Detecção de mudança e sedimentação no estuário do Rio Coreaú

O uso de novas técnicas para estudar a evolução e preenchimento de vales incisos tem fornecido, ao longo dos anos, importantes resultados para entendermos como foi a evolução costeira brasileira. Neste contexto, esta tese teve como objetivo estudar a evolução do estuário do rio Coreaú, localizado no estado do Ceará, em diferentes escalas temporais, seja “Eventual” (meses, anos), “Engenharia” anos, decádas) e Geológica” (centenas, séculos, milênios), proposta por Cowell et al. (2003), com intuíto de avaliar se as transformações/alterações ao longo dos anos foram significativas ou não. Como resultados, obteve-se no primeiro objetivo, utilizando técnicas de sensoriamento remoto, a partir de imagens dos sensores TM, ETM⁺ e OLI do satélite Landsat 5,7 e 8 e LISS-3 do satélite ResourceSat-1 de 1985 a 2013, uma alteração mínima em relação a transformações morfológicas ao longo do estuário nos últimos 28 anos (entre as escalas Eventual e de Engenharia), houve neste período um acréscimo de 0,236 km² (3%) de área, não trazendo sigificativas mudanças para o estuário. Em relação a taxa de sedimentação, correspondente ao segundo bjetivo, a partir da coleta de 9 testemunhos, de até 1 m de profundidade e utilizando o radionuclídeo ²¹⁰Pb, ao longo do estuário, obteve-se uma taxa que variou de 0,33 cm/ano a 1 cm/ano (escalas entre Engenharia e Geológica) próximo a foz do estuário, e com uma rápida sedimentação percebida na margem leste do rio, onde encontram-se sedimentos mais recentes em relação a margem oeste. Em relação ao preenchimento, terceiro e último objetivo, a partir da amostragem de testemunhos de até 18 m de profundidade, utilzando o amostrador Rammkernsonden (RKS), foram gerados perfis e seções estratigráficas que ajudaram a entender o preenchimento do vale inciso do estuário do rio Coreaú e entender que trata-se de um estuário fluvio-marinho, preenchendo os vales formados no Grupo Barreiras nos últimos 10.000 anos antes do presente. Estas análises e resultados servirão como base para comparação com outros estuários, sejam fluviais, fluvio-marinhos ou marinhos, para entendermos melhor quais os possíveis eventos que dominaram a sedimentação ao longo da costa brasileira em diferentes escalas.

Dinâmica sazonal de nutrientes em estuário amazônico

Este artigo mostra a distribuição dos nutrientes no estuário do rio Paracauari, durante um ciclo hidrológico amazônico (2008), e no final do período de La Niña (abril de 2008). Esse estuário é influenciado por clima tropical úmido e meso-marés (3 a 4m), semi-diurna. A amostragem foi realizada em 10 estações em três períodos sazonais distintos: chuvoso (março), intermediário (junho) e menos chuvoso (setembro). Medimos “in situ” os parâmetros físico-químicos utilizando uma sonda multiparâmetro; analisamos os nutrientes dissolvidos (nitrato, nitrito, n-amoniacal, fosfato e silicato) por espectofotometria e o material particulado em suspensão por gravimetria. Observamos amplas variações sazonais nas concentrações dos parâmetros estudados. A temperatura da água (média de 28,58 ºC) é bastante homogênea, típica das águas tropicais. O pH variou de ácido (5,80) à alcalino (7,86) e a salinidade entre 0,06 a 7,56 ambos com valores máximos na foz, devido à maior influência marinha. As águas são mal oxigenadas no período chuvoso (2,35 mg.L-1) e bem no menos chuvoso (6,55 mg.L-1). As concentrações de material particulado em suspensão e de nutrientes foram máximas no período chuvoso devido ao aporte natural proveniente das áreas adjacentes.

Annual, seasonal and spatial abundance of the seabob shrimp Xiphopenaeus kroyeri (Decapoda, Penaeidae) off the Southeastern coast of Brazil

We investigated the influence of environmental factors in spatial and temporal distribution of the seabob shrimp Xiphopenaeus kroyeri in Santos Bay and São Vicente Estuary, state of São Paulo, Brazil. Monthly samples were obtained, from May 2008 through April 2010, from four locations in the estuary and four in the bay. No individual was collected in the estuary and this was attributed to the low salinity means recorded in this environment. We collected 109,153 individuals in the bay and there was no difference in abundance between the two years comprised by the study period. The similarity in spatial distribution can be related to sediment grain size that in all sampling locations showed great amount of very fine sand. The largest amount of reproductive females was obtained in early 2010, when temperature was high, and this could have increased the juvenile recruitment in April 2010. According to our results, the distribution of X. kroyeri in the study area is influenced by temperature, which is related to reproduction, and salinity, limiting the entrance of individuals in the estuarine region.

