DOCSLIB.ORG

Newsletter Number 57

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

The Palaeontology Newsletter Contents 57 Association Business 2 Association Meetings 6 From our correspondents Tainting of Proc. Biol. Soc. Wash. 10 Time and time-rock again 18 Stratigraphy over-simplified? 27 Palaeo-math 101: Regression 3 32 Meeting Reports 44 Future meetings of other bodies 56 Mysterious Fossils 67 Book Reviews 68 Post-graduate opportunities 85 Discounts for PalAss members 89 Special Papers 70–72 90–95 Palaeontology vol 47 part 6 96 48th Annual Meeting Programme 98 Abstracts of Seminars 106 Abstracts of Talks 110 Abstracts of Posters 137 Reminder: The deadline for copy for Issue no 58 is 11th February 2005 On the Web: <http://www.palass.org/> Newsletter 57 2 Newsletter 57 3 Association Business 3. Election of Council and vote of thanks to retiring members i. Dr Smith extended a vote of thanks to the retiring members of Council Dr J. Clack, Dr A.L.A. Johnson, Dr I.J. Sansom, Dr S. Gabbott, Dr P. Orr and Dr Milsom. Dr Purnell 48TH ANNUAL GENERAL MEETING AND extended a vote of thanks to Dr Smith. ANNUAL ADDRESS ii. It was noted the following members of Council would be moving to new posts: Dr M.A. Purnell (Vice president), Prof. E.N.K. Clarkson (Ed.) and Dr Polly (Ed.). Dr Hilton will take over responsibility as Web Officer. 48th Annual General Meeting and Annual Address iii. New members of Council include Dr. L. Anderson (Ed., co-opted), Dr Per Ahlberg (Ed.). Saturday, 18th December 4.45 to 5.10 pm 4. Sylvester-Bradley Awards MACC Congress Centre, USTL campus at Villeneuve d’Ascq. i. Dr Smith announced eight grants had been awarded to Broughton, Gladwell, Harrington, AGENDA Hernandez-Castillo, Lane, Joomun, Tetlie and Zuykov 1. Apologies for absence 5. Proposed change to Constitution article 3 2. Annual Report for 2003 i. It was agreed to include the category of Honorary Life Membership, proposed by Prof. E.N.K. Clarkson, seconded by Dr Cusack. 3. Accounts and Balance Sheet for 2003 Howard A. Armstrong 4. Changes to subscription rates Secretary 5. Presentation of the Lapworth Medal 6. Presentation of the Hodson Fund 7. Presentation of the Mary Anning Awards Sylvester-Bradley Award 8. Election of Council and vote of thanks to retiring members 9. Annual address Awards are made to assist palaeontological research (travel, visits to museums, fieldwork etc.), with each award having a maximum value of £1,000. Preference is given to applications for H. A. Armstrong a single purpose (rather than top-ups of other grant applications) and no definite age limit is Secretary applied, although some preference may be given to younger applicants or those at the start of their careers. The award is open to both amateur and professional palaeontologists, but preference will be given to members of the Association. The awards are announced at the AGM. AGM MINUTES 2003 Council will also consider awards in excess of £1,000, particularly for pilot projects which are Minutes of the Annual General Meeting held on Wednesday, 7th May 2003 at the Natural History likely to facilitate a future application to a national research funding body. Museum, London. Electronic submission of applications, through the website, is preferred and will comprise a CV, Apologies for absence: Prof. D.E.G. Briggs, Prof. S.K. Donovan, Dr S. Evans, Dr S. Gabbott, an account of research aims and objectives (5,000 characters maximum), and a breakdown of Prof. J. Hancock, Prof. D.A.T. Harper, Dr E. Harper, Dr J. Hilton, Dr A.L.A. Johnson, Dr I.J. Sansom. the proposed expenditure. Each application should be accompanied by the names of a personal and scientific referee. Successful candidates must produce a report for Palaeontology Newsletter 1. Annual Report for 2002. Agreed, proposed by Dr Donoghue and seconded by Dr Purnell. and are asked to consider the Association’s meetings and publications as media for conveying 2. Accounts and Balance Sheet for 2002. Agreed, proposed by Dr Polly and seconded by the research results. Deadline: Friday 26th November 2004. Dr Manning. Newsletter 57 4 Newsletter 57 5 Prestigious new website award from PalAss “The Golden Trilobite Awards” Over the past few years there has been an exponential increase in the number of quality websites promoting palaeontology and its allied sciences. These are widely used by professionals and amateurs alike and are a valuable resource Palaeontology: for our science. Council has decided to recognise the work that goes into developing these sites by CALL FOR SHORT PAPERS! awarding an annual Website Award. Awards will be announced at the AGM and published on our website and in the Newsletter. There will be two awards, decided by Council members for the best institutional and amateur sites. From January 2005 Palaeontology will be published in A4 size with a new layout. In line with this development space will be reserved To get the ball rolling for this year, two websites have been recognised