Outlook on Climate Change Adaptation in the Tropical Andes Mountains
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Rapid Magma Ascent and Generation of Th Excesses in the Lower Crust At
Earth and Planetary Science Letters 255 (2007) 229–242 www.elsevier.com/locate/epsl Rapid magma ascent and generation of 230Th excesses in the lower crust at Puyehue–Cordón Caulle, Southern Volcanic Zone, Chile ⁎ Brian R. Jicha a, , Brad S. Singer a, Brian L. Beard a, Clark M. Johnson a, Hugo Moreno-Roa b,c, José Antonio Naranjo b a Department of Geology and Geophysics, University of Wisconsin—Madison, 1215 West Dayton Street, Madison WI 53706, USA b Servicio Nacional de Geología y Minería (SERNAGEOMIN), Avenida Santa María, 0104 Santiago, Chile c Observatorio Volcanologico de los Andes del Sur (OVDAS), Cerro Ñielol-Sector Antenas, Temuco, Chile Received 28 July 2006; received in revised form 7 December 2006; accepted 8 December 2006 Available online 30 January 2007 Editor: R.W. Carlson Abstract Basaltic to rhyolitic lavas and tephras erupted over the last 70 kyr at the Puyehue–Cordón Caulle volcanic complex in the Andean Southern Volcanic Zone (SVZ) were analyzed for major and trace element, Sr isotope, and U–Th isotope compositions to constrain the timescales of magmatic processes and identify the subducted and crustal components involved in magma genesis. Internal U–Th mineral isochrons from five lavas and three tephra fall deposits are indistinguishable from their eruption ages, indicating a short period (b1000 yr) of crystal residence in the magma prior to eruption. The (230Th/232Th) ratios define a narrow range (0.80–0.83) compared to that of all SVZ lavas (0.72–0.97), suggesting that Puyehue basalt was derived from a relatively uniform mantle source. Dacites and rhyolites have the largest U excesses and likely evolved via fractional crystallization of a plagioclase-dominated mineral assemblage. -
Muon Tomography Sites for Colombian Volcanoes
Muon Tomography sites for Colombian volcanoes A. Vesga-Ramírez Centro Internacional para Estudios de la Tierra, Comisión Nacional de Energía Atómica Buenos Aires-Argentina. D. Sierra-Porta1 Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia and Centro de Modelado Científico, Universidad del Zulia, Maracaibo-Venezuela, J. Peña-Rodríguez, J.D. Sanabria-Gómez, M. Valencia-Otero Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia. C. Sarmiento-Cano Instituto de Tecnologías en Detección y Astropartículas, 1650, Buenos Aires-Argentina. , M. Suárez-Durán Departamento de Física y Geología, Universidad de Pamplona, Pamplona-Colombia H. Asorey Laboratorio Detección de Partículas y Radiación, Instituto Balseiro Centro Atómico Bariloche, Comisión Nacional de Energía Atómica, Bariloche-Argentina; Universidad Nacional de Río Negro, 8400, Bariloche-Argentina and Instituto de Tecnologías en Detección y Astropartículas, 1650, Buenos Aires-Argentina. L. A. Núñez Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia and Departamento de Física, Universidad de Los Andes, Mérida-Venezuela. December 30, 2019 arXiv:1705.09884v2 [physics.geo-ph] 27 Dec 2019 1Corresponding author Abstract By using a very detailed simulation scheme, we have calculated the cosmic ray background flux at 13 active Colombian volcanoes and developed a methodology to identify the most convenient places for a muon telescope to study their inner structure. Our simulation scheme considers three critical factors with different spatial and time scales: the geo- magnetic effects, the development of extensive air showers in the atmosphere, and the detector response at ground level. The muon energy dissipation along the path crossing the geological structure is mod- eled considering the losses due to ionization, and also contributions from radiative Bremßtrahlung, nuclear interactions, and pair production. -
