DOCSLIB.ORG

Muscles and Muscle Scars in Fossil Malacostracan Crustaceans T ⁎ Adiël A

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Muscles and Muscle Scars in Fossil Malacostracan Crustaceans T ⁎ Adiël A Earth-Science Reviews 194 (2019) 306–326 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Muscles and muscle scars in fossil malacostracan crustaceans T ⁎ Adiël A. Klompmakera,b,c, , Matúš Hyžnýd,e, Roger W. Portellb, Clément Jauvionf,g, Sylvain Charbonnierf, Shane S. Fussellc, Aaron T. Klierh, Raymond Tejerac, Sten L. Jakobseni a Department of Integrative Biology & Museum of Paleontology, University of California, Berkeley, 1005 Valley Life Sciences Building #3140, Berkeley, CA 94720, USA b Florida Museum of Natural History, University of Florida, 1659 Museum Road, Gainesville, FL 32611, USA c Department of Geological Sciences, University of Florida, 241 Williamson Hall, Gainesville, FL 32611, USA d Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University, Mlynská dolina G1, Ilkovičova 6, SVK-842 15 Bratislava, Slovakia e Geological-Paleontological Department, Natural History Museum Vienna, Burgring 7, 1010 Vienna, Austria f Muséum national d'Histoire naturelle, Centre de Recherche en Paléontologie - Paris (CR2P, UMR 7207), CNRS, Sorbonne Université, 57 rue Cuvier, F-75005 Paris, France g Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie, CNRS UMR 7590, Sorbonne Université, Muséum national d'Histoire naturelle, IRD UMR 206, 61 rue Buffon, F-75005 Paris, France h Department of Biology, University of Florida, 220 Bartram Hall, Gainesville, FL 32611, USA i Geomuseum Faxe, Østervej 2, DK-4640 Faxe, Denmark ARTICLE INFO ABSTRACT Keywords: Exceptionally preserved specimens yield critical information about the soft-part anatomy and the evolution of Crustacea organisms through time. We compiled the first global dataset of exceptionally preserved muscles in malacos- Decapoda tracans consisting of 47 occurrences, including 18 new records, predominantly preserved in Mesozoic Konservat- Exceptional preservation Lagerstätten (> 70% of occurrences). Early diagenetic mineralization through phosphatization is the dominant Lagerstätten process for exceptional preservation of muscles in malacostracans. Over 70% of taxon occurrences with muscles Malacostraca preserved are compressed. Rarer, three-dimensionally preserved specimens allow more detailed study of mus- Muscle cles. One example are specimens of the mid-Holocene ghost shrimp Sergio sp. from Panama, showing exquisitely preserved strings of muscle fibers attached to the shell interior, resembling the muscle arrangement ofmodern ghost shrimps. Other fossil malacostracans, including the oldest known fossil shrimp, also show musculature similar to modern taxa. We hypothesize that this muscle conservatism may be related to the confined space within the malacostracan shell in conjunction with the relatively stable body plan of several clades. We also assembled the first dataset on muscle attachment scars in malacostracans. Unlike muscles, muscle scars aremore common. Approximately 24% of the 357 articles analyzed yielded evidence of muscle scars, but such scars were only recognized for 19% of the 162 taxon occurrences that showed muscle scars. Muscle scars are common from the Late Jurassic onwards, are found primarily in Brachyura and Axiidea, and do not suffer from a Lagerstätten- effect. Rocks with well-preserved specimens should yield an additional wealth of information on thesoftpart anatomy of malacostracans. Similarly, muscle scars represent an almost untapped, complementary source of information on muscle evolution. 1. Introduction 1930; Feldmann and Schweitzer, 2010; Wilby and Briggs, 1997). The most diverse clade among malacostracans are the Decapoda, with a The preservation of soft tissues in fossils provides exceptional in- fossil record of ~3700 species (Schweitzer and Feldmann, 2016) and sight into the biology of ancient metazoans. Muscles have been used to major species- and genus-level diversifications from the Mesozoic on- infer the functioning of organisms, their taxonomic identity, and evo- wards (Klompmaker et al., 2013; Schweitzer and Feldmann, 2015; lutionary relationships among clades (e.g., Bergström et al., 1989; Kaji Sepkoski, 2000). Other, less diverse malacostracan clades with a mac- et al., 2018; Parry et al., 2015; Trinajstic et al., 2007; Young and rofossil record are Isopoda, Phyllocarida, and Hoplocarida. Muscles in Vinther, 2017). Muscles are preserved in a variety of arthropods (e.g., fossil malacostracans are almost exclusively mentioned