The Exotic Palaeo-Thethys Terrane in Central Iran: New geological data from Anarak, Jandaq and Posht-e-Badam areas

Résumé Le « terrane » d'Anarak-Jandak occupe une position géologique clé au nord-ouest du Microcontinent Centre-East Iranien (CE1M), connecté avec le Bloc du Grand Kavir et la ceinture métamorphique de Sanandaj-Sirjan. Nous discutons ici l'origine de ces différentes unités, reliées jusqu'à présent à des épisodes orogéniques d'âge Précambrien à Paléozoïque inférieur, pour conclure finalement de leur affinité paléotéthysienne. Leur histoire commence par un épisode de rifting d'âge Ordovicien supérieur-Dévonien inférieur, pour se terminer au Trias par la collision des blocs Cimmériens dérivé du Gondwana avec le Bloc du Turan d'affinité asiatique (événement Eocimmérien). La plus importante unité métamorphique affleurant au sud-ouest de la région de Jandak-Anarak-Kaboudan est une épaisse séquence silicoclastique à grains fins contenant des blocs ophiolitiques (marginal-sea-type), et des associations basalte-gabbro à signatures géochimiques de type supra-subduction. Dans la région de Nakhlak, nous avons daté ces gabbros par la méthode U-Pb à 387f0.11 Ma ; les roches métamorphiques pélitiques ont donné des âges de refroidissement Ar-Ar pour la muscovite de 320 à 333 Ma. Ce complexe d'accrétion "varisque" a été métamorphisé dans le faciès schiste vert-amphibolite au cours de l'accrétion de la ceinture granitique d'Airekan, d'âge Cambrien inférieur (549±15 Ma par la méthode U/Pb), qui affleure aujourd'hui à l'extrémité nord-ouest du terrane d'Anarak-Jandak . La subduction vers le nord de l'océan Paléotéthys depuis le Paléazoïque supérieur jusqu'au Trias, a permis l'accumulation de grandes quantités de matériel océanique dans la zone de subduction. Par exemple, une succession de guyots (Anarak, Kaboudan, et Meraji Seamounts) et de hauts sous-marins, entrés en collision oblique avec le prisme d'accrétion, est à l'origine d'un léger métamorphisme de type HP qui affecte ces séries {âges Ar-Ar de 280 à 230 Ma). De plus, le magmatisme bimodal de Chah Gorbeh est caractérisé d'une part par des roches de type trondjémite-gabbros (262 Ma), d'autre part par des laves en coussin de type basaltes alcalins-rhyolites; ces roches magmatiques ont recoupé l'ophiolite d'Anarak lors de la mise en place de cette dernière dans la fosse interne de subduction. Quant au prisme d'accrétion de Doshakh, d'âge essentiellement Permien supérieur, i1 a été accrété le long de la marge continentale et métamorphisé dans le faciès schiste vert. La fermeture de la Paléotéthys s'enregistre finalement par la sédimentation dans le bassin d'avant pays du flysch de Bayazeh, d'âge probable Triasique. Le matériel issu de l'arc magmatique de la Paléotéthys est très bien préservé dans les dépôts infra-arc Dévonien supérieur-Carbonifère de Godar-e-Siah, ainsi que dans la succession d'avant-arc de Nakhlak. Pendant l'intervalle Paléozoïque supérieur-Trias, la région de Jandak a été soumise à un régime extensif de type bassin d'arrière-arc, dont un témoin pourrait être la ceinture ophiolitique d'Arusan, elle-même comparable aux écailles ophiolitiques d'Aghdarband au nord-est de l'Iran. Cet ensemble métamorphique est recoupé par des granites d'arc à collisionnel datés à 215±15 Ma. Dans la région de Yazd, témoin de la marge passive Cimmérienne, la sédimentation syn-rift Silurienne à Dévonienne inférieure a été interrompue pendant l'intervalle Trias moyen-Trias supérieur; il en a été de même pour les dépôts de plate-forme Paléozoïque supérieur. L'érosion, qui dans ce dernier cas a atteint le Permien, pourrait être liée au bombement flexural de la marge passive. La collision finale n'a pas induit de déformations trop importantes, et se caractérise par la mise en place de nappes sur la marge passive. Cet événement est scellé par des dépôts molassique du Lias. D'un point de vue régional, la zone s'étendant actuellement de la Mer Noire au Pamir a été soumise à six épisodes d'extension-compression du Jurassique inférieur (début du l'ouverture en position arrière-arc de la Néotéthys) à l'Eocène