Eocene calcareous nannofossils of ODP Leg 149 sites

Five sites were drilled on the Iberia Abyssal Plain, west of the Iberian Peninsula. Four holes (897C, 897D, 899B, and 900A) yielded Eocene sediments that consist of turbidites and contourites. The Eocene section above the continental crust at Site 900 is continuous (from nannofossil Zones NP10 to NP20) and considerably expanded because of the site's relatively shallow depth, which remained consistently above the carbonate compensation depth (CCD). Sites 897 and 898, situated in deeper water above the ocean/continent transition, on the other hand, have noncontinuous, relatively short Eocene sections (from Zones NP14 to NP20 at Site 897 and from Zones NP19 to NP20 at Site 899). Nannofossils are abundant, diverse, and moderately to poorly preserved; they provide the primary means of dating the Eocene sediments recovered during Leg 149.

Lettres d'un diplomate danois en Espagne, 1798-1800.

"Extrait de la Revue hispanique, tome IX".

Tractatvs de crimine laesae maiestatis insignis, et elegans ...

Title vignette.

Digital surface model, hillshade and orthophoto of the world's largest fossil oyster reef, links to GeoTIFFs

The world's largest fossil oyster reef, formed by the giant oyster Crassostrea gryphoides and located in Stetten (north of Vienna, Austria) is studied by Harzhauser et al., 2015, 2016; Djuricic et al., 2016. Digital documentation of the unique geological site is provided by terrestrial laser scanning (TLS) at the millimeter scale. Obtaining meaningful results is not merely a matter of data acquisition with a suitable device; it requires proper planning, data management, and postprocessing. Terrestrial laser scanning technology has a high potential for providing precise 3D mapping that serves as the basis for automatic object detection in different scenarios; however, it faces challenges in the presence of large amounts of data and the irregular geometry of an oyster reef. We provide a detailed description of the techniques and strategy used for data collection and processing in Djuricic et al., 2016. The use of laser scanning provided the ability to measure surface points of 46,840 (estimated) shells. They are up to 60-cm-long oyster specimens, and their surfaces are modeled with a high accuracy of 1 mm. In addition to laser scanning measurements, more than 300 photographs were captured, and an orthophoto mosaic was generated with a ground sampling distance (GSD) of 0.5 mm. This high-resolution 3D information and the photographic texture serve as the basis for ongoing and future geological and paleontological analyses. Moreover, they provide unprecedented documentation for conservation issues at a unique natural heritage site.

Mutation scanning analysis of Marteilia sydneyi populations from different geographical locations in eastern Australia

Marteilia sydneyi (Paramyxea) is the causative agent of QX disease in oysters. In spite of the economic impact of this disease, its origin and the precise reason(s) for its apparent spread in Australian waters are not yet known. Given such knowledge gaps, investigating the population genetic structure(s) of M. sydneyi populations could provide insights into the epidemiology and ecology of the parasite and could assist in its prevention and control. In this study, single strand conformation polymorphism (SSCP)-based analysis of a region (195 bp) of the first internal transcribed spacer (ITS-1) of ribosomal DNA was employed to investigate genetic variation within and among five populations of M. sydneyi from oysters from five different locations in eastern Australia. The analysis showed the existence of a genetic variant of M. sydneyi common to the Great Sandy Strait, and the Richmond and Georges Rivers, as distinct from variants at the Pimpama and Clarence Rivers. Together with historical and other information relating to the QX disease outbreaks in eastern Australia, the molecular findings support the proposal that the parasite originated in the Great Sandy Strait and/or Richmond River and then extended southward along the coast. From a technical perspective, the study demonstrated the usefulness of SSCP as a tool to study the population genetics and epidemiology of M. sydneyi. (C) 2003 Elsevier Ltd. All rights reserved.

