Un Análisis Del Cactus Columnar Echinopsis Terscheckii a Distintas
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Copyright Notice This electronic reprint is provided by the author(s) to be consulted by fellow scientists. It is not to be used for any purpose other than private study, scholarship, or research. Further reproduction or distribution of this reprint is restricted by copyright laws. If in doubt about fair use of reprints for research purposes, the user should review the copyright notice contained in the original journal from which this electronic reprint was made. Journal of Vegetation Science 7: 667-680, 1996 © IAVS; Opulus Press Uppsala. Printed in Sweden - Biogeographic patterns of Argentine cacti - 667 Species richness of Argentine cacti: A test of biogeographic hypotheses Mourelle, Cristina & Ezcurra, Exequiel Centro de Ecología, UNAM, Apartado Postal 70-275, 04510 - Mexico, D.F., Mexico; Fax +52 5 6228995; E-mail [email protected] Abstract. Patterns of species richness are described for 50 cacti and (e) pereskioid cacti. Columnar species have columnar, 109 globose and 50 opuntioid cacti species in 318 column-like stems with ribs, formed by an arrangement grid cells (1°×1°) covering Argentina. Biological richness of the areoles in longitudinal rows. These species have hypotheses were tested by regressing 15 environmental parallel vascular bundles, separated by succulent paren- descriptors against species richness in each group. We also chyma, sometimes fusing towards a woody base in the included the collection effort (estimated as the logarithm of the number of herbarium specimens collected in each cell) to adults. We broadly considered as columnar cacti: estimate the possible error induced by underrepresentation in candelabriform arborescent species, unbranched erect certain cells. -
Redalyc.Sr, C and O Isotope Composition of Marbles from The
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España Murra, J.A.; Baldo, E.G.; Galindo, C.; Casquet, C.; Pankhurst, R.J.; Rapela, C.W.; Dahlquist, J. Sr, C and O isotope composition of marbles from the Sierra de Ancasti, Eastern Sierras Pampeanas, Argentina: age and constraints for the Neoproterozoic-Lower Paleozoic evolution of the proto- Gondwana margin Geologica Acta: an international earth science journal, vol. 9, núm. 1, marzo, 2011, pp. 79-92 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50522124008 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 Geologica Acta, Vol.9, Nº 1, March 2011, 79-92 DOI: 10.1344/105.000001645 Available online at www.geologica-acta.com Sr, C and O isotope composition of marbles from the Sierra de Ancasti, Eastern Sierras Pampeanas, Argentina: age and constraints for the Neoproterozoic–Lower Paleozoic evolution of the proto-Gondwana margin 1 1 2 2 3 4 1 J.A. MURRA E.G. BALDO C. GALINDO C. CASQUET R.J. PANKHURST C.W. RAPELA J. DAHLQUIST 1 CICTERRA (Universidad Nacional de Córdoba - Conicet) Av. Vélez Sarsfield 1611, 5016 Córdoba, Argentina. Murra E-mail: [email protected] Baldo E-mail: [email protected] Dahlquist E-mail: [email protected] 2 Departamento. Petrología y Geoquímica Facultad de Ciencias Geológicas, Inst. -
University of Florida Thesis Or Dissertation Formatting
SYSTEMATICS OF TRIBE TRICHOCEREEAE AND POPULATION GENETICS OF Haageocereus (CACTACEAE) By MÓNICA ARAKAKI MAKISHI 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 2008 1 © 2008 Mónica Arakaki Makishi 2 To my parents, Bunzo and Cristina, and to my sisters and brother. 3 ACKNOWLEDGMENTS I want to express my deepest appreciation to my advisors, Douglas Soltis and Pamela Soltis, for their consistent support, encouragement and generosity of time. I would also like to thank Norris Williams and Michael Miyamoto, members of my committee, for their guidance, good disposition and positive feedback. Special thanks go to Carlos Ostolaza and Fátima Cáceres, for sharing their knowledge on Peruvian Cactaceae, and for providing essential plant material, confirmation of identifications, and their detailed observations of cacti in the field. I am indebted to the many individuals that have directly or indirectly supported me during the fieldwork: Carlos Ostolaza, Fátima Cáceres, Asunción Cano, Blanca León, José Roque, María La Torre, Richard Aguilar, Nestor Cieza, Olivier Klopfenstein, Martha Vargas, Natalia Calderón, Freddy Peláez, Yammil