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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. -
To Late-Holocene Explosive Rhyolitic Eruptions from Chaitén Volcano, Chile Andean Geology, Vol
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Watt, Sebastian F.L.; Pyle, David M.; Mather, Tamsin A. Evidence of mid- to late-Holocene explosive rhyolitic eruptions from Chaitén Volcano, Chile Andean Geology, vol. 40, núm. 2, mayo, 2013, pp. 216-226 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173927491002 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 40 (2): 216-226. May, 2013 Andean Geology doi: 10.5027/andgeoV40n2-a02 formerly Revista Geológica de Chile www.andeangeology.cl Evidence of mid- to late-Holocene explosive rhyolitic eruptions from Chaitén Volcano, Chile Sebastian F.L. Watt1, 2, David M. Pyle1, Tamsin A. Mather1 1 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, U.K. [email protected]; [email protected]; [email protected] 2 National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, U.K. ABSTRACT. The 2008 eruption of Chaitén Volcano was widely cited as the first activity at the volcano for over 9000 years. However, we have identified evidence from proximal pyroclastic deposits for three additional explosive eruptions of Chaitén within the past 5000 years. Chaitén has therefore produced at least five explosive eruptions in the Holocene, making it among the most active volcanoes, in terms of explosive output, in the southern part of the Andean Southern Volcanic Zone. -
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. -
SURNAMES in CHILE a Study of the Population of Chile Through
Page 1 of 31 American Journal of Physical Anthropology 1 2 3 SURNAMES IN CHILE 4 5 A study of the population of Chile through isonymy 6 I. Barrai, A. Rodriguez-Larralde 2, J. Dipierri 1, E.Alfaro 1, N. Acevedo 3, 7 8 E. Mamolini, M. Sandri, A.Carrieri and C. Scapoli. 9 10 Dipartimento di Biologia ed Evoluzione, Università di Ferrara, 44121- Ferrara, Italy 11 1Instituto de Biología de la Altura, Universidad Nacional de Jujuy, 4600 – San Salvador De Jujuy, 12 13 Argentina. 14 2 15 Centro de Medicina Experimental, Laboratorio de Genetica Humana, IVIC, 1020A -Caracas, 16 Venezuela. 17 18 3Museo Nacional de Ciencias Naturales, Santiago, Chile 19 20 21 Running title: Surnames in Chile 22 23 24 25 26 Correspondence to: 27 Chiara Scapoli 28 Department of Biology and Evolution 29 30 University of Ferrara, 31 Via L. Borsari 46, - I-44121 Ferrara, Italy. 32 Telephone: +39 0532 455744; FAX: : +39 0532 249761 33 Email: [email protected] 34 35 36 Number of text pages: 15 37 Literature pages: 4 38 39 Number of Tables : 2 40 41 Number of Figures: 7 42 43 44 KEYWORDS : Chile, Population Structure, Isonymy, Inbreeding, Isolation by distance 45 46 47 ACKNOWLEDGMENTS: The authors are grateful to the Director of the Servicio Electoral de la 48 49 Republica de Chile Sr. Juan Ignacio Garcia Rodríguez, who made the data available, and to Sr. 50 51 Dr.Ginés Mario Gonzalez Garcia, Embajador de la Republica Argentina en Chile. The work was 52 supported by grants of the Italian Ministry of Universities and Research (MIUR) to Chiara Scapoli. -
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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. -
Relationship Between Static Stress Change and Volcanism. How and If Tectonic Earthquake Could Influence Volcanic Activity
Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Dissertations, Master's Theses and Master's Reports - Open Reports 2014 RELATIONSHIP BETWEEN STATIC STRESS CHANGE AND VOLCANISM. HOW AND IF TECTONIC EARTHQUAKE COULD INFLUENCE VOLCANIC ACTIVITY. EXAMPLE OF EL REVENTADOR VOLCANO, ECUADOR Daniele Alami Michigan Technological University Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geology Commons, and the Volcanology Commons Copyright 2014 Daniele Alami Recommended Citation Alami, Daniele, "RELATIONSHIP BETWEEN STATIC STRESS CHANGE AND VOLCANISM. HOW AND IF TECTONIC EARTHQUAKE COULD INFLUENCE VOLCANIC ACTIVITY. EXAMPLE OF EL REVENTADOR VOLCANO, ECUADOR", Master's report, Michigan Technological University, 2014. https://doi.org/10.37099/mtu.dc.etds/770 Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geology Commons, and the Volcanology Commons RELATIONSHIP BETWEEN STATIC STRESS CHANGE AND VOLCANISM. HOW AND IF TECTONIC EARTHQUAKE COULD INFLUENCE VOLCANIC ACTIVITY. EXAMPLE OF EL REVENTADOR VOLCANO, ECUADOR. By Daniele Alami A REPORT Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE In Geology MICHIGAN TECHNOLOGICAL UNIVERSITY 2013 © 2013 Daniele Alami This report has been approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE in Geology Department of Geological & Mining Engineering & Sciences Report Co-Advisor: Gregory P.Waite Report Co-Advisor: Alessandro Tibaldi Committee Member: Simon Carn Department Chair: John Gierke 1 2 L'infinito non esiste, è solo un numero grande, e l'unico vero cuore è al centro della Terra. Vai davanti a un vulcano e poi dimmi, come ti senti? (Filippo Timi) 3 Università degli studi di Milano-Bicocca Facoltà di Scienze Matematiche, Fisiche e Naturali Dipartimento di Scienze e Tecnologie Geologiche Relationship between static stress changes and volcanism. -
