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Available Generic Names for Trilobites
AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites. -
Embryophytic Sporophytes in the Rhynie and Windyfield Cherts
Transactions of the Royal Society of Edinburgh: Earth Sciences http://journals.cambridge.org/TRE Additional services for Transactions of the Royal Society of Edinburgh: Earth Sciences: Email alerts: Click here Subscriptions: Click here Commercial reprints: Click here Terms of use : Click here Embryophytic sporophytes in the Rhynie and Windyeld cherts Dianne Edwards Transactions of the Royal Society of Edinburgh: Earth Sciences / Volume 94 / Issue 04 / December 2003, pp 397 - 410 DOI: 10.1017/S0263593300000778, Published online: 26 July 2007 Link to this article: http://journals.cambridge.org/abstract_S0263593300000778 How to cite this article: Dianne Edwards (2003). Embryophytic sporophytes in the Rhynie and Windyeld cherts. Transactions of the Royal Society of Edinburgh: Earth Sciences, 94, pp 397-410 doi:10.1017/S0263593300000778 Request Permissions : Click here Downloaded from http://journals.cambridge.org/TRE, IP address: 131.251.254.13 on 25 Feb 2014 Transactions of the Royal Society of Edinburgh: Earth Sciences, 94, 397–410, 2004 (for 2003) Embryophytic sporophytes in the Rhynie and Windyfield cherts Dianne Edwards ABSTRACT: Brief descriptions and comments on relationships are given for the seven embryo- phytic sporophytes in the cherts at Rhynie, Aberdeenshire, Scotland. They are Rhynia gwynne- vaughanii Kidston & Lang, Aglaophyton major D. S. Edwards, Horneophyton lignieri Barghoorn & Darrah, Asteroxylon mackiei Kidston & Lang, Nothia aphylla Lyon ex Høeg, Trichopherophyton teuchansii Lyon & Edwards and Ventarura lyonii Powell, Edwards & Trewin. The superb preserva- tion of the silica permineralisations produced in the hot spring environment provides remarkable insights into the anatomy of early land plants which are not available from compression fossils and other modes of permineralisation. -
COSSMANNIANA Bulletin Du Groupe D'étude Et De Recherche Macrofaune Cénozoïque
COSSMANNIANA Bulletin du Groupe d'Étude et de Recherche Macrofaune Cénozoïque Tome 3, numéro 4 Décembre 1995 ISSN 1157-4402 GROUPE D'ÉTUDE ET DE RECHERCHE MACROFAUNE CÉNOZOïQUE "Maisonpour tous" 26, rue Gérard Philippe 94120 FONTENAY-SOUS-SOIS Président . .. ... Jacques PONS Secrétaire .. PierreLOZOUET Trésorier . .. .. Philippe MAESTRATI Dessins de couverture : Jacques LERENARD Maquette et Édition: Jacques LERENARD [eau-Michel PACAUD Couverture: Campanile (Campanilopa) giganteum, d'après la figure 137-45 de l'tconographie (grossissement 3/8); et individu bréphiqu e (hauteur totale : 2 mm), muni de son périostracum et de sa protoconque (coll. LeRenard) . COSSMANNIANA, Paris, 3 (4), Décembre 1995, pp. 133-150, sans fig. ISSN: 1157-4402 . RÉVISION DES MOLLUSQUES PALÉOGÈNES DU BASSIN DE PARIS III - CHRONOLOGIE DES CRÉATEURS DE RÉFÉRENCES PRIMAIRES par Jacques ·LERENARD Laboratoire de Biologiedes Invertébrés Marins et Malacologie, Muséum.National d'Histoire Naturelle, 55,rue de Buffon- 75005 Paris - FRANCE RÉSUMÉ - La liste des 437 publications dans lesquelles ont été introduites des références primaires figurant dans la partie II (LERENARD & PACAUD, 1995, pp. 65-132) est donnée. Il s'agit de la première liste de l'ensemble des publications concernant des nouveaux noms ou des nouvelles espèces paléogènes de Mollusques du bassin de Paris. TITLE - Revision of the Paris Basin Paleogene MoIlusca. III: Chronological Iist of the authors of primary references. ABSTRACT - The 437 publications, in which the primary references cited in part II (LERENARD & PACAUD, 1995, pp. 65-132) have been introduced, are given. This constitutes the first list of aIl the publications that are conceming new species or new names of Paris Basin Paleogene Molluscan species. -
Volume 144 Index
