Bivalvia: Carditidae) on the U.S
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Silicified Eocene Molluscs from the Lower Murchison District, Southern Carnarvon Basin, Western Australia
[<ecords o{ the Western A uslralian Museum 24: 217--246 (2008). Silicified Eocene molluscs from the Lower Murchison district, Southern Carnarvon Basin, Western Australia Thomas A. Darragh1 and George W. Kendrick2.3 I Department of Invertebrate Palaeontology, Museum Victoria, 1'.0. Box 666, Melbourne, Victoria 3001, Australia. Email: tdarragh(il.Illuseum.vic.gov.au :' Department of Earth and Planetary Sciences, Western Australian Museum, Locked Bag 49, Welshpool D.C., Western Australia 6986, Australia. 1 School of Earth and Ceographical Sciences, The University of Western Australia, 35 Stirling Highway, Crawlev, Western Australia 6009, Australia. Abstract - Silicified Middle to Late Eocene shallow water sandstones outcropping in the Lower Murchison District near Kalbarri township contain a silicified fossil fauna including foraminifera, sponges, bryozoans, solitary corals, brachiopods, echinoids and molluscs. The known molluscan fauna consists of 51 species, comprising 2 cephalopods, 14 bivalves, 1 scaphopod and 34 gastropods. Of these taxa three are newly described, Cerithium lvilya, Zeacolpus bartol1i, and Lyria lamellatoplicata. 25 of these molluscs are identical to or closely comparable with taxa from the southern Australian Eocene. The occurrence of this fauna extends the Southeast Australian Province during the Eocene from southwest Western Australia along the west coast north to at least 27° present day south latitude; consequently the province is here renamed the Southern Australian Province. Keywords: siliceous fossils, Eocene, Kalbarri, molluscs, new taxa, Carnarvon Basin, biogeography, Southern Australian Province. INTRODUCTION The source deposit, a pallid to ferruginous silicified Eocene marine molluscan assemblages from sandstone, forms a weakly defined, low breakaway coastal sedimentary basins in southern Australia trending N-S and sloping gently westward. -
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CAROLINA GEOLOGICAL SOCIETY FIELD TRIP GUIDEBOOK November 13 – 15, 1992 GEOLOGICAL INVESTIGATIONS OF THE CENTRAL SAVANNAH RIVER AREA, SOUTH CAROLINA AND GEORGIA edited by Wallace Fallaw Department of Geology, Furman University, Greenville, SC 29613 Van Price Environmental Monitoring section, Westinghouse Savannah River Co., Aiken SC 29808 Front cover: Topography of the Central Savannah River Valley and surrounding area looking up-river. Copies of this guidebook can be obtained from: South Carolina Geological Survey Harbison Forest Road Columbia, South Carolina 29210-4089 ii WE THANK THESE CORPORATE SPONSORS FOR THEIR SUPPORT OF THE 1992 CAROLINA GEOLOGICAL SOCIETY MEETING J.H. HUBER CORPORATION Langley, South Carolina KENNECOTT RIDGEWAY MINING COMPANY Ridgeway, South Carolina RMT, INC. Greenville, South Carolina SOUTHEASTERN CLAY COMPANY Aiken, South Carolina GERAGHTY AND MILLER INC. Aiken, South Carolina FOSTER DIXIANA CORP. Columbia, South Carolina EXPLORATION RESOURCES INC. Athens, Georgia The United States Department of Energy and the South Carolina Geological Survey provided partial support for this guidebook. However, the opinions and interpretations expressed within are not necessarily those of the Department of Energy or the South Carolina Geological Survey. iii CONTENTS Road Log and Outcrops in the vicinity of the Savannah River Site (W.C. Fallaw, Van Price and Walter J. Sex- ton) . .. .1 Observations on general allo-stratigraphy and tectonic framework of the southeastern Atlantic Coast Regional Cross Section (DNAG E-5 Corridor) Georgia and South Carolina as they relate to the Savan- nah River Site. (Donald Colquhoun). .. .11 Outline of stratigraphy at the Savannah River Site. (W. C. Fallaw and Van Price) . .17 Stratigraphic relationships in Eocene out crops along Upper Three Runs at the Savannah River Site. -