moyen. Par exemple, le terrane d'AnarakJandak, probablement situé entre le Kopeh Dagh et la plate-forme nord Afghane, s'est complètement détaché de sa patrie d'origine au début du Crétacé supérieur. Des preuves de cet événement se retrouvent dans les séries de plate-forme de Khur (préservation de séries syn-rift puis de marge passive). Les ophiolites de Nain et de Sabzevar sont de plus interprétée comme un témoin de l'existence de ce bassin d'arrière-arc. Dans l'intervalle Eocène-Oligocène, l'indentation par la plaque indienne de l'Eurasie a été contemporaine de la rotation horaire de fragments de l'ancien microcontinent Iranien et de la formation du CEIM. Cette rotation est responsable du transport du terrane d'Anarak-Jandak vers sa position actuelle en Iran Central, et de la dislocation de Terranes de moindre importance, comme le bloc de Posht-e Badam. Depuis le Miocène supérieur, et à la suite de la collision entre l'Arabie et l'Iran, le ternane d'Anarak-Jandak a subi des déformations liées à l'activité d'une zone de cisaillement dextre parallèle à la suture du Zagros, à l'arrière de l'arc magmatique d'Uromieh-Dokhtar. Résumé large public Le Microcontinent Centre-Est Iranien occupe une position géologique clé au centre de l'Iran. Les différentes unités qui le composent, reliées jusqu'à présent à des épisodes orogéniques d'âge Précambrien à Paléozoïque inférieur, sont maintenant rajeunies et liés à la fermeture de l'océean Paléotéthys. Leur histoire commence par un épisode de rifting d'âge Ordovicien supérieur à Dévonien inférieur, pour se terminer au Trias par la collision des- blocs Cimmériens, dérivés du Gondwana, avec le Bloc du Turan d'affinité asiatique. Dans la marge active asiatique de la Paléotéthys, nous avons daté les restes d'un océan marginal à 387±0.11 Ma. Ce complexe d'accrétion a été métamorphisé au cours de la réaccrétion de la ceinture granitique d'Airekan, d'âge Cambrien inférieur (549±15 Ma), qui affleure aujourd'hui à l'extrémité nord-ouest du « terrane » d'Anarak-Jandak correspondant à la plus grande partie de la région étudiée. Le matériel issu de l'arc magmatique de la Paléotéthys est très bien préservé et daté du Dévonien supérieur-Carbonifère. Pendant l'intervalle Paléozoïque supérieur-Trias, la région a été soumise à un régime extensif de type bassin d'arrière-arc, dont un témoin pourrait être la ceinture ophiolitique d'Arusan, comparable aux écailles ophiolitiques d'Aghdarband au nord-est de l'Iran. Cet ensemble métamorphique est recoupé par des granites datés à 215±15 Ma. La subduction vers le nord de l'océan Paléotéthys depuis le Paléozoïque supérieur jusqu'au Trias, a permis l'accumulation de grandes quantités de matériel océanique dans la zone de subduction. Par exemple, une succession de volcans sous-marins, entrés en collision avec le prisme d'accrétion, est à l'origine d'un léger métamorphisme de type HP qui affecte ces séries (280 à 230 Ma). Quant au prisme d'accrétion de Doshakh, d'âge essentiellement Permien supérieur, il a été mis en place le long de la marge continentale et métamorphisé dans le faciès schiste vert. La fermeture de la Paléotéthys s'enregistre finalement par la sédimentation dans le bassin d'avant pays du flysch de Bayazeh, d'âge Triasique. Dans la région de Yazd, on trouve les témoins de la marge passive Cimmérienne, la sédimentation syn-rift Silurienne à Dévonienne inférieure a été interrompue pendant l'intervalle Trias moyen-Trias supérieur, marqué par la flexuration de la marge passive lorsqu'elle rentra en collision avec la marge active asiatique. Cet événement est scellé par des dépôts molassique à charbon du Lias. Le «terrane» d'Anarak-Jandak, probablement situé à l'origine entre le Kopeh Dagh et la plate-forme nord Afghane, s'est complètement détaché de cette région au début du Crétacé supérieur lors de l'ouverture d'un bassin d'arrière-arc, engendré, cette fois, par la subduction de l'océan Néotéthys situé au sud des blocs cimmériens. Des preuves de cet événement se retrouvent dans les séries syn-rift, puis de marge passive de Khour. Les ophiolites de Nain et de Sabzevar sont