DOCSLIB.ORG

International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution"

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013 Lindskog, Anders; Mehlqvist, Kristina 2013 Link to publication Citation for published version (APA): Lindskog, A., & Mehlqvist, K. (Eds.) (2013). International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013. (International Geological Correlation Programme, UNESCO; Vol. 3). Department of Geology, Lund University. General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 ANDERS LINDSKOG | KRISTINA MEHLQVIST Printed by Media-Tryck, Lund 2013 Proceedings of the 3rd IGCP 591 Annual Meeting Proceedings of the 3 Lund, Sweden, 9–19 June 2013 EDITED BY ANDERS LINDSKOG | KRISTINA MEHLQVIST DEPARTMENT OF GEOLOGY | LUND UNIVERSITY The abstracts within this volume were presented at the 3rd IGCP 591 Annual rd Meeting, which was held in Lund, Sweden, in June 2013. This meeting was Annual IGCP 591 Meeting co-arranged with the International Subcommission on Cambrian Stratigraphy (ISCS), the International Subcommission on Ordovician Stratigraphy (ISOS) and the International Subcommission on Silurian Stratigraphy (ISSS). The formal theme of the meeting was ‘Early Palaeozoic Global Change’. ‒ Lund, Sweden, 9–19 June 2013 Lund, Sweden, June 9–19 2013 ISBN 978-91-86746-87-2 9 789186 746872 LUND UNIVERSITY Department of Geology Sölvegatan 12 SE-223 62 Lund, Sweden ISBN: 978-91-86746-87-2 Proceedings of the 3rd IGCP 591 Annual Meeting Lund, Sweden, 9–19 June 2013 Edited by Anders Lindskog and Kristina Mehlqvist 1 Suggested reference format Lindskog, A. & Mehlqvist, K., 2013: Proceedings of the 3rd IGCP 591 Annual Meeting – Lund, Sweden, 9–19 June 2013. Lund University. 368 pp. Hinnov, L.A., 2013: Prospects for a Paleozoic Astronomical Time Scale. In A. Lind- skog & K. Mehlqvist (eds.): Proceedings of the 3rd IGCP 591 Annual Meeting – Lund, Sweden, 9–19 June 2013, 19–20. Lund University. Department of Geology Lund University Sölvegatan 12 SE-223 62 Lund Sweden http://www.geol.lu.se http://www.igcp591.org ISBN: 978-91-86746-87-2 En del av Förpacknings- och Tidningsinsamlingen (FTI) 2 Foreword and acknowledgements This abstract volume has been prepared for the 3rd annual meeting of the IUGS/UNESCO International Geoscience Programme Project 591 The Early to Middle Palaeozoic Revolution. The meeting was hosted by the Department of Geology, Lund University, in June 9–19 2013 and followed the successful annual meetings held in Madrid/Ludlow (2011) and Cincinnati (2012). The Lund conference was arranged jointly with the annual meetings of the Cambrian, Ordovician and Silurian subcommissions on stratigraphy, and included a post-conference excursion to key geological localities in Skåne, Västergötland and the Oslo Region. The conference was a focus for cutting-edge research in Lower and Middle Palaeozoic geology and palaeontology, and the presentations covered a wide range of topics from morphology and taxonomy of various fossil groups through advances in geochemistry and stratigraphy to biogeography, palaeoecology and palaeoclimatology. We would like to express our sincere gratitude to Anders Lindskog and Kristina Mehlqvist for their meticulous editing of the meeting proceedings. We are also grateful for valuable input from the organization and scientific committee associated with the meeting. We acknowledge financial support from the Swedish Research Council (grant D0013001 to MC), the Geological Survey of Sweden, the Geological Society of Sweden, the Department of Geology at Lund University, and the municipality of Lund. Lund on 8 May 2013 Mikael Calner (meeting chair) Oliver Lehnert (vice chair) Per Ahlberg 3 4 Contents Keynote: Prospects for a Paleozoic Astronomical Time Scale 19 LINDA A. HINNOV Keynote: Marine biodiversity dynamics and reef evolution in the Early Paleozoic 21 WOLFGANG KIESSLING The risk of misleading eustatic and ‘epeirogenic’ processes in the correlation of the Cambrian Series 2–3 boundary interval in rift and drift (passive margin) basins 23 J. JAVIER ÁLVARO The nature of Ordovician limestone–mudstone alternations in the Oslo-Asker area (Norway): Primary or diagenetic rhythms? 