Lineage divergence detected in the malaria vector Anopheles marajoara (Diptera: Culicidae) in Amazonian Brazil

Background: Cryptic species complexes are common among anophelines. Previous phylogenetic analysis based on the complete mtDNA COI gene sequences detected paraphyly in the Neotropical malaria vector Anopheles marajoara. The ""Folmer region"" detects a single taxon using a 3% divergence threshold. Methods: To test the paraphyletic hypothesis and examine the utility of the Folmer region, genealogical trees based on a concatenated (white + 3' COI sequences) dataset and pairwise differentiation of COI fragments were examined. The population structure and demographic history were based on partial COI sequences for 294 individuals from 14 localities in Amazonian Brazil. 109 individuals from 12 localities were sequenced for the nDNA white gene, and 57 individuals from 11 localities were sequenced for the ribosomal DNA (rDNA) internal transcribed spacer 2 (ITS2). Results: Distinct A. marajoara lineages were detected by combined genealogical analysis and were also supported among COI haplotypes using a median joining network and AMOVA, with time since divergence during the Pleistocene (< 100,000 ya). COI sequences at the 3' end were more variable, demonstrating significant pairwise differentiation (3.82%) compared to the more moderate 2.92% detected by the Folmer region. Lineage 1 was present in all localities, whereas lineage 2 was restricted mainly to the west. Mismatch distributions for both lineages were bimodal, likely due to multiple colonization events and spatial expansion (similar to 798 - 81,045 ya). There appears to be gene flow within, not between lineages, and a partial barrier was detected near Rio Jari in Amapa state, separating western and eastern populations. In contrast, both nDNA data sets (white gene sequences with or without the retention of the 4th intron, and ITS2 sequences and length) detected a single A. marajoara lineage. Conclusions: Strong support for combined data with significant differentiation detected in the COI and absent in the nDNA suggest that the divergence is recent, and detectable only by the faster evolving mtDNA. A within subgenus threshold of >2% may be more appropriate among sister taxa in cryptic anopheline complexes than the standard 3%. Differences in demographic history and climatic changes may have contributed to mtDNA lineage divergence in A. marajoara.

REPRODUCTIVE BIOLOGY AND FUNCTIONAL MATURITY IN FEMALES OF AEGLA FRANCA (DECAPODA: ANOMURA: AEGLIDAE)

We describe the reproductive period. fecundity, and average size at the onset of functional maturity of female Aegla franca, the northernmost distributed aeglid species. The reproductive period is markedly seasonal and takes place front May (austral mid-autumn) to August (late winter). Ovigerous females appear quite abruptly in the population by May, and this condition is observed in all adult females sampled regardless of their size. The average size at the onset of functional maturity in females, at which 50% of the females sampled during the reproductive period were considered adults, was 12.75 mm CL. The smallest post-ovigerous female measured 12.06 mm carapace length (CL). Mean fecundity (+/- S.D.) from 41 females bearing early and intermediate eggs was 129.1 +/- 32.2 and corresponded to a mean female CL of 14.11 mm. The elliptical-shaped eggs exhibited significant increase in size along the development stages. The third pair of pleopods bore higher number of eggs than the others. Compiled information regarding the reproductive period reported for aeglids revealed all increase in the breeding period length with latitude. The reproductive period tends to be shorter in localities under larger rainfall variation and smaller temperature variability than in sites with opposite climate conditions. Eggs tend to be fewer in number and larger in size towards lower latitudes. We present an hypothesis that stream water velocity might act as a major selective pressure during the early life history of fluvial aeglids with direct effect on the reproductive pattern.

Land-Water interactions in the amazon

Biogeochemistry is hosting this special thematic issue devoted to studies of land-water interactions, as part of the Large-scale Biosphere-Atmosphere Experiment in Amaznia (LBA). This compilation of papers covers a broad range of topics with a common theme of coupling land and water processes, across pristine and impacted systems. Findings highlighted that hydrologic flowpaths are clearly important across basin size and structure in determining how water and solutes reach streams. Land-use changes have pronounced impacts on flowpaths, and subsequently, on stream chemistry, from small streams to large rivers. Carbon is produced and transformed across a broad array of fluvial environments and wetlands. Surface waters are not only driven by, but provide feedback to, the atmosphere.