Index to Volume 144 INDEX TO VOLUME 144 This index provides coverage for both the Initial Reports and Scientific Results portions of Volume 144 of the Proceedings of the Ocean Drilling Program. Refer- ences to page numbers in the Initial Reports are preceded by “A” with a colon (A:), and to those in the Scientific Results (this book), by “B” with a colon (B:). In addi- tion, reference to material on CD-ROM is shown as “bp:CD-ROM.” The index was prepared by Earth Systems, under subcontract to the Ocean Drill- ing Program. The index contains two hierarchies of entries: (1) a main entry, defined as a keyword or concept followed by a reference to the page on which that word or concept appears, and (2) a subentry, defined as an elaboration on the main entry fol- lowed by a page reference. The index is presented in two parts: (1) a Subject Index and (2) a Taxonomic Index. Both parts cover text, figures, and tables but not core-description forms (“barrel sheets”), core photographs, smear-slide data, or thin-section descriptions; these are given in the Initial Reports. Also excluded from the index are biblio- graphic references, names of individuals, and routine front and back matter. The Subject Index follows a standard format. Geographic, geologic, and other terms are referenced only if they are subjects of discussion. This index also includes broad fossil groups such as nannofossils and radiolarians. A site chapter in the Ini- tial Reports is considered the principal reference for that site and is indicated on the first line of the site’s listing in the index. -
Applications of Calcareous Nannofossils and Stable Isotopes To
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2007 Applications of Calcareous Nannofossils and Stable Isotopes to Cenozoic Paleoceanography: Examples from the Eastern Equatorial Pacific, Western Equatorial Atlantic and Southern Indian Oceans Shijun Jiang Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] THE FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES APPLICATIONS OF CALCAREOUS NANNOFOSSILS AND STABLE ISOTOPES TO CENOZOIC PALEOCEANOGRAPHY: EXAMPLES FROM THE EASTERN EQUATORIAL PACIFIC, WESTERN EQUATORIAL ATLANTIC AND SOUTHERN INDIAN OCEANS By SHIJUN JIANG A dissertation submitted to the Department of Geological Sciences in partial fulfillment of the requirements for the degree of Doctor of Philosophy Degree Awarded: Fall Semester, 2007 The members of the Committee approve the Dissertation of Shijun Jiang defended on July 13, 2007. ____________________________________ Sherwood W. Wise, Jr. Professor Directing Dissertation ____________________________________ Richard L. Iverson Outside Committee Member ____________________________________ Anthony J. Arnold Committee Member ____________________________________ Joseph F. Donoghue Committee Member ____________________________________ Yang Wang Committee Member The Office of Graduate Studies has verified and approved the above named committee members. ii To Shuiqing and Jenny iii ACKNOWLEDGEMENTS First of all, I would like to thank my mentor Dr. Sherwood W. Wise, Jr., who constantly encouraged and supported me with his enthusiasm, reliance, guidance and, most of all, patience throughout my Ph.D adventure. He also opened a door into my knowledge of the paleo world, generously shared his time and his wealth of knowledge, patiently guided me through a western educational system totally different from my own background, and has successfully fostered my interest and enthusiasm in teaching. -
A Preliminary Assessment of Paleontological Resources at Bighorn Canyon National Recreation Area, Montana and Wyoming
A PRELIMINARY ASSESSMENT OF PALEONTOLOGICAL RESOURCES AT BIGHORN CANYON NATIONAL RECREATION AREA, MONTANA AND WYOMING Vincent L. Santucci1, David Hays2, James Staebler2 And Michael Milstein3 1National Park Service, P.O. Box 592, Kemmerer, WY 83101 2Bighorn Canyon National Recreation Area, P.O. Box 7458, Fort Smith, MT 59035 3P.O. Box 821, Cody, WY 82414 ____________________ ABSTRACT - Paleontological resources occur throughout the Paleozoic and Mesozoic formations exposed in Bighorn Canyon National Recreation Area. Isolated research on specific geologic units within Bighorn Canyon has yielded data on a wide diversity of fossil forms. A comprehensive paleonotological survey has not been previously undertaken at Bighorn Canyon. Preliminary