Culicidae (Diptera) em área de barragem em Santa Catarina e no Rio Grande do Sul

The Culicidae composition of the Barra Grande Lake Situated between the Municipalities of Esmeralda (Rio Grande do Sul State) and Anita Garibaldi (Santa Catarina State) was assessed by monthly samplings. Twenty-four species were identified from a total of 1, 185 specimens (74.7% as adults and 25.3% as immatures), with Aedes fluviatilis Lutz as the most frequent species. Several species are new records, and some of them are of public health interest. It is suggested that local environmental changes may alter the relationship between humans and vector mosquitoes.

Estudos taxonômicos e anatômicos em Mayacaceae kunth

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Levantamento de larvas de Cullicidae (Diptera) em diferentes criadouros no município de Santa Bárbara D'Oeste, SP

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Lacaziose (doença de Jorge Lobo): revisão e atualização

Lacaziose ou doença de Jorge Lobo é micose crônica, granulomatosa, causada por implantação traumática do fungo Lacazia loboi – patógeno não cultivável até o presente – nos tecidos cutâneo e subcutâneo, manifestando-se clinicamente por lesões nodulares queloidianas predominantes, envolvendo sobretudo pavilhões auriculares, face, membros superiores e inferiores, e não comprometendo as mucosas. A maioria dos casos humanos está registrada em países da América do Sul. Entretanto, a enfermidade apresenta aspectos epidemiológicos destacados, como o aparecimento em tribo Caiabi, no Brasil Central e em mamíferos não humanos, golfinhos de duas espécies (Tursiops truncatus e Sotalia guianensis) capturados na costa da Flórida (EUA), na foz do rio Suriname, na costa de Santa Catarina (Brasil), no golfo de Gasconha (baía de Biscaia-Europa), com manifestações cutâneas e achados histopatológicos muito similares às encontradas no homem. O artigo objetiva abordar características do fungo e sua taxonomia, e aspectos históricos, ecoepidemiológicos, clínicos, imuno-histoquímicos, histopatológicos, ultra-estruturais e terapêuticos.

Entomological surveillance, spatial distribution, and diversity of culicidae (diptera) immatures in a rural area of the atlantic forest biome, state of sao paulo, brazil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Disentangling social networks from spatiotemporal dynamics: the temporal structure of a dolphin society

Social networks are static illustrations of dynamic societies, within which social interactions are constantly changing. Fundamental sources of variation include ranging behaviour and temporal demographic changes. Spatiotemporal dynamics can favour or limit opportunities for individuals to interact, and then a network may not essentially represent social processes. We examined whether a social network can embed such nonsocial effects in its topology, whereby emerging modules depict spatially or temporally segregated individuals. To this end, we applied a combination of spatial, temporal and demographic analyses to a long-term study of the association patterns of Guiana dolphins, Sotalia guianensis. We found that association patterns are organized into a modular social network. Space use was unlikely to reflect these modules, since dolphins' ranging behaviour clearly overlapped. However, a temporal demographic turnover, caused by the exit/entrance of individuals (most likely emigration/immigration), defined three modules of associations occurring at different times. Although this factor could mask real social processes, we identified the temporal scale that allowed us to account for these demographic effects. By looking within this turnover period (32 months), we assessed fission-fusion dynamics of the poorly known social organization of Guiana dolphins. We highlight that spatiotemporal dynamics can strongly influence the structure of social networks. Our findings show that hypothetical social units can emerge due to the temporal opportunities for individuals to interact. Therefore, a thorough search for a satisfactory spatiotemporal scale that removes such nonsocial noise is critical when analysing a social system. (C) 2012 The Association for the Study of Animal Behaviour. Published by Elsevier Ltd. All rights reserved.

Identifizierung, Expression und Charakterisierung des Nanos-verwandten Proteins aus dem marinen Schwamm Suberites domuncula

