Relationships Within Eumalacostracan Crustacea Frederick R
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And Peracarida
Contributions to Zoology, 75 (1/2) 1-21 (2006) The urosome of the Pan- and Peracarida Franziska Knopf1, Stefan Koenemann2, Frederick R. Schram3, Carsten Wolff1 (authors in alphabetical order) 1Institute of Biology, Section Comparative Zoology, Humboldt University, Philippstrasse 13, 10115 Berlin, Germany, e-mail: [email protected]; 2Institute for Animal Ecology and Cell Biology, University of Veterinary Medicine Hannover, Buenteweg 17d, D-30559 Hannover, Germany; 3Dept. of Biology, University of Washington, Seattle WA 98195, USA. Key words: anus, Pancarida, Peracarida, pleomeres, proctodaeum, teloblasts, telson, urosome Abstract Introduction We have examined the caudal regions of diverse peracarid and The variation encountered in the caudal tagma, or pancarid malacostracans using light and scanning electronic posterior-most body region, within crustaceans is microscopy. The traditional view of malacostracan posterior striking such that Makarov (1978), so taken by it, anatomy is not sustainable, viz., that the free telson, when present, bears the anus near the base. The anus either can oc- suggested that this region be given its own descrip- cupy a terminal, sub-terminal, or mid-ventral position on the tor, the urosome. In the classic interpretation, the telson; or can be located on the sixth pleomere – even when a so-called telson of arthropods is homologized with free telson is present. Furthermore, there is information that the last body unit in Annelida, the pygidium (West- might be interpreted to suggest that in some cases a telson can heide and Rieger, 1996; Grüner, 1993; Hennig, 1986). be absent. Embryologic data indicates that the condition of the body terminus in amphipods cannot be easily characterized, Within that view, the telson and pygidium are said though there does appear to be at least a transient seventh seg- to not be true segments because both structures sup- ment that seems to fuse with the sixth segment. -
Paleoentomofauna Del Pérmico Temprano En Uruguay
UNIVERSIDAD DE LA REPÚBLICA FACULTAD DE CIENCIAS - PEDECIBA ÁREA BIOLOGÍA- SUBÁREA ZOOLOGÍA TESIS DE MAESTRÍA Paleoentomofauna del Pérmico temprano en Uruguay Viviana Calisto Directora de tesis: Dra. Graciela Piñeiro Co-director de tesis: Dr. Enrique Morelli TRIBUNAL Presidente: Dr. Claudio Gaucher Vocales: Dra. Ana Verdi y Dra. Patricia González Vainer Diciembre, 2018 1 ÍNDICE RESUMEN ………………………………………………………..………………………….……………………………..…… 4 ABSTRACT……………………………………………………………………………….…………………………….…………. 5 ÍNDICE DE FIGURAS…………………………………………….……….…………………………………..…………… 7 CAPÍTULO 1………………………………………..………………………………..………………………………..….…. 11 INTRODUCCIÓN……………………………………………………………….……………….………………….……..…. 11 a. Los primeros insectos fósiles……………………………….………………..………………..…………….…..11 b. Preservación de los insectos fósiles………………………….…………………..……….……………..…..12 c. Caracterización de la Formación Mangrullo ……………….………………………...………………..…14 d. Registros de insectos fósiles en Uruguay …………………….……………….………………..…….…...16 HIPÓTESIS…………………………………………….……………………………………………………………………….….18 OBJETIVO GENERAL………………………………….…………..…………………..…………………………………..…18 OBJETIVOS ESPECÍFICOS…….…………………………………..………………..………………………….…….……. 18 MATERIALES Y METODOLOGÍAS……………..………….……………………………………………………………. 19 a. Materiales……………………………………………………………………………..…………………………..……... 19 b. Área de estudio y colecta……………………………………………………..…………………..………….…... 19 c. Fotografías y diagramación………………………………………………..………………….....….…………… 22 CAPÍTULO 2 - BLATTARIA ………………………………….…………..…………..……………………….…..… 23 Antecedentes de Blattaria………………………………….………………….…………….………………………..… -
Fossil Calibrations for the Arthropod Tree of Life
