Eastern Cordillera Real Oriental Paramos and Montane Forests
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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. -
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. -
(1987): "Tectonomagmatic Evolution of Cenozoic Extension in the North American Cordillera"
Downloaded from http://sp.lyellcollection.org/ by Frances J Cooper on January 21, 2013 Geological Society, London, Special Publications Tectonomagmatic evolution of Cenozoic extension in the North American Cordillera Brian P. Wernicke, Philip C. England, Leslie J. Sonder and Robert L. Christiansen Geological Society, London, Special Publications 1987, v.28; p203-221. doi: 10.1144/GSL.SP.1987.028.01.15 Email alerting click here to receive free e-mail alerts when service new articles cite this article Permission click here to seek permission to re-use all or request part of this article Subscribe click here to subscribe to Geological Society, London, Special Publications or the Lyell Collection Notes © The Geological Society of London 2013 Downloaded from http://sp.lyellcollection.org/ by Frances J Cooper on January 21, 2013 Tectonomagmatic evolution of Cenozoic extension in the North American Cordillera B.P. Wernicke, R.L. Christiansen, P.C. England & L.J. Sonder SUMMARY: The spatial and temporal distributions of Cenozoic extension and magmatism in the Cordillera suggest that the onset of major crustal extension at a particular latitude was confined to a relatively narrow belt (< 100 km, pre-extension) and followed the onset of intermediate and silicic magmatism by no more than a few million years. Extension began in early Eocene time in southern British Columbia, northern Washington, Idaho and Montana. Farther S, extension began at about the Eocene- Oligocene boundary in the Great Basin and slightly later in the Mojave-Sonora Desert region. The intervening area, at the latitude of Las Vegas, remained quiescent until mid- Miocene time. Compositional and isotopic characteristics of most pre-Miocene magmas are consistent with their containing major components of melted continental crust. -
Diversity and Population Genetic Structure of the Wax Palm Ceroxylon
bioRxiv preprint doi: https://doi.org/10.1101/443960; this version posted October 15, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. 1 Diversity and population genetic structure of the wax palm 2 Ceroxylon quindiuense in the Colombian Coffee Region 3 Natalia González-Rivillas1-2, Adriana Bohórquez3, Janeth Patricia Gutierrez3, Víctor Hugo García- 4 Merchán1-2 5 6 1Grupo de Investigación en Evolución, Ecología y Conservación (EECO), Programa de Biología, 7 Universidad del Quindío, Carrera 15 Calle 12 Norte, Armenia, Quindío, Colombia. 8 2 Grupo de Investigación y Asesoría en Estadística, Universidad del Quindío. 9 3 International Center for Tropical Agriculture (CIAT), Km 17, recta Cali-Palmira, Colombia. 10 11 [email protected] (NGR), [email protected] (AB), [email protected] (JPG) & 12 [email protected] (VHGM). 13 14 The authors mentioned contributed equally to this work. 15 16 Abstract 17 The wax palm from Quindío (Ceroxylon quindiuense) is an icon of the cultural identity of the coffee growing 18 eco-region and of all Colombia. Processes of urbanization, expansion of the agricultural and livestock area, among 19 others, have increased its level of threat. Protecting this palm from extinction is important at an ecological level, given 20 its function as a key species in Andean ecosystems. This work evaluated the diversity and population genetic structure 21 of the wax palm from Quindío in five populations of the Colombian coffee region eco-region (Andean zone) by using 22 ten microsatellite molecular markers. -
Brief Overview of North American Cordilleran Geology by Cin-Ty Lee Topography Map of North America
