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A Case for Verella/Eofusulina Discrimination
SPANISH J OURNAL OF P ALAEONTOLOGY Demarcation problem in fusuline classifi cation: A case for Verella/Eofusulina discrimination Katsumi UENO1,2* & Elisa VILLA 2 1 Department of Earth System Science, Fukuoka University, Fukuoka 814-0180, Japan; [email protected] 2 Departamento de Geología, Universidad de Oviedo, c/ Jesús Arias de Velasco, s/n, 33005 Oviedo, Spain; [email protected] * Corresponding author Ueno, K. & Villa, E. 2018. Demarcation problem in fusuline classifi cation: A case for Verella/Eofusulina discrimination. [Problemas en la clasifi cación de fusulinas: el ejemplo de la distinción entre Verella y Eofusulina ]. Spanish Journal of Palaeontology, 33 (1), 215-230. Manuscript received 4 December 2017 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 5 March 2018 ABSTRACT RESUMEN The eofusulinin genera Verella and Eofusulina formed an La evolución de Verella hacia Eofusulina presenta un gran important lineage among fusulines to defi ne the Bashkirian/ interés para caracterizar paleontológicamente el intervalo Moscovian transitional interval in the Pennsylvanian (Upper de transición entre los pisos Bashkiriense y Moscoviense Carboniferous) subsystem. We studied morphologies of (Pensilvánico/Carbonífero superior). En este trabajo hemos Verella transiens , a highly evolved form in the genus, and estudiado detalladamente la morfología de Verella transiens , the fi rst Eofusulina species from the Los Tornos section in especie avanzada de este género, en ejemplares procedentes the Cantabrian Zone of northern -
Carbonaceous and Siliceous Neoproterozoic Vase-Shaped Microfossils (Urucum Formation, Brazil) and the Question of Early Protistan Biomineralization
Journal of Paleontology, 91(3), 2017, p. 393–406. Copyright © 2017, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2017.16 Carbonaceous and siliceous Neoproterozoic vase-shaped microfossils (Urucum Formation, Brazil) and the question of early protistan biomineralization Luana Morais,1 Thomas Rich Fairchild,2 Daniel J.G. Lahr,3 Isaac D. Rudnitzki,4,5 J. William Schopf,6,7,8,9 Amanda K. Garcia,6,7 Anatoliy B. Kudryavtsev,6,7 and Guilherme R. Romero1 1Graduate program in Geochemistry and Geotectonics, Institute of Geosciences, University of São Paulo. Rua do Lago, 562, Cidade Universitaria, CEP: 05508-080, São Paulo, Brazil 〈[email protected]〉, 〈[email protected]〉 2Department of Sedimentary and Environmental Geology, Institute of Geosciences, University of São Paulo, Rua do Lago, 562, Cidade Universitária, CEP: 05508-080, São Paulo, Brazil 〈[email protected]〉 3Department of Zoology, Institute of Biosciences, University of São Paulo, Rua do Matão, travessa 14, 101, Cidade Universitária, CEP: 05508-090, São Paulo, Brazil 〈[email protected]〉 4Departament of Geophysics, Institute of Astronomy, Geophysics and Atmospheric Sciences, University of São Paulo, Rua do Matão, 1226, CEP: 05508-900 São Paulo, Brazil 〈[email protected]〉 5Federal University of Ouro Preto, Department of Geology, Ouro Preto, Rua Diogo de Vasconcelos, 122, Minas Gerais, CEP: 35400-000 6Department of Earth, Planetary, and Space Sciences, 595 Charles E. -
University of Texas at Arlington Dissertation Template
MICROFAUNAL ASSEMBLAGES OF THE PLACID SHALE (MISSOURIAN, UPPER PENNSYLVANIAN), BRAZOS RIVER VALLEY, NORTH-CENTRAL TEXAS by BRITTANY E. MEAGHER Presented to the Faculty of the Graduate School of The University of Texas at Arlington in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE IN GEOLOGY THE UNIVERSITY OF TEXAS AT ARLINGTON August 2012 Copyright © by Brittany Meagher 2012 All Rights Reserved DEDICATION I would like to dedicate this thesis to my granddad Pope Meagher who as a geologist instilled in me, at a young age, my love for rocks. I don’t believe I would have gotten as far without this early love he planted and nurtured to grow within me. ACKNOWLEDGEMENTS There are many people that I would like to thank for their guidance and patience throughout this thesis project. Without these people, this thesis would not have been possible. I