25 CHLOÉ AMBERG, TIM COLLART, WOUT SALENBIEN, THIJS R. A. VANDENBROUCKE, LISA M. EGGER3, AXEL MUNNECKE, ARNE T. NIELSEN, ØYVIND HAMMER AND JACQUES VERNIERS Wenlock on the northeastern margin of the European platform 27 ANNA I. ANTOSHKINA Placing Upper Ordovician “butter shale” Lagerstätten within a sequence stratigraphic framework 29 CHRISTOPHER D. AUCOIN, CARLTON BRETT, THOMAS MALGIERI AND JAMES THOMKA 13 The Ccarb curve from the Green Point succession in western Newfoundland, Canada and correlation of the GSSP section of the Cambrian–Ordovician boundary 31 KAREM AZMY, SVEND STOUGE, GABRIELLA BAGNOLI AND UWE BRAND The early Rhuddanian survival interval of the Ordovician/Silurian extinction in the Central Oslo Region 34 B. GUDVEIG BAARLI “Cedaria” woosteri and the Cedaria Zone (Cambrian: Guzhangian) of Laurentia 37 LOREN E. BABCOCK AND MARK T. BARANOSKI Palynology and sedimentology of the Upper Ordovician–lowermost Llandovery in the Röstånga-1 core, southern Sweden 39 AHMED S. BADAWY, PER AHLBERG, MIKAEL CALNER, KRISTINA MEHLQVIST AND VIVI VAJDA New mid-Cambrian palaeoscolecid sclerites of Hadimopanella oezgueli from the Cantabrian Mountains, northern Spain 42 TANIA BARRAGÁN, JORGE ESTEVE, DIEGO C. GARCÍA-BELLIDO, SAMUEL ZAMORA AND J. JAVIER ÁLVARO1 5 Chitinozoan biostratigraphy in the Haljala Regional Stage, Upper Ordovician: A new high-resolution approach from NE Estonia 45 GARMEN BAUERT, JAAK NÕLVAK AND HEIKKI BAUERT Depositional environments of Ordovician and Silurian sediments of the Siljan impact structure (Sweden) – insights from organic geochemistry 47 ULRICH BERNER, OLIVER LEHNERT AND GUIDO MEINHOLD Middle Ordovician cephalopods from the Abarsaj area, northern Iran 50 OLGA K. BOGOLEPOVA, BJÖRN KRÖGER, MOSTAFA FALAHATGAR AND MOJABA JAVIDAN The first Silurian chitinozoans from Severnaya Zemlya, Arctic Russia 51 OLGA K. BOGOLEPOVA, FLORENTIN PARIS AND ALEXANDER P. GUBANOV A reexamination of the contributions of biotope and geographic range to extinction risk in Ordovician graptolites 52 JAMES T. BOYLE, H. DAVID SHEETS, SHUANG-YE WU, DANIEL GOLDMAN, MICHAEL J. MELCHIN, ROGER A. COOPER, PETER M. SADLER AND CHARLES E. MITCHELL Comparative facies and carbon isotope analysis of the Sheinwoodian succession in the western Baltic and eastern North America: Evidence for a composite Ireviken Event 54 CARLTON BRETT, PATRICK MCLAUGHLIN AND POUL EMSBO A 13C composite standard for the Ordovician of Sweden based on the Tingskullen (Öland) and Borenshult (Östergötland) cores 56 MIKAEL CALNER, OLIVER LEHNERT AND MICHAEL M. JOACHIMSKI First evidence of unmineralized and non-cuticular organisms in the Cambrian ‘Orsten’ assemblages of the Alum Shale Formation of Sweden 58 CHRISTOPHER CASTELLANI, ANDREAS MAAS, JOACHIM T. HAUG, CAROLIN HAUG AND DIETER WALOSZEK Re-appraisal of the faunal diversity of the ‘Orsten’ assemblages of Sweden – new insight into the late Cambrian Alum Shale ecosystem 60 CHRISTOPHER CASTELLANI, ANDREAS MAAS, JOACHIM T. HAUG AND DIETER WALOSZEK Temporal and spatial distribution of the Wufeng black shales (Upper Ordovician) in South China 62 QING CHEN, JUNXUAN FAN, MICHAEL J. MELCHIN AND LINNA ZHANG The Lower Palaeozoic palaeogeography of Gondwana 63 L. ROBIN M. COCKS AND TROND H. TORSVIK A draboviid association from Portugal: Palaeoecological and palaeogeographical significance 65 JORGE COLMENAR, ARTUR A. SÁ AND NUNO VAZ Muscles versus environment: Morphofunctional analysis of the brachiopod genus Svobodaina 67 JORGE COLMENAR, DAVID A. T. HARPER AND ENRIQUE VILLAS Revised conodont biostratigraphy of the Silurian of Cellon, Carnic Alps 69 CARLO CORRADINI, MARIA G. CORRIGA AND PEEP MÄNNIK 6 Upper Silurian and Lower Devonian conodonts and crinoids from the scyphocrinoid beds of southeastern Morocco 71 MARIA G. CORRIGA, CARLO CORRADINI, REIMUND HAUDE AND OTTO H. WALLISER(†) Rapid geochemical change in Silurian oceans: Implications for global 13C and 87Sr/86Sr systematics 73 BRADLEY D. CRAMER, MARK D. SCHMITZ, WARREN D. HUFF, STIG M. BERGSTRÖM AND DENNIS R. KOLATA A complete record of the ‘Lower’ Cambrian–Middle Ordovician succession of Öland, southern Sweden, based on the Tingskullen core 74 PETER DAHLQVIST, MIKAEL CALNER, OLIVER LEHNERT AND PER AHLBERG Latitudinal constraints on an intra-Iapetus terrane based on biotic and abiotic data from the Upper Allochthon of Västerbotten, Sweden 77 PETER DAHLQVIST AND CHRISTIAN M. Ø. RASMUSSEN New data on
Recommended publications
  • Geology and Palaeontology of the Codos Anticline, Eastern Iberian Chains, NE Spain: Age Constraints for the Ediacaran-Cambrian B

