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Ischigualasto Formation. the Second Is a Sile- Diversity Or Abundance, but This Result Was Based on Only 19 of Saurid, Ignotosaurus Fragilis (Fig
This article was downloaded by: [University of Chicago Library] On: 10 October 2013, At: 10:52 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Vertebrate Paleontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ujvp20 Vertebrate succession in the Ischigualasto Formation Ricardo N. Martínez a , Cecilia Apaldetti a b , Oscar A. Alcober a , Carina E. Colombi a b , Paul C. Sereno c , Eliana Fernandez a b , Paula Santi Malnis a b , Gustavo A. Correa a b & Diego Abelin a a Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan , España 400 (norte), San Juan , Argentina , CP5400 b Consejo Nacional de Investigaciones Científicas y Técnicas , Buenos Aires , Argentina c Department of Organismal Biology and Anatomy, and Committee on Evolutionary Biology , University of Chicago , 1027 East 57th Street, Chicago , Illinois , 60637 , U.S.A. Published online: 08 Oct 2013. To cite this article: Ricardo N. Martínez , Cecilia Apaldetti , Oscar A. Alcober , Carina E. Colombi , Paul C. Sereno , Eliana Fernandez , Paula Santi Malnis , Gustavo A. Correa & Diego Abelin (2012) Vertebrate succession in the Ischigualasto Formation, Journal of Vertebrate Paleontology, 32:sup1, 10-30, DOI: 10.1080/02724634.2013.818546 To link to this article: http://dx.doi.org/10.1080/02724634.2013.818546 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. -
Abstract Structural Controls on Extensional
ABSTRACT STRUCTURAL CONTROLS ON EXTENSIONAL-BASIN DEVELOPMENT TRIASSIC ISCHIGUALASTO FORMATION, NW ARGENTINA By Kristin Guthrie This thesis reports the results of a structural and stratigraphic field study of the Ischigualasto Formation in the Ischigualasto Basin, NW Argentina. Previous stratigraphic investigations have documented an along-strike increase in Ischigualasto Formation thickness of ~275 m over a distance of 7 km. While this thickness change has been attributed to syndepositional faulting, the exact location and characteristics of controlling faults have never been documented. In order to determine the influence of fault-related accommodation development on thickness variations in the Ischigualasto Formation a detailed structural mapping project was conducted in the eastern part of the basin. Field mapping identified two groups of intrabasinal normal faults with near perpendicular strike azimuths. These fault orientations, and their calculated extension directions, are best explained by the development of basin-margin perpendicular release faults coupled with normal-sense reactivation of preexisting basement structures. Calculation of cumulative observed displacements along intrabasinal normal faults in the study area, however, revealed a negligible contribution to accommodation. The presence of interpreted release faults in the study area, however, suggests that observed changes in Ischigualasto Formation thickness were controlled by a northwest increase in basin- bounding fault displacement during the time of deposition. STRUCTURAL CONTROLS ON EXTENSIONAL-BASIN DEPOSITION, UPPER TRIASSIC ISCHIGUALASTO FORMATION, NORTHWESTERN ARGENTINA A Thesis Submitted to the Faculty of Miami University In partial fulfillment of The requirements for the degree of Master of Science Department of Geology By Kristin Guthrie Miami University Oxford, OH 2005 Advisor ______________________________________ (Dr. Brian Currie) Reader _______________________________________ (Dr. -
The Triassic Insect Fauna from the Los Rastros Formation (Bermejo Basin), La Rioja Province (Argentina): Their Con- Text, Taphonomy and Paleobiology
