Anchoviella hildebrandi n. sp. Engraulídeo do rio Paraguaçú: Bahia

Trata o presente trabalho da descrição de Anchoviella hildebrandi n. sp., Engraulídeo da região de Caxoeira, rio Paraguaçú, na Bahia. A espécie é muito próxima de Anchoviella brasiliensis HILDEBRAND, do rio Ribeira de Iguapé (E. de S. Paulo) e de Anchoviella jamesi (JORDAN & SEALE) , do rio Jutai e lago Aleixo (E. do Amazonas). O autor apresenta a diagnose da nova especie, confrontando os caracteres que Ihe sao peculiares com os das duas especies ácima citadas. A denominacáo dada á nova especie constitue modesta homenagem á memoria do Dr. SAMUE L F. HILDEBRAND, ictiólogo do U. S. Fish & Wildlife Service, de Washington.

The Rondonian-San Ignacio Province in the SW Amazonian Craton: An overview

The Rondonian-San Ignacio Province (1.56-1.30 Ga) is a composite orogen created through successive accretion of arcs, ocean basin closure and final oblique microcontinent-continent collision. The effects of the collision are well preserved mostly in the Paragua Terrane (Bolivia and Mato Grosso regions) and in the Alto Guapore Belt and the Rio Negro-Juruena Province (Rondonia region), considering that the province was affected by later collision-related deformation and metamorphism during the Sunsas Orogeny (1.25-1.00 Ga). The Rondonian-San Ignacio Province comprises: (1) the Jauru Terrane (1.78-1.42 Ga) that hosts Paleoproterozoic basement (1.78-1.72 Ga), and the Cachoeirinha (1.56-1.52 Ga) and the Santa Helena (1.48-1.42 Ga) accretionary orogens, both developed in an Andean-type magmatic arc; (2) the Paragua Terrane (1.74-1.32 Ga) that hosts pre-San Ignacio units (>1640 Ma: Chiquitania Gneiss Complex, San Ignacio Schist Group and Lomas Manechis Granulitic Complex) and the Pensamiento Granitoid Complex (1.37-1.34 Ga) developed in an Andean-type magmatic arc; (3) the Rio Alegre Terrane (1.51-1.38 Ga) that includes units generated in a mid-ocean ridge and an intra-oceanic magmatic arc environments; and (4) the Alto Guapore Belt (<1.42-1.34 Ga) that hosts units developed in passive marginal basin and intra-oceanic arc settings. The collisional stage (1.34-1.32 Ga) is characterized by deformation, high-grade metamorphism, and partial melting during the metamorphic peak, which affected primarily the Chiquitania Gneiss Complex and Lomas Manechis Granulitic Complex in the Paragua Terrane, and the Colorado Complex and the Nova Mamore Metamorphic Suite in the Alto Guapore Belt. The Paragua Block is here considered as a crustal fragment probably displaced from its Rio Negro-Juruena crustal counterpart between 1.50 and 1.40 Ga. This period is characterized by extensive A-type and intra-plate granite magmatism represented by the Rio Crespo Intrusive Suite (ca. 1.50 Ga), Santo Antonio Intrusive Suite (1.40-1.36 Ga), and the Teotonio Intrusive Suite (1.38 Ga). Magmatism of these types also occur at the end of the Rondonian-San Ignacio Orogeny, and are represented by the Alto Candeias Intrusive Suite (1.34-1.36 Ga), and the Sao Lourenco-Caripunas Intrusive Suite (1.31-1.30 Ga). The cratonization of the province occurred between 1.30 and 1.25 Ga. (C) 2009 Elsevier Ltd. All rights reserved.

