Número de ramos na produção de figos verdes 'Roxo de Valinhos' no oeste do Paraná

O presente trabalho teve por objetivo verificar o efeito do número de ramos produtivos sobre o desenvolvimento e a produção de figos verdes 'Roxo de Valinhos'. O experimento foi conduzido com plantas de quatro anos de idade, em sistema de produção orgânica, espaçamento 2 x 3 m, de julho de 2007 a fevereiro de 2008, em Quatro Pontes-PR. Os tratamentos consistiram em plantas conduzidas com 6; 9; 12; 15; 18 e 21 ramos produtivos. Utilizou-se o delineamento experimental de blocos ao acaso, com quatro blocos e três plantas úteis por parcela. No sistema de produção orgânica, as maiores estimativas de produção e produtividade de figos verdes foram obtidas em plantas conduzidas com 21 ramos.

Diversidade e sazonalidade de crisomelídeos (Coleoptera: Chrysomelidae) em pomar, no município de Ponta Grossa, Paraná, Brasil

Este trabalho teve como objetivo levantar informações sobre os padrões de composição faunística, estrutura da comunidade e sazonalidade de Chrysomelidae num pomar localizado na região dos Campos Gerais do Paraná. Durante cerca de dois anos de amostragem, foram coletados 3.661 coleópteros e, destes, 1.103 crisomelídeos, representando 30,1% dos besouros capturados. Eumolpinae e Galerucinae foram as duas subfamílias que apresentaram maior abundância e riqueza de espécies, sendo que as oito mais representativas no pomar foram: Eumolpinae sp. 7 e Eumolpinae sp. 15, Diabrotica speciosa, Iphimeis dives, Spintherophyta semiaurata, Colaspis sp. 1 e Colaspis sp. 2 e Syphrea sp. 1, representando 91,7% dos indivíduos coletados. Em relação às árvores frutíferas, observou-se que o maior número de insetos foi coletado em laranjeira e tangerineira; a laranjeira teve a maior riqueza de espécies, e o caquizeiro apresentou o maior índice de diversidade. A redução considerável de crisomelídeos no segundo ciclo anual demonstra que a família tem uma oscilação temporal acentuada. A primavera foi a estação de maior abundância nos dois anos de coleta, e os fatores meteorológicos não apresentaram correlação com a abundância de crisomelídeos.

Runoff and sediment production in a Mediterranean basin under two different land uses

This study analyses the infl uence of two diff erent land uses on the hydrology of the Vernegà experimental basin between the years 2005 and 2009. It is located in the Northeast of the Iberian Peninsula and is infl uenced by a Mediterranean climate, with an average annual rainfall of 646 mm. The study of rainfall distributi on in the 1982 to 2009 period shows that the majority occurs during autumn, winter, and spring representi ng 33.2%, 25.5%, and 25.7% respecti vely of the total annual rainfall. Surface runoff is concentrated from October to June. Between 2005 and 2009, total runoff was 242.38 mm at the"Bosc" gauging stati on, which drains an area of 1.60 km2, and 298.54 mm at the"Campàs" gauging stati on, which drains an area of 2.57 km2 and is located at the outlet of the basin. More than 80% of the total surface runoff yielded during the study period corresponds to the 2005-2006 hydrologic year. Finally, Campàs gauging stati on registers a higher total runoff than Bosc gauging stati on. Part of this phenomenon may be due to the intercepti on of rainfall and plant biomass in the forested area of the basin. In relati on to the sediment yield, an overall increase in the two basins has been detected. Recent forest management practi ces undertaken in the catchment area are considered to be one of the most important reasons for this change.

