Vegetação e arquitetura das espécies de restinga associadas à ocorrência de Formicivora littoralis (Aves,Thamnophilidae)

O presente estudo teve como objetivo central conhecer a composição florística, a estrutura e a arquitetura das espécies da formação arbustiva fechada pós-praia e investigar possíveis associações com Formicivora littoralis, considerando tática de forrageamento, construção de ninhos e abundância da ave. F. littoralis é endêmica de restingas, e está ameaçada de extinção devido a perda acelerada de habitat. Entretanto, pouco se sabe sobre a vegetação em que ela ocorre, principalmente sobre as áreas de maior abundância da ave localizadas na formação Arbustiva Fechada Pós-praia (AFP) da Restinga da Massambaba, as quais estão inseridas em um Centro de Diversidade Vegetal (CDV) na Região de Cabo Frio. Diante disto, este estudo foi realizado em dois trechos desta formação na Restinga da Massambaba, nos municípios de Araruama e Arraial do Cabo, RJ, Brasil. Foram efetuadas 60 excursões a campo, com coletas aleatórias realizadas ao longo de toda a formação, geração de 20 parcelas de 2x50 m (0,2ha) perpendiculares ao mar, incluindo na amostragem indivíduos com DAP e DAS ≥2,5, estes, foram ainda categorizados em modelos de arquitetura de ramificação considerando número de ramos em dois patamares de altura (DAP e DAS). O levantamento florístico resultou em 327 coletas de 160 espécies, sendo pelo menos 12 espécies vegetais sob algum estado de ameaça, inclusive redescoberta uma Salicaceae (Casearia sessiliflora). Orchidaceae, Leguminosae e Myrtaceae foram as famílias mais ricas. Foram acrescentados 75% mais espécies na lista preliminar da AFP na Massambaba, além de 14 novos registros para o CDV de Cabo Frio. Na estrutura e arquitetura foram analisados 906 indivíduos de 58 espécies. Sendo os maiores valores de importância de Pilosocereus arrabidae (42,30) e Chrysophyllum lucentifolium (23,45). A diversidade de Shannon foi de 3,46 e equabilidade de 0,85. A arquitetura da maior parte dos indivíduos foi complexa, 58% de indivíduos com múltiplas ramificações, e as espécies apresentando variados padrões de ramificação. A densidade populacional de F. littoralis na AFP foi elevada, sendo estimada em 172 ind/km2. A arquitetura da AFP tem influência na ecologia da ave, pois ela foi generalista quanto à espécie utilizada como suporte na construção de ninhos e também para as táticas de forrageamento, mas houve seleção de ramos finos que formavam na horizontal ângulos de até 90 de abertura para construir ninhos. Ramos finos e mais horizontais também foram utilizados com frequência para as táticas de forrageamento. A abundância de F. littoralis esteve correlacionada positivamente à diversidade vegetal e negativamente à altura da vegetação, características marcantes nesta formação. Além disso, elevada taxa de vegetais com síndrome de dispersão zoocórica indica a importância desta formação na oferta de recursos alimentícios para a fauna e atração de pequenos artrópodes, os quais fazem parte da dieta de F. littoralis.

Osteologia craniana de Platalea ajaja (Linnaeus) (Aves, Ciconiiformes), comparada com outras espécies de Threskiornithidae

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

The evolutionary history of cockatoos (Aves: Psittaciformes: Cacatuidae)

Cockatoos are the distinctive family Cacatuidae, a major lineage of the order of parrots (Psittaciformes) and distributed throughout the Australasian region of the world. However, the evolutionary history of cockatoos is not well understood. We investigated the phylogeny of cockatoos based on three mitochondrial and three nuclear DNA genes obtained from 16 of 21 species of Cacatuidae. In addition, five novel mitochondrial genomes were used to estimate time of divergence and our estimates indicate Cacatuidae diverged from Psittacidae approximately 40.7 million years ago (95% CI 51.6–30.3 Ma) during the Eocene. Our data shows Cacatuidae began to diversify approximately 27.9 Ma (95% CI 38.1–18.3 Ma) during the Oligocene. The early to middle Miocene (20–10 Ma) was a significant period in the evolution of modern Australian environments and vegetation, in which a transformation from mainly mesic to xeric habitats (e.g., fire-adapted sclerophyll vegetation and grasslands) occurred. We hypothesize that this environmental transformation was a driving force behind the diversification of cockatoos. A detailed multi-locus molecular phylogeny enabled us to resolve the phylogenetic placements of the Palm Cockatoo (Probosciger aterrimus), Galah (Eolophus roseicapillus), Gang-gang Cockatoo (Callocephalon fimbriatum) and Cockatiel (Nymphicus hollandicus), which have historically been difficult to place within Cacatuidae. When the molecular evidence is analysed in concert with morphology, it is clear that many of the cockatoo species’ diagnostic phenotypic traits such as plumage colour, body size, wing shape and bill morphology have evolved in parallel or convergently across lineages.