    Geology and Palaeontology of the Codos Anticline, Eastern Iberian Chains, NE Spain: Age Constraints for the Ediacaran-Cambrian B

    Geological Magazine Geology and palaeontology of the Codos www.cambridge.org/geo anticline, eastern Iberian Chains, NE Spain: age constraints for the Ediacaran–Cambrian boundary in the Iberian Chains Original Article Cite this article: Streng M. Geology and Michael Streng palaeontology of the Codos anticline, eastern Iberian Chains, NE Spain: age constraints for Uppsala University, Department of Earth Sciences, Palaeobiology, Villavägen 16, 752 36 Uppsala, Sweden the Ediacaran–Cambrian boundary in the Iberian Chains. Geological Magazine https:// Abstract doi.org/10.1017/S0016756821000595 The two major structural elements of the Iberian Chains, the Datos and Jarque thrust faults, Received: 3 November 2020 have been described as occurring in proximity in the area around the village of Codos. The Revised: 16 May 2021 Accepted: 26 May 2021 purported Jarque fault corresponds to the axial plane of an anticline known as the Codos anti- cline, which exposes the oldest stratigraphic unit in this area, i.e. the Codos Bed, a limestone bed Keywords: bearing skeletal fossils of putative Ediacaran or earliest Cambrian age. Details of the geology of Paracuellos Group; Aluenda Formation; Codos the area and the age of the known fossils are poorly understood or not universally agreed upon. Bed; Cloudina; helcionelloids; Terreneuvian; New investigations in the anticline revealed the presence of a normal fault, introduced as the Heraultia Limestone Codos fault, which cross-cuts the course of the alleged Jarque fault. The vertical displacement Author for correspondence: along the axial plane of the anticline appears to be insignificant, challenging the traditional Michael Streng, interpretation of the plane as an equivalent of the Jarque thrust fault.
  • No. 40. the System of Lunar Craters, Quadrant Ii Alice P