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. -
Redalyc.Geochemistry, U-Pb SHRIMP Zircon Dating and Hf Isotopes of The
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Poma, Stella; Zappettini, Eduardo O.; Quenardelle, Sonia; Santos, João O.; Koukharsky, Magdalena; Belousova, Elena; McNaughton, Neil Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: petrogenesis and geodynamic implications Andean Geology, vol. 41, núm. 2, mayo, 2014, pp. 267-292 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173931252001 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 41 (2): 267-292. May, 2014 Andean Geology doi: 10.5027/andgeoV41n2-a01 formerly Revista Geológica de Chile www.andeangeology.cl Geochemistry, U-Pb SHRIMP zircon dating and Hf isotopes of the Gondwanan magmatism in NW Argentina: petrogenesis and geodynamic implications Stella Poma1, Eduardo O. Zappettini 2, Sonia Quenardelle 1, João O. Santos 3, † Magdalena Koukharsky 1, Elena Belousova 4, Neil McNaughton 3 1 Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (IGEBA-CONICET), Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Departamento de Ciencias Geológicas, Pabellón II-Ciudad Universitaria, Intendente Güiraldes 2160, C1428 EGA, Argentina. [email protected]; [email protected] 2 Servicio Geológico Minero Argentino (SEGEMAR), Avda. General Paz 5445, edificio 25, San Martín B1650WAB, Argentina. [email protected] 3 University of Western Australia, 35 Stirling Highway, Crawley WA 6009, Australia. -
Archaeological, Radiological, and Biological Evidence Offer Insight Into Inca Child Sacrifice
Archaeological, radiological, and biological evidence offer insight into Inca child sacrifice Andrew S. Wilsona,1, Emma L. Browna, Chiara Villab, Niels Lynnerupb, Andrew Healeyc, Maria Constanza Cerutid, Johan Reinharde, Carlos H. Previglianod,2, Facundo Arias Araozd, Josefina Gonzalez Diezd, and Timothy Taylora,3 aDepartment of Archaeological Sciences, and cCentre for Chemical and Structural Analysis, University of Bradford, Bradford BD7 1DP, United Kingdom; bLaboratory of Biological Anthropology, Department of Forensic Medicine, Faculty of Health Sciences, University of Copenhagen, Blegdamsvej 3, DK-2200 Copenhagen N, Denmark; dInstitute of High Mountain Research, Catholic University of Salta, Salta A4400FYP, Argentina; and eNational Geographic Society, Washington, DC 20036 Edited by Charles Stanish, University of California, Los Angeles, CA, and approved June 18, 2013 (received for review March 21, 2013) Examination of three frozen bodies, a 13-y-old girl and a girl and defining, element of a capacocha ritual. We also recognize that boy aged 4 to 5 y, separately entombed near the Andean summit the capacocha rite analyzed here was embedded within a multi- of Volcán Llullaillaco, Argentina, sheds new light on human sac- dimensional imperial ideology. rifice as a central part of the Imperial Inca capacocha rite, de- The frozen remains of the ∼13-y-old “Llullaillaco Maiden,” the scribed by chroniclers writing after the Spanish conquest. The 4- to 5-y-old “Llullaillaco Boy,” and the 4- to 5-y-old “Lightning high-resolution diachronic data presented here, obtained directly Girl” provide unusual and valuable analytical opportunities. Their from scalp hair, implies escalating coca and alcohol ingestion in the posture and placement within the shrine, surrounded by elite lead-up to death. -
Paleoecology of Late Quaternary Deposits in Chiloe Continental, Chile
