Iop Newsletter 120
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
New Paleobotanical Data on the Portuguese Pennsylvanian (Douro Carboniferous Basin, NW Portugal)
Versão online: http://www.lneg.pt/iedt/unidades/16/paginas/26/30/185 Comunicações Geológicas (2014) 101, Especial I, 409-414 IX CNG/2º CoGePLiP, Porto 2014 ISSN: 0873-948X; e-ISSN: 1647-581X New paleobotanical data on the Portuguese Pennsylvanian (Douro Carboniferous Basin, NW Portugal) Novos dados paleobotânicos do Pensilvaniano português (Bacia Carbonífera do Douro, NW Portugal) P. Correia1*, Z. Šimůnek2, J. Pšenička3, A. A. Sá4,5, R. Domingos6, A. Carneiro7, D. Flores1,7 Artigo Curto Short Article © 2014 LNEG – Laboratório Nacional de Geologia e Energia IP Abstract: This paper describes nine new macrofloral taxa from 1. Introduction Douro Carboniferous Basin (lower Gzhelian) of Portugal. The plant assemblage is mainly composed by pteridophylls (Sphenopteriss The fossil flora of Carboniferous of Portugal is still little arberi Kidston, Sphenopteris fayoli Zeiller, Sphenopteris tenuis known. The new megafloral occurrences recently found in Schenk, Odontopteris schlotheimii Brongniart), sphenopsids the Upper Pennsylvanian strata of Douro Carboniferous (Annularia spicata Gutbier, Stellotheca robusta (Feistmantel) Basin (DCB) provide new and important data about Surange and Prakash, Calamostachys grandis Zeiller (Jongmans) and Calamostachys calathifera Sterzel) besides the gymnosperm paleobotanical richness and diversity of the Paleozoic Cordaites foliolatus Grand`Eury. The new data provide a better floras of Portugal offering more information to previous understating of the knowledge of Late Carboniferous floras of researches reported from diverse localities and by different Portugal, showing the high plant diversity of Gzhelian floras, when authors (e.g. Wenceslau de Lima, Bernardino António considerable changes in paleogeography and climate dynamics are Gomes, Carlos Ribeiro, Carríngton da Costa, Carlos evidenced in Euramerican floristic assemblages. -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
Fossil Mosses: What Do They Tell Us About Moss Evolution?
Bry. Div. Evo. 043 (1): 072–097 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.7 Fossil mosses: What do they tell us about moss evolution? MicHAEL S. IGNATOV1,2 & ELENA V. MASLOVA3 1 Tsitsin Main Botanical Garden of the Russian Academy of Sciences, Moscow, Russia 2 Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia 3 Belgorod State University, Pobedy Square, 85, Belgorod, 308015 Russia �[email protected], https://orcid.org/0000-0003-1520-042X * author for correspondence: �[email protected], https://orcid.org/0000-0001-6096-6315 Abstract The moss fossil records from the Paleozoic age to the Eocene epoch are reviewed and their putative relationships to extant moss groups discussed. The incomplete preservation and lack of key characters that could define the position of an ancient moss in modern classification remain the problem. Carboniferous records are still impossible to refer to any of the modern moss taxa. Numerous Permian protosphagnalean mosses possess traits that are absent in any extant group and they are therefore treated here as an extinct lineage, whose descendants, if any remain, cannot be recognized among contemporary taxa. Non-protosphagnalean Permian mosses were also fairly diverse, representing morphotypes comparable with Dicranidae and acrocarpous Bryidae, although unequivocal representatives of these subclasses are known only since Cretaceous and Jurassic. Even though Sphagnales is one of two oldest lineages separated from the main trunk of moss phylogenetic tree, it appears in fossil state regularly only since Late Cretaceous, ca. -
Two LITTLE KNOWN SPECIES of SPHENOPHYLLUM from the STEPHANIAN of SPAIN and FRANCE
