Permophiles Issue #47 June 2006 EXECUTIVE NOTES Notes from the SPS Secretary IPC2006 Will Be Held Just After Editing This Issue
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Treatise on Invertebrate Paleontology
PART H, Revised BRACHIOPODA VOLUMES 2 & 3: Linguliformea, Craniiformea, and Rhynchonelliformea (part) ALWYN WILLIAMS, S. J. CARLSON, C. H. C. BRUNTON, L. E. HOLMER, L. E. POPOV, MICHAL MERGL, J. R. LAURIE, M. G. BASSETT, L. R. M. COCKS, RONG JIA-YU, S. S. LAZAREV, R. E. GRANT, P. R. RACHEBOEUF, JIN YU-GAN, B. R. WARDLAW, D. A. T. HARPER, A. D. WRIGHT, and MADIS RUBEL CONTENTS INFORMATION ON TREATISE VOLUMES ...................................................................................... x EDITORIAL PREFACE .............................................................................................................. xi STRATIGRAPHIC DIVISIONS .................................................................................................. xxiv COORDINATING AUTHOR'S PREFACE (Alwyn Williams) ........................................................ xxv BRACHIOPOD CLASSIFICATION (Alwyn Williams, Sandra J. Carlson, and C. Howard C. Brunton) .................................. 1 Historical Review .............................................................................................................. 1 Basis for Classification ....................................................................................................... 5 Methods.......................................................................................................................... 5 Genealogies ....................................................................................................................... 6 Recent Brachiopods ....................................................................................................... -
A Mixed Permian-Triassic Boundary Brachiopod Fauna from Guizhou Province, South China
Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 125(3): 609-630. November 2019 A MIXED PERMIAN-TRIASSIC BOUNDARY BRACHIOPOD FAUNA FROM GUIZHOU PROVINCE, SOUTH CHINA HUI-TING WU1, YANG ZHANG2* & YUAN-LIN SUN1 1School of Earth and Space Sciences, Peking University, Beijing, China. 2*Corresponding author. School of Earth Sciences & Resources, China University of Geosciences, Beijing, China. E-mail: [email protected] To cite this article: Wu H.-T., Zhang Y. & Sun Y.-L. (2019) - A mixed Permian-Triassic boundary brachiopod fauna from Guizhou Province, South China. Riv. It. Paleont. Strat. 125(3): 609-630. Keywords: brachiopod; Changhsingian; mixed facies; extinction; taxonomy. Abstract. Although many studies have been concerned with Changhsingian brachiopod faunas in South China, brachiopod faunas of the mixed nearshore clastic-carbonate facies have not been studied in detail. In this paper, a brachiopod fauna collected from the Changhsingian Wangjiazhai Formation and the Griesbachian Yelang Formation at the Liuzhi section (Guizhou Province, South China) is described. The Liuzhi section represents mixed clastic- carbonate facies and yields 30 species of 16 genera of brachiopod. Among the described and illustrated species, new morphological features of genera Peltichia, Prelissorhynchia and Spiriferellina are provided. Because of limited materials, four undetermined species instead of new species from these three genera are proposed. The Liuzhi brachiopod fauna from lower part of the Wangjiazhai Formation shares most genera with fauna of carbonate facies in South China, and the fauna from the upper part is similar to that from the Zhongzhai and Zhongying sections, representative shallow- water clastic facies sections in Guizhou Province. -
Permophiles Issue