Magmatic Evolution of the Nevado Del Ruiz Volcano, Central Cordillera, Colombia Minera1 Chemistry and Geochemistry
Magmatic evolution of the Nevado del Ruiz volcano, Central Cordillera, Colombia Minera1 chemistry and geochemistry N. VATIN-PÉRIGNON “‘, P. GOEMANS “‘, R.A. OLIVER ‘*’ L. BRIQUEU 13),J.C. THOURET 14J,R. SALINAS E. 151,A. MURCIA L. ” Abstract : The Nevado del RU~‘, located 120 km west of Bogota. is one of the currently active andesitic volcanoes that lies north of the Central Cordillera of Colombia at the intersection of two dominant fault systems originating in the Palaeozoïc basement. The pre-volcanic basement is formed by Palaeozoïc gneisses intruded by pre-Cretaceous and Tertiarygranitic batholiths. They are covered by lavas and volcaniclastic rocks from an eroded volcanic chain dissected during the late Pliocene. The geologic history of the Nevado del Ruiz records two periods of building of the compound volcano. The stratigraphie relations and the K-Ar dating indicate that effusive and explosive volcanism began approximately 1 Ma ago with eruption of differentiated andesitic lava andpyroclastic flows and andesitic domes along a regional structural trend. Cataclysmic eruptions opened the second phase of activity. The Upper sequences consist of block-lavas and lava domes ranging from two pyroxene-andesites to rhyodacites. Holocene to recent volcanic eruptions, controled by the intense tectonic activity at the intersection of the Palestina fawlt with the regional fault system, are similar in eruptive style and magma composition to eruptions of the earlier stages of building of the volcano. The youngest volcanic activity is marked by lateral phreatomagmatic eruptions, voluminous debris avalanches. ash flow tuffs and pumice falls related to catastrophic collapse during the historic eruptions including the disastrous eruption of 1985. -
Different Environmental Gradients Affect Different Measures of Snake Β-Diversity in the Amazon Rainforests
Different environmental gradients affect different measures of snake β-diversity in the Amazon rainforests Rafael de Fraga1,2,3, Miquéias Ferrão1, Adam J. Stow2, William E. Magnusson4 and Albertina P. Lima4 1 Programa de Pós-Graduação em Ecologia, Instituto Nacional de Pesquisas da Amazônia, Manaus, Amazonas, Brazil 2 Department of Biological Sciences, Macquarie University, Sydney, NSW, Australia 3 Programa de Pós-graduação em Sociedade, Natureza e Desenvolvimento, Universidade Federal do Oeste do Pará, Santarém, Pará, Brazil 4 Coordenação de Biodiversidade, Instituto Nacional de Pesquisas da Amazônia, Manaus, Amazonas, Brazil ABSTRACT Mechanisms generating and maintaining biodiversity at regional scales may be evaluated by quantifying β-diversity along environmental gradients. Differences in assemblages result in biotic complementarities and redundancies among sites, which may be quantified through multi-dimensional approaches incorporating taxonomic β-diversity (TBD), functional β-diversity (FBD) and phylogenetic β-diversity (PBD). Here we test the hypothesis that snake TBD, FBD and PBD are influenced by environmental gradients, independently of geographic distance. The gradients tested are expected to affect snake assemblages indirectly, such as clay content in the soil determining primary production and height above the nearest drainage determining prey availability, or directly, such as percentage of tree cover determining availability of resting and nesting sites, and climate (temperature and precipitation) causing physiological filtering. We sampled snakes in 21 sampling plots, each covering five km2, distributed over 880 km in the central-southern Amazon Basin. We used dissimilarities between sampling sites to quantify TBD, FBD and PBD, Submitted 30 April 2018 which were response variables in multiple-linear-regression and redundancy analysis Accepted 23 August 2018 Published 24 September 2018 models. -