as reaching the highest for rapid publication of short papers on topical issues, exceptional standards: new discoveries, and major developments that have important Institutional Award: The echinoid directory implications for evolution, palaeoclimate, depositional environments and other matters of general interest to palaeontologists. Papers, <http://www.nhm.ac.uk/palaeontology/echinoids/> which should not exceed 6 printed pages, should be submitted in the The echinoid directory is ostensibly a taxonomic resource for the scientific community normal way, but they will be refereed rapidly and fast tracked, on in which the genera and higher taxa of echinoids can be simply and rapidly identified. acceptance, for publication in the next available issue. There are currently over 350 pages of detailed information about echinoid taxa, including colour images of the highest quality. The site also provides an introduction to the Submission of longer review papers is also encouraged, and these anatomy, biology, ecology, ontogeny and phylogeny of echinoids, as well as a key to aid too will be given priority for rapid publication. While Palaeontology identification. The site has been designed and created by Andrew Smith of the Department maintains its reputation for scientific quality and presentation, these of Palaeontology, Natural History Museum, London. developments will ensure that the Impact Factor of the journal reflects its status as a leading publication in the field (rising to 1.19 Amateur Award: Fossils of the Gault Clay and Folkestone Beds of Kent, UK in 2003). <http://www.gaultammonite.co.uk/home.html> This site is dedicated to the fossils of the Lower Cretaceous Albian (Gault Clay and Folkestone Beds) in the county of Kent, south-east England, providing a pictorial identification to the fauna. The colour photographic images are of the highest quality. The site is based on the work and collections (much of which has subsequently been donated to the Natural History Museum, London) of the late Jim Craig, and is maintained by Fred Clouter. Please send your nominations for the 2005 Awards to <[email protected]>. NewsletterNewsletter 55 57 6 6 NewsletterNewsletter 55 577 7 ASSOCIATION MEETINGS Venue and Travel Details about the City of Lille can be found on the website at <http://www.mairie-lille.fr/>. Lille is less than two hours from London by Eurostar (<http://www.eurostar.com/>), and tickets 48th Annual Meeting of The Palaeontological Association at reduced prices are available if you book some weeks in advance. Lille can also be reached Lille, France 17 – 20 December 2004 easily from Paris and its airport Charles de Gaulle (about one hour) and from Brussels (about 40 minutes) by TGV high speed trains. The Congress Centre can easily be reached by Metro. The 48th Annual Meeting of the Palaeontological Association will be held in the Congress Centre Accommodation (MACC) of the Université des Sciences et Technologies de Lille (USTL), on its campus at Villeneuve Accommodation will mostly be organised in hotels around the Congress Centre at Villeneuve d’Ascq near Lille. The opening session with a seminar on Palaeobiogeography will be held on d’Ascq. This is approximately 15 minutes’ walk from the conference venue. Participants are Friday afternoon, 17th December, in the lecture hall of the Beaux Arts Museum in the centre of free to book alternative accommodation at a wide range of prices. Please note that the strict Lille. In the evening the Icebreaker Party will be held in the Natural History Museum of Lille, in deadline for reservation of accommodation through the organisers is 10th September. After this the heart of the Capitale Européenne de la Culture 2004 (<http://www.lille2004.fr/>). date, accommodation must be arranged by the participants themselves. The technical sessions will consist of two full days of talks in the main lecture hall of the Registration and booking Congress Centre at Villeneuve d’Ascq on Saturday 18th and Sunday 19th December, with poster sessions in an adjoining lecture hall. Technical sessions are open to all aspects of palaeontology. Booking for accommodation, field excursions and also abstract submission for the conference All talks will be scheduled for 15 minutes including five minutes for discussion; there are must be completed by Midnight on Friday 10th September 2004. After this date participants no parallel sessions so it is possible that some proposed oral contributions will have to be will have to organise their own accommodation in Lille in order to attend the meeting. After rescheduled as posters. On Monday 20th December two geological excursions will be organised; 10th September registration for the meeting is still possile but will incur additional costs. Final one to examine the Mesozoic sediments on the coastal sections in the Boullonnais area, the registration for the meeting will be Friday 3rd December.
Recommended publications
  • EAA Meeting 2016 Vilnius

