Phylogenomics of the Hyalella Amphipod Species-Flock of The
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Salt Lakes and Pans
SCIENCE FOCUS: Salt Lakes and Pans Ancient Seas, Modern Images SeaWiFS image of the western United States. The features of interest that that will be discussed in this Science Focus! article are labeled on the large image on the next page. (Other features and landmarks are also labeled.) It should be no surprise to be informed that the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) was designed to observe the oceans. Other articles in the Science Focus! series have discussed various oceanographic applications of SeaWiFS data. However, this article discusses geological features that indicate the presence of seas that existed in Earth's paleohistory which can be discerned in SeaWiFS imagery. SeaWiFS image of the western United States. Great Salt Lake and Lake Bonneville The Great Salt Lake is the remnant of ancient Lake Bonneville, which gave the Bonneville Salt Flats their name. Geologists estimate that Lake Bonneville existed between 23,000 and 12,000 years ago, during the last glacial period. Lake Bonneville's existence ended abruptly when the waters of the lake began to drain rapidly through Red Rock Pass in southern Idaho into the Snake River system (see "Lake Bonneville's Flood" link below). As the Earth's climate warmed and became drier, the remaining water in Lake Bonneville evaporated, leaving the highly saline waters of the Great Salt Lake. The reason for the high concentration of dissolved minerals in the Great Salt Lake is due to the fact that it is a "terminal basin" lake; water than enters the lake from streams and rivers can only leave by evaporation. -
The Endemic Gastropod Fauna of Lake Titicaca: Correlation Between
The endemic gastropod fauna of Lake Titicaca: correlation between molecular evolution and hydrographic history Oliver Kroll1, Robert Hershler2, Christian Albrecht1, Edmundo M. Terrazas3, Roberto Apaza4, Carmen Fuentealba5, Christian Wolff1 & Thomas Wilke1 1Department of Animal Ecology and Systematics, Justus Liebig University Giessen, Germany 2National Museum of Natural History, Smithsonian Institution, Washington, D.C. 3Facultad de Ciencias Biologicas, Universidad Nacional del Altiplano, Puno, Peru 4Instituto de Ecologıa,´ Universidad Mayor de San Andres, La Paz, Bolivia 5Departamento de Zoologia, Universidad de Concepcion, Chile Keywords Abstract Altiplano, Heleobia, molecular clock, phylogeography, species flock. Lake Titicaca, situated in the Altiplano high plateau, is the only ancient lake in South America. This 2- to 3-My-old (where My is million years) water body has had Correspondence a complex history that included at least five major hydrological phases during the Thomas Wilke, Department of Animal Ecology Pleistocene. It is generally assumed that these physical events helped shape the evo- and Systematics, Justus Liebig University lutionary history of the lake’s biota. Herein, we study an endemic species assemblage Giessen, Heinrich Buff Ring 26–32 (IFZ), 35392 in Lake Titicaca, composed of members of the microgastropod genus Heleobia,to Giessen, Germany. Tel: +49-641-99-35720; determine whether the lake has functioned as a reservoir of relic species or the site Fax: +49-641-99-35709; of local diversification, to evaluate congruence of the regional paleohydrology and E-mail: [email protected] the evolutionary history of this assemblage, and to assess whether the geographic distributions of endemic lineages are hierarchical. Our phylogenetic analyses in- Received: 17 February 2012; Revised: 19 April dicate that the Titicaca/Altiplano Heleobia fauna (together with few extralimital 2012; Accepted: 23 April 2012 taxa) forms a species flock. -
