte, el 2010 i el 2011, no van resultar especialment calorosos i no hi va haver episodis de mortalitat. És un fet molt positiu per les comunitats bentòniques però algun dels objectius específics de la meva proposta no es va poder dur a terme com havien estat platejats inicialment. Disposàvem de diferents mostres d’esponges malaltes de l’espècie Ircinia fasciculata, sanes i aigua circumdant recollides l’estiu 2009 i fixades per DNA, per això s’han pogut identificar i caracteritzar els canvis en la comunitat microbiològica de les esponges malaltes respecte de les sanes. Hem constatat que més que una infecció per un o pocs patògens puntuals, com havien proposat alguns autors, hi ha un canvi dràstic en la comunitat microbiològica associada a les esponges. Les esponges malaltes, on dominen els bacteris heterotròfics, presenten una major diversitat bacteriana que les sanes, on dominen els autòtrofs. Tot i que no es va poder realitzar un nou mostreig d’individus malalts, i algun objectiu específic no es va poder desenvolupar, vaig aprofitar l’estada en un centre de referència en estudis de la diversitat microbiana, per ampliar el coneixement general de les comunitats bacterianes associades a esponges. Es van realitzar nous estudis en què vam testar si totes les esponges (bacteriosponges i no) presenten simbionts reals o si les no-bacteriosponges presenten un enriquiment de les comunitats de l’aigua de mar però no una flora específica. El resultat és que totes les esponges presenten associacions molt específiques malgrat hi ha fortes diferències entre les comunitats microbianes associades a bacteriosponges i a no-bacteriosponges.