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Review of the Geology and Paleontology of the Ellsworth Mountains, Antarctica
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Short Research Paper 107; doi:10.3133/of2007-1047.srp107 Review of the geology and paleontology of the Ellsworth Mountains, Antarctica G.F. Webers¹ and J.F. Splettstoesser² ¹Department of Geology, Macalester College, St. Paul, MN 55108, USA ([email protected]) ²P.O. Box 515, Waconia, MN 55387, USA ([email protected]) Abstract The geology of the Ellsworth Mountains has become known in detail only within the past 40-45 years, and the wealth of paleontologic information within the past 25 years. The mountains are an anomaly, structurally speaking, occurring at right angles to the Transantarctic Mountains, implying a crustal plate rotation to reach the present location. Paleontologic affinities with other parts of Gondwanaland are evident, with nearly 150 fossil species ranging in age from Early Cambrian to Permian, with the majority from the Heritage Range. Trilobites and mollusks comprise most of the fauna discovered and identified, including many new genera and species. A Glossopteris flora of Permian age provides a comparison with other Gondwana floras of similar age. The quartzitic rocks that form much of the Sentinel Range have been sculpted by glacial erosion into spectacular alpine topography, resulting in eight of the highest peaks in Antarctica. Citation: Webers, G.F., and J.F. Splettstoesser (2007), Review of the geology and paleontology of the Ellsworth Mountains, Antarctica, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES, edited by A.K. Cooper and C.R. Raymond et al., USGS Open- File Report 2007-1047, Short Research Paper 107, 5 p.; doi:10.3133/of2007-1047.srp107 Introduction The Ellsworth Mountains are located in West Antarctica (Figure 1) with dimensions of approximately 350 km long and 80 km wide. -
Enrico SCHWABE Zoologische Staatssammlung Muenchen
. , E. SCHWABE NOVAPEX 6 (4): 89-105, 10 décembre 2005 A catalogue of Récent and fossil chitons (MoUusca: Polyplacophora) Addenda Enrico SCHWABE Zoologische Staatssammlung Muenchen, Muenchhausenstrasse 2 1 D-81247 Muenchen, Germany [email protected] KEYWORDS. MoUusca, Polyplacophora, taxon list, bibliography ABSTRACT. This paper lists species-group names of Récent and fossil Polyplacophora (MoUusca) that were published after 1998 (for the Récent species) and 1987 (for the fossil species). A total of 171 species were since then introduced, of which 123 are attributed to valid fossil taxa and 48 to valid Récent taxa. The authorship and complète références are provided for each species-group name. INTRODUCTION Considerazioni suUa famiglia Leptochitonidae Dali, 1889 (MoUusca: Polyplacophora). III. Le species Taxonomic work is impossible without an overview of terziarie e quatemarie Europee, con note sistematiche the scientific names existing in the particular taxon e filogenetiche. - Atti délia prima Giornata di Studi group. Catalogues generally are a great tool to obtain Malacologici Centra lîaliano di Studi Malacologici such overviews, as they often summarize information (1989): 19-140 (: 79; pi. 26). otherwise hard to gather and master. Type locality: Pezzo, near Villa S. Giovanni (Reggio Of the nearly 2600 taxa introduced on species level Calabria prov.); in material of upper Pleistocene, but within the Polyplacophora, 368 fossils and 914 Récent presumably originated from adjacent deposits of lower species are considered as valid (closing date: Pleistocene of bathyal faciès [Pezzo, presso Villa S. 31/10/2005). Giovanni (RC); in materiale del Pleistocene superiore, In the past, excellent catalogues of species-group ma presumibilmente originato da contigui depositi del names in Polyplacophora were compiled by Kaas & Pleistocene inferiore di faciès batiale]. -
JEFFERSONIANA Contributions from the Virginia Museum of Natural History