Ramírez, Eric Rodríguez, Percy Sandoval, and Kenneth Young (Peru); Stephan Beck, Noemí Quispe, Lorena Rey, Rosa Meneses, Alejandro Apaza, Esther Valenzuela, Mónica Zeballos, Freddy Centeno, Alfredo Fuentes, and Ramiro Lopez (Bolivia); María E. Ramírez, Mélica Muñoz, and Raquel Pinto (Chile). I thank the curators and staff of the herbaria B, F, FLAS, LPB, MO, USM, U, TEX, UNSA and ZSS, who kindly loaned specimens or made information available through electronic means. Thanks to Carlos Ostolaza for providing seeds of Haageocereus tenuis, to Graham Charles for seeds of Blossfeldia sucrensis and Acanthocalycium spiniflorum, to Donald Henne for specimens of Haageocereus lanugispinus; and to Bernard Hauser and Kent Vliet for aid with microscopy. -
Early Evolution of the Proto-Andean Margin of South America
Early evolution of the Proto-Andean margin of South America C. W. Rapela Centro de Investigaciones Geológicas, Universidad Nacional de La Plata, Calle 1 No. 644, 1900 La Plata, Argentina R. J. Pankhurst British Antarctic Survey, Cambridge CB30ET, United Kingdom C. Casquet Departamento de Petrología y Geoquímica, Universidad Complutense, 28040 Madrid, Spain E. Baldo J. Saavedra CSIC, Instituto de Agrobiología y Recursos Naturales, 37071 Salamanca, Spain C. Galindo Departamento de Petrología y Geoquímica, Universidad Complutense, 28040 Madrid, Spain ABSTRACT INTRODUCTION From a detailed study of a 500 km transect in the Sierras Pampeanas, central-west Argen- The evolution of the Gondwana margin pro- tina, two pre-Silurian tectono-magmatic episodes are recognized and defined, each culminating posed here is based on new geochemical, isotopic, in micro-continental collisions against the proto-Andean margin of Gondwana. The Pampean petrological, and sedimentological data from a orogeny started in Early Cambrian time with short-lived subduction, indicated by ca. 535 Ma 500 km traverse across the Eastern Sierras Pam- calc-alkaline granitoids. Following Pampean terrane collision, burial to granulite facies condi- peanas and Precordillera (Fig. 1). Pre-Silurian tions (ca. 9 kbar) generated widespread migmatites and ca. 520 Ma highly peraluminous gran- metamorphic and magmatic history is inferred ites in the Eastern Sierras Pampeanas. After brief quiescence, a second major episode, the from (1) dating by conventional U-Pb on abraded Famatinian orogeny, started with subduction ca. 490 Ma, forming a wide continental arc and zircons, U-Pb SHRIMP analyses, and whole-rock ensialic backarc basin. This heralded the approach of Laurentia to Gondwana, during which Rb-Sr and K-Ar, (2) thermo-barometry based on the Precordillera terrane separated from the southern Appalachian region, finally colliding with microprobe mineral analyses, and (3) Nd and Sr Gondwana in Silurian–Devonian time. -
Winter/Spring 2014
UNIVERSITY of CALIFORNIA BOTANICAL GARDEN NEWSLETTER Vol. 38 Numbers 1 & 2 | Published by the UNIVERSITY of CALIFORNIA BOTANICAL GARDEN at BERKELEY | Winter/ Spring 2014 The New World Desert Collection 'HVHUWV DUH RIWHQ GH¿QHG DV areas receiving less than 254 mm (10 in) of rainfall each year. Given that the Garden typically receives over 500 mm (20 in), this collection is a horticultural challenge. The Garden’s heavy clay soil has been greatly amended with expanded shale to improve drainage and reduce the incidence of diseases and pests, especially nematodes. Recent efforts to improve plant health with the application of compost tea and organic top dressing has shown good results, with renewed vigor DQGPRUHSUROL¿FÀRZHULQJRIPDQ\ FDFWL%HQH¿FLDOQHPDWRGHVDUHDOVR The hot south-facing exposure and rocky hardscape of the New World Desert provide a dramatic experience in the Garden. employed to keep the harmful ones Photo by Janet Williams in check. stablished early on in the Garden’s history in Strawberry Canyon, the New World Desert (NWD) is an iconic display of arid land plants from North and South America. EIt really started to take shape in the 1930s with the addition of plants collected during the Garden’s expeditions to the Andes. These expeditions focused on Peru and Chile, with forays into Bolivia. Botanical and personal highlights of these expeditions are documented in Garden Director T. Harper Goodspeed’s book, Plant Hunters of the Andes, published in 1961. The most recent desert expedition was to Baja California in 1986, led by then curator Dr. James Affolter and included Horticulturists Kurt Zadnik and Roger Raiche and current volunteer Fred Dortort. -