Brief overview of North American Cordilleran geology by Cin‐Ty Lee Note: make sure to take notes as I will talk or sketch on the board many things that are not presented explicitly in these slides Topography map of North America Topography map How does the NthNorth AiAmerican Cor dillera fit itinto a glbllobal contt?text? Dickinson 2004 P‐wave tomography: Seismic structure beneath western USA Burdick et al. 2008 Crustal provinces of North America (Laurentia) ‐Proterozoic and Archean terranes were already assembled by 1.6 Ga Hoffman, 1988 Crustal provinces in southwestern USA Hoffman, 1988 Bennett and DePaolo, 1987 Some examples of tectonic margins for your reference Dickinson and Snyder, 1978 1.1 Ga = Rodinia Super‐continent (Grenvillian age) Neo‐Proterozoic = Rodinia breaks up “western” margin of Laurentia represents a passive margin due to opening of the Panthalassan ocean 700‐400 Ma Western margin of Laurentia represents a passive margin Dickinson and Snyder, 1978 400‐250 Ma Passive margin is interrupted in Devonian times by the accretion of island arcs Antler and Sonoma orogenies Accretion of allochthonous terranes to the western margin of the NhNorth AiAmerican craton Antler/Sonoma orogenies result in the accretion of Paleozoic island arc terranes to western North America Permian Formation of Pangea “”“western” margin of NhNorth AiAmerica now didominate d by subduct ion zone 250‐50 Ma Subduction results in continued accretion of fringing island arcs and the generation of continental magmatic arcs Sierra Nevada batholith Sevier and -
OPPOSITE THRUST-VERGENCIES in the PRECORDILLERA and WESTERN CORDILLERA in NORTHERN CHILE and Structurally LINKED CENOZOIC PALEOENVIRONMENTAL EVOLUTION
Fourth /SAG. Goettingen (Germany), 04 - 06//0//999 155 OPPOSITE THRUST-VERGENCIES IN THE PRECORDILLERA AND WESTERN CORDILLERA IN NORTHERN CHILE AND STRUCTURALLy LINKED CENOZOIC PALEOENVIRONMENTAL EVOLUTION Reynaldo CHARRIER(I-7), Gérard HERAIL(2-7), John FLYNN(3), Rodrigo RIQUELME(I-7), Marcelo GARCIA(4-7), Darin CROFf(5) and André WYSS(6) (1) Departamento de Geologfa, Universidad de Chile; [email protected]. (2) IRD, 209-213, Rue La Fayette, 75010 Paris,[email protected]. (3) The Field Museum of Natural History, Chicago, USA. [email protected]. (4) SERNAGEOMIN. Av. Sta. Maria 0104, Providencia, Santiago, Chile. [email protected]. (5) The Field Museum of Natural History, Chicago, and University of Chicago, USA. (6) Department of Geological Sciences, University of California Santa Barbara, USA [email protected]. (7) Convenio IRD-Departamento de Geologïa, Universidad de Chi le. KEY WORDS: Altiplano, Chile, syntectonic sedimentation, Cenozoic paleoenvironment. INTRODUCTION Morphologie units in the northern Chilean Andes parailei one another and the offshore trench. These units are, from west to east: Coastal Cordillera, Central Depression, Precordillera, Western Cordillera and Altiplano (Fig. i). The development of the west part of the Western Cordillera (Chapiquifia-Belén Ridge), in the Chilean Altiplano, was controlled by two diverging, trench-parallel systems of thrusts and folds, one located along the Precordil1era and the other along the eastern side of the Western Cordillera. Although total shortening associated with these systems is only 12 to 14 km, their activity determined the development of fluvial and lacustrine basins which recorded the synorogenic paleoenvironmental evolution of this region. We describe here facies, geometry and chronology of the deposits associated with both systems and provide an explanation for the differing depositional environments developed on the Precordillera and the Western Cordillera. -
Outlook on Climate Change Adaptation in the Tropical Andes Mountains
MOUNTAIN ADAPTATION OUTLOOK SERIES Outlook on climate change adaptation in the Tropical Andes mountains 1 Southern Bogota, Colombia photo: cover Front DISCLAIMER The development of this publication has been supported by the United Nations Environment Programme (UNEP) in the context of its inter-regional project “Climate change action in developing countries with fragile mountainous ecosystems from a sub-regional perspective”, which is financially co-supported by the Government Production Team of Austria (Austrian Federal Ministry of Agriculture, Forestry, Tina Schoolmeester, GRID-Arendal Environment and Water Management). Miguel Saravia, CONDESAN Magnus Andresen, GRID-Arendal Julio Postigo, CONDESAN, Universidad del Pacífico Alejandra Valverde, CONDESAN, Pontificia Universidad Católica del Perú Matthias Jurek, GRID-Arendal Björn Alfthan, GRID-Arendal Silvia