interprétées comme un témoin de l'existence de ce bassin d'arrière-arc. Dans l'intervalle Eocène-Oligocène, l'indentation de l'Eurasie par la plaque indienne a été contemporaine de la rotation horaire de fragments de l'ancien microcontinent centre-Iranien. Cette rotation de près de 90° est responsable du transport du « terrane » d'Anarak-Jandak vers sa position actuelle. Abstract The Anarak-Jandaq terrane occupies a strategic geological situation at the north-western part of the Central-East Iranian Microcontinent (CEIM) and in connection with the Great Kavir Block and Sanandaj-Sirjan metamorphic belt. Our recent findings redefine the origin of these mentioned areas so far attributed to the Precambrian-Early Palaeozoic orogenic episodes, to be now directly related to the tectonic evolution of the Palaeo-Tethys Ocean, commenced by Late Ordovician-Early Devonian rifting events and terminated in the Triassic by the Eocimmerian tectonic event due to the collision of the Cimmerian blocks with the Asiatic Turan block. The most distributed metamorphic unit that is exposed from the south-west of Jandaq to the Anarak and Kaboudan areas is a thick and fine grain siliciclastic sequence accompanied by marginal-sea-basin ophiolitic blocks including basalt-gabbro association with supra-subduction-geochemical signature. These gabbros in the Nakhlak area were dated by U/Pb method at 387.6 ± 0.11 Ma and the metamorphic pelitic rocks yielded a range of 320 to 333 Ma muscovite-cooling ages based on 40Ar/39 Ar method. This "Variscan" accretionary complex was metamorphosed in greenschist-amphibolite facies during accretion to the Lower Cambrian Airekan granitic belt (549 ± 15 Ma by U/Pb method) that crops out at the northwestern edge of the Anarak-Jandaq terrane. Continued northward subduction of the Palaeo-Tethys Ocean during the entire Late Palaeozoic-Middle Triassic brought huge amount of oceanic material to the subduction zone. One chain of Carboniferous-Triassic oceanic rises and seamounts (the Anarak, Kaboudan, and Meraji Seamounts) obliquely collided with the accretionary wedge and created a mild HP metamorphic event (280-230 Ma based on 40Ar/39Ar results). Bimodal magmatism of the Chah Gorbeh area is characterized by a 262 Ma trondjemite-gabbro as well as pillow alkalibasalts-rhyolites which intruded the Anarak ophiolite when it was being emplaced within the inner-wall trench. The mainly Late Permian-Triassic Doshakh wedge was accreted along the continent and metamorphosed under lower greenschist facies and the probable Triassic Bayazeh flysch filled the foreland basin during the final closure. The Palaeo-Tethys magmatic arc products have been well preserved in the Late Devonian-Carboniferous Godar-e-Siah intra-arc deposits and the Triassic Nakhlak fore-arc succession. During the Late Palaeozoic-Triassic times, the Jandaq area has been affected by back-arc extension and probably the Arusan ophiolitic belt is the remnant of this narrow basin comparable to the Aqdarband ophiolitic remnant in north-east Iran. This metamorphic belt was intruded by 215 ± 15 Ma arc to collisional granites. In the passive margin of the Cimmerian block, on the Yazd region, the Silurian-Early Devonian syn-rift succession as well as the nearly continuous Upper Palaeozoic platform-type deposition was interrupted during the Middle to Late Triassic time, local erosion down to Devonian levels may be related to flexural bulge erosion. The collision event was not so strong to generate intensive deformation but was accompanied by some nappe thrusting onto the passive margin. It is finally unconformably covered by Liassic continental molassic deposits. Related to the onset of Neo-Tethyan back-arc opening in Early Jurassic to Mid-Eocene times, six periods of extensional-compressional events have differently influenced an elongated area, extending from the West Black Sea to Pamir. The Anarak-Jandaq terrane which was situated somewhere in this affected area, probably between the Kopeh Dagh and North Afghan platform, was completely detached from its source at the beginning of the Late Cretaceous

