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Checklist of Freshwater Symbiotic Temnocephalans (Platyhelminthes, Rhabditophora, Temnocephalida) from the Neotropics
Zoosyst. Evol. 90 (2) 2014, 147–162 | DOI 10.3897/zse.90.8688 museum für naturkunde Checklist of freshwater symbiotic temnocephalans (Platyhelminthes, Rhabditophora, Temnocephalida) from the Neotropics Andrés Martínez-Aquino1, Francisco Brusa1, Cristina Damborenea1 1 División Zoología Invertebrados, Museo de La Plata, FCNyM, UNLP, Paseo del Bosque s/n, 1900 La Plata, Argentina http://zoobank.org/286A18D5-FBB4-47E8-93D2-778718848F14 Corresponding author: Cristina Damborenea ([email protected]) Abstract Received 20 July 2014 Based on published records and original data derived from our research, we have generat- Accepted 1 September 2014 ed a checklist of symbiotic temnocephalan fauna from 57 taxa of freshwater invertebrate Published 10 October 2014 and vertebrate hosts from 16 families included in four classes from the Neotropics. The checklist contains 38 nominal species from 3 genera belonging to the Temnocephalida Academic editor: families Diceratocephalidae, Didymorchidae and Temnocephalidae. All taxa (35) of the David Gibson genus Temnocephala are endemic to the Neotropics and 14 (40%) are considered micro- endemic (i.e. only one record each from a single locality). While only one species and Key Words one variety of Didymorchis are known from the Neotropics; there are also two putative undescribed species of this genus. Only Diceratocephala boschmai (Diceratocephalidae) Temnocephala is reported as an introduced species from Uruguay. Host specificity to a particular group Didymorchis of invertebrates and vertebrates is the -
Solanaceae) (Lamarck
The JapaneseSocietyJapanese Society forforPlant Plant Systematics ISSN OOOI-6799 Acta Phytotax, Geobot. 45 (2):95-109 (1994) Distribution of infraspecific taxa of Petunia axillaris (Solanaceae) in Uruguay as revealed analyses by discriminant TOSHIO ANDOi, SHINICHI IIDAi, HISASHI KOKUBUNi, YOSHIHIRO UEDAi and EDUARDO MARCHESI2 iFkeculty 2Flicultad of Hbrticalture, Chiba U}iiversity, 648 Matsudo, Chiba 271; de Agronomia, Uhiversidad de la Republica, Garzon 780, Montevideo, U)uguay Abstract. A survey of native habitats of Petunia species over 5 seasons revealed the co- occurrence of two subspecies of P. axittaris sensu tato in Uruguay. Typical subsp. axiUaris and subsp. parodii were found in south eastern and north western departments, respectively, Using floral measurements (length of corolla tube, corolla limb, pedicel, and calyx lobes, and the length of corolla tube1length of corella limb ratio) of specimens collected in these de- partments, we performed stepwise discriminant analyses. After substituting measurements of 174 specimens collected in the whole of Uruguay into the three discriminant functions thus obtained, we determined them to bc either subsp, c[xittaris or subsp. parodii. Distribution of the two subspecies thus determined by the discriminant functions was roughly delimited by the Rio Negro. A considerable number of doubtfu1 specimens were found in the south west- ern dcpartmcnts, which are on opposite sides of the river de La Plata from the place where secondary intergradation betweell thc two subspecies had been suggested by Wijsman (1982) to have occuiTed, Key words: discriminant function, disnibution, gardcn petunia, geographical taxa, Petunia urillaris, Solanaceae. Received Plebruary 14, i994; accqpted September 30, l994 In 1834, the breeding of garden petunias was started by crossing Petu- nia axitlaris (Lamarck) Britton, Sterns & Poggenburg and P. -
Organización De Aviación Civil Internacional / International Civil