Determinação de coliformes na água e no tecido mole das ostras extraídas em Cananéia, São Paulo, Brasil

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

Diversity of hydrocarbon-degrading Klebsiella strains isolated from hydrocarbon-contaminated estuaries

To investigate the diversity and the catabolic capacity of oil-degrading Klebsiella strains isolated from hydrocarbon-contaminated sediments in Santos-Sao Vicente estuary systems in Brazil. Klebsiella strains obtained from the estuary were characterized using 16S rRNA gene sequencing and BOX-PCR patterns, testing their catabolic capacity to degrade toluene, xylene, naphthalene and nonane, and identifying the catabolic genes present in the oil-degrading strains. Results show that Klebsiella strains were widespread in the estuary. Twenty-one isolates from the Klebsiella genus were obtained; 14 had unique BOX patterns and were further investigated. Among four distinct catabolic genes tested (todC1, ndoB, xylE and alkB1), only the todC1 gene could be amplified in two Klebsiella strains. The biodegradation assay showed that most of the strains had the ability to degrade all of the tested hydrocarbons; however, the strains displayed different efficiencies. The oil-degrading Klebsiella isolates obtained from the estuary were closely related to Klebsiella pneumoniae and Klebsiella ornithinolytica. The isolates demonstrated a substantial degree of catabolic plasticity for hydrocarbon degradation. The results of this study show that several strains from the Klebsiella genus are able to degrade diverse hydrocarbon compounds. These findings indicate that Klebsiella spp. can be an important part of the oil-degrading microbial community in estuarine areas exposed to sewage.

ANATOMY OF NERITINA ZEBRA FROM GUYANA AND BRAZIL (MOLLUSCA: GASTROPODA: NERITIDAE)

Neritina zebra is a common brackish water gastropod living on muddy bottoms with poorly known morphological characters. The morphology, including the variety of colour and pattern of shells, and the anatomy are described. We mainly analyzed the animals collected in the estuary of the Ceara river, Ceara, Brazil, from "Parque Estadual do rio Coco", and specimens from other places deposited in institutional collections, from French Guyana (topotypes) to Sao Paulo. A complete anatomical description is performed, including illustration and discussion ninth concerned to systematics. Amongst the more important anatomical data are: heart diotocardian; kidneys solid; anterior esophagus with pair of ventral esophageal pouches; odontophore with 4 cartilages and 2 horizontal muscles (m6, m6a); males with penis dorsal-right to snout, bearing a terminal papilla; pallial oviduct triaulic, possessing 3 pallial apertures.

Miocene microflora and palaeoclimatic estimates of the Stetten section (Austria)

Pollen analyses have been proven to possess the possibility to decipher rapid vegetational and climate shifts in Neogene sedimentary records. Herein, a c. 21-kyr-long transgression-regression cycle from the Lower Austrian locality Stetten is analysed in detail to evaluate climatic benchmarks for the early phase of the Middle Miocene Climate Optimum and to estimate the pace of environmental change. Based on the Coexistence Approach, a very clear signal of seasonality can be reconstructed. A warm and wet summer season with c. 204-236 mm precipitation during the wettest month was opposed by a rather dry winter season with precipitation of c. 9-24 mm during the driest month. The mean annual temperature ranged between 15.7 and 20.8 °C, with about 9.6-13.3 °C during the cold season and 24.7-27.9 °C during the warmest month. In contrast, today's climate of this area, with an annual temperature of 9.8 °C and 660 mm rainfall, is characterized by the winter season (mean temperature: -1.4 °C, mean precipitation: 39 mm) and a summer mean temperature of 19.9 °C (mean precipitation: 84 mm). Different modes of environmental shifts shaped the composition of the vegetation. Within few millennia, marshes and salt marshes with abundant Cyperaceae rapidly graded into Taxodiaceae swamps. This quick but gradual process was interrupted by swift marine ingressions which took place on a decadal to centennial scale. The transgression is accompanied by blooms of dinoflagellates and of the green alga Prasinophyta and an increase in Abies and Picea. Afterwards, the retreat of the sea and the progradation of estuarine and wetland settings were a gradual progress again. Despite a clear sedimentological cyclicity, which is related to the 21-kyr precessional forcing, the climate data show little variation. This missing pattern might be due to the buffering of the precessional-related climate signal by the subtropical vegetation. Another explanation could be the method-inherent broad range of climate-parameter estimates that could cover small scale climatic changes.

Mineral and chemical composition of surface bottom sediments from the Onega Bay, White Sea

The distribution of temperature and salinity, current velocities, suspended particulate matter, bottom sediments, bottom morphology, and planktonic and benthic organisms during the summer period are studied in the estuary of the large Onega River and coastal areas of the Onega Bay (White Sea) influenced by interacting marine and riverine factors.