as part of sys- Briggs et al., 2005; Hu et al., 2017; Siveter et al., 2010; Vannier et al., tematic descriptions thus far, but have the potential to provide insight 2014), including in multiple clades of Malacostraca (e.g., Beurlen, into the evolution of myoanatomy through time. ⁎ Corresponding author. E-mail address: [email protected] (A.A. Klompmaker). https://doi.org/10.1016/j.earscirev.2019.04.012 Received 21 December 2018; Received in revised form 8 April 2019; Accepted 8 April 2019 Available online 10 April 2019 0012-8252/ © 2019 Elsevier B.V. All rights reserved. A.A. Klompmaker, et al. Earth-Science Reviews 194 (2019) 306–326 Fig. 1. Thoracic/carapace muscles (A) and muscle scars (B) in the brachyuran decapod crustacean Dromia personata (Linnaeus, 1758). Modified from McLaughlin (1980: Fig. 53A) and redrawn from Glaessner (1969: Fig. 224). Muscle attachment traces or scars on the hard parts of fossil me- 2.1. Thoracic muscles tazoans can provide complementary information on many aspects of metazoan biology in deep time. Muscle scars have helped gain insight Thoracic muscles (Fig. 1) provide support for the animal body and into the evolution of digestive tracts, the function of skeletal elements, interconnect body parts such as the thorax and pleon. The thorax in the size of soft tissues, life habit, and the relatedness among organisms decapods is rather inflexible and contains mainly thoracopleonal mus- (e.g., Doguzhaeva and Mutvei, 1991; Dzik, 2010; Knight and Morris, cles, in addition to those connecting the internal with the external 2019; Kröger and Mutvei, 2005; Lerosey-Aubril and Peel, 2018; Richter skeleton (Glaessner, 1969). Nevertheless, the thoracic musculature is and Fischer, 2002; Topper and Skovsted, 2017). Such scars have been extraordinarily complex and the number of individual muscles is large found in fossil malacostracans (e.g., Glaessner, 1960; Hof and Schram, in lobsters and most anomurans, whereas the whole arrangement in 1998; Schweigert and Koppka, 2011), but, again, they are primarily brachyurous crabs is less complicated (Pilgrim, 1973). In hoplocar- mentioned as part of taxon descriptions. idans, the thorax is more flexible and contains also bundles of flexors Here we review muscles and muscle scars in fossil malacostracans to and extensors (Pilgrim, 1964). In decapods, various paired bundles of evaluate (1) muscle preservation through geologic time based on dorsal thoracic muscles are situated either between the inner side of the known and new occurrences, (2) how fossil muscles compare to those in carapace and the endophragmal skeleton or between elements of the extant representatives, (3) the taxa with muscle attachment scars and endophragmal skeleton (Keiler et al., 2016). The attachment areas of their location, and (4) the frequency and the degree of recognition of muscles are recognizable on the inner surface of the carapace muscle scars. (Glaessner, 1960, 1969). Institutional abbreviations. GBA: Geologische Bundesanstalt, In decapods, the most important groups of muscles attached to the Vienna, Austria; MAB: Oertijdmuseum, Boxtel, The Netherlands; carapace are the epimeral attractor muscle (muscle inserting along the MGUH: Natural History Museum of Denmark, Geological Museum, branchiocardiac groove that connects the epimeral wall of the ventral University of Copenhagen, Denmark; MNHN: Muséum national thorax to the dorsal carapace), mandibular muscles (operating mand- d'Histoire naturelle, Paris, France; NHMW: Department of Geology and ibles), gastric muscles (responsible for moving the gastric mill), and a Palaeontology, Natural History Museum Vienna, Austria; SMF: small portion of the thoraco-pleonal muscles (interconnecting thorax Forschungsinstitut Senckenberg, Frankfurt am Main, Germany; UF: with pleon). Ventral thoracic muscles are extrinsic muscles (flexors + Florida Museum of Natural History at the University of Florida, extensors) of the bases of appendages and are located directly above the Gainesville, USA; UMJGPA: Geological-palaeontological Department, sternum (Keiler et al., 2016). There is considerable variation in the Universalmuseum Joanneum, Graz, Austria. development of mandibular muscles. In lobsters, the posterior (ad- ductor) muscle is very strong and its area of attachment covers a large 2. Major muscle groups and muscle scars of extant malacostracans part of the lateral internal surface of the carapace. In squat lobsters and with a fossil record crab-like decapods, this muscle is very weak and the lateral adductor muscle occupies more space on its surface (Glaessner, 1960). Skeletal muscles coupled with the nervous system provide the ne- Of the external gastric muscles, only the group of the posterior cessary equipment for organisms to actively move. The neuromuscular muscles is attached to the carapace. It is connected with two small morphology in malacostracans is responsible for distinct ways of mo- calcareous projections of its apodemes close to the median line of the tion, including swimming, tail-flipping (e.g., escape response,
