Paleoambiente e diagênese da formação Itaituba, carbonífero da bacia do Amazonas, com base em testemunho de sondagem, região de Uruará, Pará

A Formação Itaituba de idade carbonífera representa a sedimentação carbonática de depósitos transgressivos do Grupo Tapajós da Bacia do Amazonas. A sucessão Itaituba é interpretada como depósitos de planície de maré mista, constituídos de calcários fossilíferos, dolomitos finos, arenitos finos a grossos e subordinadamente siltitos avermelhados, evaporitos e folhelhos negros. A análise de fácies e microfácies do testemunho de sondagem da região de Uruará, Estado do Pará, permitiu individualizar dezenove fácies agrupadas em cinco associações: planície de maré (AF1), canal de maré (AF2), laguna (AF3), barra bioclástica (AF4) e plataforma externa (AF5). AF1 é composta por arenito fino com rip-up clasts e gretas de contração, marga com grãos de quartzo e feldspato, dolomudstone laminado com grãos terrígenos e dolomito fino silicificado, com intercalação de argilito com grãos de quartzo disseminados, dolomitizado e localmente com sílica microcristalina. AF2 consiste em arenito médio a grosso com estratificação cruzada acanalada, recoberta por filmes pelíticos nos foresets, arenito muito fino a fino com acamamento wavy, siltito laminado com falhas sinsedimentares e acamamento convoluto. AF3 é constituída de siltito vermelho maciço, mudstone com fósseis, floatstone com braquiópodes e pirita disseminada e mudstone maciço com frequentes grãos de quartzo. AF4 e AF5 exibem abundantes bioclastos representados por espinhos e fragmentos de equinodermas, conchas, fragmentos e espinhos de braquiópodes, ostracodes, foraminíferos, algas vermelhas e conchas de bivalves. AF4 é formada por grainstone oolítico fossilífero e grainstone com terrígenos principalmente grãos de quartzo monocristalino e AF5 se compõe de wackestone fossilífero, wackestone com terrígenos e mudstone maciço com grãos de quartzo monocristalino. Subarcósios (AF1), arcósios (AF2) e arcósios líticos (AF2) são os tipos de arenitos da sucessão Itaituba e apresentam como principais constituintes grãos de quartzo monocristalino e policristalino, K-feldspato, plagioclásio, pirita, muscovita detrítica, fragmento de rocha pelítica, metamórfica e chert e raros bioclastos. O cimento é de calcita espática não ferrosa, óxido/hidróxido de ferro e sobrecrescimento de sílica. A porosidade é intergranular, móldica e às vezes alongada, sem permeabilidade perfazendo até 11% da rocha. Os processos diagenéticos dos arenitos são compactação física, sobrecrescimento de sílica, cimentação de calcita, formação de matriz diagenética, compactação química, substituição de grãos, autigênese de pirita, formação de óxido/hidróxido de ferro e alteração do plagioclásio. Os processos diagenéticos dos carbonatos são: micritização, neomorfismo, colomitização, fraturamento, compactação química, cimentação de calcita, dissolução secundária e autigênese de minerais. A sucessão da Formação Itaituba representa um sistema de laguna/planície de maré ligada a uma plataforma marinha carbonática. Planícies de maré desenvolveram-se nas margens das lagunas e eram periodicamente supridas por influxos de terrígenos finos (silte) que inibiam a precipitação carbonática. Barras bioclásticas eram cortadas por canais de maré (inlet) que conectavam a laguna com a plataforma rasa rica em organismos bentônicos.

Geologia e paleontologia do biohermito da Formação Pirabas (Mioceno Inferior)

O presente trabalho compreende o estudo geológico e paleontológico detalhado da litofácies recifal da Formação Pirabas, Estado do Pará, aflorante na Praia do Maçarico, município de Salinópolis, como um corpo pequeno, isolado e lenticular, que deve ter se desenvolvido na rampa interna da plataforma do Mar de Pirabas. O conteúdo biótico é rico e variado, composto por três grupos de algas coralíneas, poríferos, corais, briozoários, equinoides, foraminíferos, ostracodes, e moluscos. Foram reconhecidos neste recife em mancha três estágios de sucessão ecológica, estabilização, colonização e diversificação, onde as finas crostas micríticas reconhecidas na parte superior do estágio diversificação indicam degradação das condições ambientais favoráveis à acreção recifal, provavelmente devido a continentalização do sítio deposicional. O exame petrográfico revelou apenas uma microfácies deposicional, biomicrito, sem consideráveis variações texturais e composicionais. A cimentação marinha é predominante, representada por massas microcristalinas e cimentos micríticos, localmente neomorfisados para bioesparito, e detritos carbonáticos advindos do fluxo biogênico inconsolidado, resultantes principalmente da dispersão de cristais de aragonita dos fragmentos algálicos, acumulados sob a forma de lama micrítica. Para a gênese da bioconstrução as algas foram fundamentais na consolidação e modelagem do arcabouço, principalmente as macroalgas vermelhas, decisivas para a proteção e cimentação dos demais organismos.

