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The Tiger Beetles (Coleoptera, Cicindelidae) of the Southern Levant and Adjacent Territories: from Cybertaxonomy to Conservation Biology
A peer-reviewed open-access journal ZooKeys 734: 43–103 The(2018) tiger beetles( Coleoptera, Cicindelidae) of the southern Levant... 43 doi: 10.3897/zookeys.734.21989 MONOGRAPH http://zookeys.pensoft.net Launched to accelerate biodiversity research The tiger beetles (Coleoptera, Cicindelidae) of the southern Levant and adjacent territories: from cybertaxonomy to conservation biology Thorsten Assmann1, Estève Boutaud1, Jörn Buse2, Jörg Gebert3, Claudia Drees4,5, Ariel-Leib-Leonid Friedman4, Fares Khoury6, Tamar Marcus1, Eylon Orbach7, Ittai Renan4, Constantin Schmidt8, Pascale Zumstein1 1 Institute of Ecology, Leuphana University Lüneburg, Universitätsallee 1, D-21335 Lüneburg, Germany 2 Ecosystem Monitoring, Research and Wildlife Conservation (SB 23 Invertebrates and Biodiversity), Black Forest National Park, Kniebisstraße 67, D-72250 Freudenstadt, Germany 3 Karl-Liebknecht-Straße 73, D-01109 Dresden. Germany 4 Steinhardt Museum of Natural History, Tel Aviv University, Ramat-Aviv, Tel Aviv, IL-69978, Israel 5 Biocentre Grindel, Universität Hamburg, Martin-Luther-King-Platz 3, D-20146 Hamburg, Germany 6 Department of Biology and Biotechnology, American University of Madaba, P.O.Box 2882, Amman, JO-11821, Jordan 7 Remez St. 49, IL-36044 Qiryat Tiv’on, Israel 8 Deichstr. 13, D-21354 Bleckede, Germany Corresponding author: Thorsten Assmann ([email protected]) Academic editor: B. Guéorguiev | Received 1 November 2017 | Accepted 15 January 2018 | Published 5 February 2018 http://zoobank.org/7C3C687B-64BB-42A5-B9E4-EC588BCD52D5 Citation: Assmann T, Boutaud E, Buse J, Gebert J, Drees C, Friedman A-L-L, Khoury F, Marcus T, Orbach E, Renan I, Schmidt C, Zumstein P (2018) The tiger beetles (Coleoptera, Cicindelidae) of the southern Levant and adjacent territories: from cybertaxonomy to conservation biology. -
“Modern-Type Plate Tectonics”?
SILEIR RA A D B E E G D E A O D L Special Session, “A tribute to Edilton Santos, a leader in Precambrian O E I G C I A Geology in Northeastern Brazil”, edited by A.N. Sial and V.P. Ferreira O BJGEO S DOI: 10.1590/2317-4889202020190095 Brazilian Journal of Geology D ESDE 1946 Dawn of metazoans: to what extent was this influenced by the onset of “modern-type plate tectonics”? Umberto G. Cordani1* , Thomas R. Fairchild1 , Carlos E. Ganade1 , Marly Babinski1 , Juliana de Moraes Leme1 Abstract The appearance of complex megascopic multicellular eukaryotes in the Ediacaran occurred just when the dynamics of a cooling Earth allowed establishment of a new style of global tectonics that continues to the present as “modern-type plate tectonics”. The advent of this style was first registered in 620 Ma-old coesite-bearing Ultra-High Pressure eclogites within the Transbrasiliano-Kandi mega-shear zone along the site of the West Gondwana Orogeny (WGO). These eclogites comprise the oldest evidence of slab-pull deep subduction capable of inducing con- tinental collisions and producing high-relief Himalayan-type mega-mountains. Life, prior to this time, was essentially microscopic. Yet with increasing Neoproterozoic oxygenation and intensified influx of nutrients to Ediacaran oceans, resulting from the erosion of these mountains, complex macroscopic heterotrophic eukaryotes arose and diversified, taking the biosphere to a new evolutionary threshold. The repeated elevation of Himalayan-type mega-mountains ever since then has continued to play a fundamental role in nutrient supply and biosphere evolution. Other authors have alluded to the influence of Gondwana mountain-building upon Ediacaran evolution, however we claim here to have identified when and where it began. -
Tabelliscolex (Cricocosmiidae: Palaeoscolecidomorpha) from the Early Cambrian Chengjiang Biota, and the Evolution of Seriation in Ecdysozoa