Línea Base De Conocimientos Sobre Los Recursos Hidrológicos E Hidrobiológicos En El Sistema TDPS Con Enfoque En La Cuenca Del Lago Titicaca ©Roberthofstede
Línea base de conocimientos sobre los recursos hidrológicos e hidrobiológicos en el sistema TDPS con enfoque en la cuenca del Lago Titicaca ©RobertHofstede Oficina Regional para América del Sur La designación de entidades geográficas y la presentación del material en esta publicación no implican la expresión de ninguna opinión por parte de la UICN respecto a la condición jurídica de ningún país, territorio o área, o de sus autoridades, o referente a la delimitación de sus fronteras y límites. Los puntos de vista que se expresan en esta publicación no reflejan necesariamente los de la UICN. Publicado por: UICN, Quito, Ecuador IRD Institut de Recherche pour Le Développement. Derechos reservados: © 2014 Unión Internacional para la Conservación de la Naturaleza y de los Recursos Naturales. Se autoriza la reproducción de esta publicación con fines educativos y otros fines no comerciales sin permiso escrito previo de parte de quien detenta los derechos de autor con tal de que se mencione la fuente. Se prohíbe reproducir esta publicación para venderla o para otros fines comerciales sin permiso escrito previo de quien detenta los derechos de autor. Con el auspicio de: Con la colaboración de: UMSA – Universidad UMSS – Universidad Mayor de San André Mayor de San Simón, La Paz, Bolivia Cochabamba, Bolivia Citación: M. Pouilly; X. Lazzaro; D. Point; M. Aguirre (2014). Línea base de conocimientos sobre los recursos hidrológicos en el sistema TDPS con enfoque en la cuenca del Lago Titicaca. IRD - UICN, Quito, Ecuador. 320 pp. Revisión: Philippe Vauchel (IRD), Bernard Francou (IRD), Jorge Molina (UMSA), François Marie Gibon (IRD). Editores: UICN–Mario Aguirre; IRD–Marc Pouilly, Xavier Lazzaro & DavidPoint Portada: Robert Hosfstede Impresión: Talleres Gráficos PÉREZ , [email protected] Depósito Legal: nº 4‐1-196-14PO, La Paz, Bolivia ISBN: nº978‐99974-41-84-3 Disponible en: www.uicn.org/sur Recursos hidrológicos e hidrobiológicos del sistema TDPS Prólogo Trabajando por el Lago Más… El lago Titicaca es único en el mundo. -
Lake Titicaca
Lake Basin Management Initiative Experience and Lessons Learned Brief Lake Titicaca Mario Francisco Revollo Vargas* Maximo Liberman Cruz Alberto Lescano Rivero 1. Description Drought and floods are the natural hazards that have the greatest environmental, social and eco- nomic impact on the Bolivian-Peruvian high plateau (altiplano) which includes the hydrological basin of Lake Titicaca, the Desaguadero River, Lake Poopo and the Salt Lake of Coipasa, collec- tively designated by the acronym TDPS. Through good management, the system can be regulated in benefit of the people who live in the region. Territorial Scope The project area (Figure 1) includes the hydrological basins of Lake Titicaca, the Desaguadero River, and lakes Poopo and Salar de Coipasa (TDPS system). The TDPS system is located in parts of Peru, Bolivia and Chile, spread between latitude 14° 03' to 20° 00' South and between longitude 66° 21' to 71° 07' West. The total area of the system is 143,900 km2 and includes the sub-region Puno in Peru and the departments of La Paz and Oruro in Bolivia. The basins included in the TDPS system have the following characteristics: Lake Titicaca This paper was presented at the Lake Basin Management Initiative 2 Regional Workshop for Europe, Central Asia and the Americas catchment area: 56,270 km 2 held at Saint Michaelʼs College in Vermont, USA, 18-21 June - average lake area: 8,400 km 2003. The workshop was organized by LakeNet in cooperation with SMC and the International Lake Environment Committee medium altitude: 3,810 m above sea level 3 with funding from the Global Environment Facility, U.S. -