    EAA Meeting 2016 Vilnius

    www.eaavilnius2016.lt PROGRAMME www.eaavilnius2016.lt PROGRAMME Organisers CONTENTS President Words .................................................................................... 5 Welcome Message ................................................................................ 9 Symbol of the Annual Meeting .............................................................. 13 Commitees of EAA Vilnius 2016 ............................................................ 14 Sponsors and Partners European Association of Archaeologists................................................ 15 GENERAL PROGRAMME Opening Ceremony and Welcome Reception ................................. 27 General Programme for the EAA Vilnius 2016 Meeting.................... 30 Annual Membership Business Meeting Agenda ............................. 33 Opening Ceremony of the Archaelogical Exhibition ....................... 35 Special Offers ............................................................................... 36 Excursions Programme ................................................................. 43 Visiting Vilnius ............................................................................... 57 Venue Maps .................................................................................. 64 Exhibition ...................................................................................... 80 Exhibitors ...................................................................................... 82 Poster Presentations and Programme ...........................................
  • The Paleoecology and Biogeography of Ordovician Edrioasteroids

    The Paleoecology and Biogeography of Ordovician Edrioasteroids

    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 8-2011 The Paleoecology and Biogeography of Ordovician Edrioasteroids Rene Anne Lewis University of Tennessee - Knoxville, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Paleontology Commons Recommended Citation Lewis, Rene Anne, "The Paleoecology and Biogeography of Ordovician Edrioasteroids. " PhD diss., University of Tennessee, 2011. https://trace.tennessee.edu/utk_graddiss/1094 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Rene Anne Lewis entitled "The Paleoecology and Biogeography of Ordovician Edrioasteroids." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Doctor of Philosophy, with a major in Geology. Michael L. McKinney, Major Professor We have read this dissertation and recommend its acceptance: Colin D. Sumrall, Linda C. Kah, Arthur C. Echternacht Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) THE PALEOECOLOGY AND BIOGEOGRAPHY OF ORDOVICIAN EDRIOASTEROIDS A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville René Anne Lewis August 2011 Copyright © 2011 by René Anne Lewis All rights reserved.
  • Exoskeletal Structures and Ultrastructures in Lower Devonian Dalmanitid Trilobites of the Prague Basin (Czech Republic)

    Exoskeletal Structures and Ultrastructures in Lower Devonian Dalmanitid Trilobites of the Prague Basin (Czech Republic)

    Exoskeletal structures and ultrastructures in Lower Devonian dalmanitid trilobites of the Prague Basin (Czech Republic) PETR BUDIL & FRANTIEK HÖRBINGER Our current studies of the exoskeletal structures and ultrastructures in Lower Devonian dalmanitid trilobites of the Prague Basin are briefly described and discussed. The interior of the exoskeleton in most specimens from the Prague Ba- sin is recrystallised and largely filled with very fine homogeneous sparitic cement. The ultrastructures sensu stricto, e.g., the lamination, layers forming the exoskeleton, and the fine pores or “Osmólska” cavities, are mostly imperceptible even at higher magnifications. However, ultrastructural relics were observed in some polished thin sections and exoskeletal fragments using electron microscopy. Larger structures, especially the eyes, the megapores penetrating the exoskeleton, and the surface sculptures (prosopon sensu Gill 1949), are relatively well preserved and show very fine details. The bio- logical significance of megapores is briefly discussed. Modification of the inner parts of the exoskeletons by diagenetic processes, obscuring most of the fine internal structures, is evident. • Key words: Trilobita, Dalmanitidae, exoskeleton microstructure. BUDIL,P.&HÖRBINGER, F. 2007. Exoskeletal structures and ultrastructures in Lower Devonian dalmanitid trilobites of the Prague Basin (Czech Republic). Bulletin of Geosciences 82(1), 27–36 (4 figures, 1 table). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript received January 17, 2007; accepted
  • THE POWER of OUR IDEAS GEOLOGICAL SURVEY of CANADA L\1EMOIR 430

