Amazon landforms and soils in relation to biological diversity

Thirteen main landform units are distinguished for the whole of the forested Amazon region, each with its specific soil pattern and vegetation structure. These landform-soil-vegetation units are delineated on a small-scale map and illustrated by a schematic cross-section. Floristic diversity of the gamma type is to be highest on the steepland-and-valley complexes of the Andean fringe, on the crystalline shield uplands, on the inselberg complexes, and on the eutric variant of the western sedimentary plains. Endemism is expected to be highest on the sandy plains, and parts of the table lands and inselberg complexes. Speciation, linked to the concept of forest refuge areas, is likely to be highest on the sandstone table lands, on the stretches of Amazon planalto, and in the areas of relict valleys, in view of the prolonged geomorphological stability of these units.

Leaf micronutrient concentrations and potential photosynthesis in Ochroma pyramidale established in a degraded land

In the Brazilian Amazon, large areas of abandoned lands may revert to secondary forest. In the process, pioneer tree species have an important role to restore productivity in old fields and improve environmental conditions. To determine potential photosynthesis (Apot), stomatal conductance (g), transpiration (E), and leaf micronutrient concentrations in Ochroma pyramidale (Cav. ex Lam.) Urban a study was carried out in the Brazilian Amazon (01o 51' S; 60o 04' W). Photosynthetic parameters were measured at increasing [CO2], saturating light intensity (1 mmol (photons) m-2 s-1), and ambient temperature. The rate of electron-transport (J), Apot,and water-use efficiency (WUE) increased consistently at increasing internal CO2 concentration (Ci). Conversely, increasing [CO2] decreased gs, E, and photorespiration (Pr). At the CO2-saturated region of the CO2 response curve (1.1 mmol (CO2) mol-1(air), J was 120 μmol (e-) m-2s-1 and Apot reached up to 24 μmol (CO2) m-2s-1. Likewise, at saturating C1 g and E were 30 and 1.4 mmol (H2O) m-2s-1, respectively, and P 2 r about 1.5 μmol (CO2) m-2s-1. Foliar nutrients were 185, 134, 50, and 10 μmol (element) m-2 (leaf area) for Fe, Mn, Zn, and Cu, respectively. It was concluded that [CO ] probably limits light saturated photosynthesis in this site. Furthermore, from a nutritional point of view, the low Fe to Cu ratio (15:1) may reflect nutritional imbalance in O. pyramidale at this site.

Diversity of the land resources in the Amazonian State of Rondônia, Brazil

Conflicting opinions are recorded in the literature concerning the suitability of Amazon lands for sustainable agriculture following deforestation. This article has been written to shed light on this question by summarizing climate, landform, soil and vegetation features from the findings of a land resource study of the Brazilian state of Rondônia in south-west Amazonia. The work, which followed the World Soils and Terrain Digital Database (SOTER) methodology, was financed by the World Bank. During the course of the survey special emphasis was given to studying soils; 2914 profiles were analyzed and recorded. The study identified a complex pattern of land units with clear differences in climate, landform, soils and native vegetation. Forested areas mosaic with lesser areas of natural savannas. The latter occur on both poorly-drained and well-drained, albeit nutrient deficient sandy soils. The tallest and most vigorous forests or their remnants were seen growing on well-drained soils formed from nutrient-rich parent materials. Many of these soils could, or are being used for productive agriculture. Soils developed on nutrient-poor parent materials support forests that are significantly lower in height, and would require large lime and fertilizer inputs for agriculture. Low forests with high palm populations and minor areas of wet land savannas cover the poorly drained soils. It is evident that forest clearing in the past was indiscriminant; this cannot be condoned. The diversity of land conditions found throughout Rondônia would suggest that many past studies in the Amazon have simply been too broad to identify significant soil differences.

Análise comparativa do consumo de biomassa para fins energéticos

Dissertação de mestrado integrado em Engenharia Mecânica

O Calcolítico e a Idade do Bronze na bacia do rio Neiva, NW de Portugal

Relatório de estágio de mestrado em Arqueologia

A importância dos espaços verdes para a promoção de Guimarães a capital verde da Europa

Relatório de estágio de mestrado em Geografia (área de especialização em Planeamento e Gestão do Território)

Dos ciclos e sistemas aos interstícios de Creixomil: entre o seu conhecimento e transformação potencial

Dissertação de mestrado integrado em Arquitectura (área de especialização em Território)

Bijdragen tot de flora van Nederlandsch Indië /uitgegeven door C.L. Blume.

1825-26 pt. 1-6

Bijdragen tot de flora van Nederlandsch Indië /uitgegeven door C.L. Blume.

1825-26 pt. 7-12

Bijdragen tot de flora van Nederlandsch Indië /uitgegeven door C.L. Blume.