Cladistic Revision of Talitroidean Amphipods (Crustacea, Gammaridea), with a Proposal of a New Classification
CladisticBlackwell Publishing, Ltd. revision of talitroidean amphipods (Crustacea, Gammaridea), with a proposal of a new classification CRISTIANA S. SEREJO Accepted: 8 December 2003 Serejo, C. S. (2004). Cladistic revision of talitroidean amphipods (Crustacea, Gammaridea), with a proposal of a new classification. — Zoologica Scripta, 33, 551–586. This paper reports the results of a cladistic analysis of the Talitroidea s.l., which includes about 400 species, in 96 genera distributed in 10 families. The analysis was performed using PAUP and was based on a character matrix of 34 terminal taxa and 43 morphological characters. Four most parsimonious trees were obtained with 175 steps (CI = 0.617, RI = 0.736). A strict consensus tree was calculated and the following general conclusions were reached. The superfamily Talitroidea is elevated herein as infraorder Talitrida, which is subdivided into three main branches: a small clade formed by Kuria and Micropythia (the Kurioidea), and two larger groups maintained as distinct superfamilies (Phliantoidea, including six families, and Talitroidea s.s., including four). Within the Talitroidea s.s., the following taxonomic changes are proposed: Hyalellidae and Najnidae are synonymized with Dogielinotidae, and treated as subfamilies; a new family rank is proposed for the Chiltoniinae. Cristiana S. Serejo, Museu Nacional/UFRJ, Quinta da Boa Vista s/n, 20940–040, Rio de Janeiro, RJ, Brazil. E-mail: [email protected] Introduction Table 1 Talitroidean classification following Barnard & Karaman The talitroideans include amphipods ranging in length from 1991), Bousfield (1996) and Bousfield & Hendrycks (2002) 3 to 30 mm, and are widely distributed in the tropics and subtropics. In marine and estuarine environments, they are Superfamily Talitroidea Rafinesque, 1815 Family Ceinidae Barnard, 1972 usually found in shallow water, intertidally or even in the supra- Family Dogielinotidae Gurjanova, 1953 littoral zone. -
The Hyalella (Crustacea: Amphipoda) Species Cloud of the Ancient Lake Titicaca Originated from Multiple Colonizations
Accepted Manuscript The Hyalella (Crustacea: Amphipoda) species cloud of the ancient Lake Titicaca originated from multiple colonizations Sarah J. Adamowicz, María Cristina Marinone, Silvina Menu Marque, Jeffery W. Martin, Daniel C. Allen, Michelle N. Pyle, Patricio R. De los Ríos-Escalante, Crystal N. Sobel, Carla Ibañez, Julio Pinto, Jonathan D.S. Witt PII: S1055-7903(17)30154-9 DOI: https://doi.org/10.1016/j.ympev.2018.03.004 Reference: YMPEV 6076 To appear in: Molecular Phylogenetics and Evolution Received Date: 18 February 2017 Revised Date: 13 February 2018 Accepted Date: 5 March 2018 Please cite this article as: Adamowicz, S.J., Cristina Marinone, M., Menu Marque, S., Martin, J.W., Allen, D.C., Pyle, M.N., De los Ríos-Escalante, P.R., Sobel, C.N., Ibañez, C., Pinto, J., Witt, J.D.S., The Hyalella (Crustacea: Amphipoda) species cloud of the ancient Lake Titicaca originated from multiple colonizations, Molecular Phylogenetics and Evolution (2018), doi: https://doi.org/10.1016/j.ympev.2018.03.004 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. The final publication is available at Elsevier via https://doi.org/10.1016/j.ympev.2018.03.004. © 2018. -