Contents Notes from the SPS Secretary ...........................................................................................................................1 Shen Shuzhong Notes from the SPS Chair ..................................................................................................................................2 Charles M. Henderson Meeting Report: Report on the Continental Siena Meeting, Italy, September 2006.....................................3 G. Cassinis, A. Lazzarotto, P. Pittau Working Group Report: Short report on 2005-2006 activities of the non-marine – marine correlation work- ing group of SPS ..................................................................................................................................................5 J.W. Schneider Report of SPS Working Group on “Using Permian transitional biotas as gateways for global correlation”7 Guang R. Shi International Permian Time Scale ...................................................................................................................10 Voting Members of the SPS ............................................................................................................................. 11 Submission guideline for Issue 49 ....................................................................................................................12 Reports: Ostracods (Crustacea) from the Permian-Triassic boundary interval of South China (Huaying Mountains, eastern Sichuan Province): paleo-oxygenation significance .......................................................12 -
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This article was downloaded by: [Deakin University] On: 11 May 2009 Access details: Access Details: [subscription number 907852123] 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.informaworld.com/smpp/title~content=t770322720 New Lopingian (Late Permian) rugosochonetid species from Sichuan, South China Monica J. Campi a; Guang R. Shi a a School of Ecology and Environment, Deakin University, Burwood, Australia Online Publication Date: 01 January 2005 To cite this Article Campi, Monica J. and Shi, Guang R.(2005)'New Lopingian (Late Permian) rugosochonetid species from Sichuan, South China',Alcheringa: An Australasian Journal of Palaeontology,29:2,275 — 285 To link to this Article: DOI: 10.1080/03115510508619306 URL: http://dx.doi.org/10.1080/03115510508619306 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan or 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. -
Coevolution of Global Brachiopod Palaeobiogeography and Tectonopalaeogeography During the Carboniferous Ning Li1,2*, Cheng-Wen Wang1, Pu Zong3 and Yong-Qin Mao4
Li et al. Journal of Palaeogeography (2021) 10:18 https://doi.org/10.1186/s42501-021-00095-z Journal of Palaeogeography ORIGINAL ARTICLE Open Access Coevolution of global brachiopod palaeobiogeography and tectonopalaeogeography during the Carboniferous Ning Li1,2*, Cheng-Wen Wang1, Pu Zong3 and Yong-Qin Mao4 Abstract The global brachiopod palaeobiogeography of the Mississippian is divided into three realms, six regions, and eight provinces, while that of the Pennsylvanian is divided into three realms, six regions, and nine provinces. On this basis, we examined coevolutionary relationships between brachiopod palaeobiogeography and tectonopalaeogeography using a comparative approach spanning the Carboniferous. The appearance of the Boreal Realm in the Mississippian was closely related to movements of the northern plates into middle–high latitudes. From the Mississippian to the Pennsylvanian, the palaeobiogeography of Australia transitioned from the Tethys Realm to the Gondwana Realm, which is related to the southward movement of eastern Gondwana from middle to high southern latitudes. The transition of the Yukon–Pechora area from the Tethys Realm to the Boreal Realm was associated with the northward movement of Laurussia, whose northern margin entered middle–high northern latitudes then. The formation of the six palaeobiogeographic regions of Mississippian and Pennsylvanian brachiopods was directly related to “continental barriers”, which resulted in the geographical isolation of each region. The barriers resulted from the configurations of Siberia, Gondwana, and Laurussia, which supported the Boreal, Tethys, and Gondwana realms, respectively. During the late Late Devonian–Early Mississippian, the Rheic seaway closed and North America (from Laurussia) joined with South America and Africa (from Gondwana), such that the function of “continental barriers” was strengthened and the differentiation of eastern and western regions of the Tethys Realm became more distinct. -
