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CONODONTS of the MOJCZA LIMESTONE -.: Palaeontologia Polonica
CONODONTS OF THE MOJCZA LIMESTONE JERZY DZIK Dzik, J. 1994. Conodonts of the M6jcza Limestone. -In: J. Dzik, E. Olemp ska, and A. Pisera 1994. Ordovician carbonate platform ecosystem of the Holy Cross Moun tains. Palaeontologia Polonica 53, 43-128. The Ordovician organodetrital limestones and marls studied in outcrops at M6jcza and Miedzygorz, Holy Cross Mts, Poland, contains a record of the evolution of local conodont faunas from the latest Arenig (Early Kundan, Lenodus variabilis Zone) to the Ashgill (Amorphognathus ordovicicus Zone), with a single larger hiatus corre sponding to the subzones from Eop/acognathus pseudop/anu s to E. reclinatu s. The conodont fauna is Baltic in general appearance but cold water genera , like Sagitto dontina, Scabbardella, and Hamarodus, as well as those of Welsh or Chinese af finities, like Comp/exodus, Phragmodus, and Rhodesognathu s are dominant in par ticular parts of the section while others common in the Baltic region, like Periodon , Eop/acognathus, and Sca/pellodus are extremely rare. Most of the lineages continue to occur throughout most of the section enabling quantitative studies on their phyletic evolut ion. Apparatuses of sixty seven species of thirty six genera are described and illustrated. Phyletic evolution of Ba/toniodus, Amorphognathu s, Comp/exodus, and Pygodus is biometrically documented. Element s of apparatu ses are homolog ized and the standard notation system is applied to all of them. Acodontidae fam. n., Drepa nodus kie/censis sp. n., and D. santacrucensis sp. n. are proposed . Ke y w o r d s: conodonts, Ordovici an, evolut ion, taxonomy. Jerzy Dzik, Instytut Paleobiologii PAN, A/eja Zwirk i i Wigury 93, 02-089 Warszawa , Poland. -
Conodonts from El Paso Group
Contents ABSTRACT 5 GENUS DREPANOISTODUS 25 D. suberectus, subsp. A, n. subsp. 25 INTRODUCTION 5 GENUS HISTIODELLA 25 OBJECTIVES 5 H. donnae, n. sp. 25 PROCEDURES 5 GENUS JUANOGNATHUS 26 FIGURED SPECIMENS 6 J. hayesi, n. sp. 26 COMMENTS ON TAXONOMY 6 J. jaanussoni 26 PREVIOUS WORK 7 J. variabilis 27 FAUNAL EVALUATION 8 CORRELATION 9 J.? n. sp. 1 27 GENUS LOXODUS 27 SYSTEMATIC PALEONTOLOGY 10 L. bransoni s.f. 27 GENUS ACANTHODUS 10 GENUS MACERODUS 28 A. lineatus s.f. 10 dianae 28 A. uncinatus s.f. 10 GENUS MICROZARKODINA 28 A. sp. s.f. 10 M. ? cf. M. marathonensis 28 GENUS ACODUS 10 GENUS OELANDODUS 29 A. delicatus 10 O.cf. O.costatus 29 A. deltatus deltatus 12 O.cf. O.elongatus 29 A. oneotensis s.f. 12 GENUS OEPIKODUS 30 A.? russoi 13 O. communis 30 A. triangularis 13 O.? n. sp. 31 GENUS A. sp. A s.f. 14 OISTODUS 31 A. sp. indet. 14 O. forceps s.f. 31 GENUS ACONTIODUS 14 O. gracilis s.f. 32 A. iowensis s.f. 14 A. propinquus s.f. 14 O.cf. 0. inaequalis s.f. 32 O. n. sp. 32 A. aff. A. propinquus s.f. 14 A. staufferi s.f. 15 O. cf. 0. lanceolatus 33 GENUS CLAVOHAMULUS 15 O. ? lecheguillensis, n. sp. 33 C. densus s.f. 15 O. mehli s.f. 33 C. lemonei, n. sp. 15 O. cf. O. multicorrugatus 35 C. n. sp. A 16 O. cf. O. parallelus s.f. 35 O. cf. O. pseudoramis s.f. 35 GENUS CORDYLODUS 16 O. -
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This article was downloaded by: [Macquarie University] On: 10 November 2008 Access details: Access Details: [subscription number 778261146] 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 Middle Cambrian to Lower Ordovician faunas from the Chingiz Mountain Range, central Kazakhstan T.Ju. Tolmacheva a; K. E. Degtyarev a; J. Samuelsson a; L. E. Holmer a a A.P. Karpinskii, Russian Geological Research Institute, Sredny pr. 74, 199106 St. Petersburg, Russia Online Publication Date: 01 December 2008 To cite this Article Tolmacheva, T.Ju., Degtyarev, K. E., Samuelsson, J. and Holmer, L. E.(2008)'Middle Cambrian to Lower Ordovician faunas from the Chingiz Mountain Range, central Kazakhstan',Alcheringa: An Australasian Journal of Palaeontology,32:4,443 — 463 To link to this Article: DOI: 10.1080/03115510802418099 URL: http://dx.doi.org/10.1080/03115510802418099 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. -