The origin and evolution of the surfactant system in fish: Insights into the evolution of lungs and swim bladders

Several times throughout their radiation fish have evolved either lungs or swim bladders as gas-holding structures. Lungs and swim bladders have different ontogenetic origins and can be used either for buoyancy or as an accessory respiratory organ. Therefore, the presence of air-filled bladders or lungs in different groups of fishes is an example of convergent evolution. We propose that air breathing could not occur without the presence of a surfactant system and suggest that this system may have originated in epithelial cells lining the pharynx. Here we present new data on the surfactant system in swim bladders of three teleost fish ( the air-breathing pirarucu Arapaima gigas and tarpon Megalops cyprinoides and the non-air-breathing New Zealand snapper Pagrus auratus). We determined the presence of surfactant using biochemical, biophysical, and morphological analyses and determined homology using immunohistochemical analysis of the surfactant proteins (SPs). We relate the presence and structure of the surfactant system to those previously described in the swim bladders of another teleost, the goldfish, and those of the air-breathing organs of the other members of the Osteichthyes, the more primitive air-breathing Actinopterygii and the Sarcopterygii. Snapper and tarpon swim bladders are lined with squamous and cuboidal epithelial cells, respectively, containing membrane-bound lamellar bodies. Phosphatidylcholine dominates the phospholipid (PL) profile of lavage material from all fish analyzed to date. The presence of the characteristic surfactant lipids in pirarucu and tarpon, lamellar bodies in tarpon and snapper, SP-B in tarpon and pirarucu lavage, and SPs ( A, B, and D) in swim bladder tissue of the tarpon provide strong evidence that the surfactant system of teleosts is homologous with that of other fish and of tetrapods. This study is the first demonstration of the presence of SP-D in the air-breathing organs of nonmammalian species and SP-B in actinopterygian fishes. The extremely high cholesterol/disaturated PL and cholesterol/PL ratios of surfactant extracted from tarpon and pirarucu bladders and the poor surface activity of tarpon surfactant are characteristics of the surfactant system in other fishes. Despite the paraphyletic phylogeny of the Osteichthyes, their surfactant is uniform in composition and may represent the vertebrate protosurfactant.

Macrozoobenthos abundance on a tropical oyster culture in an Amazon estuary, Para state, northern Brazil

The present study describes the biofouling composition of the surface of the mangrove oyster Crassostrea rhizophorae (Guilding, 1828), cultivated in an Amazon estuary, located in the state of Pará, northern Brazil. In total, 6.124 macroinvertebrates were sampled in the months of July, August, October and December 2013. Collected epifauna was presented by five taxa (Bivalvia, Gastropoda, Polychaeta, Crustacea and Anthozoa), 20 families and 37 species. Bivalvia was the most abundant class, presenting 5.183 mussels Mytella charruana (d'Orbigny, 1842). Knowledge of biofouling composition associated to the surface cultured bivalves enables the implementation of mitigation measures to the impacts caused by this association.

Distribution of diatom species as abundance estimates from vertical multinet hauls from 150 m water depth in the Indian Ocean

During the Indian Ocean Expedition of R/V METEOR phytoplankton samples were taken with a multiple closing net (Multinet) at 103 stations. In this material the diatoms were investigated. In all 247 taxa could be identified which belong to 242 species and 5 varieties of formae of 80 genera. Of these 1 variety, 15 pecies, and 3 genera are newly described. New combinations were made for 18 species, and a number of old combinations was reinstated.

