Studies in the Glossopteris Flora of India- 18
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Prepared in Cooperation with the Lllinois State Museum, Springfield
Prepared in cooperation with the lllinois State Museum, Springfield Richard 1. Leary' and Hermann W. Pfefferkorn2 ABSTRACT The Spencer Farm Flora is a compression-impression flora of early Pennsylvanian age (Namurian B, or possibly Namurian C) from Brown County, west-central Illinois. The plant fossils occur in argillaceous siltstones and sand- stones of the Caseyville Formation that were deposited in a ravine eroded in Mississippian carbonate rocks. The plant-bearing beds are the oldest deposits of Pennsylva- nian age yet discovered in Illinois. They were formed be- fore extensive Pennsylvanian coal swamps developed. The flora consists of 29 species and a few prob- lematical forms. It represents an unusual biofacies, in which the generally rare genera Megalopteris, Lesleya, Palaeopteridium, and Lacoea are quite common. Noegger- athiales, which are seldom present in roof-shale floras, make up over 20 percent of the specimens. The Spencer Farm Flora is an extrabasinal (= "upland1') flora that was grow- ing on the calcareous soils in the vicinity of the ravine in which they were deposited. It is suggested here that the Noeggerathiales may belong to the Progymnosperms and that Noeggerathialian cones might be derived from Archaeopteris-like fructifica- tions. The cone genus Lacoea is intermediate between Noeggerathiostrobus and Discini tes in its morphology. Two new species, Lesleya cheimarosa and Rhodeop- teridi urn phillipsii , are described, and Gulpenia limbur- gensis is reported from North America for the first time. INTRODUCTION The Spencer Farm Flora (table 1) differs from other Pennsylvanian floras of the Illinois Basin. Many genera and species in the Spencer Farm Flora either have not been found elsewhere in the basin or are very l~uratorof Geology, Illinois State Museum, Springfield. -
Re-Evaluation of the Genus Rubidgea in the Lower Permian of the Paraná Basin, Brazil, and Its Biostratigraphic Consequence
Versão online: http://www.lneg.pt/iedt/unidades/16/paginas/26/30/185 Comunicações Geológicas (2014) 101, Especial I, 455-457 IX CNG/2º CoGePLiP, Porto 2014 ISSN: 0873-948X; e-ISSN: 1647-581X Re-evaluation of the genus Rubidgea in the Lower Permian of the Paraná Basin, Brazil, and its biostratigraphic consequence Reavaliação do género Rubidgea, no Pérmico Inferior da Bacia do Paraná, Brasil, e suas consequências bioestratigráficas R. Iannuzzi1*, G. P. Tybusch1 Artigo Curto Short Article © 2014 LNEG – Laboratório Nacional de Geologia e Energia IP Abstract: The plant megafossil specimens revised in this study came *Corresponding author / Autor correspondente: [email protected] from the outcrops located in the São Paulo and Rio Grande do Sul states and positioned stratigraphically on top of the Itararé Group 1. Introduction and/or base of the Rio Bonito (= Tietê) Formation, Lower Permian of the Paraná Basin. The study material comprises leaves fragments The record of the genus Rubidgea in Brazil was first preserved as impressions, previously included in the morphogenus mentioned by Cazzulo-Klepzig et al. (1980) for the Itararé Rubidgea because of their supposed gangamopterid venation pattern, Group of the Rio Grande do Sul state, and it is represented lacking anastomoses. However, re-evaluation of this material showed by a specimen classified as Rubidgea sp. Later, Rubidgea that these leaves bear at some degree, rare anastomoses along the lamina. Based on this observation, we proposed that these leaves obovata Maithy (1965) and Rubidgea lanceolatus Maithy should be transferred to the morphogenus Gangamopteris, which (1965) were illustrated and reported for the outcrops displays this type of venation. -
Sementes Do Gênero Samaropsis Goeppert No Permiano Inferior Da Bacia Do Paraná, Sul Do Brasil
