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Artykuły w czasopismach na temat "Amazonian Andes"
Bush, M. B., M. R. Silman, C. McMichael i S. Saatchi. "Fire, climate change and biodiversity in Amazonia: a Late-Holocene perspective". Philosophical Transactions of the Royal Society B: Biological Sciences 363, nr 1498 (11.02.2008): 1795–802. http://dx.doi.org/10.1098/rstb.2007.0014.
Pełny tekst źródłaNores, Manuel. "The Western Amazonian Boundary for Avifauna Determined by Species Distribution Patterns and Geographical and Ecological Features". International Journal of Ecology 2011 (2011): 1–7. http://dx.doi.org/10.1155/2011/958684.
Pełny tekst źródłaBorda, Víctor, Isabela Alvim, Marla Mendes, Carolina Silva-Carvalho, Giordano B. Soares-Souza, Thiago P. Leal, Vinicius Furlan i in. "The genetic structure and adaptation of Andean highlanders and Amazonians are influenced by the interplay between geography and culture". Proceedings of the National Academy of Sciences 117, nr 51 (4.12.2020): 32557–65. http://dx.doi.org/10.1073/pnas.2013773117.
Pełny tekst źródłaSTURARO, MARCELO JOSÉ, i TERESA C. S. AVILA-PIRES. "Taxonomic revision of the geckos of the Gonatodes concinnatus complex (Squamata: Sphaerodactylidae), with description of two new species". Zootaxa 2869, nr 1 (6.05.2011): 1. http://dx.doi.org/10.11646/zootaxa.2869.1.1.
Pełny tekst źródłaLombardo, Umberto. "Alluvial plain dynamics in the southern Amazonian foreland basin". Earth System Dynamics 7, nr 2 (10.05.2016): 453–67. http://dx.doi.org/10.5194/esd-7-453-2016.
Pełny tekst źródłaLombardo, U. "Alluvial plain dynamics in the southern Amazonian foreland basin". Earth System Dynamics Discussions 6, nr 2 (20.10.2015): 2063–100. http://dx.doi.org/10.5194/esdd-6-2063-2015.
Pełny tekst źródłaCanal, Dubán, Nils Köster, Marcela Celis, Thomas B. Croat, Thomas Borsch i Katy E. Jones. "Out of Amazonia and Back Again: Historical Biogeography of the Species-Rich Neotropical Genus Philodendron (Araceae)". Annals of the Missouri Botanical Garden 104, nr 1 (7.03.2019): 49–68. http://dx.doi.org/10.3417/2018266.
Pełny tekst źródłaIRMLER, ULRICH. "New species and records of the genus Lispinus with a key to the species from Peru (Coleoptera: Staphylinidae: Osoriinae)". Zootaxa 2263, nr 1 (13.10.2009): 42–58. http://dx.doi.org/10.11646/zootaxa.2263.1.4.
Pełny tekst źródłaGovin, A., C. M. Chiessi, M. Zabel, A. O. Sawakuchi, D. Heslop, T. Hörner, Y. Zhang i S. Mulitza. "Terrigenous input off northern South America driven by changes in Amazonian climate and the North Brazil Current retroflection during the last 250 ka". Climate of the Past 10, nr 2 (28.04.2014): 843–62. http://dx.doi.org/10.5194/cp-10-843-2014.
Pełny tekst źródłaReyes-Puig, Juan Pablo, Miguel Urgilés-Merchán, Daniela Franco-Mena, Juan M. Guayasamin, Diego Batallas i Carolina Reyes-Puig. "Two new species of terrestrial frogs of the Pristimantis gladiator complex (Anura, Strabomantidae) from the Ecuadorian Andes, with insights on their biogeography and skull morphology". ZooKeys 1180 (26.09.2023): 257–93. http://dx.doi.org/10.3897/zookeys.1180.107333.
Pełny tekst źródłaRozprawy doktorskie na temat "Amazonian Andes"
Andriolli, Custodio Michele. "Evolution du système Andes-Amazonie-Océan Atlantique au cours du Cénozoïque". Electronic Thesis or Diss., Toulouse 3, 2023. http://www.theses.fr/2023TOU30262.
