Genetic variability of Aedes aegypti in the Americas using a mitochondrial gene: evidence of multiple introductions

To analyze the genetic relatedness and phylogeographic structure of Aedes aegypti, we collected samples from 36 localities throughout the Americas (Brazil, Peru, Venezuela, Guatemala, US), three from Africa (Guinea, Senegal, Uganda), and three from Asia (Singapore, Cambodia, Tahiti). Amplification and sequencing of a fragment of the mitochondrial NADH dehydrogenase subunit 4 gene identified 20 distinct haplotypes, of which 14 are exclusive to the Americas, four to African/Asian countries, one is common to the Americas and Africa, and one to the Americas and Asia. Nested clade analysis (NCA), pairwise distribution, statistical parsimony, and maximum parsimony analyses were used to infer evolutionary and historic processes, and to estimate phylogenetic relationships among haplotypes. Two clusters were found in all the analyses. Haplotypes clustered in the two clades were separated by eight mutational steps. Phylogeographic structure detected by the NCA was consistent with distant colonization within one clade and fragmentation followed by range expansion via long distance dispersal in the other. Three percent of nucleotide divergence between these two clades is suggestive of a gene pool division that may support the hypothesis of occurrence of two subspecies of Ae. aegypti in the Americas.

Sylvatic triatominae: a new challenge in vector control transmission

Over the last 10 years, Uruguay, Chile and Brazil have been certified as being free from disease transmission by Triatoma infestans, the main domiciliated vector for Chagas disease in the Southern Cone countries. This demonstrates that programmes addressing the vector for the disease's transmission are effective. These programmes have resulted in a dramatic decrease in the incidence of Chagas disease in Latin America. Guatemala was certified a few months ago as being free from disease transmission by Rhodnius prolixus, the main domiciliated vector for Chagas disease in Central American countries. However, the main concern for different countries' current control programmes is the continuity and sustainability of future vector control actions. The prevalence and incidence figures for individuals infected by Trypanosoma cruzi in Mexico and Andean and Central American countries highlights the need for broadened strategies in the struggle against the disease and its vectors. A number of triatomine insects are parasite vectors, each with a different life history. Therefore, it is important that new vector control strategies be proposed, keeping in mind that some species are found in peridomiciliary areas and wild ecotopes. The only viable control strategy is to reduce human interactions with vector insects so that the re-infestation and re-colonisation of human habitats will not take place.

Reorganization of a deeply incised drainage: role of deformation, sedimentation and groundwater flow

Deeply incised drainage networks are thought to be robust and not easily modified, and are commonly used as passive markers of horizontal strain. Yet, reorganizations (rearrangements) appear in the geologic record. We provide field evidence of the reorganization of a Miocene drainage network in response to strike-slip and vertical displacements in Guatemala. The drainage was deeply incised into a 50-km-wide orogen located along the North America-Caribbean plate boundary. It rearranged twice, first during the Late Miocene in response to transpressional uplift along the Polochic fault, and again in the Quaternary in response to transtensional uplift along secondary faults. The pattern of reorganization resembles that produced by the tectonic defeat of rivers that cross growing tectonic structures. Compilation of remote sensing data, field mapping, sediment provenance study, grain-size analysis and Ar(40)/Ar(39) dating from paleovalleys and their fill reveals that the classic mechanisms of river diversion, such as river avulsion over bedrock, or capture driven by surface runoff, are not sufficient to produce the observed diversions. The sites of diversion coincide spatially with limestone belts and reactivated fault zones, suggesting that solution-triggered or deformation-triggered permeability have helped breaching of interfluves. The diversions are also related temporally and spatially to the accumulation of sediment fills in the valleys, upstream of the rising structures. We infer that the breaching of the interfluves was achieved by headward erosion along tributaries fed by groundwater flow tracking from the valleys soon to be captured. Fault zones and limestone belts provided the pathways, and the aquifers occupying the valley fills provided the head pressure that enhanced groundwater circulation. The defeat of rivers crossing the rising structures results essentially from the tectonically enhanced activation of groundwater flow between catchments.

Revisão do gênero Sympleurotis Bates (Coleoptera, Cerambycidae, Lamiinae, Colobotheini)

Sympleurotis Bates, 1881 é revisto. Sympleurotis rudis Bates, 1881 e S. armatus Gahan, 1892 são redescritos e acrescentam-se duas espécies novas: S. wappesi sp. nov., da Guatemala e S. albofasciatus sp. nov., do México. São fornecidas ilustrações e chave de identificação para as espécies.