1825-26 pt. 13-17

Dispersión agrícola y cambio social en las Sierras de Córdoba (ca. 1000 a C.- 1600 d C.) Agricultural spread and social change in Córdoba Hills (ca. 1000 b C- 1600 a D.)

El proceso cultural en las Sierras de Córdoba fue habitualmente concebido como marginal con respecto al Noroeste Argentino. Tras el establecimiento del esquema básico de la secuencia prehispánica, a mediados del siglo pasado, se definió una etapa agroalfarera de cronología tardía, que continuaba a una extensa etapa precerámica cuyos límites se aproximaban a la transición Pleistoceno-Holoceno. Se hacía referencia, de este modo, al advenimiento de un modo de vida agrícola y aldeano, que reemplazaba a otro basado en la caza y recolección. Dicha transformación, alternativamente atribuida a la población cazadora local o a una migración de grupos agricultores desde regiones vecinas, se habría consumado hacia 1500 AP, fijando uno de los límites de la dispersión de la agricultura andina. Es necesario destacar la extremada escasez y el carácter indirecto de las evidencias arqueológicas utilizadas para sustentar la ocurrencia de tal proceso. Asimismo, la vigencia de supuestos que han comenzado a mostrar inconsistencias con los resultados de las recientes investigaciones. Entre ellos, principalmente, el que asume que la introducción de la agricultura dio paso a una transformación radical de las sociedades prehispánicas, constituyendo un hito fundamental en su devenir histórico, el comienzo de una nueva etapa. Nuestros últimos estudios en el sector central de las Sierras de Córdoba apuntaron, entre otros objetivos, a reconocer indicadores arqueológicos directos de producción agrícola, así como de la manipulación y consumo de plantas cultivadas. Los primeros resultados nos permiten vislumbrar un escenario complejo que desafía los modelos vigentes. El consumo de maíz, por ejemplo, parece haber antecedido por muchos siglos a la adopción de prácticas agrícolas. El acceso a este cultígeno, sumado a otros elementos, indicaría cambios entre los cazadores-recolectores serranos, promovidos por su integración en redes macrorregionales que los vincularon con sociedades agricultoras de la vertiente oriental andina y quizás del Chaco Santiagueño, por lo menos desde 2500 AP. En definitiva, la agricultura no parece haber sido adoptada rápidamente ni provocado transformaciones profundas e inmediatas en la organización de los grupos prehispánicos. Se ha observado, por el contrario, la incorporación gradual de distintas innovaciones que incluso permiten relacionar la manipulación y más tarde el cultivo de plantas domesticadas, con procesos de intensificación productiva de mayor escala temporal. Uno de nuestros objetivos en este proyecto consiste, básicamente, en profundizar las investigaciones en curso a fin de ampliar el cuerpo de datos con el cual analizar y discutir el problema de la dispersión agrícola en la región. Ello implica el tratamiento de diferentes líneas de evidencia, en particular: 1) la distribución regional de sitios arqueológicos y las modalidades de ocupación de las tierras cultivables; 2) la búsqueda de superficies de cultivo en sitios estratificados; y 3) estudios arqueobotánicos, polínicos y de isótopos estables. Se entiende que no le corresponde a la arqueología asumir apriorísticamente el significado histórico de la introducción de la agricultura, sino establecerlo en cada caso puntual a través de la investigación concreta. Nuestro segundo objetivo consiste, por lo tanto, en delinear los cambios (económicos, tecnológicos, políticos, sociales) que acompañaron al proceso de dispersión agrícola. Ello implica el tratamiento de diferentes problemas, entre otros: 1) las prácticas de apropiación de los recursos silvestres; 2) la continuidad y cambio tecnológico; 3) la movilidad y la articulación microambiental; y 4) los aspectos políticos y sociales ligados a prácticas como la molienda grupal y la producción del arte rupestre. The radical chage of societies from hunter-gatherers to farmers in 1500 BP was considered a milestone whitin the cultural process of pre-hispanic societies in Cordoba Hill. But there is a shortage of archaeological remains to support this change and there are weak hypotheses of absolute transformations. During the last years, our studies carried out on the central area of Cordoba Hill have tried to recognize direct archaeological signs of agriculture production as well as the handling and consumption of crops. The first results show a complex set that challenges the current theoretical models. For example, the corn was probably eatten prior to its adoption for farm practices. Our first main consists in increasing a corpus of data about the spread of agriculture in Cordoba region that we have been researching for the last years. These researches involve different lines of evidence: 1-regional location of archaeological sites and kinds of occupation on cultivable lands; 2-the search for plots at archaeological sites; 3-archaeobotanical, pollen and stable isotopes studies. Our second main consists in outlining changes within the spread of agriculture. It implies to considering different problems: 1-the practices to gatherer wild resources; 2-the continuity and changes of technologies; 3-the mobility and the articulation on the micro-environment; 4-political and social aspects in connection with activities such as groupal grinding and rock art productions.