Two LITTLE KNOWN SPECIES OF SPHENOPHYLLUM FROM THE STEPHANIAN OF SPAIN AND FRANCE ROBERT H. WAGNER Geology Department, University of Sheffield, England, U.K. ABSTRACT The impression species Sphenophyllum incisum 'Wagner is fully described for the first time. with due reference to intra-specific variation as shown by abundant mate• rial from a single locality in the Stephanian B of North-west Spain. The associated stro• bilus is also recorded. Sphenophyllum nageli Grand'Eury, a middle to late Canta• brian species, is redescribed from the type region in the Cevennes, southern France. Similar material is illustrated from Cantabrian and Stephanian A localities in North-west Spain. Brief comments are made on several other species of Sphenophyllum from the Stephanian of western Europe, and a range chart is provided. INTRODUCTION basis of a large collection of specimens from a single locality. Another little known species, Spheno• Doubingeris well overand twentyVetter (1954)years agopublishedsince phyllum nageli Grand'Eury, was actually ITa brief not~ on the various species of described in 1890, but hardly mentioned Sphenophyll1&m recorded from Stephanian afterwards. Doubinger and Vetter ignored strata. A monographic paper by Abbott it entirely in their synthesis of 1954, and (1958) filled in gaps with regard to the the species did not reappear in the literature American species; a brief note by Obrhel until 1970 when it Was mentioned again (1967) brought the description of Spheno• from the original type area, the Cevennes, phyllum nemejci Obrhel from the Stephanian by Bouroz, Gras and Wagner. The material of Bohemia; and recent work on the reported in that paper includes several Stephanian floras of Portugal and Spain well-preserved specimens which allow a has added several new species such as redescription of Sphenophyllum nageli Grand• Sphenophyllum guerreiroi Teixeira, Spheno• 'Eury, as provided in the present paper. -
Devonian Plant Fossils a Window Into the Past
EPPC 2018 Sponsors Academic Partners PROGRAM & ABSTRACTS ACKNOWLEDGMENTS Scientific Committee: Zhe-kun Zhou Angelica Feurdean Jenny McElwain, Chair Tao Su Walter Finsinger Fraser Mitchell Lutz Kunzmann Graciela Gil Romera Paddy Orr Lisa Boucher Lyudmila Shumilovskikh Geoffrey Clayton Elizabeth Wheeler Walter Finsinger Matthew Parkes Evelyn Kustatscher Eniko Magyari Colin Kelleher Niall W. Paterson Konstantinos Panagiotopoulos Benjamin Bomfleur Benjamin Dietre Convenors: Matthew Pound Fabienne Marret-Davies Marco Vecoli Ulrich Salzmann Havandanda Ombashi Charles Wellman Wolfram M. Kürschner Jiri Kvacek Reed Wicander Heather Pardoe Ruth Stockey Hartmut Jäger Christopher Cleal Dieter Uhl Ellen Stolle Jiri Kvacek Maria Barbacka José Bienvenido Diez Ferrer Borja Cascales-Miñana Hans Kerp Friðgeir Grímsson José B. Diez Patricia Ryberg Christa-Charlotte Hofmann Xin Wang Dimitrios Velitzelos Reinhard Zetter Charilaos Yiotis Peta Hayes Jean Nicolas Haas Joseph D. White Fraser Mitchell Benjamin Dietre Jennifer C. McElwain Jenny McElwain Marie-José Gaillard Paul Kenrick Furong Li Christine Strullu-Derrien Graphic and Website Design: Ralph Fyfe Chris Berry Peter Lang Irina Delusina Margaret E. Collinson Tiiu Koff Andrew C. Scott Linnean Society Award Selection Panel: Elena Severova Barry Lomax Wuu Kuang Soh Carla J. Harper Phillip Jardine Eamon haughey Michael Krings Daniela Festi Amanda Porter Gar Rothwell Keith Bennett Kamila Kwasniewska Cindy V. Looy William Fletcher Claire M. Belcher Alistair Seddon Conference Organization: Jonathan P. Wilson -
Ordovician Land Plants and Fungi from Douglas Dam, Tennessee