Sinopse do gênero Eucharassus Bates (Coleoptera, Cerambycidae)

O gênero Eucharassus é redescrito e chave para as espécies é fornecida. São descritas quatro novas espécies: Eucharassus hovorei sp. nov. e E. lingafelteri sp. nov. da Costa Rica, E. chemsaki sp. nov. do Panamá e E. wappesi sp. nov. do Panamá e Guatemala.

Clytini neotropicais II (Coleoptera, Cerambycidae, Cerambycinae)

Novas espécies são descritas e figuradas: Megacyllene (M.) nevermanni sp. nov. da Costa Rica (Limón); M. (M.) punensis sp. nov. do Peru (Puno); Neoclytus fraterculus sp. nov. da Venezuela (Guárico); N. zonatus da Guatemala (Alta Verapaz); N. vitellinus sp. nov. da Costa Rica (Guanacaste); Mecometopus erratus sp. nov. da Colômbia (Boyacá); M. latithorax sp. nov. do Panamá (Panamá).

Novos táxons em Onciderini (Coleoptera, Cerambycidae, Lamiinae)

Novos táxons descritos: Oncideres sparsemaculatus sp. nov., da Guatemala (San Marcos); Oncideres estebani sp. nov. da Costa Rica (Alajuela); Neohylus alexandrei sp. nov. e Hypsioma bahiensis, sp. nov. do Brasil (Rondônia e Bahia, respectivamente); Paraplerodia gen. nov., espécie-tipo, P. acarinata sp. nov., Hesycha biguttata sp. nov., Trestonia lateapicata sp. nov. e Pseudobeta transversa sp. nov. da Bolívia (Santa Cruz).

Novos táxons em Elaphidionini e Eburiini (Cerambycidae, Cerambycinae)

São descritos novos táxons em Cerambycinae, Elaphidionini: Parapantonyssus gen. nov., espécie-tipo, P. ipiri sp. nov. da Guatemala (San Marcos); Aposphaerion nigritum sp. nov. da Bolívia. Em Eburiini: Beraba tate sp. nov., da Bolívia; Eburodacrys translucida do Brasil (Paraíba); E. errata sp. nov. e E. fraterna sp. nov. da Bolívia.

Report CR-A-219-B - Cabo Verde Estudo do Sector Agrícola

A. A Singularidade de Cabo Verde Cabo Verde e unica entre a familia de na90es. ~ uma republica de ilhas (Fig. 1.1) suficientemente distanciadas umas das outras e do continente africano (600 km) para dissuadir visitas imprevistas ou fortuitas. Seu isolamento serviu para fortalecer sua singular cultura crioula, porem a cllsta de contactos frequentes com influencias e inforrna90es externas. Cabo Verde e muito pequeno. Sua popula9ao de 300.000 habitantes, que mal chegaria para tornar uma cidade auto-suficiente num complexo industrial, esta dividida entre nove ilhas. A capital, Praia, conta somente com 23.000 habitantes, e e, essencialmente, urna pequena e simpatica cidade onde a maior parte dos vercursos pode ser feita a pe e onde encontros casuais entre funcionarios do governo sao provavelmente tao irnportantes quanto os formais meios de comunica9ao pelo telefone ou por escrito. Cabo Verde e tambem pequeno ern termos de area territorial, embora ocupe urna area relativamente grande de ocea~o. Sua superficie total e pouco mais de 4.000 km2 , porem suas nove ilhas principais estao espalhadas por uma POr9aO grande, quadrangular, do Atlantico medindo aproximadamente 240 qUilometros de urn lado. A superficie total (nao incluindo partes da plataforma continental que se estende para alem do litoral externo das ilhas) e comparavel as republicas de Togo ou Sri Lanka, ou cerca de metade da Guatemala. A nao ser pelo servi90 de barcas entre Fogo e Brava, e entre Sao Vicente e Santo Antao, as ilhas estao demasiado distantes entre si para urn conveniente transporte maritimo. Avioes sao, portanto, essenciais as comunica90es e trafego entre as ilhas, embora para transac90es lentas e volurnosas 0 transporte maritimo, seja por embarca90es a vela ou a motor, e sempre urna alternativa devido aos ventos constantes e condi90es atmosfericas geralmente boas.