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 44 (2): 000-000. Buenos Aires, 30-6-2007 ISSN 0002-7014 The Triassic insect fauna from the Los Rastros Formation (Bermejo Basin), La Rioja Province (Argentina): their con- text, taphonomy and paleobiology Adriana C. MANCUSO1, Oscar F. GALLEGO2 and Rafael G. MARTINS-NETO3 Abstract. In the Bermejo Basin, the Los Rastros Formation bears an abundant insect fauna, mainly with terrestrial adult winged organisms related to the Blattoptera and the Coleoptera orders. The insect re- mains are found in the black shales of the offshore lacustrine facies and the insect taphonomic features suggest that the specimens were allochthonous to the lake. The individuals appear to arrived alive to the lake and suffered a rapid fall through the water column thus, preserving them intact, and some of them suffered fragmentation in air transportation and by biological attack during long periods of flotation. Resumen. LA FAUNA DE INSECTOS TRIÁSICOS DE LA FORMACIÓN LOS RASTROS (CUENCA BERMEJO), PROVINCIA DE LA RIOJA (ARGENTINA): SU CONTEXTO, TAFONOMÍA Y PALEOBIOLOGÍA. En la Cuenca Bermejo, la Formación Los Rastros es portadora de una abundante fauna de insectos, principalmente organismos adultos terrestres y alados pertenecientes a los órdenes Blattoptera y Coleoptera. Los restos de insectos son encontrados en las pelitas negras de la facies de lago abierto. Las características tafonómicas de los insectos sugieren que los especímenes son alóctonos al lago. Los individuos pudieron llegar vivos al lago y sufrir una rápida caída a través de la columna de agua, preservándose intactos, o sufrieron fragmentación en el transporte aéreo y por ataques biológicos durante largos períodos de flotación. -
Miospores and Chlorococcalean Algae from the Los Rastros Formation, Middle to Upper Triassic of Central-Western Argentina
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 42 (2): 347-362. Buenos Aires, 30-06-2005 ISSN 0002-7014 Miospores and chlorococcalean algae from the Los Rastros Formation, Middle to Upper Triassic of central-western Argentina Eduardo G. OTTONE, Adriana C. MANCUSO and Magdalena RESANO Abstract. Lacustrine strata of the Los Rastros Formation (Middle to Upper Triassic) at Río Gualo section (La Rioja province), yield a distinctive palynological assemblage of miospores and chlorococcalean algae. The miospore association is characterized by a relative abundance of corystosperm pollen grains with sub- ordinate inaperturates, diploxylonoid disaccates, spores, monocolpates, monosaccates and striate pollen grains. The phytoplankton are mostly represented by Botryococcus but also by Plaesiodictyon, a form prob- ably related to the Hydrodictyaceae. Geological data and variations in phytoplankton content indicate that the lacustrine system probably evolved from a stretcht of freshwater with eutrophic conditions, into a body with oligotrophic conditions through the middle and upper part of the Río Gualo section. The genus Variapollenites is emended in order to amplify its original diagnosis. Resumen. MIOSPORAS Y ALGAS CHLOROCOCCALES DE LA FORMACIÓN LOS RASTROS, TRIÁSICO MEDIO A SUPERIOR DEL CENTRO-OESTE DE ARGENTINA. El estudio de los niveles lacustres de la Formación Los Rastros (Triásico Medio a Superior) en la sección de Río Gualo (provincia de La Rioja), incluye una interesante palinoflora compuesta por miosporas y algas Chlorococcales. Entre las miosporas abundan los granos de polen de Corystospermales, con presencia subordinada de inaperturados, disacados diploxilonoides, esporas, monocolpados, monosacados y polen estriado. En el fitoplancton se destaca Botryococcus, pero también se observa Plaesiodictyon, que es una forma probablemente relacionada con las Hydrodictyaceae. -
Supplementary Information
SUPPLEMENTARY INFORMATION The oldest known communal latrines provide evidence of gregarism in Triassic megaherbivores Lucas E. Fiorelli*, Martín D. Ezcurra, E. Martín Hechenleitner, Eloisa Argañaraz, Jeremías R. A. Taborda, M. Jimena Trotteyn, M. Belén von Baczko & Julia B. Desojo *To whom correspondence should be addressed. E-mail: [email protected] 1. Provenance, authenticity, geological setting and stratigraphy of the communal latrines of the Chañares Formation 2. Depositional setting 3. Taphonomy 4. Statistics 5. Age of the Chañares Formation 6. Fossil tetrapods from the Chañares Formation 7. Dinodontosaurus body size 8. Dinodontosaurus as a gregarious megaherbivore 9. References 1. Provenance, authenticity, geological setting and stratigraphy of the communal latrines of the Chañares Formation. Several communal latrines were found in successive palaeontological field works conducted in 2011 and 2012 in outcrops of the Chañares Formation situated in the Talampaya National Park, La Rioja Province, northwestern Argentina (Supplementary Figure 1a). The Chañares Formation 1 crops out as part of the Ischigualasto-Villa Unión Basin, which represents a succession of continental