A-Quantitative-Taxonomic-Review-Of-Fusichonetes-And-Tethyochonetes-Chonetidina
Journal of Paleontology, 91(6), 2017, p. 1296–1305 Copyright © 2017, The Paleontological Society 0022-3360/17/0088-0906 doi: 10.1017/jpa.2017.80 Taxonomic Note A quantitative taxonomic review of Fusichonetes and Tethyochonetes (Chonetidina, Brachiopoda) Hui-ting Wu,1,2 G. R. Shi,2 and Wei-hong He1,3 1School of Earth Sciences, China University of Geosciences, Wuhan 430074, China 2School of Life and Environmental Sciences, Deakin University, Melbourne Burwood Campus, 221 Burwood Highway, Burwood, Victoria 3125, Australia 〈[email protected]〉 3State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China 〈[email protected]〉 Abstract.—Two middle Permian (Capitanian) to Early Triassic (Griesbachian) rugosochonetidae brachiopod genera, Fusichonetes Liao in Zhao et al., 1981 and Tethyochonetes Chen et al., 2000, have been regarded as two distinct taxa and used as such for a wide range of discussions including biostratigraphy, paleoecology, paleobiogeography, and the Permian-Triassic boundary mass extinction. However, the supposed morphological distinctions between the two taxa are subtle at best and appear to represent two end members of a continuum of morphological variations. In this study, we applied a range of quantitative and analytical procedures (bivariate plots, Kolmogorov-Smirnov test, categorical principle component analysis, and cladistic analysis) to a dataset of 15 quantified morphological variables, integrating both key external and internal characters, measured from 141 specimens of all well-known Fusichonetes and Tethyochonetes in order to test whether or not these two genera could be distinguished in view of the chosen characters. The results indicate that these two genera are morphologically indistinguishable and that the species classification previously applied to these two genera appears to represent polyphyletic groupings within the genus Fusichonetes. -
Chronology of Chinese History
AppendixA 1257 Appendix A Chronology of Chinese History Xla Dynasty c. 2205 - c. 1766 B. C. Shang Dynasty c. 1766 - c. 1122 B. C. Zhou Dynasty c. 1122 - 249 B. C. Western Zhou c. 1122 - 771 B.C. Eastern Zhou 770 - 249 B. C. Spring Autumn and period 770 - 481 B.C. Warring States period 403 - 221 B.C. Qin Dynasty 221 - 207 B. C. Han Dynasty 202 B. C. - A. D. 220 Western Han 202 B.C. -AD. 9 Xin Dynasty A. D. 9-23 Eastern Han AD. 25 - 220 Three Kingdoms 220 - 280 Wei 220 - 265 Shu 221-265 Wu 222 - 280 Jin Dynasty 265 - 420 Western Jin 265 - 317 Eastern Jin 317 - 420 Southern and Northern Dynasties 420 - 589 Sui Dynasty 590 - 618 Tang Dynasty 618 - 906 Five Dynasties 907 - 960 Later Liang 907 - 923 Later Tang 923 - 936 Later Jin 936 - 947 Later Han 947 - 950 Later Zhou 951-960 Song Dynasty 960-1279 Northern Song 960-1126 Southern Song 1127-1279 Liao 970-1125 Western Xia 990-1227 Jin 1115-1234 Yuan Dynasty 1260-1368 Ming Dynasty 1368-1644 Cling Dynasty 1644-1911 Republic 1912-1949 People's Republic 1949- 1258 Appendix B Map of China C ot C x VV 00 aý 3 ýý, cý ýý=ý<<ý IAJ wcsNYý..®c ýC9 0 I Jz ýS txS yQ XZL ý'Tl '--} -E 0 JVvýc ý= ' S .. NrYäs Zw3!v )along R ?yJ L ` (Yana- 'ý. ý. wzX: 0. ý, {d Q Z lýý'? ý3-ýý`. e::. ý z 4: `ý" ý i kws ". 'a$`: ýltiCi, Ys'ýlt.^laS-' tý.. -
TREATISE on INVERTEBRATE Paleontology BRACHIOPODA
