Los Páramos Del Mundo
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Floristic Composition and Animal Carrying Capacity
International Journal of Applied Research 2019; 5(12): 282-288 ISSN Print: 2394-7500 ISSN Online: 2394-5869 Exclusion of grazing on dry Puna grassland: Floristic Impact Factor: 5.2 IJAR 2019; 5(12): 282-288 composition and animal carrying capacity www.allresearchjournal.com Received: 02-10-2019 Accepted: 05-11-2019 Raúl Yaranga and Olwer Huanca Raúl Yaranga National University of Central Abstract Peru, High Mountain Research The degradation of Andean dry puna grasslands is part of the deterioration of terrestrial ecosystems. As Centre (CIAM), Av. Mariscal a response, exclusionary grazing practices have been applied. However, knowledge of the dynamics of Castilla, Huancayo, Peru, ecological restoration in grasslands is in full development, which is why the evaluation of the changes France that occur in floristic wealth and abundance, ecological condition and animal carrying capacity in two areas excluded from grazing in August 2015 in the Nor-Yauyos Cochas Landscape Reserve, Peru, was Olwer Huanca National Service of Natural proposed. The agrostological evaluation used the method of linear transection of interception points in Areas Protected by the State 32 transects of 10 meters. The evaluation began in the year of the grazing exclusion and at the end of the (SERNANP), Av. 2016 low season and continued until the 2017 low season. Wealth and abundance showed significant Huancavelica 3025, Huancayo, increases only in the rainy season (p = 0.0125), no significant difference in ecological condition or animal Peru, France carrying capacity was observed between seasonal periods, but between plots for p=0.001. In conclusion, the practice of exclusion of grazing did not show a rapid response in the change of biological indicators, which suggests that the evaluation should be carried out in a longer time. -
Plant Diversity and Composition Changes Along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon
diversity Article Plant Diversity and Composition Changes along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon Pablo Lozano 1,*, Omar Cabrera 2 , Gwendolyn Peyre 3 , Antoine Cleef 4 and Theofilos Toulkeridis 5 1 1 Herbario ECUAMZ, Universidad Estatal Amazónica, Km 2 2 vía Puyo Tena, Paso Lateral, 160-150 Puyo, Ecuador 2 Dpto. de Ciencias Biológicas, Universidad Técnica Particular de Loja, San Cayetano Alto s/n, 110-104 Loja, Ecuador; [email protected] 3 Dpto. de Ingeniería Civil y Ambiental, Universidad de los Andes, Cra. 1E No. 19a-40, 111711 Bogotá, Colombia; [email protected] 4 IBED, Paleoecology & Landscape ecology, University of Amsterdam, Science Park 904, 1098 HX Amsterdam, The Netherlands; [email protected] 5 Universidad de las Fuerzas Armadas ESPE, Av. General Rumiñahui s/n, P.O.Box, 171-5-231B Sangolquí, Ecuador; [email protected] * Correspondence: [email protected]; Tel.: +593-961-162-250 Received: 29 April 2020; Accepted: 29 May 2020; Published: 8 June 2020 Abstract: The paramo is a unique and severely threatened ecosystem scattered in the high northern Andes of South America. However, several further, extra-Andean paramos exist, of which a particular case is situated on the active volcano Sumaco, in the northwestern Amazon Basin of Ecuador. We have set an elevational gradient of 600 m (3200–3800 m a.s.l.) and sampled a total of 21 vegetation plots, using the phytosociological method. All vascular plants encountered were typified by their taxonomy, life form and phytogeographic origin. In order to determine if plots may be ensembled into vegetation units and understand what the main environmental factors shaping this pattern are, a non-metric multidimensional scaling (NMDS) analysis was performed. -
A Chronology of Middle Missouri Plains Village Sites
Smithsonian Institution Scholarly Press smithsonian contributions to botany • n u m b e r 9 2 Smithsonian Institution Scholarly Press TaxonomicA Chronology Revision of of the MiddleChiliotrichum Missouri Group Plains Villagesensu stricto Sites (Compositae: Astereae) By Craig M. Johnson Joséwith Mauricio contributions Bonifacino by Stanley A. Ahler, Herbert Haas, and Georges Bonani SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of “diffusing knowledge” was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: “It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge.” This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, com- mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropology Smithsonian Contributions to Botany Smithsonian Contributions in History and Technology Smithsonian Contributions to the Marine Sciences Smithsonian Contributions to Museum Conservation Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology In these series, the Institution publishes small papers and full-scale monographs that report on the research and collections of its various museums and bureaus. The Smithsonian Contributions Series are distributed via mailing lists to libraries, universities, and similar institu- tions throughout the world. Manuscripts submitted for series publication are received by the Smithsonian Institution Scholarly Press from authors with direct affilia- tion with the various Smithsonian museums or bureaus and are subject to peer review and review for compliance with manuscript preparation guidelines. -