deposits composed of 4,000 metres of alluvial, fluvial and lacustrine sediments 2,3 . The basin contains the reddish Talampaya and Tarjados formations as its lower- most units and corresponds to the Synrift 1 tectonic phase. The Talampaya Formation is dated as Induan/Olenekian (Early Triassic) and the Tarjados Formation as Anisian (early Middle Triassic) according to some authors 3,4 . The lower section of the Talampaya Formation is represented by alluvian fan deposits followed by fluvial and playa lake deposits in the middle and upper sections 4. The Tarjados Formation has aerealy extensive outcrops in the Talampaya National Park but at the moment no significant fossil vertebrate remains were reported. -
The Precise Temporal Calibration of Dinosaur Origins SEE COMMENTARY
The precise temporal calibration of dinosaur origins SEE COMMENTARY Claudia A. Marsicanoa, Randall B. Irmisb,c,1, Adriana C. Mancusod, Roland Mundile, and Farid Chemalef aDepartamento de Ciencias Geológicas, Instituto de Estudios Andinos-Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Ciudad Autónoma de Buenos Aires C1428EHA, Argentina; bNatural History Museum of Utah, University of Utah, Salt Lake City, UT 84108-1214; cDepartment of Geology & Geophysics, University of Utah, Salt Lake City, UT 84112-0102; dInstituto Argentino de Nivología, Glaciología y Ciencias Ambientales, Centro Científico y Tecnológico-Consejo Nacional de Investigaciones Científicas y Técnicas-Mendoza, Mendoza CC330, Argentina; eBerkeley Geochronology Center, Berkeley, CA 94709; and fInstituto de Geociências, Universidade de Brasília, Brasília-DF 70864-050, Brazil Edited by Paul E. Olsen, Columbia University, Palisades, NY, and approved November 6, 2015 (received for review June 25, 2015) Dinosaurs have been major components of ecosystems for over 200 composition across Pangea appears to be particularly heteroge- million years. Although different macroevolutionary scenarios exist neous (11–13). Without precise independent age control (other to explain the Triassic origin and subsequent rise to dominance of than vertebrate biostratigraphic correlations), it is impossible to dinosaurs and their closest relatives (dinosauromorphs), all lack critical determine if these faunal differences vary across time, space, or a support from a precise biostratigraphically independent temporal combination of both. framework. The absence of robust geochronologic age control for Among the many uncertainties regarding dinosaur evolution is comparing alternative scenarios makes it impossible to determine if the timing of the origin and subsequent radiation of this clade and observed faunal differences vary across time, space, or a combination their closest relatives (early dinosauromorphs). -
Abstract a Triassic Syndepositional
ABSTRACT A TRIASSIC SYNDEPOSITIONAL DETACHMENT SYSTEM, ISCHIGUALASTO PROVINCIAL PARK, NORTHWESTERN ARGENTINA Tony L. Albrecht The Ischigualasto basin of northwest Argentina contains ~4 km of non-marine strata. In the southeast part of the basin, the Middle Triassic Los Rastros Formation contains a ~1 km2 area where rocks exhibit both extensional and contractional deformation features. To the east, both high angle and listric normal faults are the dominant structures. To the west, deformation consists of reverse and thrust faults, in addition to upright and overturned folds. Faults in both areas sole into a sub-horizontal detachment surface, below which rocks are undeformed. Deformed Los Rastros Formation strata are overlain by lightly-deformed/undeformed rocks of the Upper Triassic Ischigualasto Formation. The Agua de la Peña detachment system is interpreted to have formed as a result of gravity spreading/depositional loading of lacustrine delta platform and fluvial deposits above an overpressured shale décollement. Although 2-3 orders of magnitude smaller, the cross- sectional shape and interpreted driving mechanisms of the Agua de la Peña detachment are similar to paired extensional-contractional fault systems formed along continental margins. Based on reconstructed geometry and interpreted rheology, the contractional portion of the detachment can be modeled as a critical-tapered wedge, and provides a small-scale analogue for fold-thrust belts formed in passive-margin settings. A TRIASSIC SYNDEPOSITIONAL DETACHMENT SYSTEM, ISCHIGUALASTO PROVINCIAL PARK, NORTHWESTERN ARGENTINA A Thesis Submitted to the Faculty of Miami University in partial fulfillment of the requirements for the degree of Master of Science Department of Geology by Tony L. Albrecht Miami University Oxford, Ohio 2005 Advisor______________________________________ Dr. -