Implementação e validação de um método cromatográfico para a Detecção e Quantificação de Furano em Feijão Enlatado

O furano tem sido detectado em diversos alimentos em particular nos que são sujeitos a tratamento térmico durante o processo de preparação industrial. É considerado um composto potencialmente cancerígeno para seres humanos, pelo que a sua presença nos alimentos se tornou uma questão de segurança alimentar. Desde 2007 que a Autoridade Europeia para a Segurança Alimentar tem procurado recolher o maior número de informação possível, relativa à presença de furano nos alimentos. Neste trabalho utilizou-se a técnica de Cromatografia Gasosa de Espaço de Cabeça acoplada a um espectrómetro de massa (HS-GC/MS) para avaliar os teores de furano em feijões enlatados. Foram analisadas 10 amostras (latas) independentes, seleccionadas aleatoriamente no mercado, de três marcas comercializadas em Portugal. A concentração média obtida foi de 3,27 ng/g, numa gama que variou entre 2,61 e 4,45 ng/g. Os limites de detecção calculados foram de 0,80 ng/g para as amostras PD, 1,26 ng/g para as amostras C e de 0,58 ng/g para as amostras F. Os limites de quantificação foram, respectivamente, de 2,44, 3,82 e 1,77 ng/g. Os coeficientes de variação do método foram inferiores a 10% e a percentagem de recuperação foi de 95%. Para estudar o efeito do tratamento térmico doméstico, foram também, analisadas amostras aquecidas à temperatura de 80°C, tendo-se verificado um aumento significativo na concentração do furano detectada. Comparou-se ainda a concentração média do furano obtido nos feijões em lata com a concentração média para o mesmo tipo de feijão conservado em frascos de vidro, tendose constatado não existirem diferenças significativas.

A Comparison of the Management Models of Protected Areas between China and the Southern African Region

A Comparison of the Management Models of Protected Areas between China and the African South Region allows reading and evaluating the similarities and differences in the use of management model as a management tool for protected areas in China and South African Region. Specifically, some positive and negative features of the management approaches for the two regions. Secondary data was collected from various related literature such as policy documents, students‟ dissertations/thesis, scientific articles and magazines. Based on the method above, the study found out that China's first nature reserve was the Dingus Mountain Nature Reserve in Zhaoqing, Guangdong province established in 1956. By the end of 2005, about 2,349 nature reserves of various kinds were set up throughout the country, covering a total area of 149.95 million ha and accounting for 15 percent of the total land territory. The study further found that Southern Africa has approximately 4,390 protected areas out of 11487920 total land areas and Eastern Africa has approximately 1838144 protected areas, which is equivalent to 15.0% of the total land areas. South Africa in this region had its first declared natural park in 1926 after Paul Kruger (a war hero) had alerted the authorities of the extinguishing threat of some animal species of region.