Giada, UNEP This synthesis publication builds on the main findings and results available on projects and activities that have been conducted. Contributors It is based on available information, such as respective national Angela Soriano, CONDESAN communications by countries to the United Nations Framework Bert de Bievre, CONDESAN Convention on Climate Change (UNFCCC) and peer-reviewed Boris Orlowsky, University of Zurich, Switzerland literature. It is based on review of existing literature and not on new Clever Mafuta, GRID-Arendal scientific results generated through the project. Dirk Hoffmann, Instituto Boliviano de la Montana - BMI Edith Fernandez-Baca, UNDP The contents of this publication do not necessarily reflect the Eva Costas, Ministry of Environment, Ecuador views or policies of UNEP, contributory organizations or any Gabriela Maldonado, CONDESAN governmental authority or institution with which its authors or Harald Egerer, UNEP contributors are affiliated, nor do they imply any endorsement. -
Diversidad De Plantas Y Vegetación Del Páramo Andino
Plant diversity and vegetation of the Andean Páramo Diversidad de plantas y vegetación del Páramo Andino By Gwendolyn Peyre A thesis submitted for the degree of Doctor from the University of Barcelona and Aarhus University University of Barcelona, Faculty of Biology, PhD Program Biodiversity Aarhus University, Institute of Bioscience, PhD Program Bioscience Supervisors: Dr. Xavier Font, Dr. Henrik Balslev Tutor: Dr. Xavier Font March, 2015 Aux peuples andins Summary The páramo is a high mountain ecosystem that includes all natural habitats located between the montane treeline and the permanent snowline in the humid northern Andes. Given its recent origin and continental insularity among tropical lowlands, the páramo evolved as a biodiversity hotspot, with a vascular flora of more than 3400 species and high endemism. Moreover, the páramo provides many ecosystem services for human populations, essentially water supply and carbon storage. Anthropogenic activities, mostly agriculture and burning- grazing practices, as well as climate change are major threats for the páramo’s integrity. Consequently, further scientific research and conservation strategies must be oriented towards this unique region. Botanical and ecological knowledge on the páramo is extensive but geographically heterogeneous. Moreover, most research studies and management strategies are carried out at local to national scale and given the vast extension of the páramo, regional studies are also needed. The principal limitation for regional páramo studies is the lack of a substantial source of good quality botanical data covering the entire region and freely accessible. To meet the needs for a regional data source, we created VegPáramo, a floristic and vegetation database containing 3000 vegetation plots sampled with the phytosociological method throughout the páramo region and proceeding from the existing literature and our fieldwork (Chapter 1). -
Plate Tectonic Setting of the Andean Cordillera
183 by Victor A. Ramos Plate tectonic setting of the Andean Cordillera Laboratorio de Tectónica Andina, Universidad de Buenos Aires, Argentina. E-mail: [email protected] The Andes are a natural laboratory for the study of the acterize the different segments are widely variable. The present interaction between subduction of the oceanic plate and overview will focus on the major geological differences among these segments, based on today’s plate-tectonic knowledge of this moun- active geological processes. Inter- and intraplate seis- tain chain. micity, volcanic activity, thick- and thin-skinned fold and thrust belts, and foreland basin subsidence, in con- junction with space geodetic observations, contribute to Major geological provinces characterize the present plate tectonic setting of discrete The Andes north of the Golfo de Guayaquil are unique, as estab- segments of the Andes. The inherited geological history, lished by Gansser (1973). The Northern Andes record an important as well as the present tectonic setting, is responsible for accretion of oceanic crust during Jurassic, late Cretaceous, and Pale- the unique geology of the Northern, Central, and