JEFFERSONIANA Contributions from the Virginia Museum of Natural History Number 19 10 January 2009 Unusual Cambrian Thrombolites from the Boxley Blue Ridge Quarry, Bedford County, Virginia Alton C. Dooley, Jr. ISSN 1061-1878 Virginia Museum of Natural History Jeffersoniana, Number 19, pp. 1-14 Scientific Publications Series Virginia Museum of Natural History The Virginia Museum of Natural History produces five scientific Unusual Cambrian Thrombolites from the Boxley Blue publication series, with each issue published as suitable material becomes Ridge Quarry, Bedford County, Virginia available and each numbered consecutively within its series. Topics consist of original research conducted by museum staff or affiliated ALTON C. DOOLEY , JR. investigators based on the museum’s collections or on subjects relevant to Virginia Museum of Natural History the museum’s areas of interest. All are distributed to other museums and 21 Starling Avenue libraries through our exchange program and are available for purchase by Martinsville, Virginia 24112, USA individual consumers. [email protected] Memoirs are typically larger productions: individual monographs on ABSTRACT a single subject such as a regional survey or comprehensive treatment of an entire group. The standardized format is an 8.5 x 11 inch page with two Three unusual thrombolites were collected in June 2008 from the Late columns. Cambrian Conococheague Formation at the Boxley Materials Blue Ridge Quarry in Bedford County, Virginia. These specimens are isolated low domes Jeffersoniana is an outlet for relatively short studies treating a single with a thrombolitic core and a pustulate, stromatolitic outer layer. The two subject, allowing for expeditious publication. The standardized format is largest domes have a distinctive thickened rim around their margins. -
Morphology and Systematic Position of Tryhlidium Canadense Whiteaves
Morphology and systematic position of Tryblidium canadense Whiteaves, 1884 (Mollusca) from the Silurian of North America JOHNS. PEEL Peel, J. S.: Morphology and systematic position of Tryblidium Canadense Whiteaves, 1884 (Mollusca) from the Silurian of North America. Bull. geol. Soc. Denmark, vol. 38, pp. 43-51. Copenhagen, April 25th, 1990. https://doi.org/10.37570/bgsd-1990-38-04 The nomenclative history of Tryblidium canadense Whiteaves, 1884, a large, oval, univalved mollusc originally described from the Silurian Guelph Formation of Ontario, is reviewed. Following comparison to Archinace/la Ulrich & Scofield, 1897, in which genus it has generally been placed for almost a century, Whiteaves' species is redescribed and assigned to a new gastropod genus, Guelphinace/la. John S. Peel, Geological Survey of Greenland, Oster Voldgade JO, 1350 Copenhagen K, Denmark. February 10th, 1989. Whiteaves (1884) described a single internal the sub-apical wall. He commented that the mould of a large (45 mm), oval, univalved mol structure seemed to be a single continuous mus lusc from the Guelph Formation (Silurian) of cular impression and not two separate depres Hespeler, Ontario, Canada as Tryblidium Cana sions, as suggested by Lindstrom (1884), al dense (Fig. 1). Uncertainty surrounding its sys though he did not refer directly to the latter's tematic position developed immediately when description. He made no reference to the thin Lindstrom (1884) questioned the assignment to dorsal band which Lindstrom (1884) had consid the genus Tryblidium -
Shell Microstructures in Early Cambrian Molluscs
Shell microstructures in Early Cambrian molluscs ARTEM KOUCHINSKY Kouchinsky, A. 2000. Shell microstructures in Early Cambrian molluscs. - Acta Palaeontologica Polonica 45,2, 119-150. The affinities of a considerable part of the earliest skeletal fossils are problematical, but investigation of their microstructures may be useful for understanding biomineralization mechanisms in early metazoans and helpful for their taxonomy. The skeletons of Early Cambrian mollusc-like organisms increased by marginal secretion of new growth lamel- lae or sclerites, the recognized basal elements of which were fibers of