Rev. bras. paleontol. 10(2):95-106, Maio/Agosto 2007 © 2007 by the Sociedade Brasileira de Paleontologia SEMENTES DO GÊNERO SAMAROPSIS GOEPPERT NO PERMIANO INFERIOR DA BACIA DO PARANÁ, SUL DO BRASIL JULIANE MARQUES DE SOUZA & ROBERTO IANNUZZI Departamento de Paleontologia e Estratigrafia, Instituto de Geociências, UFRGS, Cx. P. 15001, 91501-970, Porto Alegre, RS, Brasil. [email protected], [email protected] RESUMO – O afloramento Morro do Papaléo, localizado no município de Mariana Pimentel, Rio Grande do Sul, tem se mostrado uma importante fonte de sementes fósseis preservadas na forma de impressões, as quais são provenientes do Grupo Itararé e da Formação Rio Bonito, Permiano Inferior da bacia do Paraná. Neste estudo são descritos seis diferentes morfotipos para o gênero Samaropsis Goeppert que, possivelmente, correspondem a seis diferentes morfoespécies. Características como a largura da sarcotesta, a forma geral da semente e do nucelo e a textura de sua superfície permitiram a proposição de uma nova espécie, Samaropsis gigas nov. sp., e identificar a presença de Samaropsis kurtzii Leguizamón, S. aff. S. millaniana Oliveira & Pontes e S. aff. S. rigbyi Millan. Além disso, uns poucos espécimes foram classificados apenas a nível genérico, tendo sido designados como Samaropsis sp. 1 e Samaropsis sp. 2. Palavras-chave: Sementes fósseis, Grupo Itararé, Formação Rio Bonito, bacia do Paraná, Rio Grande do Sul. ABSTRACT – SEEDS OF THE GENUS SAMAROPSIS GOEPPERT IN THE LOWER PERMIAN OF THE PARANÁ BASIN, SOUTHERN BRAZIL. The Morro do Papaléo outcrop is located in Mariana Pimentel town, Rio Grande do Sul, and has been an important source of fossil seeds. -
Plant Fossils from the Ellsworth Mountains
of different lithology. In the absence of diagnostic paleontologic References evidence, this proposal can only be postulated. Finally, the Cretaceous/Tertiary contact may occur at some other, as yet undefined, horizon between the highest ammonite level in the uppermost Lopez de Bertodano Formation and the level of the first Paleocene silicoflagellates in the lowermost Askin, R.A. 1984. Palynological investigations of the James Ross Island Sobral Formation. This is based on the assumption that am- basin and Robertson Island, Antarctic Peninsula. Antarctic Journal of monites were restricted to the Cretaceous. The possibility that the U.S., 19(5), 6 - 7. ammonites may have survived into the Tertiary should not be Harwood, D.M. 1985. Personal communication. ignored, however. Huber, B.T., D.M. Harwood, and P.N. Webb. 1983. Upper Cretaceous microfossil biostratigraphy of Seymour Island, Antarctic Peninsula. Because of the absence of Tertiary indicator species between Antarctic Journal of the U.S., 18(5), 72 - 74. the glauconite bed of the upper Lopez de Bertodano Formation Huber, B.T., D.M. Harwood, and P.N. Webb. 1985. Distribution of micro- and the lower Sobral Formation, a zone of uncertainty, repre- fossils and diagenetic features associated with the Cretaceous - Tertiary senting 73 meters of section, is shown for the location of the boundary on Seymour Island, Antarctic Peninsula. (Unpublished ab- Cretaceous/Tertiary contact on Seymour Island (figure 1). It is stract.) Conference on Rare Events, International Geological Correla- hoped that examination of sample material collected during the tion Programme, Project 199, GWATT, Switzerland, May 20 - 22. 1985 field season will reveal age-diagnostic microfossils in this Macellari, CE., and W.J. -
08-Schneider Et Al. (Arthropleura).P65