Paleontology and Sedimentology of Middle Eocene Rocks in Lago Argentino Area, Santa Cruz Province, Argentina
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 46 (1): 27-47. Buenos Aires, 30-04-2009 ISSN 0002-7014 Paleontology and sedimentology of Middle Eocene rocks in Lago Argentino area, Santa Cruz Province, Argentina Silvio CASADÍO1,2, Miguel GRIFFIN1,2, Sergio MARENSSI3,2, Laura NET4, Ana PARRAS1,2, Martín RODRÍGUEZ RAISING5,2 and Sergio SANTILLANA3 Abstract. Sedimentological and paleontological study of the Man Aike Formation at the Estancia 25 de Mayo, SW of Santa Cruz Province, Argentina, represents the evolution of an incised valley from fluvial to marine environment during the late middle Eocene. At the base of the unit there is an unconformity that corresponds to fluvial channels which cut down into the underlying Maastrichtian sandstones of the Calafate Formation. The fauna of invertebrates (mostly molluscs) illustrated herein was collected from shell beds interpreted as tidal ravinement surfaces. The fauna includes terebratulid brachiopods, bivalves of the families Malletiidae, Mytilidae, Pinnidae, Ostreidae, Pectinidae, Carditidae, Crassatellidae, Lahillidae, Mactridae, Veneridae, and Hiatellidae, and gastropods of the families Trochidae and Calyptraeidae, and a member of Archaeogastropoda of uncertain affinities. The similarities of this fauna with that recorded in the Upper Member of the Río Turbio Formation, together with 87Sr/86Sr ages, sug- gest a late Middle Eocene age for the Man Aike Formation. Resumen. PALEONTOLOGÍA Y SEDIMENTOLOGÍA DE LAS ROCAS DEL EOCENO MEDIO EXPUESTAS EN EL ÁREA DE LAGO ARGENTINO, PROVINCIA DE SANTA CRUZ, ARGENTINA. Los estudios sedimentológicos y paleontológicos real- izados en rocas asignadas a la Formación Man Aike, expuestas en la estancia 25 de Mayo, al sur de Calafate, provincia de Santa Cruz, Argentina, sugieren que esta unidad representa la evolución de un valle inciso desde ambientes fluviales a marinos durante el Eoceno medio tardío. -
The Recent Molluscan Marine Fauna of the Islas Galápagos
THE FESTIVUS ISSN 0738-9388 A publication of the San Diego Shell Club Volume XXIX December 4, 1997 Supplement The Recent Molluscan Marine Fauna of the Islas Galapagos Kirstie L. Kaiser Vol. XXIX: Supplement THE FESTIVUS Page i THE RECENT MOLLUSCAN MARINE FAUNA OF THE ISLAS GALApAGOS KIRSTIE L. KAISER Museum Associate, Los Angeles County Museum of Natural History, Los Angeles, California 90007, USA 4 December 1997 SiL jo Cover: Adapted from a painting by John Chancellor - H.M.S. Beagle in the Galapagos. “This reproduction is gifi from a Fine Art Limited Edition published by Alexander Gallery Publications Limited, Bristol, England.” Anon, QU Lf a - ‘S” / ^ ^ 1 Vol. XXIX Supplement THE FESTIVUS Page iii TABLE OF CONTENTS INTRODUCTION 1 MATERIALS AND METHODS 1 DISCUSSION 2 RESULTS 2 Table 1: Deep-Water Species 3 Table 2: Additions to the verified species list of Finet (1994b) 4 Table 3: Species listed as endemic by Finet (1994b) which are no longer restricted to the Galapagos .... 6 Table 4: Summary of annotated checklist of Galapagan mollusks 6 ACKNOWLEDGMENTS 6 LITERATURE CITED 7 APPENDIX 1: ANNOTATED CHECKLIST OF GALAPAGAN MOLLUSKS 17 APPENDIX 2: REJECTED SPECIES 47 INDEX TO TAXA 57 Vol. XXIX: Supplement THE FESTIVUS Page 1 THE RECENT MOLLUSCAN MARINE EAUNA OE THE ISLAS GALAPAGOS KIRSTIE L. KAISER' Museum Associate, Los Angeles County Museum of Natural History, Los Angeles, California 90007, USA Introduction marine mollusks (Appendix 2). The first list includes The marine mollusks of the Galapagos are of additional earlier citations, recent reported citings, interest to those who study eastern Pacific mollusks, taxonomic changes and confirmations of 31 species particularly because the Archipelago is far enough from previously listed as doubtful. -
