Erythrina velutina willd. (Leguminosae-Papilionoideae) ocorrente em caatinga e brejo de altitude de Pernambuco: biometria, embebição e germinação

O objetivo deste trabalho foi comparar a biometria de frutos e sementes, a embebição e germinação de duas populações de Erythrina velutina coletadas na região semiárida do Estado de Pernambuco, nas áreas de caatinga (Alagoinha) e no brejo de altitude (Poção). Os frutos e as sementes foram avaliados quanto ao comprimento, largura, espessura (cm) e peso (g). Com relação às sementes, foram analisados o número por fruto, o volume (cm³) e a embebição, bem como a germinação com e sem escarificação mecânica, na presença constante de luz a 25 ºC. Os frutos e sementes do brejo apresentaram os valores assim discriminados: 9,65 x 1,57 x 1,22 cm, 1,43 g e 1,34 x 0,92 x 0,78 cm, 0,46 g; e na caatinga: 6,85 x 1,19 x 1,03 cm, 0,21 g e 1,06 x 0,63 x 0,63 cm e 0,26 g. O número de sementes e o volume no brejo e caatinga foram de 2,33 e 1,38 cm³ e 1,40 e 0,23 cm³, respectivamente. Todas as sementes escarificadas apresentaram maiores valores de embebição e porcentagem de germinação. Quanto à velocidade de germinação, foi maior na caatinga. Esses resultados indicam que as condições ambientais do brejo de altitude favorecem o desenvolvimento dos frutos e das sementes.

Composição florística em trechos de vegetação de caatinga e brejo de altitude na região do Vale do Pajeú, Pernambuco

(Composição florística em trechos de vegetação de caatinga e brejo de altitude na região do Vale do Pajeú, Pernambuco). Realizou-se um levantamento florístico em quatro áreas do vale do Pajeú, objetivando caracterizar a composição florística da vegetação ocorrente nas altitudes de 1100, 900, 700 e 500 m, em áreas dos municípios de Triunfo e Serra Talhada, PE. No período de setembro de 1991 a março de 1993 foram coletadas 159 espécies lenhosas. distribuídas em 45 famílias. As famílias com maior número de espécies na cota de 1100 m foram Myrtaceae (9), Flacourtiaceae e Rubiaceae (6); na cota de 900 m, foram Asteraceae, Myrtaceae e Mimosaceae (6); na de 700 m, Euphorbiaceae (6), Mimosaceae (4), Caesalpiniaceae e Anacardiaceae (3); e na de 500 m, Mimosaceae, Euphorbiaceae (7) e Caesalpiniaceae (4). Entre as quatro áreas, houve maior semelhança florística de 1100 com 900 m e de 700 com 500 m. A área de maior altitude, 1100 m, é ocupada por uma vegetação de brejo de altitude; as áreas de menores altitudes, 700 e 500 m, caracterizam-se como áreas de caatinga; enquanto a de 900 m apresenta predominantemente elementos de brejo, associados a outros de caatinga.

O que são campos rupestres e campos de altitude nos topos de montanha do leste do Brasil?

(O que são campos rupestres e campos de altitude nos topos de montanha do Leste do Brasil?). Os campos rupestres e os campos de altitude do leste do Brasil ocorrem nas partes mais elevadas da Cadeia do Espinhaço, da Serra da Mantiqueira e da Serra do Mar. Uma vez que há certa confusão sobre a caracterização e os limites geográficos destes dois tipos de vegetação, o objetivo deste trabalho é apresentar uma síntese das opiniões sobre tais ambientes campestres, discutindo sobre a história de suas denominações, localização geográfica, aspectos fisionômicos e afinidades biogeográficas. Embora os campos rupestres e os campos de altitude apresentem certas semelhanças fisionômicas e compartilhem alguns táxons vegetais, ambos os tipos de vegetação devem ser considerados distintos.

