Helminofauna da sarda (Scomber scombrus L. ) peixe da Costa Continental Portuguesa

Dos primerios 80 espécimens da sarda examinados (de janeiro a maio de 1982), apenas seis (7,5%) estavam livres de helmintos, apresentando os demais as espécies de parasitos seguintes, por ordem de freqüência dentro de cada grupo taxonômico: Kuhnia scombri (Kuhn, 1829) e Grubea cochlear (Diesing, 1858) (classe Monogenea); Lecithocladium excisum (Rudolph, 1819) e Opechona basillaris (Molin, 1859)(classe Digenea); pelrocercoides de Lacistrorhynchus tenuis (Beneden, 1858) de Scolex pleuronectis (Muller, 1788) e de Echeneibothrium sp. (classe Cestoda); Rhadinorhynchus tenuicornis (Linton, 1891) (filo Acanthocephala); formas dos tipos larvares Anisakis e Contracaecum e ainda, larvas de Goezia sp. (classe Nematoda). São referidas, pela primeira vez, neste hospedeiro, formas larvares do cestóide Echeneibothrium sp. e do nematóide Goezia sp.

Padrões distributivos e zoogeografia dos moluscos da plataforma continental brasileira: Parte III. Comissão Oceanográfica Espiríto Santo I

One hundred senventy-five species of marine mollusks have been identified in the Expedition Espírito Santo I. Standing out the species Margarites olivaceus (Brown, 1827); Cyclostremiscus caraboboensis Weishord, 1962; Balcis gibba Folin, 1867; Triphora compsa (Dall, 1927); Henrya af. goldmani Bartsh, 1947 and Limaea subovata Jeffreys, 1876 as they have not been previously assigned to Brazil. The analysis of the geographical distribution patterns points out the dominance of the species with thermophiles affinities. This situation evidences the importance of the Brazilian Current in the maintanance of the biogeographical structure of the studied region. However, it is the analysis of the cryophiles species that shows the Cabo Frio region as an ecological filter quite more permeable to the species with thermophile affinities than to the cryophiles ones. The existence of this barrier and the endemism rate (4.27%) characterize the region that extends from the south of Cabo Frio as a transition between the two patterns cited above. Therefore they do not corroborate in malacological parameters the proposition made by Palacio (1982) for the individualization of the Paulista Province.

The Budget 2009 Tax Proposals and Activity in the UK Continental Shelf (UKCS)

NORTH SEA STUDY OCCASIONAL PAPER No. 113

Taxation and Total Government Take from the UK Continental Shelf (UKCS) Following Phase 3 of the European Emissions Trading Scheme (EU ETS)

NORTH SEA STUDY OCCASIONAL PAPER No. 117

Economic Principles and Determination of Infrastructure Third Party Tariffs in the UK Continental Shelf (UKCS)

NORTH SEA STUDY OCCASIONAL PAPER No. 116

The Effects of Budget 2011 on Activity in the UK Continental Shelf

NORTH SEA STUDY OCCASIONAL PAPER No. 120

The Long Term Prospects for Activity in the UK Continental Shelf

NORTH SEA STUDY OCCASIONAL PAPER No. 119

A Futuristic Least-cost Optimisation Model of CO2 Transportation and Storage in the UK/UK Continental Shelf

NORTH SEA STUDY OCCASIONAL PAPER No. 112

The Prospects for Activity in the UK Continental Shelf to 2040: the 2009 Perspective

NORTH SEA STUDY OCCASIONAL PAPER No. 114

The Effects of the European Emissions Trading Scheme (EU ETS) on Activity in the UK Continental Shelf (UKCS) and CO2 Leakage

NORTH SEA STUDY OCCASIONAL PAPER No. 115

Bimodal magmatism as a consequence of the post-collisional readjustment of the thickened Variscan continental lithosphere (Aiguilles Rouges - Mont Blanc Massifs, Western Alps)

High Precision U-Pb zircon and monazite dating in the Aiguilles Rouges-Mont Blanc area allowed discrimination of three short-lived bimodal magmatic pulses: the early 332 Ma Mg-K Pormenaz monzonite and associated 331 Ma peraluminous Montees Pelissier monzogranite; the 307 Ma cordierite-bearing peraluminous Vallorcine and Fully intrusions; and the 303 Fe-K Mont Blanc syenogranite. All intruded syntectonically along major-scale transcurrent faults at a time when the substratum was experiencing tectonic exhumation, active erosion recorded in detrital basins and isothermal decompression melting dated at 327-320 Ma. Mantle activity and magma mixing are evidenced in all plutons by coeval mafic enclaves, stocks and synplutonic dykes. Both crustal and mantle sources evolve through time, pointing to an increasingly warm continental crust and juvenile asthenospheric mantle sources. This overall tectono-magmatic evolution is interpreted in a scenario of post-collisional restoration to normal size of a thickened continental lithosphere. The latter re-equilibrates through delamination and/or erosion of its mantle root and tectonic exhumation/erosion in an overall extensional regime. Extension is related to either gravitational collapse or back-are extension of a distant subduction zone.