paleontologic resource data is presented in this report as an effort to establish baseline data. ____________________ INTRODUCTION ighorn Canyon National Recreation Area (BICA) consists of approximately 120,000 acres within the Bighorn Mountains of north-central Wyoming and south-central Montana B (Figure 1). The northwestern trending Bighorn Mountains consist of over 9,000 feet of sedimentary rock. The predominantly marine and near shore sedimentary units range from the Cambrian through the Lower Cretaceous. Many of these formations are extremely fossiliferous. The Bighorn Mountains were uplifted during the Laramide Orogeny beginning approximately 70 million years ago. Large volumes of sediments, rich in early Tertiary paleontological resources, were deposited in the adjoining basins. This report provides a preliminary assessment of paleontological resources identified at Bighorn Canyon National Recreation Area. STRATIGRAPHY The stratigraphic record at Bighorn Canyon National Recreation Area extends from the Cambrian through the Cretaceous (Figure 2). The only time period during this interval that is not represented is the Silurian. -
The Texan Permian and Its Mesozoic Types of Fossils.. .1891
WHITE, C.A. ...The Texan Permian and its Mesozoic types of fossils.. .1891. I*- b37(245 ¥58 jj DEPARTMENT OP THE INTERIOR OF THK UNITED STATES GEOLOGICAL SURVEY No. 77 THE TEXAN PERMIAN AND ITS MESOZOIC TYPES OF FOSSILS WASHINGTON GOVERNMENT PRINTING OFFICE 1891 LIBRARY CATALOGUE SLIPS. United States, Department of the interior. (U. S. geological survey). Department of the interior |- | Bulletin | of the | United States | geological survey | mo. 77 | [Seal of the department] | Washington \ government printing office | 1891 Second title: United States geological survey | J. W. Powell, director | | The Texau Permian | and its | Mesozoio types of fossils | by | Charles A. White | [Vignette] | Washington | government printing office | 1891 8°. 5lpp. 4 pi. White (Charles A.). United States geological survey | J.W. Powell, director | The Texau Permian | audits | Mesozoic types of fossils | by | Charles A. White | [Vignette] | Washington | government printing office | 1891. 8«. 5t pp. 4 pi. [UNITED STATES. Department of the interior. (U. S. geological survey). Bulletin 77.] United States geological survey J. W. Powell, director | | The Texan Permian | and its | Mesozoic types of fossils | by | Charles A. White | [Vignette] | Washingto:a | government printing office | 1891 8". 5lpp. 4 pi. [UNITED STATES. Department <tf the interior. (U. S. geological survey). Bnlletin 77.] A.D'VBRTISEMKN'T. [Bulletin No. 77.] The publications of the United States Geological Survey are issued in accordance with the statute approved March 3, 1879, which declares that "Thepublicationsof tb.eGeological Survey shall consist of the annual report of operations, geological and economic maps illustrating the resources and classification of the lauds, and reports upon general and economic geology and paleontology. -
The Classification of Early Land Plants-Revisited*
The classification of early land plants-revisited* Harlan P. Banks Banks HP 1992. The c1assificalion of early land plams-revisiled. Palaeohotanist 41 36·50 Three suprageneric calegories applied 10 early land plams-Rhyniophylina, Zoslerophyllophytina, Trimerophytina-proposed by Banks in 1968 are reviewed and found 10 have slill some usefulness. Addilions 10 each are noted, some delelions are made, and some early planls lhal display fealures of more lhan one calegory are Sel aside as Aberram Genera. Key-words-Early land-plams, Rhyniophytina, Zoslerophyllophytina, Trimerophytina, Evolulion. of Plant Biology, Cornell University, Ithaca, New York-5908, U.S.A. 14853. Harlan P Banks, Section ~ ~ ~ <ltm ~ ~-~unR ~ qro ~ ~ ~ f~ 4~1~"llc"'111 ~-'J~f.f3il,!"~, 'i\'1f~()~~<1I'f'I~tl'1l ~ ~1~il~lqo;l~tl'1l, 1968 if ~ -mr lfim;j; <fr'f ~<nftm~~Fmr~%1 ~~ifmm~~-.mtl ~if-.t~m~fuit ciit'!'f.