SAM ATSRO/7 INTERNATIONAL CIVIL AVIATION ORGANIZATION South American Regional Office RLA/06/901 Regional Project SEVENTH SAM MEETING ON ATS ROUTES NETWORK OPTIMISATION (SAM ATSRO/7) FINAL REPORT Lima, Peru, 12 to 16 October 2015 The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of ICAO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. i-1 i – Index SAM ATSRO/7 INDEX i - Index .............................................................................................................................................. i-1 ii - History of the Meeting .................................................................................................................. ii-1 Place and duration of the Meeting ................................................................................................ ii-1 Opening ceremony and other matters ........................................................................................... ii-1 Schedule, organization, working methods, Officers and Secretariat ............................................ ii-1 Working languagues ..................................................................................................................... ii-1 Agenda .......................................................................................................................................... ii-1 Attendance -
The World Bank
Docummntof The World Bank FOR OMF AL USE ONLY Public Disclosure Authorized Rqpt NO. 13295 PROJECT COMPLETIONREPORT URUGUAY Public Disclosure Authorized THIRD HIGHWAYPROJECT (LOAN 2238-UR) JUNE 30, 1994 Public Disclosure Authorized Infrastructureand Energy Division Country Department IV Latin America and the Caribbean Regional Office Public Disclosure Authorized This document has a restricted distribution and may be used bv recipients only in the performance of their ofricial duties. Its contents may not otherwise be disclosed witbout World Bank authorization. Fia Year January 1 - December 31 CurrencyEquivaents Year-end 1981 - US$1.00 = Np. 11.59 Year-end 1982 - US$1.00 = Np. 33.75 Year-end 1983 - US$1.00 = Np. 43.25 Year-end 1984 - US$1.00 = Np. 74.25 Year-end 1985 - US$1.00 = Np. 125.00 Year-end 1986 - US$1.00 = Np. 181.00 Year-end 1987 - US$1.00 = Np. 281.00 Year-end 1988 - US$1.00 = Np. 457.50 Year-end 1989 - US$1.00 = Np. 805.00 Year-end 1990 - US$1.00 = Np. 1,594.00 Units of Weightsand Measures: Metric 1 kilometer (kIn) = 0.62 mile (mi) 1 meter (m) = 3.28 feet (ft) 1 kilogram (kg) = 2.20 pounds (lbs) i metric ton = 2,206 pounds (lbs) PrincipalAbbreviations and Acronyms AFE State Railroad Administration (Administraci6nde Ferrocarrilesdel Estado) ANP National Port Administration (Administraci6nNacional de Puertos) DNT National TransportationDirectorate (DirectorateNacional de Transportaci6n) HDM HighwayDesign Model IDB Inter-AmericanDevelopment Bank Intendencia Municipaladministration in each district MTOP Ministry of Transport and Public Works Np. New Uruguayan Pesos TPU Transport Planning Unit of DNT Ualidad National HighwaysDirectorate FOR OFFICIALUSE ONLY THE WORLD BANK Washington, D.C. -
Late Cretaceous Stratigraphy of the Southeastern Chaco - Paraná Basin (“Norte Basin” - Uruguay): the Maastrichtian Age of the Calcretization Process
ISSN: 1980-900X (online) LATE CRETACEOUS STRATIGRAPHY OF THE SOUTHEASTERN CHACO - PARANÁ BASIN (“NORTE BASIN” - URUGUAY): THE MAASTRICHTIAN AGE OF THE CALCRETIZATION PROCESS ESTRATIGRAFIA DO CRETÁCEO SUPERIOR DAS BACIAS DO SUDESTE DO CHACO E DO PARANÁ (“BACIA DO NORTE” – URUGUAI): IDADE MAASTRICHITIANA DO PROCESSO DE CALCRETIZAÇÃO Gerardo VEROSLAVSKY1; Natalie AUBET2; Sergio A. MARTÍNEZ1; Larry M. HEAMAN3; Fernanda CABRERA1; Valeria MESA1 1Universidad de la República de Uruguay. Instituto de Ciencias Geológicas. Iguá 4225 –Montevideo, Uruguay Emails: [email protected]; [email protected]; [email protected]; [email protected] 2Universidad Tecnologica del Uruguay. Departamento de Ciencias Ambientales, Francisco Maciel s/n – Durazno, Uruguay Email: [email protected] 3University of Alberta. Faculty of Earth Sciences. 116 St and 85 Ave., Edmonton, Alberta, Canada Email:[email protected] Introduction Geological Setting Methodology Results Stratigraphic section The Queguay quarry section Lithofacies description General micromorphological features U-Pb geochronology Discussion Lithostratigraphy Non-pedogenic calcretization in the Late Cretaceous Conclusions Acknowledgments References ABSTRACT - In the last 40 years, successive revisions have been introduced to the lithostratigraphy of the Late Cretaceous of the Norte Basin, whose record is formed by predominantly siliciclastic continental fossiliferous sedimentary rocks. A factor that contributed to the terminology proliferation was the misplaced importance attributed to the