Buletini I Shkencave Gjeologjike
BULETINI I SHKENCAVE GJEOLOGJIKE Vol. 1/2020 Viti 39 (56) i Botimit TIRANË 2020 Buletini i Shkencave Gjeologjike 1/2020 Buletin of Geological Sciences Buletini i Shkencave Gjeologjike 1/2020 Buletin of Geological Sciences BORDI EDITORIAL Dr. Arben Pambuku-Kryeredaktor Dr. Lavdie Moisiu-Sekretare Prof. Ass. Dr. Veip Gjoni-Anëtar Prof. Dr. Kujtim Onuzi-Anëtar Prof. Dr. Vilson Silo-Anëtar Prof. Dr. Irakli Prifti-Anëtar Prof. Ass. Dr. Agim Mësonjësi-Anëtar Ing. Elisa Prendi-Redaktore Përgjegjëse ISSN 0254-5276 Buletini i Shkencave Gjeologjike 1/2020 Buletin of Geological Sciences Disa konsiderata mbi ndërtimin gjeologjik të zonave tektonike Kru- ja dhe Jonike në jugun e Shqipërisë dhe veriun e Greqisë [Some considerations on the geological setting of Kruja and Ionian tectonic zones in southern Albania and northern Greece] Dhurata Ndreko, Shaqir Nazaj ................................................ 7 [21] Roli i prishjeve tektonike gjatësore e tërthore në brezin flishor të rajonit të Plashnikut, në kontrollin e trashësisë së depozitimeve [The role of longitudinal and transversal tectonic faults in the flysch belt of Plashnik region, controlling the deposit thickness] Arjol Lule, Shaqir Nazaj .......................................................... 35 [45] Modeli i mundshëm gjeotektonik i termetit të 26 nëntorit 2019 [Hypothetical geotectonic model of the November 26, 2019 earth- quake] Viktor Doda, Rakip Hysenaj, Donald Deda ............................ 55 [65] Përdorimi i metodave sizmike aktive dhe pasive për studimin e rrëshqitjeve në fshatin Bagoj [The use of active and passive seismic methods for the study of landslides in the Bagoj village] Erald Silo, Mentor Lamaj....................................................... 75 [85] “Revolucioni” konodontik ne stratigrafi [Conodontic “revolution” in stratigraphy] Selam Meço ........................................................................ 95 [123] Bul. Shk. Gjeol. (Nr. 1/2020) Ndreko Dh., Nazaj Sh. -
Author-Title Index
AUTHOR-TITLE INDEX A ___. Paleoecology of cyclic sediments of the lower Green River Formation, central Utah. 1969. 16(1):3- Ahlborn, R. C. Mesozoic-Cenozoic structural develop 95. ment of the Kern Mountains, eastern Nevada-western Utah. 1977. 24(2):117-131. ___ and J. K. Rigby. Studies for students no. 10: Ge ologic guide to Provo Canyon and Weber Canyon, Alexander, D. W. Petrology and petrography of the Bridal Veil Limestone Member of the Oquirrh Formation at central Wasatch Mountains, Utah. 1980. 27(3):1-33. Cascade Mountain, Utah. 1978. 25(3):11-26. ___. See Chamberlain, C. K. 1973. 20(1):79-94. Anderson, R. E. Quaternary tectonics along the inter ___. See George, S. E. 1985. 32(1):39-61. mountain seismic belt south of Provo, Utah. 1978. ___. See Johnson, B. T. 1984. 31(1):29-46. 25(1):1-10. ___. See Young, R. B. 1984. 31(1):187-211. Anderson, S. R. Stratigraphy and structure of the Sunset Bagshaw, L. H. Paleoecology of the lower Carmel Forma- Peak area near Brighton, Utah. 1974. 21(1):131-150. tion of the San Rafael Swell, Emery County, Utah. Anderson, T. C. Compound faceted spurs and recurrent 1977. 24(2):51-62. movement in the Wasatch fault zone, north central Bagshaw, R. L. Foraminiferal abundance related to bento Utah. 1977. 24(2):83-101. nitic ash beds in the Tununk Member of the Mancos Armstrong, R. M. Environmental geology of the Provo Shale (Cretaceous) in southeasternUtah. 1977. Orem area. 1975. 22(1):39-67. 24(2):33-49. -
Ordovician Turbidites and Black Shales of Bennett Island