<nftmciit~%1 ~ ~ ~ -.m t ,P1T ~ ~~ lfiu ~ ~ -.t 3!ftrq; ~ ;j; <mol ~ <Rir t ;j; w -.m tl FIRST, may I express my gratitude to the Sahni, to survey briefly the fate of that Palaeobotanical Sociery for the honour it has done reclassification. Several caveats are necessary. I recall me in awarding its International Medal for 1988-89. discussing an intractable problem with the late great May I offer the Sociery sincere thanks for their James M. Schopf. His advice could help many consideration. aspiring young workers-"Survey what you have and Secondly, may I join in celebrating the work and write up that which you understand. The rest will the influence of Professor Birbal Sahni. The one time gradually fall into line." That is precisely what I did I met him was at a meeting where he was displaying in 1968. -
Ocean Drilling Program Scientific Results Volume
von Rad, U., Haq, B. U., et al., 1992 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 122 27. PALEONTOLOGICAL EVIDENCE FOR THE TRIASSIC AGE OF ROCKS DREDGED FROM THE NORTHERN EXMOUTH PLATEAU (TETHYAN FORAMINIFERS, ECHINODERMS, AND OSTRACODES)1 Edith Kristan-Tollmann2 and Franz Gramann3 ABSTRACT A very Late Triassic age can be proven by the microfaunal investigation of samples dredged from the northern Exmouth Plateau close to Ocean Drilling Program Site 764. The samples were previously regarded as Lower Jurassic sediments. The microfossils of known stratigraphic ranges show predominant Tethyan affinities. In samples dredged during Sonne cruise 8 (1979) from the northern slope of the Wombat Plateau, an Early Jurassic age is excluded by the presence of Frondicularia rhaetica, Berthelinella rhaetica, Fissobractites subsymmetrica, Ophioflabellum cristatum, Ophiacantha ? binitorulosa, Mostlerella n. sp., and Hasibuana asiatica. As a whole, a Rhaetian age is indicated. This age is also suggested by the foraminifers Coronipora austriaca and Variostoma sp., from determinations in limestone thin sections. Samples from Rig Seismic cruise 56 (1986), also from the northern slope of the Wombat Plateau, contain an assemblage of foraminifers known from the Triassic and observed in thin sections of carbonate rocks. They include Trocholina crassa, Trocholina laevis, Variostoma sp., and Variostoma coniforme. In combination with the lithofacies, the assemblage is characteristic for the Rhaetian Dachsteinkalk facies of the Northern Calcareous Alps of Austria. Thin sections from rocks dredged from Cygnet Canyon are rich in Glomospirella friedli and suggest a Norian to Rhaetian age. A thin section from the nearby Emu Escarpment contains sections of the Anomuran coprolite Octotriangulella septemtriangula Kristan-Tollmann, which is also present in upper Anisian rocks of Papua New Guinea. -
Sedimentology and Carbon Isotope Stratigraphy of the Rhaetian Hochalm Section (Late Triassic, Austria)
ORE Open Research Exeter TITLE Sedimentology and carbon isotope stratigraphy of the Rhaetian Hochalm section (Late Triassic, Austria) AUTHORS Rizzi, M; Thibault, N; Ullmann, CV; et al. JOURNAL Global and Planetary Change DEPOSITED IN ORE 21 May 2020 This version available at http://hdl.handle.net/10871/121120 COPYRIGHT AND REUSE Open Research Exeter makes this work available in accordance with publisher policies. A NOTE ON VERSIONS The version presented here may differ from the published version. If citing, you are advised to consult the published version for pagination, volume/issue and date of publication This is the author-formatted final version of Rizzi et al. (2020), Global and Planetary Change, accepted May 4th 2020, article 103210 https://doi.org/10.1016/j.gloplacha.2020.103210 1 Sedimentology and carbon isotope stratigraphy of the Rhaetian 2 Hochalm section (Late Triassic, Austria) 3 4 Małgorzata Rizzi1, Nicolas Thibault1, Clemens V. Ullmann1,2, Micha Ruhl1,3,4, Troels K. 5 Olsen1, Julien Moreau1, Marie-Emilie Clémence5, Wolfgang Mette5, Christoph Korte1 6 7 1 University of Copenhagen, Department of Geosciences and Natural Resource Management, 8 Øster Voldgade 10, 1350 København K, Denmark 9 2 Camborne School of Mines, College of Engineering, Mathematics and Physical Sciences, 10 University of Exeter, Penryn Campus, Penryn, Cornwall TR10 9FE, U.K. 11 3 University of Oxford, Department of Earth Sciences, South Parks Road, Oxford OX1 3AN, 12 U.K. 13 4 Department of Geology, Trinity College Dublin, The University of Dublin, College Green, 14 Dublin 2, Ireland. 15 5 Institute of Geology, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria 16 17 Keywords: Rhaetian, sedimentology, carbon isotopes, Upper Triassic This is the author-formatted final version of Rizzi et al. -
