Focus on Fossils Third - Fifth
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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. -
Meet the Gilded Lady 2 Mummies Now Open
Member Magazine Spring 2017 Vol. 42 No. 2 Mummies meet the gilded lady 2 mummies now open Seeing Inside Today, computerized inside of mummies, revealing CT scans of the Gilded Lady tomography (CT) scanning details about the person’s reveal that she was probably offers researchers glimpses age, appearance, and health. in her forties. They also suggest of mummified individuals “Scans like these are noninvasive, that she may have suffered like never before. By combining they’re repeatable, and they from tuberculosis, a common thousands of cross-sectioned can be done without damaging disease at the time. x-ray images, CT scans let the history that we’re trying researchers examine the to understand,” Thomas says. Mummy #30007, known as the Gilded Lady, is one of the most beautifully preserved mummies from The Field Museum’s collection, and one of 19 now on view in the special exhibition Mummies. For decades, keeping mummies like this one well preserved also meant severely limiting the ability of researchers to study them. The result is that little was known about the Gilded Lady beyond what could be gleaned from the mummy’s exterior, with its intricate linen bindings, gilded headdress, and painted facial features. Exterior details do offer some clues. The mummy dates from 30 BC–AD 395, a period when Egypt was a province of the Roman Empire. While the practice of mummification endured in Egypt, it was being transformed by Roman influences. Before the Roman era, for example, mummies had been placed in wooden coffins, while the Gilded Lady is preserved in only linen wrappings and cartonnage, a papier mâché-like material. -
Place Names Describing Fossils in Oral Traditions
Place names describing fossils in oral traditions ADRIENNE MAYOR Classics Department, Stanford University, Stanford CA 94305 (e-mail: [email protected]) Abstract: Folk explanations of notable geological features, including fossils, are found around the world. Observations of fossil exposures (bones, footprints, etc.) led to place names for rivers, mountains, valleys, mounds, caves, springs, tracks, and other geological and palaeonto- logical sites. Some names describe prehistoric remains and/or refer to traditional interpretations of fossils. This paper presents case studies of fossil-related place names in ancient and modern Europe and China, and Native American examples in Canada, the United States, and Mexico. Evidence for the earliest known fossil-related place names comes from ancient Greco-Roman and Chinese literature. The earliest documented fossil-related place name in the New World was preserved in a written text by the Spanish in the sixteenth century. In many instances, fossil geonames are purely descriptive; in others, however, the mythology about a specific fossil locality survives along with the name; in still other cases the geomythology is suggested by recorded traditions about similar palaeontological phenomena. The antiquity and continuity of some fossil-related place names shows that people had observed and speculated about miner- alized traces of extinct life forms long before modern scientific investigations. Traditional place names can reveal heretofore unknown geomyths as well as new geologically-important sites. Traditional folk names for geological features in the Named fossil sites in classical antiquity landscape commonly refer to mythological or and modern Greece legendary stories that accounted for them (Vitaliano 1973). Landmarks notable for conspicuous fossils Evidence for the practice of naming specific fossil have been named descriptively or mythologically locales can be found in classical antiquity. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Viruses and the Origin of Microbiome Selection and Immunity
The ISME Journal (2017) 11, 835–840 © 2017 International Society for Microbial Ecology All rights reserved 1751-7362/17 www.nature.com/ismej PERSPECTIVE Viruses and the origin of microbiome selection and immunity Steven D Quistad1,2,3, Juris A Grasis1, Jeremy J Barr1,4 and Forest L Rohwer1 1Department of Biology, San Diego State University, San Diego, CA, USA; 2Laboratoire de Colloïdes et Matériaux Divisés (LCMD), Institute of Chemistry, Biology, and Innovation, ESPCI ParisTech/CNRS UMR 8231/PSL Research University, Paris, France; 3Laboratoire de Colloïdes et Matériaux Divisés (LCMD), Institute of Chemistry, Biology, and Innovation, ESPCI ParisTech/CNRS UMR 8231/PSL Research University, Paris, France and 4School of Biological Sciences, Monash University, Clayton, Victoria 3800, Australia The last common metazoan ancestor (LCMA) emerged over half a billion years ago. These complex metazoans provided newly available niche space for viruses and microbes. Modern day contemporaries, such as cnidarians, suggest that the LCMA consisted of two cell layers: a basal endoderm and a mucus-secreting ectoderm, which formed a surface mucus layer (SML). Here we propose a model for the origin of metazoan immunity based on external and internal microbial selection mechanisms. In this model, the SML concentrated bacteria and their associated viruses (phage) through physical dynamics (that is, the slower flow fields near a diffusive boundary layer), which selected for mucin-binding capabilities. The concentration of phage within the SML provided the LCMA with an external microbial selective described by the bacteriophage adherence to mucus (BAM) model. In the BAM model, phage adhere to mucus protecting the metazoan host against invading, potentially pathogenic bacteria. -
