867 resultados para Actinoptychus intermedius


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This material is based upon work supported by the National Science Foundation through the Florida Coastal Everglades Long-Term Ecological Research program under Cooperative Agreements #DBI-0620409 and #DEB-9910514. This image is made available for non-commercial or educational use only.

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S. milleri -ryhmän bakteerit ovat osa ihmisen suun, nielun, suoliston ja genitaalialueen normaaliflooran bakteeristoa. Kommensaalien lisäksi ryhmään kuuluu myös merkittäviä patogeenejä, jotka esiintyvät varsin runsaina löydöksinä monenlaisissa märkivissä infektioissa. Ryhmään kuuluu kolme lajia: S. anginosus, S. constellatus ja S. intermedius. Lajit ovat varsin samankaltaisia ja raportoidaankin usein vain ryhmänimellä. Lajit ovat kuitenkin erotettavissa, sillä ne eroavat toisistaan tuottamiensa entsyymien suhteen ja esiintyvyydessään kehon eri osissa. Työn tarkoituksena oli tunnistaa erityyppisistä kliinisistä infektioista otetuista näytteistä eristettyjä S. milleri -ryhmään luokiteltuja kantoja lajitasolle ja selvittää niiden esiintymisyleisyyttä näissä infektioissa. Näytteenottopaikat jaettiin viiteen ryhmään: naisten urogenitaalialue (15 kantaa), miesten urogenitaalialue (8 kantaa), oraaliset (28 kantaa), umpisuoli (34 kantaa) ja "muut" (12 kantaa). Lajitunnistuksen lisäksi selvitettiin kantojen hemolyyttisyys ja mahdollinen Lancefield-seroryhmä (A, C, F, G). Lajien erottelu perustuu eroihin bakteerien kyvyissä hajottaa tiettyjä substraatteja (entsyymiprofilointi), hemolyyttisyys määritettiin verimaljalla ja seroryhmitys tehtiin kaupallisella vasta-aine-sakkautumistestillä (Streptex latex Z1- 50). Työssä testattiin käytössä olevia ja kehiteltiin uusia, lähinnä ennalta muodostuneiden entsyymien tunnistamiseen perustuvia erottelumenetelmiä. Vertailtavina oli kolme entsyymiprofiliontimenetelmää, joista yksi on fluorogeeninen (4-Metyyli-umbelliferyyli-subtraatit) ja kaksi kromogeenistä (Weetabs ja RoscoDiagnostic tablets). Kannoilta määritettiin seuraavat aktiivisuudet: ?-fukosidaasi, (?-glukosidaasi, glukosidaasi, ?-galaktosidaaasi, ?-N-asetyyli-galaktosaminidaasi, ?-N-asetyyli-glukosaminidaasi, sialidaasi ja hyaluronidaasi. Työhön sisältyy myös erilaisten kasvatusalustojen sekä pH:n vaikutusten arviointia bakteerienentsyymiaktiivisuuksiin ja testituloksiin. Lisäksi työssä testattiin kromatografisensoluseinärasvahappoanalyysin soveltuvuutta lajien erotteluun. Menetelmiä tarkasteltiin herkkyyden sekäkäytännön suorittamisen ja aiheutuvien kustannusten kannalta. Asetetut tavoitteet saavutettiin. Kaikki käytetyt menetelmät osoittautuivat toimiviksi. Entsyymitestien tuloksetkorreloivat keskenään ja kirjallisuuden kanssa hyvin. Kannat karakterisoitiin, tunnistettiin lajitasolle ja lajiensiintyvyyttä kehon eri osissa voitiin vertailla. Mikään entsyymitesti ei osoittautunut ylivoimaisesti parhaaksi tai huonoimmaksi, vaikkakin yksittäistensubstraattien kohdalla eri testien herkkyydet vaihtelivatkin huomattavasti. Rasvahappoanalyysi ei erotellutkantoja toivotulla tavalla, joten sen käytöstä luovuttiin työn melko varhaisessa vaiheessa. Tutkituista 97 S. milleri -kannasta tunnistettiin 58 S. anginosus-kantaa, 29 S. constellatus-kantaa ja 10 S.ntermedius-kantaa. Eri lajit noudattivat entsyymiprofiiliaan muutamaa poikkeusta lukuunottamatta hyvinkinsäännöllisesti. Lajien sisäinen variaatio hemolyysiominaisuuksissa oli merkittävää ja S. inilleri -ryhmän erilajien sekä hemolyysisltään ja seroryhmältään erilaisten kantojen esiintyvyydessä kehon eri osissa havaittiinselkeitä eroja. Avainsanat: entsyymiprofilointi, fluorogeeniset ja kromogeeniset substraatit, seroryhmä, hemolyysi, esiintyvyys