Novas espécies de Esthlogena s. str. Thomson (Coleoptera, Cerambycidae, Lamiinae)

Novas espécies de Esthlogena s. str. Thomson (Coleoptera, Cerambycidae, Lamiinae). Novas espécies de Pteropliini descritas: Esthlogena (E.) nigrosuturalis do México e Panamá; E. (E.) chicacaoensis e E. (E.) amaliae da Guatemala; E. (E.) dissimilis do Peru. Todas as espécies são ilustradas.

Guatemalan lestadiolaisuudesta

Summary: Apostolic-Lutheran Church in Guatemala

Las rutas del libro atlántico: libros enviados en el navío de Honduras (1557-1700)

En este trabajo se analizan los envíos de libros en el navío de Honduras, que viajaba entre Sevilla y los puertos atlánticos de la costa centroamericana. Examinamos una muestra de 52 registros de navíos, que suponen un 20% del total. Esto nos ha permitido localizar lotes de libros declarados en 34 barcos, en los que se han encontrado 130 envíos de libros. Este conjunto ayuda a detectar las claves del circuito de llegada de los libros, muy poco conocido, por medio de comerciantes, libreros y particulares. El estudio de los intermediarios también permitió localizar algunas de las redes que intervienen en ese tráfico de libros. Por último, el estudio de los títulos embarcados ha llevado a encontrar una muestra significativa de los textos impresos en Europa que llegaron en los siglos XVI y XVII al área de Guatemala y Honduras.

Ophiolite-related ultramafic rocks (Serpentinites) in the Caribbean region: a review of their occurrence, composition, origin, emplacements and Ni-Laterite soil formation

Ultramafic rocks, mainly serpentinized peridotites of mantle origin, are mostly associated with the ophiolites of Mesozoic age that occur in belts along three of the margins of the Caribbean plate. The most extensive exposures are in Cuba. The ultramafic-mafic association (ophiolites) were formed and emplaced in several different tectonic environments. Mineralogical studies of the ultramafic rocks and the chemistry of the associated mafic rocks indicate that most of the ultramafic-mafic associations in both the northern and southern margins of the plate were formed in arc-related environments. There is little mantle peridotite exposed in the ophiolitic associations of the west coast of Central America, in the south Caribbean in Curacao and in the Andean belts in Colombia. In these occurrences the chemistry and age of the mafic rocks indicates that this association is mainly part of the 89 Ma Caribbean plateau province. The age of the mantle peridotites and associated ophiolites is probably mainly late Jurassic or Early Cretaceous. Emplacement of the ophiolites possibly began in the Early Cretaceous in Hispaniola and Puerto Rico, but most emplacement took place in the Late Cretaceous to Eocene (e.g. Cuba). Along the northern South America plate margin, in the Caribbean mountain belt, emplacement was by major thrusting and probably was not completed until the Oligocene or even the early Miocene. Caribbean mantle peridotites, before serpentinization, were mainly harzburgites, but dunites and lherzolites are also present. In detail, the mineralogical and chemical composition varies even within one ultramafic body, reflecting melting processes and peridotite/melt interaction in the upper mantle. At least for the northern Caribbean, uplift (postemplacement tectonics) exposed the ultramafic massifs as a land surface to effective laterization in the beginning of the Miocene. Tectonic factors, determining the uplift, exposing the peridotites to weathering varied. In the northern Caribbean, in Guatemala, Jamaica, and Hispaniola, uplift occurred as a result of transpresional movement along pre-existing major faults. In Cuba, uplift occurred on a regional scale, determined by isostatic adjustment. In the south Caribbean, uplift of the Cordillera de la Costa and Serrania del Interior exposing the peridotites, also appears to be related to strike-slip movement along the El Pilar fault system. In the Caribbean, Ni-laterite deposits are currently being mined in the central Dominican Republic, eastern Cuba, northern Venezuela and northwest Colombia. Although apparently formed over ultramafic rocks of similar composition and under similar climatic conditions, the composition of the lateritic soils varies. Factors that probably determined these differences in laterite composition are geomorphology, topography, drainage and tectonics. According to the mineralogy of principal ore-bearing phases, Dominican Ni-laterite deposits are classified as the hydrous silicate-type. The main Ni-bearing minerals are hydrated Mg-Ni silicates (serpentine and ¿garnierite¿) occurring deeper in the profile (saprolite horizon). In contrast, in the deposits of eastern Cuba, the Ni and Cooccurs mainly in the limonite zone composed of Fe hydroxides and oxides as the dominant mineralogy in the upper part of the profile, and are classified as the oxide-type.