PROOF The Palaeobotanist 68(2019): 1–33 The Palaeobotanist 68(2019): xxx–xxx 0031–0174/2019 0031–0174/2019 Ordovician land plants and fungi from Douglas Dam, Tennessee GREGORY J. RETALLACK Department of Earth Sciences, University of Oregon, Eugene, OR 97403, USA. *Email: gregr@uoregon. edu (Received 09 September, 2019; revised version accepted 15 December, 2019) ABSTRACT The Palaeobotanist 68(1–2): Retallack GJ 2019. Ordovician land plants and fungi from Douglas Dam, Tennessee. The Palaeobotanist 68(1–2): xxx–xxx. 1–33. Ordovician land plants have long been suspected from indirect evidence of fossil spores, plant fragments, carbon isotopic studies, and paleosols, but now can be visualized from plant compressions in a Middle Ordovician (Darriwilian or 460 Ma) sinkhole at Douglas Dam, Tennessee, U. S. A. Five bryophyte clades and two fungal clades are represented: hornwort (Casterlorum crispum, new form genus and species), liverwort (Cestites mirabilis Caster & Brooks), balloonwort (Janegraya sibylla, new form genus and species), peat moss (Dollyphyton boucotii, new form genus and species), harsh moss (Edwardsiphyton ovatum, new form genus and species), endomycorrhiza (Palaeoglomus strotheri, new species) and lichen (Prototaxites honeggeri, new species). The Douglas Dam Lagerstätte is a benchmark assemblage of early plants and fungi on land. Ordovician plant diversity now supports the idea that life on land had increased terrestrial weathering to induce the Great Ordovician Biodiversification Event in the sea and latest Ordovician (Hirnantian) -
The Fossil Flora and Age of the Wamsutta Red Beds (Middle
Document generated on 10/01/2021 10:12 p.m. Atlantic Geology Journal of the Atlantic Geoscience Society Revue de la Société Géoscientifique de l'Atlantique The fossil flora and age of the Wamsutta red beds (Middle Pennsylvanian), Narragansett Basin, southeastern Massachusetts, USA and correlation with the Cumberland Group of the Maritime Provinces of Canada Paul C. Lyons and Robert G. Sproule Volume 54, 2018 Article abstract New collections of plant macrofossils provide a precise Middle Pennsylvanian URI: https://id.erudit.org/iderudit/1055420ar age for the lower Wamsutta Formation red beds of the Narragansett Basin, DOI: https://doi.org/10.4138/atlgeol.2018.011 southeastern Massachusetts, USA. The Wamsutta assemblage indicates strong correlation with the Cumberland Group of the Maritimes Provinces of Canada, See table of contents which was earlier considered to be of late Langsettian to early Duckmantian age. This correlation is supported by the presence in the Wamsutta Formation of the following plant-fossil species: Neuralethopteris schlehanii, Neuropteris Publisher(s) obliqua, Senftenbergia plumosa, Calamites suckowii, Annularia asteris, Annularia cf. microphylla,Asterophyllites charaeformis, Asterophyllites Atlantic Geoscience Society grandis, Asterophyllites lindleyanus, Sphenophyllum cuneifolium, and Sphenopteris valida. Moreover, the new fossil flora resembles the Middle ISSN Pennsylvanian florules of western Europe, such as the Laveineopteris loshii Subzone. The new flora is especially similar to those of the Iberian Peninsula, 0843-5561 (print) where there is a complete succession of Carboniferous macrofloral zones, and 1718-7885 (digital) this similarity confirms a late Langsettian or early Duckmantian age for the lower Wamsutta macroflora. The new collections of Wamsutta Formation Explore this journal plant fossils, along with a smaller existing collection, represent the oldest known macroflora in the Narragansett Basin. -
Answers to the Top 50 Questions About Genesis, Creation, and Noah's Flood
ANSWERS TO THE TOP 50 QUESTIONS ABOUT GENESIS, CREATION, AND NOAH’S FLOOD Daniel A. Biddle, Ph.D. Copyright © 2018 by Genesis Apologetics, Inc. E-mail: [email protected] www.genesisapologetics.com A 501(c)(3) ministry equipping youth pastors, parents, and students with Biblical answers for evolutionary teaching in public schools. The entire contents of this book (including videos) are available online: www.genesisapologetics.com/faqs Answers to the Top 50 Questions about Genesis, Creation, and Noah’s Flood by Daniel A. Biddle, Ph.D. Printed in the United States of America ISBN-13: 978-1727870305 ISBN-10: 1727870301 All rights reserved solely by the author. The author guarantees all contents are original and do not infringe upon the legal rights of any other person or work. No part of this book may be reproduced in any form without the permission