Lucas et al., eds., 2010, Carb-Permian transition in Cañon del Cobre. New Mexico Museum of Natural History and Science Bulletin 49. 49 EURAMERICAN LATE PENNSYLVANIAN / EARLY PERMIAN ARTHROPLEURID/TETRAPOD ASSOCIATIONS – IMPLICATIONS FOR THE HABITAT AND PALEOBIOLOGY OF THE LARGEST TERRESTRIAL ARTHROPOD JÖRG W. SCHNEIDER1, SPENCER G. LUCAS2, RALF WERNEBURG3 AND RONNY RÖßLER4 1 TU Bergakademie Freiberg, Institut für Geologie, B.v.Cotta-Strasse 2, D-09596 Freiberg, Germany; 2 New Mexico Museum of Natural History and Science, 1801 Mountain Road N.W., Albuquerque, New Mexico 87104; 3 Naturhistorisches Museum Schloss Bertholdsburg, Burgstrasse 6, D-98553 Schleusingen, Germany; 4 Museum für Naturkunde, Moritzstrasse 20, D-09111 Chemnitz, Germany Abstract—The giant arthropod Arthropleura was a common member of the late Paleozoic continental biota of paleo-equatorial biomes for more than 35 million years, from the Early Carboniferous late Visean (FOD; Middle Mississippian, Asbian/Brigantian) up to the Early Permian lower Rotliegend (LOD = ?LAD; Asselian). In Upper Pennsylvanian red beds in Cañon del Cobre of northern New Mexico, trackways of Arthropleura are present in strata that also yield body fossils of the amphibian Eryops. We review the Arthropleura tracksite from Cañon del Cobre, New Mexico, as well as other tracksites of this animal and arthropleurid/eryopid associations in order to better interpret the paleoenvironmental preference and the paleobiology of Arthropleura. This review supports the conclusion that Arthropleura was well adapted to alluvial environments of ever wet humid to seasonally dry and semihumid climates. Preferred habitats of semi-adult and adult Arthropleura were open, vegetated, river landscapes. They co-occurred in these habitats with semi-aquatic eryopid amphibians and terrestrial pelycosaurs. -
A High-Latitude Gondwanan Lagerstätte
University of Birmingham A high-latitude Gondwanan lagerstätte : the Permian permineralised peat biota of the Prince Charles Mountains, Antarctica Slater, Ben J.; Mcloughlin, Stephen; Hilton, Jason DOI: 10.1016/j.gr.2014.01.004 License: Creative Commons: Attribution (CC BY) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Slater, BJ, Mcloughlin, S & Hilton, J 2014, 'A high-latitude Gondwanan lagerstätte : the Permian permineralised peat biota of the Prince Charles Mountains, Antarctica', Gondwana Research. https://doi.org/10.1016/j.gr.2014.01.004 Link to publication on Research at Birmingham portal Publisher Rights Statement: Eligibility for repository : checked 03/06/2014 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. -
Novas Evidências E Análise Quantitativa Das Interações Inseto-Planta No Permiano Inferior Da Bacia Do Paraná
UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS NOVAS EVIDÊNCIAS E ANÁLISE QUANTITATIVA DAS INTERAÇÕES INSETO-PLANTA NO PERMIANO INFERIOR DA BACIA DO PARANÁ ESTHER REGINA DE SOUZA PINHEIRO ORIENTADOR – Prof. Dr. Roberto Iannuzzi Porto Alegre - 2011 UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS NOVAS EVIDÊNCIAS E ANÁLISE QUANTITATIVA DAS INTERAÇÕES INSETO-PLANTA NO PERMIANO INFERIOR DA BACIA DO PARANÁ ESTHER REGINA DE SOUZA PINHEIRO ORIENTADOR – Prof. Dr. Roberto Iannuzzi BANCA EXAMINADORA Prof. Dr. Karen Adami-Rodrigues – Universidade Federal de Pelotas Prof. Dr. Rosemarie Rohn Davies– Universidade Estadual Paulista Prof. Dr. Tânia Lindner Dutra – Universidade do Vale do Rio dos Sinos Dissertação de Mestrado apresentada como requisito parcial para a obtenção do Título de Mestre em Geociências. Porto Alegre – 2011 Pinheiro, Esther Regina de Souza Novas evidências e análise quantitativa das interações inseto-planta no permiano inferior da Bacia do Paraná. / Esther Regina de Souza Pinheiro. - Porto Alegre : IGEO/UFRGS, 2010. [72 f.] il. Dissertação (Mestrado). - Universidade Federal do Rio Grande do Sul. Instituto de Geociências. Programa de Pós-Graduação em Geociências. Porto Alegre, RS - BR, 2010. Orientação: Prof. Dr. Roberto Iannuzzi 1. Herbivoria. 2. Análise multivariada. 3. Folhas glossopterídeas. 4. Folhas cordaitaleanas. 5. Bacia do Paraná. I. Título _____________________________ Catalogação na Publicação Biblioteca Geociências - UFRGS Miriam Alves CRB 10/1947 DEDICATÓRIA Dedico essa dissertação a pessoa que mais apoiou minha trajetória acadêmica. Me apresentou a ciência da forma mais bonita que ela pode ser. Foi muito mais que um amigo, muitas vezes um orientador. -
Early Permian Palaeofloras from Southern Brazilian Gondwana: a Palaeoclimatic Approach
