Smithsonian Miscellaneous Collections

Total Page:16

File Type:pdf, Size:1020Kb

Smithsonian Miscellaneous Collections SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 119, NUMBER 1 Cfjarles; ». anb ifllarj> 'Vm\ OTalcott l^esiearcf) Jfunb CAMBRIAN STRATIGRAPHY AND PALEONTOLOGY NEAR CABORCA, NORTHWESTERN SONORA, MEXICO (With 31 Plates) BY G. ARTHUR COOPER A. R. V. ARELLANO J. HARLAN JOHNSON VLADIMIR J. OKULITCH ALEXANDER STOYANOW CHRISTINA LOCHMAN (Publication 4085) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION AUGUST 6, 1952 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 119, NUMBER 1 Cljarless ©. anb JHarj> "^aux OTalcott i^esiearci) Jfunb CAMBRIAN STRATIGRAPHY AND PALEONTOLOGY NEAR CABORCA, NORTHWESTERN SONORA, MEXICO (With 31 Plates) BY G. ARTHUR COOPER A. R. V. ARELLANO J. HARLAN JOHNSON VLADIMIR J. OKULITCH ALEXANDER STOYANOW CHRISTINA LOCHMAN (Publication 4085) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION AUGUST 6, 1952 Z^t Botb (g>afttntov< (pr<et« BALTIMORE, MO., U. S. A. CONTENTS Page Introduction and Stratigraphy, by G. Arthur Cooper and A. R. V. Arellano i Localities 2 Proveedora Hills (locality 8oi ) 2 Canedo Hill (locality 812) 9 Prieto Hill (locality 809) 10 Difuntos Hills (locality 802) 12 Buelna Hills (locality 807) 12 Lista Blanca (locality 811) 13 Arrojos Hills (locality 800) 13 Additional localities of Cambrian rocks 15 Summary of Cambrian stratigraphy and correlation between localities . 16 Localities and faunal lists 18 GiRVANELLA, by J. Harlan Johnson 24 Systematic description 24 References 25 Pleospongia, by Vladimir J. OkuHtch 2."] List of species 2^ Systematic description 28 References 34 Brachiopoda, by G. Arthur Cooper 36 Introduction 36 Description 37 References 48 The Original Collection of Cambrian Trilobites from Sonora, by Alexander Stoj'^anow 49 Introduction 49 Description 50 References 59 Trilobites, by Christina Lochman 60 Introduction 60 Structure 62 Ecology 65 Collection and preparation of Cambrian fossils 66 Identification of trilobites 70 Discussion of the faunas 70 Lower Cambrian faunas 70 Composition 70 Correlation 71 Middle Cambrian faunas 73 Faunal zones TZ Composition 76 Correlation 78 iii iv SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. II9 Page Systematic descriptions 81 Lower Cambrian faunas 81 Middle Cambrian faunas 109 References I59 Explanation of Plates 163 Index 181 ILLUSTRATIONS Plates (All plates following page i8o.) 1. North end of the Arrojos Hills and Proveedora Hills. 2. Aerial view of the Proveedora Hills. 3. Difuntos Hills, north end of the Arrojos Hills, and pleosponge reef. 4. Puerto Blanco formation, Prieto Hill; Cafiedo Hill; Buelna and Cerro Prieto formations, Proveedora Hills. 5. Lista Blanca; West Buelna Hill; Girvanella on slope of Prieto Hill. 6. Girvanella. 7. Ethmophyllum cooperi Okulitch, new species, E. americanum Okulitch, new species, and Ajacicyathus ncvadensis (Okulitch). 8. Syringocnema species and Ethmophylluin whitneyi Meek. 9. Coscinocyatlms species, Protopharetra species, Cambrocyathus cf. C. occi- dentalis Okulitch, Ethmophylluin cooperi Okulitch, new species, Ajacicya- thus nevadensis (Okulitch), A. rimonski Okulitch, and Syringocnema species. 10. Archaeocyathus yavorskii (Vologdin). 11. Dictyonina minutipuncta Cooper, new species, Paterina species, and Sco- lithtis tubes. 12. Acrothele concava Cooper, new species, Dictyonina species, Pegmatreta rara Cooper, new species, and Obolella mexicana Cooper, new species. 13. Micrometre species, Lingulella proveedorensis Cooper, new species, Pegma- treta arellanoi Cooper, new species, Wimanella species, Diraphora arro- josensis Cooper, new species, and Nisusia species. 14. Sonoraspis torresi Stoyanow, new species, S. gomesi Stoyanow, new species, and Amecephalus cf. A. piochensis (Walcott), incertae sedis. 