of the author. The views expressed in this book are not necessarily those of the publisher. Scripture taken from the New King James Version®. Copyright © 1982 by Thomas Nelson. Used by permission. All rights reserved. Print Version November 2019 Dedication To my wife, Jenny, who supports me in this work. To my children Makaela, Alyssa, Matthew, and Amanda, and to your children and your children’s children for a hundred generations—this book is for all of you. We would like to acknowledge Answers in Genesis (www.answersingenesis.org), the Institute for Creation Research (www.icr.org), and Creation Ministries International (www.creation.com). Much of the content herein has been drawn from (and is meant to be in alignment with) these Biblical Creation ministries. -
Reappraisal of the Genus Dicroidium Gothan from the Triassic Sediments of India
The Palaeobotanist 63(2014): 137–155 0031–0174/2014 Reappraisal of the genus Dicroidium Gothan from the Triassic sediments of India PANKAJ K. PAL1*, AMIT K. GHOSH2, RATAN KAR2, R.S. SINGH2, MANOBIKA SARKAR1 AND RESHMI CHATTERJEE2 1Department of Botany, UGC Centre of Advanced Study, University of Burdwan, Burdwan–713 104, West Bengal, India. 2Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India. *Corresponding author: [email protected] (Received 28 August, 2014; revised version accepted 25 September, 2014) ABSTRACT Pal PK, Ghosh AK, Kar R, Singh RS, Sarkar M & Chatterjee R 2014. Reappraisal of the genus Dicroidium Gothan from the Triassic sediments of India. The Palaeobotanist 63(2): 137–155. The genus Dicroidium Gothan, belonging to Corystospermaceae, is characterised by pinnately compound leaves with proximally forked primary rachis. The genus was earlier included under the genus Thinnfeldia Ettingshausen. Dicroidium is the most consistent macrofloral element in the Triassic strata of Southern Hemisphere. The present reassessment deals with the morphotaxonomy and stratigraphic significance of the species of Dicroidium in India. A critical review of the literature reveals that the specimens of Dicroidium described so far from India require reassessment, because same morphotypes have often been placed under different species names and sometimes dissimilar elements have been assigned to the same species. In view of this, a thorough analysis of Indian Dicroidium was undertaken based on fresh collections along with the species described earlier by previous workers. The present reappraisal reveals that the genus in the Triassic of Peninsular India is represented by eight species. These are D. hughesii (Feistmantel) Lele, D. -
Millerocaulis Tekelili Sp. Nov., a New Species of Osmundalean Fern from the Aptian Cerro Negro Formation (Antarctica) Ezequiel I
This article was downloaded by: [INASP - Pakistan ] On: 28 July 2011, At: 10:58 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 Alcheringa: An Australasian Journal of Palaeontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/talc20 Millerocaulis tekelili sp. nov., a new species of osmundalean fern from the Aptian Cerro Negro Formation (Antarctica) Ezequiel I. Vera Available online: 27 Jul 2011 To cite this article: Ezequiel I. Vera (2011): Millerocaulis tekelili sp. nov., a new species of osmundalean fern from the Aptian Cerro Negro Formation (Antarctica), Alcheringa: An Australasian Journal of Palaeontology, DOI:10.1080/03115518.2011.576541 To link to this article: http://dx.doi.org/10.1080/03115518.2011.576541 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.tandfonline.com/page/terms-and-conditions This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan, sub-licensing, systematic supply or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. The accuracy of any instructions, formulae and drug doses should be independently verified with primary sources. The publisher shall not be liable for any loss, actions, claims, proceedings, demand or costs or damages whatsoever or howsoever caused arising directly or indirectly in connection with or arising out of the use of this material. -