GSA TODAY • Radon in Water, P
Vol. 8, No. 11 November 1998 INSIDE • Field Guide Editor, p. 5 GSA TODAY • Radon in Water, p. 10 • Women Geoscientists, p. 12 A Publication of the Geological Society of America • 1999 Annual Meeting, p. 31 Gas Hydrates: Greenhouse Nightmare? Energy Panacea or Pipe Dream? Bilal U. Haq, National Science Foundation, Division of Ocean Science, Arlington, VA 22230 ABSTRACT Recent interest in methane hydrates has resulted from the recognition that they may play important roles in the global carbon cycle and rapid climate change through emissions of methane from marine sediments and permafrost into the atmosphere, and in causing mass failure of sediments and structural changes on the continental slope. Their presumed large volumes are also consid- ered to be a potential source for future exploitation of methane as a resource. Natural gas hydrates occur widely on continental slope and rise, stabilized in place by high hydrostatic pressure and frigid bottom-temperature condi- tions. Change in these conditions, Figure 1. This seismic profile, over the landward side of Blake Ridge, crosses a salt diapir; the profile has either through lowering of sea level or been processed to show reflection strength. The prominent bottom simulating reflector (BSR) swings increase in bottom-water temperature, upward over the diapir because of the higher conductivity of the salt. Note the very strong reflections of may trigger the following sequence of gas accumulations below the gas-hydrate stability zone and the “blanking” of energy above it. Bright events: dissociation of the hydrate at its Spots along near-vertical faults above the diapir represent conduits for gas venting. -
Taxonomía Y Filogenia De Trichocereus (Berg.) Riccob
UNIVERSIDAD NACIONAL DE LA PLATA FACULTAD DE CIENCIAS NATURALES Y MUSEO ―Taxonomía y filogenia de Trichocereus (Berg.) Riccob. (Trichocereeae- Cactaceae)‖ Tesis presentada para optar al grado de Doctor en Ciencias Naturales de la Universidad Nacional de La Plata Bióloga M. Sc. Adriana Sofía Albesiano Hoyos Director: Dr. Roberto Kiesling Co-Directora: Dra. Susana Freire La Plata, Argentina Agosto 3 de 2015 COMISIÓN ASESORA Dr. Roberto Kiesling, Instituto Argentino de Investigaciones de las Zonas Áridas-IADIZA, CONICET. Dra. Susana Freire, Instituto de Botánica Darwinion-San Isidro. Prof. Titular, Cátedra de Botánica Sistemática II, Facultad Ciencias Naturales y Museo, Universidad Nacional de La Plata. DEFENSA ORAL Y PÚBLICA Lugar y Fecha: Calificación: TRIBUNAL Firma:………………………………………………………...Aclaración………… Firma:………………………………………………………...Aclaración………… Firma:………………………………………………………...Aclaración………… TABLA DE CONTENIDO AGRADECIMIENTOS .............................................................................................................................. iii RESUMEN............................................................................................................................................... iv ABSTRACT ............................................................................................................................................ viii I. INTRODUCCIÓN ................................................................................................................................... 1 II. MATERIALES Y MÉTODOS ................................................................................................................ -
Cactus Explorer the first Free On-Line Journal for Cactus and Succulent Enthusiasts
TheCactus Explorer The first free on-line Journal for Cactus and Succulent Enthusiasts 1 Schlumbergera opuntioides 2 Parodia mammulosa Number 13 3 Explorers Weekend 2014 ISSN 2048-0482 4 Crassulaceae at Lyon B.G. December 2014 5 Schlumbergera truncata The Cactus Explorer ISSN 2048-0482 Number 13 December 2014 THE POSITION OF PARODIA TURECEKIANA IN THE PARODIA MAMMULOSA COMPLEX In this article, Giovanna Anceschi & Alberto Magli discuss Parodia turecekiana R. Kiesling, part of the Parodia mammulosa (Lemaire) Taylor complex. Photographs by the authors Fig.1 Parodia mammulosa (turecekiana populations). Uruguay, Rio Negro, Nuevo Berlin. 