15. Problematica I and H, Orthotheca buelna Lochman, new species, Scenella cf. S. reticulata Billings, Hyolithes aff. H. pvinceps Billings, and Sal- terella mexicana Lochman, new species. 16. Salterella cf. 5". pulchella Billings, Hyolithes whitei Resser, and Salterella mexicana Lochman, new species. 17. Salterella mexicana Lochman, new species, and Salterella, species undeter- mined. 18. Wanneria mexicana prima Lochman, new species and new variety, Olenellus (Fremontia) fremonti Walcott, and O. (Olenellus) truemani Walcott. 19. Wanneria walcottana buelnacnsis Lochman, new variety, Wanneria? species undetermined, and Paedeumias pucrtoblancoensis Lochman, new species. 20. Sombrerella mexicana Lochman, new species, Onchocephaliis mexicanus Lochman, new species, and O. buclnaensis Lochman, new species. 21. Bonnia sonora Lochman, new species, Antagmiis solitarius Lochman, new species, Genus and species undetermined i, Antagmus buttsi (Resser), Proveedoria starquistae Lochman, and Strotocephalus arrojosensis Loch- man, new species. V vi SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. II9 22. Ptarmigania bispinosa Lochman, new species, and Mexicaspis difuntosensis Lochman, new species. 23. Albertella provecdora Lochman, new species, A. aft'. A. proveedora Loch- man, new species, and Mexicaspis stenopyge Lochman. 24. Mexicella mexicana Lochman, Pachyaspis, species undetermined, and Ko- chaspis aff. K. celer (Walcott). 25. Glossopleura leona Lochman, new species. Genus and species undetermined 2, Kochaspis? species undetermined, Pachyaspis dehorra Lochman, new species, and Kochaspis cooperi Lochman, new species. 26. Kootenia exilaxata Deiss and Pachyaspis isabella Lochman, new species. 27. Alokistocarella mexicana Lochman, new species, Alokistocare althea Wal- cott, A. cf. A. modcstum Lochman, new species, A. modestnm Lochman, new species, and Hyolithes sonora Lochman, new species. 28. Chancelloria eras Walcott, Problematicum III, Kistocare corbini Lochman, Helcionella, species undetermined, and Kistocare tontoensis (Resser). 29. Athabaskia bela (Walcott), Caborcella arrojosensis Lochman, Arellanella sonora Lochman, new species, A. aff. A. sonora Lochman, new species, and A. caborcajia Lochman. 30. Inglefieldia imperfecta Lochman, new species, and Zacanthoides aff. Z. holopygus Resser. 31. Athabaskia minor (Resser), Cf. Middle Cambrian trilobites, Parehmania, species undetermined. Genus and species undetermined 3, Glossopleura species =zSonoraspis torresi Stoyanow, G. species = Sonoraspis gomezi Stoyanow, Glossopleura species. Figures Page 1. Map showing location of Cambrian sections by locality numbers 3 2. Topographic map showing the Proveedora Hills and collecting local- ities following page 4 3. Topographic map of the Arrojos Hills showing collecting localities following page 4 strati- 4. Cross section of the Proveedora Hills showing formations and graphic position of collections 5 5. Columnar sections showing sequence in the Proveedora Hills and com- paring Arrojos formation of the Arrojos Hills with same formation in the Proveedora Hills 6 6. Columnar sections of the Proveedora Hills and Arrojos Hills compared. 8 il 7. Columnar sections of Prieto Hill and the Buelna Hills compared 8. Diagram showing nomenclature of parts of a trilobite 62 9. Cambrian trilobite appendage 64 Charts 1. Correlation of Mexican Cambrian formations 79 2. Known stratigraphic range of Mexican Middle Cambrian trilobite genera 80 Cf)arle£{ B. anb Jflarp ¥^aux Halcott a^ejfearcfj Jfunb CAMBRIAN STRATIGRAPHY AND PALEON- TOLOGY NEAR CABORCA, NORTH- WESTERN SONORA, MEXICO INTRODUCTION AND STRATIGRAPHY By G. ARTHUR COOPER United States National Museum, Washington, D. C. AND A. R. V. ARELLANO Institiiio Geologico de Mexico, Mexico, D. F. (Plates 1-5) Prior to 1941 Cambrian rocks were unknown in Mexico. But in that year Isauro G. Gomez L. and L. Torres, while making investiga- tions for Petroleos Mexicanos, discovered