Agroforestry in the Amazon Basin: practice, theory and limits of a promising land use

Includes bibliography

Port planning parameters of the Caribbean Basin

Includes bibliography

Caribbean Basin Plan or Iniciative: some comments, 30 March 1982. Summary and comments on the remarks by President Reagan about the Caribbean Basin Plan", 1 March 1982"

Resume y comenta la iniciativa o plan de ayuda del Presidente Reagan a los paises de la Cuenca del Caribe, presentado al Congreso de los Estados Unidos, como proyecto de ley. Comenta ademas el discurso pronunciado por el Presidente Reagan ante la Organizacion de Estados Americanos, en el que analizo los aspectos principales de dicho Plan.

The State and strategies for river basin management in the Andean region

Includes bibliography

Market and trade perspectives for the food and forestry sectors of Latin America in the Asia-Pacific Basin

Includes bibliography

Estudio de caso: el sistema de la cuenca del río Bogotá: resumen = Case study: the Bogota river basin: summary

Incluye Bibliografía

Tourist Cruise Ships and the Trade in Services: Recent Trends in Countries of the Caribbean Basin

This issue of the Bulletin reviews the main trends of trade in goods and services for the countries of the Association of Caribbean States (ACS) in 2004. The strong recovery of trade in goods and the robust expansion of trade in services are highlighted, emphasizing the increase in services as a proportion of total exports for the smaller Caribbean economies, which may even exceed 80%.A detailed analysis of the performance of the tourism component, especially travel, showed that in 2004 there was a boom in cruise ship arrivals, a situation which poses a real challenge for some islands in terms of ensuring a permanent flow of tourists and making use of the main comparative advantages -sun, sea and beaches- and possible linkages with the rest of the economy such as the hotel industry, restaurants, business and entertainment centres, guided excursions, transport, yachting, and others. In some islands, the ratio of cruise passengers to inhabitants is particularly high, and can reach a significant factor of about 11 tourists for every inhabitant in the Bahamas, 8 in Aruba, 7 in Antigua and Barbuda and 5 in Dominica, and around 4 for a sample of eleven countries.One of the main challenges for a number of Caribbean islands is how to capitalize on such linkages by developing sustainable tourism that minimizes the possible adverse impacts on the environment and the everyday life of the citizens.

Facies analysis of the Codó formation (Late Aptian) in the Grajaú area, Southern São Luís-Grajaú Basin

Facies descriptions of the Codó Formation in the Grajaú area are provided for the first time, and its sedimentary characteristics compared to those from the Codó area to allow paleoenvironmental reconstructions. Deposits in the Grajaú area include evaporites, limestones and argillites bearing features indicative of a shallow, low energy, subaqueous, saline environment exposed to meteoric and/or capillary conditions. Floodingevaporative concentration-desiccation cycles suggest a saline pan complex surrounded by extensive evaporitic mudflats. The location of the system, whether coastal or inland, is a matter open for debate. However, the later hypothesis is favored considering: 1. Sr isotopic data, with values higher than those expected for Late Aptian marine waters; 2. calcitic composition of limestones (instead of dolomitic and/or magnesitic as expected in coastal settings); and 3. presence of continental ostracods and lack of marine fauna. This interpretation is consistent with that proposed for UpperAptian deposits of the Codó area, but the depositional system there was one dominated by more stable, well-stratified, anoxic waters and evaporite precipitation in central lacustrine areas, while in the Grajaú area the salt pan was more oxygenated and ephemeral, with salt precipitation mainly in marginal areas or along surrounding mudflats.

Araçatuba formation: palustrine deposits from the initial sedimentation phase of the Bauru Basin

A Bacia Bauru (Cretáceo Superior), acumulou uma seqüência sedimentar continental essencialmente arenosa. Numa fase inicial desértica, o seu substrato basáltico foi soterrado por extensa e monótona cobertura de areias eólicas com intercalações subordinadas de depósitos de loesse. O relevo original do substrato favoreceu a formação de uma drenagem regional endorrêica, sob clima semi-árido, propiciando assim condições de formação do Paleopantanal Araçatuba. Os depósitos paludiais (Formação Araçatuba) constituem estratos tabulares de siltitos e arenitos de cor cinza claro esverdeado típica, eventualmente cimentados por carbonato de cálcio. Moldes e pseudomorfos de cristais de gipsita e dolomita foram identificados na unidade. Aparentemente, estão associados com gretas de ressecação, marcas de raízes e intervalos com laminação tipo climbing ripple, que indicam ambiente de águas salinas rasas e relativamente calmas, submetidas a fases de exposição subaérea e ressecação. Nos limites da área de ocorrência da Formação Araçatuba, as unidades arenosas podem exibir feições sigmóides e estratificação contorcida, comuns em depósitos deltaicos marginais. A Formação Araçatuba é contornada e posteriormente encoberta por depósitos eólicos da Formação Vale do Rio do Peixe.