Biochemical and physiological characteristics of actinomycetes isolated from high altitude shola soils of tropical Montane forest

Actinomycetes are gram-positive, free-living, saprophytic bacteria widely distributed in soil, water and colonizing plants showing marked chemical and morphological diversity. They are potential source of many bioactive compounds, which have diverse clinical effects and important applications in human medicine. In the present work, we have studied some of the physiological and biochemical characteristics of 36 actinomycete strains isolated from the shola soils of tropical montane forest; a relatively unexplored biodiversity hotspot. Ability of actinomycetes isolates to ferment and produce acids from various carbohydrate sources such as innositol, mannose, sorbitol, galactose, mannitol, xylose, rhamnose, arabinose, lactose and fructose were studied. Almost all the carbon compounds were utilized by one or other actinomycete isolates. The most preferred carbon sources were found to be xylose (94.44%) followed by fructose and mannose (91.66%). Only 41.76% of the isolates were able to ferment lactose. The ability of actinomycetes isolates to decompose protein and amino acid differ considerably. 72.22% of the isolates were able to decompose milk protein casein and 61.11% of the isolates decompose tyrosine. Only 8.33% of the strains were able to decompose amino acid hypoxanthine and none of them were able to decompose amino acid xanthine. Potential of the actinomycetes isolates to reduce esculin, urea and hippurate and to resist lysozyme was also checked. 91.66% of the isolates showed ability to decompose esculin and 63.88% of the isolates had the capacity to produce urease and to decompose urea. Only 25% of the isolate were able to decompose hippurate and 94.44% showed lysozyme resistance

SPATIOTEMPORAL VARIATION AND ANTIBACTERIAL ACTIVITY OF ACTINOMYCETES ISOLATED FROM HIGH ALTITUDE GRASSLAND SOILS OF TROPICAL MONTANE FOREST – KERALA, INDIA

TThe invention of novel antibiotics and other bioactive microbial metabolites continues to be an important aim in new drug discovery programmes. Actinomycetes have the potential to synthesize lots of diverse biologically vigorous secondary metabolites and in the last decades actinomycetes became the most productive source for antibiotics. Therefore in the present study we analyze the antibacterial activity of the actinomycetes isolated from grassland soil samples of Tropical Montane forest. A total of 33 actinomycete strains isolated were characterized and screened for antibacterial activities using well diffusion method against six specific pathogenic organisms. Identification of the isolates revealed that the majority of them were belonging to Streptomycetes followed by Nocardia, Micromonospora, Pseudonocardia, Streptosporangium, Nocardiopsis and Saccharomonospora. Among the 33 isolates, Gr1 strain showed antagonistic activity against all checked pathogens. Nine strains showed antibacaterial activity against Listeria, Vibrio cholera, Bacillus cereus, Staphylococcus aureus and Salmonella typhi and only 2 strains (Gr1and Gr25) showed antagonism to E. coli. The overall percentage of activity of actinomycetes isolates against each pathogenic bacterium was also calculated. While 63.63% of the actinomycetes were antagoinistic against Listeria, Vibrio cholerae, and Bacillus cereus, 60.6% of them were antagonistic to Staphylococcus aureus. Very few isolates (6.06%) showed antibacterial activity against E. coli. In general most of the actinomycetes isolates were antagonistic to grampositive bacteria such as Listeria, Bacillus and Staphylococcus than Gram-negative bacteria Vibrio cholerae, E. coli and Salmonella

Low-altitude aerial photography for optimum N fertilization of winter wheat on the North China Plain

Previous research has shown that site-specific nitrogen (N) fertilizer recommendations based on an assessment of a soil’s N supply (mineral N testing) and the crop’s N status (sap nitrate analysis) can help to decrease excessive N inputs for winter wheat on the North China Plain. However, the costs to derive such recommendations based on multiple sampling of a single field hamper the use of this approach at the on-farm level. In this study low-altitude aerial true-color photographs were used to examine the relationship between image-derived reflectance values and soil–plant data in an on-station experiment. Treatments comprised a conventional N treatment (typical farmers’ practice), an optimum N treatment (N application based on soil–plant testing) and six treatments without N (one to six cropping seasons without any N fertilizer input). Normalized intensities of the red, green and blue color bands on the photographs were highly correlated with total N concentrations, SPAD readings and stem sap nitrate of winter wheat. The results indicate the potential of aerial photography to determine in combination with on site soil–plant testing the optimum N fertilizer rate for larger fields and to thereby decrease the costs for N need assessments.