Load more

Recommended publications
  • A Classification of Living and Fossil Genera of Decapod Crustaceans
    RAFFLES BULLETIN OF ZOOLOGY 2009 Supplement No. 21: 1–109 Date of Publication: 15 Sep.2009 © National University of Singapore A CLASSIFICATION OF LIVING AND FOSSIL GENERA OF DECAPOD CRUSTACEANS Sammy De Grave1, N. Dean Pentcheff 2, Shane T. Ahyong3, Tin-Yam Chan4, Keith A. Crandall5, Peter C. Dworschak6, Darryl L. Felder7, Rodney M. Feldmann8, Charles H. J. M. Fransen9, Laura Y. D. Goulding1, Rafael Lemaitre10, Martyn E. Y. Low11, Joel W. Martin2, Peter K. L. Ng11, Carrie E. Schweitzer12, S. H. Tan11, Dale Tshudy13, Regina Wetzer2 1Oxford University Museum of Natural History, Parks Road, Oxford, OX1 3PW, United Kingdom [email protected] [email protected] 2Natural History Museum of Los Angeles County, 900 Exposition Blvd., Los Angeles, CA 90007 United States of America [email protected] [email protected] [email protected] 3Marine Biodiversity and Biosecurity, NIWA, Private Bag 14901, Kilbirnie Wellington, New Zealand [email protected] 4Institute of Marine Biology, National Taiwan Ocean University, Keelung 20224, Taiwan, Republic of China [email protected] 5Department of Biology and Monte L. Bean Life Science Museum, Brigham Young University, Provo, UT 84602 United States of America [email protected] 6Dritte Zoologische Abteilung, Naturhistorisches Museum, Wien, Austria [email protected] 7Department of Biology, University of Louisiana, Lafayette, LA 70504 United States of America [email protected] 8Department of Geology, Kent State University, Kent, OH 44242 United States of America [email protected] 9Nationaal Natuurhistorisch Museum, P. O. Box 9517, 2300 RA Leiden, The Netherlands [email protected] 10Invertebrate Zoology, Smithsonian Institution, National Museum of Natural History, 10th and Constitution Avenue, Washington, DC 20560 United States of America [email protected] 11Department of Biological Sciences, National University of Singapore, Science Drive 4, Singapore 117543 [email protected] [email protected] [email protected] 12Department of Geology, Kent State University Stark Campus, 6000 Frank Ave.
    [Show full text]
  • National Monitoring Program for Biodiversity and Non-Indigenous Species in Egypt
    UNITED NATIONS ENVIRONMENT PROGRAM MEDITERRANEAN ACTION PLAN REGIONAL ACTIVITY CENTRE FOR SPECIALLY PROTECTED AREAS National monitoring program for biodiversity and non-indigenous species in Egypt PROF. MOUSTAFA M. FOUDA April 2017 1 Study required and financed by: Regional Activity Centre for Specially Protected Areas Boulevard du Leader Yasser Arafat BP 337 1080 Tunis Cedex – Tunisie Responsible of the study: Mehdi Aissi, EcApMEDII Programme officer In charge of the study: Prof. Moustafa M. Fouda Mr. Mohamed Said Abdelwarith Mr. Mahmoud Fawzy Kamel Ministry of Environment, Egyptian Environmental Affairs Agency (EEAA) With the participation of: Name, qualification and original institution of all the participants in the study (field mission or participation of national institutions) 2 TABLE OF CONTENTS page Acknowledgements 4 Preamble 5 Chapter 1: Introduction 9 Chapter 2: Institutional and regulatory aspects 40 Chapter 3: Scientific Aspects 49 Chapter 4: Development of monitoring program 59 Chapter 5: Existing Monitoring Program in Egypt 91 1. Monitoring program for habitat mapping 103 2. Marine MAMMALS monitoring program 109 3. Marine Turtles Monitoring Program 115 4. Monitoring Program for Seabirds 118 5. Non-Indigenous Species Monitoring Program 123 Chapter 6: Implementation / Operational Plan 131 Selected References 133 Annexes 143 3 AKNOWLEGEMENTS We would like to thank RAC/ SPA and EU for providing financial and technical assistances to prepare this monitoring programme. The preparation of this programme was the result of several contacts and interviews with many stakeholders from Government, research institutions, NGOs and fishermen. The author would like to express thanks to all for their support. In addition; we would like to acknowledge all participants who attended the workshop and represented the following institutions: 1.