Revista Brasileira de Geociências 30(3):486-490, setembro de 2000 EARLY PERMIAN PALAEOFLORAS FROM SOUTHERN BRAZILIAN GONDWANA: A PALAEOCLIMATIC APPROACH MARGOT GUERRA-SOMMER AND MIRIAM CAZZULO-KLEPZIG ABSTRACT In evaluating the parameters supplied by the taphofloras from different sedimentary facies in the Early Permian sedimentary sequences of the southern part of the Paraná basin, Brazil, it has become evident that the palaeofloristic evolution was related to palaeoecological and palaeoclimatic evolution. The homogeneous composition of Early Permian floral assemblages, which are characterized mainly by herbaceous to shrub-like plants considered to be relicts from the rigorous climate of an ice age (e.g. Botrychiopsis plantiana) suggest the persistence of the cold climate. The dominance of Rubidgea and Gangamopteris leaves with palmate venation associated with glossopterids with penate venation seems to indicate a gradual warming of climate. In roof-shales of coalbearing strata pinnate glossopterids related to Glossopteris are common, while Gangamopteris and Rubidgea (palmate forms) are poorly represented. The sudden enrichment of herbaceous articulates and filicoids fronds is characteristic of this stage and trunks of arborescents lycophytes become important elements. These antrocophilic paleofloras are characterized by typical elements of the "Glossopteris flora" associated to tree lycophytes and ferns communities. Therefore, the cool seasonal climate of Early Permian changed into the moist seasonal interval during the Artinskian-Kungurian. This climatic change was significant to the meso-hygrophitic to hygrophitic vegetation registered in roof-shale ferns of the Gondwana Southern Brazilian coalbearing strata. Keywords: roof-shale floras, Gondwana, Southern Brazil, Paraná basin, Glossopteris Flora INTRODUCTION The intracratonic Paraná basin, with a total area proposed by Milani et al. -
Notes on the Upper Paleozoic Plants of Central New Mexico Sidney R
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/33 Notes on the upper Paleozoic plants of central New Mexico Sidney R. Ash and William D. Tidwell, 1982, pp. 245-248 in: Albuquerque Country II, Wells, S. G.; Grambling, J. A.; Callender, J. F.; [eds.], New Mexico Geological Society 33rd Annual Fall Field Conference Guidebook, 370 p. This is one of many related papers that were included in the 1982 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
III Unit- GYMNOSPERMS )
CORE COURSE II PLANT BIODIVERSITY II ( III Unit- GYMNOSPERMS ) Unit III : A general account of the characteristic features of Gymnosperms. Origin of Gymnosperms. Classification of Gymnosperms (Sporne, 1965). General structure and interrelationships of Pteridospermales, Bennetittales, Pentoxylales and Cordaitales. 1. General account on characteristic features of Gymnosperms. The word “Gymnosperm” comes from the Greek words “gymnos”(naked) and “sperma”(seed), hence known as “Naked seeds.” Gymnosperms are the seed- producing plants, but unlike angiosperms, they produce seeds without fruits. These plants develop on the surface of scales or leaves, or at the end of stalks forming a cone-like structure. Gymnosperms belong to kingdom ‘Plantae‘ and sub-kingdom ‘Embryophyta’. The fossil evidence suggested that they originated during the Paleozoic era, about 390 million years ago. Basically, gymnosperms are plants in which the ovules are not enclosed within the ovary wall, unlike the angiosperms. It remains exposed before and after fertilisation, and before developing into a seed. The stem of gymnosperms can be branched or unbranched. The thick cuticle, needle-like leaves, and sunken stomata reduce the rate of water loss in these plants. The family of gymnosperms consist of conifers, the cycads, the gnetophytes, and the species of Gynkgophyta division and Ginkgo biloba. Following are the important characteristics of gymnosperms: 1. Habit: Gymnosperms are a small group of seed plants which are represented by only 900 living species.The living gymnosperms are woody, evergreen (except Larix Dr.P.PRABAKARAN Assist .Prof.Botany MRGAC Page 1 and a Taxodium) perennials grow as trees or shrubs. Tallest trees are Sequoia sempervirens (366ft) and S. -