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I REPORT OF THE PICES WORKSHOP ON THE OKHOTSK SEA AND ADJACENT AREAS (pdf, 0.1 Mb) 1. Outline of the workshop 2. Summary reports from sessions 3. Recommendations of the workshop 4. Acknowledgments II SCIENTIFIC PAPERS SUBMITTED FROM SESSIONS 1. Physical Oceanography Sessions (pdf, 4 Mb) A. Circulation and water mass structure of the Okhotsk Sea and Northwestern Pacific Valentina D. Budaeva & Vyacheslav G. Makarov Seasonal variability of the pycnocline in La Perouse Strait and Aniva Gulf Valentina D. Budaeva & Vyacheslav G. Makarov Modeling of the typical water circulations in the La Perouse Strait and Aniva Gulf region Nina A. Dashko, Sergey M. Varlamov, Young-Ho Han & Young-Seup Kim Anticyclogenesis over the Okhotsk Sea and its influence on weather Boris S. Dyakov, Alexander A. Nikitin & Vadim P. Pavlychev Research of water structure and dynamics in the Okhotsk Sea and adjacent Pacific Howard J. Freeland, Alexander S. Bychkov, C.S. Wong, Frank A. Whitney & Gennady I. Yurasov The Ohkotsk Sea component of Pacific Intermediate Water Emil E. Herbeck, Anatoly I. Alexanin, Igor A. Gontcharenko, Igor I. Gorin, Yury V. Naumkin & Yury G. Proshjants Some experience of the satellite environmental support of marine expeditions at the Far East Seas Alexander A. Karnaukhov The tidal influence on the Sakhalin shelf hydrology Yasuhiro Kawasaki On the formation process of the subsurface mixed water around the Central Kuril Islands Lloyd D. Keigwin Northwest Pacific paleohydrography Talgat R. Kilmatov Physical mechanisms for the North Pacific Intermediate Water formation Vladimir A. Luchin Water masses in the Okhotsk Sea Andrey V. Martynov, Elena N. Golubeva & Victor I. Kuzin Numerical experiments with finite element model of the Okhotsk Sea circulation Nikolay A. Maximenko, Anatoly I. Kharlamov & Raissa I. Gouskina Structure of Intermediate Water layer in the Northwest Pacific Nikolay A. Maximenko & Andrey Yu. Shcherbina Fine-structure of the North Pacific Intermediate Water layer Renat D. Medjitov & Boris I. Reznikov An experimental study of water transport through the Straits of Okhotsk Sea by electromagnetic method Valentina V. Moroz Oceanological zoning of the Kuril Islands area in the spring-summer period Yutaka Nagata Note on the salinity balance in the Okhotsk Sea Alexander D. Nelezin Variability of the Kuroshio Front in 1965-1991 Vladimir I. Ponomarev, Evgeny P. Varlaty & Mikhail Yu. Cheranyev An experimental study of currents in the near-Kuril region of the Pacific Ocean and in the Okhotsk Sea Stephen C. Riser, Gennady I. Yurasov & Mark J. Warner Hydrographic and tracer measurements of the water mass structure and transport in the Okhotsk Sea in early spring Konstantin A. Rogachev & Andrey V. Verkhunov Circulation and water mass structure in the southern Okhotsk Sea, as observed in summer, 1994 Lynne D. Talley North Pacific Intermediate Water formation and the role of the Okhotsk Sea Anatoly S. Vasiliev & Fedor F. Khrapchenkov Seasonal variability of integral water circulation in the Okhotsk Sea B. Sea ice and its relation to circulation and climate V.P. Gavrilo, G.A. Lebedev & A.P. Polyakov Acoustic methods in sea ice dynamics studies Nina M. Pestereva & Larisa A. Starodubtseva The role of the Far-East atmospheric circulation in the formation of the ice cover in the Okhotsk Sea Yoshihiko Sekine Anomalous Oyashio intrusion and its teleconnection with Subarctic North Pacific circulation, sea ice of the Okhotsk Sea and air temperature of the northern Asian continent C. Waves and tides Vladimir A. Luchin Characteristics of the tidal motions in the Kuril Straits George V. Shevtchenko On seasonal variability of tidal constants in the northwestern part of the Okhotsk Sea D. Physical oceanography of the Japan Sea/East Sea Mikhail A. Danchenkov, Kuh Kim, Igor A. Goncharenko & Young-Gyu Kim A “chimney” of cold salt waters near Vladivostok Christopher N.K. Mooers & Hee Sook Kang Preliminary results from a numerical circulation model of the Japan Sea Lev P. Yakunin Influence of ice production on the deep water formation in the Japan Sea 2. Fisheries and Biology Sessions (pdf, 2.8 Mb) A. Communities of the Okhotsk Sea and adjacent waters: composition, structure and dynamics Lubov A. Balkonskaya Exogenous succession of the southwestern Sakhalin algal communities Tatyana A. Belan, Yelena V. Oleynik, Alexander V. Tkalin & Tat’yana S. Lishavskaya Characteristics of pelagic and benthic communities on the North Sakhalin Island shelf Lev N. Bocharov & Vladimir K. Ozyorin Fishery and oceanographic database of Okhotsk Sea Victor V. Lapko Interannual dynamics of the epipelagic ichthyocen structure in the Okhotsk Sea Valentina I. Lapshina Quantitative seasonal and year-to-year changes of phytoplankton in the Okhotsk Sea and off Kuril area of the Pacific Lyudmila N. Luchsheva Biological productivity in anomalous mercury conditions (northern part of Okhotsk Sea) Inna A. Nemirovskaya Origin of hydrocarbons in the ecosystems of coastal region of the Okhotsk Sea Tatyana A. Shatilina Elements of the Pacific South Kuril area ecosystem Vyacheslav P. Shuntov & Yelena P. Dulepova Biota of the Okhotsk Sea: Structure of communities, the interannual dynamics and current status B. Abundance, distribution, dynamics of the common fishes of the Okhotsk Sea Yuri P. Diakov Influence of some abiotic factors on spatial population dynamics of the West Kamchatka flounders (Pleuronectidae) Gordon A. McFarlane, Richard J. Beamish & Larisa M. Zverkova An examination of age estimates of walleye pollock (Theragra chalcogramma) from the Sea of Okhotsk using the burnt otolith method and implications for stock assessment and management Larisa P. Nikolenko Migration of Greenland turbot (Reinhardtius hippoglossoides) in the Okhotsk Sea Galina M. Pushnikova Fisheries impact on the Sakhalin-Hokkaido herring population Vidar G. Wespestad Is pollock overfished? C. Salmon of the Okhotsk Sea: biology, abundance and stock identification Vladimir A. Belyaev, Alexander Yu. Zhigalin Epipelagic Far Eastern sardine of the Okhotsk Sea Yuri E. Bregman, Victor V. Pushnikov, Lyudmila G. Sedova & Vladimir Ph. Ivanov A preliminary report on stock status and productive capacity of horsehair crab Erimacrus isenbeckii (Brandt) in the South Kuril Strait Natalia T. Dolganova Mezoplankton distribution in the West Japan Sea Vladimir V. Efremov, Richard L. Wilmot, Christine M. Kondzela, Natalia V. Varnavskaya, Sharon L. Hawkins & Maria E. Malinina Application of pink and chum salmon genetic baseline to fishery management Vyacheslav N. Ivankov & Valentina V. Andreyeva Strategy for culture, breeding and numerous dynamics of Sakhalin salmon populations Alla M. Kovalevskaya, Natalia I. Savelyeva & Dmitry M. Polyakov Primary production in Sakhalin shelf waters Tatyana N. Krupnova Some reasons for resource reduction of Laminaria japonica (Primorye region) Lyudmila N. Luchsheva & Anatoliy I. Botsul Mercury in bottom sediments of the northeastern Okhotsk Sea Pavel A. Luk’yanov, Natalia I. Belogortseva, Alexander A. Bulgakov, Alexander A. Kurika & Olga D. Novikova Lectins and glycosidases from marine macro and micro-organisms of Japan and Okhotsk Seas Boris A. Malyarchuk, Olga A. Radchenko, Miroslava V. Derenko, Andrey G. Lapinski & Leonid L. Solovenchuk PCR-fingerprinting of mitochondrial genome of chum salmon, Oncorhynchus keta Alexander A. Mikheev Chaos and relaxation in dynamics of the pink salmon (Oncorhynchus gorbuscha) returns for two regions Yuri A. Mitrofanov & Larisa N. Lesnikova Fish-culture of Pacific Salmons increases the number of heredity defects Larisa P. Nikolenko Abundance of young halibut along the West Kamchatka shelf in 1982-1992 Sergey A. Nizyaev Living conditions of golden king crab Lithodes aequispina in the Okhotsk Sea and near the Kuril Islands Ludmila A. Pozdnyakova & Alla V. Silina Settlements of Japanese scallop in Reid Pallada Bay (Sea of Japan) Galina M. Pushnikova Features of the Southwest Okhotsk Sea herring Vladimir I. Radchenko & Igor I. Glebov Present state of the Okhotsk herring stock and fisheries outlook Alla V. Silina & Ida I. Ovsyannikova Distribution of the barnacle Balanus rostratus eurostratus near the coasts of Primorye (Sea of Japan) Galina I. Victorovskaya Dependence of urchin Strongylocentrotus intermedius reproduction on water temperature Anatoly F. Volkov, Alexander Y. Efimkin & Valery I. Chuchukalo Feeding habits of Pacific salmon in the Sea of Okhotsk and in the Pacific waters of Kuril Islands in summer 1993 Larisa M. Zverkova & Georgy A. Oktyabrsky Okhotsk Sea walleye pollock stock status Tatyana N. Zvyagintseva, Elena V. Sundukova, Natalia M. Shevchenko & Ludmila A. Elyakova Water soluble polysaccharides of some Far-Eastern seaweeds 3. Biodiversity Program (pdf, 0.2 Mb) A. Biodiversity of island ecosystems and seasides of the North Pacific Larissa A. Gayko Productivity of Japanese scallop Patinopecten yessoensis (IAY) culture in Posieta Bay (Sea of Japan) III APPENDICES 1. List of acronyms 2. List of participants (Document pdf contains 431 pages)