Bioassessment of Lake Mexia
Bioassessment of Lake Mexia Adam Whisenant Water Resources Branch Texas Parks and Wildlife Department Tyler, TX and Wilson Snyder Field Operations Division Texas Commission on Environmental Quality Waco, TX February 2010 Water Quality Technical Series WQTS-2010-01 Acknowledgments Appreciation is extended to Melissa Mullins, Greg Conley, John Tibbs, Floyd Teat, Milton Cortez, and Michael Baird of the Texas Parks and Wildlife Department (TPWD), and Robert Ozment and Rodney Adams of the Texas Commission on Environmental Quality (TCEQ), for extensive assistance with field work, to Gordon Linam, TPWD, for plankton analyses and to Bill Harrison, TCEQ, who provided assistance with the benthic macroinvertebrate analysis. Appreciation is also extended to Pat Radloff with TPWD and the TPWD-TCEQ Water Quality Standards interagency workgroup for providing a forum to discuss the water quality concerns at Lake Mexia. Thanks to the reviewers who provided invaluable input: Pat Radloff, Cindy Contreras, Roy Kleinsasser, Gordon Linam, Joan Glass, John Tibbs and Mark Fisher with TPWD; Bill Harrison, Lori Hamilton, Ann Rogers, Jill Csekitz, and Pat Bohannon with TCEQ; Jack Davis with the Brazos River Authority and Ryan King with Baylor University. 2 Executive Summary Lake Mexia (Segment 1210) was included on the 2002 Texas list of impaired water bodies (“303(d) list”) as a concern due to depressed dissolved oxygen concentrations. In response to the concern, a dissolved oxygen monitoring project and concurrent bioassessment were conducted by the Texas Commission on Environmental Quality (TCEQ) and Texas Parks and Wildlife Department (TPWD) in 2002 and 2003. The bioassessment included fish, benthic macroinvertebrate, zooplankton, aquatic macrophyte and shoreline habitat surveys. -
Lake Titicaca
III. PALEOHYDROLOGY IIL1. A 20,000 years paleohydrological record from Lake Titicaca DENIS WIRRMANN, JEAN-PIERRE YBERT and PHILIPPE MOURGUIART The Bolivian Altiplano is an endorheic basin which extends from 16° to 20° S. Lat. and from 65° to 69°W. Long., with altitudes ranging from 3700 to 4600 metres, covering 200,000 km2 between the Western and Eastern Cordilleras which are 6500 m high (Fig. 1). From north to south, three major lacustrine areas occupy this high plateau: 2 - Lake Titicaca at 3809 metres above sea level, covering 8562 km ; 2 - Lake Poopo at 3686 m.a.s.l. covering 2530 km ; - Coipasa-Uyuni, a group of dry salt lakes, covering 11 ,000 km2 at 3653 m.a.s.l. Over the last 1.8 million years these basins have registered episodes of greatly enlarged lake areas. According to Lavenu et al. (1984) and to Servant and Fontes (1978, 1984), the Pleistocene record of Titicaca lake level fluctu ations can be summarised as follows: - during the Early Pleistocene the paleolake Mataro rose with a water level established at 140 metres above the present level. This stage is related to the end of the Calvario glaciation (Servant, 1977) and the corresponding deposits are recognisable mainly at the NW edge of the basin; - the paleolake Cabana occurred during the middle Pleistocene with a water level established at 90 metres above the present Lake Titicaca level: the associated sediments are present on the eastern and western shores of the basin; - then with the retreat of the Sorata glaciation (Servant, 1977) the Ballivian stage occurred with -
Estudio Del Registro Histórico Del Contenido De Metales Y Metaloides