Stable carbon and oxygen isotope record of foraminifera from DSDP Hole 30-289

Sediments accumulate on the sea floor far from land with rates of a few millimetres to a few centimetres per thousand years. Sediments have been accumulating under broadly similar conditions, subject to similar controls, for the past 10 8 years and more. In principle we should be able to study the distribution of climatic variance with frequencies over the range 10**-3 to 10**-7 cycles per year with comparative ease. In fact, nearly all our data are heavily weighted towards the youngest part of the geological record. We study frequencies higher than 10**-4 cycles per year in the special case of a Pleistocene interglacial (the present one), and frequencies in the range 10**-4 to 10**-5 cycles per year in the special case of an ice-age. Although these may be of more direct interest to mankind than earlier periods, it may well be that we will understand the causes of climatic variability better if we can examine their operation over a longer time scale and under different boundary conditions. Rather than review the available data, I have collected some new data to show the feasibility of gathering a data base for examining climatic variability without this usual bias toward the recent. The most widely applicable tool for extracting climatic information from deep-sea sediments is oxygen isotope analysis of calcium carbonate microfossils. It is generally possible to select from the sediment both specimens of benthonic Foraminifera (that is, those that lived in ocean deep water at the sediment-water interface) and specimens of planktonic Foraminifera (that is, those that lived and formed their shells near the ocean surface, and fell to the sediment after death). Thus one is able to monitor conditions at the surface and at depth at simultaneous moments in the geological past. The necessity to analyse calcareous microfossils restricts investigation to calcareous sediments, but even with this restriction in sediment type there are many factors governing the rate of sediment accumulation. On a global scale, sediment accumulates so as to balance the input to the oceans from continental erosion. Even when averaged globally, long-term accumulation rates have varied by almost a factor of ten (Davies et al., 1977, doi:10.1126/science.197.4298.53). At the regional scale, surface productivity and deep-water physical and chemical conditions also affect the sediment accumulation rate. Since all these are susceptible to variation and may well vary in response to climatic change as well as other factors, it is extremely hazardous to attempt to express any climatic variable as a function of time on the basis of measurements originally made as a function of depth in sediment. Although time has been used as a basis for plotting Figs. i-8, these should be regarded as freehand sketches of climatic history rather than as time-series plots.

Microbial community of black band disease on infection, healthy and dead part of scleractinian Montipora sp. colony at Seribu islands, Indonesia

It is crucial to understand the microbial community associated with the host when attempting to discern the pathogen responsible for disease outbreaks in scleractinian corals. This study determines changes in the bacterial community associated with Montipora sp. in response to black band disease in Indonesian waters. Healthy, diseased, and dead Montipora sp. (n = 3 for each sample type per location) were collected from three different locations (Pari Island, Pramuka Island, and Peteloran Island). DGGE (Denaturing Gradient Gel Electrophoresis) was carried out to identify the bacterial community associated with each sample type and histological analysis was conducted to identify pathogens associated with specific tissues. Various Desulfovibrio species were found as novelty to be associated with infection samples, including Desulfovibrio desulfuricans, Desulfovibrio magneticus, and Desulfovibrio gigas, Bacillus benzoevorans, Bacillus farraginis in genus which previously associated with pathogenicity in corals. Various bacterial species associated with uninfected corals were lost in diseased and dead samples. Unlike healthy samples, coral tissues such as the epidermis, endodermis, zooxanthellae were not present on dead samples under histological observation. Liberated zooxanthellae and cyanobacteria were found in black band diseased Montipora sp. samples.

El recurso calamar gigante en la costa peruana y El Niño.

El presente artículo es una revisión del estado de conocimiento del calamar gigante frente a la costa peruana y su variabilidad en relación a los eventos El Niño, para lo cual se analizan sus desembarques, estructura de tallas, áreas de pesca y cambios en los índices de abundancia en el periodo 1991-2015.

Reprodução e engorda do pirarucu: levantamento de processos produtivos e tecnologias.

Dados gerais das pisciculturas de reprodução e engorda. Propriedades de reprodução: número médio de reprodutores e idade; origem dos reprodutores por bacias hidrográficas; estruturas de cultivo, densidade de estocagem e casais formados; manejo alimentar de reprodutores; monitoramento da qualidade da água e fertilização dos viveiros e barragens; manejos no acasalamento e comportamento reprodutivo; caracterização de ninhos; período reprodutivo e idade na primeira reprodução; manejo e sanidade dos reprodutores; captura dos alevinos; alevinagem; treinamento alimentar; sanidade dos alevinos; pré-comercialização e comercialização dos alevinos; transporte e destinação dos alevinos. Propriedades de engorda: aquisição de alevinos; estruturas de cultivo; preparação dos viveiros; fase de recria; manejo alimentar na recria; fase de engorda; manejo alimentar na engorda; biometrias; mortalidades e sanidade; monitoramento da qualidade da água; assistência técnica, abate e comercialização.

Respostas fisiológicas de pirarucu ao probiótico Bacillus subtilis (Cohn 1872).

