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Gfe Full Program 13.02.2019
Joint Meeting of the German and Israeli Societies of Developmental Biology Vienna, February 17-20, 2019 https://gfe2019.univie.ac.at/home/ Organizers Ulrich Technau, Eli Arama Co-Organizers Michael Brand, Fred Berger, Elly Tanaka, David Sprinzak, Peleg Hasson GfE https://www.vbio.de/gfe-entwicklungsbiologie IsSDB http://issdb.org Gesellschaft für Entwicklungsbiologie e.V. Geschäftsstelle: Dr. Thomas Thumberger Centre for Organismal Studies Universität Heidelberg Im Neuenheimer Feld 230 69120 Heidelberg E-mail: [email protected] Contents Sponsors ......................................................................................................................................... 4 General information ..................................................................................................................... 5 Venue .......................................................................................................................................... 5 Getting there................................................................................................................................ 5 From the airport ...................................................................................................................... 6 If you come by long distance train .......................................................................................... 6 Taxi ......................................................................................................................................... 6 If you -
Dorset and East Devon Coast for Inclusion in the World Heritage List
Nomination of the Dorset and East Devon Coast for inclusion in the World Heritage List © Dorset County Council 2000 Dorset County Council, Devon County Council and the Dorset Coast Forum June 2000 Published by Dorset County Council on behalf of Dorset County Council, Devon County Council and the Dorset Coast Forum. Publication of this nomination has been supported by English Nature and the Countryside Agency, and has been advised by the Joint Nature Conservation Committee and the British Geological Survey. Maps reproduced from Ordnance Survey maps with the permission of the Controller of HMSO. © Crown Copyright. All rights reserved. Licence Number: LA 076 570. Maps and diagrams reproduced/derived from British Geological Survey material with the permission of the British Geological Survey. © NERC. All rights reserved. Permit Number: IPR/4-2. Design and production by Sillson Communications +44 (0)1929 552233. Cover: Duria antiquior (A more ancient Dorset) by Henry De la Beche, c. 1830. The first published reconstruction of a past environment, based on the Lower Jurassic rocks and fossils of the Dorset and East Devon Coast. © Dorset County Council 2000 In April 1999 the Government announced that the Dorset and East Devon Coast would be one of the twenty-five cultural and natural sites to be included on the United Kingdom’s new Tentative List of sites for future nomination for World Heritage status. Eighteen sites from the United Kingdom and its Overseas Territories have already been inscribed on the World Heritage List, although only two other natural sites within the UK, St Kilda and the Giant’s Causeway, have been granted this status to date. -
Bodily Complexity: Integrated Multicellular Organizations for Contraction-Based Motility
fphys-10-01268 October 11, 2019 Time: 16:13 # 1 HYPOTHESIS AND THEORY published: 15 October 2019 doi: 10.3389/fphys.2019.01268 Bodily Complexity: Integrated Multicellular Organizations for Contraction-Based Motility Argyris Arnellos1,2* and Fred Keijzer3 1 IAS-Research Centre for Life, Mind & Society, Department of Logic and Philosophy of Science, University of the Basque Country, San Sebastián, Spain, 2 Department of Product and Systems Design Engineering, Complex Systems and Service Design Lab, University of the Aegean, Syros, Greece, 3 Department of Theoretical Philosophy, University of Groningen, Groningen, Netherlands Compared to other forms of multicellularity, the animal case is unique. Animals—barring some exceptions—consist of collections of cells that are connected and integrated to such an extent that these collectives act as unitary, large free-moving entities capable of sensing macroscopic properties and events. This animal configuration Edited by: Matteo Mossio, is so well-known that it is often taken as a natural one that ‘must’ have evolved, UMR8590 Institut d’Histoire et given environmental conditions that make large free-moving units ‘obviously’ adaptive. de Philosophie des Sciences et des Techniques (IHPST), France Here we question the seemingly evolutionary inevitableness of animals and introduce Reviewed by: a thesis of bodily complexity: The multicellular organization characteristic for typical Stuart A. Newman, animals requires the integration of a multitude of intrinsic bodily features between its New York Medical -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