    No. 40. the System of Lunar Craters, Quadrant Ii Alice P

    NO. 40. THE SYSTEM OF LUNAR CRATERS, QUADRANT II by D. W. G. ARTHUR, ALICE P. AGNIERAY, RUTH A. HORVATH ,tl l C.A. WOOD AND C. R. CHAPMAN \_9 (_ /_) March 14, 1964 ABSTRACT The designation, diameter, position, central-peak information, and state of completeness arc listed for each discernible crater in the second lunar quadrant with a diameter exceeding 3.5 km. The catalog contains more than 2,000 items and is illustrated by a map in 11 sections. his Communication is the second part of The However, since we also have suppressed many Greek System of Lunar Craters, which is a catalog in letters used by these authorities, there was need for four parts of all craters recognizable with reasonable some care in the incorporation of new letters to certainty on photographs and having diameters avoid confusion. Accordingly, the Greek letters greater than 3.5 kilometers. Thus it is a continua- added by us are always different from those that tion of Comm. LPL No. 30 of September 1963. The have been suppressed. Observers who wish may use format is the same except for some minor changes the omitted symbols of Blagg and Miiller without to improve clarity and legibility. The information in fear of ambiguity. the text of Comm. LPL No. 30 therefore applies to The photographic coverage of the second quad- this Communication also. rant is by no means uniform in quality, and certain Some of the minor changes mentioned above phases are not well represented. Thus for small cra- have been introduced because of the particular ters in certain longitudes there are no good determi- nature of the second lunar quadrant, most of which nations of the diameters, and our values are little is covered by the dark areas Mare Imbrium and better than rough estimates.
  • Glossary Glossary

    Glossary Glossary

    Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts.
  • International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution"

    International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution"

    International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013 Lindskog, Anders; Mehlqvist, Kristina 2013 Link to publication Citation for published version (APA): Lindskog, A., & Mehlqvist, K. (Eds.) (2013). International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013. (International Geological Correlation Programme, UNESCO; Vol. 3). Department of Geology, Lund University. Total number of authors: 2 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 ANDERS LINDSKOG | KRISTINA MEHLQVIST Printed by Media-Tryck, Lund 2013 Proceedings of the 3rd IGCP 591 Annual Meeting Proceedings of the 3 Lund, Sweden, 9–19 June 2013 EDITED BY ANDERS LINDSKOG | KRISTINA MEHLQVIST DEPARTMENT OF GEOLOGY | LUND UNIVERSITY The abstracts within this volume were presented at the 3rd IGCP 591 Annual rd Meeting, which was held in Lund, Sweden, in June 2013.
  • The Case of the Diminutive Trilobite Flexicalymene Retrorsa Minuens from the Cincinnatian Series (Upper Ordovician), Cincinnati Region

    The Case of the Diminutive Trilobite Flexicalymene Retrorsa Minuens from the Cincinnatian Series (Upper Ordovician), Cincinnati Region

    EVOLUTION & DEVELOPMENT 9:5, 483–498 (2007) Evaluating paedomorphic heterochrony in trilobites: the case of the diminutive trilobite Flexicalymene retrorsa minuens from the Cincinnatian Series (Upper Ordovician), Cincinnati region Brenda R. Hundaa,Ã and Nigel C. Hughesb aCincinnati Museum Center, 1301 Western Avenue, Cincinnati, OH 45203, USA bDepartment of Earth Sciences, University of California, Riverside, CA 92521, USA ÃAuthor for correspondence (email: [email protected]) SUMMARY Flexicalymene retrorsa minuens from the upper- rate of progress along a common ontogenetic trajectory with most 3 m of the Waynesville Formation of the Cincinnatian respect to size, coupled with growth cessation at a small size, Series (Upper Ordovician) of North America lived ‘‘sequential’’ progenesis, or non-uniform changes in the rate of approximately 445 Ma and exhibited marked reduction in progress along a shared ontogenetic trajectory with respect to maximum size relative to its stratigraphically subjacent sister size, can also be rejected. Rather, differences between these subspecies, Flexicalymene retrorsa retrorsa. Phylogenetic subspecies are more consistent with localized changes in analysis is consistent with the notion that F. retrorsa retrorsa rates of character development than with a global hetero- was the ancestor of F. retrorsa minuens. F. retrorsa minuens chronic modification of the ancestral ontogeny. The evolution has been claimed to differ from F. retrorsa retrorsa ‘‘in size of F. retrorsa minuens from F. retrorsa retrorsa was largely alone,’’ and thus presents a plausible example of global dominated by modifications of the development of characters paedomorphic evolution in trilobites. Despite strong similarity already evident in the ancestral ontogeny, not by the origin of in the overall form of the two subspecies, F.
  • Shell Microstructures in Early Cambrian Molluscs