trilobites in the Arrojos Hills 12 miles west-southwest of Caborca. The Mexican geologists sent their specimens to Dr. Alexander Stoyanow, University of Ari- zona, who identified them as Middle Cambrian trilobites. The pub- lished report of this discovery stimulated interest in Mexico and in the Smithsonian Institution, long a leader in Cambrian stratigraphy and paleontology. The Smithsonian Institution therefore sent G. A. Cooper, representing its staff, and Ing. Alberto Arellano, representing the Instituto Geologico de Mexico, to Caborca, Sonora, to investigate the reported Cambrian and other Paleozoic deposits. Happily, these geologists easily located the trilobite beds in the Arrojos Hills, but in addition they found several other areas exposing Cambrian rocks, especially one long and unbroken sequence 6 miles west of Caborca. Here Lower Cambrian rocks, as well as the previously reported Mid- dle Cambrian, are well exposed. Several weeks in 1943 and 1944 were devoted to investigations of these rocks and making collections of fossils. The collection of fossils obtained from the vicinity of Caborca is a very fine one and consists of numerous kinds of animals. In the in- terest of accuracy and to lend utmost authority to this report on the Mexican Cambrian it seemed best to invite specialists to describe the SMITHSONIAN MISCELLANEOUS COLLECTIONS, VOL. 119, NO. 1 2 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. II9 various groups. Accordingly, Dr. J. Harlan Johnson, Colorado School of Mines, Golden, Colo., was invited to describe the peculiar algae known as Girvanella; Dr. Vladimir J. Okulitch, authority on the Pleo- spongia, contributed the chapter on these interesting and bizarre animals ; G. A. Cooper, who has long been interested in the Brachi- opoda, prepared the discussion of this group ; Dr. Alexander Stoya- now, University of Arizona, who was the first to announce the dis- covery of Cambrian in this portion of
Recommended publications
  • The Viruan (Middle Ordovician) of Öland
    The Viruan (Middle Ordovician) of Öland By Valdar Jaanusson ABSTRACT.-The stratigraphy and lithology of the Viruan (Middle Ordovician) Iimestones of the bed-rock of Öland are described based on three bares and on field work in the outcrop area. A combined litho- and bio-stratigraphic classification (termed topo-stratigraphic) is introduced for the described sequence. The names of the Estonian stages (Aserian, Lasnamägian, Uhakuan, and Kukrusean) are used as chrono-stratigraphic references instead of the previous Swedish names of the units of stage category (Platyurus, Schroeteri, Crassicauda, and Ludibundus, re­ spectivcly). New topo-stratigraphic divisions are Segerstad Limestone (of Aserian age), Skärlöv, Seby, and Folkeslunda Limestones (of Lasnamägian age), Furudal, Källa, and Persnäs Lime­ stones (of Uhakuan age), and Dalby Limestone (of Kukrusean age in the bed-rock of Öland). The Aserian Lasnamägian topo-stratigraphic divisions have the same lithological characteris­ and tics throughout Öland. The Uhakuan beds are developed as calcilutites (Furudal Limestone) on southern Öland continuing as a tongue (Källa Limestone) on northern Öland. The middle and upper part of the Uhakuan beds of northern Öland consist of calcarenites (Persnäs Limestone) lithologically indistiguishable from the Kukrusean Dalby Limestone which forms the bed-rock only on northern Öland. Within the Segerstad Limestone two zones are distinguished (z. of Angelinoceras latum and z. of Illaenus planifrons).H ouvr ' s zones of Lituites discors, L. lituus, and L. perfectus are of Lasna­ mägian age, and their stratigraphic position and fauna! characteristics are described. Contents Introduction . 207 Methods .............. 209 Classification of the Viruan rocks of Öland 2I2 Historical survey . 2I9 Taxonornie and nomenclatural notes 22I Viruan rocks of northern Öland .