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ENGLISH: 1. Quantitative phytoplankton samples were collected by the Inter-American Tropical Tuna Commission at the surface and ten meters in the Gulf of Panama, as follows: a) 18-21 March, 1958 (31 stations)-during the height of the upwelling season, b) 10-12 July, 1957 (10 stations)-during the transition to the rainy season at a time when mild upwelling winds reappear, c) 7-8 November, 1957 (15 stations)-during the height of the rainy season. 2. Maximum phytoplankton populations occurred during the upwelling season, followed by a considerable decline during July, and a further Subsidence during November. 3. A remarkable regional uniformity in species composition was observed during the surveys despite regional differences in growth conditions. Diatoms overwhelmingly dominated the communities. 4. During all surveys, the innermost regions, generally north of 8°30'N, were the most productive. The least productive areas were in the offing of San Miguel Bay and Parita Bay, suggesting that nutrient accretion via runoff is inadequate to sustain sizeable autotrophic plant populations in those regions. 5. During all surveys, phytoplankton growth appeared to be limited by nutrient availability. 6. During all surveys, phytoplankton growth appeared to be related to depth of the water column. 7. Although below average rainfall contributed to unusually favorable growth conditions (reduced stability, increased transparency and, presumably, nutrient reserves) during the November survey relative to November 1955 and 1956 at 8°45'N, 79°23'W, the anticipated heightened phytoplankton response was not observed. 8. During the November survey, the local diatom responses and their regional fluctuations could be satisfactorily related to the accompanying surface salinity conditions. However, this correspondence is undoubtedly attributable to factors associated with the observed salinity levels, probably nutrients, rather than salinity directly. 9. Unusually warm conditions occurred during the March survey, attributable to considerably weaker upwelling winds than normally occurring then, which contributed to a considerably lower standing crop and a retardation in succession of three to five weeks relative to that observed during 1955-1957 at 8°45'N, 79°23'W in the Gulf of Panama. 10. During the March survey, a well defined inverse relationship existed between mean temperature and mean diatom abundance in the upper ten meters, and between transparency and mean diatom abundance. A direct relationship occurred between surface salinity and mean diatom abundance in the upper ten meters. These relationships are interpreted to indicate that diatom abundance primarily reflected the nutrient concentrations associated with a given upwelling intensity, rather than describing casual relationships. 11. The survey results indicate that the phytoplankton dynamics observed at 8°45'N, 79°23'W from November, 1954 through May, 1957 are generally representative of the Gulf of Panama. 12. The following new forms, to be described in a later publication, were observed during the surveys: Actinoptychus undulatus f. catenata n.f., Asterionella japonica f. tropicum n.f., Leptocylindrus maximus n. sp., Skeletonema costatum f. tropicum n.f. SPANISH: 1. La Comisión Interamericana del Atun Tropical recolectó en el Golfo de Panama muestras cuantitativas de fitoplancton en la superficie y a los diez metros, como sigue: a) Del 18 al 21 de marzo de 1958 (31 estaciones)-durante el maximum de la estación de afloramiento. b) Del 10 al 12 de julio de 1957 (10 estaciones)-durante la epóca de transición a la estación lluviosa cuando reaparecen los vientos ligeros que causan el afloramiento. c) Del 7 al 8 de noviembre de 1957 (15 estaciones)-durante el maximum de la estación lluviosa. 2. Las poblaciones maximas de fitoplancton aparecieron durante la estación de afloramiento, seguido por una considerable disminución durante el mes de julio y una calma durante noviembre. 3. Durante la investigación se observó una remarcable uniformidad regional en la composición de las especies a pesar de las diferencias regionales en las condiciones de crecimiento. Las diatomeas predominaban en gran numero en las comunidades. 4. Durante todas las investigaciones, las regiones mas cerca de la costa, generalmente al norte de los 8°30'N, eran las mas productivas. Las areas menos productivas fueron las mar afuera de las Bahias de San Miguel y Parita, lo que sugiere que el aumento en las sales nutritivas causado por las escorrentias es inadecuado para sostener poblaciones grandes de plantas autotróficas en estas regiones. 5. Durante todas las investigaciones, el crecimiento del fitoplancton parecio estar limitado por la disponibilidad de las. sales nutritivas. 6. Durante todas las investigaciones el crecimiento del fitoplancton parecio estar relacionado con la profundidad de la columna de agua. 7. Aunque las precipitacion por debajo del promedio normal contribuyo a condiciones desusadamente favorables de crecimiento (estabilidad reducida, aumento de la transparencia y, presumiblemente, de la reserva de sales nutritivas) durante la investigación de noviembre en relación a noviembre de 1955 y de 1956 en los 8°45'N, 79°23'W, no se observo-la alta reacción de fitoplancton que se esperaba. 8. Durante la investigación de noviembre, las reacciones locales de las diatomeas y sus fluctuaciones regionales pudieron relacionarse en forma satisfactoria con condiciones asociadas con la salinidad de la superficie. Sin embargo, esta correspondencia puede atribuirse sin duda a factores asociados con los niveles observados de salinidad, probablemente con las sales nutritivas, en lugar de directamente con la salinidad. 9. Condiciones calurosas no comunes ocurrieron durante la investigación de marzo, las que pueden atribuirse a que los vientos que ocasionan el afloramiento fueran mas debiles que los normales, lo que contribuyó a que la cosecha estable fuera considerablemente mas baja y a la demora de tres a cinco semanas en la sucecion relativa a la que se observó durante 1955-1957 en los 8°45'N, 8°23'W, en el Golfo de Panama. 10. Durante la investigación de marzo, existió una relación inversa bien definida entre la temperatura y la abundancia media de las diatomeas en los diez metros superiores, y entre la transparencia y la abundancia media de las diatomeas. Una relación directa ocurrio entre la salinidad de superficie y la abundancia media de las diatomeas en los diez metros superiores. Estas relaciones se interpretan como indicadoras de que la abundancia de diatomeas refleja primeramente las concentraciones de las sales nutritivas asociadas con una intensidad de afloramiento dada, en lugar de describir relaciones causales. 11. Los resultados de la investigacion indican que la dinamica del fitoplancton observada en los 8°45'N, 79°23'W, desde noviembre de 1954 a mayo de 1957, es generalmente representativa del Golfo de Panama. 12. Durante las investigaciones se observaron las siguientes formas nuevas, las que seran descritas en una publicación posterior: Actinoptychus undulatus f. catenata n.f., Asterionella japonica f. tropicum n.f., Leptocylindrus maximus n. sp., Skeletonema costatum f. tropicum n.f.