    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.
  • Available Generic Names for Trilobites

    Available Generic Names for Trilobites

    AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites.
  • Copertina Guida Ai TRILOBITI V3 Esterno

    Copertina Guida Ai TRILOBITI V3 Esterno

    Enrico Bonino nato in provincia di Bergamo nel 1966, Enrico si è laureato in Geologia presso il Dipartimento di Scienze della Terra dell'Università di Genova. Attualmente risiede in Belgio dove svolge attività come specialista nel settore dei Sistemi di Informazione Geografica e analisi di immagini digitali. Curatore scientifico del Museo Back to the Past, ha pubblicato numerosi volumi di paleontologia in lingua italiana e inglese, collaborando inoltre all’elaborazione di testi e pubblicazioni scientifiche a livello nazonale e internazionale. Oltre alla passione per questa classe di artropodi, i suoi interessi sono orientati alle forme di vita vissute nel Precambriano, stromatoliti, e fossilizzazioni tipo konservat-lagerstätte. Carlo Kier nato a Milano nel 1961, Carlo si è laureato in Legge, ed è attualmente presidente della catena di alberghi Azul Hotel. Risiede a Cancun, Messico, dove si dedica ad attività legate all'ambiente marino. All'età di 16 anni, ha iniziato una lunga collaborazione con il Museo di Storia Naturale di Milano, ed è a partire dal 1970 che prese inizio la vera passione per i trilobiti, dando avvio a quella che oggi è diventata una delle collezioni paleontologiche più importanti al mondo. La sua instancabile attività di ricerca sul terreno in varie parti del globo e la collaborazione con professionisti del settore, ha permesso la descrizione di nuove specie di trilobiti ed artropodi. Una forte determinazione e la costruzione di un nuovo complesso alberghiero (AZUL Sensatori) hanno infine concretizzzato la realizzazione
  • Howard Associate Professor of Natural History and Curator Of

    Howard Associate Professor of Natural History and Curator Of

    INGI AGNARSSON PH.D. Howard Associate Professor of Natural History and Curator of Invertebrates, Department of Biology, University of Vermont, 109 Carrigan Drive, Burlington, VT 05405-0086 E-mail: [email protected]; Web: http://theridiidae.com/ and http://www.islandbiogeography.org/; Phone: (+1) 802-656-0460 CURRICULUM VITAE SUMMARY PhD: 2004. #Pubs: 138. G-Scholar-H: 42; i10: 103; citations: 6173. New species: 74. Grants: >$2,500,000. PERSONAL Born: Reykjavík, Iceland, 11 January 1971 Citizenship: Icelandic Languages: (speak/read) – Icelandic, English, Spanish; (read) – Danish; (basic) – German PREPARATION University of Akron, Akron, 2007-2008, Postdoctoral researcher. University of British Columbia, Vancouver, 2005-2007, Postdoctoral researcher. George Washington University, Washington DC, 1998-2004, Ph.D. The University of Iceland, Reykjavík, 1992-1995, B.Sc. PROFESSIONAL AFFILIATIONS University of Vermont, Burlington. 2016-present, Associate Professor. University of Vermont, Burlington, 2012-2016, Assistant Professor. University of Puerto Rico, Rio Piedras, 2008-2012, Assistant Professor. National Museum of Natural History, Smithsonian Institution, Washington DC, 2004-2007, 2010- present. Research Associate. Hubei University, Wuhan, China. Adjunct Professor. 2016-present. Icelandic Institute of Natural History, Reykjavík, 1995-1998. Researcher (Icelandic invertebrates). Institute of Biology, University of Iceland, Reykjavík, 1993-1994. Research Assistant (rocky shore ecology). GRANTS Institute of Museum and Library Services (MA-30-19-0642-19), 2019-2021, co-PI ($222,010). Museums for America Award for infrastructure and staff salaries. National Geographic Society (WW-203R-17), 2017-2020, PI ($30,000). Caribbean Caves as biodiversity drivers and natural units for conservation. National Science Foundation (IOS-1656460), 2017-2021: one of four PIs (total award $903,385 thereof $128,259 to UVM).
  • Conodonts from the Niur Formation (Silurian) of the Derenjal Mountains, Central Iran