    [Show full text]
  • Fossils from the Lower Cambrian of Bornholm
    CHR. POULSEN FOSSILS FROM THE LOWER CAMBRIAN OF BORNHOLM Det Kongelige Danske Videnskabernes Selskab Matematisk-fysiske Meddelelser 36, 2 Kommissionær: Munksgaard København 1967 Synopsis A Lower Cambrian fauna from Bornholm consisting of 34 species is described. The ol- dest of the Lower Cambrian rocks, the Balka quartzite, contains trace fossils referable to Diplocraterion, Tigillites, and Skolithos, and in addition to these some worm remains com- parable to Byronia MATTHEW. After a hiatus follows siltstone („Green shales” of several au- thors) and Bispebjerg sandstone which represent one single cycle of sedimentation. The silt- stone contains a rich fauna which is essentially endemic. Two new genera and seventeen new species are established. The Lower Cambrian age of the siltstone appears clearly from the occurrence of Fordilla troyensis WALCOTT and Hyolilhellus micans BILLINGS. The Bispebjerg sandstone has only yielded a fragment of Hyolithellus micans and a single specimen of the trace fossil Cruziana dispar LINNARSSON. The conditions of sedimentation and the stratigra- phical position of the Bornholm Lower Cambrian are disscussed. PRINTED IN DENMARK BIANCO LUNOS BOGTRYKKERI A-S CONTENTS Page Preface 5 Introduction 6 The sediments 7 Fossils from the Balka quartzite 13 Annelida 13 Genus et sp. ind. (cf. Byronia MATTHEW) 13 Trace fossils 13 Fossils from the siltstone ("Green shales") 14 Porifera 14 Genus et sp. ind. I (cf. Pyrifonema MCov) 14 — — — — II 15 III 15 Pelecypoda 15 Fordilla Iroyensis WALCOTT 15 Genus et sp. ind. 16 Monoplacophora 17 Proplina? prfsca n. sp. 17 Pollicino? cambrica (MOBERG) 18 Gastropoda 19 Prosinuites bornholmensis n. g. et n. sp. 19 Calyptoptomatida 20 Circotheca sp.
    [Show full text]
  • United States
    DEPARTMENT OF THE INTERIOR BULLETIN OF THE UNITED STATES ISTo. 146 WASHINGTON GOVERNMENT Pit IN TING OFFICE 189C UNITED STATES GEOLOGICAL SURVEY CHAKLES D. WALCOTT, DI11ECTOK BIBLIOGRAPHY AND INDEX NORTH AMEEICAN GEOLOGY, PALEONTOLOGY, PETEOLOGT, AND MINERALOGY THE YEA.R 1895 FEED BOUGHTON WEEKS WASHINGTON Cr O V E U N M K N T P K 1 N T I N G OFFICE 1890 CONTENTS. Page. Letter of trail smittal...... ....................... .......................... 7 Introduction.............'................................................... 9 List of publications examined............................................... 11 Classified key to tlio index .......................................... ........ 15 Bibliography ............................................................... 21 Index....................................................................... 89 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTEEIOE, UNITED STATES GEOLOGICAL SURVEY, DIVISION OF GEOLOGY, Washington, D. 0., June 23, 1896. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the year 1895, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINER­ ALOGY FOR THE YEAR 1895. By FRED BOUGHTON WEEKS. INTRODUCTION. The present work comprises a record of publications on North Ameri­ can geology, paleontology, petrology, and mineralogy for the year 1895. It is planned on the same lines as the previous bulletins (Nos. 130 and 135), excepting that abstracts appearing in regular periodicals have been omitted in this volume. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica­ tion in which the paper is printed, and a brief summary of the con­ tents, each paper being numbered for index reference.