Isolation of microsatellite loci in the Capricorn silvereye, Zosterops lateralis chlorocephalus (Aves: Zosteropidae)

The Capricorn silvereye (Zosterops lateralis chlorocephalus) is ideally suited to investigating the genetic basis of body size evolution. We have isolated and characterized a set of microsatellite markers for this species. Seven out of 11 loci were polymorphic. The number of alleles detected ranged from two to five and observed heterozygosities between 0.12 and 0.67. One locus, ZL49, was found to be sex-linked. This moderate level of diversity is consistent with that expected in an isolated, island population.

Interpretation of morphological data to inform design Bridge to Bridge: Ridge to Ridge urban design workshop

The importance of design practice informed by urban morphology has led to intensification in interest, signalled by the formation of the ISUF Research and Practice Task Force and voiced through several recent academic publications cognisant of this current debate, this paper reports on a recent urban design workshop at which morphology was set as one of the key themes. Initially planned to be programmed as a augmented concurrent event to the 2013 20th ISUF conference held in Brisbane, the two day Bridge to Bridge: Ridge to Ridge urban design workshop nevertheless took place the following month, and involved over one hundred design professionals and academics. The workshop sought to develop several key urban design principles and recommendations addressing a major government development proposal sited in the most important heritage precinct of the city. The paper will focus specifically on one of the nine groups, in which the design proposal was purposefully guided by morphological input. The discussion will examine the design outcomes and illicit review and feedback from participants, shedding critical light on the issues that arise from such a design approach.

Analysis of Ridge-Loaded Folded-Waveguide Slow-Wave Structures for Broadband Traveling-Wave Tubes

An E-plane serpentine folded-waveguide slow-wave structure with ridge loading on one of its broad walls is proposed for broadband traveling-wave tubes (TWTs) and studied using a simple quasi-transverse-electromagnetic analysis for the dispersion and interaction impedance characteristics, including the effects of the beam-hole discontinuity. The results are validated against cold test measurements, an approximate transmission-line parametric analysis, an equivalent circuit analysis, and 3-D electromagnetic modeling using CST Microwave Studio. The effect of the structure parameters on widening the bandwidth of a TWT is also studied.

Elastic thickness structure of the Andaman subduction zone: Implications for convergence of the Ninetyeast Ridge

We use the Bouguer coherence (Morlet isostatic response function) technique to compute the spatial variation of effective elastic thickness (T-e) of the Andaman subduction zone. The recovered T-e map resolves regional-scale features that correlate well with known surface structures of the subducting Indian plate and the overriding Burma plate. The major structure on the India plate, the Ninetyeast Ridge (NER), exhibits a weak mechanical strength, which is consistent with the expected signature of an oceanic ridge of hotspot origin. However, a markedly low strength (0< T-e <3 km) in that region, where the NER is close to the Andaman trench (north of 10 N), receives our main attention in this study. The subduction geometry derived from the Bouguer gravity forward modeling suggests that the NER has indented beneath the Andaman arc. We infer that the bending stresses of the viscous plate, which were reinforced within the subducting oceanic plate as a result of the partial subduction of the NER buoyant load, have reduced the lithospheric strength. The correlation, T-e < T-s (seismogenic thickness) reveals that the upper crust is actively deforming beneath the frontal arc Andaman region. The occurrence of normal-fault earthquakes in the frontal arc, low Te zone, is indicative of structural heterogeneities within the subducting plate. The fact that the NER along with its buoyant root is subducting under the Andaman region is inhibiting the subduction processes, as suggested by the changes in trench line, interrupted back-arc volcanism, variation in seismicity mechanism, slow subduction, etc. The low T-e and thinned crustal structure of the Andaman back-arc basin are attributed to a thermomechanically weakened lithosphere. The present study reveals that the ongoing back-arc spreading and strike-slip motion along the West Andaman Fault coupled with the ridge subduction exerts an important control on the frequency and magnitude of seismicity in the Andaman region. (C) 2013 Elsevier Ltd. All rights reserved.