South- ogene times. As a result, the Western Cordillera of Colombia and Ecuador is mainly constituted of an oceanic basement that during ern Andes. The Northern Andes are the result of Meso- accretion was related to ophiolite obduction, important penetrative zoic and Cenozoic collisions of oceanic terranes, prior deformation and metamorphism, in cases up to blue schist facies. to the present Andean-type setting. The Central Andes Further north, the emplacement of the Caribbean nappes was related to the collision of an island arc system, the Bonaire block, during have a long history of subduction and volcanic arc Paleogene times (Bosch and Rodríguez, 1992, Kellogg and Bonini, activity, while the Southern Andes record the closing of 1982). -
The Cordillera of the Andes Boundary Case (Argentina, Chile)
REPORTS OF INTERNATIONAL ARBITRAL AWARDS RECUEIL DES SENTENCES ARBITRALES The Cordillera of the Andes Boundary Case (Argentina, Chile) 20 November 1902 VOLUME IX pp. 37-49 NATIONS UNIES - UNITED NATIONS Copyright (c) 2006 37 AWARD BY HIS MAJESTY KING EDWARD VII IN THE ARGENTINE- CHI LE BOUNDARY CASE, 20 NOVEMBER 1902 x WHEREAS, by an Agreement dated the 17th day of April 1896, the Argentine Republic and the Republic of Chile, by Their respective Representatives, determined: THAT should differences arise between their experts as to the boundary-line to be traced between the two States in conformity with the Treaty of 1881 and the Protocol of 1893, and in case such differences could not be amicably settled by accord between the two Governments, they should be submitted to the decision of the Government of Her Britannic Majesty; AND WHEREAS such differences did arise and were submitted to the Govern- ment of Her late Majesty Queen Victoria; AND WHEREAS the Tribunal appointed to examine and consider the differences which had so arisen, has — after the ground has been examined by a Com- mission designated for that purpose — now reported to Us, and submitted to Us, after mature deliberation, their opinions and recommendations for Our consideration ; Now, WE, EDWARD, by the grace of God, King of the United Kingdom of Great Britain and Ireland and of the British Dominions beyond the Seas King, Defender of the Faith, Emperor of India, etc., etc., have arrived at the following decisions upon the questions in dispute, which have been referred to Our arbitration, viz. : 1. -
Present Knowledge of the Magmatic Evolution of the Eastern Cordillera of Peru
Earth-Science Reviews, 18 (1982) 253-283 253 Elsevier Scientific Publishing Company, Amsterdam-Printed in The Netherlands Present Knowledge of the Magmatic Evolution of the Eastern Cordillera of Peru G. Carlier', G. Grandin', G. Laubacher', R. and F. M6gard2 ' ORSTOM, Mission Peru, Apartado 270, Lima 18 (Peru) and 2'4 rue Bayard75008 Paris (France) ' Institut Francais #Etudes Andines, Apartado 278, Lima I8 (Peru) Pontificia Universidad Catdica del Perú, Avda S. Boliuar, Lima 27 (Peru) ABSTRACT Carlier, G., Grandin, G., Laubacher, G., Marócco, R. and Mégard, F., 1982. Present knowledge of the magmatic evolution of the Eastern Cordillera of Peru. Earth-Sci. Rev., 18: 253-283. The studies which have been carried out in the Eastern Cordillera of Peru over the past 20 years prove the existence of at least three orogenic cycles: the Late Precambrian, the Hercynian and the Andean, each one accompanied by a more or less abundant magmatism. (1) The Precambrian. Leaving aside the prasinites, possibly derived from synsedimentary , volcanites, Precambrian magmatism (in the Huanuco region) consists of: a meta-igneous ultramafic to mafic association (serpentinites, meta-gabbros, meta-diorites); syntectonic meta-tonalites; and post-tectonic dioritic and granitic intrusive bodies. (2) The Hercynian (550 to 220 my.). From the Cambrian to the Upper Devonian the existence of a synsedimentary magmatism is known. Syntectonic granites were emplaced during the Eohercynian phase, but the major part of magmatism is of a Late Permian to Early Trias age, and is characterized by the intrusion of granitoids and by volcanism of calc-al- kaline tendency. It appears that the nepheline syenite of Macusani may belong to a terminal episode of this magmatic period.