Hastings & District Geological Society Journal
Hastings & District Geological Society Journal Hastings and District Geological Society affiliated to the Geologists’ Association President Professor G. David Price, UCL Founded 1992 Rock fall east of Ecclesbourne Glen, Hastings - 11th December 2009 Picture by David Burr Volume 16 December 2010 Cover picture: Rock fall east of Ecclesbourne Glen, Hastings - photo: David Burr (see page 46 for article) Taxonomic/Nomenclatural Disclaimer - This publication is not deemed to be valid for taxonomic/nomenclatural purposes. CONTENTS - Vol. 16, December 2010 2010 Officials and Committee …………………………………………………………………………………... 1 Minutes of the last AGM – 13 th December 2009 ………………………………………………………………... 2 Statement of Income & Expenditure for the Year Ending 31st December 2009 ……………………………….. 5 The Nautilus and the Ammonite - by Ken Brooks …………………….……………….……………………….. 6 Dinocochlea - ‘The Giant Gastropod Mystery’ - by Peter Austen ……………….……………………………... 11 Field trip to the Building Stones of Canterbury - by Trevor Devon …………………….………………………. 19 Coastal Erosion and Sea Defences in the Hastings area - by Siân Elder ………………………………………... 22 On Mantell, Buckland and Castle Hill, Newhaven - by Anthony Brook …………………….…………………. 32 From my Bookshelf - Book Reviews by Trevor Devon …………………….…………………………………... 34 What on Earth is under Sussex? - Book Review by Peter Austen …………………….……………………….... 35 Geology and Palaeontology in the News ………………………………………………………………………... 37 Extracts from ‘ Wealden News ’ - by Peter Austen ………………………………………………………………. 44 Geological Websites …………………………………………….………………………………………………. -
Mesodermal Anatomies in Cnidarian Polyps and Medusae
Int. J. Dev. Biol. 50: 589-599 (2006) doi: 10.1387/ijdb.062150ks Review Mesodermal anatomies in cnidarian polyps and medusae KATJA SEIPEL and VOLKER SCHMID* Institute of Zoology, University of Basel, Biocenter/Pharmacenter, Basel, Switzerland Introduction .............................................................................................................................................................................................................................. 589 Diploblasty in the historical perspective .......................................................................................................................................... 589 The cnidarian mesoderm unearthed ...................................................................................................................................................... 591 What is a mesoderm? ....................................................................................................................................................................................... 591 Muscle cells in Cnidaria ............................................................................................................................................................................... 592 Mesodermal muscle in Hydrozoa? ................................................................................................................................................. 592 Mesodermal differentiation in Scyphozoa, Cubozoa and Anthozoa ............................................... -
Evolution of Striated Muscle: Jellyfish and the Origin of Triploblasty
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Elsevier - Publisher Connector Developmental Biology 282 (2005) 14 – 26 www.elsevier.com/locate/ydbio Review Evolution of striated muscle: Jellyfish and the origin of triploblasty Katja Seipel, Volker Schmid* Institute of Zoology, Biocenter/Pharmacenter, Klingelbergstrasse 50, CH-4056 Basel, Switzerland Received for publication 6 October 2004, revised 9 March 2005, accepted 27 March 2005 Available online 26 April 2005 Abstract The larval and polyp stages of extant Cnidaria are bi-layered with an absence of mesoderm and its differentiation products. This anatomy originally prompted the diploblast classification of the cnidarian phylum. The medusa stage, or jellyfish, however, has a more complex anatomy characterized by a swimming bell with a well-developed striated muscle layer. Based on developmental histology of the hydrozoan medusa this muscle derives from the entocodon, a mesoderm-like third cell layer established at the onset of medusa formation. According to recent molecular studies cnidarian homologs to bilaterian mesoderm and myogenic regulators are expressed in the larval and polyp stages as well as in the entocodon and derived striated muscle. Moreover striated and smooth muscle cells may have evolved directly and independently from non-muscle cells as indicated by phylogenetic analysis of myosin heavy chain genes (MHC class II). To accommodate all evidences we propose that striated muscle-based locomotion coevolved with the nervous and digestive systems in a basic metazoan Bauplan from which the ancestors of the Ctenophora (comb jellyfish), Cnidaria (jellyfish and polyps), as well as the Bilateria are derived. -