    Conodonts from the Niur Formation (Silurian) of the Derenjal Mountains, Central Iran

    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/239735578 Conodonts from the Niur Formation (Silurian) of the Derenjal Mountains, Central Iran Article in Geological Magazine · July 2013 DOI: 10.1017/S001675681200088X CITATIONS READS 15 315 3 authors: Peep Mannik C. Giles Miller Tallinn University of Technology Natural History Museum, London 101 PUBLICATIONS 2,383 CITATIONS 81 PUBLICATIONS 586 CITATIONS SEE PROFILE SEE PROFILE Vachik Hairapetian Islamic Azad University Isfahan (Khorasgan) Branch 77 PUBLICATIONS 587 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: TERSANE: Temperature-Related Stresses as a Unifying Principle in Ancient Extinctions View project Studies on Silurian conodonts from eastern Qinling and the related strata View project All content following this page was uploaded by C. Giles Miller on 27 May 2014. The user has requested enhancement of the downloaded file. Geol. Mag. 150 (4), 2013, pp. 639–650. c Cambridge University Press 2013 639 doi:10.1017/S001675681200088X Conodonts from the Niur Formation (Silurian) of the Derenjal Mountains, Central Iran ∗ P. MÄNNIK †, C. G. MILLER‡ & V. HAIRAPETIAN§ ∗ Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia ‡Department of Palaeontology, Natural History Museum, London SW7 5BD, UK §Department of Geology, Khorasgan (Esfahan) Branch, Islamic Azad University, PO Box 81595−158, Esfahan, Iran (Received 5 October 2011; accepted 25 September 2012; first published online 24 January 2013) Abstract – A Llandovery to Ludlow age for the Niur Formation in the Derenjal Mountains (east-central Iran) is proposed based on new conodont data and previous work on other fossils.
  • 2Nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS

    2Nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS

    2nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS. Characters and Parsimony. Jonathan M. Adrain, Department of Palaeontology, The Natural History Museum, London SW7 5BD, United King- dom; Gregory D. Edgecombe, Centre for Evolutionary Research, Australian Museum, 6 College Street, Sydney South, New South Wales 2000, Australia Character analysis is the single most important element of any phylogenetic study. Characters are simply criteria for comparing homologous organismic parts between taxa. Homology of organismic parts in any phylogenetic study is an a priori assumption, founded upon topological similarity through some or all stages of ontogeny. Once homolo- gies have been suggested, characters are invented by specifying bases of comparison of organismic parts from taxon to taxon within the study group. Ideally, all variation in a single homology occurring within the study group should be accounted for. Comparisons are between attributes of homologous parts, (e.g., simple presence, size of some- thing, number of something), and these attributes are referred to as character states. Study taxa are assigned member- ship in one (or more, in the case of polymorphisms) character-state for each character in the analysis. A single char- acter now implies discrete groupings of taxa, but this in itself does not constitute a phylogeny. In order to suggest or convey phylogenetic information, the historical status of each character-state, and of the the group of taxa it sug- gests, must be evaluated. That is, in the case of any two states belonging to the same character, we need to discover whether one state is primitive (broadly speaking, ancestral) or derived (representative of an evolutionary innovation) relative to the other.
  • Durham Research Online

    Durham Research Online

    Durham Research Online Deposited in DRO: 23 May 2017 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Betts, Marissa J. and Paterson, John R. and Jago, James B. and Jacquet, Sarah M. and Skovsted, Christian B. and Topper, Timothy P. and Brock, Glenn A. (2017) 'Global correlation of the early Cambrian of South Australia : shelly fauna of the Dailyatia odyssei Zone.', Gondwana research., 46 . pp. 240-279. Further information on publisher's website: https://doi.org/10.1016/j.gr.2017.02.007 Publisher's copyright statement: c 2017 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Accepted Manuscript Global correlation of the early Cambrian of South Australia: Shelly fauna of the Dailyatia odyssei Zone Marissa J.