Accepted Manuscript Journal of the Geological Society Tabelliscolex (Cricocosmiidae: Palaeoscolecidomorpha) from the early Cambrian Chengjiang Biota, and the evolution of seriation in Ecdysozoa Xiaomei Shi, Richard J. Howard, Gregory D. Edgecombe, Xianguang Hou & Xiaoya Ma DOI: https://doi.org/10.1144/jgs2021-060 To access the most recent version of this article, please click the DOI URL in the line above. When citing this article please include the above DOI. This article is part of the Advances in the Cambrian Explosion collection available at: https://www.lyellcollection.org/cc/advances-cambrian-explosion Received 26 May 2021 Revised 2 August 2021 Accepted 7 August 2021 © 2021 The Author(s). This is an Open Access article distributed under the terms of the Creative Commons Attribution 4.0 License (http://creativecommons.org/licenses/by/4.0/). Published by The Geological Society of London. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics Supplementary material at https://doi.org/10.6084/m9.figshare.c.5551565 Manuscript version: Accepted Manuscript This is a PDF of an unedited manuscript that has been accepted for publication. The manuscript will undergo copyediting, typesetting and correction before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Although reasonable efforts have been made to obtain all necessary permissions from third parties to include their copyrighted content within this article, their full citation and copyright line may not be present in this Accepted Manuscript version. Before using any content from this article, please refer to the Version of Record once published for full citation and copyright details, as permissions may be required. -
Aysheaia Prolata from the Utah Wheeler Formation (Drumian, Cambrian) Is a Frontal Appendage of the Radiodontan Stanleycaris
Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris STEPHEN PATES, ALLISON C. DALEY, and JAVIER ORTEGA-HERNÁNDEZ Pates, S., Daley, A.C., and J. Ortega-Hernández, J. 2017. Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris. Acta Palaeontologica Polonica 62 (3): 619–625. Aysheaia prolata, was described as the only lobopodian from the Drumian (Cambrian) Wheeler Formation in Utah, USA, and the sole representative of this genus besides the type species Aysheaia pedunculata, from the Cambrian (Stage 5) Stephen Formation, British Columbia. A redescription of Aysheaia prolata reveals previously overlooked morphological features, including segmental boundaries between putative lobopods, and curved terminal spines on the putative anterior end. These observations undermine lobopodian affinities of Aysheaia prolata, and instead we interpret this specimen as an isolated radiodontan frontal appendage. The presence of 11 podomeres, five of which possess elongate and anteri- orly recurved ventral blades with auxiliary spines, together with shorter robust dorsal spines, identify the specimen as Stanleycaris. This represents the first report of Stanelycaris outside of the Cambrian Stage 5 thin Stephen Formation in British Columbia, expanding its palaeobiogeographic and stratigraphic range. Aysheaia is left as a monotypic genus endemic to the Burgess Shale. The Spence Shale luolishaniid Acinocrinus stichus is currently the only lobopodian known from the Cambrian of Utah. Key words: Euarthropoda, Radiodonta, Hurdiidae, Cambrian, United States. Stephen Pates [[email protected]], Department of Zoology, University of Oxford, Oxford, OX1 3PS, UK. Allison C. Daley [[email protected]], Institute of Earth Sciences, University of Lausanne, Géopolis, CH-1015, Lausanne, Switzerland. -
The Origin of Tetraradial Symmetry in Cnidarians
The origin of tetraradial symmetry in cnidarians JERZY DZIK, ANDRZEJ BALINSKI AND YUANLIN SUN Dzik, J., Balinski, A. & Sun, Y. 2017: The origin of tetraradial symmetry in cnidarians. Lethaia, DOI: 10.1111/let.12199. Serially arranged sets of eight septa-like structures occur in the basal part of phosphatic tubes of Sphenothallus from the early Ordovician (early Floian) Fenxi- ang Formation in Hubei Province of China. They are similar in shape, location and number, to cusps in chitinous tubes of extant coronate scyphozoan polyps, which supports the widely accepted cnidarian affinity of this problematic fossil. However, unlike the recent Medusozoa, the tubes of Sphenothallus are flattened at later stages of development, showing biradial symmetry. Moreover, the septa (cusps) in Sphenothallus are obliquely arranged, which introduces a bilateral component to the tube symmetry. This makes Sphenothallus similar to the Early Cambrian Paiutitubulites, having similar septa but with even more apparent bilat- eral