660 resultados para Pirarucu arapaima gigas


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A Bacia sedimentar do Araripe é uma das mais ricas localidades fossilíferas do mundo e representa algumas das principais fases da evolução tectônica ligadas ao processo de abertura do Atlântico Sul. Essa bacia se subdivide em dois pacotes estratigráficos distintos: o Grupo Cariri (constituído pelas formações Cariri, Missão Velha e Rio Batateiras) e o Grupo Araripe (constituído pelas formações Crato, Ipubi, Santana e Exu). No caso do Grupo Cariri, apenas a Formação Missão Velha (= Brejo Santo para alguns autores) apresenta restos de peixes fósseis. Essa fauna, típica da fase rift da separação da parte oeste do Gondwana, pode ser comparada à ictiofauna já descrita no Grupo Bahia e à fauna encontrada em diversas bacias interiores do Nordeste do Brasil. O presente trabalho constou da realização de coletas na Formação Missão Velha, identificação, preparação e descrição dos espécimes coletados; comparação da paleoictiofauna dessa formação com a de outras bacias de mesma idade; análise da distribuição paleobiogeográfica dos grupos ali presentes. Apesar de desarticulados, foram identificados seis táxons de peixes, assim como fragmentos de teleósteos não identificados. Os táxons identificados a partir do material coletado são: dentes, espinhos cefálicos e espinhos de nadadeira dorsal de Hybodontiformes; escamas, dentes e ossos desarticulados de Lepidotes sp.; escamas de Pleuropholidae; diversos ossos desarticulados de Mawsonia cf. gigas; placa dentária e outros ossos isolados de Ceratodus sp. Essa fauna é muito importante, pois representa uma biota lacustrina do Neocomiano do Brasil, depositada durante os estágios pré-rift/rift da separação do oeste do Gondwana. Durante a fase pré-rift e rift pode ser observada uma correlação estratigráfica entre a Formação Missão Velha e as bacias marginais da África ocidental. Portanto, a biota presente na Formação Missão Velha auxilia a compreensão da diversidade faunística presente nos estágios pré-rift e rift do Brasil e da África.

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Conservation and the potential and need for aquaculture of three major fish (Catlocarpio siamensis, Probarbus spp. and Pangasius gigas) of the Mekong River are discussed. Different steps being undertaken by the Cambodian government in doing such activities are highlighted.

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Representados aualmente por apenas duas espécies: Latimeria chalumnae e L. menadoensis, os celacantos (Infraordem Actinistia) já foi muito mais numeroso, prolífico desde os tempos de seu surgimento no Devoniano Inferior. Dentro de Actinistia a família Mawsoniidae se destaca por abranger as maiores espécies do grupo, algumas atingindo até três metros de comprimento. A entrada de Mawsoniidae no continente Gondwana se deu durante o Jurássico superior, período o qual é atribuído a espécie Parnaibaia maranhoensis da bacia do Parnaíba (Maranhão). No cretáceo a família se ramificou em dois outros gêneros Mawsonia (com conhecidas ocorrências brasileiras e africanas) e Axelrodichthys (gênero brasileiro com alguns indícios de presença na África). Este trabalho teve por objetivo realizar uma redescrição e comparação de seis espécies do ramo gondwânico da família Mawsoniidae: Parnaibaia maranhoensis, Axelrodichthys araripensis, Mawsonia gigas, M. minor, M. lavocati e M. brasiliensis. Os espécimes estão depositados em oito instituições: três nacionais e cinco internacionais. Após uma criteriosa descrição anatômica dos exemplares caracteres foram selecionados para a realização de uma análise filogenética restrita ao grupo. Os resultados das observações anatômicas revelaram diversas estruturas ainda não descritas na literatura, incluindo o primeiro elemento medial do esqueleto apendicular de Mawsoniidae a ser observado, além de diversas diferenças e afinidades entre as seis espécies. P. maranhoensis apresentou um conjunto de caracteres plesiomórfico que foram interpretados como sendo o resultado de um evento de neotenia, algo inédito na literatura de celacantos. Todas as espécies do gênero Mawsonia apresentaram características diagnósticas que validam sua separação em espécies distintas. A análise filogenética resultou em duas árvores igualmente parcimoniosas. Ambas concordam com a posição de Parnaibaia na base do grupo. Mas diferem com relação à posição de A. araripensis e as espécies do gênero Mawsonia. Conclui-se que Parnaibaia é o gênero mais plesiomórfico do grupo, estando na base do ramo gondwânico da família. Axelrodichthys representa a ligação deste com as demais espécies do gênero.