Pełny tekst źródłaThe Andes-Amazon-South American Equatorial Margin (AAMESA) source-sedimentation system (S2S), which extends for around 3,200 km and is located north of the South American platform, is one of the largest S2S systems in the world. Currently, the AAMESA system is controlled by the Andes from a sedimentary point of view, as 95% of the average annual flow of suspended sediment supplied by the Amazon to the Atlantic Ocean comes from Andean tributaries. Despite scientific advances detailing the influences of Andean construction and erosion processes on the origin, evolution and sedimentary record of the S2S AAMESA system from the end of the Cretaceous to the beginning of the Paleocene in Western Amazonia and the establishment of the transcontinental Amazon River at the end of the Miocene (Neogene) in Eastern Amazonia, the geological history and, in particular, the pre-Neogene and Pliocene configurations of the AAMESA system have yet to be clarified. The main objective of this thesis is to propose a paleogeographic reconstruction of the Andes-Amazon-Equatorial Margin system during the Cenozoic, based on new stratigraphic, sedimentological and sedimentary provenance data obtained from one of the basins that make up the foreland basin system of the Amazonian backarc (Huallaga Basin, northern Peru) and the main basin of the Amazonian equatorial margin (Foz do Amazonas Basin). We show that, from the Paleocene to the Lower Eocene (Danian - Ypresian) (66 - 43.5 Ma), a depositional hiatus developed in the basins of the Amazonian backarc linked to an episode of tectonic quiescence in the Andes. This tectonic quiescence is contemporaneous with the formation of the "South American" laterite surfaces in Central Amazonia and the low sedimentation rates in the Foz do Amazonas Basin. The resumption of uplift and erosion of the Peruvian Andes in the middle to late Eocene (Lutetian - Bartonian) (43.5 - 37.6 Ma) was recorded in the sedimentation of the foreland basin of the Amazonian backarc by the presence of debris from the magmatic arcs of the Cordillera Occidental and by a Bartonian transgression marked by the presence of tidal deposits in continental lacustrine deposits. The beginning of the rise of the Eastern Cordillera is recorded in the sediments of the foreland basin of the Amazonian backarc (Huallaga Basin) 30 Ma ago, in the Rupelian. From the Rupelian to the Middle Miocene, the Eastern Cordillera continued to rise, creating a topographic relief capable of acting as an orographic barrier to atmospheric flows from the Atlantic Ocean. This continuous elevation may have led to the presence of wetter climates in western Amazonia, which could have favored the formation of laterite surfaces in central Amazonia between the Oligocene and the Lower Miocene, in relation to the intense phase of alteration that occurred between 30 and 18 Ma. Our provenance data record a new period of exhumation of the Cordillera Oriental from the Upper Miocene to the present day. This period of rejuvenation of the relief of the Eastern Cordillera is linked to a period of propagation of the Amazonian orogenic prism towards the craton. This led to a reorganization of the Amazon drainage network and is probably one of the driving forces behind the transcontinentalization of Amazonia in the Middle-Upper Miocene. Finally, the AAMESA system did not exist in "source-to-sink" (S2S) terms until the late Miocene, with the transcontinental establishment of the Amazon River. The preceding period was marked by the dominance of two different systems, represented by the Eastern Amazon craton and the NE region of South America (Borborema province, São Luís craton, Gurupi belt)
Calderón, Ysabel. "Architecture structurale, bilans sédimentaires et potentiel hydrocarburifère d'une zone de transition "wedgetop-foredeep" de rétro-bassin d'avant-pays : exemple des bassins Marañon et Huallaga du Nord-Pérou". Thesis, Toulouse 3, 2018. http://www.theses.fr/2018TOU30038/document.