South Carolina State Water Assessment, 2Nd Ed., Chapter 1
SOUTH Carolina IN PERSPECTIVE SOCIOECONOMIC ENVironment influx of capital and population advanced the economy from an agricultural base to a 21st-century economy that Geography has played an important role in South is dominated by manufacturing and is well diversified by Carolina’s history and development. Archaeological agriculture and tourism. evidence shows us that early Indian inhabitants found the land and climate well suited for hunting and gathering Population and later for agriculture. Spanish, French, and English explorers discovered that South Carolina’s harbors and South Carolina’s population increased from rivers provided ingress to the New World and its vast about 250,000 in 1790 to more than 4 million in 2005 resources. The settlers who followed on the heels of (Figure 1-1). The nearly one-million person increase exploration exploited the land and streams of the lower between 1980 and 2005 accounted for 27 percent of the Coastal Plain, and for almost 200 years they enjoyed a state’s growth during the past two centuries. Population predominantly agricultural economy based first on indigo growth is above the national average and is expected to and rice and later on cotton, tobacco, and timber. Abundant continue at an above-average rate owing to factors such as land, water, and labor and a mild climate attracted the state’s mild climate, natural attractions, favorable tax national and international investment and a migration to and labor laws, and relatively low cost of living. the State during the middle and late 20th century. That 6,000 5,000 4,000 3,000 opulation, in thousands P 2,000 1,000 0 0 1790 1800 1810 1820 1830 1840 1850 1860 1870 1880 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 200 2010 2020 2030 Year Figure 1-1. -
Thyasirid Bivalves from Cretaceous and Paleogene Cold Seeps
Thyasirid bivalves from Cretaceous and Paleogene cold seeps KRZYSZTOF HRYNIEWICZ, KAZUTAKA AMANO, ROBERT G. JENKINS, and STEFFEN KIEL Hryniewicz, K., Amano, K., Jenkins, R.G., and Kiel, S. 2017. Thyasirid bivalves from Cretaceous and Paleogene cold seeps. Acta Palaeontologica Polonica 62 (4): 705–728. We present a systematic study of thyasirid bivalves from Cretaceous to Oligocene seep carbonates worldwide. Eleven species of thyasirid bivalves are identified belonging to three genera: Conchocele, Maorithyas, and Thyasira. Two spe- cies are new: Maorithyas humptulipsensis sp. nov. from middle Eocene seep carbonates in the Humptulips Formation, Washington State, USA, and Conchocele kiritachiensis sp. nov. from the late Eocene seep deposit at Kiritachi, Hokkaido, Japan. Two new combinations are provided: Conchocele townsendi (White, 1890) from Maastrichtian strata of the James Ross Basin, Antarctica, and Maorithyas folgeri (Wagner and Schilling, 1923) from Oligocene rocks from California, USA. Three species are left in open nomenclature. We show that thyasirids have Mesozoic origins and appear at seeps be- fore appearing in “normal” marine environments. These data are interpreted as a record of seep origination of thyasirids, and their subsequent dispersal to non-seep environments. We discuss the age of origination of thyasirids in the context of the origin of the modern deep sea fauna and conclude that thyasirids could have deep sea origins. This hypothesis is supported by the observed lack of influence of the Cretaceous and Paleogene Oceanic Anoxic Events on the main evolutionary lineages of the thyasirids, as seen in several other members of the deep sea fauna. Key words: Bivalvia, Thyasiridae, cold seeps, deep sea, ecology, evolution, Cretaceous, Paleogene. -