Glossary Glossary
Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts. -
Tungurahua Volcano, Ecuador: Structure, Eruptive History and Hazards
Journal of Volcanology and Geothermal Research 91Ž. 1999 1±21 www.elsevier.comrlocaterjvolgeores Tungurahua Volcano, Ecuador: structure, eruptive history and hazards Minard L. Hall a,1, Claude Robin b,), Bernardo Beate c, Patricia Mothes a,1, Michel Monzier a,d,2 a Instituto Geofõsico,ÂÂ Escuela Politecnica Nacional, P.O. Box 1701-2759, Quito, Ecuador b Institut de Recherches Pour le DeÂÕeloppement() IRD, ex-ORSTOM , UR 6, OPGC, 5 Rue Kessler, 63038, Clermont-Ferrand, France c Departamento de Geologõa,ÂÂÂ Facultad de Geologõa, Minas y Petroleos, Escuela Politecnica Nacional, P.O. Box 1701-2759, Quito, Ecuador d Institut de Recherches pour le DeÂÕeloppement() IRD, ex-ORSTOM , UR 6, A.P. 17-11-6596, Quito, Ecuador Accepted 25 March 1999 Abstract Tungurahua, one of Ecuador's most active volcanoes, is made up of three volcanic edifices. Tungurahua I was a 14-km-wide andesitic stratocone which experienced at least one sector collapse followed by the extrusion of a dacite lava series. Tungurahua II, mainly composed of acid andesite lava flows younger than 14,000 years BP, was partly destroyed by the last collapse event, 2955"90 years ago, which left a large amphitheater and produced a ;8-km3 debris deposit. The avalanche collided with the high ridge immediately to the west of the cone and was diverted to the northwest and southwest for ;15 km. A large lahar formed during this event, which was followed in turn by dacite extrusion. Southwestward, the damming of the Chambo valley by the avalanche deposit resulted in a ;10-km-long lake, which was subsequently breached, generating another catastrophic debris flow. -
Multiple Sources for Tephra from AD 1259 Volcanic Signal in Antarctic Ice
Multiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino To cite this version: Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino. Mul- tiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores. Quaternary Science Reviews, Elsevier, 2019, 210, pp.164-174. 10.1016/j.quascirev.2019.03.005. hal-02350371 HAL Id: hal-02350371 https://hal.archives-ouvertes.fr/hal-02350371 Submitted on 25 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Manuscript Details Manuscript number JQSR_2019_21 Title MULTIPLE SOURCES FOR TEPHRA FROM AD 1259 VOLCANIC SIGNAL IN ANTARCTIC ICE CORES Abstract Strong volcanic signals simultaneously recorded in polar ice sheets are commonly assigned to major low-latitude eruptions that dispersed large quantities of aerosols in the global atmosphere with the potential of inducing climate perturbations. Parent eruptions responsible for specific events are typically deduced from matching to a known volcanic eruption having coincidental date. However, more robust source linkage can be achieved only through geochemical characterisation of the airborne volcanic glass products (tephra) sometimes preserved in the polar strata. -
Plantae, Magnoliophyta, Asterales, Asteraceae, Senecioneae, Pentacalia Desiderabilis and Senecio Macrotis: Distribution Extensions and First Records for Bahia, Brazil
Check List 4(1): 62–64, 2008. ISSN: 1809-127X NOTES ON GEOGRAPHIC DISTRIBUTION Plantae, Magnoliophyta, Asterales, Asteraceae, Senecioneae, Pentacalia desiderabilis and Senecio macrotis: Distribution extensions and first records for Bahia, Brazil. Aristônio M. Teles João R. Stehmann Universidade Federal de Minas Gerais, Instituto de Ciências Biológicas, Departamento de Botânica. Caixa Postal 486, CEP 31270-091, Belo Horizonte, MG, Brazil. E-mail: [email protected] Senecioneae is the biggest Tribe of the Asteraceae state of Minas Gerais (Cabrera 1957; Hind (Nordestam 1996), comprising 150 genera (more 1993a). Senecio macrotis is a robust herb or than 9 % of all genera) and 3,500 species (about shrub, with lyrate-pinnatisect leaves, discoid 15 % of all species of the Family) (Nordenstam heads, and paniculate