Pełny tekst źródłaThis thesis, through its multidisciplinary approach and the interpretation of a large amount of industrial data, brings new elements in the understanding of foreland basin systems, especially in the Andino-Amazonian field of northern Peru. It proposes a new stratigraphic and structural model of this region, reconstructs and quantifies the history of the deformation and sedimentation that constitutes the key data to model the petroleum systems and to reduce the risks in exploration. The results show that the structural architecture of the Marañon Foreland Basin, the largest of the central Andes, evolves laterally from a wedgetop zone in the SE to a foredeep zone in the NW. In the SE, it forms a thrust wedge partly eroded, connected to the wedgetop basins of Huallaga and Moyabamba. This set constitutes a single foreland basin system, deformed by the interference of an east-verging thin-skinned tectonics and a largely west-verging tectonics. The total horizontal shortening varies between 70 and 76 km. The western vergence of this thick-skinned tectonics is controlled by the inheritance of the Gondwanide orogeny (Middle Permian). We show that it is at the origin of the important crustal and destructive earthquakes in the Moyabamba basin. The east-verging thin-skinned tectonics shows a strong shortening and is confined to the wedgetop basins of Huallaga and Moyabamba, where it is controlled by the geographical distribution of a large level of Late Permian evaporites sealing the structures of the Gondwanide orogenesis. Towards the NW, the deformation of the Marañon basin is progressively amortized, which is reflected in the transition to a foredeep type deposition zone. The deformation, although not very important, is still active and responsible for shallow earthquakes. From a sedimentary point of view, this thesis has made it possible to differentiate four foreland mega-sequences in the Marañon basin, defined from well stratigraphic correlations and regional discontinuities identified in seismic. A structural section through the Marañon-Huallaga system has been restored in three stages since the Middle Eocene to reconstruct and quantify the propagation of the foreland basin system. The four foreland mega-sequences and the sequential restoration show that the Marañon-Huallaga system developed since the Albian during two stages separated by an important period of erosion during the Middle Eocene. They recorded successively the uplifts of the western and eastern Cordilleras of the Andes of northern Peru, and that of the Arch of Fitzcarrald. From a quantitative point of view, the calculated sedimentation rates show a gradual increase since the Albian, interrupted by the erosion of the Middle Eocene. The 2D petroleum modeling, carried out from a revision of the petroleum systems and the sequential restoration of the Huallaga-Marañon system, valorizes a large part of the results obtained in this thesis by simulating the expulsion of the hydrocarbons at the different stages of the deformation of the Huallaga-Marañon system, and showing its potential trapping areas
Hermoza, Wilber. "Dynamique tectono-sédimentaire et restauration séquentielle du rétro-bassin d'avant-pays des Andes centrales". Toulouse 3, 2004. http://www.theses.fr/2004TOU30134.
Pełny tekst źródłaThe retro-arc foreland basin of the Central Andes is considered as a type-example of a foreland basin system (Horton & DeCelles, 1997). Three regions have been studied : the North Amazonian basin (3-8ʿS), the South Amazonian basin (11-12ʿS) and the south-eastern Bolivian basin (19-20ʿS). The foreland basin system of the Central Andes constitutes a favoured area where studies of the deformation and sedimentary fill can be coupled. This study enabled us to arrive at a clearer understanding of the longitudinal and latitudinal structural/sedimentary evolutions and of the tectono-sedimentary dynamics of the basin and adjacent orogen, and to a sequential restoration of the basins at key-periods in the evolution of the range from the Eocene to present-day. During the early and middle Eocene, the Western Cordillera of northern Peru between 3 and 8ʿS experienced large uplift and erosion. This event is interpreted as a stage of tectonic quiescence and erosional unloading. To the south of 11ʿS, no such event is recorded in the sedimentary fill and the sedimentary arrangement indicates the development of a flexural basin related to orogenic loading. Because the North Amazonian foreland basin system is situated at the junction between the Central Andes and the Northern Andes, this change in the geodynamic process can be ascribed to the interference with the Northern Andes. .
Guibovich, Pérez Pedro M. "Monnier, Marcel. De los Andes hasta Pará. Ecuador - Perú - Amazonas". Pontificia Universidad Católica del Perú, 2012. http://repositorio.pucp.edu.pe/index/handle/123456789/122181.
Pełny tekst źródłaFilizola, Naziano. "Transfert sédimentaire actuel par les fleuves amazoniens". Toulouse 3, 2003. http://www.theses.fr/2003TOU30162.
Pełny tekst źródłaRoddaz, Martin. "Transition des stades alimentés à suralimentés dans les systèmes de rétro-bassin d'avant-pays : du bassin amazonien". Toulouse 3, 2004. http://www.theses.fr/2004TOU30133.