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Catch data were collected from three beaches in the Mwanza area of lake Victoria, Tanzania for Oreochromis niloticus (L.), Rastrineobola argentea (Pellegrin) and Lates niloticus (L.). Sampling took place in October 1997 and February, June and September 1998. The CPUE for O. niloticus was 3.9 to 6kg boat super(-1) and for R. argentea from 98 to 282 kg boat super(-1). There was no obvious trend in catch rates for L. niloticus. The modal length for O. niloticus recorded at Chole beach was 34cm TL. In February, fish were larger (41-45 cm) than in the other surveys. Rastrineobola argentea caught in October 1997 had modal length at 65 mm TL with some smaller fish. In February and June prominent length modes occurred at 45 and 58 mm respectively, which may represent the same cohort as the small fish caught in October 1997. In September 1998, there were two length modes at 46 and 60 mm. The 60 mm fish may represent the same cohort seen in previous surveys, suggesting growth from approximately 30 mm to 60 mm in an eleven-month period. Lates niloticus landed at Kayenze beach over the four surveys had a modal length of 46 cm TL. Fish species encountered on the three beaches during the surveys were O. niloticus, R. argentea, Bagrus docmak Forsskall, Clarias gariepinus (Burchell), Protopterus aethiopicus Heckel, Labeo victorians Boulenger, Synodontis afrofischeri Hilgendorf, Synodontis victoriae Boulanger, Schilbe intermedius (L.), Brycinus jacksonii (Boulanger), Mormyrus kannume Forsskall and Haplochromine cichlids

