Phosphatic 'Inarticulate'
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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. -
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 ....................................................................................................... -
Durham Research Online
Durham Research Online Deposited in DRO: 23 May 2017 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Betts, Marissa J. and Paterson, John R. and Jago, James B. and Jacquet, Sarah M. and Skovsted, Christian B. and Topper, Timothy P. and Brock, Glenn A. (2017) 'Global correlation of the early Cambrian of South Australia : shelly fauna of the Dailyatia odyssei Zone.', Gondwana research., 46 . pp. 240-279. Further information on publisher's website: https://doi.org/10.1016/j.gr.2017.02.007 Publisher's copyright statement: c 2017 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Accepted Manuscript Global correlation of the early Cambrian of South Australia: Shelly fauna of the Dailyatia odyssei Zone Marissa J. -
Facies, Phosphate, and Fossil Preservation Potential Across a Lower Cambrian Carbonate Shelf, Arrowie Basin, South Australia
Palaeogeography, Palaeoclimatology, Palaeoecology 533 (2019) 109200 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Facies, phosphate, and fossil preservation potential across a Lower Cambrian T carbonate shelf, Arrowie Basin, South Australia ⁎ Sarah M. Jacqueta,b, , Marissa J. Bettsc,d, John Warren Huntleya, Glenn A. Brockb,d a Department of Geological Sciences, University of Missouri, Columbia, MO 65211, USA b Department of Biological Sciences, Macquarie University, Sydney, New South Wales 2109, Australia c Palaeoscience Research Centre, School of Environmental and Rural Science, University of New England, Armidale, New South Wales 2351, Australia d Early Life Institute and Department of Geology, State Key Laboratory for Continental Dynamics, Northwest University, Xi'an 710069, China ARTICLE INFO ABSTRACT Keywords: The efects of sedimentological, depositional and taphonomic processes on preservation potential of Cambrian Microfacies small shelly fossils (SSF) have important implications for their utility in biostratigraphy and high-resolution Calcareous correlation. To investigate the efects of these processes on fossil occurrence, detailed microfacies analysis, Organophosphatic biostratigraphic data, and multivariate analyses are integrated from an exemplar stratigraphic section Taphonomy intersecting a suite of lower Cambrian carbonate palaeoenvironments in the northern Flinders Ranges, South Biominerals Australia. The succession deepens upsection, across a low-gradient shallow-marine shelf. Six depositional Facies Hardgrounds Sequences are identifed ranging from protected (FS1) and open (FS2) shelf/lagoonal systems, high-energy inner ramp shoal complex (FS3), mid-shelf (FS4), mid- to outer-shelf (FS5) and outer-shelf (FS6) environments. Non-metric multi-dimensional scaling ordination and two-way cluster analysis reveal an underlying bathymetric gradient as the main control on the distribution of SSFs. -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 53, NUMBER 6 CAMBRIAN GEOLOGY AND PALEONTOLOGY No. 6.-0LENELLUS AND OTHER GENERA OF THE MESONACID/E With Twenty-Two Plates CHARLES D. WALCOTT (Publication 1934) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION AUGUST 12, 1910 Zl^i £orb (gaitimovt (pnee BALTIMORE, MD., U. S. A. CAMBRIAN GEOLOGY AND PALEONTOLOGY No. 6.—OLENELLUS AND OTHER GENERA OF THE MESONACID^ By CHARLES D. WALCOTT (With Twenty-Two Plates) CONTENTS PAGE Introduction 233 Future work 234 Acknowledgments 234 Order Opisthoparia Beecher 235 Family Mesonacidas Walcott 236 Observations—Development 236 Cephalon 236 Eye 239 Facial sutures 242 Anterior glabellar lobe 242 Hypostoma 243 Thorax 244 Nevadia stage 244 Mesonacis stage 244 Elliptocephala stage 244 Holmia stage 244 Piedeumias stage 245 Olenellus stage 245 Peachella 245 Olenelloides ; 245 Pygidium 245 Delimitation of genera 246 Nevadia 246 Mesonacis 246 Elliptocephala 247 Callavia 247 Holmia 247 Wanneria 248 P.'edeumias 248 Olenellus 248 Peachella 248 Olenelloides 248 Development of Mesonacidas 249 Mesonacidas and Paradoxinas 250 Stratigraphic position of the genera and species 250 Abrupt appearance of the Mesonacidse 252 Geographic distribution 252 Transition from the Mesonacidse to the Paradoxinse 253 Smithsonian Miscellaneous Collections, Vol. 53, No. 6 232 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. 53 Description of genera and species 256 Nevadia, new genus 256 weeksi, new species 257 Mcsonacis Walcott 261 niickwitzi (Schmidt) 262 torelli (Moberg) 264 vermontana -