Dinosaur Diversification Linked with the Carnian Pluvial Episode
ARTICLE DOI: 10.1038/s41467-018-03996-1 OPEN Dinosaur diversification linked with the Carnian Pluvial Episode Massimo Bernardi 1,2, Piero Gianolla 3, Fabio Massimo Petti 1,4, Paolo Mietto5 & Michael J. Benton 2 Dinosaurs diversified in two steps during the Triassic. They originated about 245 Ma, during the recovery from the Permian-Triassic mass extinction, and then remained insignificant until they exploded in diversity and ecological importance during the Late Triassic. Hitherto, this 1234567890():,; Late Triassic explosion was poorly constrained and poorly dated. Here we provide evidence that it followed the Carnian Pluvial Episode (CPE), dated to 234–232 Ma, a time when climates switched from arid to humid and back to arid again. Our evidence comes from a combined analysis of skeletal evidence and footprint occurrences, and especially from the exquisitely dated ichnofaunas of the Italian Dolomites. These provide evidence of tetrapod faunal compositions through the Carnian and Norian, and show that dinosaur footprints appear exactly at the time of the CPE. We argue then that dinosaurs diversified explosively in the mid Carnian, at a time of major climate and floral change and the extinction of key herbivores, which the dinosaurs opportunistically replaced. 1 MUSE—Museo delle Scienze, Corso del Lavoro e della Scienza 3, 38122 Trento, Italy. 2 School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK. 3 Dipartimento di Fisica e Scienze della Terra, Università di Ferrara, via Saragat 1, 44100 Ferrara, Italy. 4 PaleoFactory, Dipartimento di Scienze della Terra, Sapienza Università di Roma, Piazzale Aldo Moro, 5, 00185 Rome, Italy. 5 Dipartimento di Geoscienze, Universitàdegli studi di Padova, via Gradenigo 6, I-35131 Padova, Italy. -
Fossil Perspectives on the Evolution of Insect Diversity
FOSSIL PERSPECTIVES ON THE EVOLUTION OF INSECT DIVERSITY Thesis submitted by David B Nicholson For examination for the degree of PhD University of York Department of Biology November 2012 1 Abstract A key contribution of palaeontology has been the elucidation of macroevolutionary patterns and processes through deep time, with fossils providing the only direct temporal evidence of how life has responded to a variety of forces. Thus, palaeontology may provide important information on the extinction crisis facing the biosphere today, and its likely consequences. Hexapods (insects and close relatives) comprise over 50% of described species. Explaining why this group dominates terrestrial biodiversity is a major challenge. In this thesis, I present a new dataset of hexapod fossil family ranges compiled from published literature up to the end of 2009. Between four and five hundred families have been added to the hexapod fossil record since previous compilations were published in the early 1990s. Despite this, the broad pattern of described richness through time depicted remains similar, with described richness increasing steadily through geological history and a shift in dominant taxa after the Palaeozoic. However, after detrending, described richness is not well correlated with the earlier datasets, indicating significant changes in shorter term patterns. Corrections for rock record and sampling effort change some of the patterns seen. The time series produced identify several features of the fossil record of insects as likely artefacts, such as high Carboniferous richness, a Cretaceous plateau, and a late Eocene jump in richness. Other features seem more robust, such as a Permian rise and peak, high turnover at the end of the Permian, and a late-Jurassic rise. -
Dinosaur Diversification Linked with the Carnian Pluvial Episode