Pełny tekst źródłaIn contrast with southern Andean retro-foreland basins, which are characterized by continental sedimentation, tidal sedimentation was the rule in the Amazonian foreland basin during the Miocene. At this time, the Amazonian foreland basin is considered as "filled". Incipient tectonic loading was responsible for Late Miocene tidal transgression. In the Pliocene times, tectonic loading increased as a result of eastward thrust-propagation causing an increase in elevation and relief creation. Successive uplifts of the Iquitos flexural forebulge played a considerable role in the establishment of the modern Amazon drainage system by enhancing subsidence and separating an Andean drainage from a cratonic drainage system. The Amazonian drainage network is no younger than the Pliocene
Bes, de Berc Séverine. "Tectonique de chevauchement, surrection et incision fluviatile : (exemple de la zone subandine équatorienne, Haut bassin amazonien)". Toulouse 3, 2003. http://www.theses.fr/2003TOU30072.
Pełny tekst źródłaEspinoza, Villar Jhan Carlo. "Impact de la variabilité climatique sur l'hydrologie du bassin amazonien". Paris 6, 2009. https://tel.archives-ouvertes.fr/tel-00379116.
Pełny tekst źródłaLouterbach, Mélanie. "Propagation du front orogénique Subandin et réponse sédimentaire associée dans le bassin d'avant-pays amazonien (Madre de Dios, Pérou)". Toulouse 3, 2014. http://thesesups.ups-tlse.fr/2530/.
Pełny tekst źródłaThe Madre de Dios basin (12º-14ºS) is situated at the south of Peru in the present-day Subandean zone (SAZ), between the Eastern Cordillera (EC) at the West and the Amazonian basin at the Est. Low temperature thermochronological results (apatite fission tracks and (U-Th)/He) obtained for the EC and the SAZ, as well as the growth strata documented in seismic data and on the field allow to determine two main deformation periods in southern Peru: i) from the Oligocene to Middle Miocene (~25-14 Ma, Period 1), and ii) from the Late Miocene to Pleistocene (~10-2. 8 Ma, Period 2). The cooling induced by the erosion of the EC in southern Peru is not controlled by climatic change, but better by the development of duplex in the Andean front. The study of the sedimentary infilling of the Madre de Dios basin indicates that the present day SAZ was already part of a classical foreland basin during the Late Maastrichtian, as attested by the presence of a forebulge at that period. During the Late Paleocene (Thanetian), the basin was covered by a shallow marine incursion documented at the north of the study-area. The Neogene to Pleistocene deposits of the Madre de Dios basin are characterized by a 4500 meter-thick megasequence. Sedimentary infilling is mainly continental and is interpreted as resulting from an eastward migrating Megafan fluvial system. During main tectonic pulses in the EC, the accommodation space increases in the basin. At the final stage of such orogenic loading periods, this flexure could promote shallow marine incursions such as those described in the Madre de Dios basin for the Early Miocene, Middle Miocene and Pliocene (3,45 Ma) times. These new data and interpretations allow a review of the Petroleum system of the Madre de Dios basin
Maurice, Laurence. "Sur les traces du mercure au fil de l'eau, des Andes à l'Amazone". Habilitation à diriger des recherches, Université Paul Sabatier - Toulouse III, 2008. http://tel.archives-ouvertes.fr/tel-00288015.
Pełny tekst źródłaKsiążki na temat "Amazonian Andes"
Bolivie: De la Amazonia a los Andes. Paris: Editions de l'Adret, 1997.
Znajdź pełny tekst źródłaDenevan, William M. Cultivated landscapes of native Amazonia and the Andes. Oxford: Oxford University Press, 2002.
Znajdź pełny tekst źródłaDe los Andes hasta Pará: Ecuador - Perú - Amazonas. Lima: Instituto Francés de Estudios Andinos, 2005.
Znajdź pełny tekst źródłaR, Chuquimamani V. Nonato, Godenzzi Juan Carlos i Centro de Estudios Regionales Andinos "Bartolomé de las Casas.", red. Educación e interculturalidad en los Andes y la Amazonía. Cusco, Perú: Centro de Estudios Regionales Andinos "Bartolomé de Las Casas", 1996.
Znajdź pełny tekst źródła1950-, Monnier Alain, red. L' Amazonie d'une Baronne russe: Des Andes à l'Atlantique en 1903. Genève: Musée d'ethnographie de Genève, 1994.