O uso de probióticos na alimentação dos peixes pode estimular o sistema imunológico e agir na prevenção de enfermidades. O presente estudo avaliou a fisiologia de pirarucu Arapaima gigas após alimentação por 30 dias com dietas enriquecidas com probiótico Bacillus subtilis em 3 níveis de inclusão: 0 (Controle); 0,02 (BS0,02%) e 0,05% (BS0,05%) (triplicata), sendo realizada biometria e coleta de amostras de sangue. Os grupos foram comparados entre si (P<0,05). O peso, comprimento e o índice hepatossomático (IHS) dos pirarucus BS0,05% foram menores que os do Controle. As análises hematológicas e bioquímicas indicaram que BS0,02% promoveu aumento do hematócrito e da albumina, com relação aos demais grupos; e diminuição da concentração de hemoglobina corpuscular média (CHCM) e da glicose plasmática com relação ao Controle. A hemoglobina corpuscular média (HCM) e atividade respiratória dos leucócitos do BS0,05% diminuíram com relação ao Controle. BS0,02% apresentaram redução do número de leucócitos, com relação ao Controle, que refletiu na diminuição de monócitos, neutrófilos, LG-PAS e eosinófilos. Assim, os níveis de B. subtilis avaliados não promoveram crescimento ou alterações fisiológicas nos pirarucus, que indiquem melhoria do seu sistema imune.

Caracterização fenotípica de bactérias patogênicas isoladas de peixes e água de piscicultura de Macapá, Estado do Amapá.

O município de Macapá encontra-se no sudeste do Estado do Amapá e possui em sua maioria, as pisciculturas utilizando o sistema de cultivo semi-intensivo ou intensivo com áreas de 0,5 a 3,0 hectares de lâmina de água. A maioria das pisciculturas cultiva principalmente tambaqui (Colossoma macropomum) e híbrido tambatinga (C. macropomum x Piaractus brachypomum), enquanto poucos cultivam pirarucu (Arapaima gigas) e híbrido tambacu (C. macropomum x Piaractus mesopotamicus). Porém, 21% da produção é destinada a subsistência e 32% para fins comerciais, mas 45% é destinada a ambas as finalidades. A comercialização é feita diretamente aos consumidores ou aos feirantes locais. Um dos veículos importantes que contribuem para as infecções no homem causadas por microrganismos patogênicos podem ser os peixes, especialmente quando são consumidos crus ou após tratamento térmico inadequado. Esses microrganismos estão presentes também em peixe estocados em baixas temperaturas, condição física que permite a esses sobreviver, multiplicar e produzir fatores de virulência, sendo ainda capazes de causar doenças oportunistas. Microrganismos patogênicos tais como Staphylococcus aureus, Salmonella spp., Escherichia coli e Aeromonas spp., bem como outros, podem acarretar infecções gastrointestinais, quando não são observadas boas práticas de manipulação e conservação desse alimento, causando risco de agravos na Saúde Pública. Este trabalho teve como objetivo isolar, caracterizar e verificar fenotipicamente a frequência de indicadores bacterianos para a qualidade da água e peixes oriundos de pisciculturas de Macapá, estado do Amapá, visando fornecer informações de interesse da Saúde Pública. Em 15 pisciculturas foram analisados um total de 45 tambaquis e tambatinga para qualidade microbiológica, e 45 amostras de água para qualidade microbiológica, física e química. As análises foram realizadas no laboratório de Microbiologia de Alimentos e Água do Laboratório Central de Saúde Pública do Amapá (LACEN-AP), e no Laboratório Especial de Microbiologia Aplicada (LEMA) da UNIFAP. Os resultados revelaram que os peixes e água das 15 pisciculturas avaliadas encontram-se dentro dos padrões legais vigentes quando analisadas a qualidade microbiológicas, físico e química da água dos tanques, assim como os peixes cultivados apresentaram resultados dentro dos limites satisfatórios quanto à adequada segurança alimentar. Portanto, há garantia do equilíbrio em quantidade e em qualidade desses peixes consumidos para o alcance de uma nutrição adequada, diminuindo desta maneira os riscos de doenças transmitidas por água e alimentos promovendo assim, a minimização dos riscos à Saúde Pública.