Spatial variations of effective elastic thickness over the Ninetyeast Ridge and implications for its structure and tectonic evolution

We present new data on the strength of oceanic lithosphere along the Ninetyeast Ridge (NER) from two independent methods: spectral analysis (Bouguer coherence) using the fan wavelet transform technique, and spatial analysis (flexure inversion) with the convolution method. The two methods provide effective elastic thickness (T-e) patterns that broadly complement each other, and correlate well with known surface structures and regional-scale features. Furthermore, our study presents a new high resolution database on the Moho configuration, which obeys flexural isostasy, and exhibit regional correlations with the T-e variations. A continuous ridge structure with a much lower T-e value than that of normal oceanic lithosphere provides strong support for the hotspot theory. The derived T-e values vary over the northern (higher T-e similar to 10-20 km), central (anomalously low T-e similar to 0-5 km), and southern (low T-e similar to 5 km) segments of the NER. The lack of correlation of the T-e value with the progressive aging of the lithosphere implies differences in thermo-mechanical setting of the crust and underlying mantle in different parts of the NER, again indicating diversity in their evolution. The anomalously low T-e and deeper Moho (similar to 22 km) estimates of the central NER (between 0.5 degrees N and 17 degrees S) are attributed to the interaction of a hotspot with the Wharton spreading ridge that caused significant thermal rejuvenation and hence weakening of the lithosphere. The higher mechanical strength values in the northern NER (north of 0.5 degrees N) may support the idea of off-ridge emplacement and a relatively large plate motion at the time of volcanism. The low T-e and deeper Moho (similar to 22 km) estimates in the southern part (south of 17 degrees S) suggest that the lithosphere was weak and therefore younger at the time of volcanism, and this supports the idea that the southern NER was emplaced on the edge of the Indian plate. (C) 2013 Elsevier B.V. All rights reserved.

The 2014 M-w 6.1 Bay of Bengal, Indian Ocean, Earthquake: A Possible Association with the 85 degrees E Ridge

Oceanic intraplate earthquakes are known to occur either on active ridge-transform structures or by reactivation of their inactive counterparts, generally referred to as fossil ridges or transforms. The Indian Ocean, one of the most active oceanic intraplate regions, has generated large earthquakes associated with both these types of structures. The moderate earthquake that occurred on 21 May 2014 (M-w 6.1) in the northern Bay of Bengal followed an alternate mechanism, as it showed no clear association either with active or extinct ridge-transform structures. Its focal depth of >50 km is uncommon but not improbable, given the similar to 90 Ma age of the ocean floor with 12-km-thick overlying sediments. No tectonic features have been mapped in the near vicinity of its epicenter, the closest being the 85 degrees E ridge, located similar to 100 km to its west, hitherto regarded as seismically inactive. The few earthquakes that have occurred here in the past are clustered around its southern or northern limits, and a few are located midway, at around 10 degrees N. The 2014 earthquake, sourced close to the northern cluster, seems to be associated with a northwest-southeast-oriented fracture, located on the eastern flanks of the 85 degrees E ridge. If this causal association is possible, we believe that reactivation of fossil hotspot trails could be considered as another mechanism for oceanic intraplate seismicity.

Estudio sobre peligro aviario: Análisis del riesgo de impactos entre aves y aeronaves en el Aeropuerto Internacional Augusto C. Sandino, Managua, Nicaragua