Revista Chilena de Historia Natural 65:235-245,1992 Paleoecology of Late Quaternary Deposits in Chiloe Continental, Chile Paleoecología de los dep6sitos del Cuaternario tardio en Chiloe Continental, Chile 1 2 3 CALVIN J. HEUSSER , LINDA E. HEUSSER and ARTURO HAUSER 1 Clinton Woods, Tuxedo, New York 10987, USA. 2 Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964, USA. 3 Servicio Nacional de Geologia y Mineria, Casilla 10465, Santiago, Chile. ABSTRACT Two stratigraphic records of the late Quaternary vegetation and paleoenvironmental setting of Chiloe Continental, heretofore unstudied, are from (1) a 7.2 m deposit of mire peat at Cuesta Moraga (43025's), dated at 12,310 yr B.P. and interrupted by multiple tephra layers, resting on glacial drift, and (2) a 3-m road cut near Chaiten (42°54'S), 75 km north of Cuesta Moraga, containing a peat bed with wood, dated 11,850 yr B.P., underlying a thick tephra layer and overlying drift. Records are of fossil pollen, spores, and matrix macroremains, loss on ignition, lithology, and ra- diocarbon chronology. There is throughout in the data no indication of fire in predominantly Nothofagus forest com- munities, which during the late-glacial at Chaiten contained, among other tree species, Drimys, Pseudopanax, and Po- docarpus. At Cuesta Moraga, where the forest was relatively open and continued to be open during the Holocene, late- glacial ground cover of Empetrum, Gunnera, and polypodiaceous ferns was supplanted on the mire largely by mi- nerotrophic Cyperaceae until about 8,000 yr B.P.; later, especially after 5,000 yr B.P., ombrotrophic cushion plants, notably Astelia, Donatia, and Tetroncium, with Dacrydium, proliferated on the surface of the mire. -
To Late-Holocene Explosive Rhyolitic Eruptions from Chaitén Volcano, Chile
Andean Geology 40 (2): 216-226. May, 2013 Andean Geology doi: 10.5027/andgeoV40n2-a02 formerly Revista Geológica de Chile www.andeangeology.cl Evidence of mid- to late-Holocene explosive rhyolitic eruptions from Chaitén Volcano, Chile Sebastian F.L. Watt1, 2, David M. Pyle1, Tamsin A. Mather1 1 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, U.K. [email protected]; [email protected]; [email protected] 2 National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, U.K. ABSTRACT. The 2008 eruption of Chaitén Volcano was widely cited as the first activity at the volcano for over 9000 years. However, we have identified evidence from proximal pyroclastic deposits for three additional explosive eruptions of Chaitén within the past 5000 years. Chaitén has therefore produced at least five explosive eruptions in the Holocene, making it among the most active volcanoes, in terms of explosive output, in the southern part of the Andean Southern Volcanic Zone. All of the five identified Holocene explosive eruptions produced homogeneous high-silica rhyolite, with near identical compositions. Based on our pyroclastic sequence, we suggest that the largest-volume Holocene eruption of Chaitén occurred at ~4.95 ka, and we correlate this with the Mic2 deposit, which was previously thought to originate from the nearby Michinmahuida Volcano. Keywords: Chaitén Volcano, Andean southern volcanic zone, Holocene tephra stratigraphy, Rhyolite, Explosive volcanism. RESUMEN. Evidencia de erupciones riolíticas del Holoceno medio a tardío del volcán Chaitén, Chile. La erupción del volcán Chaitén en el año 2008 ha sido mencionada ampliamente como la primera actividad de este en los últimos 9 mil años. -
The South American Indian As a Pioneer Alpinist
TI-lE SOUTH AMERICAN INDIAN AS A PIONEER ALPINIST 81 THE SOUTH AMERICAN INDIAN AS A PIONEER ALPINIST BY EVELIO ECHEVARRfA C. ECENTL Y it has become kno\vn that a number of very high Andean mountain tops had not only been ascended but also permanently occupied by the Indians, possibly as much as three centuries before de Saussure's ascent of Mont Blanc. They climbed peaks of up to 22,ooo ft., they constructed shelters on or near their tops, and they used the high places as watch-towers or as sacrificial shrines. Some authorities believe that this activity took place as early as the late four teenth century, though we cannot prove that some of it did not take place long after, possibly as late as the nineteenth century. These Indian accomplishments have been left unmentioned in practi cally all mountaineering history books. In this article, which may be the first to attempt a comprehensive survey,1 my purpose is to review briefly the location and the nature of each discovery. The area in which these Indian mountain ascents took place is what in physical geography is known as the Atacama desert (although this name is nowadays used in political and cultural geography for a much more restricted area). It is a treeless, sandy and volcanic waste-land seldom visited by mountaineers. It stretches from the neighbourhood of Arequipa, in Peru, as far south as Elqui in Chile; to the east it reaches the Andean slopes that face the jungles of Argentina and Bolivia, and to the west, the Pacific Ocean.