Geological Magazine Ordovician turbidites and black shales of www.cambridge.org/geo Bennett Island (De Long Islands, Russian Arctic), and their significance for Arctic correlations and palaeogeography Original Article 1 1 2,3 Cite this article: Danukalova MK, Maria K. Danukalova , Alexander B. Kuzmichev , Nikolai V. Sennikov Kuzmichev AB, Sennikov NV, and and Tatiana Yu. Tolmacheva4 Tolmacheva TY (2020) Ordovician turbidites and black shales of Bennett Island (De Long 1 2 Islands, Russian Arctic), and their significance Geological Institute, Russian Academy of Sciences, Pyzhevsky lane 7, Moscow, 119017, Russia; Trofimuk Institute for Arctic correlations and palaeogeography. of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, Koptug ave. 3, Geological Magazine 157: 1207–1237. https:// Novosibirsk, 630090, Russia; 3Novosibirsk State University, Pirogov St. 2, Novosibirsk, 630090, Russia and doi.org/10.1017/S0016756819001341 4Karpinsky Russian Geological Research Institute, Sredny ave. 74, St. Petersburg, 199106, Russia Received: 23 January 2019 Revised: 7 October 2019 Abstract Accepted: 17 October 2019 Bennett Island stands alone in a remote part of the Arctic and information on its geology is First published online: 17 January 2020 essential to ascertain relations with other terranes in order to restore the early Palaeozoic Keywords: Arctic palaeogeography. Lower Palaeozoic sedimentary rocks throughout the island were stud- New Siberian Islands; Siberia; graptolites; ied thoroughly for the first time. The Ordovician section (> 1.1 km thick) comprises three units: conodonts; early Palaeozoic; depositional Tremadocian, lowest Floian black shale (130–140 m); Floian, lower Dapingian carbonate environments; palaeoreconstructions turbidite (> 250 m); and Dapingian, lower Darriwilian siliciclastic turbidite (> 730 m). -
Pander Society Newsletter
Pander Society Newsletter Compiled and edited by R. J. Aldridge, M. A. Purnell, and A. Thomas DEPARTMENT OF GEOLOGY UNIVERSITY OF LEICESTER LEICESTER LE1 7RH, UK Number 32 May 2000 http://www.le.ac.uk/geology/map2/pander/ INTRODUCTORY REMARKS ELCOME. We are pleased to welcome all Heinz Beckmann readers to the 2000 edition of the Pander Willi Ziegler writes: In 1999 Prof. Dr. Heinz Beckmann Society Newsletter. Last year we produced passed away at an age of nearly 80. He was a German the first Newsletter to be distributed conodontologist who started work on conodonts in 1948, Welectronically and, with just a few small glitches, the about 16 years after Hermann Schmidt had published his operation appears to have been a success. We will study on Westfalian assemblages. Beckmann completed continue to send hard copies to conodont workers who a dissertation at Marburg on Middle-Upper Devonian do not have access to the network or who request a massive limestones in Westfalia, where he discovered printed version, but we hope that issue 32 will continue conodonts in marly interlayers. He initially studied thin a smooth transition to exclusively electronic distribution. sections of Icriodus and Polygnathus, and while he was As can be seen in the reports listed in this Newsletter, scientific assistant at the University of Cologne he 1999 was another busy year for conodont specialists, became interested in the stratigraphic value of crowned by the Pander Society Meeting in Calgary. conodonts. He published several papers in the early 50s, Many thanks to the organizers, Charles Henderson, Mei his major contribution to conodontology being to Shilong and Godfrey Nowlan for their efforts in making emphasize sampling at small intervals in order to the meeting such a success. -
Conodonts from the Andes