    [Show full text]
  • SMC 95 Resser 1936 4 1-29.Pdf
    SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 95, NUMBER 4 SECOND CONTRIBUTION TO NOMENCLATURE OF CAMBRIAN TRILOBITES BY CHARLES ELMER RESSER Curator, Division of Invertebrate Paleontology, U. S. National Museum V i. 1936 (Publication 3383) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 1, 1936 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 95, NUMBER 4 SECOND CONTRIBUTION TO NOMENCLATURE OF CAMBRIAN TRILOBITES BY CHARLES ELMER RESSER Curator, Division of Invertebrate Paleontology, U. S. National Museum (Publication 3383) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 1, 1936 BALTIMOUE, MD., V. 8. A, 4 SECOND CONTRIBUTION TO NOMENCLATURE OF CAMBRIAN TRILOBITES By CHARLES ELMER RESSER Curator, Division of Invertebrate Paleontology U. S. National Museum This is the second paper in a series deaHng with nomenclatural changes necessary for certain Cambrian species/ In this contribution several Atlantic Province genera and species are discussed. As in the previous paper, only published species are considered because illustrations are not possible. Most of the text is arranged in alphabetical order according to genera, exceptions being made in a few cases where several members of a family are kept together. ALBERTELLA Walcott, 1908 Four species were described by Walcott as belonging to Alhertella, viz, the genotype A. helena, and A. bosworthi, A. levis, and A. pa- cifica. The last named, which comes from Asia, is in reality an inde- terminate fragment and must await the finding of further material before its proper generic assignment can be made. Several new spe- cies of Albertella are in hand beside those recognized below in the disr cussion of the three previously described American species.
    [Show full text]
  • An Appraisal of the Great Basin Middle Cambrian Trilobites Described Before 1900
    An Appraisal of the Great Basin Middle Cambrian Trilobites Described Before 1900 By ALLISON R. PALMER A SHORTER CONTRIBUTION TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 264-D Of the 2ty species described prior to I(?OO, 2/ are redescribed and 2C} refigured, and a new name is proposedfor I species UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1 (paper cover) CONTENTS Page Abstract..__________________________________ 55 Introduction ________________________________ 55 Original and present taxonomic names of species. 57 Stratigraphic distribution of species ____________ 57 Collection localities._________________________ 58 Systematic descriptions.______________________ 59 Literature cited____________________________ 82 Index __-_-__-__---_--______________________ 85 ILLUSTRATIONS [Plates 13-17 follow page 86] PLATE 13. Agnostidae and Dolichometopidae 14. Dorypygidae 15. Oryctocephalidae, Dorypygidae, Zacanthoididae, and Ptychoparioidea 16. Ptychoparioidea 17. Ptychoparioidea FIGUBE 3. Index map showing collecting localities____________________________ . Page 56 in A SHORTER CONTRIBUTION TO GENERAL GEOLOGY AN APPRAISAL OF THE GREAT BASIN MIDDLE CAMBRIAN TRILOBITES DESCRIBED BEFORE 1900 By ALLISON R. PALMER ABSTRACT the species and changes in their generic assignments All 29 species of Middle Cambrian trilobites
    [Show full text]
  • Smithsonian Miscellaneous Collections
    SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 75. NUMBER 3 CAMBRIAN GEOLOGY AND PALEONTOLOGY V No. 3—CAMBRIAN AND OZARKIAN TRILOBITES (With Plates 15 to 24) BY CHARLES D. WALCOTT es'^ VorbH (Publication 2823) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JUNE 1, 1925 Z^e. JSorb Q0affttttorc (preee BALTIMORE, MD., U. S. A, . CAMBRIAN GEOLOGY AND PALEONTOLOGY V No. 3.—CAMBRIAN AND OZARKIAN TRILOBITES By CHARLES D. WALCOTT (With Plates 15 to 24) CONTENTS PAGE Introduction 64 Description of genera and species 65 Genus Amecephalus Walcott 65 Amecephalus piochensis (Walcott), Middle Cambrian (Chis- holm) 66 Genus Anoria Walcott 67 Anorta tovtoensis (Walcott), Upper Cambrian 68 Genus Armonia Walcott 69 Armonia pelops Walcott, Upper Cambrian (Conasauga) 69 Genus Beliefontia Ulrich 69 Beliefontia collieana (Raymond) Ulrich, Canadian 72 Belief07itia nonius (Walcott), Ozarkian (Mons) y2 Genus Bowmania, new genus 73 Bonmiania americana (Walcott), Upper Cambrian y^ Subfamily Dikelocephalinae Beecher 74 Genus Briscoia Walcott _. 74 Briscoia sinclairensis Walcott, Ozarkian (Mons) 75 Genus Burnetia Walcott yj Burnetia urania (Walcott), Upper Cambrian yj Genus Bynumia Walcott 78 Bynumia eumus Walcott, Upper Cambrian (Lyell) 78 Genus Cedaria Walcott 78 Cedaria proUUca Walcott, Upper Cambrian (Conasauga) 79 Cedaria tennesseensis, species, .' new Upper Cambrian . 79 Genus Chancia Walcott 80 Chancia ebdome Walcott, Middle Cambrian 80 Chancia evax, new species, Middle Cambrian 81 Genus Corbinia Walcott 81 Corbinia horatio Walcott, Ozarkian (Mons) 81 Corbinia valida, new species, Ozarkian (Mons) 82 Genus Crusoia Walcott 82 Crusoia cebes Walcott, Middle Cambrian 82 Genus Desmetia, new genus 83 Desmetia annectans (Walcott) , Ozarkian (Goodwin) 83 Smithsonian Miscellaneous Collections, Vol. 75, No. 3 61 62 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL.
    [Show full text]
  • An Inventory of Trilobites from National Park Service Areas
    Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 179 AN INVENTORY OF TRILOBITES FROM NATIONAL PARK SERVICE AREAS MEGAN R. NORR¹, VINCENT L. SANTUCCI1 and JUSTIN S. TWEET2 1National Park Service. 1201 Eye Street NW, Washington, D.C. 20005; -email: [email protected]; 2Tweet Paleo-Consulting. 9149 79th St. S. Cottage Grove. MN 55016; Abstract—Trilobites represent an extinct group of Paleozoic marine invertebrate fossils that have great scientific interest and public appeal. Trilobites exhibit wide taxonomic diversity and are contained within nine orders of the Class Trilobita. A wealth of scientific literature exists regarding trilobites, their morphology, biostratigraphy, indicators of paleoenvironments, behavior, and other research themes. An inventory of National Park Service areas reveals that fossilized remains of trilobites are documented from within at least 33 NPS units, including Death Valley National Park, Grand Canyon National Park, Yellowstone National Park, and Yukon-Charley Rivers National Preserve. More than 120 trilobite hototype specimens are known from National Park Service areas. INTRODUCTION Of the 262 National Park Service areas identified with paleontological resources, 33 of those units have documented trilobite fossils (Fig. 1). More than 120 holotype specimens of trilobites have been found within National Park Service (NPS) units. Once thriving during the Paleozoic Era (between ~520 and 250 million years ago) and becoming extinct at the end of the Permian Period, trilobites were prone to fossilization due to their hard exoskeletons and the sedimentary marine environments they inhabited. While parks such as Death Valley National Park and Yukon-Charley Rivers National Preserve have reported a great abundance of fossilized trilobites, many other national parks also contain a diverse trilobite fauna.