apparently aragon- ite. The juvenile part of some composite shells consisted of needle-like sclerites; the adult part was built of hollow leaf-like sclerites. A layer of mineralized prism-like units (low aragonitic prisms or flattened spherulites) surrounded by an organic matrix possibly existed in most of the shells with continuous walls. The distribution of initial points of the prism-like units on a periostracurn-like sheet and their growth rate were mostly regular. The units may be replicated on the surface of internal molds as shallow concave poly- gons, which may contain a more or less well-expressed tubercle in their center. Tubercles are often not enclosed in concave polygons and may co-occur with other types of tex- tures. Convex polygons seem to have resulted from decalcification of prism-like units. They do not co-occur with tubercles. The latter are interpreted as casts of pore channels in the wall possibly playing a role in biomineralization or pits serving as attachment sites of groups of mantle cells. Casts of fibers and/or lamellar units may overlap a polygonal tex- ture or occur without it. -
Zootaxa, the Youngest Rostroconch Mollusc from North America
Zootaxa 2603: 61–64 (2010) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Correspondence ZOOTAXA Copyright © 2010 · Magnolia Press ISSN 1175-5334 (online edition) The youngest rostroconch mollusc from North America, Minycardita capitanensis n. sp. MICHAEL J. VENDRASCO1, RICHARD D. HOARE2 & GORDEN L. BELL, JR3 1Department of Biological Science, California State University, Fullerton, Fullerton, CA 92834-6850, USA. E-mail: [email protected] 2Department of Geology, Bowling Green State University, Bowling Green, OH 43403, USA. E-mail: [email protected] 3Guadalupe Mountains National Park, 400 Pine Canyon Drive, Salt Flat, TX 79847, USA. E-mail: [email protected] Rostroconchs are an extinct class of mollusc that lived worldwide through most or all of the Paleozoic Era (Runnegar 1978). They were most diverse in the early Paleozoic (Pojeta 1985), perhaps due to a lower rate of evolution in the rostroconch clade that survived the end-Ordovician mass extinction event (Wagner 1997). Rostroconchs have a univalved larval shell and a pseudo-bivalved adult shell. Their ecology appears to have ranged from infaunal to rarely epifaunal, and from deposit to suspension feeding (Pojeta et al. 1972, Pojeta & Runnegar 1976, Runnegar 1978, Pojeta 1987). A single but well-preserved, essentially complete rostroconch specimen was recovered from the region surrounded by the famous Capitan Reef of the Permian of West Texas (Newell et al. 1953). In particular, the specimen is from the upper scaphopod bed of the Reef Trail Member of the Bell Canyon Formation exposed in the Guadalupe Mountains National Park (Rigby & Bell 2005: fig. 2). The fusulinid biostratigraphic zonal indicator Paraboultonia splendens Skinner & Wilde, 1954 occurs both below the upper scaphopod bed and above it, indicating that this horizon was deposited during the latest Guadalupian (late middle Permian) (Rigby & Bell 2006), and thus is the youngest known deposit in North America to contain a rostroconch. -
The Youngest Representatives of the Genus Ribeiria Sharpe, 1853 from the Late Katian of the Prague Basin (Bohemia)
Estonian Journal of Earth Sciences, 2015, 64, 1, 84–90 doi: 10.3176/earth.2015.15 The youngest representatives of the genus Ribeiria Sharpe, 1853 from the late Katian of the Prague Basin (Bohemia) Marika Polechová Czech Geological Survey, Klárov 3, 11821 Prague 1, Czech Republic; [email protected] Received 2 July 2014, accepted 6 October 2014 Abstract. Ribeiria apusoides and Ribeiria johni sp. nov. are described from the late Katian of the Prague Basin (Bohemia) as the youngest representatives of the genus Ribeiria. The Ordovician ribeirioids from Bohemia (Perunica) show close affinities to the ribeirioids from Armorica and Iberia. The functional morphology of ribeirioids, mainly the pedal muscle system, is discussed, based on very