Upper Devonian Deposits At. G6rno in the Holy Cross M Ts
.: .......; ': aCla' :" geologlca polonica Vot 31. No. 3-4 . :; ... KRlZYBZTOF MALKOWSKJ Upper Devonian deposits at . G6rno In the Holy Cross M ts ..,' '1 · ' . -.. .. '. ; .. ~ ~ : , . .. AlBS'IlRA.OT: The lith010gy af the Upper lDevionian >oarobona'te deposits of the· -e:nvlTons off Gor.no, alo.ni· wiih .thed.r oonc.doni Stratigra,phy ga.ve a ibaSis ror reco gniti'On af the Sedimen'ta'i!ion and pa:leogeography ·of the lI'egtcm wJ.1ftun .\the Upper'. Dev.onian ibasiJll of the Holy OrQSS Mts. The tecto.ni<: gaPs reoognized between 1he ' Givetian and FrasnJi.an. as well as !between the Devonian and Cal1borllil£erous depo sits, led ,t.o the .corredti,OiIl.s in the r~to.nalJ. tectonics.. Three S'pedi.es .()f oonodoms, viz. Polygnathus ancyrognathotde1LS Zieg1er, Schmidtognatnu.s aff. pietzneri Ziegler and Spath,ognathodu.s sannemanrrr;i treptv.s lZiegler, s·o far unknown Ifrom the De- vQ.IlJian 'Of the lHoIJ.y Oross Mts. halVe 'been described. :.: , " ,., iNrnoDuCTION .' .. ', .. :... ~ , . .;": ' ... ~.: .. .. .'. ~ne!a!l stra!ti.:gxaphicframework, based on the COI1J9Clonts, . was . pr-e- . sent~ Jor the Upper Devonlian d€lposits of the Holy croSs ,Mts by g.Z'Ui~ czewsJ9.:(19711).The sicoipe Olf the pre£'ent 'contrllbu1li.oJ:?. is to, apply .'the ~noqon't straltigraphy to a more detailletd recognition of !the p.rach~n~· , t~~lill.e. ·. of yar.nlo, lhaviingacomplex tectonic sb-uCi1nlre' an ith~ centx-aLpart ~ .t}},~,Holy Gross.iM'ts. I(se~ rr~-1i;g. 1; and IMallkowski 19U); ,Mosl; : ~SO far , avaia.ab)re~ dataon Ithe strat~phy a~fac1;€S deV1el~t , Of ~ Itll:e :P ,~N1OIl4aIl deposiltsin ~ larea .come from~IOOlalIwOTks .oov'~ring -e2d;ep.- . -
Eastern Anti Atlas Phanerozoic Granular Iron Formations (Ifs): Nomenclature and Classification, Case of Ordovician Basin of Tafilalt
Available online www.ejaet.com European Journal of Advances in Engineering and Technology, 2016, 3(12): 30-38 Research Article ISSN: 2394 - 658X Eastern Anti Atlas Phanerozoic Granular Iron Formations (IFs): Nomenclature and Classification, Case of Ordovician Basin of Tafilalt Saoud N1, Charroud M1, Dahire M2, Hinaj S1 and Mounir S1 1Laboratory of Georesources and Environment, Faculty of Sciences and Technologies, Sidi Mohammed Ben Abdellah University, Fez-Morocco 2 Laboratory of Geodynamics and Natural Resources, Faculty of Science Dhar el Mehrez, Sidi Mohammed Ben Abdellah University, Fez-Morocco [email protected] _____________________________________________________________________________________________ ABSTRACT In Morocco, the variety of ferruginous resources (dated Archean, Paleozoic and Mesozoic) shows a specific char- acter illustrating the relationship between the geographic position and the geodynamic setting which allows depo- sition of several iron mineralized structures. The sedimentary iron is well manifested in the Paleozoic terranes, and assigns great relation with the Hercynean geodynamic regime, which marks the Gondwanean environment during this time. The results of these processes manifest as the establishment of exploitable iron Formations depos- it situated in the Tafilalt Ordovician basin of the eastern Anti Atlas of Morocco. Key words: Hercynean, Gondwanean, exploitable iron deposits, Tafilalt Ifs, Ordovician, Anti Atlas, Morocco _____________________________________________________________________________________ INTRODUCTION Iron Formations (IFs) originates from sedimentary deposition processing, and they are characterized by a high grade iron tenor which manifest as tiny or laminated chemical facies and contains more than 15% sedimentary iron. The ore is formed by iron oxides and hydroxides such as hematite (Fe2O3) and magnetite (Fe3O4) both consti- tute the major part of the mineralized rock.