Phylogenesis and the System of the Cambrian Univalved Mollusks P
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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. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
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, -
The Functional Morphology of the Cambrian Univalved Mollusks— Helcionellids
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/236216830 The Functional Morphology of the Cambrian Univalved Mollusks— Helcionellids. 1 Article in Paleontological Journal · July 2000 CITATIONS READS 29 411 1 author: Pavel Parkhaev Russian Academy of Sciences 85 PUBLICATIONS 1,150 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Worldwide Cambrian molluscan fauna View project All content following this page was uploaded by Pavel Parkhaev on 29 May 2014. The user has requested enhancement of the downloaded file. Paleontological Journal, Vol. 34, No. 4, 2000, pp. 392–399. Translated from Paleontologicheskii Zhurnal, No. 4, 2000, pp. 32–39. Original Russian Text Copyright © 2000 by Parkhaev. English Translation Copyright © 2000 by åÄIä “Nauka /Interperiodica” (Russia). The Functional Morphology of the Cambrian Univalved Mollusks—Helcionellids. 1 P. Yu. Parkhaev Paleontological Institute, Russian Academy of Sciences, ul. Profsoyuznaya 123, Moscow, 117868 Russia Received October 21, 1998 Abstract—The soft-body anatomy of helcionellids is reconstructed on the basis of a morphofunctional analy- ses of their shells. Evidently, two systems for the internal organization of helcionellids are possible: the first corresponds to that of the gastropodian class; the second, to that of the monoplacophorian. INTRODUCTION maximum number of analogies and the least number of contradictions with recent animals. Intensive study of the Cambrian fauna and stratigra- phy during recent decades shows us a diverse biota of Helcionellids were common elements of the mala- this geological period. Mollusks are well represented cofauna in the Early–Middle Cambrian and achieved a among the numerous newly described taxa in a variety rather high taxonomic diversity in comparison with of groups. -
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. -
Totoralia, a New Conical-Shaped Mollusk from the Middle Cambrian of Western Argentina
Geologica Acta, Vol.9, Nº 2, June 2011, 175-185 DOI: 10.1344/105.000001692 Available online at www.geologica-acta.com Totoralia, a new conical-shaped mollusk from the Middle Cambrian of western Argentina M.F. TORTELLO and N.M. SABATTINI CONICET-División Paleozoología Invertebrados, Museo de La Plata Paseo del Bosque s/nª, 1900 La Plata, Argentina. Tortello E-mail: [email protected] Sabatini E-mail: [email protected] ABS TRACT The new genus Totoralia from the Late Middle Cambrian of El Totoral (Mendoza Province, western Argentina) is described herein. It is a delicate, high, bilaterally symmetrical cone with a sub-central apex and five to seven prominent comarginal corrugations. In addition, its surface shows numerous fine comarginal lines, as well as thin, closely spaced radial lirae. Totoralia gen. nov., in most respects, resembles the Cambrian helcionellids Scenella BILLINGS and Palaeacmaea HALL and WHITFIELD. Although Scenella has been considered as a chondrophorine cnidarian by some authors in the past, now the predominant view is that it is a mollusk. Likewise, several aspects of Totoralia gen. nov. morphology indicate closer affinities with mollusks. The specimens studied constitute elevated cones that are rather consistent in height, implying that they were not flexible structures like those of the chondrophorines. The presence of a short concave slope immediately in front of the apex can also be interpreted as a mollusk feature. In addition, the numerous comarginal lines of the cone are uniform in prominence and constant in spacing, and are only represented on the dorsal surface of the shell; thus, they are most similar to the incremental growth lines of shells of mollusks. -
Shell Microstructures in Early Mollusks