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Corynebacterium diphtheriae é um importante patógeno humano e agente causal da difteria. Embora seja observada uma redução mundial no número de casos da doença, a difteria permanece endêmica em muitos países e surtos são esporadicamente notificados. No Brasil, o último surto ocorreu no estado no Maranhão e revelou mudanças em aspectos clínico-epidemiológicos da doença. Diferentemente da maioria das cepas de difteria brasileiras, que pertencem ao biovar mitis, nesse surto dois diferentes pulsotipos de C. diphtheriae biovar intermedius foram isolados. Além disso, sinais patognomônicos da doença não foram relatados em parte dos casos. C. diphtheriae também vem sendo relacionado com quadros de infecções invasivas, apesar de ser reconhecido como patógeno tipicamente extracelular. Em conjunto, estas mudanças no perfil das infecções por C. diphtheriae sugerem a existência de outros fatores de virulência além da produção da toxina diftérica. Neste sentindo, foram realizadas análises de tipagem molecular e de genômica comparativa para avaliar a diversidade genética e o potencial de virulência de cepas de C. diphtheriae isoladas de difteria clássica e infecções invasivas. Os resultados obtidos demonstram a circulação de diferentes clones invasores no Brasil. Além disso, revelaram diferenças marcantes na presença e na composição de ilhas de patogenicidade entre as amostras, bem como nos genes sob regulação do DtxR e nas sequências dos corinefagos integradas ao cromossomo bacteriano. Uma vez que o potencial invasor bacteriano e a persistência no ambiente podem estar relacionados à tolerância ao estresse oxidativo, foram procurados nos genomas sequenciados, genes possivelmente envolvidos neste processo. Dentre estes, os genes DIP0906, predito como gene de resistência ao oxidante telurito (TeO32-), e DIP1421, codificador do regulador transcricional OxyR, foram caracterizados funcionalmente e tiveram seus papéis na patogenicidade investigados. Ensaios in vivo utilizando o nematódeo Caenorhabditis elegans demonstraram que ambos são importantes para a virulência de C. diphtheriae. Além da resistência ao TeO32, DIP0906 parece contribuir para a resistência ao peróxido de hidrogênio (H2O2) e para a viabilidade no interior de células respiratórias humanas. Já OxyR, além de controlar negativamente a resposta ao H2O2, parece estar envolvido com a ligação de C. diphtheriae a proteínas plasmáticas e de matriz extracelular. Adicionalmente, foi investigada resistência e a capacidade de adaptação de C. diphtheriae frente a agentes oxidantes, através da indução de resposta adaptativa e/ou resistência cruzada e da formação de biofilme. As cepas de C. diphtheriae apresentaram diferentes níveis de resistência e um comportamento heterogêneo na presença dos agentes oxidantes, o que sugere a existência de diferentes estratégias de sobrevivência e adaptação de C. diphtheriae nas condições de estresse oxidativo.