capitulescences (Cabrera 2007). The circumscription of many Senecioneae 1957). It is found typically in the Campos genera has changed, especially Senecio L., with Rupestres of the Espinhaço range, growing in about 1,250 species (Bremer 1994; Frodin 2004; altitudes ranging from 900 to 1,000 m (Vitta 2002). Nordenstam 2007). To Brazilian Senecioneae, Hind (1993a) estimated the occurrence of 97 The genus Pentacalia Cass., formerly included in species belonging to eight genera, and the more the synonymy of Senecio (lato sensu) (Barkley useful works to identify them are Cabrera (1950, 1985) and resurrected by Robinson and 1957), Cabrera and Klein (1975), Robinson Cuatrecasas (1978), comprises about 205 species (1980), Hind (1993a; 1993b; 1994; 1999), and distributed along Tropical America (Jeffrey 1992). Teles et al. (2006). Hind (1993a) cited the occurrence of two Brazilian species, P. desiderabilis (Vell.) Cuatrec. Senecio (stricto sensu) is characterized by annual and P. -
La Cultura Como Factor De Innovación Económica Y Social Abril 2012
tom0 01 la Cultura Como faCtor de InnovaCIÓn eConÓmica y social Abril 2012 Projet cofinancé par le Fonds Européen de Développement Régional et l’Instrument d’Aide de Pré-Adhésion Project cofinanced by the European Regional Development Fund and the Instrument for Pre-Accession Assistance Coordinación científica: Pau Rausell Köster Coordinación editorial: Raúl Abeledo Sanchis Colaboradores: Blanco Sierra, Óscar (Econcult, UV) Boix Doménech, Rafael (Departamento de Estructura Económica, UV) De Miguel Molina, Blanca (UPV) Hervás Oliver, José Luis (UPV) Marco-Serrano, Francisco (K|P|K, UV) Pérez-Bustamante Yábar, Diana (Universidad Rey Juan Carlos) Pérez Vázquez, Pedro (MC2, UV) Vila Lladosa, Luis (MC2, UV) Diseño y maquetación: Priska Vigo Traducción: Redactalia, Gabriela Harsulescu, Annabel Kay Corrección: Júlia Sorribes Agradecimientos: Nos gustaría dar las gracias tanto a todos los colaboradores como a los demás socios del proyecto Sostenuto, que nos proporcionaron información de gran valor para nuestras investigaciones. Este informe ha sido elaborado por la Unidad de Investigación en Economía de la Cultura y Turismo (Econcult) – Instituto Interuniversitario de Desarrollo Local (IIDL) – de la Universitat de València, en el marco del Proyecto Sostenuto, co-financiado por el Programa Interreg IV B Med de la Unión Europea. Para saber más sobre el proyecto Sostenuto: http://sostenutoblog.wordpress.com Informe publicado bajo una licencia Creative Commons (Reconocimiento-No Comercial-Sin obras Derivadas 3.0). http://creativecommons.org/licenses/by-nc-nd/3.0/ Nota El proyecto Sostenuto, que reunió a siete socios de muy distinta naturaleza, tenía el objetivo de promover la reflexión sobre la innovación económica y social en el espacio Med. -
Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: the Indonesian Example
geosciences Review Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: The Indonesian Example Mukhamad N. Malawani 1,2, Franck Lavigne 1,3,* , Christopher Gomez 2,4 , Bachtiar W. Mutaqin 2 and Danang S. Hadmoko 2 1 Laboratoire de Géographie Physique, Université Paris 1 Panthéon-Sorbonne, UMR 8591, 92195 Meudon, France; [email protected] 2 Disaster and Risk Management Research Group, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta 55281, Indonesia; [email protected] (C.G.); [email protected] (B.W.M.); [email protected] (D.S.H.) 3 Institut Universitaire de France, 75005 Paris, France 4 Laboratory of Sediment Hazards and Disaster Risk, Kobe University, Kobe City 658-0022, Japan * Correspondence: [email protected] Abstract: This paper discusses the relations between the impacts of volcanic eruptions at multiple- scales and the related-issues of disaster-risk reduction (DRR). The review is structured around local and global impacts of volcanic eruptions, which have not been widely discussed in the literature, in terms of DRR issues. We classify the impacts at local scale on four different geographical features: impacts on the drainage system, on the structural morphology, on the water bodies, and the impact Citation: Malawani, M.N.; on societies and the environment. It has been demonstrated that information on local impacts can Lavigne, F.; Gomez, C.; be integrated into four phases of the DRR, i.e., monitoring, mapping, emergency, and recovery. In Mutaqin, B.W.; Hadmoko, D.S. contrast, information on the global impacts (e.g., global disruption on climate and air traffic) only fits Review of Local and Global Impacts the first DRR phase. -
University of Florida Thesis Or Dissertation Formatting