The biometeorology of high-altitude insect layers.

Flight at high altitude is part of a migration strategy that maximises insect population displacement. This thesis represents the first substantial analysis of insect migration and layering in Europe. Vertical-looking entomological radar has revealed specific characteristics of high-altitude flight: in particular layering (where a large proportion of the migrating insects are concentrated in a narrow altitude band). The meteorological mechanisms underpinning the formation of these layers are the focus of this thesis. Aerial netting samples and radar data revealed four distinct periods of high-altitude insect migration: dawn, daytime, dusk, and night-time. The most frequently observed nocturnal profiles during the summertime were layers. It is hypothesised that nocturnal layers initiate at a critical altitude (200–500 m above ground level) and time (20:00–22:00 hours UTC). Case study analysis, statistical analysis, and a Lagrangian trajectory model showed that nocturnal insect layers probably result from the insects’ response to meteorological conditions. Temperature was the variable most correlated with nocturnal insect layer presence and intensity because insects are poikilothermic, and temperatures experienced during high-altitude migration in temperate climates are expected to be marginal for many insects’ flight. Hierarchical effects were detected such that other variables—specifically wind speed—were only correlated with insect layer presence and intensity once temperatures were warm. The trajectory model developed comprised: (i) insect flight characteristics; (ii) turbulent winds (which cause vertical spread of the layer); and (iii) mean wind speed, which normally leads to horizontal displacements of hundreds of kilometres in a single migratory flight. This thesis has revealed that there is considerable migratory activity over the UK in the summer months, and a range of fascinating phenomena can be observed (including layers). The UK has moved from one of the least studied to perhaps the best studied environments of aerial insect migration and layering in the world.

Flight periodicity and the vertical distribution of high-altitude moth migration over southern Britain

The continuous operation of insect-monitoring radars in the UK has permitted, for the first time, the characterization of various phenomena associated with high-altitude migration of large insects over this part of northern Europe. Previous studies have taken a case-study approach, concentrating on a small number of nights of particular interest. Here, combining data from two radars, and from an extensive suction- and light-trapping network, we have undertaken a more systematic, longer-term study of diel flight periodicity and vertical distribution of macro-insects in the atmosphere. Firstly, we identify general features of insect abundance and stratification, occurring during the 24-hour cycle, which emerge from four years’ aggregated radar data for the summer months in southern Britain. These features include mass emigrations at dusk and to a lesser extent at dawn, and daytime concentrations associated with thermal convection. We then focus our attention on the well-defined layers of large nocturnal migrants that form in the early evening, usually at heights of 200–500 m above ground. We present evidence from both radar and trap data that these nocturnal layers are composed mainly of noctuid moths, with species such as Noctua pronuba, Autographa gamma, Agrotis exclamationis, A. segetum, Xestia c-nigrum and Phlogophora meticulosa predominating.

Layers of nocturnal insect migrants at high-altitude: the influence of atmospheric conditions on their formation

1 Radar studies of nocturnal insect migration have often found that the migrants tend to form well-defined horizontal layers at a particular altitude. 2 In previous short-term studies, nocturnal layers were usually observed to occur at the same altitude as certain meteorological features, most notably at the altitudes of temperature inversions or nocturnal wind jets. 3 Statistical analyses are presented of four years’ data that compared the presence, sharpness and duration of nocturnal layer profiles (observed using continuously-operating entomological radar) with meteorological variables at typical layer altitudes over the UK. 4 Analysis of these large datasets demonstrated that temperature was the foremost meteorological factor persistently associated with the presence and formation of longer-lasting and sharper layers of migrating insects over southern UK.