Viabilidade da cultura do morangueiro no Paraná - BR

Avaliou-se a viabilidade da exploração do morangueiro, no Paraná, em duas áreas, 0,3 ha (área média cultivada pela agricultura familiar) e 1 ha, por um ano. Elaborou-se uma planilha de fluxo de caixa a partir da qual se calcularam: Período de Recuperação do Capital (PRC), Retorno sobre Investimento (RI), Valor Presente Líquido (VPL) e Taxa Interna de Retorno (TIR). Todos para Custo Operacional Efetivo (COE), Custo Operacional Total (COT) e Custo Total de Produção (CTP). Para uma situação considerada normal, os indicadores de rentabilidade calculados foram (Tipo de custo: VPL área-padrão (TIR área- padrão) / VPL área efetiva (TIR área efetiva)) COE: US$ 17.856,55 (42%) / US$ 4.795,85 (39%); COT: US$ 5.182,40 (11%) / - US$ 1.691,97 (-13%); CPT: US$ 4.846,26 (10%) / -US$ 1.792,80 (-14%). Fez-se a análise de cenários para os fatores produtividade, preço de venda e mão de obra, analisando o VPL e a TIR. Verificou-se que o tamanho da área influenciou na viabilidade econômica, mostrando a importância de se determinar anualmente a área mínima viável para a agricultura familiar. Os resultados indicaram que a cultura é viável em curto prazo, quando considerado o COE como parâmetro de análise, mas pode não se sustentar em prazos maiores quando se consideram o COT, o CTP e a variação de alguns fatores de produção. Pela análise de cenários definidos pelos fatores de produção analisados, o VPL e a TIR alteram-se para níveis que oferecem risco à exploração.

Coal deposition in carbonate rich shallow Lacustrine systems: The Calaf and Mequinenza sequences (Oligocene, eastern Ebro Basin, NE Spain)

Two main coal-bearing sequences developed during the Oligocene in the Tertiary Ebro Basin, the Calaf (early Oligocene) and Mequinenza (late Oligocene) coal basins. Coal deposition took place in shallow marsh-swamp-lake complexes which sometimes became closed and evolved under warm climatic conditions with fluctuating humidity. These shallow lacustrine systems are closely interrelated with the terminal parts of the distributive fluvial systems which spread from the tectonically active Ebro basin margins. Laterally extensive lignite-bearing sequences, including rather thin, lenticular autochthonous and/or hypautochthonous coal seams with high ash and sulphur contents, characterized coal deposition in the shallow lacustrine systems. Coal seam geometry, which makes them nearly subeconomic, resulted from the tectonic instability during basin margin evolution and the sometimes closed, arid conditions under which the lacustrine systems evolved. High ash and sulphur contents resulted from the inadequate isolation of peat forming environments from clastic influx and from the very low acidity and sometimes high sulphate contents of the lacustrine waters. Coal exploration in shallow lacustrine sequences similar to those described here must take into account that the spread of coal-forming environments and maxima of coal deposition are usually coincident with lake expansions and retraction or shifting of the terminal fluvial zones interrelated with the lacustrine areas.

Zoneamento agroclimático para a cultura do abacateiro no Estado do Paraná

O abacateiro apresenta grande diversidade de tolerância a baixas temperaturas devido às suas regiões de origem. As raças mexicanas são mais tolerantes, as raças antilhanas são mais sensíveis e as guatemalenses têm comportamento intermediário. Neste trabalho o zoneamento de riscos climáticos fundamentou-se na severidade das geadas, por meio da análise de séries históricas de temperaturas mínimas em um ambiente de Sistema de Informação Geográfica. Foram identificadas quatro zonas distintas de risco, caracterizando geadas muito fortes e frequentes, onde não se recomenda o cultivo; geadas fortes, onde somente a cultivar Fuerte é recomendada; geadas moderadas, onde somente as cultivares Primavera e Margarida não são recomendadas, e uma zona de baixo risco, no norte e oeste do Paraná, onde todas as cultivares são indicadas. As diversidades de climas no Paraná e as exigências térmicas das cultivares possibilitam a colheita em grande parte do ano por meio da combinação de diferentes cultivares e regiões de plantio.