Lignin phenols used to infer organic matter sources to Sepetiba Bay - RJ, Brasil

Lignin phenols were measured in the sediments of Sepitiba Bay, Rio de Janeiro, Brazil and in bedload sediments and suspended sediments of the four major fluvial inputs to the bay: Sao Francisco and Guandu Channels and the Guarda and Cacao Rivers. Fluvial suspended lignin yields (Sigma 8 3.5-14.6 mgC 10 g dw(-1)) vary little between the wet and dry seasons and are poorly correlated with fluvial chlorophyll concentrations (0.8-50.2 mu gC L(-1)). Despite current land use practices that favor grassland agriculture or industrial uses, fluvial lignin compositions are dominated by a degraded leaf-sourced material. The exception is the Guarda River, which has a slight influence from grasses. The Lignin Phenol Vegetation Index, coupled with acid/aldehyde and 3.5 Db/V ratios, indicate that degraded leaf-derived phenols are also the primary preserved lignin component in the bay. The presence of fringe Typha sp. and Spartina sp. grass beds surrounding portions of the Bay are not reflected in the lignin signature. Instead, lignin entering the bay appears to reflect the erosion of soils containing a degraded signature from the former Atlantic rain forest that once dominated the watershed, instead of containing a significant signature derived from current agricultural uses. A three-component mixing model using the LPVI, atomic N:C ratios, and stable carbon isotopes (which range between -26.8 and -21.8 parts per thousand) supports the hypothesis that fluvial inputs to the bay are dominated by planktonic matter (78% of the input), with lignin dominated by leaf (14% of the input) over grass (6%). Sediments are composed of a roughly 50-50 mixture of autochthonous material and terrigenous material, with lignin being primarily sourced from leaf. (C) 2010 Elsevier Ltd. All rights reserved.

Facies, delta(13)C, delta(15)N and C/N analyses in a late Quaternary compound estuarine fill, northern Brazil and relation to sea level

The present work integrates sedimentary facies, (14)C dating, delta(13)C, delta(15)N, and C/N with geologic and geomorphologic data available from literature. The aim was to characterize the depositional settings of a late Quaternary estuary in northeastern Marajo Island and analyze its evolution within the context of relative sea level fluctuations. The data derive from four continuous cores along a proximal-to-distal transect of a paleoestuary, previously recognized using remote sensing information. Fifteen sediment samples recorded ages ranging from 42,580 +/- 1430 to 3184 +/- 37 (14)C yr B.P. Fades analysis indicated fine- to coarse-grained sands with parallel lamination or cross stratification, massive or laminated muds and heterolithic deposits. delta(13)C (-28.1 parts per thousand to -19.7 parts per thousand, mean = -23.0 parts per thousand), delta(15)N (+ 14.8 parts per thousand to + 4.7 parts per thousand, mean = + 9.2 parts per thousand) and C/N (14.5 to 1.5, mean = 7.9) indicate mostly marine and freshwater phytoplankton sources for the organic matter. The results confirm a large late Quaternary paleoestuary in northeastern Marajo Island. The distribution of delta(13)C, delta(15)N, and C/N, together with fades associations, led to identify depositional settings related to fluvial channel, floodplain, tidal channel/tidal flat, central basin, tidal delta, and tidal inlet/sand barrier. These deposits are consistent with a wave-dominated estuary. Variations in stratigraphy and geochemistry are controlled by changes in relative sea level, revealing a main transgression from an undetermined time around 42,000 (14)C yr B.P. and 29,340 (+/- 200) (14)C yr B.P., which is synchronous to the overall drop in sea level after the last interglacial. Following this period, and probably until 9110 +/- 37 (14)C yr B.P., i.e., during a time interval encompassing two glacial episodes including the Last Glacial and the Younger Dryas, there was a pronounced drop in sea level, recorded by the development of a major erosional discontinuity due to valley re-incision. Sea level rose again until 5464 +/- 40 (14)C yr B.P, just before the main worldwide mid-Holocene transgressive peak. Mid to late Holocene coastal progradation ended the Marajo paleoestuarine history, and promoted the establishment of continental conditions throughout the island. The divergence comparing the Marajo sea level behavior with the eustatic curve allows hypothesizing that post-rifting tectonics along the Brazilian Equatorial margin influenced the sedimentary evolution of the studied paleoestuary. Considering that sedimentary facies in estuarine settings are highly variable both laterally and vertically, the present integration of facies with isotope and elemental analyses was crucial to provide a more precise interpretation of the Late Pleistocene and Holocene Marajo paleoestuary, and analyze its sea level history within the eustatic and tectonic context. (C) 2010 Elsevier B.V. All rights reserved.