Znajdź pełny tekst źródłaKroeger, Axel. La lucha por la salud en el alto Amazonas y en los Andes. Quito: Abya-Yala, 1992.
Znajdź pełny tekst źródłaLuna, Carmen. Volkskunst aus Peru: Lebendige Traditionen der Küste der Anden und Amazoniens. Freiburg i. Br. [i.e. Freiburg im Breisgau]: Das Museum, 1992.
Znajdź pełny tekst źródłaM, Jones David. Mythology of the Incas: Myths and legends of the ancient Andes, Western Valleys, desert and Amazonia. London: Southwater, 2003.
Znajdź pełny tekst źródłaEl mundo es como uno lo sueña: Enseñanzas chamánicas del Amazonas y los Andes. México, D.F: Lasser Press Mexicana, 1995.
Znajdź pełny tekst źródłaSamper, Diego. Las voces de la tierra: Paisajes sonoros del Amazonas, los Andes y el Caribe. Santafé de Bogotá [Colombia]: Diego Samper Ediciones, 1999.
Znajdź pełny tekst źródłaCzęści książek na temat "Amazonian Andes"
Sabogal, Ana. "Biodiversity and Endemism of the Andes". W Ecosystem and Species Adaptations in the Andean-Amazonian Region, 49–58. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-44385-5_5.
Pełny tekst źródłaWanderley, Fernanda, Horacio Vera Cossio i Jean Paul Benavides. "Paradoxes of development in the Andes and Amazonia". W Buen Vivir and the Challenges to Capitalism in Latin America, 149–73. New York : Routledge, 2020. | Series: Routledge critical development studies: Routledge, 2020. http://dx.doi.org/10.4324/9781003091516-11.
Pełny tekst źródłaMora, Andres, Patrice Baby, Martin Roddaz, Mauricio Parra, Stéphane Brusset, Wilber Hermoza i Nicolas Espurt. "Tectonic History of the Andes and Sub-Andean Zones: Implications for the Development of the Amazon Drainage Basin". W Amazonia: Landscape and Species Evolution, 38–60. Oxford, UK: Wiley-Blackwell Publishing Ltd., 2011. http://dx.doi.org/10.1002/9781444306408.ch4.
Pełny tekst źródłaTyuleneva, Vera. "The Amazonian Indians as viewed by three Andean chroniclers". W Rethinking the Andes–Amazonia Divide, tłumacz Adrian J. Pearce, 285–96. UCL Press, 2020. http://dx.doi.org/10.2307/j.ctv13xps7k.30.
Pełny tekst źródłaKaulicke, Peter. "Early social complexity in northern Peru and its Amazonian connections". W Rethinking the Andes–Amazonia Divide, 103–14. UCL Press, 2020. http://dx.doi.org/10.2307/j.ctv13xps7k.17.
Pełny tekst źródłaAdelaar, Willem F. H. "Linguistic connections between the Altiplano region and the Amazonian lowlands". W Rethinking the Andes–Amazonia Divide, 239–49. UCL Press, 2020. http://dx.doi.org/10.2307/j.ctv13xps7k.26.
Pełny tekst źródłaHastings, Charles M. "Herders in the Jungle". W The Archaeology of the Upper Amazon, 188–207. University Press of Florida, 2021. http://dx.doi.org/10.5744/florida/9780813066905.003.0010.
Pełny tekst źródłaDenevan, William M. "Pre-European Forest Cultivation". W Cultivated Landscapes of Native Amazonia And the Andes, 115–32. Oxford University PressOxford, 2001. http://dx.doi.org/10.1093/oso/9780198234074.003.0007.
Pełny tekst źródłaArthur, John W. "Meso- and South America". W Beer, 136–67. Oxford University Press, 2022. http://dx.doi.org/10.1093/oso/9780197579800.003.0006.
Pełny tekst źródłaSerna Jeri, Angelica. "Glaciers, the Colonial Archive and the Brotherhood of the Lord of Quyllur Rit’i". W Indigenous and Black Confraternities in Colonial Latin America. Nieuwe Prinsengracht 89 1018 VR Amsterdam Nederland: Amsterdam University Press, 2022. http://dx.doi.org/10.5117/9789463721547_ch07.