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by CONICET Digital Publicación Especial Nº 13 ASOCIACIÓN PALEONTOLÓGICA ARGENTINA CONODONTS FROM THE ANDES Proceedings of the 3rd International Conodont Symposium & Regional Field Meeting of the IGCP project 591 Edited by Guillermo L. Albanesi and Gladys Ortega BUENOS AIRES 2013 CONODONTS FROM THE ANDES - Publicación Especial Nº 13 - Julio 2013 - PALEONTOLOGICAL NOTE MIDDLE ORDOVICIAN CONODONTS AND GRAPTOLITES AT LOS CAUQUENES RANGE, CENTRAL PRECORDILLERA OF SAN JUAN, ARGENTINA VOLDMAN, G. G.1, 2, ORTEGA, G 1 AND ALBANESI, G. L. 1, 2 1 CONICET-Museo de Paleontología, CIGEA, Facultad de Ciencias Exactas, Físicas y Naturales, Universidad Nacional de Córdoba, X5000JJC, Córdoba, Argentina; [email protected], [email protected], [email protected] 2 CICTERRA-CONICET, Córdoba, Argentina. Keywords: Conodonts. Graptolites. Biostratigraphy. Middle Ordovician. Precordillera. Argentina. THE Ordovician System is superbly represented in the Pre- stones and calcarenites (upper Sandbian). A hiatus covering the cordillera of western Argentina, at the Andean foothills. During highest Darriwilian and the lowest Sandbian is recorded be- the Middle Ordovician, an important paleogeographical re- tween the middle and upper members. arrangement of depocenters and source areas took place asso- The Los Azules Formation is arranged in small isolated out- ciated with the demise of the Eopaleozoic carbonate platform crops aligned in narrow elongated belts with meridian orienta- of the Precordillera. This critical interval is recorded in the basin tion. The best exposures of the Los Azules Formation are located through widespread deposition of black shales over the fossil- at the foothill of the Cerro Viejo, between 30º 11’ 40" and 30º iferous limestones of the San Juan Formation, punctuated by 15’ 30" S Latitude, and 68º 34’30" and 68º 35’20" W Longi- local deposition of olistostromes, debris flows, conglomerates, tude, uplifted by the Niquivil Thrust (e.g., Ortega et al., 2007). -
Biogeographic and Biostratigraphic Implications of the <I>Serratognathus Bilobatus</I> Fauna (Conodonta) from the Em
© The Authors, 2009. Journal compilation © Australian Museum, Sydney, 2009 Records of the Australian Museum (2009) Vol. 61: 1–30. ISSN 0067-1975 doi:10.3853/j.0067-1975.61.2009.1520 Biogeographic and Biostratigraphic Implications of the Serratognathus bilobatus Fauna (Conodonta) from the Emanuel Formation (Early Ordovician) of the Canning Basin, Western Australia YONG YI ZHEN 1* AND ROBE R T S. NICOLL 2 1 Australian Museum, 6 College Street, Sydney NSW 2010, Australia [email protected] 2 Research School of Earth Science, Australian National University, Canberra ACT 0200, Australia [email protected] AB S T R ACT . Discovery of Serratognathus bilobatus in the Early Ordovician Emanuel Formation of the Canning Basin, Western Australia, has regional biogeographic and biostratigraphic implications. Distribution of Serratognathus indicates a close biogeographic link between Australia and adjacent eastern Gondwanan plates and terranes during the latest Tremadocian to early Floian (Early Ordovician), and the formation of the so-called “Australasian Province”, a distinctive biogeographic entity that existed throughout most of the Ordovician. The S. bilobatus fauna from the Canning Basin is much more diverse in comparison with those assemblages bearing Serratognathus from coeval Chinese Lower Ordovician successions and probably represents an assemblage inhabiting relatively deeper water (mid-outer shelf) environments. The Canning Basin fauna contains many pandemic forms, and bridges the gap in the regional correlation of this widely -
ENGLISH - CHINESE English-Chinese-Pinyin Dictionary
ENGLISH - CHINESE English-Chinese-Pinyin Dictionary English Chinese Pinyin Group abdomen 腹节;腹 fù jié ; fù Radiolaria aboral 反口;反口面;反口的 fǎn kǒu ; fǎn kǒu miàn ; fǎn kǒu de Conodonta aboral 反口面 fǎn kǒu miàn Foraminifera aboral attachment scar 反口面附着痕 fǎn kǒu miàn fù zhuó hén Conodonta aboral edge 反口缘脊 fǎn kǒu yuán jǐ Conodonta aboral extension 反口(方)延伸 fǎn kǒu (fāng) yán shēn Conodonta aboral furrow 反口齿槽 fǎn kǒu chǐ cáo Conodonta aboral groove 反口齿沟 fǎn kǒu chǐ gōu Conodonta aboral margin 反口缘 fǎn kǒu yuán Conodonta aboral side 反口边;反口面 fǎn kǒu biān; fǎn kǒu miàn Conodonta aboral surface 反口面 fǎn kǒu miàn Conodonta aboral view 反口视 fǎn kǒu shì Conodonta Abrograptidae 娇笔石科 jiāo bǐ shí kē Graptolithina Acantharina 棘放射虫亚目 jǐ fàng shè