TREA T ISE ON INVER T EBRA T E PALEON T OLOGY Part H BRACHIO P ODA Revised Volume 6: Supplement ALWYN WILLIA ms , C. H. C. BRUNTON , and S. J. CARL S ON with FERNANDO ALVAREZ , A. D. AN S ELL , P. G. BA K ER , M. G. BA ss ETT , R. B. BLOD G ETT , A. J. BOUCOT , J. L. CARTER , L. R. M. COC ks , B. L. CO H EN , PAUL CO pp ER , G. B. CURRY , MA gg IE CU S AC K , A. S. DA G Y S , C. C. EM I G , A. B. GAWT H RO P , RÉ M Y GOURVENNEC , R. E. GRANT , D. A. T. HAR P ER , L. E. HOL M ER , HOU HON G -FEI , M. A. JA M E S , JIN YU-G AN , J. G. JO H N S ON , J. R. LAURIE , STANI S LAV LAZAREV , D. E. LEE , CAR S TEN LÜTER , SARA H MAC K AY , D. I. MAC KINNON , M. O. MANCEÑIDO , MIC H AL MER G L , E. F. OWEN , L. S. PEC K , L. E. PO P OV , P. R. RAC H E B OEUF , M. C. RH ODE S , J. R. RIC H ARD S ON , RON G JIA -YU , MADI S RU B EL , N. M. SAVA G E , T. N. SM IRNOVA , SUN DON G -LI , DERE K WALTON , BRUCE WARDLAW , and A. D. WRI gh T Prepared under Sponsorship of The Geological Society of America, Inc. The Paleontological Society SEPM (Society for Sedimentary Geology) The Palaeontographical Society The Palaeontological Association RAY M OND C. -
(Early Permian) from the Itararé Group, Paraná Basin (Brazil): a Paleobiogeographic W–E Trans-Gondwanan Marine Connection
Palaeogeography, Palaeoclimatology, Palaeoecology 449 (2016) 431–454 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Eurydesma–Lyonia fauna (Early Permian) from the Itararé group, Paraná Basin (Brazil): A paleobiogeographic W–E trans-Gondwanan marine connection Arturo César Taboada a,e, Jacqueline Peixoto Neves b,⁎, Luiz Carlos Weinschütz c, Maria Alejandra Pagani d,e, Marcello Guimarães Simões b a Centro de Investigaciones Esquel de Montaña y Estepa Patagónicas (CIEMEP), CONICET-UNPSJB, Roca 780, Esquel (U9200), Chubut, Argentina b Departamento de Zoologia, Instituto de Biociências, Universidade Estadual Paulista “Júlio Mesquita Filho” (UNESP), campus Botucatu, Distrito de Rubião Junior s/n, 18618-970 Botucatu, SP, Brazil c Universidade do Contestado, CENPALEO, Mafra, SC, Brazil d Museo Paleontológico Egidio Feruglio(MEF), Avenida Fontana n° 140, Trelew (U9100GYO), Chubut, Argentina e CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina article info abstract Article history: Here, the biocorrelation of the marine invertebrate assemblages of the post-glacial succession in the uppermost Received 14 September 2015 portion of the Late Paleozoic Itararé Group (Paraná Basin, Brazil) is for the first time firmly constrained with other Received in revised form 22 January 2016 well-dated Gondwanan faunas. The correlation and ages of these marine assemblages are among the main con- Accepted 9 February 2016 troversial issues related to Brazilian Gondwana geology. In total, 118 brachiopod specimens were analyzed, and Available online 23 February 2016 at least seven species were identified: Lyonia rochacamposi sp. nov., Langella imbituvensis (Oliveira),? Keywords: Streptorhynchus sp.,? Cyrtella sp., Tomiopsis sp. cf. T. harringtoni Archbold and Thomas, Quinquenella rionegrensis Itararé group (Oliveira) and Biconvexiella roxoi Oliveira. -
Peninsular Malaysia)
Geol. Mag. 140 (5), 2003, pp. 523–538. c 2003 Cambridge University Press 523 DOI: 10.1017/S0016756803007854 Printed in the United Kingdom Palaeobiogeographic implications of Middle Permian brachiopods from Johore (Peninsular Malaysia) MASATOSHI SONE*†,IAN METCALFE* & MOHD SHAFEEA LEMAN*‡ *Asia Centre, University of New England, Armidale, NSW 2351, Australia ‡School of Environmental Sciences and Natural Resources, Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor, Malaysia (Received 13 June 2002; accepted 24 March 2003) Abstract –Anew Middle Permian locality in northern Johore, Peninsular Malaysia, yields a small- sized, but compositionally unique, brachiopod fauna consisting of eight species: Pseudoleptodus sp., Caricula cf. salebrosa Grant, Neochonetes (Nongtaia) aff. arabicus (Hudson & Sudbury), Karavankina sp., Transennatia cf. insculpta (Grant), Hustedia sp., Orthothetina sp., and martiniid indet. The first four genera are new records for Malaysia; in particular, the rare taxa Pseudoleptodus and Caricula characterize the fauna. The brachiopods occur together with the ammonoid Agathiceras sp., the nautiloid Foordiceras?sp., bivalves, and crinoid stems. The locality belongs to the East Malaya terrane of the Cathaysian