Aperçus D'un Écosystème Marin Et De Ses Abords Au Maastrichtien
Aperçus d’un écosystème marin et de ses abords au Maastrichtien supérieur: le site nigérien d’In Daman et la mer épicontinentale du bassin des Iullemmeden Marc Michaut To cite this version: Marc Michaut. Aperçus d’un écosystème marin et de ses abords au Maastrichtien supérieur: le site nigérien d’In Daman et la mer épicontinentale du bassin des Iullemmeden. 2013. hal-00797424 HAL Id: hal-00797424 https://hal.archives-ouvertes.fr/hal-00797424 Preprint submitted on 6 Mar 2013 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Aperçus d’un écosystème marin et de ses abords au Maastrichtien supérieur : le site nigérien d’In Daman et la mer épicontinentale du bassin des Iullemmeden Marc Michaut Institut préparatoire aux études scientifiques et techniques, Université de Tunis, La Marsa, Tunisie 5 mars 2013 Abstract Many studies were performed for several decades about Nigerian maastrichtian sites and other fossiliferous sites of the same epoch in their vicinity, which allow us to reconstruct the marine epicontinental ecosystem and associated coastal ecosystems with a fair amount of accuracy. We begin with a detailed compilation of the re- sults obtained about biotope and taphocenose. -
Spissatella Trailli (Lectotype TM2859 – Awamoa, Oamaru, New Zealand)
JOURNEYS THROUGH SHAPE AND TIME: PALAEOBIOLOGY OF CENOZOIC NEW ZEALAND SPISSATELLA AND EUCRASSATELLA (BIVALVIA, CRASSATELLIDAE) by Katie Susanna Collins A thesis submitted to the Victoria University of Wellington in fulfillment of the requirements for the degree of Doctor of Philosophy Victoria University of Wellington 2013 Spissatella trailli (Lectotype TM2859 – Awamoa, Oamaru, New Zealand) i ii ABSTRACT A novel, highly-integrated approach combining morphometric, stratocladistic and sclerochronological methods has been applied to two genera of New Zealand Cenozoic crassatellid bivalve (Family Crassatellidae): Spissatella Finlay, 1926 and Eucrassatella Iredale, 1924. This study builds on previous work on Spissatella that demonstrated their amenability to shape analysis and provided a foundation for evolutionary studies of the group. The taxonomy of these crassatellids has been in need of revision; a number of changes to generic placement having been proposed in recent publications without redescription. These bivalves are character-depauperate and known only from fossil material within New Zealand, making them challenging subjects for the phylogenetic analysis that would, ideally, inform taxonomic revision. Geometric morphometric methods have been used to characterise the morphological variation of the study group in terms of shape. Landmarks/semilandmarks that capture internal hard-part morphology and external shell shape, have been compared with internal landmarks only, outline shape semilandmarks only, and outline shape Fourier transform methods, and are shown to best combine comprehensive coverage of total shell form with high correct reassignment of individuals to taxa in multidimensional morphospace. Procrustes- superimposed landmark/semilandmark configurations have been ordinated using Principal Components Analysis (PCA), and PCA plots have been used to compare the shape variation of each species. -