bioRxiv preprint doi: https://doi.org/10.1101/044859; this version posted June 10, 2016. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. FOSSIL CALIBRATIONS FOR THE ARTHROPOD TREE OF LIFE AUTHORS Joanna M. Wolfe1*, Allison C. Daley2,3, David A. Legg3, Gregory D. Edgecombe4 1 Department of Earth, Atmospheric & Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA 2 Department of Zoology, University of Oxford, South Parks Road, Oxford OX1 3PS, UK 3 Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PZ, UK 4 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK *Corresponding author: [email protected] ABSTRACT Fossil age data and molecular sequences are increasingly combined to establish a timescale for the Tree of Life. Arthropods, as the most species-rich and morphologically disparate animal phylum, have received substantial attention, particularly with regard to questions such as the timing of habitat shifts (e.g. terrestrialisation), genome evolution (e.g. gene family duplication and functional evolution), origins of novel characters and behaviours (e.g. wings and flight, venom, silk), biogeography, rate of diversification (e.g. Cambrian explosion, insect coevolution with angiosperms, evolution of crab body plans), and the evolution of arthropod microbiomes. We present herein a series of rigorously vetted calibration fossils for arthropod evolutionary history, taking into account recently published guidelines for best practice in fossil calibration. -
The Place of the Hoplocarida in the Malacostracan Pantheon
The University of Maine DigitalCommons@UMaine Marine Sciences Faculty Scholarship School of Marine Sciences 6-1-2009 The lP ace of the Hoplocarida in the Malacostracan Pantheon Les Watling University of Maine - Main, [email protected] C. H.J. Hof F. R. Schram Follow this and additional works at: https://digitalcommons.library.umaine.edu/sms_facpub Repository Citation Watling, Les; Hof, C. H.J.; and Schram, F. R., "The lP ace of the Hoplocarida in the Malacostracan Pantheon" (2009). Marine Sciences Faculty Scholarship. 134. https://digitalcommons.library.umaine.edu/sms_facpub/134 This Article is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Marine Sciences Faculty Scholarship by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. JOURNALOF CRUSTACEANBIOLOGY, 20, SPECIALNUMBER 2: 1-11, 2000 THE PLACE OF THE HOPLOCARIDA IN THE MALACOSTRACAN PANTHEON Les Watling, Cees H. J. Hof, and Frederick R. Schram (LW,corresponding) Darling MarineCenter, University of Maine, Walpole, Maine 04573, U.S.A. (e-mail: [email protected]);(CHJH) Department of EarthSciences, University of Bristol, Wills MemorialBuilding, Queens Road, Bristol BS8 1RJ, United Kingdom (e-mail: [email protected]); (FRS) Zoological Museum, University of Amsterdam,Post Box 94766, NL-1090 GT Amsterdam, The Netherlands(e-mail: [email protected]) ABSTRACT The stomatopodbody plan is highly specializedfor predation,yet the SuperorderHoplocarida originatedfrom something other than the "lean,mean, killing machine" seen today.The fossil record of the groupindicates that it originatedearly on froma non-raptorialancestor, with the specialized predatorymorphology developing much later. -
Pygocephalomorph Crustaceans from the Early Permian of Uruguay: Constraints on Taxonomy
Rev. bras. paleontol. 15(1):33-48, Janeiro/Abril 2012 © 2012 by the Sociedade Brasileira de Paleontologia doi:10.4072/rbp.2012.1.03 PYGOCEPHALOMORPH CRUSTACEANS FROM THE EARLY PERMIAN OF URUGUAY: CONSTRAINTS ON TAXONOMY GRACIELA PIÑEIRO, ELIZABETH MOROSI, ALEJANDRO RAMOS Departamento de Evolución de Cuencas, Facultad de Ciencias, Iguá, 4225, 11400, Montevideo, Uruguay. [email protected], [email protected], [email protected] FABRIZIO SCARABINO Museo Nacional de Historia Natural, 25 de Mayo, 582, 11000, Montevideo, Uruguay. [email protected] ABSTRACT – Hoplita ginsburgi comb. nov. (Fabre & Huard) is described from the Early Permian Mangrullo Formation of Uruguay. It is a large to very large pygocephalomorph characterized by a combination of characters that includes the presence of a round carapace bearing short, anterolateral, spine-like processes and a posteriorly extended, V-shaped cervical groove. Other traits include well-developed angular or round pleomeral pleurae bearing terminal spine-like processes, a tail fan with large and rounded uropod exopod, lacking diaresis, a roughly trapezoidal telson that gives support to small lateral spines and a relatively large triangular caudal spine. This species is also distinguished by the presence of a putative, simplified endophragmal skeleton, a structure not previously described in pygocephalomorphs, but present in fossil and extant higher crustaceans, where its function, although not so well understood, has been related to support for the limb musculature. Sexual dimorphism appears in Hoplita with the recognition of gonopods in males and seminal receptacles in the females. The studied specimens include moulting exuvia distinct from live individuals. The status of Notocarididae, the only currently recognized Gondwanan family, was examined, as well as the strength of the characters previously recognized as diagnostic. -