    THE POWER of OUR IDEAS GEOLOGICAL SURVEY of CANADA L\1EMOIR 430

    THE POWER OF OUR IDEAS GEOLOGICAL SURVEY OF CANADA l\1EMOIR 430 SUBSURFACE GEOLOGY OF PRE-MESOZOIC STRATA, GREAT BEAR RIVER MAP AREA, DISTRICT OF MACKENZIE D.C. Pugh 1993 'f' Minister of Supply and Services Canada 1993 Avai lable in Canada through authorized bookstore agcnts and other bookstores or by mail from Canada Communication Group - Publishing Ottawa. Canada KI A OS9 and from Geological Survey of Canada otTiccs: 60 I Booth Street Ottawa. Canada KI A OE8 3303-33rd Street N.W .. Calgary. Alberta T2L :lA7 A deposit copy of this publication is also <wailahk for n:J'crcnce in public libraries across Canada Cat. No. M46-430E ISBN 0-660-14271\-3 Price suhject to change without notice Critical readers J.D. Ailken D./I", Morro\!' D.G. Cook 8.S XOIford N.J. :\lcillillan Scientific editor l\',C OllerenshalV Editor Jo MacGillivray Typesetting and layout Institute o/SedimelJ/Gly and Petroleum Geology Cartography unit Instilute o/Sedimentary and Petroleum Geology Author's address ]()7. 92./ - 7th Ave. SW Calgary. Alberta T2P IA./ Original manuscript received: 85-(}6- 1./ Final version approved/or publication: 87-()8-U PREFACE Over the last forty years much has been published on the sedimentary geology of Great Bear River area. The discoveries of oil in the Devonian reef at Norman Wells and in Cambrian sands at Tedji Lake have attested to the area's hydrocarbon potential. Surface mapping and local studies have revealed rock sequences and crustal structures of great potential value to our understanding of global geology. The aim of this report is to assist evaluation of the economic potential and to improve the interpretation of the geological history.
  • Conodonts in Ordovician Biostratigraphy

    Conodonts in Ordovician Biostratigraphy

    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Archivio istituzionale della ricerca - Università di Modena e Reggio Emilia 1 Conodonts in Ordovician biostratigraphy STIG M. BERGSTRÖM AND ANNALISA FERRETTI Conodonts in Ordovician biostratigraphy The long time interval after Pander’s (1856) original conodont study can in terms of Ordovician conodont biostratigraphic research be subdivided into three periods, namely the Pioneer Period (1856-1955), the Transition Period (1955-1971), and the Modern Period (1971-Recent). During the pre-1920s, the few published conodont investigations were restricted to Europe and North America and were not concerned about the potential use of conodonts as guide fossils. Although primarily of taxonomic nature, the pioneer studies by Branson & Mehl, Stauffer, and Furnish during the 1930s represent the beginning of the use of conodonts in Ordovician biostratigraphy. However, no formal zones were introduced until Lindström (1955) proposed four conodont zones in the Lower Ordovician of Sweden, which marks the end of the Pioneer Period. Because Lindström’s zone classification was not followed by similar work outside Baltoscandia, the time interval up to the late 1960s can be regarded as a Transition Period. A milestone symposium volume, entitled ‘Conodont Biostratigraphy’ and published in 1971, 2 summarized much new information on Ordovician conodont biostratigraphy and is taken as the beginning of the Modern Period of Ordovician conodont biostratigraphy. In this volume, the Baltoscandic Ordovician was subdivided into named conodont zones whereas the North American Ordovician succession was classified into a series of lettered or numbered Faunas. Although most of the latter did not receive zone names until 1984, this classification has been used widely in North America.
  • Chapter 2 Paleozoic Stratigraphy of the Grand Canyon