Invertebrate-Paleontology-By-Clarkson.Pdf
Invertebrate Palaeontology and Evolution E.N.K. Clarkson Professor of Palaeontology Department of Geology University of Edinburgh Scotland Fourth edition b Blackwell Science Invertebrate Palaeontology and Evolution Invertebrate Palaeontology and Evolution E.N.K. Clarkson Professor of Palaeontology Department of Geology University of Edinburgh Scotland Fourth edition b Blackwell Science © 1979,1986,1993,1998 by E. N. K. Clarkson Published by Blackwell Science Ltd, a Blackwell Publishing company BLACKWELL PUBLlSHING 350 Mam Street, Malden, MA 02148-5020, USA %00 Garsington Road, Oxford OX4 2DQ, UK 550 Swanston Street, Carlton, Victoria 3053, Australia The right of E. :'\I. K. Clarkson to be identified as the Author of this Work has been asserted in accordance with the UK Copyright, Designs and Patents Act 1988. All rights reserved. No pad of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, ml'Chanical, photocopying, recording or otherwise, except as permitted by the UK Copyright, Designs and Patents Act 1988, WIthout the prior permission of the publisher. First published 1979 by Unwin Hyman Ltd Second edition 1986 Third edition 1993 by Chapman & Hall Fourth edition 1998 by Blackwell Science Ltd 10 2008 Library (If Congress Catalogins-in-Puhlicatioll Unta has bccn applied/or ISBN 978-0-632-05238-7 A catalogue record for this title is available from the British Library. Set by Wyvern 21 Ltd, Bristol Printed and bound in Singapore by C.Os. Printers Pte Ltd The publisher's policy is to use permanent paper from mills that operate a sustainable forestry policy, and which has been manufactured from pulp processed using acid-free and elementary chlorine-free practices. -
The Upper Jurassic of Europe: Its Subdivision and Correlation
The Upper Jurassic of Europe: its subdivision and correlation Arnold Zeiss In the last 40 years, the stratigraphy of the Upper Jurassic of Europe has received much atten- tion and considerable revision; much of the impetus behind this endeavour has stemmed from the work of the International Subcommission on Jurassic Stratigraphy. The Upper Jurassic Series consists of three stages, the Oxfordian, Kimmeridgian and Tithonian which are further subdivided into substages, zones and subzones, primarily on the basis of ammonites. Regional variations between the Mediterranean, Submediterranean and Subboreal provinces are discussed and correlation possibilities indicated. The durations of the Oxfordian, Kimmeridgian and Tithonian Stages are reported to have been 5.3, 3.4 and 6.5 Ma, respectively. This review of the present status of Upper Jurassic stratigraphy aids identification of a num- ber of problems of subdivision and definition of Upper Jurassic stages; in particular these include correlation of the base of the Kimmeridgian and the top of the Tithonian between Submediterranean and Subboreal Europe. Although still primarily based on ammonite stratigraphy, subdivision of the Upper Jurassic is increasingly being refined by the incorporation of other fossil groups; these include both megafossils, such as aptychi, belemnites, bivalves, gastropods, brachiopods, echino- derms, corals, sponges and vertebrates, and microfossils such as foraminifera, radiolaria, ciliata, ostracodes, dinoflagellates, calcareous nannofossils, charophyaceae, dasycladaceae, spores and pollen. Important future developments will depend on the detailed integration of these disparate biostratigraphic data and their precise combination with the abundant new data from sequence stratigraphy, utilising the high degree of stratigraphic resolution offered by certain groups of fos- sils. -
The Ammonite Faunas of the English Portland Beds and the Zones of the Portlandian Stage