well-preserved specimens of R. apusoides. The ribeirioids attained their diversity in the Lower Ordovician, since the Middle Ordovician their diversity declines, and during the late Katian only three genera are known worldwide. They are unknown from the Hirnantian but the last ribeirioids are recorded from the lower Silurian in South China. Key words: Ribeirioida, systematics, functional morphology, Ordovician, Prague Basin. INTRODUCTION Pojeta & Runnegar (1976) briefly described and figured all known species of rostroconchs, including also species The study of rostroconchs was started by Martin (1809) of ribeirioids from the Ordovician of the Prague Basin and Sowerby (1815), but the systematic position of the (Czech Republic). The rich material of rostroconchs group was for a long time unclear. Rostroconchs were from the Czech Republic is one of the best-preserved allied mainly to bivalves (Branson et al. 1969) or materials. It includes ribeirioids from the late Katian even to arthropods (Schubert & Waagen 1904; Kobayashi (Králův Dvůr Formation), among them the worldwide 1933). -
Falcidens Longus2.Pdf
Falcidens longus Scheltema 1998 Mollusca, Caudofoveata: Falcidentidae SCAMIT Supplement Vol. 23 SCAMIT CODE: None Date Examined: 05 April 2005 Voucher By: K. Barwick/D. Cadien SYNONYMY: Falcidens sp B SCAMIT 1985§ LITERATURE: Scheltema, 1998 DIAGNOSTIC CHARACTERS: 1. Body regionated (Figure A), BLI 5.5-8.9; anterium somewhat inflated, separated from neck by a constriction; neck short, separated from anterior trunk by constriction; anterior trunk significantly longer than posterior trunk; posterior trunk larger in diameter than any other region except anterium. 2. Posterium slightly expanded, not set off from posterior trunk by a narrowing; spicular fring of posterium long, extending well beyond peribranchial plate (Figure C); plate flat to very slightly convex, covered with radiating spicules; no peribranchial skirt evident 3. Oral shield dorsally incised, wider than tall (Figure B), with small, poorly defined dorsal lobes; about ½ as wide as anterium. 4. Radular denticles large, sickle-shaped, and meeting at the top of the radular cone; triangular plate present (can be lost); radular cone barely tapering in frontal view (Figure D), normally tapering in lateral view; cone much narrower in frontal than in lateral view. 5. Mid-anterior trunk spicules centrally keeled, with thickened edges; a few lateral ridges may be present. Under birefringence mid-anterior spicule colors, typically are white with yellowish brown ridges with the central keel being darkest. (Figures F) RELATED SPECIES AND CHARACTER DIFFERENCES: 1. Despite its name, Falcidens longus has a BLI which places it among the short group of chaetodermomorph species in the NEP. Other members of this group are Chaetoderma californicum, C. nanulum, C. -
Cambrian Substrate Revolution
Vol. 10, No. 9 September 2000 INSIDE • Research Grants, p. 12 • Section Meetings Northeastern, p. 16 GSA TODAY Southeastern, p. 18 A Publication of the Geological Society of America • Happy Birthday, NSF, p. 22 The Cambrian Substrate Revolution David J. Bottjer, Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, [email protected] James W. Hagadorn, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, [email protected] Stephen Q. Dornbos, Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, [email protected] ABSTRACT The broad marine ecological settings prevalent during the late Neo- proterozoic–early Phanerozoic (600–500 Ma) interval of early metazoan body plan origination strongly impacted the subsequent evolution and development of benthic metazoans. Recent work demonstrates that late Neoproterozoic seafloor sediment had well-developed microbial mats and poorly developed, vertically oriented bioturbation, thus producing fairly stable, relatively low water content substrates and a sharp water-sediment interface. Later in the Cambrian, seafloors with microbial mats became increasingly scarce in shallow-marine environments, largely due to the evolution of burrowing organisms with an increasing vertically oriented component to their bioturba- tion. The evolutionary and ecological effects of these substrate changes on Figure 1. Looping and meandering trace fossil Taphrhelminthopsis, made by a large Early Cambrian benthic metazoans, referred to as the bioturbator, on a bedding plane from Lower Cambrian Poleta Formation, White-Inyo Mountains, California. Such traces, consisting of a central trough between lateral ridges, occur in sandstones Cambrian substrate revolution, are deposited in shallow-marine environments. -