    Chapter 2 Paleozoic Stratigraphy of the Grand Canyon

    CHAPTER 2 PALEOZOIC STRATIGRAPHY OF THE GRAND CANYON PAIGE KERCHER INTRODUCTION The Paleozoic Era of the Phanerozoic Eon is defined as the time between 542 and 251 million years before the present (ICS 2010). The Paleozoic Era began with the evolution of most major animal phyla present today, sparked by the novel adaptation of skeletal hard parts. Organisms continued to diversify throughout the Paleozoic into increasingly adaptive and complex life forms, including the first vertebrates, terrestrial plants and animals, forests and seed plants, reptiles, and flying insects. Vast coal swamps covered much of mid- to low-latitude continental environments in the late Paleozoic as the supercontinent Pangaea began to amalgamate. The hardiest taxa survived the multiple global glaciations and mass extinctions that have come to define major time boundaries of this era. Paleozoic North America existed primarily at mid to low latitudes and experienced multiple major orogenies and continental collisions. For much of the Paleozoic, North America’s southwestern margin ran through Nevada and Arizona – California did not yet exist (Appendix B). The flat-lying Paleozoic rocks of the Grand Canyon, though incomplete, form a record of a continental margin repeatedly inundated and vacated by shallow seas (Appendix A). IMPORTANT STRATIGRAPHIC PRINCIPLES AND CONCEPTS • Principle of Original Horizontality – In most cases, depositional processes produce flat-lying sedimentary layers. Notable exceptions include blanketing ash sheets, and cross-stratification developed on sloped surfaces. • Principle of Superposition – In an undisturbed sequence, older strata lie below younger strata; a package of sedimentary layers youngs upward. • Principle of Lateral Continuity – A layer of sediment extends laterally in all directions until it naturally pinches out or abuts the walls of its confining basin.
  • Naracoorte Caves National Park

    Naracoorte Caves National Park

    Department for Environment and Heritage Naracoorte Caves National Park Australian Fossil Mammal Site World Heritage Area www.environment.sa.gov.au Naracoorte Caves Vegetation Wonambi Fossil Centre National Par The vegetation is predominantly Brown Stringybark Step through the doors of the Wonambi Fossil Australian Fossil Mammal Site on the limestone ridge, with River Red Gum lining the Centre into an ancient world where megafauna World Heritage Area banks of the Mosquito Creek. The understorey on the once roamed. The display in the Wonambi Fossil ridge is bracken fern over a diverse array of orchids Centre ‘brings to life’ the megafauna fossils found in the Naracoorte Caves. The self-guided walk Naracoorte Caves National Park covers that flower during spring. through the simulated forest and swampland is approximately 600 hectares of limestone wheelchair accessible and suitable for all ages. ranges and is situated in the Some of the park was cleared for pine forests in the south-east of South Australia, mid 1800s, with other exotic species planted around The Flinders University Gallery has information 10 km south of Naracoorte. the caves. Many of the pines have now been cleared and areas revegetated with endemic species. The panels depicting the various sciences studied at Naracoorte, and touch screen computers to answer The area was first gardens now consist of native plants although a few questions you may have relating to the Wonambi dedicated a forestry of the historic trees remain. Fossil Centre and the fossils of Naracoorte Caves. reserve in 1882, with Fauna the first caretaker Southern employed to look Bentwing Bat The National Parks Code after the caves in The most common marsupial seen at Naracoorte is the Western Grey Kangaroo.
  • Identifying Heterogeneity in Rates of Morphological Evolution: Discrete Character Change in the Evolution of Lungfish (Sarcopterygii; Dipnoi)

    Identifying Heterogeneity in Rates of Morphological Evolution: Discrete Character Change in the Evolution of Lungfish (Sarcopterygii; Dipnoi)