A review of the tectonic evolution of the Sunsas belt, SW Amazonian Craton

The Sunsas-Aguapei province (1.20-0.95 Ga), SW Amazonian Craton, is a key area to study the heterogeneous effects of collisional events with Laurentia, which shows evidence of the Grenvillian and Sunsas orogens. The Sunsas orogen, characterized by an allochthonous collisional-type belt (1.11-1.00 Ga), is the youngest and southwestern most of the events recorded along the cratonic fringe. Its evolution occurred after a period of long quiescence and erosion of the already cratonized provinces (>1.30 Ga), that led to sedimentation of the Sunsas and Vibosi groups in a passive margin setting. The passive margin stage was roughly contemporary with intraplate tectonics that produced the Nova Brasilandia proto-oceanic basin (<1.21 Ga), the reactivation of the Ji-Parana shear zone network (1.18-1.12 Ga) and a system of aborted rifts that evolved to the Huanchaca-Aguapei basin (1.17-1.15 Ga). The Sunsas belt is comprised by the metamorphosed Sunsas and Vibosi sequences, the Rincon del Tigre mafic-ultramafic sill and granitic intrusive suites. The latter rocks yield epsilon(Nd(t)) signatures (-0.5 to -4.5) and geochemistry (S,1, A-types) suggesting their origin associated with a continental arc setting. The Sunsas belt evolution is marked by ""tectonic fronts"" with sinistral offsets that was active from c. 1.08 to 1.05 Ga, along the southern edge of the Paragua microcontinent where K/Ar ages (1.27-1.34 Ga) and the Huanchaca-Aguapei flat-lying cover attest to the earliest tectonic stability at the time of the orogen. The Sunsas dynamics is coeval with inboard crustal shortening, transpression and magmatism in the Nova Brasilandia belt (1.13-1.00 Ga). Conversely, the Aguapei aulacogen (0.96-0.91 Ga) and nearby shear zones (0.93-0.91 Ga) are the late tectonic offshoots over the cratonic margin. The post-tectonic to anorogenic stages took place after ca. 1.00 Ga, evidenced by the occurrences of intra-plate A-type granites, pegmatites, mafic dikes and sills, as well as of graben basins. Integrated interpretation of the available data related to the Sunsas orogen supports the idea that the main nucleus of Rodinia incorporated the terrains forming the SW corner of Amazonia and most of the Grenvillian margin, as a result of two independent collisional events, as indicated in the Amazon region by the Ji-Parana shear zone event and the Sunsas belt, respectively. (C) 2009 Elsevier Ltd. All rights reserved.

The Rondonian-San Ignacio Province in the SW Amazonian Craton: An overview

The Rondonian-San Ignacio Province (1.56-1.30 Ga) is a composite orogen created through successive accretion of arcs, ocean basin closure and final oblique microcontinent-continent collision. The effects of the collision are well preserved mostly in the Paragua Terrane (Bolivia and Mato Grosso regions) and in the Alto Guapore Belt and the Rio Negro-Juruena Province (Rondonia region), considering that the province was affected by later collision-related deformation and metamorphism during the Sunsas Orogeny (1.25-1.00 Ga). The Rondonian-San Ignacio Province comprises: (1) the Jauru Terrane (1.78-1.42 Ga) that hosts Paleoproterozoic basement (1.78-1.72 Ga), and the Cachoeirinha (1.56-1.52 Ga) and the Santa Helena (1.48-1.42 Ga) accretionary orogens, both developed in an Andean-type magmatic arc; (2) the Paragua Terrane (1.74-1.32 Ga) that hosts pre-San Ignacio units (>1640 Ma: Chiquitania Gneiss Complex, San Ignacio Schist Group and Lomas Manechis Granulitic Complex) and the Pensamiento Granitoid Complex (1.37-1.34 Ga) developed in an Andean-type magmatic arc; (3) the Rio Alegre Terrane (1.51-1.38 Ga) that includes units generated in a mid-ocean ridge and an intra-oceanic magmatic arc environments; and (4) the Alto Guapore Belt (<1.42-1.34 Ga) that hosts units developed in passive marginal basin and intra-oceanic arc settings. The collisional stage (1.34-1.32 Ga) is characterized by deformation, high-grade metamorphism, and partial melting during the metamorphic peak, which affected primarily the Chiquitania Gneiss Complex and Lomas Manechis Granulitic Complex in the Paragua Terrane, and the Colorado Complex and the Nova Mamore Metamorphic Suite in the Alto Guapore Belt. The Paragua Block is here considered as a crustal fragment probably displaced from its Rio Negro-Juruena crustal counterpart between 1.50 and 1.40 Ga. This period is characterized by extensive A-type and intra-plate granite magmatism represented by the Rio Crespo Intrusive Suite (ca. 1.50 Ga), Santo Antonio Intrusive Suite (1.40-1.36 Ga), and the Teotonio Intrusive Suite (1.38 Ga). Magmatism of these types also occur at the end of the Rondonian-San Ignacio Orogeny, and are represented by the Alto Candeias Intrusive Suite (1.34-1.36 Ga), and the Sao Lourenco-Caripunas Intrusive Suite (1.31-1.30 Ga). The cratonization of the province occurred between 1.30 and 1.25 Ga. (C) 2009 Elsevier Ltd. All rights reserved.