Fluid flow processes at basin scale

S u b s u r face fluid flow plays a significant role in many geologic processes and is increasingly being studied in the scale of sedimentary basins and geologic time perspective. Many economic resources such as petroleum and mineral deposits are products of basin scale fluid flow operating over large periods of time. Such ancient flow systems can be studied through analysis of diagenetic alterations and fluid inclusions to constrain physical and chemical conditions of fluids and rocks during their paleohy d r og e o l ogic evolution. Basin simulation models are useful to complement the paleohy d r og e o l ogic record preserved in the rocks and to derive conceptual models on hydraulic basin evolution and generation of economic resources. Different types of fluid flow regimes may evo l ve during basin evolution. The most important with respect to flow rates and capacity for transport of solutes and thermal energy is gr avitational fluid flow driven by the topographic configuration of a basin. Such flow systems require the basin to be elevated above sea level. Consolidational fluid flow is the principal fluid migration process in basins below sea level, caused by loading of compressible rocks. Flow rates of such systems are several orders of magnitude below topogr a p hy driven flow. Howeve r, consolidation may create significant fluid ove rpressure. Episodic dewatering of ove rpressured compart m e n t s m ay cause sudden fluid release with elevated flow velocities and may cause a transient local thermal and chemical disequilibrium betwe e n fluid and rock. This paper gives an ove rv i ew on subsurface fluid flow processes at basin scale and presents examples related to the Pe n e d è s basin in the central Catalan continental margin including the offshore Barcelona half-graben and the compressive South-Pyrenean basin.

PRODUÇÃO E QUALIDADE DE FRUTOS HÍBRIDOS DE MARACUJAZEIRO-AMARELO NO NORTE DO PARANÁ

RESUMOAtualmente, encontram-se quatorze cultivares de maracujazeiro-amarelo no Registro Nacional de Cultivares do Ministério da Agricultura. É de grande importância o aprimoramento de trabalhos de melhoramento genético nessa cultura, para favorecer a disponibilização de novas cultivares adaptadas às regiões produtoras. Assim, o objetivo deste trabalho foi avaliar a produção e as características qualitativas dos frutos de treze híbridos de maracujazeiro-amarelo cultivados no norte do Paraná. As avaliações foram realizadas durante dois ciclos de produção da cultura, de abril a julho de 2009 e de janeiro a julho de 2010, com coletas semanais dos frutos maduros. A produção foi determinada por meio da pesagem dos frutos colhidos e do número de frutos por planta. Para as características qualitativas, foram avaliados: massa, comprimento, diâmetro, relação entre comprimento e diâmetro dos frutos, espessura da casca, rendimento de polpa, teor de sólidos solúveis totais (SST), acidez total titulável (ATT ) e relação SST/ATT . Os híbridos ‘66’ e ‘65’ apresentaram, respectivamente, maior produção e maior número de frutos no acumulado das duas safras. Os frutos do híbrido ‘72’ destacaram-se no atendimento das características desejáveis de qualidade para o consumo in natura, enquanto o híbrido ‘69’ apresentou caracteristicas importantes para a indústria de suco.

Approach to the Lower Pliocene marine-continental correlation from southern Spain. The micrommamal site of Alhaurín el Grande-1 (Málaga Basin, Betic Cordillera, Spain)

A new micromammal site at Alhaurín el Grande (Málaga, southern Spain) located above early Pliocene marine deposits allows an approach to the marine-continental correlation for this age. The early Pliocene marine filling throughout the Málaga Basin is developed in three transgressive-regressive sequences (Pl-1, Pl-2, and Pl-3 units) bounded by discontinuities. At the top of the intermediate sequence Pl-2, peaty sediments have yielded fossils of Rodentia, Lagomorpha, Insectivora, and Crocodylia. The presence of Cricetus barrieri Mein & Michaux, 1970 in combination with murids, both of primitive morphology, such as Apodemus gudrunae Van de Weerd, 1976, and more advanced forms (i.e. Occitanomys brailloni Michaux, 1969 and Stephanomys donnezani cordii Ruiz Bustos, 1986), points to an early Ruscinian age (MN 14 biozone). Based on the planktonic foraminifers, the biostratigraphic data indicate that marine sediments just below the micromammal beds belong to the MPl-2 biozone of the early Zanclean. Available paleomagnetic data from the marine sediments show that the micromammal bed must be located between the normal geomagnetic subchron C3n3n (4.89-4.80 Ma) and the subchron C3n2n (4.63-4.49 Ma), limiting the age of this site to the late part of the early Zanclean.

Upper Eocene-Lowermost Miocene charophyte succession in the Ebro Basin (Spain). Contribution to the charophyte biozonation in Western Europe

A charophyte succession has been established in nineteen sections and eight isolated outcrops from the Ebro Basin, ranging from the Priabonian ro the Aquitanian. Most assemblages were recovered fmm continuous sections and their abundance and diversity allow to define a new zonal scheme for the Upper Eocene-Lower Miocene of Europe. The new zonation includes nine subdivisions, based on the distribution of thirty-two species and directly correlated with the mammal standard levels. Changes in diversity, occurring mainly in the Middle and Upper Oligocene, have been related to climatíc variations. A new species, Chara sp. A. is also described and figured.