Paleozoic Cumaceans (Crustacea, Malacostraca, Peracarida) from North America
Contributions to Zoology, 72 (I) 1-16 (2003) SPB Academic Publishing hv, The Hague Paleozoic cumaceans (Crustacea, Malacostraca, Peracarida) from North America ² Frederick+R. Schram Cees+H.J. Hof Mapes³ & Snowdon² ¹, Royal+H. Polly 1 Institute for Biodiversity and Ecosystem Dynamics, University ofAmsterdam, Post Box 94766, 1090 GT 2 Amsterdam, Netherlands, [email protected]; Dept. ofEarth Sciences, University of Bristol, Bristol 3 BS8 IRJ, UK; Dept. of Geological Sciences, Ohio University, Athens, Ohio 45701, USA, e-mail: mapes@oak. cats, ohiou.edu Keywords:: Cumacea, North America, Paleozoic, Peracarida Abstract forms inhabit the fine sand and coarse silts perfect for fossilization (Schram, 1986). Bachmayer, (1960) Thiee new species of are described from North malacostracans recorded a poorly preserved cumacean-like speci- America in the UpperMississippian Into Formation ofArkansas, men Palaeocuma hessi from the Callovian, Middle and the Pennsylvanian Eudora Shale of southeastern Kansas. of France’. These Jurassic, Subsequently, Malzahn (1972) appear to be the oldest fossils attributed to the Cumacea and studied two Permian are well-preserved species of the only the third collection of fossil cumaceansanywhere to be described. Permian genus O. and O. Previously depicted forms occur in the Opthalmdiastylis, inflata costata, and Jurassic of Europe. We herein double the numberof described from the marl beds ofZechstein I, Kamp-Lintfort, fossil cumacean species and suggest some adjustments necessary Germany. These latter taxa are noteworthy in that tothe higher ofthe accommodate taxonomy group to apomorphic they exhibit lobed as the features of distinctly eyes, generic the fossil and Recent forms. name implies. This describes paper three new species of Car- Contents boniferous cumaceans from the lino Formation (Up- per Mississippian) of northwestern Arkansas, and the Eudora Shale (Pennsylvanian) of southeastern Introduction 1 Localities and Kansas. -
Ch 21 Crustacea.Pdf
rustaceansare one of the most popular invertebrate groups, even amongnonbiologists, for they include someof the world's most delec- table gourmet fare,such as lobsters,crabs, and shrimps (Figure 21.1). There are an estimated 70,000described living speciesof Crustacea,and probably five or ten times that number waiting to be discovered and named. They exhibit an incredible diversity of form, habit, and size. The smallest known crustaceans are less than 100 pm in length and live on the antennules of cope- pods. The largest are Japanesespider crabs (Macrocheiraknempferi),withleg spans of 4m, and giant Tasmanian crabs (Pseudocarcinusgigas) with carapace widths of 46 cm. The heaviest crustaceans are probablv American lobsters (Homarus americanus),which, before the present era of overfishing, attained weights in excessof 20 kilograms. The world's largest land arthropod by weight (and possibly the largest land invertebrate) is the coconut crab (Birgus latro), Classificationof The Animal weighing in at up to 4 kg. Crustaceans are found Kingdom(Metazoa) at all depths in every marine, brackislu and fresh- water envfuonment on Earth, including in pools at Non-Bilateria* Lophophorata 6,000m elevation (fairy shrimp and cladocerans in (a.k.a. the diploblasts) PHYLUM PHORONIDA northem Chile). Afew have become PHYLUM PORIFERA PHYLUM BRYOZOA successful on PHYLUM PLACOZOA PHYLUM BRACHIOPODA. land, the mostnotablebeing sowbugs and pillbugs I PHYLUM CNIDARIA EcpYsozoA (the terrestrial isopods). PHYLUM CTENOPHORA Nematoida Crustaceans are commonly the dominant or- PHYLUM NEMATODA Bilateria ganisms in aquatic subterranean ecosystems, and PHYLUM NEMATOMORPHA (a.k.a.the triploblasts) new species of these stygobionts continue to be Scalidophora PHYLUM XENACOELOMORPHA discovered as new caves are explored. -
New Pygocephalomorph Crustaceans from the Permian of China and Their Phylogenetic Significance