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采用PCR技术获得了中国鮡科褶鮡属(Pseudecheneis)5种鱼类及外群种类巨魾[Bagarius yarrelli(Sykes)]和红河纹胸鮡(Glyptothorax fukiensis honghensis Li)的线粒体部分基因序列.序列分析结果表明:间褶鮡(Pseudecheneis intermedius Chu)与平吻褶鮡(P.paviei Vaillant)在Cyt b基因片段上完全无差异,形成单倍型,支持间褶鮡应为平吻褶鮡的同物异名.凭Cyt b基因片段构建了它们的NJ,MP和ML分子树,3棵分子树基本一致,均支持褶鮡属构成一单系群;怒江和伊洛瓦底江"黄斑褶鮡"不同样品分别聚在一起,但二水系的样品未能形成一单系;其他各种的不同样品均能分别聚在一起形成单系.怒江和伊洛瓦底江"黄斑褶鮡"的分类地位值得今后进一步研究.

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Mitochondrial DNA polymorphisms in 15 specimens of three species of slow lorises-Nycticebus coucang, N. intermedius, and N. pygmaeus-were analyzed in order to study the evolutionary relationships among the species. Eight restriction types were observed in the samples. Phylogenetic trees constructed on the basis of genetic distances showed that the slow lorises sort into two clusters: four types of N. coucang and three types of N. intermedius plus one type of N. pygmaeus. Our results suggest that there are two valid species in the genus Nycticebus-N. coucang and N. pygmaeus-and that N. intermedius should be included within N. pygmaeus. Divergence between the two species may have begun 2.7 Ma (million years ago). Evolution of gross morphology, chromosomes, and mitochondrial DNA in the slow lorises appears to be concordant.