Pełny tekst źródłaStreszczenia konferencji na temat "Amazonian Andes"
Pettinger, Alfred M., i Robert Montgomery. "Project Management Considerations of Pipelines Crossing the Andes". W 2010 8th International Pipeline Conference. ASMEDC, 2010. http://dx.doi.org/10.1115/ipc2010-31303.
Pełny tekst źródłaMoya, John Malpartida, Edward Francisco Oliveros Montes i Giancarlo Massucco De la Sota. "Integration of Monitoring and Inspection Systems for Geohazard Assessment on Pipelines That Cross Amazonian Jungles and the Andes". W 2012 9th International Pipeline Conference. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/ipc2012-90501.
Pełny tekst źródłaMoya, John Erick Malpartida. "Managing Geohazards in Hard Conditions: Monitoring and Risk Assessment of Pipelines That Crosses Amazonian Jungles and the Andes". W ASME 2015 International Pipeline Geotechnical Conference. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/ipg2015-8532.
Pełny tekst źródłaRibera Torró, Esteve. "KUÉLAP VIRTUAL: VIRTUALIZACIÓN DE UNA CIUDADELA PREINCA EN LOS ANDES AMAZÓNICOS DEL PERÚ MEDIANTE FOTOGRAFÍA ESFÉRICA, MODELADO 3D E IMPRESIÓN 3D". W ARQUEOLÓGICA 2.0 - 8th International Congress on Archaeology, Computer Graphics, Cultural Heritage and Innovation. Valencia: Universitat Politècnica València, 2016. http://dx.doi.org/10.4995/arqueologica8.2016.3567.
Pełny tekst źródłaMalpartida Moya, John. "Integrity Management System Based on Risk Analysis: A Tool To Prevent Failures on Pipelines Which Crossing Amazonian Jungles and the Andes". W SPE Latin-American and Caribbean Health, Safety, Environment and Social Responsibility Conference. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/165601-ms.
Pełny tekst źródłaGaibor, Janeth, Santiago Guerrero, Martina Grefa, Anne Valdez i Angel Villavicencio. "High-Resolution Resistivity Image Interpretation to Improve Stratigraphic Model of the ITT Field – Oriente Basin, Ecuador". W SPE Annual Technical Conference and Exhibition. SPE, 2022. http://dx.doi.org/10.2118/210088-ms.
Pełny tekst źródłaMoya, John Malpartida, i Giancarlo Massucco De la Sota. "Alternative Geohazard Risk Assessment and Monitoring for Pipelines With Limited Access: Amazon Jungle Example". W 2014 10th International Pipeline Conference. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/ipc2014-33628.
Pełny tekst źródłaMontes, Edward Francisco Oliveros. "Unprovoked Errors in Geotechnical Monitoring Activities in an RoW". W ASME 2015 International Pipeline Geotechnical Conference. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/ipg2015-8518.
Pełny tekst źródłaLopez, Byron G. "Implications of Reduced Heating of Heavy Crude Pipeline on Pump Lubrication Systems". W 2012 9th International Pipeline Conference. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/ipc2012-90315.
Pełny tekst źródłaMiola, Evandro Carlos. "O auxílio-doença acidentário no Amazonas, antes e depois do FAP/NTEP". W 17º Congresso da Associação Nacional de Medicina do Trabalho. 17 - Supl.1, 2019. http://dx.doi.org/10.5327/z16794435201917s1tl084.
Pełny tekst źródłaRaporty organizacyjne na temat "Amazonian Andes"
Flores, Bernardo M., Adriane Esquivel-Muelbert, Marco Ehrlich, Emilio Vilanova, Raquel Chaves, Marina Hirota i Michelle Kalamandeen. NUEVE MANERAS DE EVITAR EL PUNTO DE NO RETORNO EN LA AMAZONÍA. Sustainable Development Solutions Network (SDSN), grudzień 2023. http://dx.doi.org/10.55161/oqrm8068.
Pełny tekst źródłaDiversidad Biológica de Tres Tipos de Vertebrados en Cinco Paisajes de Conservación de los Andes-Amazonía Apoyados por Wildlife Conservation Society. Wildlife Conservation Society, 2020. http://dx.doi.org/10.19121/2020.report.42014.
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