1 Tommotiids from the Early Cambrian (Series 2, Stage 3) of Morocco and the Evolution Of
1 1 Tommotiids from the early Cambrian (Series 2, stage 3) of Morocco and the evolution of 2 the tannuolinid scleritome and setigerous shell structures in stem group brachiopods 3 4 by CHRISTIAN B. SKOVSTED1, SÉBASTIEN CLAUSEN2, J. JAVIER ÁLVARO3 and 5 DEBORAH PONLEVÉ2 6 7 1 Department of Palaeozoology, Swedish Museum of Natural History, P.O. Box 50007, SE- 8 104 05 Stockholm, Sweden, [email protected]. 9 2 UMR 8217 Géosystèmes, UFR Sciences de la Terre, Université Lille 1, 10 [email protected], [email protected]. 11 3 Centro de Astrobiología (CSIC/INTA), Ctra. de Torrejón a Ajalvir km 4, 28850 Torrejón de 12 Ardoz, Spain, [email protected] 13 14 Abstract: An assemblage of tannuolinid sclerites is described from the Amouslek Formation 15 (Souss Basin) of the Anti-Atlas Mountains in Morocco. The assemblage contains two species, 16 Tannuolina maroccana n. sp. which is represented by a small number of mitral and sellate 17 sclerites and Micrina sp., represented by a single mitral sclerite. Tannuolina maroccana 18 differs from other species of the genus in the presence of both bilaterally symmetrical and 19 strongly asymmetrical sellate sclerites. This observation suggests that the scleritome of 20 Tannuolina was more complex than previously thought and that this tommotiid may have held 21 a more basal position in the brachiopod stem group than previously assumed. The shell 22 structure of both T. maroccana and Micrina sp. is well preserved and exhibits two 23 fundamentally different sets of tubular structures, only one of which was likely to contain 24 shell penetrating setae. -
A Chancelloriid-Like Metazoan from the Early Cambrian Chengjiang
OPEN A chancelloriid-like metazoan from the SUBJECT AREAS: early Cambrian Chengjiang Lagersta¨tte, PALAEONTOLOGY ENVIRONMENTAL SCIENCES China Xianguang Hou1, Mark Williams2, David J. Siveter2, Derek J. Siveter3,4, Sarah Gabbott2, David Holwell2 Received & Thomas H. P. Harvey2 23 July 2014 Accepted 1Yunnan Key Laboratory for Palaeobiology, Yunnan University, Kunming 650091, China, 2Department of Geology, University of 17 November 2014 Leicester, Leicester LE1 7RH, UK, 3Earth Collections, Oxford University Museum of Natural History, Parks Road, Oxford, OX1 3PW, UK, 4Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3PR, UK. Published 9 December 2014 Nidelric pugio gen. et sp. nov. from the Cambrian Series 2 Heilinpu Formation, Chengjiang Lagersta¨tte, Yunnan Province, China, is an ovoid, sac-like metazoan that bears single-element spines on its surface. N. Correspondence and pugio shows no trace of a gut, coelom, anterior differentiation, appendages, or internal organs that would suggest a bilateral body plan. Instead, the sac-like morphology invites comparison with the radially requests for materials symmetrical chancelloriids. However, the single-element spines of N. pugio are atypical of the complex should be addressed to multi-element spine rosettes borne by most chancelloriids and N. pugio may signal the ancestral X.G.H. (xghou@ynu. chancelloriid state, in which the spines had not yet fused. Alternatively, N. pugio may represent a group of edu.cn) radial metazoans that are discrete from chancelloriids. Whatever its precise phylogenetic position, N. pugio expands the known disparity of Cambrian scleritome-bearing animals, and provides a new model for reconstructing scleritomes from isolated microfossils. -
Mem170-Bm.Pdf by Guest on 30 September 2021 452 Index