    [Show full text]
  • High Level Environmental Screening Study for Offshore Wind Farm Developments – Marine Habitats and Species Project
    High Level Environmental Screening Study for Offshore Wind Farm Developments – Marine Habitats and Species Project AEA Technology, Environment Contract: W/35/00632/00/00 For: The Department of Trade and Industry New & Renewable Energy Programme Report issued 30 August 2002 (Version with minor corrections 16 September 2002) Keith Hiscock, Harvey Tyler-Walters and Hugh Jones Reference: Hiscock, K., Tyler-Walters, H. & Jones, H. 2002. High Level Environmental Screening Study for Offshore Wind Farm Developments – Marine Habitats and Species Project. Report from the Marine Biological Association to The Department of Trade and Industry New & Renewable Energy Programme. (AEA Technology, Environment Contract: W/35/00632/00/00.) Correspondence: Dr. K. Hiscock, The Laboratory, Citadel Hill, Plymouth, PL1 2PB. [email protected] High level environmental screening study for offshore wind farm developments – marine habitats and species ii High level environmental screening study for offshore wind farm developments – marine habitats and species Title: High Level Environmental Screening Study for Offshore Wind Farm Developments – Marine Habitats and Species Project. Contract Report: W/35/00632/00/00. Client: Department of Trade and Industry (New & Renewable Energy Programme) Contract management: AEA Technology, Environment. Date of contract issue: 22/07/2002 Level of report issue: Final Confidentiality: Distribution at discretion of DTI before Consultation report published then no restriction. Distribution: Two copies and electronic file to DTI (Mr S. Payne, Offshore Renewables Planning). One copy to MBA library. Prepared by: Dr. K. Hiscock, Dr. H. Tyler-Walters & Hugh Jones Authorization: Project Director: Dr. Keith Hiscock Date: Signature: MBA Director: Prof. S. Hawkins Date: Signature: This report can be referred to as follows: Hiscock, K., Tyler-Walters, H.
    [Show full text]
  • Sedimentology, Taphonomy, and Palaeoecology of a Laminated
    Palaeogeography, Palaeoclimatology, Palaeoecology 243 (2007) 92–117 www.elsevier.com/locate/palaeo Sedimentology, taphonomy, and palaeoecology of a laminated plattenkalk from the Kimmeridgian of the northern Franconian Alb (southern Germany) ⁎ Franz Theodor Fürsich a, , Winfried Werner b, Simon Schneider b, Matthias Mäuser c a Institut für Paläontologie, Universität Würzburg, Pleicherwall 1, 97070 Würzburg, Germany LMU b Bayerische Staatssammlung für Paläontologie und Geologie and GeoBio-Center , Richard-Wagner-Str. 10, D-80333 München, Germany c Naturkunde-Museum Bamberg, Fleischstr. 2, D-96047 Bamberg, Germany Received 8 February 2006; received in revised form 3 July 2006; accepted 7 July 2006 Abstract At Wattendorf in the northern Franconian Alb, southern Germany, centimetre- to decimetre-thick packages of finely laminated limestones (plattenkalk) occur intercalated between well bedded graded grainstones and rudstones that blanket a relief produced by now dolomitized microbialite-sponge reefs. These beds reach their greatest thickness in depressions between topographic highs and thin towards, and finally disappear on, the crests. The early Late Kimmeridgian graded packstone–bindstone alternations represent the earliest plattenkalk occurrence in southern Germany. The undisturbed lamination of the sediment strongly points to oxygen-free conditions on the seafloor and within the sediment, inimical to higher forms of life. The plattenkalk contains a diverse biota of benthic and nektonic organisms. Excavation of a 13 cm thick plattenkalk unit across an area of 80 m2 produced 3500 fossils, which, with the exception of the bivalve Aulacomyella, exhibit a random stratigraphic distribution. Two-thirds of the individuals had a benthic mode of life attached to hard substrate. This seems to contradict the evidence of oxygen-free conditions on the sea floor, such as undisturbed lamination, presence of articulated skeletons, and preservation of soft parts.
