Biologia termal das tartarugas Trachemys dorbigni (Duméril & Bibron, 1835) e Trachemys scripta elegans (Wied, 1839) dos lagos de Porto Alegre, RS, Brasil (Testudines, Emydidae)

Nos lagos artificiais dos parques de Porto Alegre, pode-se observar um número muito grande de tartarugas, tanto a nativa Trachemys dorbigni quanto a norte-americana Trachemys scripta elegans estando abundantemente presentes nos mesmos. Este trabalho realizou-se nos lagos do Parque Moinhos de Vento e Jardim Botânico com o objetivo de se obter dados a respeito do comportamento de assoalhamento, interações agressivas realizadas durante esta atividade e biologia termal desses quelônios. Nessas coletas, os exemplares foram marcados, suas temperaturas cloacais registradas e dados morfométricos foram medidos. Realizou-se amostragens no período de setembro de 2003 a outubro de 2004, com coletas de dados para comportamento de assoalhamento e biologia termal ocorrendo quinzenalmente em ambos lagos. As amostragens a respeito das interações agressivas ocorreram durante quatro dias por estação do ano somente no Parque Moinhos de Vento. O padrão de comportamento de assoalhamento encontrado para ambas as espécies foi basicamente do tipo unimodal simétrico para os dois locais de coleta, sendo T. scripta elegans a espécie que ocupou previamente os locais disponíveis para esta atividade. As temperaturas corpóreas de ambas espécies coletadas dentro d’água, foram altamente relacionadas com a temperatura da água, enquanto indivíduos coletados em assoalhamento, apresentaram temperaturas cloacais mais relacionadas com as temperaturas do substrato que estava sendo utilizado, do que com as temperaturas do ar. Foi obtida uma taxa de 2,3 interações agressivas por hora observada, considerando-se esta atividade como bastante freqüente entre as espécies observadas. T. scripta elegans demonstrou-se mais agressiva que T. dorbigni causando, assim, uma interferência no comportamento de assoalhamento da mesma, e apresentando um perfil muito semelhante às características termorregulatórias que possui em seu hábitat natural.

Análise da dieta de Trachemys dorbigni (duméril & Bibron, 1835) no sul do Rio Grande do Sul (Testudines : Emydidae)

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DINÂMICAS MERCANTIS COLONIAIS : Capitania do Rio Grande do Norte (1760-1821)

The size and dynamics of the market producer, consumer and exporter of the Captaincy of Rio Grande do Norte, in the period between 1760 and 1821 is the primary goal of this dissertation. In order to establish relations between the founding of new towns built from 1750 and its incorporation into the water supply and domestic market, showing more specifically the colonial economic relations established between the coast and the hinterland of the Province. Based on references by authors such as Edward Shils and Immanuel Wallerstein have investigated topics such as formation of colonial space, deployment-action of colonial institutions regarding business practices, and the dynamic market of the Province of Rio Grande do Norte.

Larval stages of Paradasygyius depressus (Bell, 1835) (Crustacea : Decapoda : Brachyura : Majidae) and a phylogenetic analysis for 21 genera of Majidae

All larval stages and the first crab instar of Paradasygyius depressus (Bell) were obtained in laboratory culture. Larval development consists of two zoeal stages, followed by the megalopa. Each larval stage is described in detail. Beginning with the first zoea, the duration of each stage was 4--7 (4.5 +/- 0.7), 4-5 (4.5 +/- 0.5), and 7 days, the megalopa and first crab instar appearing 11 +/- 1 and 15 days after hatching, respectively. A phylogenetic analysis of 21 genera of Majidae is provided based on 34 zoeal and three megalopal characters. The phylogenetic analysis resulted in four equally parsimonious trees 173 steps long (CI = 0.66, RI = 0.71, and RC = 0.47) supporting the monophyly of Oregoniinae, Majinae, and Inachinae (with the exclusion of Macrocheira de Haan incertae sedis). Based on general agreement of sister-group hypotheses, we provide sets of larval characters that define Oregoniinae, Majinae, and Inachinae. Our phylogenetic hypothesis suggests that Oregoniinae is the most basal clade within the Majidae, and Majinae and the clade (Epialtus H. Milne Edwards + Inachinae [excluding Macrocheira incertae sedis]) are sister taxa. Within Inachinae, all trees suggest that Inachus Weber and Macropodia Leach are sister taxa nested as the most derived clade, followed by Achaeus Leach, Pyromaia Stimpson, Paradasygyius Garth, Anasimus A. Milne-Edwards, and the most basal Stenorhynchus Lamarck. The sister-group relationships of the clade (Pisa Leach (Taliepus A. Milne-Edwards + Libinia Leach)), Mithrax Latreille and Microphrys H. Milne Edwards remained unresolved.

Reproductive biology of the Brazilian sharpnose shark (Rhizoprionodon lalandii) from southeastern Brazil

The reproductive biology of the Brazilian sharpnose shark, Rhizoprionodon lalandii, off southeastern Brazil was investigated using data from gillnet landings. The size-at-maturity for males and females was estimated to be 59 and 62 cm total length (LT), respectively. Ovarian fecundity ranged from 3 to 7 follicles (mean = 4.S4), and uterine fecundity from 1 to S embryos (mean = 3.3). There was a slight positive relationship between female LT and the number of ovarian follicles, but uterine fecundity was not related to female LT. Embryonic growth is fast following fertilization during summer and autumn. Gestation requires 11 - 12 months, and peak parturition is between August and September. A comparison of size-at-maturity between animals from northeastern and southeastern Brazil suggests the existence of at least two stocks of R. lalandii along the Brazilian coast.

A case study of the 9 August 1988 South Atlantic storm: Numerical simulations of the wave activity

During 9-11 August 1988, a cyclone developed over Uruguay in the lee of the Andes Mountains and moved over the South Atlantic Ocean, where it redeveloped into an intense storm. This storm was responsible for unusual wave activity along the Brazilian shoreline from 22° to 32°S. The Brazilian news media reported the loss of at least one life, waves of 3 m and higher, and the disappearance of a drainage pipe, which weighed 8000 kg, off the shores of Rio de Janeiro. In this paper, the evolution of this intense storm and the associated ocean wave response is studied through European Centre for Medium-Range Weather Forecasts analyses, a hydrostatic limited-area meteorological model, and a second-generation prognostic wave model. The atmospheric model results indicated the presence of a long-lived and large fetch with surface wind velocities higher than 12 m s -1 directed toward the coast. Some areas with velocities of 20 m s -1 were embedded in the fetch. The wave model forced by this wind field was able to simulate waves with a significant height of 8 m far from the coast and about 4 m in regions very close to the Brazilian coast in agreement with the occurrence reported at Rio de Janeiro. The swell propagation toward the coast of Rio de Janeiro was obstructed by a northeastward 10-m wind during the first 24-h period of the model's integration. During the second 24-h period, the fetch was still large and strong, but the obstacle was removed by a counterclockwise rotation of wind direction favoring the swell and windsea propagation toward the Rio de Janeiro coast.