THE ANATOMY OF ROMAN EPIC: A STUDY OF POETIC VIOLENCE By JAMES MOSS LOHMAR A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2013 1 © 2013 James Moss Lohmar 2 Meis parentibus sororibusque bellis 3 ACKNOWLEDGMENTS I must first thank my mother, for forcing me to take Latin, and my father, for always talking shop. My sisters, Sarah and Elizabeth, have supported me throughout my studies, and their enthusiasm for my progress is always welcome. I have profound respect for Dr. Robert Burgess and Professors Mario Erasmo and James Anderson, without whose enthusiasm and instruction my decision to pursue a Ph.D. would have never come about. My gratitude goes to Professor Victoria Pagán and the students of her Lucan seminar during Fall 2009, whence the nascent stages of this project were born. My thanks go to Seth Boutin, Megan Daly and George Hendren, in particular, for their erudition and collegial support in this process. Lindsay Rogers offered me much support in the way of professional and academic advice throughout my graduate studies. I have appreciated the criticisms of Professor Gene Witmer in UF Philosophy, who has offered help in making this project appeal to a non-specialist audience. His suggestions of horror bibliography and modern film comparanda have been indispensible. Professor Kostas Kapparis has been a steady mentor in my teaching and writing since I began Ph.D. work, and his objectivity has kept my argument grounded in the text. -
Determinación Del Volumen Del Casquete De Hielo Del Volcán Cotopaxi
DETERMINACIÓN DEL VOLUMEN DEL CASQUETE DE HIELO DEL VOLCÁN COTOPAXI M. Hall – P. Mothes INAMHI Instituto Nacional de Meteorología e Hidrología IRD Institut de Recherche pour le Développement IG-EPN Instituto de Geofísica de la Escuela Politécnica Nacional INGEOMINAS Instituto Colombiano de Geología y Minería Por Bolívar Cáceres, Jair Ramírez, Bernard Francou, Jean-Philippe Eissen, Jean-Denis Taupin, Ekkehard Jordan, Lars Ungerechts, Luis Maisincho, Diego Barba, Eric Cadier, Rodolphe Bucher, Arturo Peñafiel, Pablo Samaniego, Patricia Mothes 2 “Un nevado de los alrededores, que se llama Cotopaxi, se había despertado después de 200 años, después de tantos años de silencio, para recomenzar a echar fuego y llamas y una gran cantidad de polvo sulfuroso que se iba disipando hasta perderse en las inmediaciones: la hierba y las praderas se ahogaron. La mayor parte del ganado, que no encontró nada que pastar en los campos, murió de hambre y necesidad, y este polvo se extendió más de 60 leguas a la redonda. El año pasado, desde el mes de noviembre hasta ahora, hubo los daños más terribles; el fuego interno, que fundió la nieve de la cual estaba cubierta la cima de la montaña, formó un torrente tan terrible que se llevó consigo casas, terrenos, hombres, mujeres, manufacturas de textiles de las comarcas, echó abajo la mayoría de los puentes que desde las calles del poblado cruzan las diferentes corrientes de agua que descienden de esta montaña y nos causaron además, por infección del aire, una enfermedad también llamada Cotopaxi, que no era otra cosa que la parodititis conglomerada”. Joseph de Jussieu, 16 de marzo, 1745, Lettre à son frère. -
Géologie Et Biodiversité Végétale Quelques Rappels
Géologie et Biodiversité végétale Quelques rappels Modifications climatiques Isolement géographique génèrent de la biodiversité Rift Est-Africain : Longueur : 6000 km Ecartement : 1 cm/an Début : il y a 20 MA Sommets : Volcans sauf Rwenzori Ages : 2 à 3 Ma Kili : activité récente Meru : encore actif Petite parenthèse Cette région est considérée comme le berceau de l’humanité Théorie développée par Yves Coppens… Mais… Mais revenons à la botanique… avec les Seneçons géants Du genre Dendrosenecio Dendrosenecio adnivalis 11 espèces. erici-rosenii elgonensis Initialement comprises dans le genre Senecio cheranganensis Se rencontrent entre 2500 m et 4600 m sur brassiciformis les montagnes d’Afrique de l’Est. battiscombei keniodendron keniensis kilimandjari Senecio ovatus (Seneçon de Fuchs) johnstonii meruensis Dendrosenecio adnivalis Rwenzori erici-rosenii elgonensis Elgon cheranganensis Cherangani brassiciformis battiscombei Aderb . keniodendron Kenya keniensis kilimandjari Kilimandjaro johnstonii meruensis Meru Dendrosenecio adnivalis Rwenzori erici-rosenii elgonensis Elgon cheranganensis Cherangani brassiciformis battiscombei Aderb . keniodendron Kenya keniensis kilimandjari Kilimandjaro johnstonii meruensis Meru Mt Stanley 5109 m Rwenzori Lobelia 3500 m 3800 m Lobelia deckenii Dendrosenecio keniensis 4500 m Lobelia telekiii 4300 m Dendrosenecio keniodendron Kilimandjaro 4000 m Dendrosenecio kilimandjari Lien de parenté avec les genres proches: Euryops brownei Cineraria deltoidea Dendrosenecio Le genre Dendrosenecio est très isolé, les genres