Vol. XLII(4): 2010 THE FESTIVUS Page 43 SHELL MICROSTRUCTURES IN EARLY MOLLUSKS MICHAEL J. VENDRASCO1*, SUSANNAH M. PORTER1, ARTEM V. KOUCHINSKY2, GUOXIANG LI3, and CHRISTINE Z. FERNANDEZ4 1Institute for Crustal Studies, University of California, Santa Barbara, CA, 93106, USA 2Department of Palaeozoology, Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden 3LPS, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, P.R. China, 414601 Madris Ave., Norwalk, CA 90650, USA Abstract: Shell microstructures in some of the oldest known mollusk fossils (from the early to middle Cambrian Period; 542 to 510 million years ago) are diverse, strong, and in some cases unusual. We herein review our recent work focused on different aspects of shell microstructures in Cambrian mollusks, briefly summarizing some of the major conclusions from a few of our recent publications and adding some new analysis. Overall, the data suggest that: (1) mollusks rapidly evolved disparate shell microstructures; (2) early mollusks had a complex shell with a different type of shell microstructure in the outer layer than in the inner one; (3) the modern molluscan biomineralization system, with precise control over crystal shapes and arrangements in a mantle cavity bounded by periostracum, was already in place during the Cambrian; (4) shell microstructure data provide a suite of characters useful in phylogenetic analyses of mollusks and mollusk-like Problematica, allowing better determination -
Terreneuvian Stratigraphy and Faunas from the Anabar Uplift, Siberia
Terreneuvian stratigraphy and faunas from the Anabar Uplift, Siberia ARTEM KOUCHINSKY, STEFAN BENGTSON, ED LANDING, MICHAEL STEINER, MICHAEL VENDRASCO, and KAREN ZIEGLER Kouchinsky, A., Bengtson, S., Landing, E., Steiner, M., Vendrasco, M., and Ziegler, K. 2017. Terreneuvian stratigraphy and faunas from the Anabar Uplift, Siberia. Acta Palaeontologica Polonica 62 (2): 311‒440. Assemblages of mineralized skeletal fossils are described from limestone rocks of the lower Cambrian Nemakit-Daldyn, Medvezhya, Kugda-Yuryakh, Manykay, and lower Emyaksin formations exposed on the western and eastern flanks of the Anabar Uplift of the northern Siberian Platform. The skeletal fossil assemblages consist mainly of anabaritids, molluscs, and hyoliths, and also contain other taxa such as Blastulospongia, Chancelloria, Fomitchella, Hyolithellus, Platysolenites, Protohertzina, and Tianzhushanella. The first tianzhushanellids from Siberia, including Tianzhushanella tolli sp. nov., are described. The morphological variation of Protohertzina anabarica and Anabarites trisulcatus from their type locality is documented. Prominent longitudinal keels in the anabaritid Selindeochrea tripartita are demon- strated. Among the earliest molluscs from the Nemakit-Daldyn Formation, Purella and Yunnanopleura are interpreted as shelly parts of the same species. Fibrous microstructure of the outer layer and a wrinkled inner layer of mineralised cuticle in the organophosphatic sclerites of Fomitchella are reported. A siliceous composition of the globular fossil Blastulospongia -
Anomalocaris
Life of the Paleozoic Tuesday, November 22, 11 Life of the Paleozoic • Overview: • Cambrian, Vast expansion of shelly marine life forms and jawless fish • Ordovician - most modern phyla established • Late Paleozoic- land plants and vertebrates (tetrapods and amniotes) Tuesday, November 22, 11 Invertebrates • Marine environments • Nektic, planktic, benthic • Adaptions: • Epifaunal- animals living on the sea floor • Infaunal – animals that burrow into the sea floor Tuesday, November 22, 11 Early cambrian • Small Shelly fossils • Rarely more than a few millimeters long • A- Anabarella • B- Camanella • C- Aldanella • D- Sponge Spicule • E- Formitchella • F- Lapworthella Tuesday, November 22, 11 Early Soft-body fossils • The Burgess shale: • Most fossils reduced to shiny black impressions What type of fossilization is this? • Viewed as one of the most important finds of the fossil record • Altogether, over 60,000 species have been collected Tuesday, November 22, 11 The Burgess shale • Four Groups of Arthropods • Trilobites • Crustaceans • Scorpions • Insects • Sponges • Onycophorans • Crinoids • Sea Cucumbers • Chordates Tuesday, November 22, 11 Chordates • Shows evolution of early notochord • Notochord- dorsally situated nerve cord Why is this important? • Pikaia- small animal that has notochord and also shows evidence of v-shaped muscle bands (this indicated sinosoidal swimming motion THESE ANIMALS ARE ANCESTORS TO ALL MODERN VERTEBRATES Tuesday, November 22, 11 Other Notable Fossils • Anomalocaris- fierce predator over 50cm long (~2ft) • Opabinia- -
Constraining the Ediacaran-Cambrian Boundary in South China Using Acanthomorphic Acritarchs and Plaeopascichnus Fossils Kenneth Hugh O’Donnell