Bernardi, M., Gianolla, P., Petti, F. M., Mietto, P., & Benton, M. J. (2018). Dinosaur diversification linked with the Carnian Pluvial Episode. Nature Communications, 9, [1499]. https://doi.org/10.1038/s41467-018-03996-1 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1038/s41467-018-03996-1 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 Nature at http://www.nature.com/articles/s41467-018-03996-1 . 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/ ARTICLE DOI: 10.1038/s41467-018-03996-1 OPEN Dinosaur diversification linked with the Carnian Pluvial Episode Massimo Bernardi 1,2, Piero Gianolla 3, Fabio Massimo Petti 1,4, Paolo Mietto5 & Michael J. Benton 2 Dinosaurs diversified in two steps during the Triassic. They originated about 245 Ma, during the recovery from the Permian-Triassic mass extinction, and then remained insignificant until they exploded in diversity and ecological importance during the Late Triassic. Hitherto, this 1234567890():,; Late Triassic explosion was poorly constrained and poorly dated. Here we provide evidence that it followed the Carnian Pluvial Episode (CPE), dated to 234–232 Ma, a time when climates switched from arid to humid and back to arid again. -
The Late Triassic Ischigualasto Formation at Cerro Las Lajas
www.nature.com/scientificreports OPEN The Late Triassic Ischigualasto Formation at Cerro Las Lajas (La Rioja, Argentina): fossil tetrapods, high‑resolution chronostratigraphy, and faunal correlations Julia B. Desojo1,2*, Lucas E. Fiorelli1,3, Martín D. Ezcurra1,4, Agustín G. Martinelli1,4, Jahandar Ramezani5, Átila. A. S. Da Rosa6, M. Belén von Baczko1,4, M. Jimena Trotteyn1,7, Felipe C. Montefeltro8, Miguel Ezpeleta1,9 & Max C. Langer10 Present knowledge of Late Triassic tetrapod evolution, including the rise of dinosaurs, relies heavily on the fossil‑rich continental deposits of South America, their precise depositional histories and correlations. We report on an extended succession of the Ischigualasto Formation exposed in the Hoyada del Cerro Las Lajas (La Rioja, Argentina), where more than 100 tetrapod fossils were newly collected, augmented by historical fnds such as the ornithosuchid Venaticosuchus rusconii and the putative ornithischian Pisanosaurus mertii. Detailed lithostratigraphy combined with high‑precision U–Pb geochronology from three intercalated tufs are used to construct a robust Bayesian age model for the formation, constraining its deposition between 230.2 ± 1.9 Ma and 221.4 ± 1.2 Ma, and its fossil-bearing interval to 229.20 + 0.11/− 0.15–226.85 + 1.45/− 2.01 Ma. The latter is divided into a lower Hyperodapedon and an upper Teyumbaita biozones, based on the ranges of the eponymous rhynchosaurs, allowing biostratigraphic correlations to elsewhere in the Ischigualasto‑Villa Unión Basin, as well as to the Paraná Basin in Brazil. The temporally calibrated Ischigualasto biostratigraphy suggests the persistence of rhynchosaur-dominated faunas into the earliest Norian. Our ca. 229 Ma age assignment to Pi. -
Invertebrate Trace Fossils from Triassic Continental Successions of San Juan Province, Argentina
Asociación Paleontológica Argentina. Publicación Especial 7 ISSN 0328-347X VII International Symposium on Mesozoic Terrestrial Ecosystems: 127-131. Buenos Aires, 30-6-2001 INVeRTebRate Trace fossils from Triassic continental successiONS of San Juan Province, Argentina J 2 3 Ricardo N. MELCHOR , Jorge F. GENISE and Mariano VERDE Abstract. This paper is the first report on invertebrate trace fossil assemblages from Marayes-El Carrizal and Ischigualasto-Villa Unión Basins (Triassic),San Juan Province, northwestern Argentina. The four an- alyzed lithostratigraphic units consist of three different fluvial systems (Carrizal, Ischigualasto, and Los Colorados Formations) and a lacustrine delta (Los Rastros Formation). The ichnofossil content of the Late Triassic Carrizal Formation (fluvial channels and shallow floodplain lakes) includes Taenidium barretti (Bradshaw), and Skolithos isp. The Los Rastros Formation (Middle Triassic) yielded a subaqueous ich- noassemblage that consist of Helminthopsis d. H. abeli Ksiazkiewicz, Skolithos d. S. verticalis (Hall), and Palaeophvcus isp. Floodplain facies of the Ischigualasto Formation (Late Triassic) contain Taenidium, Skolithos and laterally spreading root systems. Most trace fossils of the Los Colorados Formation (Late Triassic) come from sandy sheetflood facies -with two interbedded paleosols- and consist of Palaeophycus tubularis Hall, d. Skolithos isp. Taenidium barretti, and Cochlichnus isp, All alluvial successions contain Taenidium and Skolithos, and lack evidence for a fully terrestrial ichnofauna