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The karyotypes of three species (N. coucang, N. intermedius, and N. pygmaeus) of genus Nycticebus, collected from the southern Yunnan of China, have been studied. All individuals from three species possess 2n=50 chromosomes, and all chromosomes in their complement are biarm chromosomes. The karyotype of slow loris (N. coucang) is characterized by having a secondary constriction and Ag-NORs in the short arms of pair No. 1. The G-banding patterns of three species are very similar. Three species are found to have multiple Ag-NORs. In N. coucang, NORs were observed on five pairs (Nos. 1, 6, 9, 15, and 23) and in N. intermedius and N. pygmaeus, NORs were found on four pairs (Nos. 6, 9, 15, and 20). This finding indicates that slow lorises, as primitive primates, also have multiple NOR-bearing chromosomes. Finally, the classification of genus Nycticebus by karyotype analysis is discussed, and our results suggest that there are at least two valid species, namely: N. coucang and N. pygmaeus.

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The first fishery survey of Lake Victoria was conducted between 1927 and 1928 (Graham 1929). Atthat time, the lake had a diverse fish fauna and the fishery was dominated by two endemic tilapiine cichlids; Oreochromis esculentus (Graham 1929) and O. variabilis (Boulenger 1906). There were a number of other species such as Protopterus aethiopicus Heckel 1851, Bagrus docmac (Forsk.) 1775, Clarias gariepinus (Burchell), Barbus species, mormyrids, Synodontis spp, Schilbe intermedius (Linn.) 1762 and Rastrineobola argentea Pellegrin, 1904 that were also abundant in the lake most of which made a significant contribution to the fishery (Graham 1929, Worthington 1929, 1932, Kudhongania & Cordone 1974). Haplochromine cichlids were represented by at least 300 species more than 99% of them endemic (Greenwood, 1974; Witte et al., 1992 a & b). The fishery of Lake Victoria was similar to that of lakes Kyoga and Nabugabo (Worthington 1929; Trewavas 1933; Greenwood 1965, 1966; Beadle 1962, 1981). There were also important fisheries on the inflowing rivers of Lake Victoria, the most important of which were Labeo victorianus and Barbus altianalis (Cadwallader 1965). The small sized species notably Rastrineobola argentea and haplochromines cichlids were not originally commercially exploited.

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Until the 1970s, Lake Victoria had a multi-species fishery dominated by the tilapiine and haplochromine cichlids. There were important subsidiary fisheries for more than 20 genera of non-cichlid fishes, including catfishes (Bagrus docmak, Clarias gariepinus, Synodontis spp and Schilbe intermedius), the lungfish (Protopterus aethiopicus) and Labeo victorianus) (Kudhongania and Cordone 1974). Stocks of most of these species declined and others disappeared following the introduction of four tilapiines (Oreochromis niloticus, Oreochromis leucostictus, Tilapia rendalli and Tilapia zillit) and Nile perch (Lates niloticus) during the 1950s. Since then the commercial fishery in the Uganda portion of Lake Victoria has been dominated by the Nile perch, Nile tilapia (Oreochromis niloticus) and the native cyprinid species, Rastrineobola argentea (Mukene).

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An overview of the biology and ecology of some of the constantly less important commercial species is given below. These included Bagrus docmac, Clarias gariepinus, Protopterus aethiopicus, Labeo victorianus, Barbus spp, Mormyrids, Synodontis spp, and Schilbe intermedius. The stocks of most of these species declined due to over-exploitation and introduction of non-native fishes especially Nile perch. A few of these taxa still survive in the main lake and others in satellite lakes. The current status of these species in the Victoria lake basin is not known but the available information provided some information on some habitat and other requirements of some of these originally important species of the Victoria lake basin.

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不饱和脂肪酯是人及动物生长发育的必需物质。本论文分析了海洋动植物脂和脂肪酸的组成,并对不饱和脂肪酸的分离提纯方法进行了研究。一、海洋动植物的中性脂主要包括三酰甘油和胆固醇。动物极性脂主要为磷脂,包括磷脂酰丝馆酸(PS)、磷脂酸(PA)、磷脂酰肌醇(PI)、溶解性磷脂酰乙醇胺(LPE)、神经鞘磷脂(CAEP)、磷脂酰胆碱(PC)、磷脂酰乙醇胺(PE),双磷脂酰甘油(DPG)。其中LPE、DPG为动物所特有的磷脂。植物极性脂包括PI、PC、PE、双半乳糖苷地酰甘油酯(DGDG)、硫代6-脱氧葡萄糖苷二酰甘油酯(SQDG)、单半乳糖苷二酰甘油酯(MGDG)、磷脂酰甘油(PG)及植物脑苷脂(Plant Cerebrosides)。其中MGDG、DGDG、SQDG为植物所特有的三种糖脂。二、海洋动植物含有丰富的不饱和脂肪酸,多聚不饱和脂肪酸(PUFA)含量尤为显著。灰凹贻贝(Crenomythilus graiaynus)的二十碳五烯酸(EPA)含量为10.6%,二十碳四烯酸(AA)为3.7%,二十二碳六烯酸(DHA)为14.26%。中间球海胆(Strongylocentrotus intermedius)的AA含量为7.36%,EPA为15.98%。内枝多管藻(Polysiphonia morroωii)PUFA含量非常高,AA占2.43%,20:4ω3占4.97%,EPA占45.03%。裙带菜(Undaria pinnatifida)的PUFA中,十八碳二烯酸占6.16%,AA占12.99%,EPA占7.83%这些PUFA大都为人及动物生长发育的必需脂肪酸。三、尿素诱导法是大量提取混合PUFA的有效方法。在产品中,饱和脂肪酸的含量可以忽略不计,单烯脂肪酸含量降低很多;高吸附能力的柱层析是提取PUFA单体的较好方法,其产物的纯度达98%以上。