Index [Italic page numbers indicate major references] acacamite, 437 anticlines, 21, 385 Bathyholcus sp., 135, 136, 137, 150 Acanthagnostus, 108 anticlinorium, 33, 377, 385, 396 Bathyuriscus, 113 accretion, 371 Antispira, 201 manchuriensis, 110 Acmarhachis sp., 133 apatite, 74, 298 Battus sp., 105, 107 Acrotretidae, 252 Aphelaspidinae, 140, 142 Bavaria, 72 actinolite, 13, 298, 299, 335, 336, 339, aphelaspidinids, 130 Beacon Supergroup, 33 346 Aphelaspis sp., 128, 130, 131, 132, Beardmore Glacier, 429 Actinopteris bengalensis, 288 140, 141, 142, 144, 145, 155, 168 beaverite, 440 Africa, southern, 52, 63, 72, 77, 402 Apoptopegma, 206, 207 bedrock, 4, 58, 296, 412, 416, 422, aggregates, 12, 342 craddocki sp., 185, 186, 206, 207, 429, 434, 440 Agnostidae, 104, 105, 109, 116, 122, 208, 210, 244 Bellingsella, 255 131, 132, 133 Appalachian Basin, 71 Bergeronites sp., 112 Angostinae, 130 Appalachian Province, 276 Bicyathus, 281 Agnostoidea, 105 Appalachian metamorphic belt, 343 Billingsella sp., 255, 256, 264 Agnostus, 131 aragonite, 438 Billingsia saratogensis, 201 cyclopyge, 133 Arberiella, 288 Bingham Peak, 86, 129, 185, 190, 194, e genus, 105 Archaeocyathidae, 5, 14, 86, 89, 104, 195, 204, 205, 244 nudus marginata, 105 128, 249, 257, 281 biogeography, 275 parvifrons, 106 Archaeocyathinae, 258 biomicrite, 13, 18 pisiformis, 131, 141 Archaeocyathus, 279, 280, 281, 283 biosparite, 18, 86 pisiformis obesus, 131 Archaeogastropoda, 199 biostratigraphy, 130, 275 punctuosus, 107 Archaeopharetra sp., 281 biotite, 14, 74, 300, 347 repandus, 108 Archaeophialia, -
Re-Evaluation of the Stratigraphically Important Olenellid Trilobite Holmia Cf. Mobergi from the Cambrian Series 2, Stage 3
NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 1 https://dx.doi.org/10.17850/njg99-1-04 Re-evaluation of the stratigraphically important olenellid trilobite Holmia cf. mobergi from the Cambrian Series 2, Stage 3 and its implications for the lower Cambrian stratigraphy in the Mjøsa area, Norway Magne Høyberget1, Jan Ove R. Ebbestad2 & Bjørn Funke3 1Rennesveien 14, N–4513 Mandal, Norway. 2Museum of Evolution, Uppsala University, Norbyvägen 16, SE–752 36 Uppsala, Sweden. 3Gjelleråsveien 10, N–1481 Hagan, Norway. E-mail corresponding author (Magne Høyberget): [email protected] The olenellid trilobite Holmia cf. mobergi, known from a single cephalon in the upper lower Cambrian strata from a river section in Flagstadelva, Hamar, has played a significant stratigraphic role in interpreting the lower Cambrian informal Series 2, Stage 3 in the Mjøsa area, Norway, since its discovery in the early 1950s. It was considered one of the oldest trilobite taxa in the lower Cambrian of Scandinavia, but the stratigraphic level and biozonation of the cephalon were problematic and a matter of discussion for decades. Moreover, organic-walled microfossil biostratigraphy questioned the supposed age of the trilobite. New specimens of this taxon collected from the type locality show that the species occurs at a different stratigraphic level than first reported, prompting a new description of the species and a re-evaluation of the taxon’s biostratigraphic significance. Holmia cf. mobergi is compared with new and well-preserved topotype material of Holmia inusitata, a very rare taxon hitherto known from one single outcrop in an autochthonous setting in Norway. Holmia cf. -
Arthropod Pattern Theory and Cambrian Trilobites
Bijdragen tot de Dierkunde, 64 (4) 193-213 (1995) SPB Academie Publishing bv, The Hague Arthropod pattern theory and Cambrian trilobites Frederick A. Sundberg Research Associate, Invertebrate Paleontology Section, Los Angeles County Museum of Natural History, 900 Exposition Boulevard, Los Angeles, California 90007, USA Keywords: Arthropod pattern theory, Cambrian, trilobites, segment distributions 4 Abstract ou 6). La limite thorax/pygidium se trouve généralementau niveau du node 2 (duplomères 11—13) et du node 3 (duplomères les les 18—20) pour Corynexochides et respectivement pour Pty- An analysis of duplomere (= segment) distribution within the chopariides.Cette limite se trouve dans le champ 4 (duplomères cephalon,thorax, and pygidium of Cambrian trilobites was un- 21—n) dans le cas des Olenellides et des Redlichiides. L’extrémité dertaken to determine if the Arthropod Pattern Theory (APT) du corps se trouve généralementau niveau du node 3 chez les proposed by Schram & Emerson (1991) applies to Cambrian Corynexochides, et au niveau du champ 4 chez les Olenellides, trilobites. The boundary of the cephalon/thorax occurs within les Redlichiides et les Ptychopariides. D’autre part, les épines 1 4 the predicted duplomerenode (duplomeres or 6). The bound- macropleurales, qui pourraient indiquer l’emplacement des ary between the thorax and pygidium generally occurs within gonopores ou de l’anus, sont généralementsituées au niveau des node 2 (duplomeres 11—13) and node 3 (duplomeres 18—20) for duplomères pronostiqués. La limite prothorax/opisthothorax corynexochids and ptychopariids, respectively. This boundary des Olenellides est située dans le node 3 ou près de celui-ci. Ces occurs within field 4 (duplomeres21—n) for olenellids and red- résultats indiquent que nombre et distribution des duplomères lichiids. -