Distribuição geográfica da fauna e flora da Baía de Guanabara

The author studied, the horizontal and vertical distribution of most common part of the flora and fauna of the bay of Guanabara at Rio de Janeiro. In this paper the eulittoral, poly, meso and oligohaline regions were localised and studied; and the first chart of its distribution was presented (fig. 2). The salinity of superficial waters was established through determinations based on 30 trips inside the buy for collecting biological materials. Some often 409 determinations which were previous reported together with the present ones served for the eleboration of a salinity map of the bay of Guanabara (fig. 1). This map of fig. 2 shows the geographic locations of the water regions. EULITTORAL WATER REGIME — Fig. 3 shows the diagram scheme of fauna and flora of this regime. Sea water salinity 34/1.000, density mean 1.027, transparent greenish waters, sea coast with moderate bursting waves. Limpid sea shore with white sand, gneiss with the big barnacle Tetraclita squamosa var. stalactifera (Lam. Pilsbry. Vertical distributions: barna¬cles layers with a green region in which are present the oyster Ostrea pa-rasitica L., the barnacles Tetraclita, Chthamalus, Balanus tintinnabulum var. tintinnabulum (L.) e var. antillensis Pilsbry in connection with several mollusca and the sea beatle Isopoda Lygia sp. Covered by water and exposed to air by the tidal ritms, there is a stratum of brown animals that is the layer of mussels Mytilus perna L., with others brown and chestnut animals : the Crustacea Pachygrapsus, the little crab Porcellana sp., the stone crab Me-nippe nodifrons Stimpson, the sea stars Echinaster brasiliensis (Mull. & Tr.), Astropecten sp. and the sea anemones Actinia sp. Underneath and never visible there is a subtidal region with green tubular algae of genus Codium and amidst its bunches the sea urchin Lycthchinus variegatus (Agass.) walks and more deeply there are numerous sand-dollars Encope emarginata (Leske). The microplancton of this regime is Ceratiumplancton. POLYHALINE WATER REGIMB — Water almost sea water, but directly influenced by continental lands, with rock salts dissolved and in suspension. Salinity: 33 to 32/1.000. This waters endure the actions of the popular nicknamed «water of the hill» (as the waters of mesohaline and oligohaline regimes), becoming suddenly reddish during several hours. That pheno¬menon returns several times in the year and come with great mortality of fishes. In these waters, according to Dr. J. G. FARIA there are species of Protozoa : Peridinea, the Glenoidinium trochoideum St., followed by its satellites which he thinks that they are able to secret toxical substances which can slaughter some species of fishes. In these «waters of the hill» was found a species of Copepoda the Charlesia darwini. In August 1946 the west shore of the Guanabara was plenty of killed fishes occupying a area of 8 feet large by 3 nautical miles of lenght. The enclosure for catching fishes in the rivers mouthes presents in these periods mass dead fishes. The phenomenon of «waters of the hill» appears with the first rains after a period of long dryness. MESOHALINE WATER REGIME — Fig. 4 shows the the diagramm scheme. Salt or brackish water from 30 to 17/1.000 salinity, sometimes until 10/1.000. Turbid waters with mud in suspension, chestnut, claveyous waters; shore dirty black mud without waving bursting; the waters are warmer and shorner than those of the polihaline regime. Mangrove shore with the mangrove trees : Rhizophora mangle L., Avicennia sp., Laguncularia sp., and the »cotton tree of sea» Hibiscus sp. Fauna: the great land crab «guaimú» Cardisoma guanhumi Latr., ashore in dry firm land. There is the real land crab Ucides cordatus (L.) in wetting mud and in neigh¬ bourhood of the burrows of the fiddler-crabs of genus Uca. On stones and in the roots of the Rhizophora inhabits the brightly colored mangrove-tree-crab («aratu» Portuguese nickname) Goniopsis cruentata (Latreille) and the sparingly the big oyster Ostrea rhizophorae Guild. Lower is the region of barnacles Balanus amphitrite var. communis Darwin and var. niveus Darwin; Balanus tintinnabulum var. tintinnabulum (L.) doesn't grow in this brackish water; lower is the region of Pelecipoda with prepollency of Venus and Cytherea shell-fishes and the Panopeus mud crab; there are the sea lettuce Ulva and the Gastreropod Cerithium. The Paguridae Clibanarius which lives in the empty shells of Gasteropod molluscs, and the sessile ascidians Tethium plicatum (Lesuer) appears in some seasons. In the bottom there is a black argillous mud where the «one landed shrimps» Alpheus sp. is hidden. OLIGOHALINE WATER REGIME — The salinity is lower than 10/1.000. average 8/1.000. There are no barnacles and no sea-beetles Isopods of genus Lygia; on the hay of the shore there are several graminea. This brackish water pervades by mouthes of rivers and penetrates until about 3 kilometers river above. While there is some salt dissolved in water, there are some mud crabs of the genus Uca, Sesarma, Metasesarma and Chasmagnatus. The presence of floating green plants coming from the rivers in the waters of a region indicated the oligohaline waters, with low salt content because when the average of NaCl increases above 8/1.000 these plants die and become rusty colored.