disposition. Biradial symmetry also characterizes the Early Cambrian tubular fossil Hexaconularia, showing a similarity to the conulariids. However, instead of being strictly tetraradial like conulariids, Hexaconularia shows hexaradial symme- try superimposed on the biradial one. A conulariid with a smooth test showing signs of the ‘origami’ plicated closure of the aperture found in the Fenxiang For- mation supports the idea that tetraradial symmetry of conulariids resulted from geometrical constrains connected with this kind of closure. Its minute basal attachment surface makes it likely that the holdfasts characterizing Sphenothallus and advanced conulariids are secondary features. This concurs with the lack of any such holdfast in the earliest Cambrian Torellella, as well as in the possibly related Olivooides and Quadrapyrgites. -
Of Time and Taphonomy: Preservation in the Ediacaran
See discussions, stats, and author profiles for this publication at: http://www.researchgate.net/publication/273127997 Of time and taphonomy: preservation in the Ediacaran CHAPTER · JANUARY 2014 READS 36 2 AUTHORS, INCLUDING: Charlotte Kenchington University of Cambridge 5 PUBLICATIONS 2 CITATIONS SEE PROFILE Available from: Charlotte Kenchington Retrieved on: 02 October 2015 ! OF TIME AND TAPHONOMY: PRESERVATION IN THE EDIACARAN CHARLOTTE G. KENCHINGTON! 1,2 AND PHILIP R. WILBY2 1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK <[email protected]! > 2British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK ABSTRACT.—The late Neoproterozoic witnessed a revolution in the history of life: the transition from a microbial world to the one known today. The enigmatic organisms of the Ediacaran hold the key to understanding the early evolution of metazoans and their ecology, and thus the basis of Phanerozoic life. Crucial to interpreting the information they divulge is a thorough understanding of their taphonomy: what is preserved, how it is preserved, and also what is not preserved. Fortunately, this Period is also recognized for its abundance of soft-tissue preservation, which is viewed through a wide variety of taphonomic windows. Some of these, such as pyritization and carbonaceous compression, are also present throughout the Phanerozoic, but the abundance and variety of moldic preservation of body fossils in siliciclastic settings is unique to the Ediacaran. In rare cases, one organism is preserved in several preservational styles which, in conjunction with an increased understanding of the taphonomic processes involved in each style, allow confident interpretations of aspects of the biology and ecology of the organisms preserved. -
Darwin's Doubt
Debating Darwin’s Doubt A Scientific Controversy that Can No Longer Be Denied DAVID KLINGHOFFER, EDITOR DISCOVERY INSTITUTE PRESS SEATTLE 2015 Description This book contains essays responding to criticism of Darwin’s Doubt: The Explosive Origin of Animal Life and the Case for Intelligent Design by Stephen Meyer. The book explores topics such as orphan genes, cladistics, small shelly fossils, protein evolution, the length of the Cambrian explosion, the God-of-the-Gaps objection to intelligent design, and criticisms raised by proponents of theistic evolution. Contributors include Stephen Meyer, Douglas Axe, David Berlinski, William Dembski, Ann Gauger, Casey Luskin, and Paul Nelson. Edited by David Klinghoffer. Copyright Notice Copyright © 2015 by Discovery Institute. All Rights Reserved. Publisher’s Note This book is part of a series published by the Center for Science & Culture at Discovery Institute in Seattle. Previous books include Signature of Controversy: Responses to CritiCs of Signature in the Cell, edited by David Klinghoffer; The Myth of Junk DNA by Jonathan Wells; The Deniable Darwin & Other Essays by David Berlinski; and DisCovering Intelligent Design: A Journey into the SCientifiC EvidenCe by Gary Kemper, Hallie Kemper, and Casey Luskin. Library Cataloging Data Debating Darwin’s Doubt: A SCientifiC Controversy that Can No Longer Be Denied Edited by David Klinghoffer. BISAC Subject: SCI027000 SCIENCE / Life Sciences / Evolution BISAC Subject: SCI080000 SCIENCE / Essays BISAC Subject: SCI034000 SCIENCE / History ISBN-13: 978-1-936599-30-1 (Kindle) 978-1-936599-31-8 (EPUB) 978-1-936599-28-8 (paperback) Publisher Information Discovery Institute Press, 208 Columbia Street, Seattle, WA 98101 Internet: http://www.discoveryinstitutepress.com/ First Edition. -