Liquens de Mato Grosso do Sul: estudo químico e avaliação da atividade biológica

Pós-graduação em Química - IQ

Composição e diversidade dos camarões marinhos (Crustacea: Decapoda: Penaeoidea) e dinâmica populacional de Xiphopenaeus kroyeri (Heller, 1862) no litoral do Brasil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Distribuição ecológica e dinâmica populacional do camarão barriga branca Nematopalaemon schmitti (Holthuis, 1950) (Caridea, Palaemonidae) na região de Macaé-RJ, Brasil

Pós-graduação em Ciências Biológicas (Zoologia) - IBB

Revisão das seções Acarporophytum, Aristata e Macrospora do gênero Batrachospermum (Rhodophyta, Batrachospermales)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Ocorrência de algas cianofíticas em água de dessedentação de bovinos criados extensivamente

In extensive animal husbandry, natural or artificial ponds allow direct access of cattle to water but result in degradation of water quality and in increased health risks. Under such circumstances eutrophication occurs and consequently algal bloom, among them toxigenic cyanobacteria. The present study aimed to report the occurrence of cyanobacteria in the drinking water of cattle and to describe their physical and chemical parameters, as pH, temperature and dissolved oxygen. Nineteen samples of natural ponds or water troughs formed predominantly as result of rainfall from six farms located in the Southeast and Midwest regions of Brazil were analyzed for the presence of cyanobacteria, and pH, temperature and dissolved oxygen was measured. Microcystis and/or Merismopedia were detected in two ponds; one of them was covered with intense flowering. The values of pH, temperature and dissolved oxygen in 19 collections were pH 7.2-9.7, 31-34ºC and 7.8-30mg/l respectively. Also non-pathogenic algae of several genera were detected besides the occurrence or not of cianogenics. Under these conditions, the common practices of drinking water supply for extensively raised cattle and the possibilities of eutrophication and cyanobacterial growth bring potential risks for animal health.

Progressive recovery of a tropical deforested stream community after a flash flood

AIM: In this study, we evaluated and compared community attributes from a tropical deforested stream, located in a pasture area, in a period before (PRED I) and three times after (POSD I, II, and III) a flash flood, in order to investigate the existence of temporal modifications in community structure that suggests return to conditions previous to the flash flood. METHODS: Biota samples included algae, macrophytes, macroinvertebrates, and fish assemblages. Changes in stream physical structure we also evaluated. Similarity of the aquatic biota between pre and post-disturbance periods was examined by exploratory ordination, known as Non-Metric Multidimensional Scaling associated with Cluster Analysis, using quantitative and presence/absence Bray-Curtis similarity coefficients. Presence and absence data were used for multivariate correlation analysis (Relate Analysis) in order to investigate taxonomic composition similarity of biota between pre and post-disturbance periods. RESULTS: Our results evidenced channel simplification and an expressive decrease in richness and abundance of all taxa right after the flood, followed by subsequent increases of these parameters in the next three samples, indicating trends towards stream community recovery. Bray-Curtis similarity coefficients evidenced a greater community structure disparity among the period right after the flood and the subsequent ones. Multivariate correlation analysis evidenced a greater correlation between macroinvertebrates and algae/macrophytes, demonstrating the narrow relation between their recolonization dynamics. CONCLUSIONS: Despite overall community structure tended to return to previous conditions, recolonization after the flood was much slower than that reported in literature. Finally, the remarkably high flood impact along with the slow recolonization could be a result of the historical presence of anthropic impacts in the region, such as siltation, riparian forest complete depletion, and habitat simplification, which magnified the effects of a natural disturbance.