Spontaneous pre-stimulus fluctuations in the activity of right fronto-parietal areas influence inhibitory control performance.

Inhibitory control refers to the ability to suppress planned or ongoing cognitive or motor processes. Electrophysiological indices of inhibitory control failure have been found to manifest even before the presentation of the stimuli triggering the inhibition, suggesting that pre-stimulus brain-states modulate inhibition performance. However, previous electrophysiological investigations on the state-dependency of inhibitory control were based on averaged event-related potentials (ERPs), a method eliminating the variability in the ongoing brain activity not time-locked to the event of interest. These studies thus left unresolved whether spontaneous variations in the brain-state immediately preceding unpredictable inhibition-triggering stimuli also influence inhibitory control performance. To address this question, we applied single-trial EEG topographic analyses on the time interval immediately preceding NoGo stimuli in conditions where the responses to NoGo trials were correctly inhibited [correct rejection (CR)] vs. committed [false alarms (FAs)] during an auditory spatial Go/NoGo task. We found a specific configuration of the EEG voltage field manifesting more frequently before correctly inhibited responses to NoGo stimuli than before FAs. There was no evidence for an EEG topography occurring more frequently before FAs than before CR. The visualization of distributed electrical source estimations of the EEG topography preceding successful response inhibition suggested that it resulted from the activity of a right fronto-parietal brain network. Our results suggest that the fluctuations in the ongoing brain activity immediately preceding stimulus presentation contribute to the behavioral outcomes during an inhibitory control task. Our results further suggest that the state-dependency of sensory-cognitive processing might not only concern perceptual processes, but also high-order, top-down inhibitory control mechanisms.

Model endophenotype for bipolar disorder: Qualitative Analysis, etiological factors, and research areas

The aim of this study is to present an updated view of the writings on the endophenotype model for bipolar disorder using analytical methodologies. A review and analysis of networks was performed through descriptors and keywords that characterize the composition of the endophenotype model as a model of health. Information was collected from between 1992 and 2014, and the main thematic areas covered in the articles were identified. We discuss the results and question their cohesion, emphasizing the need to strengthen and identify the points of connection between etiological factors and characteristics that make up the model of endophenotypes for bipolar disorder.

New data on the distribution and conservation status of some angiosperms of the Cape Verde Islands, W Africa

New data on the distributibn and conservation status of some angiosperms of the Cape Verde Islands, W Africa Intensive field work aud analysis of the state of biodiversity ou all islands during the years iYY.3 lo IYYY Icd lo lhc publication ol’several contributions lo the flora and vegelalion of the archipclago of Cabo Verde (Brochniann & al. 1997, Gornes & Vera-Cruz 1993. Gonles & al. I9YSa-h. 1998, Games 1997. Kilian & Leyens 1994, Leyens 1998. Leyens & Lobin 1995, Lobin & al. 1995) as well as to the compilation of the First Red Data List for the Cape Verde Islnuds (Lcyrus & Lobin 1996). the elaboration of the National Strategy for Biodiversity Conservation (SIPA 19YY) and ! compilation of all areas in urgent need of protection (Leyens unpubl. diplonla thc.\is IYYJ. Gwnes & al. iu prep.). As part UC the activities of the lnstituto National de Invcstig;u$o c Dcscnvolvitucnto Agriirio (INIDA) and the Dcpurtamcnto de GeociSncias do Institute Supcriot de Educ;u$o t ISE) iutcnsive t’icld studies were conducted PI many diffcrctu localilics OII xcvcr;~I islands. resulting in a thesis tGo~nes IY97) and several terminal study papers (Luz IYYY. Cosi;t 1994. Gonsalvez 1999). The results show that the vegetation and flora of the islands arc still IWI fully known and much more field work is needed. hllhot~gh Sanliiqw is one of lhc islands whcrc lhc firs1 holanicill iIlVcxligilliollx wcrr c:crriul WI (Wcbh 1x49. Schruidt 1x52. Chcvalicr IY35) and where uu~ny intensive field studirs wcrc