Estudio del registro histórico del contenido de metales y metaloides en sedimentos lacustres del Altiplano de Bolivia y su relación con la minería y el fenómeno El Niño Joseline Tapia 1* y Brian Townley 2 1Facultad de Ingeniería, Escuela de Ciencias de la Tierra, Universidad Andrés Bello, Halimeda s/n esq. Talasia, Reñaca, Viña del Mar, Chile 2Facultad de Ciencias Físicas y Matemáticas, Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile * E-mail: [email protected] Resumen. El Altiplano de Bolivia ha sufrido históricamente completamente a fines de este siglo (García et al. 2005). fluctuaciones climáticas a una escala de tiempo interanual, variando desde condiciones estivales australes En los comienzos de la República, la minería de Bolivia extremadamente secas a extremadamente húmedas, las que han sido asociadas al fenómeno de Oscilación del Sur estaba en ruinas y no fue sino hasta mediados del siglo El Niño (ENSO). Además, a través del siglo XX, la minería XIX que la explotación de Ag mejoró y comenzó la de Sn fue la industria más importante de Bolivia, produciendo (1860). A comienzos del siglo XX la explotación de Sn cantidades importantes de Sb-Bi-Pb-Ag-Sn-W-Zn a nivel relegó a la de Ag a un segundo puesto y Bolivia se mundial. Dataciones, información histórica y el análisis de convirtió en uno de los principales productores de Sn a componentes principales (PCA) de datos obtenidos de nivel mundial. Luego de 1930 la industria del Sn fue digestiones totales, paralelas y datación de sedimentos, afectada por los precios de mercado, y a pesar de su alta permitieron proponer que durante el último siglo la demanda durante la Segunda Guerra Mundial, Bolivia lo explotación y producción de Sn ha influido en la deposición exportó muy por debajo del precio internacional (García et de Sb-Ag-Pb en sedimentos del Altiplano de Oruro y los eventos ENSO han jugado un rol importante en la al., 2005). -
University of Birmingham the Toxicogenome of Hyalella
University of Birmingham The Toxicogenome of Hyalella azteca Poynton, Helen C.; Colbourne, John K.; Hasenbein, Simone; Benoit, Joshua B.; Sepulveda, Maria S.; Poelchau, Monica F.; Hughes, Daniel S.T.; Murali, Shwetha C.; Chen, Shuai; Glastad, Karl M.; Goodisman, Michael A.D.; Werren, John H.; Vineis, Joseph H.; Bowen, Jennifer L.; Friedrich, Markus; Jones, Jeffery; Robertson, Hugh M.; Feyereisen, René; Mechler-Hickson, Alexandra; Mathers, Nicholas DOI: 10.1021/acs.est.8b00837 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Poynton, HC, Colbourne, JK, Hasenbein, S, Benoit, JB, Sepulveda, MS, Poelchau, MF, Hughes, DST, Murali, SC, Chen, S, Glastad, KM, Goodisman, MAD, Werren, JH, Vineis, JH, Bowen, JL, Friedrich, M, Jones, J, Robertson, HM, Feyereisen, R, Mechler-Hickson, A, Mathers, N, Lee, CE, Biales, A, Johnston, JS, Wellborn, GA, Rosendale, AJ, Cridge, AG, Munoz-Torres, MC, Bain, PA, Manny, AR, Major, KM, Lambert, FN, Vulpe, CD, Tuck, P, Blalock, BJ, Lin, YY, Smith, ME, Ochoa-Acuña, H, Chen, MJM, Childers, CP, Qu, J, Dugan, S, Lee, SL, Chao, H, Dinh, H, Han, Y, Doddapaneni, H, Worley, KC, Muzny, DM, Gibbs, RA & Richards, S 2018, 'The Toxicogenome of Hyalella azteca: A Model for Sediment Ecotoxicology and Evolutionary Toxicology', Environmental Science and Technology, vol. 52, no. 10, pp. 6009-6022. https://doi.org/10.1021/acs.est.8b00837 Link to publication on Research at Birmingham portal Publisher Rights Statement: This document is the Accepted Manuscript version of a Published Work that appeared in final form in Environmental Science and Technology, copyright © American Chemical Society after peer review and technical editing by the publisher. -
Lake Titicaca (Peru-Bolivia)