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RESEARCH ARTICLES The paleoflora of Figueira in the context of the neopaleozoic of the Paraná Basin, Brazil Fresia Ricardi-Branco Institute of Geosciences University of Campinas UNICAMP Oscar Rösler Paleontologic Center CENPALEO University of Contestado UNC ABSTRACT This study involved the Paleoflora of the Figueira Region (City of Figueira, PR, Brazil), which is part of the Triunfo Member of the Rio Bonito Formation. The specimens were collected from the refuse in the mining fields of the Companhia Carbonífera do Cambuí. After the systematic study, it was found that the species belong to the lycopodiaceous group and to the coniferae group. In the lycopsids species it was possible to study the stem, microphyllous, and megaspores. Three vegetal communities were represented in a general form in the studied Paleoflora: a swamp community, composed mainly of Brasilodendron cf. B. pedroanum, a community found in the composed flooding plain, formed of glossopterids among others, and a community of more elevated or less frequently flooded terrains, dominated by conifers (example: Paranocladus dusenii). Based on the results it can be concluded that the studied Paleoflora had great similarity to the other Early Permian taphofloras found in Paraná State at the Triunfo Member of the Rio Bonito Formation. KEYWORDS Permian, Paraná Basin, Rio Bonito Formation, Glossopteris Flora Introduction fication shown in Santa Catarina State, by the ab- sence of the upper Member, called Siderópolis The Paraná Basin is a large Paleozoic-Mesozoic (Soares and Cava 1982). Inside the Triunfo or lower intracratonic basin that extends throughout Brazil, Member of the Rio Bonito Formation, in the Paraguay, Uruguay, and northeast of Argentina Figueira area, a coal seam was found where the stud- (Zalán et al. -
Glossopteris Flora Nova Abordagem Para O Estudo Das Paleofloras Utilizando Sistemas De Informação Geográfica Aplicada a Flora Glossopteris
DOI: 10.5327/Z23174889201400040011 ARTICLE New approach for the study of paleofloras using geographical information systems applied to Glossopteris Flora Nova abordagem para o estudo das paleofloras utilizando sistemas de informação geográfica aplicada a Flora Glossopteris Isabel Cortez Christiano-de-Souza1*, Fresia Ricardi-Branco1, Adalene Moreira Silva2, Linda Gentry El Dash3, Rafael Souza Faria1 ABSTRACT: This paper introduces a methodology which makes RESUMO: O presente artigo introduz a uma metodologia na qual será possible the visualization of the spatial distribution of plant fossils possível a visualização da distribuição espacial de fitofósseis. Tal metod- and applies it to the occurrences of the Gondwana Floristic Province ologia será aplicada a ocorrências da Província Florística do Gondwana present on the eastern border of the Brazilian portion of the Paraná presente na borda leste da porção brasileira da Bacia do Paraná durante Basin during the Neopaleozoic. This province was chosen due to the o Neopaleozóico. Essa província foi escolhida tendo em vista que nela existence of a large number of publications referring to their occur- há grande número de publicações referentes às suas ocorrências. Isso tor- rence, so that a meta-analysis of their distribution could be based on na possível a meta-análise de sua distribuição, uma vez que há ampla ample information. The first step was the construction of a composite gama de informações. O primeiro passo foi a construção de uma base de database including geographical location, geology, and the botanical dados composta, incluindo localização geográfica, geologia e sistemática systematics of each relevant fossil. The geographical locations were botânica de cada fóssil de interesse.