Quaternary paleoenvironments and relative sea-level changes in Marajo Island (Northern Brazil): Facies, delta(13)C, delta(15)N and C/N

The reconstruction of physical environments of Amazonian areas is of great interest to determine the dynamic evolution of the Amazon drainage basin. However. few studies have emphasized the Quaternary deposits in this region. which is mostly due to the lack of natural exposures imposed by the low topography. This work integrates facies analysis. radiocarbon dating, delta(13)C, delta(15)N, and C/N of an 124 m-thick core from an area located at the mouth of the Amazon River. northeastern Amazonia. The study records deposits up to 50.795 (14)C yr B P. in age. which formed in a variety of depositional environments including fluvial channel, tidal flat, outer estuarine basin to shallow marine. inner estuarine basin, estuarine channel and lagoon. Facies interpretation was significantly improved with the inclusion of delta(13)C, delta(15)N, and C/N analyses of organic matter extracted from the sediments The obtained values conform to a transitional. mostly estuarine paleosetting evolved during successive relative sea-level fluctuations. The results suggest fluvial deposition between 40,950 (+/- 590) and 50.795 (14)C yr B P, with a rise in relative sea level that commenced between 35,567 (+/- 649) and 39,079 (+/- 1114) (14)C yr B P. An overall transgression took place until 29,340 (+/- 340) (14)C yr B P., after which the relative sea level dropped, favoring valley rejuvenation and incision. Following this time up to 10,479 (+/- 34) (14)C yr B.P. a rise in relative sea level filled up the valley with estuarine deposits After 10.479(+/- 34) (14)C yr B.P., the estuary was replaced by a lagoon At the end of the Holocene, the coastline prograided approximately 45 km northward, replaci ng the lagoon by a lake system Despite the influence of eustatic fluctuations. regional tectonics played a significant role to create new space where these Late Pleistocene and Holocene sediments accumulated. (C) 2009 Elsevier B V All rights reserved.

TOPOGRAPHIC REGISTERS OF PALEO-VALLEYS ON THE SOUTHEASTERN BRAZILIAN CONTINENTAL SHELF

The evolution of paleo-incised-valleys in the Sao Paulo State region of the southeastern Brazilian continental shelf is presented in this study in relation to the post Last Glacial Maximum (LGM) sea-level rises based on the submarine topography modeled by a detailed Digital Elevation Model and evidences noted in high resolution seismic profiles. The hypothesis that has guided this study is that the set of paleo-valley characteristics (i.e. the fluvial parameters of modern coastal drainage systems, the topographical shape and dimensions of the valleys and of the subsurface channels) may indicate aspects of the relation between the influence of the fluvial and the eustatic variation regime in geomorphological-stratigraphic registers. Models described in the literature sustain the view that faster marine transgressions tend to increase erosion in estuaries, which may explain the lack of registers of paleo-drainage both in topography and the sub-surface in areas with wider shelves. On the other hand, on narrower shelves, with a higher slope angle, the transgression process can preserve, or even enhance, the incised valley registers during shoreface retreat. In the area studied, we observed that the dimensions and form of the continental shelf varies from the northern to the southern part of the area, affecting aspects of the geomorphological registers of the submerged incised valleys.