Effects of some parameters in upscale culture of Haematococcus pluvialis Flotow

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Cyanobacteria detection in Guarapiranga Reservoir (São Paulo State, Brazil) using Landsat TM and ETM+ images

Algae bloom is one of the major consequences of the eutrophication of aquatic systems, including algae capable of producing toxic substances. Among these are several species of cyanobacteria, also known as blue-green algae, that have the capacity to adapt themselves to changes in the water column. Thus, the horizontal distribution of cyanobacteria harmful algae blooms (CHABs) is essential, not only to the environment, but also for public health. The use of remote sensing techniques for mapping CHABs has been explored by means of bio-optical modeling of phycocyanin (PC), a unique inland waters cyanobacteria pigment. However, due to the small number of sensors with a spectral band of the PC absorption feature, it is difficult to develop semi-analytical models. This study evaluated the use of an empirical model to identify CHABs using TM and ETM+ sensors aboard Landsat 5 and 7 satellites. Five images were acquired for applying the model. Besides the images, data was also collected in the Guarapiranga Reservoir, in São Paulo Metropolitan Region, regarding the cyanobacteria cell count (cells/mL), which was used as an indicator of CHABs biomass. When model values were analyzed excluding calibration factors for temperate lakes, they showed a medium correlation (R²=0.81, p=0.036), while when the factors were included the model showed a high correlation (R²=0.96, p=0.003) to the cyanobacteria cell count. The empirical model analyzed proved useful as an important tool for policy makers, since it provided information regarding the horizontal distribution of CHABs which could not be acquired from traditional monitoring techniques.

Shading effects on community composition and food web structure of a deforested pasture stream: Evidences from a field experiment in Brazil

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Variance partitioning of deconstructed periphyton communities: does the use of biological traits matter?

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Performance evaluation of multi-stage filtration with use of granular activated carbon and synthetic non-woven fabrics

The multi stage filtration (MSF) is an alternative that permits to enlarge the spectrum of application of the slow sand filtration as for the effluent quality and run duration. In this research the use of MSF technology associated to a granular activated carbon (GAC) column as polishing mechanism of the final effluent was evaluated; in the slow sand filters GAC was used as an intermediate layer and non-woven synthetic fabrics were utilized as a first layer of the filter media. Five different tests were conducted, where the systems subjected to the treatment were: water from the Ipe Lake (Ilha Solteira, Sao Paulo, Brazil); water from the lake with water from a recreational fish pond; water from the lake with a phytoplankton and cyanobacteria overload simulation, with and without the use of the pre-filters as a stage of the treatment. The synthetic fabrics and GAC use resulted in the best turbidity removal and an efficient apparent and true color removal; in spite that the polishing columns reported similar results for those parameters. The utilization of GAC as an intermediate layer contributed to a better organic matter removal and the fabrics improved chlorophyll-a removal. The pre-filtration columns made an efficient algae and cyanobacteria removal, a function that was completed by the filters and reached >98% efficiency. The synthetic non-woven fabrics and GAC inclusion in MSF operation improved performance of this technology with ease of application and operation.

Cyanobacteria, microcystins and cylindrospermopsin in public drinking supply reservoirs of Brazil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

The plants by Daniel Rolander (c. 1723-1793) in Diarium Surinamicum (1754-1765) and herbaria

The manuscripts of Diarium Surinamicum by Daniel Rolander practically remained ignored and unpublished for over 240 years, till the recent publication of its translation into English, which occurred in 2008. In this, the names of species described and/or cited by Rolander were faithfully retained, hence preserving the indication of them without authorship, for the vast majority. In the present work, all the names of plants that were treated by Rolander in his journal, about 664, including by tradition the fungi and algae, are contextualised in relation to the authorship, reference to the publication of the protologue, pagination of citations/descriptions in the manuscripts and in the published translation, indication of probable misidentifications with possible alternative names, vernacular names, and related literature. Additionally, we searched for the vouchers collected by Rolander, scattered in several herbaria, which have been linked to the probable names and descriptions in the diary. Given the considerable time till the publication of these names, and by the lack of indication of their nomenclatural types in the English version, the great majority of the new species described by Rolander, which would have priority if published in due time, became invalid names according to the ICN. Nevertheless, the list of Rolandrian species here presented, from his work that has finally taken a place in the history of natural sciences, shows that he was also a competent botanist, besides being a skilled entomologist, having recognised and detailedly described many of the Surinamese plants hitherto unknown to science.