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How does fire affect the plant and animal community of the boreal forest? This study attempted to examine the changes in plant composition and productivity, and small mammal demography brought about by fire in the northern boreal environment at Chick Lake, N.W.T. (65053fN, 128°14,W). Two 5*6 ha plots measuring 375m x 150m were selected for study during the summers of 1973 and 197^. One had been unburned for 120 years, the other was part of a fire which burned in the spring of 1969. Grids of 15m x 15m were established in each plot and meter square quadrats taken at each of the 250 grid intersections in order to determine plant composition and density. Aerial primary production was assessed by clipping and drying 80 samples of terminal new production for each species under investigation. Small mammal populations were sampled by placing a Sherman live trap at each grid intersection for ten days in every month. The two plots were similar in plant species composition which suggested that most regrowth in the burned area was from rootstocks which survived the fire. The plant data were submitted to a cluster analysis that revealed nine separate species associations, six of which occured in the burned area and eight of which occured in the control. These were subsequently treated as habitats for purposes of comparison with small mammal distributions. The burned area showed a greater productivity in flowers and fruits although total productivity in the control area was higher due to a large contribution from the non-vascular component. Maximum aerial productivity as dry wieght was measured at 157.1 g/m and 207.8 g/m for the burn and control respectively. Microtus pennsylvanicus and Clethrionomys rutilus were the two most common small mammals encountered; Microtus xanthognathus, Synaptomys borealis, and Phenacomys intermedius also occured in the area. Populations of M. pennsylvanicus and C. rutilus were high during the summer of 1973; however, M. pennsylvanicus was rare on the control but abundant on the burn, while C. rutilus was rare on the burn but abundant in the control. During the summer of 197^ populations declined, with the result that few voles of any species were caught in the burn while equal numbers of the two species were caught in the control. During the summer of 1973 M. pennsylvanicus showed a positive association to the most productive habitat type in the burn which was avoided by C. rutilus. In the control £• rutilus showed a similar positive association to the most productive habitat type which was avoided by M. pennsylvanicus. In all cases for the high population year of 1973# the two species never overlapped in habitat preference. When populations declined in 197^f "both species showed a strong association for the most productive habitat in the control. This would suggest that during a high population year, an abundant species can exclude competitors from a chosen habitat, but that this dominance decreases as population levels decrease. It is possible that M. pennsylvanicus is a more efficient competitor in a recently burned environment, while C. rutilus assumes this role once non-vascular regrowth becomes extensive.

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Cette étude comparative est une révision de la famille des Harrimaniidae basée sur les caractères morphologiques d'espèces connues et nouvelles provenant des collections de William E. Ritter, Theodore H. Bullock et Kandula P. Rao rassemblées au cours du 20e siècle. Les descriptions présentées ici portent le total des genres de cinq à neuf par l'ajout de Horstia n. gen., Mesoglossus n. gen., Ritteria n. gen et Saxipendium, un genre auparavant attribué à la famille monospécifique des Saxipendidae. Le nombre d'espèces est porté à 34 par la description de cinq nouvelles espèces du Pacifique oriental: Horstia kincaidi, Mesoglossus intermedius, Mesoglossus macginitiei, Protoglossus mackiei et Ritteria ambigua. La description d'une sixième espèce, Stereobalanus willeyi Ritter et Davis, 1904 (nomen nudum) est présentée ici pour la première fois, ainsi qu'une description abrégée de Saxipendium coronatum. Quatre espèces précédemment attribuées au genre Saccoglossus sont transférées au genre Mesoglossus: M. bournei, M. caraibicus, M. gurneyi, et M. pygmaeus et Saccoglossus borealis est transféré au genre Harrimania. Une hypothèse phylogénétique sur la famille des Harrimaniidae est émise, présentant l'évolution possible des caractères morphologiques au sein du groupe. Finalement, des notes sur la distribution géographique étendue mais discontinue de plusieurs espèces suggère que les entéropneustes auraient pu avoir une distribution ancienne continue et plus grande qui aurait été fragmentée par la suite.