Disaggregation of polygons of surficial geology and soil maps using spatial modelling and legacy data

Examples from the Murray-Darling basin in Australia are used to illustrate different methods of disaggregation of reconnaissance-scale maps. One approach for disaggregation revolves around the de-convolution of the soil-landscape paradigm elaborated during a soil survey. The descriptions of soil ma units and block diagrams in a soil survey report detail soil-landscape relationships or soil toposequences that can be used to disaggregate map units into component landscape elements. Toposequences can be visualised on a computer by combining soil maps with digital elevation data. Expert knowledge or statistics can be used to implement the disaggregation. Use of a restructuring element and k-means clustering are illustrated. Another approach to disaggregation uses training areas to develop rules to extrapolate detailed mapping into other, larger areas where detailed mapping is unavailable. A two-level decision tree example is presented. At one level, the decision tree method is used to capture mapping rules from the training area; at another level, it is used to define the domain over which those rules can be extrapolated. (C) 2001 Elsevier Science B.V. All rights reserved.

Repeated flood events and fossil forests at Curio Bay (Middle Jurassic), New Zealand

During the Middle Jurassic, the regional environment of Curio Bay, southeast South Island, New Zealand, was a fluvial plain marginal to volcanic uplands. Intermittent flashy, poorly-confined flood events buried successive conifer forests. With the termination of each flood, soils developed and vegetation was reestablished. In most cases, this developed into coniferous forest. In approximately 40 m of vertical section, 10 fossil forest horizons can be distinguished, highlighting a type of fluvial architecture which is poorly documented. Flood-basin material is minimal, but a short-Lived floodbasin lake is inferred to have developed within the interval of study. Paleocurrent indicators suggest enclosure of the basin on more than one side. Sedimentation style suggests a relatively dry (less than humid but not arid) climate with seasonal rainfall. (C) 2001 Elsevier Science B.V. All rights reserved.

Boletim eletr??nico de bibliografias especializadas: meio ambiente e sustentabilidade

A 3a edi????o de 2013 do Boletim Eletr??nico de Bibliografias Especializadas re??ne publica????es do acervo da Biblioteca Graciliano Ramos com a tem??tica Meio Ambiente e Sustentabilidade, por ocasi??o do Dia Mundial do Meio Ambiente, comemorado anualmente em 5 de junho. A data busca chamar a aten????o e a a????o pol??tica de povos e pa??ses a fim de aumentar a conscientiza????o e a preserva????o ambiental. A divulga????o das publica????es a seguir - que tratam de ecologia, saneamento b??sico, polui????o, desenvolvimento sustent??vel, economia verde, gest??o ambiental, entre outros - tem como expectativa apoiar a forma????o e a capacita????o de servidores p??blicos, bem como a aplica????o desse conhecimento em pol??ticas p??blicas, em benef??cio da popula????o

Saberes em gest??o p??blica: um ambiente colaborativo de constru????o do conhecimento e de dissemina????o das inova????es em gest??o p??blica

Apresenta o SabeRES em Gest??o P??blica (www.saberes.seap.pr.gov.br), um reposit??rio institucional de acesso livre, aberto a todos os temas relativos ?? gest??o nas organiza????es p??blicas, com ampla tipologia multim??dia de documentos. Inserida no Movimento Mundial do Open Access, dos Recursos Educacionais Abertos e da Ecologia do Conhecimento (pol??tica de compartilhamento), a Escola de Governo do Paran?? desenvolveu, em 2008, um espa??o digital de armazenamento, preserva????o, divulga????o e acesso ?? produ????o do conhecimento em Gest??o P??blica. A metodologia constou de uma an??lise SWOT, seguida de planejamento gr??fico e estrutural, defini????o da arquitetura (conte??do e forma), constru????o da interface gr??fica com ferramenta XOOPS (software livre) e defini????o da ??rvore inicial de menus. Ap??s a constru????o da arquitetura da informa????o come??ou o treinamento da equipe para a gest??o e a manuten????o, a inser????o dos documentos (publica????es, artigos, v??deos, materiais de curso), a disponibiliza????o e a difus??o na Internet, a constitui????o de C??mara T??cnica para apreciar os documentos recebidos e a gest??o continuada do SabeRES. Definiu-se que no SabeRES em Gest??o P??blica ser??o inclu??das publica????es em gest??o p??blica de outros Estados, do Conselho Nacional de Secret??rios de Estado da Administra????o (CONSAD) e da Rede Nacional de Escolas de Governo. A tend??ncia ?? que num futuro pr??ximo seja poss??vel oportunizar o auto-arquivamento dos documentos, preenchendo os metadados relacionados ao seu tema. Al??m disso, espera-se que o sistema estabelecido pela Institui????o seja compat??vel e gere interoperabilidade com o portal de reposit??rios O??sis do Instituto Brasileiro de Informa????o em Ci??ncia e Tecnologia (IBICT) / Minist??rio da Ci??ncia e Tecnologia. Partindo do princ??pio que s?? se cria conhecimento novo a partir da informa????o que est?? acess??vel, com a cria????o do SabeRES em Gest??o P??blica amplia-se a visibilidade e a acessibilidade da produ????o do conhecimento, para que se produza cada vez mais e com mais qualidade