    [Show full text]
  • Sedimentology and Palaeontology of the Withycombe Farm Borehole, Oxfordshire, UK
    Sedimentology and Palaeontology of the Withycombe Farm Borehole, Oxfordshire, England By © Kendra Morgan Power, B.Sc. (Hons.) A thesis submitted to the School of Graduate Studies in partial fulfillment of the requirements for the degree of Master of Science Department of Earth Sciences Memorial University of Newfoundland May 2020 St. John’s Newfoundland Abstract The pre-trilobitic lower Cambrian of the Withycombe Formation is a 194 m thick siliciclastic succession dominated by interbedded offshore red to purple and green pyritic mudstone with minor sandstone. The mudstone contains a hyolith-dominated small shelly fauna including: orthothecid hyoliths, hyolithid hyoliths, the rostroconch Watsonella crosbyi, early brachiopods, the foraminiferan Platysolenites antiquissimus, the coiled gastropod-like Aldanella attleborensis, halkieriids, gastropods and a low diversity ichnofauna including evidence of predation by a vagile infaunal predator. The assemblage contains a number of important index fossils (Watsonella, Platysolenites, Aldanella and the trace fossil Teichichnus) that enable correlation of strata around the base of Cambrian Stage 2 from Avalonia to Baltica, as well as the assessment of the stratigraphy within the context of the lower Cambrian stratigraphic standards of southeastern Newfoundland. The pyritized nature of the assemblage has enabled the study of some of the biota using micro-CT, augmented with petrographic studies, revealing pyritized microbial filaments of probable giant sulfur bacteria. We aim to produce the first complete description of the core and the abundant small pyritized fossils preserved in it, and develop a taphonomic model for the pyritization of the “small” shelly fossils. i Acknowledgements It is important to acknowledge and thank the many people who supported me and contributed to the successful completion of this thesis.
    [Show full text]
  • Newsletter Number 79
    The Palaeontology Newsletter Contents 79 Editorial 2 Association Business 3 News: awards and prizes 10 Association Meetings 16 From our correspondents Encore des Buffonades, mon cher … 20 PalaeoMath 101: Elliptic Fourier … 29 Future meetings of other bodies 44 Meeting Reports Silicofossil/Palynology joint meeting 50 Lyell Meeting 2011 53 55th PalAss Annual Meeting 2011 55 Obituary Arthur Cruickshank 64 Reporter: the Palaeontology of Pop 71 Sylvester-Bradley reports 75 Virtual Palaeontology 82 Book Reviews 88 Palaeontology vol 55 parts 1 & 2 101–102 Reminder: The deadline for copy for Issue no 80 is 11th June 2012. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 79 2 Editorial The publication of Newsletter 79 marks the end of the beginning of my new post as Newsletter editor. Many thanks to my predecessor Dr Richard Twitchett, who prepared a most useful guide to my editorial duties and tasks before moving to the even more demanding Council role of Secretary. Unlike the transition to editor in the world of journalism, I did not inherit an expenses account, tastefully furnished office and a PA, but I do now have the <[email protected]> account. That is how to contact me about Newsletter matters, send me articles, and let me, and Council, know what you want, and don’t want, from the Newsletter. The Newsletter has expanded greatly in the past decade and there is a great deal more copy and content, which you can check by investigating the Newsletter archive on the Association website. Such an expansion relies on a steady flow of copy from the membership and our regular columnists.
    [Show full text]
  • A Cambrian Meraspid Cluster: Evidence of Trilobite Egg Deposition in a Nest Site
    PALAIOS, 2019, v. 34, 254–260 Research Article DOI: http://dx.doi.org/10.2110/palo.2018.102 A CAMBRIAN MERASPID CLUSTER: EVIDENCE OF TRILOBITE EGG DEPOSITION IN A NEST SITE 1 2 DAVID R. SCHWIMMER AND WILLIAM M. MONTANTE 1Department of Earth and Space Sciences, Columbus State University, Columbus, Georgia 31907-5645, USA 2Tellus Science Museum, 100 Tellus Drive, Cartersville, Georgia, 30120 USA email: [email protected] ABSTRACT: Recent evidence confirms that trilobites were oviparous; however, their subsequent embryonic development has not been determined. A ~ 6cm2 claystone specimen from the upper Cambrian (Paibian) Conasauga Formation in western Georgia contains a cluster of .100 meraspid trilobites, many complete with librigenae. The juvenile trilobites, identified as Aphelaspis sp., are mostly 1.5 to 2.0 mm total length and co-occur in multiple axial orientations on a single bedding plane. This observation, together with the attached free cheeks, indicates that the association is not a result of current sorting. The majority of juveniles with determinable thoracic segment counts are of meraspid degree 5, suggesting that they hatched penecontemporaneously following a single egg deposition event. Additionally, they are tightly assembled, with a few strays, suggesting that the larvae either remained on the egg deposition site or selectively reassembled as affiliative, feeding, or protective behavior. Gregarious behavior by trilobites (‘‘trilobite clusters’’) has been reported frequently, but previously encompassed only holaspid adults or mixed-age assemblages. This is the first report of juvenile trilobite clustering and one of the few reported clusters involving Cambrian trilobites. Numerous explanations for trilobite clustering behavior have been posited; here it is proposed that larval clustering follows egg deposition at a nest site, and that larval aggregation may be a homing response to their nest.