Hospitales a Nivel Nacional
HOSPITALES A NIVEL NACIONAL PROVINCIA: AZUAY ZONA 6 ( 072-822-201) ITEM HOSPITAL TELEFONO 1 HOSPITAL VICENTE CORRAL MOSCOZO 074-096-606/074-096-598 2 HOSPITAL DE SIGSIG 072-266-115/ 072-267-629 3 HOSPITAL EL GIRON 072-276-136/074-275-115 4 HOSPITAL PAUTE 072-250-107/074-250-027 5 HOSPITAL GUALACEO 072-255-064/074-256-537 6 HOSPITAL SANTA ISABEL 072-270-147/072-270-437/074-270-295 7 HOSPITAL MARIANO ESTRELLA 072-847-427 8 CENTRO DE SALUD 1 PUMAPUNGO 072-867-071/072-869-642 9 AREA DE SALUD 2 MIRAFLORES 072-837-665/072-838-155/072-845-015 10 CENTRO DE SALUD 3 TOMEBAMBA 072-822-202/072-836-352 11 CENTRO DE SALUD 4 YANUNCAY 072-893-150/072-892-444/074-2892-390 PROVINCIA: BOLIVAR ZONA 5 ITEM HOSPITAL TELEFONO 1 HOSPITAL ALFREDO NOBOA MONTENEGRO 032-980-230 2 HOSPITAL SAN MIGUEL 032-989-112/032-989-416 3 HOSPITAL CHILLANES 032-978-522/032-978-522 4 CENTRO DE SALUD 1 CORDERO CRESPO 032-985-904/032-980-290 5 CENTRO DE SALUD CALUMA 032-974-394/032-974-709 6 CENTRO DE SALUD EHCEANDIA 032-970-376/032-970-545/032-971-221 HOSPITALES A NIVEL NACIONAL PROVINCIA: CARCHI/TULCÁN ZONA 1 ITEM HOSPITAL TELEFONO 1 HOSPITAL LUIS G. DAVILA 062-980-316/062-980-315 2 HOSPITAL EL ANGEL 062-977-166 3 HOSPITAL SAN GABRIEL 062-290-153/062-290-161 4 CENTRO DE SALUD 1 062-980-396 5 CENTRO DE SALUD SAN JUAN DEL ACHAS 062-648-672 PROVINCIA: CAÑAR ZONA 6 ITEM HOSPITAL TELEFONO 1 HOSPITAL HOMERO C. -
Appendix A. Supplementary Material to the Manuscript
Appendix A. Supplementary material to the manuscript: The role of crustal and eruptive processes versus source variations in controlling the oxidation state of iron in Central Andean magmas 1. Continental crust beneath the CVZ Country Rock The basement beneath the sampled portion of the CVZ belongs to the Paleozoic Arequipa- Antofalla terrain – a high temperature metamorphic terrain with abundant granitoid intrusions that formed in response to Paleozoic subduction (Lucassen et al., 2000; Ramos et al., 1986). In Northern Chile and Northwestern Argentina this Paleozoic metamorphic-magmatic basement is largely homogeneous and felsic in composition, consistent with the thick, weak, and felsic properties of the crust beneath the CVZ (Beck et al., 1996; Fig. A.1). Neodymium model ages of exposed Paleozoic metamorphic-magmatic basement and sediments suggest a uniform Proterozoic protolith, itself derived from intrusions and sedimentary rock (Lucassen et al., 2001). AFC Model Parameters Pervasive assimilation of continental crust in the Central Andean ignimbrite magmas is well established (Hildreth and Moorbath, 1988; Klerkx et al., 1977; Fig. A.1) and has been verified by detailed analysis of radiogenic isotopes (e.g. 87Sr/86Sr and 143Nd/144Nd) on specific systems within the CVZ (Kay et al., 2011; Lindsay et al., 2001; Schmitt et al., 2001; Soler et al., 2007). Isotopic results indicate that the CVZ magmas are the result of mixing between a crustal endmember, mainly gneisses and plutonics that have a characteristic crustal signature of high 87Sr/86Sr and low 145Nd/144Nd, and the asthenospheric mantle (low 87Sr/86Sr and high 145Nd/144Nd; Fig. 2). In Figure 2, we model the amount of crustal assimilation required to produce the CVZ magmas that are targeted in this study. -
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. -
Climate Change and Biodiversity in the Tropical Andes Author(S): Andreas Haller Source: Mountain Research and Development, 32(2):258-259