Base flutuante de fiscaliza????o federal integrada

Este projeto consiste na celebra????o de conv??nios entre a Superintend??ncia Regional da Secretaria da Receita Federal no Par?? com as principais institui????es envolvidas nas atividades de policiamento da Amaz??nia, visando reduzir a pr??tica do contrabando, narcotr??fico e a devasta????o do meio-ambiente causada pela extra????o indiscriminada de madeiras. O conv??nio foi celebrado entre a Pol??cia Federal, IBAMA, SUFRAMA e Secretaria de Estado da Fazenda. No munic??pio de ??bidos ??? PA, por onde passam todas as embarca????es procedentes da Zona Franca de Manaus com destino ??s cidades de Santar??m e Bel??m ??? PA, foi constru??da uma base flutuante denominada Candiru, a qual se constitui em um eficiente mecanismo de vigil??ncia e repress??o ?? pr??tica do contrabando via fluvial

Prevbarcos: estrat??gia de inclus??o pela Previd??ncia Social

Este estudo de caso faz an??lise do programa Prevbarco, Unidade M??vel Flutuante da Previd??ncia Social, no qual barcos navegam pelos rios da bacia amaz??nica, prestando servi??os previdenci??rios para as comunidades locais - ribeirinhas, quilombolas, extrativistas, ind??genas entre outras - que n??o t??m acesso adequado aos servi??os oferecidos pelas unidades fixas da Previd??ncia Social localizadas nas ??reas urbanas. Faz-se a descri????o do tipo de servi??o prestado pelos Prevbarcos, que desenvolve a inclus??o social e cidadania da popula????o assistida, assim como identifica dificuldades nessa presta????o que se caracteriza desde a contrata????o dos servidores que se voluntariam para os longos percursos de barco, passando pela falta de conhecimento da popula????o sobre cidadania e seus direitos previdenci??rios. A partir deste caso, espera-se reflex??o dos servidores sobre motiva????o para pr??ticas inovadoras e, pelo estudo em quest??o, releva-se a necessidade de pensar e formular pol??ticas p??blicas que atendam, de fato, ??s necessidades de benefici??rios e cidad??os

Morfologia e distribuição sedimentar em um sistema estuarino tropical : Baía de Vitória, ES

A Baía de Vitória é um sistema estuarino da costa leste do Brasil que apresenta grande importância econômica e características ímpares, já que se desenvolveu entre três unidades geomorfológicas distintas. Apesar disto, este ambiente apresenta poucos estudos relacionados às suas características geológicas e oceanográficas. O presente trabalho se focou no preenchimento desta lacuna através da descrição da morfologia, da distribuição sedimentar e dos padrões sonográficos da Baía de Vitória, buscando relações entre os mesmos e inferindo os processos sedimentares dominantes em cada trecho do estuário. A análise integrada mostrou boa correlação entre os métodos e revelou a grande complexidade deste sistema estuarino. Três diferentes regiões foram identificadas mostrando processos distintos: o estuário superior apresentou input sedimentar fluvial e processos estuarinos; um largo trecho da região central do sistema apresentou características erosivas, relacionadas a adaptações morfológicas e ao aumento das correntes provocadas pelos estreitamentos artificiais da baía, propiciando a formação de formas de fundo; e a boca do estuário se apresentou dominada por processos marinhos. Parte da região central do estuário mostrou características mascaradas pela atividade antrópica através da instalação de pontes, aterros e dragagens.