Lobopodian Phylogeny Reanalysed
BRIEF COMMUNICATIONS ARISING Phylogenetic position of Diania challenged ARISING FROM J. Liu et al. Nature 470, 526–530 (2011) Liu et al.1 describe a new and remarkable fossil, Diania cactiformis. absent. For example, character 6 (position of frontal appendage) can This animal apparently combined the soft trunk of lobopodians (a only be coded in taxa that possess a frontal appendage (character 5) in group including the extant velvet worms in addition to many the first instance (such that a ‘‘0’’ for character 5 necessitates a ‘‘-’’ for Palaeozoic genera) with the jointed limbs that typify arthropods. character 6). In morphological analyses such as this, inapplicable They go on to promote Diania as the immediate sister group to the states are usually assumed to have no bearing on the analysis, being arthropods, and conjecture that sclerotized and jointed limbs may reconstructed passively in the light of known states. In analyses of therefore have evolved before articulated trunk tergites in the imme- nucleotide data, by contrast, gaps may alternatively be construed as a diate arthropod stem. The data published by Liu et al.1 do not un- fifth and novel state, because shared deletions from some ancestral ambiguously support these conclusions; rather, we believe that Diania sequence may actually be informative. If this assumption is made with probably belongs within an unresolved clade or paraphyletic grade of morphological data, however, all the logically uncodable states in a lobopodians. character are initially assumed to be homologous, and a legitimate Without taking issue with the interpretation of Diania offered by basis for recognizing clades. -
Hallucigenia's Onychophoran-Like Claws
LETTER doi:10.1038/nature13576 Hallucigenia’s onychophoran-like claws and the case for Tactopoda Martin R. Smith1 & Javier Ortega-Herna´ndez1 The Palaeozoic form-taxon Lobopodia encompasses a diverse range of Onychophorans lack armature sclerites, but possess two types of ap- soft-bodied‘leggedworms’ known from exceptionalfossil deposits1–9. pendicular sclerite: paired terminal claws in the walking legs, and den- Although lobopodians occupy a deep phylogenetic position within ticulate jaws within the mouth cavity9,23.AsinH. sparsa, claws in E. Panarthropoda, a shortage of derived characters obscures their evo- kanangrensis exhibit a broad base that narrows to a smooth conical point lutionary relationships with extant phyla (Onychophora, Tardigrada (Fig. 1e–h). Each terminal clawsubtends anangle of130u and comprises and Euarthropoda)2,3,5,10–15. Here we describe a complex feature in two to three constituent elements (Fig. 1e–h). Each smaller element pre- the terminal claws of the mid-Cambrian lobopodian Hallucigenia cisely fills the basal fossa of its container, from which it can be extracted sparsa—their construction from a stack of constituent elements— with careful manipulation (Fig. 1e, g, h and Extended Data Fig. 3a–g). and demonstrate that equivalent elements make up the jaws and claws Each constituent element has a similar morphology and surface orna- of extant Onychophora. A cladistic analysis, informed by develop- ment (Extended Data Fig. 3a–d), even in an abnormal claw where mental data on panarthropod head segmentation, indicates that the element tips are flat instead of pointed (Extended Data Fig. 3h). The stacked sclerite components in these two taxa are homologous— proximal bases of the innermost constituent elements are associated with resolving hallucigeniid lobopodians as stem-group onychophorans. -
Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2017PR005 Globusphyton Wang et al., an Ediacaran macroalga, crept on seafloor in the Yangtze Block, South China AcceptedYE WANG1 AND YUE WANG2 1School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China 2School of Resources and Environments, Guizhou University, Guiyang 550025, China (e-mail: [email protected]) Abstract. The Ediacaran genus Globusphyton Wang et al., only including one species G. lineare Wang et al., is a eukaryotic macroalgamanuscript in the Wenghui biota from black shale of the upper Doushantuo Formation (ca. 560–551 Ma) in northeastern Guizhou, South China. It was assigned as one of significant fossils in the assemblage and biozone divisions in the middle-late Ediacaran Period. Morphologically, Globusphyton is composed of several structural components, displaying that it had tissue differentiation to serve various bio-functions. Its prostrate stolon, a long ribbon bundled by unbranching filaments, crept by holdfasts on the seafloor. Its pompon-like thalli, the circular to oval thallus-tuft composed of many filamentous dichotomies, may have served for photosynthesis. -