Constraining the Ediacaran-Cambrian boundary in South China using acanthomorphic acritarchs and Plaeopascichnus fossils Kenneth Hugh O’Donnell Thesis submitted to the faculty of Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of Master of Science In Geosciences S. Xiao, Committee Chair Kenneth A. Eriksson Patricia E. Dove May 7, 2013 Blacksburg, VA Keywords: Biostratigraphy; Heliosphaeridium; Palaeopascichnus; acritarchs; acanthomorphic; Yanjiahe; Liuchapo; Niutitang; Ediacaran; Cambrian; South China Copyright 2013 Constraining the Ediacaran-Cambrian boundary in South China using acanthomorphic acritarchs and Palaeopascichnus fossils Kenneth O’Donnell ABSTRACT The Ediacaran-Cambrian boundary is arguably the most critical transition in Earth history. This boundary is currently defined by the GSSP (Global Stratotype Section and Point) at Fortune Head (Newfoundland, Canada) at a point that was once regarded as the first appearance of the branching trace fossil Treptichnus pedum. However, T. pedum has been subsequently found below the GSSP, and its distribution is largely restricted to sandstone facies where chemostratigraphic correlation tools are difficult to apply. Thus, the stratigraphic value of the Fortune Head GSSP has come under scrutiny, and there is a need to search for an alternative definition of this boundary using other biostratigraphic criteria. Investigations of acanthomorphic acritarchs in basal Cambrian strata of South China suggest that these microfossils may -
Redalyc.Totoralia, a New Conical-Shaped Mollusk from The
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España TORTELLO, M.F.; SABATTINI, N.M. Totoralia, a new conical-shaped mollusk from the middle Cambrian of western Argentina Geologica Acta: an international earth science journal, vol. 9, núm. 2, junio, 2011, pp. 175-185 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50521609004 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.9, Nº 2, June 2011, 175-185 DOI: 10.1344/105.000001692 Available online at www.geologica-acta.com Totoralia, a new conical-shaped mollusk from the Middle Cambrian of western Argentina M.F. TORTELLO and N.M. SABATTINI CONICET-División Paleozoología Invertebrados, Museo de La Plata Paseo del Bosque s/nª, 1900 La Plata, Argentina. Tortello E-mail: [email protected] Sabatini E-mail: [email protected] ABS TRACT The new genus Totoralia from the Late Middle Cambrian of El Totoral (Mendoza Province, western Argentina) is described herein. It is a delicate, high, bilaterally symmetrical cone with a sub-central apex and five to seven prominent comarginal corrugations. In addition, its surface shows numerous fine comarginal lines, as well as thin, closely spaced radial lirae. Totoralia gen. nov., in most respects, resembles the Cambrian helcionellids Scenella BILLINGS and Palaeacmaea HALL and WHITFIELD. -
Natural Resource Inventory Report of the Fiji Islands 2010 Volume 2
NATURAL RESOURCE INVENTORY REPORT OF THE FIJI ISLANDS 2010 VOLUME 2: MARINE RESOURCES INVENTORY OF THE FIJI ISLANDS Prepared by: Professor Biman Chand Prasad Dean Faculty of Business and Economics University of the South Pacific Suva Fiji 1 ACKNOWLEDGEMENTS The preparation of the Natural Resource Inventory (NRI) report was a challenging task and the contribution of the following people cannot be left unmentioned. The following organisations and government departments who actively contributed in making the Natural Resource Inventory a success are: ` Department of Energy Fiji Electricity Authority Fiji Locally Managed Marine Areas Fisheries Food Agriculture Organisation Hydrology department Institute of Applied Science Mareqeti Viti Meteorological Office Mineral Resource Department Ministry of Agriculture Ministry of Lands Ministry of Primary Industries Ministry of Town Planning National Trust Native Land Trust Board Non Government Organisations Secretariat for the Pacific Islands Applied Geoscience Commission Secretariat of the Pacific Community South Pacific Regional Environment Programme University of the South Pacific Wetland International Wildlife Conservation Society 2 ABBREVIATIONS AIMS Australian Institute of Marine Science DoF Department of Fisheries EEZ Economic Exclusive Zone EOI Expression of Interest GoF Government of Fiji Islands MPA Marine Protected Areas NWVL Natural Waters of Viti Ltd PIFS Pacific Islands Forum Secretariat SE South East W/NW West/North West 3 EXECUTIVE SUMMARY The preparation of the Natural Resource Inventory Report (NRI) is a requirement under the Environment Management Act (2005). Under the Environment Management Act (2005) s.13, the resource management unit is required to prepare the NRI report after consulting the important stakeholders such as the resource owners. Notably, this is the first NRI that has been prepared for Fiji.