Quantification of an Archaean to Recent Earth Expansion Process Using Global Geological and Geophysical Data Sets
Department of Applied Geology Quantification of an Archaean to Recent Earth Expansion Process Using Global Geological and Geophysical Data Sets James Maxlow This thesis is presented as part of the requirement for the award of the Doctor of Philosophy of Curtin University of Technology June 2001 i Abstract Global geological and geophysical data, while routinely used in conventional plate tectonic studies, has not been applied to models of an expanding Earth. Crustal reconstructions on Archaean to Recent models of an expanding Earth presented here are the first time that reconstructions have been extended back to the Archaean, and the first time that continental and oceanic geology has been utilised to constrain plate assemblage and palaeoradius of the Earth. A set of twenty four spherical models have been constructed, twenty three covering the Archaean to Recent and one projected to five million years into the future. Construction of these spherical models relies on the fundamental premise that crustal lithosphere is cumulative with time, and historical markers preserved in the oceanic and continental geology accurately constrain both palaeoradius and plate reconstruction from the Archaean to Recent. Post-Triassic reconstructions of oceanic lithosphere demonstrate a plate fit- together along each plate margin at better than 99% fit. During the Triassic, continents envelope the Earth as a complete continental shell at a reduced Earth radius, and marginal and epi-continental sedimentary basins merge to form a global network surrounding continental cratons and orogenic zones. Continental crust is reconstructed on Pre-Jurassic models using the primary crustal elements of cratons, orogens and basins, with expansion primarily manifested as crustal extension within an established network of epi-continental rifts, orogens and sedimentary basins. -
Subclase Equisetidae ¿Tienes Alguna Duda, Sugerencia O Corrección Acerca De Este Taxón? Envíanosla Y Con Gusto La Atenderemos
subclase Equisetidae ¿Tienes alguna duda, sugerencia o corrección acerca de este taxón? Envíanosla y con gusto la atenderemos. Ver todas las fotos etiquetadas con Equisetidae en Banco de Imagénes » Descripción de WIKIPEDIAES Ver en Wikipedia (español) → Ver Pteridophyta para una introducción a las plantas Equisetos vasculares sin semilla Rango temporal: Devónico-Holoceno PreЄ Є O S D C P T J K Pg N Los equisetos , llamados Equisetidae en la moderna clasificación de Christenhusz et al. 2011,[1] [2] [3] o también Equisetopsida o Equisetophyta, y en paleobotánica es más común Sphenopsida, son plantas vasculares afines a los helechos que aparecieron en el Devónico, pero que actualmente sobrevive únicamente el género Equisetum, si bien hay representantes de órdenes extintos que se verán en este artículo. Este grupo es monofilético, aun con sus representantes extintos, debido a su morfología distintiva. Son plantas pequeñas, aunque en el pasado una variedad de calamitácea alcanzó los 15 metros durante el pérmico.[4] Índice 1 Filogenia 1.1 Ecología y evolución 2 Taxonomía 2.1 Sinonimia Variedades de Equisetum 2.2 Sistema de Christenhusz et al. 2011 Taxonomía 2.3 Clasificación sensu Smith et al. 2006 2.4 Otras clasificaciones Reino: Plantae 3 Caracteres Viridiplantae 4 Véase también Streptophyta 5 Referencias Streptophytina 6 Bibliografía Embryophyta (sin rango) 7 Enlaces externos Tracheophyta Euphyllophyta Monilophyta Filogenia[editar] Equisetopsida o Sphenopsida Introducción teórica en Filogenia Clase: C.Agardh 1825 / Engler 1924 Equisetidae Los análisis moleculares y genéticos de filogenia solo Subclase: se pueden hacer sobre representantes vivientes, Warm. 1883 como circunscripto según Smith et al. (2006) (ver la Órdenes ficha), al menos Equisetales es monofilético (Pryer et Equisetales (DC.