Decoding the Fossil Record of Early Lophophorates
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1284 Decoding the fossil record of early lophophorates Systematics and phylogeny of problematic Cambrian Lophotrochozoa AODHÁN D. BUTLER ACTA UNIVERSITATIS UPSALIENSIS ISSN 1651-6214 ISBN 978-91-554-9327-1 UPPSALA urn:nbn:se:uu:diva-261907 2015 Dissertation presented at Uppsala University to be publicly examined in Hambergsalen, Geocentrum, Villavägen 16, Uppsala, Friday, 23 October 2015 at 13:15 for the degree of Doctor of Philosophy. The examination will be conducted in English. Faculty examiner: Professor Maggie Cusack (School of Geographical and Earth Sciences, University of Glasgow). Abstract Butler, A. D. 2015. Decoding the fossil record of early lophophorates. Systematics and phylogeny of problematic Cambrian Lophotrochozoa. (De tidigaste fossila lofoforaterna. Problematiska kambriska lofotrochozoers systematik och fylogeni). Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1284. 65 pp. Uppsala: Acta Universitatis Upsaliensis. ISBN 978-91-554-9327-1. The evolutionary origins of animal phyla are intimately linked with the Cambrian explosion, a period of radical ecological and evolutionary innovation that begins approximately 540 Mya and continues for some 20 million years, during which most major animal groups appear. Lophotrochozoa, a major group of protostome animals that includes molluscs, annelids and brachiopods, represent a significant component of the oldest known fossil records of biomineralised animals, as disclosed by the enigmatic ‘small shelly fossil’ faunas of the early Cambrian. Determining the affinities of these scleritome taxa is highly informative for examining Cambrian evolutionary patterns, since many are supposed stem- group Lophotrochozoa. The main focus of this thesis pertained to the stem-group of the Brachiopoda, a highly diverse and important clade of suspension feeding animals in the Palaeozoic era, which are still extant but with only with a fraction of past diversity. -
Inarticulate Brachiopods from the Lower Ordovician in Northern Poland
Annales Societatis Geologorum Poloniae (1986); vol. 56: 409—418 PL ISSN 0208-9068 INARTICULATE BRACHIOPODS FROM THE LOWER ORDOVICIAN IN NORTHERN POLAND Wiesław Bednarczyk Institute of Geological Sciences, Polish Academy of Sciences, Żwirki i Wigury 93, 02-089 Warszawa Bednarczyk, W ., 1986. Inarticulate brachiopods from the Lower Ordovician in northern Poland. Ann. Soc. Geol. Polon., 56: 409—418. A bstract: Some inarticulate brachiopods, including 6 new species and 1 new genus, are described from lowermost Ordovician limestone from vicinity of Łeba, northern Poland. The as semblage is dominated by acrotretids some of which are closely related to some Scandinavian species. The described taxa may be of value in correlating upper Tremadocian and lower Arenigian deposits. Key words: Ordovician, brachiopods, Inarticulata, morphology, taxonomy, new genus, new species. Manuscript received December 1985, accepted January 1986. INTRODUCTION Minute inarticulate brachiopods dominated by ac.otietids were found during the preparation of conodonts from Lower Ordovician of northern Poland. The present paper contains descriptions of Pomeraniotreta biernati n. gen. et n. sp. and of six other species belonging to Rowellella, Conotreta, Eurytreta, Myotreta, and Paterula. The remaining part of the collection is being studied. Recently, the author received a written information from Dr Lars Holmer from the University of Uppsala on his collection of inarticulate brachiopods from the Ceratopyge Limestone of Scandinavia. This collection includes brachial valves apparently identical with those described here as Pomeraniotreta biernati n. gen. et n. sp., and also articulated shells, i.e. those in which the brachial and pedicle valves are still joined. The pedicle valves appear to be identical with those described by Bednarczyk (1979) as Torynelasma lebaensis n.