Upper Triassic to Cretaceous radiolaria from Nicaragua and northern Costa Rica - The Mesquito composite oceanic terrane

We propose a new terrane subdivision of Nicaragua and Northern Costa Rica, based on Upper Triassic to Upper Cretaceous radiolarian biochronology of ribbon radiolarites, the newly studied Siuna Serpentinite Mélange, and published 40Ar/39Ar dating and geochemistry of mafic and ultramafic igneous rock units of the area. The new Mesquito Composite Oceanic Terrane (MCOT) comprises the southern half of the Chortis Block, that was assumed to be a continental fragment of N-America. The MCOT is defined by 4 corner localities characterized by ultramafic and mafic oceanic rocks and radiolarites of Late Triassic, Jurassic and Early Cretaceous age: 1. The Siuna Serpentinite Mélange (NE-Nicaragua), 2. The El Castillo Mélange (Nicaragua/Costa Rica border), 3.The Santa Elena Ultramafics (N-Costa Rica) and, 4. DSDP Legs 67/84. 1. The Siuna Serpentinite Mélange contains, high pressure metamorphic mafics and Middle Jurassic (Bajocian-Bathonian) radiolarites in original, sedimentary contact with arc-metandesites. The Siuna Mélange also contains Upper Jurassic black detrital chert formed in a marginal (fore-arc?) basin shortly before subduction. A phengite 40Ar/39Ar -cooling age dates the exhumation of the high pressure rocks as 139 Ma (earliest Cretaceous). 2. The El Castillo Mélange comprises a radiolarite block tectonically embedded in serpentinite that yielded a diverse Rhaetian (latest Triassic) radiolarian assemblage, the oldest fossils recovered so far from S-Central America. 3. The Santa Elena Ultramafics of N-Costa Rica together with the serpentinite outcrops near El Castillo (2) in Southern Nicaragua, are the southernmost outcrops of the MCOT. The Santa Elena Unit (3) itself is still undated, but it is thrust onto the middle Cretaceous Santa Rosa Accretionary Complex (SRAC), that contains Lower to Upper Jurassic, highly deformed radiolarite blocks, probably reworked from the MCOT, which was the upper plate with respect to the SRAC. 4. Serpentinites, metagabbros and basalts have long been known from DSDP Leg 67/84 (3), drilled off Guatemala in the Nicaragua-Guatemala forearc basement. They have been restudied and reveal 40Ar/39Ar dated Upper Triassic to middle Cretaceous enriched Ocean Island Basalts and Jurassic to Lower Cretaceous depleted Island arc rocks of probable Pacific origin. The area between localities 1-4 is largely covered by Tertiary to Recent arcs, but we suspect that its basement is made of oceanic/accreted terranes. Earthquake seismic studies indicate an ill-defined, shallow Moho in this area. The MCOT covers most of Nicaragua and could extend to Guatemala to the W and form the Lower (southern) Nicaragua Rise to the NE. Some basement complexes of Jamaica, Hispaniola and Puerto Rico may also belong to the MCOT. The Nicoya Complex s. str. has been regarded as an example of Caribbean crust and the Caribbean Large Igneous Province (CLIP). However, 40Ar/39Ar - dates on basalts and intrusives indicate ages as old as Early Cretaceous. Highly deformed Jurassic and Lower Cretaceous radiolarites occur as blocks within younger intrusives and basalts. Our interpretation is that radiolarites became first accreted to the MCOT, then became reworked into the Nicoya Plateau in Late Cretaceous times. This implies that the Nicoya Plateau formed along the Pacific edge of the MCOT, independent form the CLIP and most probably unrelated with he Galapagos hotspot. No Jurassic radiolarite, no older sediment age than Coniacian-Santonian, and no older 40Ar/39Ar age than 95 Ma is known from S-Central America between SE of Nicoya and Colombia. For us this area represents the trailing edge of the CLIP s. str.