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Unmanaged and unquantified artisanal fishing is ongoing at Navassa Island, a small oceanic island about 70 km west of Haiti that is part of the U.S. Caribbean Islands National Wildlife Refuge. Concern has been expressed regarding the possible impact of these fishing activities on reef resources, and no quantitative catch or effort data are available. However, informal qualitative observations made during a cruise in November 2002 suggest that escalation in fishing activity (and impact) has occurred since previous observations made in April 2000. Namely, size structure of fish was markedly reduced and the adoption of net fishing has allowed the exploitation of queen conch, Strombas gigas, and hawksbill turtles, Eretmochelys imbricata.

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Aboriginal Australians consumed oysters before settlement by Europeans as shown by the large number of kitchen middens along Australia's coast. Flat oysters, Ostrea angasi, were consumed in southeastern Australia, whereas both flat and Sydney rock oysters, Saccostrea glomerata, are found in kitchen middens in southern New South Wales (NSW), but only Sydney rock oysters are found in northern NSW and southern Queensland. Oyster fisheries began with the exploitation of dredge beds, for the use of oyster shell for lime production and oyster meat for consumption. These natural oyster beds were nealy all exhausted by the late 1800's, and they have not recovered. Oyster farming, one of the oldest aquaculture industries in Australia, began as the oyster fisheries declined in the late 1800's. Early attempts at farming flat oysters in Tasmania, Victoria, and South Australia, which started in the 1880's, were abandoned in the 1890's. However, a thriving Sydney rock oyster industry developed from primitive beginnings in NSW in the 1870's. Sydney rock oysters are farmed in NSW, southern Queensland, and at Albany, Western Australia (WA). Pacific oysters, Crassostrea gigas, are produced in Tasmania, South Australia, and Port Stephens, NSW. FLant oysters currently are farmed only in NSW, and there is also some small-scale harvesting of tropical species, the coarl rock or milky oyster, S. cucullata, and th black-lip oyster, Striostrea mytiloides, in northern Queensland. Despite intra- and interstate rivalries, oyster farmers are gradually realizing that they are all part of one industry, and this is reflected by the establishment of the national Australian Shellfish Quality Assuarance Program and the transfer of farming technology between states. Australia's oyster harvests have remained relatively stable since Sydney rock oyster production peaked in the mid 1970's at 13 million dozen. By the end of the 1990's this had stabilized at around 8 million dozen, and Pacific oyster production reached a total of 6.5 million dozen from Tasmania, South Australia, and Port Stephens, a total of 14.5 million dozen oysters for the whole country. This small increase in production during a time of substantial human population growth shows a smaller per capita consumption and a declining use of oysters as a "side-dish."

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Mexico has an oyster industry of substantial size, ranking about sixth in the world. In 1993, among the top ten oyster producers, Korea, Japan, the United States, China, and France ranked ahead of Mexico, while the Philippines, Australia, Canada, and New Zealand trailed it (Fig. 1). On its east coast, the species landed is the eastern oyster, Crassostrea virginica, while on its west coast C. corteziensis, C. iridescens, and the Pacific oyster, C. gigas, are landed. During the last 10-15 years, annual production often was at least 50,000 t of shelled oysters, or nearly 1.5 million bushels (Anonymous, 1995), with the great preponderance (90%) coming from a series of lagoons connecting with the Gulf of Mexico along the east coast (Fig. 2) and the remainder produced on the west coast.

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Oyster landings in the United States and Canada have been based mainly on three species, the native eastern oyster, Crassostrea virginica, native Olympia oyster, Ostreola conchaphila, and introduced Pacific oyster, C. gigas. Landings reached their peak of around 27 million bushels/year in the late 1800's and early 1900's when eastern oysters were a common food throughout the east coast and Midwest. Thousands of people were involved in harvesting them with tongs and dredges and in shucking, canning, packing, and transporting them. Since about 1906, when the United States passed some pure food laws, production has declined. The causes have been lack of demand, siltation of beds, removal of cultch for oyster larvae while harvesting oysters, pollution of market beds, and oyster diseases. Production currently is about 5.6 million bushels/year.

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Honduras has many communities of artisanal fishermen who land various species of crustaceans and mollusks, using hands, nets, traps, and free diving from shore and from dugout canoes. It also has industrial fisheries for spiny lobster, Panulirus argus; queen conch, Strombus gigas; and mainly pink shrimp, Penaeus notialis, using traps, scuba divers, and trawl nets.

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Trace metal analysis of 23 species of common Pacific Coast marine foods revealed high cadmium values for Bent-nosed clams (Macoma nasuta), Bay mussels (Mytilus edulis), Bay oysters (Osrtrea lurida), Pacific oysters (Crassostrea gigas), and Littleneck clams (Protothaca staminea). Metals were found to concentrate in the gills, heart, and visceral mass of all 10 species of bivalve mollusks examined. Swordfish (Xiphias gladius) and Salmon (Oncorhynchus tshawytscha) demonstrated the highest cadmium values for fish flesh.