UvA-DARE (Digital Academic Repository) The fossil Crustacea of China: their taxonomy, palaeobiology, biogeography and phylogenetic relationships Taylor, R.S. Publication date 1999 Link to publication Citation for published version (APA): Taylor, R. S. (1999). The fossil Crustacea of China: their taxonomy, palaeobiology, biogeography and phylogenetic relationships. Fac. der Biologie. General rights It is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), other than for strictly personal, individual use, unless the work is under an open content license (like Creative Commons). Disclaimer/Complaints regulations If you believe that digital publication of certain material infringes any of your rights or (privacy) interests, please let the Library know, stating your reasons. In case of a legitimate complaint, the Library will make the material inaccessible and/or remove it from the website. Please Ask the Library: https://uba.uva.nl/en/contact, or a letter to: Library of the University of Amsterdam, Secretariat, Singel 425, 1012 WP Amsterdam, The Netherlands. You will be contacted as soon as possible. UvA-DARE is a service provided by the library of the University of Amsterdam (https://dare.uva.nl) Download date:07 Oct 2021 Permian Pygocephalomorph Taxonomy and Phytogeny Chapter 2 New Pygocephalomorph Crustaceans from the Permian of China and their Phylogenetic Significance Abstract Members of the malacostracan Order Pygocephalomorpha are among the most charac teristic elements in nearshore marine and fresh water communities in Carboniferous and Permian of Europe and North America. A new family of pygocephalomorph Eumalacostraca, the Tylocarididae, with two new monospecific genera, is described from China, where it occurs in the Early Permian Tungtzeyen Formation of Fujian, and in the Late Permian Lungtan Formation of Hunan. -
The Crustacea of China: a Palaeobiogeographical Perspective
UvA-DARE (Digital Academic Repository) The fossil Crustacea of China: their taxonomy, palaeobiology, biogeography and phylogenetic relationships Taylor, R.S. Publication date 1999 Link to publication Citation for published version (APA): Taylor, R. S. (1999). The fossil Crustacea of China: their taxonomy, palaeobiology, biogeography and phylogenetic relationships. Fac. der Biologie. General rights It is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), other than for strictly personal, individual use, unless the work is under an open content license (like Creative Commons). Disclaimer/Complaints regulations If you believe that digital publication of certain material infringes any of your rights or (privacy) interests, please let the Library know, stating your reasons. In case of a legitimate complaint, the Library will make the material inaccessible and/or remove it from the website. Please Ask the Library: https://uba.uva.nl/en/contact, or a letter to: Library of the University of Amsterdam, Secretariat, Singel 425, 1012 WP Amsterdam, The Netherlands. You will be contacted as soon as possible. UvA-DARE is a service provided by the library of the University of Amsterdam (https://dare.uva.nl) Download date:29 Sep 2021 Fossil Crustacea of China Chapter 5 The Crustacea of China: a Palaeobiogeographical Perspective Abstract The fossil record in China has been much discussed in the scientific literature of late with the recent discovery of new localities there with many new and informative fossil taxa. One group in particular has received attention, the Crustacea (and the Arthropoda in general). -
Tesis De Maestrïa Estudio Comparativo Del Cráneo En
UNIVERSIDAD DE LA REPUBLICA PEDECIBA, FACULTAD DE CIENCIAS ÁREA BIOLOGÍA, SUBÁREA ZOOLOGÍA TESIS DE MAESTRÏA ESTUDIO COMPARATIVO DEL CRÁNEO EN MESOSAURIDAE DE LA FORMACION MANGRULLO (PÉRMICO TEMPRANO) DE URUGUAY ELIZABETH MOROSI 2011 ORIENTADORA: DRA. GRACIELA PIÑEIRO TRIBUNAL: Dr. ERNESTO BLANCO Dr. MICHEL LAURIN Dr. MARTIN UBILLA 1 CONTENIDO RESUMEN Y ABSTRACT…………………………………………………… 4 Índice de figuras……………………………………………………… 8 Índice de tablas...…………………………………………………… 11 I - INTRODUCCION ....... …………………………………………………….. 13 1.1 – Los primeros estudios paleontológicos…………………….. 13 1.2 – Formaciones Permo-Carboníferas………………………….. 16 1.3 – Objetivos ... ……………………………………………………... 19 II – MATERIALES Y METODOS……………………………………….….. 20 2.1 – Materiales ... ………………………………………………….… 20 2.1.1 – Materiales estudiados………………………..……… 20 2.2 – Métodos ..... …………………………………….………………. 30 2.2.1 – Localidad relevada………………………………….. 30 2.2.2 – Colecta y preparación de materiales……………. 31 2.2.3 – Fotografía y diagramación………………………… 32 III – ANTECEDENTES de los MESOSAURIDAE………………………… 34 3.1 – Reseña histórica……………………………………………….. 34 3.2 – Descripción de los tres géneros de los Mesosauridae…….. 