I1 geol. Soc. Lond. Vol. 135. 1978, pp. 183-190, 2 figs.. 3 plates. Printed in Northern Ireland. The ammonite faunas of the English Portland Beds and the zones of the Portlandian Stage W. A. Wimbledon & J. C. W. Cope SUMMARY: On the basis of new and large collections of ammonites, a succession of ammonite faunas is described from the Portland Beds of southern England and a revised schemc of Standard Zones (=chronozones) proposed. The faunas of the Portland Freestone of Dorset are shown to consist largely of hitherto undescribed species; Titanites anguiformis sp. no". is described and figured therefrom. Correla- tions are oranosed. with other arcas where the Portland Beds occur. and the scheme is ~nr~,qr;.!cJullh 'hc ,.10.11 rchc.mr.pr~q,o.d.l In ('A,:) 114-1 cur th: ).wn>ur I'\,rll,ndi.>n ftun ir l:.U R J S I I die rl.Jcl!r,c.l u~th11~1. aid of new material. 'Portlandian' h preferred as stagc name for thc terminal Jurassic stage, The first scheme of zones for the Portlandian Stage of The faunal succession the Upper Jurassic was proposed by Salfeld (1913) but has suffered because some of the index species used A succession of distinctive ammonite faunas has been were of dubious interpretation. and it was based on recognised throughout the Portland 8eds (Fig. 1). In sections in the S Midlands now known to be incomplete. ascending stratigraphical order these are: Salfeld's zonal table was succeeded by Buckman's hemeral scheme. Buckman was the first person to Fauna 1: Progalbanites-Epiuirgatites fauna attempt any really detailed stratigraphical work on the The genus Progalbanires Spath 1933 appears to be Portland Beds, and he obtained, from quarries in the quite distinct from the earlier Volgian genus Zarais- Thame district ammonites which were described half a kites with which it has long been confused (see Casey century ago in 'Type Ammonites' under a multiplicity 1967, p. -
Invertebrate Zoology (BIO-225)
Bergen Community College Division of Mathematics, Science and Technology Department of Biology and Horticulture Invertebrate Zoology (BIO-225) General Course Syllabus SPRING 2016 Course Title Invertebrate Zoology (BIO-225) Course Description: This course is a survey of the organisms without backbones, the invertebrates. Topics include the taxonomic concepts of cladistics versus the Linnaean phylogenetic study of these organisms. Concepts such as prostomates vs. deuterostomates, the development of the coelom, metamorphosis, etc. will be discussed. Laboratory sessions include external and internal examinations (dissections) of these organisms and descriptive and practical reinforcement of lecture materials. Prerequisites: BIO 101, BIO 203 General Education Course: No Course Credits; 4.0 Hours per week: 6.0 3 hours lecture and 3 hours lab Course Coordinator: Elena Tartaglia Required Lecture Pechenik, J.A. 2010. Biology of the Invertebrates. 6th Edition, McGraw-Hill Textbook: Publishers. ISBN 978-0-07-302826-2 Laboratory Manual: Hickman, C.P., Kats, L.B., Dolphin, W.D., Dean, H.L., and R.S. Schuhmacher: Customized Laboratory Manual for General Biology II, McGraw-Hill Companies, Dubuque, IA, 2006. Student Learning Objectives - Lecture The student will be able to: 1. Describe the environment in which invertebrates exist and some of their adaptations. Assessment will be based upon performance on exam questions. 2. Explain how evolution works and how it leads to greater biodiversity. Assessment will be based upon performance on exam questions. 1 3. Discuss how invertebrates are classified. Assessment will be based upon performance on exam questions. 4. Describe the protists, phylogentically, morphologically, and their lifestyles Assessment will be based upon performance on exam questions. -
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This Manuscript has been submitted for publication in LITHOS. Please note that despite having undergone peer-review, the manuscript has not been formally accepted yet for publication and, therefore, it may be subject to some changes. Subsequent versions of the manuscript may include slightly different content. If accepted the final version of the manuscript will be available through the “PEER REVIEW PUBLICATION DOI” link Nature and timing of anatectic event of the Hida Belt (Japan): Constraints from titanite geochemistry and U-Pb age of clinopyroxene-bearing leucogranite Hironobu Harada1, [email protected] Tatsuki Tsujimori1,2, [email protected] Yoshiaki Kon3, [email protected] Shogo Aoki4,5, [email protected] Kazumasa Aoki4, [email protected] 1 Graduate School of Science, Tohoku University, Sendai 980-8578, Japan 2 Center for Northeast Asian Studies, Tohoku University Sendai 980-8576, Japan 3 Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, Tsukuba, Ibaraki 305-8567, Japan 4 Department of Applied Science, Okayama University of Science, Okayama 700-0005, Japan 5 Graduate School of International Resource Sciences, Akita University, Akita 010-8502, Japan Corresponding author: Hironobu Harada Abstract The Hida Belt, central Japan, is a continental fragment, which was once a part of the crustal basement of the East Asian continental margin. It consists mainly of Permo-Triassic granite-gneiss complexes with both syn-to-late-metamorphic migmatite or granite bodies. Clinopyroxene-bearing leucogranite, locally called as 'Inishi'-type migmatite, occurs characteristically in the migmatite zone associated with amphibolite and marble.