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

Citric acid production by Y. lipolytica W29 from crude glycerol: strain improvement by mutagenesis

[Excerpt] Citric acid, an important and versatile organic acid extensively used in several industries, is originally produced by Aspergillus niger in submerged fermentation from molasses [1]. However, Yarrowia lipolytica have been studied and demonstrate a great potential as citric acid producer from several carbon sources [1–5] including crude glycerol, a low cost byproduct from the biodiesel industry [6]. The simultaneous production of the isomer isocitric acid is the major problem in using this yeast in the citric acid production. (...)

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.

Reproductive biology of Hyla goiana (Anura, Hylidae)

Male-male and male-female interactions, reproductive habitat, and vocalizations of Hyla goiana B. Lutz, 1968 a member of H. polytaenia species group, are described. Three groups of calling males were surveyed along a small stream, at the Estação de Pesquisa e Desenvolvimento Ambiental de Galheiro, Perdizes municipality, State of Minas Gerais, Brazil. The mean distance between the nearest calling neighbors was 2.7 m, in accordance with an uniform distribution. Clutches (mean 180 eggs) were deposited in the stream, submerged and attached to plants. In two observed courtships the female moved towards a calling male that rapidly clasped her. In the male-male interaction, the males emitted advertisement and encounter calls and then engaged in physical combat. The males have a prepollical fang-like spine on each hand and several of them were observed with scratches on dorsum. The advertisement call consists of alternating harsh notes and a trilled of brief notes. The frequency of the call is lower than that of H. aff. polytaenia and H. cipoensis B. Lutz, 1968. The clutch characteristics of H. goiana are similar to those described for H. polytaenia Cope, 1870 and H. cipoensis.

Seasonal variation of the effect of high-carbohydrate and high-protein diets on the intermediate metabolism of Parastacus brasiliensis (Crustacea, Decapoda, Parastacidae) maintained in the laboratory

The goal of this study was to evaluate the effect of a high-carbohydrate diet (HC) and a high-protein diet (HP) on the metabolism of the crayfish Parastacus brasiliensis (Von Martens, 1869), collected in different seasons and maintained in the laboratory for 15 days. Crayfish were collected monthly from January 2002 to January 2004 at São Francisco de Paula, Southern Brazil, in Guarapirá stream. In the laboratory, the animals were kept submerged in aquariums under controlled conditions. They were fed ad libitum, for 15 days with either a HC or HP diet. At the end of this period, haemolymph samples were collected, as were hepatopancreas, gills, and abdominal muscle that were removed for determination of glycogen, free glucose, lipids, and triglycerides. The haemolymph samples were used for determination of glucose, proteins, lipids, and triglycerides. Statistical analysis (ANOVA) revealed significant seasonal differences in biochemical composition in crayfish maintained on HC or HP diets. Independent of the diets offered to the animals and the controlled conditions for 15 days, the indications of seasonality were unchanged. The observed changes seemed to be related to the reproductive period. Moreover, the HC diet increased all energy reserves in adult parastacids, which may aid in reproduction.

Macroinvertebrates under stochastic hydrological disturbance in Cerrado streams of Central Brazil

In the Cerrado vegetation, where the seasonal is well defined, rainfall has an important role in controlling the flow of streams and consequently on the structure of macroinvertebrates community. Despite the effects of rainfall associated with seasonality are well studied, little is known about the effects of stochastic rains on the community. In the present study we evaluated the structure and faunal composition of four first-order streams in Central Brazil during the dry season in two years, with and without stochastic rains. Community sampling was done by colonization of boards of high density polyethylene (HDPE), removed after one month submerged in streams. Analysis of Variance (ANOVA) performed indicated no difference in rarefied richness between the two periods, different from numeric density of organisms that was higher in the period without disturbance; moreover, the Detrended Correspondence Analysis (DCA) revealed differences in faunal composition between the two periods. Our results indicate that stochastic rainfall is an important factor in structuring the macroinvertebrates community in studied region.

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...