would like to thank Dr. Merlynd Nestell, Committee Chairman, for suggesting this project to me. His advice and assistance throughout this research project has helped me learn as much as possible about various types of microfauna. His review and editing of this manuscript is greatly appreciated. Dr. Galina Nestell, thesis committee member, for teaching me exactly what goes into taxonomically describing a microfossil. Her expertise on the identification of foraminifers contributed to the completion of this thesis. Dr. John Wickham, thesis committee member, for his guiding and teaching me various topics throughout my time at University of Texas Arlington. His time, in both reviewing this manuscript and serving on my committee, is invaluable and greatly appreciated. -
Carbonaceous and Siliceous Neoproterozoic Vase-Shaped Microfossils (Urucum Formation, Brazil) and the Question of Early Protistan Biomineralization
Journal of Paleontology, 91(3), 2017, p. 393–406. Copyright © 2017, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2017.16 Carbonaceous and siliceous Neoproterozoic vase-shaped microfossils (Urucum Formation, Brazil) and the question of early protistan biomineralization Luana Morais,1 Thomas Rich Fairchild,2 Daniel J.G. Lahr,3 Isaac D. Rudnitzki,4,5 J. William Schopf,6,7,8,9 Amanda K. Garcia,6,7 Anatoliy B. Kudryavtsev,6,7 and Guilherme R. Romero1 1Graduate program in Geochemistry and Geotectonics, Institute of Geosciences, University of São Paulo. Rua do Lago, 562, Cidade Universitaria, CEP: 05508-080, São Paulo, Brazil 〈[email protected]〉, 〈[email protected]〉 2Department of Sedimentary and Environmental Geology, Institute of Geosciences, University of São Paulo, Rua do Lago, 562, Cidade Universitária, CEP: 05508-080, São Paulo, Brazil 〈[email protected]〉 3Department of Zoology, Institute of Biosciences, University of São Paulo, Rua do Matão, travessa 14, 101, Cidade Universitária, CEP: 05508-090, São Paulo, Brazil 〈[email protected]〉 4Departament of Geophysics, Institute of Astronomy, Geophysics and Atmospheric Sciences, University of São Paulo, Rua do Matão, 1226, CEP: 05508-900 São Paulo, Brazil 〈[email protected]〉 5Federal University of Ouro Preto, Department of Geology, Ouro Preto, Rua Diogo de Vasconcelos, 122, Minas Gerais, CEP: 35400-000 6Department of Earth, Planetary, and Space Sciences, 595 Charles E. -
New Permian Radiolarians from East Asia and The
www.nature.com/scientificreports OPEN New Permian radiolarians from east Asia and the quantitative reconstruction of their evolutionary and ecological signifcances Yifan Xiao1*, Noritoshi Suzuki2, Tsuyoshi Ito3 & Weihong He1 The biostratigraphically important Permian radiolarian genera Pseudoalbaillella sensu stricto and Follicucullus (Follicucullidae, Polycystinea) are discriminated by morphological gaps in their wings and segmentation. Previous statistical analyses demonstrated that Longtanella flls morphological gaps between these two genera. Longtanella has long been regarded as a junior synonym of Parafollicucullus, and only a few species have been described. Herein several true Longtanella species are recognized from South China, and eight new species and fve indeterminate species are described and illustrated to prove the validity of the genus Longtanella. In addition, a new genus, Parafollicucullinoides gen. nov., is described. Their palaeogeographic distributions and living environments are explored by applying correspondence analysis (CA), with occurrence datasets of selected fusulinacean genera from the Japanese Islands, China and Sundaland. CA results indicate that Longtanella was present to a limited extent in warmer conditions in the fusulinacean Province B and C during Kungurian–Roadian time, and possibly lived above the thermocline and below the deepest limit of fusulinaceans. The Pseudoalbaillella and the Follicucullus group preferred open ocean conditions, living below the thermocline and distributed not only in the ‘Equatorial Warm Water Province’, but also the northern peri-Gondwana Cool Water Province and the southern North Cool Water Province. Te radiolarian order Albaillellaria is of particular importance because it includes index fossils for the Upper Devonian to the end-Permian1. Albaillellarians are characterized by poreless coverage with an internal bony triangular frame made of three intersecting rods and they are precisely identifable at the species level thanks to rapid evolution. -