27 Jan 2014, A&M 966 During the seven months of our 2013/2014 Parodia turecekiana R. Kiesling was one of journey, out of the 70 new taxa we investigated our “black sheep”. In fact, before this year’s in habitat for a forthcoming classification in the happy discovery, we failed to find the above Cactusinhabitat system, 11 belong to the genus mentioned taxon of the Pampa Biome on three Parodia Spegazzini (precisely, 10 are Andean occasions. The first time was in November taxa and one from the Pampa Biome). Parodia 2008, in Uruguay, Dpt. Río Negro, on Ruta 25, being one of our genera of preference, during between Bellaco and Young, following the our next journey we hope to find or deepen the reference R. Kiesling 8368 (Kiesling 1995, 67: knowledge of the last four taxa that will allow 18). The second time, again in November 2008, us to have a complete overview of Parodia s.l., in Uruguay, Dpt. Río Negro, Young, northwest based on study experience in the habitats of all of Young, locality Paso Uleste, in the its components. -
List of Approved Plants
APPENDIX "X" – PLANT LISTS Appendix "X" Contains Three (3) Plant Lists: X.1. List of Approved Indigenous Plants Allowed in any Landscape Zone. X.2. List of Approved Non-Indigenous Plants Allowed ONLY in the Private Zone or Semi-Private Zone. X.3. List of Prohibited Plants Prohibited for any location on a residential Lot. X.1. LIST OF APPROVED INDIGENOUS PLANTS. Approved Indigenous Plants may be used in any of the Landscape Zones on a residential lot. ONLY approved indigenous plants may be used in the Native Zone and the Revegetation Zone for those landscape areas located beyond the perimeter footprint of the home and site walls. The density, ratios, and mix of any added indigenous plant material should approximate those found in the general area of the native undisturbed desert. Refer to Section 8.4 and 8.5 of the Design Guidelines for an explanation and illustration of the Native Zone and the Revegetation Zone. For clarity, Approved Indigenous Plants are considered those plant species that are specifically indigenous and native to Desert Mountain. While there may be several other plants that are native to the upper Sonoran Desert, this list is specific to indigenous and native plants within Desert Mountain. X.1.1. Indigenous Trees: COMMON NAME BOTANICAL NAME Blue Palo Verde Parkinsonia florida Crucifixion Thorn Canotia holacantha Desert Hackberry Celtis pallida Desert Willow / Desert Catalpa Chilopsis linearis Foothills Palo Verde Parkinsonia microphylla Net Leaf Hackberry Celtis reticulata One-Seed Juniper Juniperus monosperma Velvet Mesquite / Native Mesquite Prosopis velutina (juliflora) X.1.2. Indigenous Shrubs: COMMON NAME BOTANICAL NAME Anderson Thornbush Lycium andersonii Barberry Berberis haematocarpa Bear Grass Nolina microcarpa Brittle Bush Encelia farinosa Page X - 1 Approved - February 24, 2020 Appendix X Landscape Guidelines Bursage + Ambrosia deltoidea + Canyon Ragweed Ambrosia ambrosioides Catclaw Acacia / Wait-a-Minute Bush Acacia greggii / Senegalia greggii Catclaw Mimosa Mimosa aculeaticarpa var. -
Volume 8, Issue 2, 2017 ISSN 2191-3099 This Document Was Published in Pdf Format: August 19Th 2017
Schütziana The Gymnocalycium Online Journal Volume 8, Issue 2, 2017 ISSN 2191-3099 This document was published in pdf format: August 19th 2017 Content Papsch, Wolfgang Editorial p. 2 Marx, Ulf p. 3-10 Franz Strigl – 80 years and still young at heart Kulhánek, Tomáš Papsch, Wolfgang On the Distribution of Gymnocalycium platense p. 11-23 (Spegazzini) Britton & Rose (Cactaceae) Kulhánek, Tomáš Gymnocalycium alenae Kulhánek, a new species p. 24-38 from the northern part of province Córdoba Published: August 19th 2017 Legal notice Publisher: WORKING GROUP SCHÜTZIANA, Fichtenweg 43, 14547 Fichtenwalde, Germany Editorial team and responsible for the content: www.schuetziana.org/contact.php Mario Wick, 14547 Fichtenwalde, Fichtenweg 43, Germany, [email protected] Massimo Meregalli, 10123 Torino, V. Accademia Albertina, 17, Italia, [email protected] Wolfgang Papsch, 8401 Kalsdorf, Ziehrenweg 6, Austria, [email protected] Tomáš Kulhánek, 67201 Moravský Krumlov, Tylova 673, Czech Republic, [email protected]. SCHÜTZIANA is the journal of the WORKING GROUP SCHÜTZIANA. Source of supply: SCHÜTZIANA is available only as a pdf-file via World Wide Web and can be downloaded from: www.schuetziana.org/download.php. The content of the respective article expresses the opinion of the author and need not being in agreement with the opinion of the WORKING GROUP SCHÜTZIANA. The issues of SCHÜTZIANA are free of charge and may be distributed freely. The content and the pictures of the articles of SCHÜTZIANA are property of the author and may not be used for other purposes than reading, printing and storing without permission. © 2017 WORKING GROUP SCHÜTZIANA. -