38 3.2.1 – Morfología básica……………………………………. 38 3.2.2 – Cráneo………………………………………………… 41 2 IV – DESCRIPCION ....... …………………………………………………….. 44 4.1 – Descripción cráneo FC-DPV 2061…………………………….. 44 4.1.1 – Descripción general……………………..…………… 44 4.1.2 – Cráneo: descripción anatómica……………………… 44 4.1.3 – Morfología dentaria…………………………………… 57 4.1.4 – Ventana temporal…………………………………….. 58 4.2 – Descripción cráneo FC-DPV 2534……………………………. 58 4.2.1 – Descripción general………………………………….. 58 4.2.2 – Cráneo: descripción anatómica…………………….. 58 4.2.3 – FC-DPV 2534 a (parte), vista dorsal………………… 59 4.2.3.1 – Fenestra temporal…………………………. 66 4.2.4 – FC-DPV 2534 b (contraparte), vista palatal……….. 68 4.3 – Descripción de FC-DPV 2636 y FC-DPV 2318……………… 74 V – TAFONOMIA. NUEVA CLASE TAFONOMICA……………….……. 78 5.1 – Antecedentes…………………………………………………… 78 5.1.1 – Tafonomía de los mesosáuridos…………………… 78 5.1.2 – Tafofacies de los mesosáuridos……………………. -
Fossil Crustacea Ranges and Localities
UvA-DARE (Digital Academic Repository) The fossil Crustacea of China: their taxonomy, palaeobiology, biogeography and phylogenetic relationships Taylor, R.S. Publication date 1999 Link to publication Citation for published version (APA): Taylor, R. S. (1999). The fossil Crustacea of China: their taxonomy, palaeobiology, biogeography and phylogenetic relationships. Fac. der Biologie. General rights It is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), other than for strictly personal, individual use, unless the work is under an open content license (like Creative Commons). Disclaimer/Complaints regulations If you believe that digital publication of certain material infringes any of your rights or (privacy) interests, please let the Library know, stating your reasons. In case of a legitimate complaint, the Library will make the material inaccessible and/or remove it from the website. Please Ask the Library: https://uba.uva.nl/en/contact, or a letter to: Library of the University of Amsterdam, Secretariat, Singel 425, 1012 WP Amsterdam, The Netherlands. You will be contacted as soon as possible. UvA-DARE is a service provided by the library of the University of Amsterdam (https://dare.uva.nl) Download date:25 Sep 2021 Fossil Crustacea: Ranges and Localities Appendix 2: Crustacea: Ranges and Localities: Class Phyllopoda Latreille, 1825 Subclass Phyllocarida Packard, 1879 (L. Cambrian - Recent) Order Leptostraca Claus, 1880: U. Permian - Recent F Nebaliidae Baird, 1850: U. Permian - Recent G Nebalia Leach, 1814 N. herbstii Leach, 1814 (Cancer bipes Farricus, 1780?): Recent, cosmopolitan (synonyms on R313) N. -
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Nauplius ORIGINAL ARTICLE Ontogenetic development captured in amber – the first record of aquatic representatives of Isopoda in Cretaceous e-ISSN 2358-2936 www.scielo.br/nau amber from Myanmar www.crustacea.org.br Mario Schädel1 orcid.org/0000-0001-7945-4205 Matúš Hyžný2 orcid.org/0000-0002-8960-2846 Joachim T. Haug1,3 orcid.org/0000-0001-8254-8472 1 Ludwig-Maximilians-Universität München, Department of Biology II, Zoomorphology group. Großhaderner Straße 2, 82152 Planegg-Martinsried, Germany. 2 Comenius University in Bratislava, Department of Geology and Paleontology. Mlynská dolina, Ilkovičova 6, 842 15 Bratislava, Slovakia. 3 Ludwig-Maximilians-Universität München, GeoBio-Center. Richard-Wagner-Str. 10, 80333 München, Germany. ZOOBANK: http://zoobank.org/urn:lsid:zoobank.org:pub:4817F86A-F0E9-41F8- B841-6B0A5ABE0221 ABSTRACT Two fossils from Burmese amber are the subject of this study. The specimens differ in size; yet, they appear to be conspecific because of the profound morphological similarity. The fossils are interpreted as representatives of Isopoda, more precisely of the group Cymothoida, due to the presence of a triangular basipod of the uropod. Cymothoida comprises parasitic forms of Isopoda as well as many other types of feeding-habits. The morphology in the studied fossils suggests that they are not representatives of any of the parasitic ingroups of Cymothoida. Since there are no other findings of Isopoda from the Cretaceous with the same morphological features, the fossils at hand are described as a new species – Electrolana madelineae sp. nov. The smaller specimen lacks well-developed walking appendages on trunk segment seven; it can thus be interpreted as a manca stage (immature) individual.