Im Rahmen dieser Arbeit konnte in dem marinen Schwamm Suberites domuncula ein Gen identifiziert werden, dessen C-terminale konservierte Domäne eine hohe Sequenzähnlichkeit zu den Zinkfingerdomänen der Nanos-Proteine aufweist. Weiter konnte ein N-terminales Sequenzmotiv identifiziert werden, das eine hohe Sequenzidentität zu den konservierten NIM Motiven (CNOT1-interagierendes-Motiv) von Nanos zeigt. Nach der Klonierung der cDNA erfolgte die Expression des als Sd_nrp bezeichneten Proteins in E. coli Bakterien, für dessen 231 Aminosäuren umfassende Polypeptidkette eine theoretische Molekülmasse von 25.8 kDa berechnet wurde. Anschließend gelang ein Nachweis des Proteins mithilfe eines polyklonalen, gegen Sd_nrp gerichteten Antikörpers in drei Gewebetypen, dem Pinacoderm, den Primmorphen (3D-Zellaggregate) und den Gemmulae (Dauerstadien der Schwämme). Dabei konnte die höchste Expression von Sd_nrp in den als totipotent geltenden Stammzellen der Schwämme, den Archaeocyten innerhalb der Gemmulae beobachtet werden. Die Identifizierung der Zellstrukturen, erfolgte dabei aufgrund morphologischer Vergleiche. Speziell die Merkmale der Zellen in den Gemmulae, der große Nukleus, die amöboide Form sowie die granulären Reservesubstanzen, entsprechen den typischen morphologischen Eigenschaften der Archaeocyten, und bestätigen die Interpretation der Ergebnisse. Weiter konnte mit Hilfe des Anti-Sd_nrp Antikörpers das native Protein in Proteinextrakten aus Gewebe adulter Tiere nachgewiesen werden. Die vergleichende Sequenzanalyse von Sd_nrp mit dem Nanos-verwandten Protein der Schwammspezies Ephydatia fluviatilis und die phylogenetische Stammbaum-Analyse mit Nanos-Homologen unterschiedlicher Invertebraten und Vertebraten lässt die Schlussfolgerung zu, dass es sich bei dem hier identifizierten Protein Sd_nrp um ein Nanos-verwandtes Protein handelt. Darüber hinaus konnte anhand eines Homologiemodells bestätigt werden, dass es sich bei der konservierten C-terminalen Domäne des Proteins Sd_nrp um die für Nanos-Proteine spezifische Zinkfingerstruktur mit dem konservierten Sequenzmotiv CCHC handelt. Dieses Ergebnis konnte auch bei einem Vergleich der Zinkfingerdomäne von Sd_nrp mit den Zinkfingerdomänen der Nanos-Homologen unterschiedlicher Invertebraten- und Vertebratenspezies bestätigt werden.

Pollen and macroremains from three sediment cores from Göttingen, Germany

In a borehole in the southern outskirts of the town of Göttingen, limnic sediments of several Pleistocene warm periods occur intercalated with coarse solifluction debris and gravel of the river Leine. Pollen analysis of the limnic sediments in a borehole at Ottostrasse gave evidence of three warm periods of interglacial character, followed by three interstadial phases. The warm phases are separated one from another by stadial phases with, at least in one case, indications of periglacial solifluction. This sequence belongs to the Brunhes magnetic epoch. The pollen data allow to exclude an Eemian or Holsteinian age of the warm period sediments. Thus a Cromerian age is assumed, though the exact position of the newly described warm periods within the ''Cromerian'' remains uncertain. A section in a borehole at Akazienweg is of Holsteinian age.

Pollen record from Muggesfelder See and Plussee in Germany

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.

Pollen and macrofossils profiles and age determination from the Pittsburg Basin in the lowlands of south-central Illinois

Pollen and macrofossil evidence for the nature of the vegetation during glacial and interglacial periods in the regions south of the Wisconsinan ice margin is still very scarce. Modern opinions concerning these problems are therefore predominantly derived from geological evidence only or are extrapolated from pollen studies of late Wisconsinan deposits. Now for the first time pollen and macrofossil analyses are available from south-central Illinois covering the Holocene, the entire Wisconsinan, and most probably also Sangamonian and late Illinoian time. The cores studied came from three lakes, which originated as kettle holes in glacial drift of Illinoian age near Vandalia, Fayette County. The Wisconsinan ice sheet approached the sites from the the north to within about 60 km distance only. One of the profiles (Pittsburg Basin) probably reaches back to the late Illinoian (zone 1), which was characterized by forests with much Picea. Zone 2, most likely of Sangamonian age, represents a period of species-rich deciduous forests, which must have been similar to the ones that thrive today south and southeast of the prairie peninsula. During the entire Wisconsinan (14C dates ranging from 38,000 to 21,000 BP) thermophilous deciduous trees like Quercus, Carya, and Ulmus occurred in the region, although temporarily accompanied by tree genera with a more northerly modern distribution, such as Picea, which entered and then left south-central Illinois during the Woodfordian. Thus it is evident that arctic climatic conditions did not prevail in the lowlands of south-central Illinois (about 38°30' lat) during the Wisconsinan, even at the time of the maximum glaciation, the Woodfordian. The Wisconsinan was, however, not a period of continuous forest. The pollen assemblages of zone 3 (Altonian) indicate prairie with stands of trees, and in zone 4 the relatively abundant Artemisia pollen indicates the existence of open vegetation and stands of deciduous trees, Picea, and Pinus. True tundra may have existed north of the sites, but if so its pollen rain apparently is marked by pollen from nearby stands of trees. After the disappearance of Pinus and Picea at about 14,000 BP (estimated!), there developed a mosaic of prairies and stands of Quercus, Carya, and other deciduous tree genera (zone 5). This type of vegetation persisted until it was destroyed by cultivation during the 19th and 20th century. Major vegetational changes are not indicated in the pollen diagram for the late Wisconsinan and the Holocene. The dating of zones 1 and 2 is problematical because the sediments are beyond the14C range and because of the lack of stratigraphic evidence. The zones dated as Illinoian and Sangamonian could also represent just a Wisconsinan stadial and interstadial. This possibility, however, seems to be contradicted by the late glacial and interglacial character of the forest vegetation of that time.