    ORIGINAL ARTICLE doi:10.1111/j.1558-5646.2011.01460.x IDENTIFYING HETEROGENEITY IN RATES OF MORPHOLOGICAL EVOLUTION: DISCRETE CHARACTER CHANGE IN THE EVOLUTION OF LUNGFISH (SARCOPTERYGII; DIPNOI) Graeme T. Lloyd,1,2 Steve C. Wang,3 and Stephen L. Brusatte4,5 1Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom 2E-mail: [email protected] 3Department of Mathematics and Statistics, Swarthmore College, Swarthmore, Pennsylvania 19081 4Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024 5Department of Earth and Environmental Sciences, Columbia University, New York, New York 10025 Received February 9, 2010 Accepted August 15, 2011 Data Archived: Dryad: doi:10.5061/dryad.pg46f Quantifying rates of morphological evolution is important in many macroevolutionary studies, and critical when assessing possible adaptive radiations and episodes of punctuated equilibrium in the fossil record. However, studies of morphological rates of change have lagged behind those on taxonomic diversification, and most authors have focused on continuous characters and quantifying patterns of morphological rates over time. Here, we provide a phylogenetic approach, using discrete characters and three statistical tests to determine points on a cladogram (branches or entire clades) that are characterized by significantly high or low rates of change. These methods include a randomization approach that identifies branches with significantly high rates and likelihood ratio tests that pinpoint either branches or clades that have significantly higher or lower rates than the pooled rate of the remainder of the tree. As a test case for these methods, we analyze a discrete character dataset of lungfish, which have long been regarded as “living fossils” due to an apparent slowdown in rates since the Devonian.
  • 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.
  • CONODONTS of the MOJCZA LIMESTONE -.: Palaeontologia Polonica

    CONODONTS of the MOJCZA LIMESTONE -.: Palaeontologia Polonica

    CONODONTS OF THE MOJCZA LIMESTONE JERZY DZIK Dzik, J. 1994. Conodonts of the M6jcza Limestone. -In: J. Dzik, E. Olemp ska, and A. Pisera 1994. Ordovician carbonate platform ecosystem of the Holy Cross Moun­ tains. Palaeontologia Polonica 53, 43-128. The Ordovician organodetrital limestones and marls studied in outcrops at M6jcza and Miedzygorz, Holy Cross Mts, Poland, contains a record of the evolution of local conodont faunas from the latest Arenig (Early Kundan, Lenodus variabilis Zone) to the Ashgill (Amorphognathus ordovicicus Zone), with a single larger hiatus corre­ sponding to the subzones from Eop/acognathus pseudop/anu s to E. reclinatu s. The conodont fauna is Baltic in general appearance but cold water genera , like Sagitto­ dontina, Scabbardella, and Hamarodus, as well as those of Welsh or Chinese af­ finities, like Comp/exodus, Phragmodus, and Rhodesognathu s are dominant in par­ ticular parts of the section while others common in the Baltic region, like Periodon , Eop/acognathus, and Sca/pellodus are extremely rare. Most of the lineages continue to occur throughout most of the section enabling quantitative studies on their phyletic evolut ion. Apparatuses of sixty seven species of thirty six genera are described and illustrated. Phyletic evolution of Ba/toniodus, Amorphognathu s, Comp/exodus, and Pygodus is biometrically documented. Element s of apparatu ses are homolog ized and the standard notation system is applied to all of them. Acodontidae fam. n., Drepa­ nodus kie/censis sp. n., and D. santacrucensis sp. n. are proposed . Ke y w o r d s: conodonts, Ordovici an, evolut ion, taxonomy. Jerzy Dzik, Instytut Paleobiologii PAN, A/eja Zwirk i i Wigury 93, 02-089 Warszawa , Poland.
  • Download Curriculum Vitae