biotic region, but some affinities to species of the Sibumasu province are recognized. The Malaysian forms of Pseudoleptodus, Caricula and Transennatia are similar to those of the Ratburi Limestone (southern Thailand). A Roadian–early Wordian age is interpreted for the Johore fauna. The similarity of brachiopods reported here with those from the Ratburi Limestone suggests that there was species interchange or one-way migration between shallow waters of East Malaya and Sibumasu across the main Palaeo-Tethys. The Tethyan seaway between the two terranes must have been narrower than previously interpreted by some authors to allow such faunal traffic during the Roadian–Wordian time period. -
Abstract and Content In
1 PERMIAN AND TRIASSIC STRATIGRAPHY AND FOSSILS OF THE HIMALAYA IN NORTHERN NEPAL By J. B. WATERHOUSE Earthwise volume 6 2 ISBN 0-476-004180-7 Date of Publication March 31, 2004 Copyright J. B. Waterhouse Reproduction in full or in part, with acknowledgement, is authorized. Printed by Brackens, Oamaru 3 PREFACE This study focuses on Permian stratigraphy of the Manang district, north-central Nepal, and Carboniferous and Permian brachiopods significant from a regional Himalayan and world perspective. Fossiliferous Late Paleozoic rocks in the Manang district of north-central Nepal are exposed north of the Annapurna Range along the north side of the Marsyangdi valley from east of Braga settlement (11500ft, 3505m) to beyond Manang settlement (11650ft, 3551m), south of the peaks of Chulu (21672ft, 6630m and 20321ft, 6200m). The rocks persist westwards for 15km across Puchenpra Peak (16883ft, 4950m) and an unnamed peak at 17315ft, 5146m, along the north and west side of a huge glacial amphitheatre called Plateau of Lakes, and continue to Mesokanto Pass (16730ft, 5099m), then descend 5km along the Thini River valley to the Kali Gandaki River and the settlement of Jomson (8900ft, 2713m). Further west lies the region of Dolpo in northwest Nepal, where similar Permian-Triassic rocks are exposed north of the Dhaulagiri massif (Fuchs 1967, 1975, 1977, Waterhouse 1977, 1978). Overall these geological observations on Late Paleozoic and Early Mesozoic rocks and fossils extend over 160km, in a band 5-20km broad. General geological studies and maps of the Manang region by Bordet et al. (1975) and Fuchs et al. (1988) provide critical data on the regional setting, and Garzanti et al. -
Landscape Planning of Urban Lake Park in China a Case Study on Nanjing
Spatial Planning with an emphasis on Urban Design in China and Europe Tianci Yuan Spatial Planning with an emphasis on Urban Design in China and Europe Landscape Planning of Urban Lake Park in China A case study on Nanjing Author: Tianci Yuan Supervisor: Agneta Sundberg Tutor: Ana Mafalda Madureira Karlskrona, Sweden 1 Spatial Planning with an emphasis on Urban Design in China and Europe Tianci Yuan Table of contents Abstract………………………………………………………………………………4 Introduction………………………………………………………………………….5 Chapter 1 Background of Xuanwu Lake Park………………………………………10 1.1 History and culture in Xuanwu Lake Park……………………………………...10 1.2 Evolution of Nanjing city and Xuanwu Lake Park through times………….......11 1.3 Xuanwu Lake Park today……………………………………………………….14 1.4 Chapter summary………………………………………………………………..16 Chapter 2 Users and designers with human-nature connection……………………..17 2.1 Users’ and designers’ perception and association in design process………........17 2.2 Urban Design: Human – Nature Connection……………………………………20 2.3 Color guidelines………………………………………………………………….22 2.4 Historical-cultural landscape…………………………………………………….27 2.5 Chapter summary………………………………………………………………...28 Chapter 3 Analysis of Xuanwu Lake Park…………………………………………..30 3.1 The area outside Xuanwu Lake………………………………………………….30 3.2 The area inside Xuanwu Lake…………………………………………………...39 3.3 The questionnaire survey results---what do users tell the designers?...................51 3.4 Chapter summary………………………………………………………………..55 Chapter 4 Case study: New designer proposal for Xuanwu Lake Park (In separate