Contribuição para o conhecimento das doenças do grupo tifo exantemático no Brasil

In this work, the author considers that in Brazil, there exist three forms of the disease of the Exanthematic Typhus group, that have been well studied: Neotropic Exanthematic Typhus, Murine Typhus and "Q" fever. The first of these forms has existed in this country, perhaps, for over five hundred years. He says that modern antibiotic, Aureomycin, Chloromycetin and, principally, Terramcin have resolved the problem of the therapeutic treatment of the disease. The modern insecticides, D. D. T., Gammexane and Toxafeno have resolved the prophylactic problem. The author studies minutely the question of denomination, showing, by means of drawing and history, the origin of the diseases, both Norte American and Brazilian. The name Neotropic Exanthematic Typhus (in BRazil, Colombia, United States or India) should substitute the erroneous anme "Spotted Fever"; the disease is exanthematic, a very different thing. He formulates two hypotheses about these diseases: first - it passed from the neotropic to the neartic region, where it acquired individual properties; second - they developed independently in a more rmeote epoch, acquiring each its own characteristics. The disease is today rather of the neotropic than of the neartic region. As it also exists in India it cannot be named American exanthematic Typhus. The author finds it unnecessary to change the name to "Rikettsioses"; we do not call bacillar dysentery "Schigeloses"or malignant edema "Chlostridiose". The name exanthematic typhus is classic, precise, scientific, expressive and the denomination "neotropical" completes the localisation. The author thinks that all the diseases of the exanthematic typhus group, in the world had a simple primitive common origin. At first, the rickettsias or the virus had a free life, perhaps in the waters of the marshes or grass-lands. Later, in the struggle for life, came the parasitism of the plants. They became fitoparatifs. The mode of life...

The Greying Church: The Impact of Life Expectancy on Religiosity

Many churches are concerned about older and dwindling congregations. We develop a theoretical framework to explain not only the downward trend in church attendance, but also the increase in the proportion of older people in the congregations. Religiosity depends positively on the expected social and spiritual benefits attached to religious adherence, as well as the probability of entering heaven in the afterlife. While otherworldly compensation in terms of salvation and spiritual benefits motivates religiosity, the costs of formal religion in terms of time allocated to communal activities and foregone income work in the opposite direction. We show that higher life expectancy discounts expected benefits in the afterlife and is hence likely to lead to postponement of religiosity. For this reason, religious organizations should be prepared to attract older members to their congregations, while emphasizing contemporaneous religious benefits to increase overall church attendance.

La reconversion du quartier Gare/Crêt-Taconnet à Neuchâtel: réflexions sur la densification qualifiée

La reconversion des friches industrielles des secteurs de gare est prometteuse dans l'optique d'un développement urbain dense alternatif à l'étalement. Elles constituent en effet une réserve foncière centrale et bien desservie par les transports publics. La densification de ces terrains stratégiques ne pourra cependant freiner l'étalement urbain qu'à condition d'offrir un cadre de vie attractif pour l'habitat. Notre hypothèse est que l'engagement des pouvoirs publics est déterminant pour assurer cette densification qualifiée. Brown fields regeneration in railway station areas is particularly promising in the perspective of a compact urban development alternative to sprawl. They indeed constitute a central land stock which is well connected to public transportation networks. However, the densification of these strategic lands will make it possible to moderate urban sprawl only by providing an attractive environment for residential activities. Our hypothesis is that public authorities involvement is decisive to ensure such a qualified densification. Die Umnutzung von Industriebrachen in Bahnhofsarealen scheint viel versprechend im Hinblick auf eine Stadtentwicklung nach innen als Alternative zur Ausbreitung. Zentralgelegen, stellen diese ungenutzten Flächen eine strategische Bodenreserve dar, welche gut an das öffentliche Verkehrsmittelnetz angeschlossen ist. Ihre Verdichtung kann jedoch die Stadtausbreitung nur eindämmen unter der Bedingung, einen attraktiven Lebens- und Wohnraum zu bieten. Unsere Hypothese lautet, dass das Ausmass des Engagements der öffentlichen Hand bestimmend ist um diese qualitative Verdichtung sicherzustellen.