Keeping a Lid on It: Muscle Scars and the Mystery of the Mobergellidae
1 Keeping a lid on it: muscle scars and the mystery of the 2 Mobergellidae 3 4 TIMOTHY P. TOPPER1,2* and CHRISTIAN B. SKOVSTED1 5 6 1Department of Palaeobiology, Swedish Museum of Natural History, P.O. Box 50007, 7 SE-104 05, Stockholm, Sweden. 8 2Palaeoecosystems Group, Department of Earth Sciences, Durham University, Durham 9 DH1 3LE, UK. 10 11 Mobergellans were one of the first Cambrian skeletal groups to be recognized yet have 12 long remained one of the most problematic in terms of biological function and affinity. 13 Typified by a disc-shaped, phosphatic sclerite the most distinctive character of the 14 group is a prominent set of internal scars, interpreted as representing sites of former 15 muscle attachment. Predominantly based on muscle scar distribution, mobergellans 16 have been compared to brachiopods, bivalves and monoplacophorans, however a 17 recurring theory that the sclerites acted as operculum remains untested. Rather than 18 correlate the number of muscle scars between taxa, here we focus on the percentage of 19 the inner surface shell area that the scars constitute. We investigate two mobergellan 20 species, Mobergella holsti and Discinella micans comparing the Cambrian taxa with the 21 muscle scars of a variety of extant and fossil marine invertebrate taxa to test if the 22 mobergellan muscle attachment area is compatible with an interpretation as operculum. 23 The only skeletal elements in our study with a comparable muscle attachment 24 percentage are gastropod opercula. Complemented with additional morphological 25 information, our analysis supports the theory that mobergellan sclerites acted as an 26 operculum presumably from a tube-living organism. -
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, -
2020 Interim Receiving Waters Monitoring Report
POINT LOMA OCEAN OUTFALL MONTHLY RECEIVING WATERS INTERIM RECEIVING WATERS MONITORING REPORT FOR THE POINTM ONITORINGLOMA AND SOUTH R EPORTBAY OCEAN OUTFALLS POINT LOMA 2020 WASTEWATER TREATMENT PLANT NPDES Permit No. CA0107409 SDRWQCB Order No. R9-2017-0007 APRIL 2021 Environmental Monitoring and Technical Services 2392 Kincaid Road x Mail Station 45A x San Diego, CA 92101 Tel (619) 758-2300 Fax (619) 758-2309 INTERIM RECEIVING WATERS MONITORING REPORT FOR THE POINT LOMA AND SOUTH BAY OCEAN OUTFALLS 2020 POINT LOMA WASTEWATER TREATMENT PLANT (ORDER NO. R9-2017-0007; NPDES NO. CA0107409) SOUTH BAY WATER RECLAMATION PLANT (ORDER NO. R9-2013-0006 AS AMENDED; NPDES NO. CA0109045) SOUTH BAY INTERNATIONAL WASTEWATER TREATMENT PLANT (ORDER NO. R9-2014-0009 AS AMENDED; NPDES NO. CA0108928) Prepared by: City of San Diego Ocean Monitoring Program Environmental Monitoring & Technical Services Division Ryan Kempster, Editor Ami Latker, Editor June 2021 Table of Contents Production Credits and Acknowledgements ...........................................................................ii Executive Summary ...................................................................................................................1 A. Latker, R. Kempster Chapter 1. General Introduction ............................................................................................3 A. Latker, R. Kempster Chapter 2. Water Quality .......................................................................................................15 S. Jaeger, A. Webb, R. Kempster,