    [Show full text]
  • On the Nature of Polylopia
    On the Nature of Polylopia GEOLOGICAL SURVEY PROFESSIONAL PAPER 593-F On the Nature of Polylopia By ELLIS L. YOCHELSON CONTRIBUTIONS TO PALEONTOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 593-F A reinvestigation of a rare Middle Ordovician conical mollusk UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 20 cents (paper cover) CONTENTS Page Abstract___________________________________________________________________ F1 Introduction_______________________________________________________________ 1 Material examined__________________________________________________________ 1 Preparation________________________________________________________________ 1 Morphology of Polylopia___ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 2 Stratigraphic distribution____________________________________________________ 3 Paleoecology_______________________________________________________________ 4 Systematic position of Polylopia_ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 5 References cited____________________________________________________________ 7 PLATE [Plate follows references cited] 1. Polylopia and Biconculites. III CONTRIBUTIONS TO PALEONTOLOGY ON THE NATURE OF POL YLOPIA By ELLIS L. y OCHELSON ABSTRACT work, responsibility for the conclusions rests solely with Polylopia bilUngsi (Safford), from the Middle Ordovician the author. Murfreesboro Limestone of central Tennessee, is redescribed. MATERIAL EXAMINED The shell is interpreted as a simple exceedingly high closed cone, bearing longitudinal lirae on the exterior and lacking any Polylopia is best known frmn outcrops of the Mur­ interior structures.
    [Show full text]
  • Resolving Details of the Nonbiomineralized Anatomy of Trilobites Using Computed
    Resolving Details of the Nonbiomineralized Anatomy of Trilobites Using Computed Tomographic Imaging Techniques Thesis Presented in Partial Fulfillment of the Requirements for the Master of Science in the Graduate School of The Ohio State University By Jennifer Anita Peteya, B.S. Graduate Program in Earth Sciences The Ohio State University 2013 Thesis Committee: Loren E. Babcock, Advisor William I. Ausich Stig M. Bergström Copyright by Jennifer Anita Peteya 2013 Abstract Remains of two trilobite species, Elrathia kingii from the Wheeler Formation (Cambrian Series 3), Utah, and Cornuproetus cornutus from the Hamar Laghdad Formation (Middle Devonian), Alnif, Morocco, were studied using computed tomographic (CT) and microtomographic (micro-CT) imaging techniques for evidence of nonbiomineralized alimentary structures. Specimens of E. kingii showing simple digestive tracts are complete dorsal exoskeletons preserved with cone-in-cone concretions on the ventral side. Inferred stomach and intestinal structures are preserved in framboidal pyrite, likely resulting from replication by a microbial biofilm. C. cornutus is preserved in non- concretionary limestone with calcite spar lining the stomach ventral to the glabella. Neither species shows sediment or macerated sclerites of any kind in the gut, which tends to rule out the possibilities that they were sediment deposit-feeders or sclerite-ingesting durophagous carnivores. Instead, the presence of early diagenetic minerals in the guts of E. kingii and C. cornutus favors an interpretation of a carnivorous feeding strategy involving separation of skeletal parts of prey prior to ingestion. ii Dedication This manuscript is dedicated to my parents for encouraging me to go into the field of paleontology and to Lee Gray for inspiring me to continue.
    [Show full text]