Carboniferous and Permian Fusulinids from Fukuji, Central Japan
Title Carboniferous and Permian Fusulinids from Fukuji, Central Japan Author(s) Niikawa, Isao Citation 北海道大学理学部紀要, 18(4), 533-610 Issue Date 1978-09 Doc URL http://hdl.handle.net/2115/36672 Type bulletin (article) File Information 18_4_p533-610.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP Jour. Fac. Sci., Hokkaido Univ., Ser. IV, vol. 18, no. 4, Sept., 1978, pp. 533-610 533 CARBONIFEROUS AND PERMIAN FUSULINIDS FROM FUKUJI,CENTRALJAPAN by Isao Niikawa (with 3 text·figures and 14 plates) (Co ntribution from the Department of Geology and Mineralogy, Faculty of Science, Hokkaido University, No. 1553) Abstract Altogether sixty species of fusulinids are described from the Carboniferous Ichinotani Formation and the Permian Mizuyagadani Formation, Fukuji, Gifu Prefecture, Central Japan. Of them six species are new. They are Pseudosta//eJla minaroi, P. subrotunda, FusulineJla rhomboidalis, Triticites katol, T. iehinotaniensis and T. elongatus. The following fusulind zones are established; Zone of Eosta//ella, Zone of Pro /usulinella, Lower Zone of FuslllineiJa-Fusulina, Zone of Beedeina, Upper Zone of Fusulinella-Fusulina, Zone of Tritieites, Zone of Pseudosch wagerina, and Zone of Pseudo /usulina. As a whole fusulinid s treated in this paper show similarity to those of China, Korea, and especially to those of the USSR. Lithologic sequence and fusulinid succession suggest that the fusulinid fauna in Fukuji ranges continuously from the Upper Visean to the Sakmarian, although evidence for Namurian, Vereyan , and Upper UraHan is not at all clear. Introduction Fukuji is a small hot spring spa, some 5 km west of an active volcano, Mt. Yake on the border between the Nagano and Gifu Prefecture, Central Japan. -
(Permian Fusulinacea) from Limestone Pebbles in the Dobaru Formation, the Lowest Part of the Lower Cretaceous Wakino Subgroup, in Kitakyushu City, Japan
Bull. Kitakyushu Mm. Nat. Hist., 20: 1-15, pis. 1-2. March 31, 2001 Neoschwagerina (Permian fusulinacea) from limestone pebbles in the Dobaru Formation, the lowest part of the Lower Cretaceous Wakino Subgroup, in Kitakyushu City, Japan Yasuhiro Ota Kitakyushu Museum and Institute of Natural History, 3-6-1, Nishihonmachi, Yahata-higashi-ku, Kitakyushu 805-0061,JAPAN (Received December 20, 2000) Abstract Well-preserved Neoschwagerina aff. cheni lisinghaiana Shung with Parafusulina sp. and Chusenella sp. was recovered from limestone pebbles within the basal conglom erate in the Dobaru Formation, the lowest part of the Lower Cretaceous Wakino Sub group, in Kitakyushu City,Japan. The conglomerate has also yielded well-preserved Parafusulina species: Parafusulhia cf. kaerimizensis (Ozawa), Parafusulina sp. A and Parafusulina sp. B (Ota, 2000). These occurrences support the interpretation that the provenance of this non-crystalline limestone was near the sedimentary basin of the Dobaru Formation in the Early Cretaceous time. These limestone pebbles with Neoschwagerina are considered to have been transported from limestone of the Neoschwagerina simplex Zone in the Tethyan region or with correlatives of Middle Per mian age. Introduction Well-preserved fusulinaceans have recently been found in the basal conglomer ate within the Dobaru Formation, the lowest part of the Lower Cretaceous Wakino Subgroup, in Kitakyushu City (Ota, 2000). The conglomerate with fusulinaceans is highly significant for deciphering the provenance of the limestone in Kitakyushu City and for inferring the paleoenvironment and sedimentological environment of the Wakino Subgroup in the Early Cretaceous time. The PaleozoicYobuno Group (Ota et al, 1992; Nakae, 1998),one of the Carboniferous to Permian groups in the Akiyoshi Terrane, is widely distributed in Kitakyushu City.