Pollen record from sediment core M77/2_056-3 (Bay of Guayaquil, Peru)

We analyzed the pollen content of a marine core located near the bay of Guayaquil in Ecuador to document the link between sea surface temperatures (SST) and changes in rainfall regimes on the adjacent continent during the Holocene. Based on the expansion/regression of five vegetation types, we observe three successive climatic patterns. In the first phase, between 11,700 and 7700 cal yr BP, the presence of a cloud (Andean) forest in the mid altitudes and mangroves in the estuary of the Guayas Basin, were associated with a maximum in boreal summer insolation, a northernmost position of the Intertropical Convergence Zone (ITCZ), a land- sea thermal contrast, and dryness. Between 7700 and 2850 cal yr BP, the expansion of the coastal herbs and the regression of the mangrove indicate a drier climate with weak ITCZ and low ENSO variability while austral winter insolation gradually increased. The interval between 4200 and 2850 cal yr BP was marked by the coolest and driest climatic conditions of the Holocene due to the weak influence of the ITCZ and a strengthening of the Humboldt Current. After 2850 cal yr BP, high variability and amplitude of the Andean forest changes occurred when ENSO frequency and amplitude increased, indicating high variability in land-sea connections. The ITCZ reached the latitude of Guayaquil only after 2500 cal yr BP inducing the bimodal precipitation regime we observe today. Our study shows that besides insolation, the ITCZ position and ENSO frequency, changes in eastern equatorial Pacific SSTs play a major role in determining the composition of the ecosystems and the hydrological cycle of the Ecuadorian Pacific coast and the Western Cordillera in Ecuador.

Shell condition and survival of Puget Sound pteropods are impaired by ocean acidification conditions

We tested whether the thecosome pteropod Limacina helicina from Puget Sound, an urbanized estuary in the northwest continental US, experiences shell dissolution and altered mortality rates when exposed to the high CO2, low aragonite saturation state (Omega a) conditions that occur in Puget Sound and the northeast Pacific Ocean. Five, week-long experiments were conducted in which we incubated pteropods collected from Puget Sound in four carbon chemistry conditions: current summer surface (460-500 µatm CO2, Omega a=1.59), current deep water or surface conditions during upwelling (760 and 1600-1700 µatm CO2, Omega a=1.17 and 0.56), and future deep water or surface conditions during upwelling (2800-3400 µatm CO2, Omega a=0.28). We measured shell condition using a scoring regime of five shell characteristics that capture different aspects of shell dissolution. We characterized carbon chemistry conditions in statistical analyses with Omega a, and conducted analyses considering Omega a both as a continuous dataset and as discrete treatments. Shell dissolution increased linearly as aragonite saturation state decreased. Discrete treatment comparisons indicate that shell dissolution was greater in undersaturated treatments compared to oversaturated treatments. Survival increased linearly with aragonite saturation state, though discrete treatment comparisons indicated that survival was similar in all but the lowest saturation state treatment. These results indicate that, under starvation conditions, pteropod survival may not be greatly affected by current and expected near-future aragonite saturation state in the NE Pacific, but shell dissolution may. Given that subsurface waters in Puget Sound's main basin are undersaturated with respect to aragonite in the winter and can be undersaturated in the summer, the condition and persistence of the species in this estuary warrants further study.

Los cerramientos verticales de Jean Prouvé variables de intercambio con el exterior