Andean Flat-Slab Subduction Through Time
Andean flat-slab subduction through time VICTOR A. RAMOS & ANDRE´ S FOLGUERA* Laboratorio de Tecto´nica Andina, Universidad de Buenos Aires – CONICET *Corresponding author (e-mail: [email protected]) Abstract: The analysis of magmatic distribution, basin formation, tectonic evolution and structural styles of different segments of the Andes shows that most of the Andes have experienced a stage of flat subduction. Evidence is presented here for a wide range of regions throughout the Andes, including the three present flat-slab segments (Pampean, Peruvian, Bucaramanga), three incipient flat-slab segments (‘Carnegie’, Guan˜acos, ‘Tehuantepec’), three older and no longer active Cenozoic flat-slab segments (Altiplano, Puna, Payenia), and an inferred Palaeozoic flat- slab segment (Early Permian ‘San Rafael’). Based on the present characteristics of the Pampean flat slab, combined with the Peruvian and Bucaramanga segments, a pattern of geological processes can be attributed to slab shallowing and steepening. This pattern permits recognition of other older Cenozoic subhorizontal subduction zones throughout the Andes. Based on crustal thickness, two different settings of slab steepening are proposed. Slab steepening under thick crust leads to dela- mination, basaltic underplating, lower crustal melting, extension and widespread rhyolitic volcan- ism, as seen in the caldera formation and huge ignimbritic fields of the Altiplano and Puna segments. On the other hand, when steepening affects thin crust, extension and extensive within-plate basaltic flows reach the surface, forming large volcanic provinces, such as Payenia in the southern Andes. This last case has very limited crustal melt along the axial part of the Andean roots, which shows incipient delamination. -
Variabilidad Morfológica Y Modelos Arqueológicos
1 El presente trabajo se orientó al estudio de la variación craneofacial de los grupos humanos que habitaron el sector austral de las Sierras Pampeanas y llanuras circundantes en tiempos prehispánicos desde una perspectiva que combina análisis morfológicos cuali-cuantitativos y análisis basados en la morfometría geométrica. Como objetivos específicos se planteó: a) caracterizar morfológicamente colecciones arqueológicas inéditas de restos óseos, b) estudiar la variación craneofacial de las mencionadas colecciones a partir de análisis de morfometría geométrica, c) establecer relaciones genéticas entre las poblaciones de la región central del país y demás regiones geográfico-ecológicas de Argentina y Sudamérica (Andes, Amazonia, Gran Chaco, Patagonia-Tierra del Fuego), d) poner a prueba diferentes modelos sobre las posibles vías de poblamiento del centro del país. Los resultados sugieren importantes similitudes a nivel de morfología craneal y variación epigenética entre muestras principalmente del lado oriental de las sierras –actual territorio de la provincia de Córdoba- y poblaciones del centro y Noreste de Patagonia, y región pampeana. Teniendo en cuenta los resultados generales, consideramos que el poblamiento de la región austral de las Sierras Pampeanas se relaciona con aquel ocurrido desde el Noreste del país, siguiendo un derrotero general Norte-Sur a través del Litoral Atlántico. Mariana Fabra Doctora en Historia (Facultad de Filosofía y Humanidades, Universidad Nacional de Córdoba, Argentina) y Magister en Antropología (FFyH, UNC), se desempeña actualmente como Investigadora Adjunta del Consejo Nacional de Investigaciones Científicas y Técnicas. Es Profesora Asistente la licenciatura en Antropología (Departamento de Antropología, Área Antropología Biológica, FFyH, UNC). Ha dirigido diversos proyectos de investigación (PIP CONICET, PID MiNCyT Córdoba), sobre temáticas vinculadas al poblamiento de la región central de Argentina y el estilo de vida de las poblaciones originarias del centro del país desde una perspectiva bioarqueológica.