An Armoured Cambrian Lobopodian from China with Arthropod-Like Appendages
LETTER doi:10.1038/nature09704 An armoured Cambrian lobopodian from China with arthropod-like appendages Jianni Liu1,2, Michael Steiner2, Jason A. Dunlop3, Helmut Keupp2, Degan Shu1,4, Qiang Ou4, Jian Han1, Zhifei Zhang1 & Xingliang Zhang1 Cambrian fossil Lagersta¨tten preserving soft-bodied organisms expanded compared to the trunk and shows no sign of becoming have contributed much towards our understanding of metazoan thinner towards the end. No mouth can be observed (Figs 2a–e and origins1–3. Lobopodians are a particularly interesting group that 3). A small projection occurs at the posterior end of the body (Figs 2a–c diversified and flourished in the Cambrian seas. Resembling and 3). The main body trunk is sub-circular in outline and composed ‘worms with legs’, they have long attracted much attention in that of nine segments, each comprising five rows of sub-parallel transverse they may have given rise to both Onychophora (velvet worms)4–6 annulations alternating with five rings of tubercles with tiny spines and Tardigrada (water bears)7,8,aswellastoarthropodsingeneral9–12. (Fig. 1a, b); each with 10–12 tubercles. The tiny spines are not well- Here we describe Diania cactiformis gen. et sp. nov. as an ‘armoured’ preserved, possibly as an artefact of taphonomy, and in most cases only lobopodian from the Chengjiang fossil Lagersta¨tte (Cambrian Stage the tubercles of these spines are observable (Figs 1a, b and 2b–c). 3), Yunnan, southwestern China. Although sharing features with A pair of strongly armoured appendages protrudes from the ven- other typical lobopodians, it is remarkable for possessing robust trolateral region of each segment, each limb attached robustly at its and probably sclerotized appendages, with what appear to be articu- base to the otherwise slender trunk. -
Phylogenetic Position of Diania Challenged
Mounce, R. C. P. and Wills, M. A. (2011) Phylogenetic position of Diania challenged. Nature, 476 (7359). E1-E4. ISSN 0028-0836 Link to official URL (if available): http://dx.doi.org/10.1038/nature10266 Opus: University of Bath Online Publication Store http://opus.bath.ac.uk/ This version is made available in accordance with publisher policies. Please cite only the published version using the reference above. See http://opus.bath.ac.uk/ for usage policies. Please scroll down to view the document. BRIEF COMMUNICATIONS ARISING ; Phylogenetic position of Diania challenged ARISING FROM J. Liu et al. Nature 470, 526–530 (2011) Liu et al.1 describe a new and remarkable fossil, Diania cactiformis. absent. For example, character 6 (position of frontal appendage) can This animal apparently combined the soft trunk of lobopodians (a only be coded in taxa that possess a frontal appendage (character 5) in group including the extant velvet worms in addition to many the first instance (such that a ‘‘0’’ for character 5 necessitates a ‘‘-’’ for Palaeozoic genera) with the jointed limbs that typify arthropods. character 6). In morphological analyses such as this, inapplicable They go on to promote Diania as the immediate sister group to the states are usually assumed to have no bearing on the analysis, being arthropods, and conjecture that sclerotized and jointed limbs may reconstructed passively in the light of known states. In analyses of therefore have evolved before articulated trunk tergites in the imme- nucleotide data, by contrast, gaps may alternatively be construed as a diate arthropod stem. The data published by Liu et al.1 do not un- fifth and novel state, because shared deletions from some ancestral ambiguously support these conclusions; rather, we believe that Diania sequence may actually be informative.