El peligro aviario es el riesgo de coliciones entre aves y aeronaves. Para reducir ese peligro es necesario entender la naturaleza de las aves que habitan dentro y alrededor del aeropuerto y clasificarlas numericamente en base a la peligrosidad que representan, conociendo a la vez las estaciones del año, los meses del año, horas del día, condiciones climáticas, focos de atracción (cobertura, alimentación y agua) que incrementan la abundancia y la riqueza de aves en las áreas aeroportuarias. Para obtener la información se seleccionaron dos sitios de observación: uno en las áreas verdes alrededor de la pista de aterrizaje, con el objetivo de registrar las especies de aves hacen uso de este sitio permanente o temporalmente, y otro en la torre de control, para determinar rutas de aves de mayor peso, gregarias y de alto vuelo en un radio de 3000 m con centro en la torre de control. Las especies observadas con mayor frecuencia en la pista de aterrizaje fueron: Hirundo rustica, Quiscalus mexicanus, Molothrus aeneus, Columbina talpacoti y Columba livia. Desde la torre de control se observaron con mayor frecuencia: Coragyps atratus, Zenaida asiatica, Molotrus aeneus y Quiscalus mexicanus. En la pista de aterrizaje y desde la torre de control la abundancia y riqueza de aves no varió significativamente a lo largo dlos meses del año. En la pista de aterrizaje la abundancia incrementa significativamente en el período seco en horarios de 06:00-07:00 am, principalmente por la presencia de Q. mexicanus y H. rustica. La riqueza en el periodo seco y la abundancia y riqueza en el período lluvioso no varió significativamente. Desde la torre de control no se registraron incrementos significativos de la abundancia y riqueza de aves en el período seco, pero si de la abundancia en el período lluvioso, con alzas a las 11:00 y 13:00, principalmente por la mayores actividades de la especie C. atratus a esas horas. La abundancia de aves en la pista de aterrizaje dependió de las condiciones climáticas, aumentando al aumentar la precipitación y la nubosidad y reduciéndose al aumentar la velocidad del viento y la temperatura. La actividad de las aves observadas desde la torre de control no varió significativamente con las variaciones climáticas diarias. Las especies que hacen mayor uso del enmallado perimetral del aeropuerto para perchar fueron: Passers domesticus, Columbina talpacoti, Tyrannus melancholicus, Crotophaga sulcirostris y Tyrannus forficatus. Los sitios preferidos para anidación dentro del aeropuerto fueron árboles de Almendra ( Terminalia catapa ), Mango ( Manguifera indica ) y dentro del las instalacones del cuerpo de Bomberos, torre de control y los hangares. Se concluye que C. atratus y Q. mexicanus son las especies que más peligro representan para la aviación, seguidas en menor escala de C. livia , C. talpocati, H. rustica y M. aeneus. Los sectores norte, oeste y una parte del sector sur del aeropuerto son áreas de mayor riesgo aviario por una mayor frecuencia de observación de C. atratus en esa zona. La especie Q. mexicanus esta distribuida principalmente en el sector sureste. Las fuentes de atracción para las aves van desde sitios ideales para hábitat, refugio, anidación y perchaje hasta fuente de alimentos que incluyen vegetales, insectos, vertebrados, basureros y mataderos.

Diversidad de aves en ocho comunidades del territorio Miskitu Indian Tasbaisca Kum, Reserva de Biósfera Bosawás, Nicaragua

La introducción de ganado en las áreas tradicionalmente agrícolas en el territorio Miskitu Indian Tasbaiska Kum ha influido en una modificación en su orden territorial para dar cabida a éste nuevo rubro por parte de sus habitantes. Es comúnmente conocido que la ganadería es una de las actividades productivas más incompatiblescon el bosque y la conservación de los elementos dentro de éste último, pero la rotación de las áreas de cultivo y pastoreo, y el uso de sistemas silvopastoriles podría reducir el impacto hacia los ambientes naturales. Con este estudio se plantea determinar la diversidad biológica de avifauna en los sistemas silvopastoriles ubicados en las cercanías de ocho comunidades del territorio Miskitu Indian Tasbaiska Kum, con el fin de determinar su potencial para preservar aves, en especial, aves de importancia para la conservación nacional. Para lograr los objetivos se realizó conteos de aves mediante el uso de puntos de conteo por comunidad, en las áreas donde suele llevarse a pastorear al ganado. En el estudio se invirtieron tres días por comunidad y se realizaron al menos dos observaciones por día, una entre las 06:00-10:00 y otra entre las 16:00 – 18:00. Con los datos obtenidos se calculó diferentes parámetros de diversidad biológica. Como resultado se observó un total de 423 individuos los cuales están agrupados en 67 especies y 27 familias. Las especies de aves más abundantes fueron: Brotogeris jugularis,Ramphocelus passerinii y Amazona auropaliata. Las comunidades Amarrana,Shiminka y Yakalpanani son las que registraron los mayores valores de los parámetros de biodiversidad. Se determinaron 14 especies en algún grado de conservación según la lista de los apéndices de CITES para Nicaragua y las listas del Sistema Nacional de Vedas 2012, entre éstas se incluyen Brotogeris jugularis y Amazona aurapaliata,as cuales resultaron también abundantes. La comunidad que concentró la mayor cantidad de aves en algún estado de con servación fue Yakalpanani. Las especies de plantas asociadas con la mayor diversidad de aves fueron especies de estadíos tempranos de sucesión como:Cecropia peltata ,Inga sp, Guazuma ulmifolia y Muntingia calabura. Aunque Yakalpanani es una de las comunidades más grandes, comparado con Boca de Plis, la ubicación de su área de pastoreo entre masas boscosas conservadas ha garantizado que los parámetros de diversidad biológica hayan resultado significativamente mayores en ésta, dado a una conectividad hasta el momento poco irrumpida.