Architectural characterization of a delta-front reservoir analogue combining ground penetrating radar and electrical resistivity tomography: Roda Sandstone (Lower Eocene, Graus-Tremp basin, Spain)

Three-dimensional reconstruction of reservoir analogues can be improved combining data from different geophysical methods. Ground Penetrating Radar (GPR) and Electrical Resistivity Tomography (ERT) data are valuable tools, since they provide subsurface information from internal architecture and facies distribution of sedimentary rock bodies, enabling the upgrading of depositional models and heterogeneity reconstruction. The Lower Eocene Roda Sandstone is a well-known deltaic complex widely studied as a reservoir analogue that displays a series of sandstone wedges with a general NE to SW progradational trend. To provide a better understanding of internal heterogeneity of a 10m-thick progradational delta-front sandstone unit, 3D GPR data were acquired. In addition, common midpoints (CMP) to measure the sandstone subsoil velocity, test profiles with different frequency antennas (25, 50 and 100MHz) and topographic data for subsequent correction in the geophysical data were also obtained. Three ERT profiles were also acquired to further constrain GPR analysis. These geophysical results illustrate the geometry of reservoir analogue heterogeneities both depositional and diagenetic in nature, improving and complementing previous outcrop-derived data. GPR interpretation using radar stratigraphy principles and attributes analysis provided: 1)tridimensional geometry of major stratigraphic surfaces that define four units in the GPR Prism, 2) image the internal architecture of the units and their statistical study of azimuth and dips, useful for a quick determination of paleocurrent directions. These results were used to define the depositional architecture of the progradational sandbody that shows an arrangement in very-high-frequency sequences characterized by clockwise paleocurrent variations and decrease of the sedimentary flow, similar to those observed at a greater scale in the same system. This high-frequency sequential arrangement has been attributed to the autocyclic dynamics of a supply-dominated delta- front where fluvial and tidal currents are in competition. The resistivity models enhanced the viewing of reservoir quality associated with cement distribution caused by depositional and early diagenetic processes related to the development of transgressive and regressive systems tracts in igh-frequency sequences.

Quaternary Glacial Geology of Alta Ribagorqa Basin (Central Southern Pyrenees)

This paper is an abstract of the doctoral thesis presented by the autor at the University of Barcelona on September 1983. It constitutes a regional study about the Quatemary Glacial Geology in the Ribagorca high valleys. It is the first work in relation to the geomorphology, sedimentology and stratigraphy of the glacial and related deposits in this zone of the Pyrenees. Several formations of quatemary deposits have been studied in detail (mainly in Llauset Valley and in Tall area); and the local quatemary stratigraphy is established and finally a correlation with some previously studied areas in the Pyrenees is attemped.

Preliminary integrated magnetostratigraphic and biostratigraphic correlation in the Miocene Lorca Basin (Murcia, SE Spain).

The Lorca basin is one of the Neogene basins OS South Eastern Spain. The infilling Tortonian-Messinian deposits are mainly composed OS marls and reach up to 1,200 m in thickness. A biostratigraphic survey OS these deposits, assisted by the determination OS the magnetic polarity reversal pattern Sor most OS these deposits (900 m), has enabled the Tortonian-Messinian chronostratigraphy to be precised. The close sampling space for biostratigraphic determination has enabled the accurate location OS Sour main biostratigraphic events than can be correlated with charactenstic events of the Mediterranean biostratigraphic Zones. In addition, the location OS the TortonianNessinian boundary has been accurately placed at some 150 m below the main gypsurn unit outcropping in the basin. The integrated bio-magnetostratigraphic data fiom the studied section allows a tentative interpretation OS the identified magnetozones. Thus, a correlation to the Geomagnetic Polarity Time Scale is presented for more than 900 m of pre-evaporite Miocene stratigraphic succession fiom the Lorca basin. Moreover, about 15' OS anticlockwise rotation has been detected. Its significance is evaluated in the basin geodynamic framework.