Issue of the FOSSIL
Official Publication of The Fossils, The Historians of Amateur Journalism The Fossil Volume 116, No. 3, Whole No. 383 Sunnyvale, California April 2020 Fossil Profile My Ajay Mentors by Linda Donaldson FOSSIL EDITOR Dave Tribby has asked me to provide a the beginning of a long love affair. It was almost the few thoughts on my friends and mentors in the world last press I saw exit my door. of amateur journalism. Though I’m not active now, He also introduced me to ajayers in my hometown thanks mostly to vision problems that make it hard to of Portsmouth, Ohio: Karl X. Williams and Charlie read the bundles, I was fortunate Phillips. The two of them were to have had several good men happy to share or sell me some of tors. I am still a Fossil—it’s hard their treasure troves of type or to totally desert the realm. necessary equipment. Much has It started with the one and been written of Karl, a Lone only J. Hill Hamon, whom I met Scout young printer in the 1920s, as my Biology professor at AAPA founding father, and a Transylvania University in Lex Fossil. To this day I possess a pa ington, Kentucky in January of per cutter I bought from Katie, 1972. I didn’t start learning the Karl’s widow. I was employed printing part until a short term about five years as a rubber class in December of 1972. He set stamp maker by Karl’s daughter out lots of old type on the Bio Pam and soninlaw Gary. -
Raymond M. Alf Museum of Paleontology EDUCATOR's GUIDE
Raymond M. Alf Museum of Paleontology EDUCATOR’S GUIDE Dear Educator: This guide is recommended for educators of grades K-4 and is designed to help you prepare students for their Alf Museum visit, as well as to provide resources to enhance your classroom curriculum. This packet includes background information about the Alf Museum and the science of paleontology, a summary of our museum guidelines and what to expect, a pre-visit checklist, a series of content standard-aligned activities/exercises for classroom use before and/or after your visit, and a list of relevant terms and additional resources. Please complete and return the enclosed evaluation form to help us improve this guide to better serve your needs. Thank you! Paleontology: The Study of Ancient Life Paleontology is the study of ancient life. The history of past life on Earth is interpreted by scientists through the examination of fossils, the preserved remains of organisms which lived in the geologic past (more than 10,000 years ago). There are two main types of fossils: body fossils, the preserved remains of actual organisms (e.g. shells/hard parts, teeth, bones, leaves, etc.) and trace fossils, the preserved evidence of activity by organisms (e.g. footprints, burrows, fossil dung). Chances for fossil preservation are enhanced by (1) the presence of hard parts (since soft parts generally rot or are eaten, preventing preservation) and (2) rapid burial (preventing disturbance by bio- logical or physical actions). Many body fossils are skeletal remains (e.g. bones, teeth, shells, exoskel- etons). Most form when an animal or plant dies and then is buried by sediment (e.g. -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
The Carbon Cycle
The Carbon Cycle Overview of the Carbon Cycle The movement of carbon from one area to another is the basis for the carbon cycle. Carbon is important for all life on Earth. All living things are made up of carbon. Carbon is produced by both natural and human-made (anthropogenic) sources. Carbon Cycle Page 1 Nature’s Carbon Sources Carbon is found in the Carbon is found in the lithosphere Carbon is found in the Carbon is found in the atmosphere mostly as carbon in the form of carbonate rocks. biosphere stored in plants and hydrosphere dissolved in ocean dioxide. Animal and plant Carbonate rocks came from trees. Plants use carbon dioxide water and lakes. respiration place carbon into ancient marine plankton that sunk from the atmosphere to make the atmosphere. When you to the bottom of the ocean the building blocks of food Carbon is used by many exhale, you are placing carbon hundreds of millions of years ago during photosynthesis. organisms to produce shells. dioxide into the atmosphere. that were then exposed to heat Marine plants use cabon for and pressure. photosynthesis. The organic matter that is produced Carbon is also found in fossil fuels, becomes food in the aquatic such as petroleum (crude oil), coal, ecosystem. and natural gas. Carbon is also found in soil from dead and decaying animals and animal waste. Carbon Cycle Page 2 Natural Carbon Releases into the Atmosphere Carbon is released into the atmosphere from both natural and man-made causes. Here are examples to how nature places carbon into the atmosphere. -
Unit- V Paleobotany