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Jumbo squid (Dosidicus gigas) and purpleback squid (Sthenoteuthis oualaniensis) (Teuthida: Ommastrephidae) are thought to spawn in the eastern tropical Pacific. We used 10 years of plankton tow and oceanographic data collected in this region to examine the reproductive habits of these 2 ecologically important squid. Paralarvae of jumbo squid and purpleback squid were found in 781 of 1438 plankton samples from surface and oblique tows conducted by the Southwest Fisheries Science Center (NOAA) in the eastern tropical Pacific over the 8-year period of 1998–2006. Paralarvae were far more abundant in surface tows (maximum: 1588 individuals) than in oblique tows (maximum: 64 individuals). A generalized linear model analysis revealed sea-surface temperature as the strongest environmental predictor of paralarval presence in both surface and oblique tows; the likelihood of paralarval presence increases with increasing temperature. We used molecular techniques to identify paralarvae from 37 oblique tows to species level and found that the purpleback squid was more abundant than the jumbo squid (81 versus 16 individuals).

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The monthly average temperatures at Puttalam Lagoon, Dutch Bay, Portugal Bay towards Kovilmunai and Portugal Bay towards Pallugaturai showed a distinct annual cycle. The peak was in April and values gradually fell till September. There was a further gradual fall in temperature from October to January. The highest temperatures in all four stations were in April. The highest salinities in all the stations were from May to October i.e., during the south-west monsoon. The salinities at Dutch Bay and Portugal Bay were high in March and April corresponding to the highest temperatures reached during these months. Two maxima have been observed in phytoplankton production. A primary maximum in May-June and a secondary maximum in October. The primary and secondary maxima are due to the influx of nutrient laden waters from the rivers Kal Aru and Pomparippu Aru. The phytoplankton producing blooms were Rhizosolenia alata. Rhizosolenia imbricata, Chaetoceros lascinosus, Chaetoceros pervianus, Ch,aetoceros diversus, Coscinodiscus gigas, Thallasionema nitzschioides, Thalassiosira subtilis, Thallassiothrix frauenfeldii, Asterionella japonica, Sceletonema costatum, Bacteriastrum varians and Biddulphia sinensis. Sudden outbursts of a single species were common. These diatoms were species of Chaetoceros and Rhizosolenia, and Thallassiothrix frauenfeldii. Wide fluctuations have been observed in the distribution of phytoplankton but no definite conclusions can be drawn as the period of observation was only one year.

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Karyotype and chromosomal location of the major ribosomal RNA genes (rDNA) were studied using fluorescence in situ hybridization (FISH) in five species of Crassostrea: three Asian-Pacific species (C. gigas, C. plicatula, and C. ariakensis) and two Atlantic species (C. virginica and C. rhizophorae). FISH probes were made by PCR amplification of the intergenic transcribed spacer between the 18S and 5.8S rRNA genes, and labeled with digoxigenin-11-dUTP. All five species had a haploid number of 10 chromosomes. The Atlantic species had 1-2 submetacentric chromosomes, while the three Pacific species had none. FISH with metaphase chromosomes detected a single telomeric locus for rDNA in all five species without any variation. In all three Pacific species, rDNA was located on the long arm of Chromosome 10 (10q)-the smallest chromosome. In the two Atlantic species, rDNA was located on the short arm of Chromosome 2 (2p)-the second longest chromosome. A review of other studies reveals the same distribution of NOR sites (putative rDNA loci) in three other species: on 10q in C. sikamea and C. angulata from the Pacific Ocean and on 2p in C. gasar from the western Atlantic. All data support the conclusion that differences in size and shape of the rDNA-bearing chromosome represent a major divide between Asian-Pacific and Atlantic species of Crassostrea. This finding suggests that chromosomal divergence can occur under seemingly conserved karyotypes and may play a role in reproductive isolation and speciation.

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Cu, Zn superoxide dismutases (SODs) are rnetalloenzymes that represent one important line of defence against reactive oxygen species (ROS). A cytoplasmic Cu. Zn SOD cDNA sequence was cloned from scallop Chlamys farreri by the homology-based cloning technique. The full-length cDNA of scallop cytoplasmic Cu, Zn SOD (designated CfSOD) was 1022 bp with a 459 bp open reading frame encoding a polypeptide of 153 amino acids. The predicted amino acid sequence of CfSOD shared high identity with cytoplasmic Cu. Zn SOD in molluscs, insects, mammals and other animals, such as cytoplasmic Cu, Zn SOD in oyster Crassostrea sostrea gigas (CAD42722), mosquito Aedes aegypti (ABF18094), and cow Bos taurus (XP_584414). A quantitative reverse transcriptase real-time PCR (qRT-PCR) assay was developed to assess the mRNA expression of CfSOD in different tissues and the temporal expression of CfSOD in scallop challenged with Listonella anguillarum, Micrococcus luteus and Candida lipolytica respectively. Higher-level mRNA expression of CfSOD was detected in the tissues of haemocytes, gill filaments and kidney. The expression of CfSOD dropped in the first 8-16 h and then recovered after challenge with L. anguillarum and M. litteus, but no change was induced by the C. lipolytica challenge. The results indicated that CfSOD was a constitutive and inducible acute-phase protein, and could play an important role in the immune responses against L. anguillarum and M. luteus infection. (C) 2007 Elsevier Ltd. All rights reserved.