Utilização de bioensaios e marcadores moleculares para detecção da resistência de coleópteros de produtos armazenados a inseticidas

The qualitative and quantitative losses caused by stored product insects are of great concern, and since there is only a few active ingredients available for their control it is very important to have a frequent insect resistance monitoring. The objective of this research is to evaluate combination of bioassays and molecular marker techniques to detect insecticide resistance in stored product beetles. The Coleoptera species used for the tests were Sitophilus oryzae (L.) (Curculionidae), Rhyzopertha dominica (F.) (Bostrichidae) and Oryzaephilus surinamensis (L.) (Silvanidae). For the bioassays it was used the impregnated filter paper technique, applying 1 mL of deltamethrin (K-Obiol 25 CE TM) using four concentrations and five replicates, including a control with solvent only. Ten adults of each species were liberated separately on each dish. The mortality was evaluated after 24 h and resistance determined by probit analysis. The samples used for the PCR-RAPD were either in vivo or preserved in 70% ethanol, kept in -18°C freezer. After extraction, quantification and DNA quality analysis, the 25 µL samples had the DNA amplified and tested with six primers. The bioassays showed a crescent mortality proportional to insecticide concentration. The resistance factor for R. dominica, S. zeamais and S. oryzae were: 2,2; 3,2 and 9,2, respectively, compared to the susceptible populations of each species. The PCR-RAPD analysis revealed bands which indicate inter and intraspecific variability in the populations, but it was not possible to correlate them to resistance. The association of bioassay and PCR-RAPD represents a precise and valuable tool for resistance management of stored product insects, but more populations and primers should be tested.

Density and distribution of nests of Mycetophylax simplex (Emery) (Hymenoptera, Formicidae) in areas with mobile dunes on the northern coast of Rio Grande do Sul, Brazil

Studies on lower attines are scarce, especially on nesting and foraging ecology and behavior. This study aimed to contribute to the knowledge of an Attini in dunes ecosystems through the description of density and spatial distribution of Mycetophylax simplex (Emery, 1887) nests in a strip of mobile dunes in the Praia Grande beach, Torres, northern coast of Rio Grande do Sul, Brazil. The density and spatial distribution of nests were estimated in four plots of 2,500 m² each, in which were found 20, 209, 284 and 324 nests, with average densities of 0.01 nests/m², 0.09, 0.11 and 0.13 nests/m², respectively. The nests were found near to the vegetation and showed clumped distribution. The density and distribution pattern of the nests seem to be related to the availability of nesting places and foraging resources.

The flower-visiting social wasps (Hymenoptera, Vespidae, Polistinae) in two areas of Rio Grande do Sul State, southern Brazil

The flower-visiting social wasps (Hymenoptera, Vespidae, Polistinae) in two areas of Rio Grande do Sul State, southern Brazil. The structure of flower-visiting social wasps' assemblages in the CPCN Pró-Mata of São Francisco de Paula and in the Green Belt of Santa Cruz do Sul, Rio Grande do Sul, are characterized. A total of 879 polistine wasps were collected, of which 475 (11 spp.) in the CPCN and 404 (21 spp.) in the Green Belt, from September 1997 to April 2001 and from September 2001 to April 2004, respectively. Foraging social wasps were observed on flowers of 36 species of angiosperms (20 families) in the Green Belt, and on flowers of 54 species of angiosperms (21 families) in the CPCN. Asteraceae was the most visited plant family on both studied localities. A list of pant species visited by the polistines is provided.

An assessment of empirical Bayes and composite estimators for small areas

We compare a set of empirical Bayes and composite estimators of the population means of the districts (small areas) of a country, and show that the natural modelling strategy of searching for a well fitting empirical Bayes model and using it for estimation of the area-level means can be inefficient.