TREATISE ONLINE Number 48
TREATISE ONLINE Number 48 Part N, Revised, Volume 1, Chapter 31: Illustrated Glossary of the Bivalvia Joseph G. Carter, Peter J. Harries, Nikolaus Malchus, André F. Sartori, Laurie C. Anderson, Rüdiger Bieler, Arthur E. Bogan, Eugene V. Coan, John C. W. Cope, Simon M. Cragg, José R. García-March, Jørgen Hylleberg, Patricia Kelley, Karl Kleemann, Jiří Kříž, Christopher McRoberts, Paula M. Mikkelsen, John Pojeta, Jr., Peter W. Skelton, Ilya Tëmkin, Thomas Yancey, and Alexandra Zieritz 2012 Lawrence, Kansas, USA ISSN 2153-4012 (online) paleo.ku.edu/treatiseonline PART N, REVISED, VOLUME 1, CHAPTER 31: ILLUSTRATED GLOSSARY OF THE BIVALVIA JOSEPH G. CARTER,1 PETER J. HARRIES,2 NIKOLAUS MALCHUS,3 ANDRÉ F. SARTORI,4 LAURIE C. ANDERSON,5 RÜDIGER BIELER,6 ARTHUR E. BOGAN,7 EUGENE V. COAN,8 JOHN C. W. COPE,9 SIMON M. CRAgg,10 JOSÉ R. GARCÍA-MARCH,11 JØRGEN HYLLEBERG,12 PATRICIA KELLEY,13 KARL KLEEMAnn,14 JIřÍ KřÍž,15 CHRISTOPHER MCROBERTS,16 PAULA M. MIKKELSEN,17 JOHN POJETA, JR.,18 PETER W. SKELTON,19 ILYA TËMKIN,20 THOMAS YAncEY,21 and ALEXANDRA ZIERITZ22 [1University of North Carolina, Chapel Hill, USA, [email protected]; 2University of South Florida, Tampa, USA, [email protected], [email protected]; 3Institut Català de Paleontologia (ICP), Catalunya, Spain, [email protected], [email protected]; 4Field Museum of Natural History, Chicago, USA, [email protected]; 5South Dakota School of Mines and Technology, Rapid City, [email protected]; 6Field Museum of Natural History, Chicago, USA, [email protected]; 7North -
Mollusca, Bivalvia): Protocardiinae, Laevicardiinae, Lahilliinae, Tulongocardiinae Subfam
Zoologica Scripta, Vol. 24, No. 4, pp. 321-346, 1995 Pergamon Elsevier Science Ltd The Norwegian Academy of Science and Letters Printed in Great Britain 0300-3256(95)00011-9 Phytogeny of the Cardiidae (Mollusca, Bivalvia): Protocardiinae, Laevicardiinae, Lahilliinae, Tulongocardiinae subfam. n. and Pleuriocardiinae subfam. n. JAY A. SCHNEIDER Accepted 7 June 1995 Schneider, J.A. 1995. Phytogeny of the Cardiidae (Mollusca, Bivalvia): Protocardiinae, Laevicar- diinae, Lahilliinae, Tulongocardiinae subfam.n. and Pleuriocardiinae subfam.n.—Zool. Scr. 24: 321-346. In a preliminary cladistic analysis of the bivalve family Cardiidae (Schneider 1992), members of the subfamilies Protocardiinae, Lahilliinae, and Laevicardiinae, plus the genus Nemocardium, were found to be the least derived taxa of cardiids. A cladistic analysis is undertaken of the genera and subgenera of these cardiid taxa, plus several Mesozoic taxa which have never been assigned to any subfamily. The Late Triassic Tulongocardium, which is placed in Tulongocardiinae subfam. n., is the sister taxon to all other cardiids. Protocardiinae is restricted to the genus Protocardia. Most other Mesozoic taxa which have been placed in the Protocardiinae are found to be members of the Lahilliinae. Nemocardium is placed in the Laevicardiinae. Incacardium, Pleuriocardia, and Dochmocardia form a monophyletic group, Pleuriocardiinae subfam. n. Pleuriocardiinae, Laevi- cardiinae, and the remaining members of the Cardiidae (herein informally termed "cucardiids") form a monophyletic group. Jay A. Schneider, Smithsonian Tropical Research Institute, Box2072, Balboa, Republic of Panama. Present address: Department of Geology, Youngstown State University, Youngstown, OH 44555- 3672, C/.S./l. re7..2;6-742-77JJ;Fa%.276-742-/7J4 Introduction Bivalves of the family Cardiidae (cockles and giant clams) Outgroup Palaeocardita originated in the Late Triassic and have a present-day Septocardia diversity of nearly 200 species (Rosewater 1965; Fischer- Protocardia | PROTOCARDIINAE Integricardium I Piette 1977). -