Diversidade morfológica, genética e química de populações naturais de Anemopaegma arvense (Vell.) Stellf

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Los espacios portuarios : Un lugar de encuentro entre disciplinas

Tabla de contenidos: "Las villas nuevas" cantábricas en el marco de su primitiva organización territorial : Valles, alfoques, solares y linajes en los enclaves portuarios del litoral marítimo del reino de Castilla entre los siglos XII al XIV / Osvaldo Víctor Pereyra. El puerto Gaditano en el Inico del Ocaso de la Época Colonial [1810-1812] / Luis López Molina. Reflexiones sobre la incidencia del puerto en la vida de la ciudad de Montevideo / Arturo Ariel Bentancur. Los cargadores de cuero del Complejo Portuario Rioplatense / Maximiliano Camarda. El consulado de Buenos Aires y el quiebre de la Monarquía : Los préstamos y contribuciones de los comerciantes, 1808-1816 / Javier Kraselsky. Comercio, orden y derechos de propiedad de un puerto alternativo del Río de La Plata : La boca del Río Salado ebtre dos bloqueos [1838-1848] / Antonio Galarza. Entre el viento y el humo : Embarcaciones, puertos y tripulantes en la provincia de Buenos Aires en los primeros censos nacionales [1869-1914] / José Mateo, José Luis Nogueira. La cuestión del Muelle Nacional y reactivación de Arroyo Pareja / Gustavo Chalier. Génesis y desarrollo de la pesquería de camarón en el puerto de Mazatlán, 1949-1958 : El empresario como centro del engranaje productivo / Ulises Suárez Estavillo. Puertos y embarcaderos en la "Carrera de Paragua" (Siglo XVIII) / Isabel Paredes. La reactivación de los puertos del río Paraná en el discurso del desarrollismo antifrigerista, 1958-1976 / Miguel Angel De Marco. Redescubriendo la ruta hacia el norte : Del puerto de Buenos Aires a Potosí, en las postrimerías del siglo XVIII / María Claudia Errecart. Faenados a contravención : Decomisos de cueros en la Banda oriental durante 1784 y 1785 / Nicolás Biangardi. Fiscalidad en el Antiguo Régimen : Indagaciones en torno a la estructura fiscal del Virreinato del Río de La Plata. El caso de la Real Aduana de Buenos Aires [1776-1810] / María Evangelina Vaccani. La ruta del cacao : Circuito comercial de la élite pamplonesa, Virreinato de Nueva Granada, siglos XVIII-XIV / Lina Constanza Díaz Boada. El turismo como fenómeno económico, soail y cultural : Caso Mazatlán, México / Yasser Orlando Espinoza García, Héctor Manuel Pimienta Fernández. Delitos sexuales en el espacio portuario : Sexualidad y derecho en la encrucijada / Betina Clara Riva. La ciudad y el puerto : Transformaciones de áreas portuarias en desuso. El caso de puerto madero / Claudia Carut. Un Hada en La Boca : Imágenes post modernas de un puerto "inactivo! / Marcelo N. Weissel.