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A basic understanding of abundance and diversity of antibiotic-resistant microbes and their genetic determinants is necessary for finding a way to prevent and control the spread of antibiotic resistance. For this purpose, chloramphenicol and multiple antibiotic-resistant bacteria were screened from a mariculture farm in northern China. Both sea cucumber and sea urchin rearing ponds were populated with abundant antibiotic-resistant bacteria, especially marine vibrios. Sixty-five percent chloramphenicol-resistant isolates from sea cucumber harbored a cat gene, either cat IV or cat II, whereas 35% sea urchin isolates harbored a cat gene, actually cat II. The predominant resistance determinant cat IV gene mainly occurred in isolates related to Vibrio tasmaniensis or Pseudoalteromonas atlantica, and the cat II gene mainly occurred in Vibrio splendidus-like isolates. All the cat-positive isolates also harbored one or two of the tet genes, tet(D), tet(B), or tet(A). As no chloramphenicol-related antibiotic was ever used, coselection of the cat genes by other antibiotics, especially oxytetracycline, might be the cause of the high incidence of cat genes in the mariculture farm studied.

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应用稳定碳、氮同位素比值法和脂肪酸标志分析法,较为系统地研究了贝藻混养系统中滤食性贝类的食物来源,评估了大型藻类对混养系统及滤食性贝类的物质贡献。主要研究结果如下: 1.综述了典型生态系统中大型藻类和滤食性贝类各自的生态学地位和作用,大型藻类与滤食性贝类不仅在水体营养盐方面存在互利关系,二者在物质循环与收支方面同样具有耦合性,大型藻类提供的颗粒态有机质可以为滤食性贝类提供饵料来源。 2.总结了稳定同位素比值法和脂肪酸标志法在海洋生态系统食物来源及食物网分析中的应用,并建立了两种方法的具体操作规程。 3.分析了栉孔扇贝Chlamys farreri和海带Laminaria japonica混养系统中海带碎屑形成及释放不同阶段的生态学特征,评估了碎屑对扇贝的饵料贡献。海带在6周内释放了自身约27%的碳;碎屑形成及释放过程中C:N比值显著下降,同时伴随着旺盛的细菌降解,碎屑中也发现有大量硅藻类和原生动物存在。稳定同位素分析证实海带碎屑是混养期间扇贝的主要食物来源。 4.查明了春季胶州湾潮间带自然分布的长牡蛎Crassostrea gigas、紫贻贝Mytilus galloprovincialis和湾内浅海筏式养殖栉孔扇贝的可能食物来源。湾内栉孔扇贝饵料组成中浮游硅藻类为最主要部分,同时混杂有陆源有机质和细菌类物质;潮间带自然生长的牡蛎和贻贝饵料组成中,浮游植物占86.2-89.0%,种类组成中除硅藻外还包括一定比例的金藻和甲藻类;潮间带繁盛的孔石莼Ulva pertusa藻床为两种贝类提供了8.7-11.0%的补充食物来源。 5.揭示了桑沟湾贝藻混养海区春、夏季栉孔扇贝饵料来源组成情况及其季节变化,评估了海带养殖区碎屑碳量季节变化及海带来源碳对扇贝组织碳的贡献。结果表明,湾内贝藻混养区碎屑碳量为75.52-265.19 μg l-1,其在水体总颗粒态有机碳中的比例为25.6-73.8%。海带来源碎屑碳对栉孔扇贝组织碳的贡献比例为14.1-42.8%,且与水体碎屑碳比例的季节变化存在极显著相关性(F=0.992, P=0.004)。5月份湾外海带养殖区水体碎屑碳量为110.12-144.71 μg l-1,显著高于湾内无海带区(75.52 μg l-1),湾外养殖的扇贝组织中海带来源碳比例为22.0-24.1%,显著高于湾内单养区扇贝(9.6%)。估算结果表明,桑沟湾每年收获的6967吨(总湿重)栉孔扇贝中,海带提供了约57.1吨碳,换算为海带干物质为219.6吨。脂肪酸标志分析结果表明,2月份至8月份硅藻类在扇贝饵料组成中比例逐渐下降,而细菌类比例逐渐升高。整个采样期间,EPA/DHA比例较低,说明扇贝饵料组成中可能包括高DHA含量的组分。