18MBO21C-U5 PAPER – IV PLANT DIVERSITY - II (PTERIDOPHYTES, GYMNOSPERMS AND PALEOBOTANY) Unit- V Paleobotany Dr. A. SANKARAVADIVOO, Assistant Professor, Department of Botany Government Arts College(Autonomous), Coimbatore-641018. Mobile:9443704273 GEOLOGICAL TIME SCALE Fossilization The method by which fossils are formed is termed as fossilization. Optimal conditions for fossilization are that an organism is buried very soon after its death and in the absence of bacterial or fungal decay, that mineral-rich waters and sediments surround the site, and the immediate environment is cool and hypoxic. The root of the word fossil derives from the Latin verb ‘to dig’ (fodere). A fossil is the mineralized partial or complete form of an organism, or of an organism’s activity, that has been preserved as a cast, impression or mold. A fossil gives tangible, physical evidence of ancient life and has provided the basis of the theory of evolution in the absence of preserved soft tissues. A Pectinatites Mould of a bivalve ammonite, shell Preserved insect trapped in amber Fossil recod . The totality of fossils - their placement in fossiliferous, rock formations, sedimentary layers (strata) . Fossil record - important functions of the science of paleontology - vary in size . A fossil normally preserves only a portion of the deceased organism, bones and teeth of vertebrates, the chitinous or calcareous exoskeletons of invertebrates. The oldest human fossil, where human refers to Homo erectus, Homo ergaster, and Homo georgicus, was a set of five skulls found in Dmanisi in Georgia between 1999 and 2005. These date back to approximately 1.8 million years ago. The oldest fossil remains depict five different species of microbe, preserved in a 3.5-billion-year-old rock in Australia. -
The Mummy of All Dinosaurs Compare and Contrast Careful Work
Careful Work © Clipart.com Scientists are very careful when they © iClipart work on dinosaur presented by Science a-z a division of Learning A-Z fossils. They use bright The Mummy of All Dinosaurs lights and small tools. By Jane Sellman They use toothbrushes March 2008: Scientists have found the most to clean away dirt. complete dinosaur mummy ever. A dinosaur They do not want to © Louis Tremblay mummy is a kind of fossil. A fossil is a living hurt the fossils! It thing that died and turned into rock. A mummy takes a long time to Tyler Lyson, who found the dinosaur fossil has bones and skin or muscles. With this uncover a fossil. mummy, works on a fossil. mummy, even the insides turned into rock. Scientists are Compare and Contrast learning amazing things from this mummy. © National Geographic Television Art and Animation, © National Geographic Television Julius T. Csotonyi and 3D model by 422 South Julius T. Scientists have T. rex Hadrosaur learned that • Length: 40’ • Length: 36’ dinosaurs were • Speed: 20 mph • Speed: 28 mph © Louis Tremblay • Teeth: pointed for • Teeth: flat for even bigger than tearing meat chewing plants we thought! How else can you compare these two dinosaurs? See Mummy of All Dinos Tyler Lyson (on the right) uses a jackhammer © BigStockPhoto, Digital Studio on page 2 to remove rock from around fossils. © Learning A–Z, Inc. All rights reserved. 4 www.sciencea-z.com 1 Mummy of All Dinos Continued from page 1 Writing Prompt: There was a little space between each piece of How is this the mummy’s backbone. -
Mineralogy of Non-Silicified Fossil Wood
Article Mineralogy of Non-Silicified Fossil Wood George E. Mustoe Geology Department, Western Washington University, Bellingham, WA 98225, USA; [email protected]; Tel: +1-360-650-3582 Received: 21 December 2017; Accepted: 27 February 2018; Published: 3 March 2018 Abstract: The best-known and most-studied petrified wood specimens are those that are mineralized with polymorphs of silica: opal-A, opal-C, chalcedony, and quartz. Less familiar are fossil woods preserved with non-silica minerals. This report reviews discoveries of woods mineralized with calcium carbonate, calcium phosphate, various iron and copper minerals, manganese oxide, fluorite, barite, natrolite, and smectite clay. Regardless of composition, the processes of mineralization involve the same factors: availability of dissolved elements, pH, Eh, and burial temperature. Permeability of the wood and anatomical features also plays important roles in determining mineralization. When precipitation occurs in several episodes, fossil wood may have complex mineralogy. Keywords: fossil wood; mineralogy; paleobotany; permineralization 1. Introduction Non-silica minerals that cause wood petrifaction include calcite, apatite, iron pyrites, siderite, hematite, manganese oxide, various copper minerals, fluorite, barite, natrolite, and the chromium- rich smectite clay mineral, volkonskoite. This report provides a broad overview of woods fossilized with these minerals, describing specimens from world-wide locations comprising a diverse variety of mineral assemblages. Data from previously-undescribed fossil woods are also presented. The result is a paper that has a somewhat unconventional format, being a combination of literature review and original research. In an attempt for clarity, the information is organized based on mineral composition, rather than in the format of a hypothesis-driven research report.