Climate Change and Biodiversity in the Tropical Andes Author(s): Andreas Haller Source: Mountain Research and Development, 32(2):258-259. 2012. Published By: International Mountain Society DOI: http://dx.doi.org/10.1659/mrd.mm097 URL: http://www.bioone.org/doi/full/10.1659/mrd.mm097 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Mountain Research and Development (MRD) MountainMedia An international, peer-reviewed open access journal published by the International Mountain Society (IMS) www.mrd-journal.org cultural ecosystem services are dis- Geographies’’ aims at facilitating the Climate Change and tinguished, and their strong relation- assessment of the impacts of global Biodiversity in the Tropical ship to human societies is underlined. change on plants, animals, and Andes Chapter 2 analyzes the direct and ecosystems. The authors cover aspects indirect impacts of climate change on of geomorphology, atmospheric Edited by Sebastian K. -
Juvenile Resilience and Adult Longevity Explain Residual Populations of the Andean Wax Palm Ceroxylon Quindiuense After Deforestation
Juvenile Resilience and Adult Longevity Explain Residual Populations of the Andean Wax Palm Ceroxylon quindiuense after Deforestation María José Sanín1*, Fabien Anthelme2,3, Jean-Christophe Pintaud3, Gloria Galeano1, Rodrigo Bernal1 1 Instituto de Ciencias Naturales, Universidad Nacional de Colombia, Bogotá, Distrito Capital, Colombia, 2 Botanique et Bioinformatique de l’Architecture des Plantes, Recherche Agronomique pour Le Développement, Institut de recherche pour le développement, Montpellier, Hérault, France, 3 Botanique et Bioinformatique de l’Architecture des Plantes and Diversité Adaptation et Développement des plantes, Institut de recherche pour le développement, Montpellier, Hérault, France Abstract Wax palms are an important element of the cloud forests in the tropical Andes. Despite heavy deforestation, the density of adults seems to be similar in deforested pastures as in forests. We aimed to infer the mechanisms responsible for this apparent resilience in pastures and we tested two hypotheses to explain it: 1) adult palms survived in pastures because they were spared from logging, and 2) adults occurred in pastures through the resilience of large juvenile rosettes, which survived through subterranean meristems and later developed into adults. For this purpose, we characterized the demographic structure of C. quindiuense in a total of 122 plots of 400 m2 in forests and pastures at two sites with contrasted land use histories in Colombia and Peru. Additionally, we implemented growth models that allowed us to estimate the age of individuals at four sites. These data were combined with information collected from local land managers in order to complete our knowledge on the land use history at each site. At two sites, the presence of old individuals up to 169 years and a wide age range evidenced that, at least, a portion of current adults in pastures were spared from logging at the time of deforestation. -
Full-Text PDF (Final Published Version)
Pritchard, M. E., de Silva, S. L., Michelfelder, G., Zandt, G., McNutt, S. R., Gottsmann, J., West, M. E., Blundy, J., Christensen, D. H., Finnegan, N. J., Minaya, E., Sparks, R. S. J., Sunagua, M., Unsworth, M. J., Alvizuri, C., Comeau, M. J., del Potro, R., Díaz, D., Diez, M., ... Ward, K. M. (2018). Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes. Geosphere, 14(3), 954-982. https://doi.org/10.1130/GES01578.1 Publisher's PDF, also known as Version of record License (if available): CC BY-NC Link to published version (if available): 10.1130/GES01578.1 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Geo Science World at https://doi.org/10.1130/GES01578.1 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Research Paper THEMED ISSUE: PLUTONS: Investigating the Relationship between Pluton Growth and Volcanism in the Central Andes GEOSPHERE Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes GEOSPHERE; v. 14, no. 3 M.E. Pritchard1,2, S.L. de Silva3, G. Michelfelder4, G. Zandt5, S.R. McNutt6, J. Gottsmann2, M.E. West7, J. Blundy2, D.H. -