The Family Carditidae (Bivalvia) in the Early Danian of Patagonia (Argentina)
Journal of Paleontology, 91(6), 2017, p. 1148–1165 Copyright © 2017, The Paleontological Society 0022-3360/17/0088-0906 doi: 10.1017/jpa.2017.69 The family Carditidae (Bivalvia) in the early Danian of Patagonia (Argentina) Damián E. Pérez and Claudia J. del Río Museo Argentino de Ciencias Naturales Bernardino Rivadavia, División Paleoinvertebrados, Av. Ángel Gallardo 470 (C1405DJR), Buenos Aires, Argentina. 〈[email protected]〉; 〈[email protected]〉 Abstract.—The first systematic analysis of the Danian carditids of Patagonia is presented, which includes four genera—one new genus and the first records of three other genera in South America. They consist of Claibornicardia paleopatagonica (Ihering, 1903), a widely distributed species occuring in the Jagüel, Roca and Salamanca formations (Neuquén, Río Negro and Chubut Provinces); Rotundicardia Heaslip, 1968, represented by the new species R. mariobrosorum n.sp.,whichisrestrictedtotheRocaFormation(RíoNegroProvince);Cardites feruglioi (Petersen, 1846) (Roca and Lefipán formations, Río Negro and Chubut Provinces); and by Kalelia new genus, which includes K. burmeisteri (Böhm, 1903) from the Salamanca and Roca formations (Río Negro and Chubut Provinces), which is rela- ted to the Paris Basin species K. multicostata (Lamarck, 1806) n. comb. and K. pectuncularis (Lamarck, 1806) n. comb. ‘Venericardia’ iheringi (Böhm, 1903), a species known only from internal molds, is described and regarded as a carditid with uncertain affinities. The presence of Claibornicardia, Rotundicardia,andCardites in Patagonia constitutes the most ancient record of these genera and confirms biogeographical connections previously established between the Danian Argentinian and North American/European fossil faunas. Introduction Although an abundant and greatly diversified group in Patagonia, Cenozoic carditids, and particularly those of Danian The family Carditidae Férussac, 1822 comprises a large group age, remain almost completely unstudied. -
Chec List Marine and Coastal Biodiversity of Oaxaca, Mexico
Check List 9(2): 329–390, 2013 © 2013 Check List and Authors Chec List ISSN 1809-127X (available at www.checklist.org.br) Journal of species lists and distribution ǡ PECIES * S ǤǦ ǡÀ ÀǦǡ Ǧ ǡ OF ×±×Ǧ±ǡ ÀǦǡ Ǧ ǡ ISTS María Torres-Huerta, Alberto Montoya-Márquez and Norma A. Barrientos-Luján L ǡ ǡǡǡǤͶǡͲͻͲʹǡǡ ǡ ȗ ǤǦǣ[email protected] ćĘęėĆĈęǣ ϐ Ǣ ǡǡ ϐǤǡ ǤǣͳȌ ǢʹȌ Ǥͳͻͺ ǯϐ ʹǡͳͷ ǡͳͷ ȋǡȌǤǡϐ ǡ Ǥǡϐ Ǣ ǡʹͶʹȋͳͳǤʹΨȌ ǡ groups (annelids, crustaceans and mollusks) represent about 44.0% (949 species) of all species recorded, while the ʹ ȋ͵ͷǤ͵ΨȌǤǡ not yet been recorded on the Oaxaca coast, including some platyhelminthes, rotifers, nematodes, oligochaetes, sipunculids, echiurans, tardigrades, pycnogonids, some crustaceans, brachiopods, chaetognaths, ascidians and cephalochordates. The ϐϐǢ Ǥ ēęėĔĉĚĈęĎĔē Madrigal and Andreu-Sánchez 2010; Jarquín-González The state of Oaxaca in southern Mexico (Figure 1) is and García-Madrigal 2010), mollusks (Rodríguez-Palacios known to harbor the highest continental faunistic and et al. 1988; Holguín-Quiñones and González-Pedraza ϐ ȋ Ǧ± et al. 1989; de León-Herrera 2000; Ramírez-González and ʹͲͲͶȌǤ Ǧ Barrientos-Luján 2007; Zamorano et al. 2008, 2010; Ríos- ǡ Jara et al. 2009; Reyes-Gómez et al. 2010), echinoderms (Benítez-Villalobos 2001; Zamorano et al. 2006; Benítez- ϐ Villalobos et alǤʹͲͲͺȌǡϐȋͳͻͻǢǦ Ǥ ǡ 1982; Tapia-García et alǤ ͳͻͻͷǢ ͳͻͻͺǢ Ǧ ϐ (cf. García-Mendoza et al. 2004). ǡ ǡ studies among taxonomic groups are not homogeneous: longer than others. Some of the main taxonomic groups ȋ ÀʹͲͲʹǢǦʹͲͲ͵ǢǦet al.