Relatório - Detecção de Tuta Absoluta (Myerick, 1917) em Cabo Verde

Tuta absoluta é praga minadora de folhas desenvolve-se principalmente no tomate (Lycopersicon esculentum) e não só mas também em outras espécies de Solanáceas tais como batata comum (Solanum tuberosum), beringela (Solanum melongina), Pimentos (Capsicum sp.) e no tomate silvestre (Lycopersicon hirsutum), (Solanum dulcamara), (Solanum nigrum), (Solanum elaeagnifolium), (Datura stramonium), (Datura ferox) e (Nicotiana glauca). No entretanto, esta praga ataca espécies de tomate em grande escala a nível dos trópicos, Sub-trópicos e regiões temperadas causando prejuízos económicos consideráveis (USDA, 2011). Esta praga encontra-se presente na América do Sul, (Chili, Bolívia, Brasil, Colômbia, Equador, Uruguai, Perú, Venezuela, Argentina). No continente Africano ela encontra-se na Africa Ocidental e Central designadamente no Benim, Camarões Cabo-Verde, Costa do Marfim, Congo Brazzaville, Gambia, Gabão, Ghana, Guiné-Conakry, Guiné- Bissau, Mali, Mauritânia, Niger, Nigéria, República Democrático do Congo, Serra Leoa, Senegal, Tchad e Togo. Pela primeira vez T. absoluta foi assinalada na Europa em 2006, e em Espanha na comunidade Valenciana em 2007 (Vieira, 2008). O cultivo de tomate em Cabo Verde tem aumentado nos últimos anos. Atualmente tomate é o legume mais cultivado em Cabo Verde. A sua quota parte na produção hortícola que não ultrapassavam os 1.000 t há uns anos, atinge atualmente 4200 t, o que representa 23% da produção total dos legumes. Apesar de alguns constrangimentos, nomeadamente problemas de ordem fitossanitária e escassez de água de rega a disponibilidade e a utilização generalizada das variedades locais, permitiram um escalonamento da produção durante o na, compreendendo o período quente e húmido. Um outro fator que contribui para o aumento substancial da produção, é a salinização de água de rega, em várias zonas do regadio. Os agricultores destas zonas viram nesta cultura a única saída para obterem algum rendimento (MAP/ CPDA/INIDA/ FAO GCP/CV/036/NET s/data). Em Cabo Verde a área média de um campo de produção de tomate é de 750 m2 sendo máxima de 1.400 m2. Este trabalho teve como objetivo estabelecimento instantâneo de presença ou ausência da nova praga Tuta absoluta no país que foi recentemente encontrada na Sub-região Saariana na Costa Ocidental e Central de África.

Relatório Detecção de Tuta Absoluta (Myerick,1917) em Cabo Verde

Tuta absoluta é praga minadora de folhas desenvolve-se principalmente no tomate (Lycopersicon esculentum) e não só mas também em outras espécies de Solanáceas tais como batata comum (Solanum tuberosum), beringela (Solanum melongina), Pimentos (Capsicum sp.) e no tomate silvestre (Lycopersicon hirsutum), (Solanum dulcamara), (Solanum nigrum), (Solanum elaeagnifolium), (Datura stramonium), (Datura ferox) e (Nicotiana glauca). No entretanto, esta praga ataca espécies de tomate em grande escala a nível dos trópicos, Sub-trópicos e regiões temperadas causando prejuízos económicos consideráveis (USDA, 2011). Esta praga encontra-se presente na América do Sul, (Chili, Bolívia, Brasil, Colômbia, Equador, Uruguai, Perú, Venezuela, Argentina). No continente Africano ela encontra-se na Africa Ocidental e Central designadamente no Benim, Camarões Cabo-Verde, Costa do Marfim, Congo Brazzaville, Gambia, Gabão, Ghana, Guiné-Conakry, Guiné- Bissau, Mali, Mauritânia, Niger, Nigéria, República Democrático do Congo, Serra Leoa, Senegal, Tchad e Togo. Pela primeira vez T. absoluta foi assinalada na Europa em 2006, e em Espanha na comunidade Valenciana em 2007 (Vieira, 2008). O cultivo de tomate em Cabo Verde tem aumentado nos últimos anos. Atualmente tomate é o legume mais cultivado em Cabo Verde. A sua quota parte na produção hortícola que não ultrapassavam os 1.000 t há uns anos, atinge atualmente 4200 t, o que representa 23% da produção total dos legumes. Apesar de alguns constrangimentos, nomeadamente problemas de ordem fitossanitária e escassez de água de rega a disponibilidade e a utilização generalizada das variedades locais, permitiram um escalonamento da produção durante o na, compreendendo o período quente e húmido. Um outro fator que contribui para o aumento substancial da produção, é a salinização de água de rega, em várias zonas do regadio. Os agricultores destas zonas viram nesta cultura a única saída para obterem algum rendimento (MAP/ CPDA/INIDA/ FAO GCP/CV/036/NET s/data). Em Cabo Verde a área média de um campo de produção de tomate é de 750 m2 sendo máxima de 1.400 m2. Este trabalho teve como objetivo estabelecimento instantâneo de presença ou ausência da nova praga Tuta absoluta no país que foi recentemente encontrada na Sub-região Saariana na Costa Ocidental e Central de África.