Tesis Mildred Ollague
UNIVERSIDAD DE GUAYAQUIL FACULTAD DE CIENCIAS ADMINISTRATIVAS TRABAJO DE TITULACIÓN PRESENTADO COMO REQUISITO PARA OPTAR POR EL TÍTULO DE INGENIERÍA EN SISTEMAS ADMINISTRATIVOS COMPUTACIONALES TEMA: “PROTOTIPO DE APLICACIÒN WEB PARA EL CONTROL DE NUTRICIÓN Y CRECIMIENTO PARA NIÑOS DE 1 A 10 AÑOS” AUTORA: OLLAGUE MOSQUERA MILDRED LISSETTE TUTOR: ING. ROMAN BARREZUETA LUGIO DAVID GUAYAQUIL, SEPTIEMBRE 2017 REPOSITORIO NACIONAL EN CIENCIAS Y TECNOLOGÍA FICHA DE REGISTRO DE TESIS TÍTULO: PROTOTIPO DE APLICACIÓN WEB PARA EL CONTROL DE NUTRICIÓN Y CRECIMIENTO PARA NIÑOS DE 1 A 10 AÑOS AUTOR/ES: REVISORES: Mildred Lissette Ollague Mosquera Ing.Cecibel Alexandra León Arriaga INSTITUCIÓN: Universidad de FACULTAD: Facultad de Ciencias Guayaquil Administrativas CARRERA: Ingeniería en Sistemas Administrativos Computarizados FECHA DE PUBLICACIÓN: NO. DE PÁGS: ÁREA TEMÁTICA: Tecnología PALABRAS CLAVES: Prototipo Aplicación Web Nutrición Crecimiento RESUMEN El presente trabajo investigativo se centra en la creación de un aplicativo web para el control de nutrición y crecimiento de niños de 1 a 10 años, en la que se registra peso y talla de niños para despues evaluar su IMC, Perímetro Cefálico y Perímetro medio del brazo para lo cual se utiliza las tablas percentiles de la OMS con esto se emite un diagnóstico básico y se puede observar gráficamente como va el desarrollo del niño, también se puede enviar un correo con el historial del paciente al médico de su preferencia. N° DE REGISTRO (en base de N° DE CLASIFICACIÓN: datos): DIRECCIÓN URL (propuesta tecnológica en la web) ADJUNTO URL (propuesta tecnológica en la web): ADJUNTO PDF: SI NO CONTACTO CON AUTOR/ES: Teléfono: E-mail: Mildred Lissette Ollague Mosquera 0989194863 [email protected] CONTACTO EN LA Nombre: Ing. -
UNIVERSITY of CALIFORNIA Los Angeles Southern California
UNIVERSITY OF CALIFORNIA Los Angeles Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Geography by Katherine Colby Glover 2016 © Copyright by Katherine Colby Glover 2016 ABSTRACT OF THE DISSERTATION Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains by Katherine Colby Glover Doctor of Philosophy in Geography University of California, Los Angeles, 2016 Professor Glen Michael MacDonald, Chair Long sediment records from offshore and terrestrial basins in California show a history of vegetation and climatic change since the last interglacial (130,000 years BP). Vegetation sensitive to temperature and hydroclimatic change tended to be basin-specific, though the expansion of shrubs and herbs universally signalled arid conditions, and landscpe conversion to steppe. Multi-proxy analyses were conducted on two cores from the Big Bear Valley in the San Bernardino Mountains to reconstruct a 125,000-year history for alpine southern California, at the transition between mediterranean alpine forest and Mojave desert. Age control was based upon radiocarbon and luminescence dating. Loss-on-ignition, magnetic susceptibility, grain size, x-ray fluorescence, pollen, biogenic silica, and charcoal analyses showed that the paleoclimate of the San Bernardino Mountains was highly subject to globally pervasive forcing mechanisms that register in northern hemispheric oceans. Primary productivity in Baldwin Lake during most of its ii history showed a strong correlation to historic fluctuations in local summer solar radiation values.