THE LIMNOLOGY OF LAKE TITICACA (PERU-BOLIVIA), A Large, High A1 titude Tropical Lake Peter J. Richerson Division of hv.1:ronmentaL Studies ard Institute of EcoZogy Universi* of CaLi,com?ia, Wis Carl Widmer ELbert Cove12 College Uniuer~ityof the PackjYc Stock ton, CaZ-ifimCc Timothy Ki ttel Dfviston of ,%~irortwntatStudies and Ee"coZogy Graduate Group University of California, Davis Institute of Ecology Pub? ication #14, June, 1979 - - esta sincera - Dedicamos monograffa a1 pueblo del Altiplano, con una gratitud profunda y par su ayuda y pacimcia para con nosotros, y a nuestros colegas del Instituto del Mar del * Perb y de la Unjversidad Nacional Tgcnica del A1 tiplano, sin cuya colaboraci6n continua no hubiera sido posible este trabajo. Estamos concientes de que estas personas viven, estudian y enfrentan su realidad para transformarla y enr-iquecerla acorde con el proceso peruano nacional actual. Querems ofre- cer esta monograffa corn nuestra propia contribuci611, aun limitada, de participacidn en ese proceso. The authors are grateful for the financial support provided by the National Geographic Society, the Faresta Institute for Ocean and Mountain Studies, the University of Cal ifornia (through a Rockefel 1er Foundation institutional development grant), the Jastro-Shiel ds Scholarship Comi ttee and the University sf the RacifSc. Widmer was supported by an Organ- ization of American States fellowship and Richerson was partly supported by National Sci- ence EMS during this study. -\ Foundation grants GA-34099 and 75-14273 We are a1 so indebted - to the Instituto del Mar del PerG, the Universidad Nacional Tecnica del A1 tiplano, the Ser- - vf cio Nacional de Meteorelogfa e Midrol ogfa, and to individual s including Victoria Val cgr- cel , Roger Srni th, Fl orentino Tito, Gerald Fisher , John Me1 ack , dswal do Zea , Linda Thorpe , Tim Long, Mayne Wurtsbaugh, Kenso Kawahira, Leigh Speichinger, Fathers Patrick, Eugene and John, and Sister Margaret. -
Evaluation Multicritere Des Techniques De Gestion a La
11e Colloque GEOFCAN 20 et 21 novembre 2018, Antony CONTRIBUTION OF TIME-DOMAIN ELECTROMAGNETICS (TDEM) TO THE KNOWLEDGE OF LAKE TITICACA AQUIFER SYSTEMS, BOLIVIA GABRIELA P. FLORES AVILÉS 1,a, MARC DESCLOITRES 1, CELINE DUWIG 1, ANATOLY LEGCHENKO 1, ÁLVARO SORUCO 2, MAYRA PÉREZ 2, WALDO MEDINACELI 3 1Univ. Grenoble Alpes, CNRS, IRD, Grenoble-INP, IGE, 38000 Grenoble, France, [email protected] 2 University Mayor of San Andres (UMSA), La Paz, Bolivia 3 Ministerio de Medio Ambiente y Agua (Ministry of Water and Environment of Bolivia), La Paz, Bolivia ABSTRACT The increasing demand for water in Bolivia implies a better knowledge of the resources. The aim of this study is to provide the first insight of hydrogeological functioning of a major aquifer between La Paz-El Alto cities and Lake Titicaca. A total of 171 TDEM geophysical soundings, hydrogeological and hydro-geochemical measurements were acquired, and correlated with geological, borehole lithology and topographic information. The results allowed identifying two multilayered aquifer systems (Piedmont and Lacustrine) and the geometry of the different geological layers. The TDEM method proved to be an appropriate method since the results showed a consistent picture of the hydrogeological functioning of the Katari and Lago Menor Aquifer systems. RÉSUMÉ La demande accrue en eau de surface et souterraine en Bolivie implique une meilleure connaissance des ressources. Le but de cette étude est de donner les premières indications sur le fonctionnement des aquifères entre les villes de La-El Alto et le lac Titicaca. 171 sondages géophysiques TDEM et des mesures hydrogeologiques et hydrochimiques ont été mis en œuvre et corrélés avec des informations géologiques (logs de forage) et topographiques.