    Download Curriculum Vitae

    NEIL H. LANDMAN CURATOR, CURATOR-IN-CHARGE AND PROFESSOR DIVISION OF PALEONTOLOGY HIGHEST DEGREE EARNED Ph.D. AREA OF SPECIALIZATION Evolution, life history, and systematics of externally shelled cephalopods EDUCATIONAL EXPERIENCE Ph.D. in Geology, Yale University, 1982 M. Phil. in Geology, Yale University, 1977 M.S. in Earth Sciences, Adelphi University, 1975 B.S. in Mathematics, summa cum laude, Polytechnic University of New York, 1972 PREVIOUS EXPERIENCE IN DOCTORAL EDUCATION FACULTY APPOINTMENTS Adjunct Professor, Department of Biology, City College Adjunct Professor, Department of Geology, Brooklyn College GRADUATE ADVISEES Susan Klofak, Biology, CUNY, 1999-present Krystal Kallenberg, Marine Sciences, Stony Brook, 2003-present GRADUATE COMMITTEES Christian Soucier, Biology, Brooklyn College, 2004-present Krystal Kallenberg, Marine Sciences, Stony Brook, 2003-present Yumiko Iwasaki, Geology, CUNY, 2000-2009 Emily Allen, Geology, University of Chicago, 2002-2005 Susan Klofak, Biology, CUNY, 1996-present Claude Monnet, University of Zurich, presently Sophie Low, Geology, Harvard University RESEARCH GRANT SUPPORT Kosciuszko Foundation. Comparative study of ammonite faunas from the United States Western Interior and Polish Lowland. Post-doc: Izabela Ploch, Geological Museum of Polish Geological Institute. 2011. NSF Grant MR1-R2 (Co-PI): Acquisition of a High Resolution CT-Scanner at the American Museum of Natural History: 2010-2013. NSF Grant No. DBI 0619559 (Co-PI): Acquisition of a Variable Pressure SEM at the AMNH: 2006-2009 NSF Grant No. EAR 0308926 (PI): Collaborative Research: Paleobiology, paleoceanography, and paleoclimatology of a time slice through the Western Interior Seaway: 2003-2006 National Science Foundation, Collaborative Research: Soft Tissues and Membrane Preservation in Permian Cephalopods, $40,000, February 1, 2002-January 31, 2006.
  • Corals (Anthozoa, Tabulata and Rugosa)

    Corals (Anthozoa, Tabulata and Rugosa)

    Bulletin de l’Institut Scientifique, Rabat, section Sciences de la Terre, 2008, n°30, 1-12. Corals (Anthozoa, Tabulata and Rugosa) and chaetetids (Porifera) from the Devonian of the Semara area (Morocco) at the Museo Geominero (Madrid, Spain), and their biogeographic significance Andreas MAY Saint Louis University - Madrid campus, Avenida del Valle 34, E-28003 Madrid, Spain e-mail: [email protected] Abstract. The paper describes the three tabulate coral species Caliapora robusta (Pradáčová, 1938), Pachyfavosites tumulosus Janet, 1965 and Thamnopora major (Radugin, 1938), the rugose coral Phillipsastrea ex gr. irregularis (Webster & Fenton in Fenton & Fenton, 1924) and the chaetetid Rhaphidopora crinalis (Schlüter, 1880). The specimens are described for the first time from Givetian and probably Frasnian strata of Semara area (Morocco, former Spanish Sahara). The material is stored in the Museo Geominero in Madrid. The tabulate corals and the chaetetid demonstrate close biogeographic relationships to Central and Eastern Europe as well as to Western Siberia. The fauna does not show any special influence of the Eastern Americas Realm. Key words: Anthozoa, biogeography, Devonian, tabulate corals, Morocco, West Sahara palaeogeographic province Coraux (Anthozoa, Tabulata et Rugosa) et chaetétides (Porifera) du Dévonien de la région de Smara (Maroc) déposés au Museo Geominero (Madrid) et leur signification biogéographique. Résumé. L´article décrit trois espèces de coraux tabulés : Caliapora robusta (Pradáčová, 1938), Pachyfavosites tumulosus Janet, 1965, et Thamnopora major (Radugin, 1938), le corail rugueux Phillipsastrea ex gr. irregularis (Webster & Fenton in Fenton & Fenton, 1924) ainsi que le chaetétide Rhaphidopora crinalis (Schlüter, 1880). Les spécimens, entreposés au Museo Geominero de Madrid, proviennent des couches givétiennes et probablement frasniennes de différents gisements de la région de Smara (Maroc, ancien Sahara espagnol), d’où elles sont décrites pour la première fois.