A finales del siglo XIX y principios del XX, la aparición de nuevos materiales, como el acero y el hormigón armado, y la experimentación en procedimientos industriales provocan un cambio en el concepto de cerramiento y en la forma de construir. La fachada se libera y se independiza de la estructura principal, y el nuevo cerramiento debe responder a los principios arquitectónicos y constructivos de este momento. Se busca, por tanto, un cerramiento nuevo. Un cerramiento ligero, de poco peso, de poco espesor, autoportante, multicapa, montado en seco, de grandes dimensiones y que cumpla las exigencias de todo cerramiento. Se puede afirmar que, hasta que Jean Prouvé experimenta con distintos materiales y sistemas de fabricación, la técnica de los cerramientos ligeros no se desarrolla por completo. En sus trabajos se pueden encontrar aplicaciones de los nuevos materiales y nuevas técnicas, e investigaciones sobre prefabricación ligera en acero y aluminio, en un intento de aplicar la producción industrial y en serie a la construcción. Esta Tesis realiza un análisis en profundidad, tanto gráfico como escrito, de los cerramientos verticales desarrollados por Jean Prouvé, sin tratarlos como objetos aislados, entendiendo que forman parte de una obra arquitectónica concreta y completa. Dicho análisis sirve para clasificarlos según las funciones esenciales que debe garantizar un cerramiento: aislar, iluminar, ventilar y proteger, y para comprender cuáles son las claves, los recursos e intenciones, utilizadas por el autor para conseguir este propósito. El resultado de la investigación se plasma de dos formas diferentes. En la primera, se realizan reflexiones críticas para extraer los temas importantes de los elementos analizados, lo que posibilita el acercamiento a otros arquitectos y ampliar el campo de visión. En la segunda, de tipo gráfico, se elabora un atlas de los distintos tipos de cerramientos verticales desarrollados por Jean Prouvé. ABSTRACT In the late nineteenth and the early twentieth century, the appearance of new materials, like steel or reinforced concrete, and the experimentation in industrial procedures cause a change in the concept of façade and in the way of build. The façade is released and become independent of the main structural frame, and the new building enclosure must answer the architectural and construction principles of that moment. A new façade is therefore looked for. A light, thin, self supported, multi layer, dry mounted and big dimensions façade that meet the exigencies of all building enclosure. You can ensure that until Jean Prouvé experiment with several materials and fabrication systems, the light façade technic does not develop completely. In his work we can find new materials applications and new technics and studies about light prefabrication with steel and aluminium, in an attempt of apply the mass production to construction. This Thesis carries out a deep analysis, graphic and written, of the vertical enclosure panels of Jean Prouvé’s work. This is made without studying them like isolated objects, but understanding that they are part of a particular architectural work, as a whole. The analysis is used for classify the panels according to main functions that a façade must satisfy: isolate, light up, ventilate and protect. And also to understand which are the keys, the resources and intentions used by Prouvé to achieve this goal. The result of the research is presented in two different ways. In the first one, a critical reflection is made in order to extract the important issues of the analyzed elements. That makes possible the approach to other architects and gives us a bigger range of vision. In the second, graphic, an atlas of the different types of vertical façade panels of Jean Prouvé is made.

(Figure 2) Dissolved manganese concentrations during POLARSTERN Cruise ANT-XXIV/3

The first comprehensive dataset (492 samples) of dissolved Mn in the Southern Ocean shows extremely low values of 0.04 up to 0.64 nM in the surface waters and a subsurface maximum with an average concentration of 0.31 nM (n=20; S.D.=0.08 nM). The low Mn in surface waters correlates well with the nutrients PO4 and NO3 and moderately well with Si(OH)4 and fluorescence. Furthermore, elevated concentrations of Mn in the surface layer coincide with elevated Fe and light transmission and decreased export (234Th/238U deficiency) and fluorescence. It appears that Mn is a factor of importance in partly explaining the HNLC conditions in the Southern Ocean, in conjunction with significant controls by the combination of Fe limitation and light limitation. No input of Mn from the continental margins was observed. This is ascribed to the protruding continental ice sheet that covers the shelf and shuts down the usual biological production, microbial breakdown and sedimentary geochemical cycling. The low concentrations of Mn in the deep ocean basins (0.07-0.23 nM) were quite uniform, but some elevations were observed. The highest deep concentrations of Mn were observed at the Bouvet Triple Junction region and coincided with high concentrations of Fe and are deemed to be from hydrothermal input. The deep basins on both sides of the ridge were affected by this input. In the deep Weddell Basin the input of Weddell Sea Bottom Water appears to be the source of the slightly elevated concentrations of Mn in this water layer.

The behaviour of the rare earth elements during estuarine mixing-revisited

Complete rare earth element (except Eu) and Y concentrations from the estuarine mixing zone (salinity =0.2 to 33) of Elimbah Creek, Queensland, Australia, were measured by quadrupole ICP-MS without preconcentration. High sampling density in the low salinity regime along with high quality data allow accurate tracing of the development of the typical marine rare earth element anomalies as well as Y/Ho fractionation. Over the entire estuary, the rare earth elements are strongly removed relative to a freshwater endmember (60-80% removal). This large overall removal occurs despite a strong remineralisation peak (190% for La, 130% for Y relative to the freshwater endmember) in the mid-salinity zone. Removal and remineralisation are accompanied by fractionation of the original (freshwater) rare earth element pattern, resulting in light rare earth element depletion. Estuarine fractionation generates a large positive La anomaly and a superchondritic Y/Ho ratio. Conversely, we observe no evidence to support the generation of the negative Ce anomaly in the estuary. With the exception of Ce, the typical marine rare earth element features can thus be attributed to estuarine mixing processes. The persistence of these features in hydrogenous sediments for at least 3.71 Ga highlights the importance of estuarine processes for marine chemistry on geological timescales. (c) 2005 Elsevier B.V. All rights reserved.