Detecção e Monitorização de Tuta Absoluta (Meyrick, 1917) em Cabo Verde

Tuta absoluta (Meyrick, 1917) (Microlepidoptera:Gelechiidae) é praga minadora de folhas desenvolve-se principal-mente no tomate (Lycopersicon esculentum) e não só mas também em outras espécies de Solanáceas tais como batata comum (Solanum tuberosum), beringela (Solanum melongina), Pimentos (Capsicum sp.) e no tomate silvestre (Lycopersicon hirsutum), (Solanum dulcamara), (Solanum nigrum), (Solanum elaeagnifolium), (Datura stramonium), (Datura ferox) e (Nicotiana glauca). Esta praga ataca espécies de tomate em grande escala a nível dos trópicos, Sub-trópicos e regiões temperadas causando prejuízos económicos consideráveis (USDA, 2011). Esta praga encontra-se presente na América do Sul, (Chili, Bolívia, Brasil, Colômbia, Equador, Uruguai, Perú, Venezuela, Argentina). No continente Africano ela encontra-se na Africa Ocidental e Central designadamente no Benim, Camarões, Cabo-Verde, Costa do Marfim, Congo Brazzaville, Gambia, Gabão, Ghana, Guiné-Conakry, Guiné- Bissau, Mali, Mauritâ-nia, Niger, Nigéria, República Democrático do Congo, Serra Leoa, Senegal, Tchad e Togo. Pela primeira vez T. abso-luta foi assinalada na Europa em 2006, e em Espanha na comunidade Valenciana em 2007 (Vieira, 2008). O cultivo de tomate em Cabo Verde tem aumentado nos últimos anos. Actualmente tomate é o legume mais cultivado em Cabo Verde. A sua quota parte na produção hortícola que não ultrapassavam os 1.000 t há uns anos, atinge actualmente 4200 t, o que representa 23% da produção total dos legumes. Apesar de alguns constrangimentos, nomeadamente problemas de ordem fitossanitária e escassez de água de rega a disponibi-lidade e a utilização generalizada das variedades locais, permitiram um escalonamento da produção durante o ano, compreendendo o período quente e húmido. Um outro fator que contri-bui para o aumento substancial da produção, é a salinização de água de rega, em várias zonas do regadio. Os agricultores destas zonas viram nesta cultura a única saída para obterem algum rendimento (MAP/ CPDA/INIDA/ FAO GCP/CV/036/NET s/data). Em Cabo Verde a área média de um campo de produção de tomate é de 750 m2 sendo máxima de 1.400 m2. Este trabalho teve como objetivo estabelecimento instantâneo de presença ou ausência da nova praga Tuta absoluta no país que foi recentemente encontrada na Sub-região Saariana na Costa Ocidental e Central de África.