chóng yà mù Radiolaria acanthine septum 刺隔壁 cì gé bì Coelenterata Acanthodus 棘刺 jǐ cì Conodonta Acanthograptidae 刺笔石科 cì bǐ shí kē Graptolithina Acanthophyllidae 针珊瑚科 zhēn shān hú kē Coelenterata acanthus 刺状堆积 cì zhuàng duī jī Foraminifera accessory aperture 辅助口孔 fǔ zhù kǒu kǒng Foraminifera accessory lobe 辅齿叶 fǔ chǐ yè Conodonta Acervulariidae 堆珊瑚科 duī shān hú kē Coelenterata acervuline 泡沫状的 pào mò zhuàng de Foraminifera Acervulinidae 堆房虫科 duī fáng chóng kē Foraminifera acetyl-cellulose 醋酸盐赛璐珞 cù suān yán sài lù luò Coelenterata Acnidaria 无刺胞亚门 wú cì bāo yà mén Coelenterata Acodina 小针锐刺 xiǎo zhēn ruì cì Conodonta Acodus 针锐齿刺 zhēn ruì chǐ cì Conodonta Acontiodus 矢齿刺 shǐ chǐ cì Conodonta acontium 枪丝 qiāng sī Coelenterata acraspedote medusae 无缘膜水母 wú yuán mó shuǐ mǔ Coelenterata Acrophyllinae 锥顶珊瑚亚科 zhuī dǐng shān hú yà -
Early Ordovician Conodonts from the Barrandian and Bohemian-Baltic Faunal Relationships
Acta Palacontologica Po lon ica Vo l. 28, N o. 3-4 p p. 327- 368; p ls , 1- 6 W a rsza w a 1983 .JER ZY DZIK EARL Y ORDOVICIANCONODONTS F ROM THE BARRA NDIAN AND BOHEMIAN-BALTICFAUN AL RELATION SHIPS DZIK. J .: Early Ordovician conodonts from the Barrandian and Bohemian-Baltic faunal relationships. Acta P a la eon tol ogica Polonica, 28, 3-4, 327-31;B, 1983 (issu e d 1984). The typical Baltic conodont Baltoniodus has been Identified in the Bohemian Early Ordovician K labavian and Sarkan stages. In the upper part of the Klabava Formation (locality s.vatostepanskv r y bnik near My to) Baltoniodus is associated with species of the genera Drepanoistodus, Sca lpel lodus and Drepanodus, which also occur in the Baltic a rea. This contrasts with dissimilarity , st r es sed b y many autnors., b etween Baltic and Bohemian faunas thought to belong to different pa le c zoogeographic provinces. A r ev iew of other groups of fossils indicates that migrations between these r egions in the Ea r ly Ordovician w ere not uncommon. Klabavian B. bohemicus sp. n , is morphologically intermediate b et w een Acodus de ltatus, B . crassulus, and B . triangularis sen su Lindstrom, 1971 and may be identical with the oldest populations of B . navis sensu Van Wamel, 1974. According to the interpretation presented of the evolutionary r el a ti on sh i ps of B . bohemicus s p. n ., the upper part of the Klabava Formation is correIa fed with the La torpian -Volkhovian bou n d a r y . -
Pander Society Newsletter
Pander Society Newsletter DEPARTMENT OF GEOLOGY UNIVERSITY OF LEICESTER LEICESTER LE1 7RH, UK Number 31 April 1999 http://www.le.ac.uk/geology/map2/pander/ INTRODUCTORY REMARKS elcome to the 1999 edition of the Pander potential for Great Basin Paleozoic and Triassic conodont Society Newsletter! This is the first biostratigraphy. However, at the conclusion of the first Newsletter to be distributed electronically, award period, we decided to divide the Great Basin although we are still sending hard copies to section. Ray was going to work on the Ordovician, while Wthose who do not have access to the network or who I was to work on the rest of the Paleozoic and Triassic. request a printed version. We hope this will mark a Why this strange division? transition to exclusively electronic distribution; this will The story of tonight's award and of the division of cut costs dramatically and will also allow us to update labor (and stratigraphy) that occurred more than 30 the Newsletter on a regular basis. If members of the years ago is directly related to three years of field work conodonting community have any comments to make on with Ray. 30 years ago there was limited motel space in this, the Chief Panderer would be pleased to hear from places like Eureka and Lund, Nevada, and Garrison, them. Utah, so we shared motel rooms, at least where there At the outset, I am delighted to have the opportunity was a motel. Now, there are two problems in sharing a to thank my predecessor, Ray Ethington, for all the work motel room with Ray.