    [Show full text]
  • Decapode.Pdf
    We are pleased and honored to welcome at the Paléospace Museum of Villers-sur-Mer the “6th Symposium on Mesozoic and Cenozoic Decapod Crustaceans”. Villers-sur-Mer is a place universally known by specialists and amateurs of palaeontology due to its famous Vaches Noires cliffs. Villers-sur-Mer has also the distinction of being the only French seaside resort located on the Greenwich Meridian line. The Paléospace is a Museum funded in 2011 with the label Musée de France. Three main animations linked to the Time are presented: palaeontology, astronomy and nature with the neighbouring marsh. The museum is in a constant evolution. For instance, an exhibition specially dedicated to dinosaurs was opened two years ago and a planetarium will open next summer. Every year a very high quality temporary exhibition takes place during the summer period with very numerous animations during all the year. The Paléospace does not stop progressing in term of visitors (56 868 in 2015) and its notoriety is universally recognized both by the other museums as by the scientific community. We are very proud of these unexpected results. We thank the dynamism and the professionalism of the Paléospace team which is at the origin of this very great success. We wish you a very good stay at Villers-sur-Mer, a beautiful visit of the Paléospace and especially an excellent congress. Jean-Paul Durand, Mayor and President of Paléospace MOT DU MAIRE DE VILLERS-SUR-MER Nous sommes très heureux et très honorés d’accueillir à Villers-sur-Mer, le « 6e Symposium on Mesozoic and Cenozoic Decapod Crustaceans » dans le cadre du Paléospace.
    [Show full text]
  • From the Upper Triassic (Norian) of Northern Carnic Pre-Alps (Udine, Northeastern Italy)
    GORTANIA. Geologia,GORTANIA Paleontologia, Paletnologia 35 (2013) Geologia, Paleontologia, Paletnologia 35 (2013) 11-18 Udine, 10.IX.2014 ISSN: 2038-0410 Alessandro Garassino ACANTHOCHIRANA TRIASSICA N. SP. Günter Schweigert Giuseppe Muscio AND ANTRIMPOS COLETTOI N. SP. (DECAPODA: AEGERIDAE, PENAEIDAE) FROM THE UPPER TRIASSIC (NORIAN) OF NORTHERN CARNIC PRE-ALPS (UDINE, NORTHEASTERN ITALY) Acanthochirana TRIASSICA N. SP. E AntrimPOS COLETTOI N. SP. (DECAPODA: AEGERIDAE, PENAEIDAE) DAL TRIASSICO SUPERIORE (NORICO) DELLA PREALPI CARNICHE SETTENTRIONALI (UDINE, ITALIA NORDORIENTALE) Riassunto breve - I crostacei decapodi del Triassico superiore (Norico) della Dolomia di Forni sono stati descritti da Ga- rassino et al. (1996). La recente scoperta di un piccolo campione, rivenuto nella Valle del Rio Seazza e in quella del Rio Rovadia, ha permesso un aggiornamento relativo ai crostacei decapodi delle Prealpi Carniche. Gli esemplari studiati sono stati assegnati a Acanthochirana triassica n. sp. (Aegeridae Burkenroad, 1963) e Antrimpos colettoi n. sp. (Penaeidae Rafinesque, 1815). Acanthochirana triassica n. sp. estende il range stratigrafico di questo genere nel Triassico superiore, mentre Antrimpos colettoi n. sp. rappresenta la seconda specie di questo genere segnalata nel Triassico superiore d’Italia. La scoperta di queste due nuove specie incrementa il numero delle specie di peneidi conosciuti nel Norico dell’alta Val Ta- gliamento (Prealpi Carniche settentrionali). Parole chiave: Crustacea, Decapoda, Aegeridae, Penaeidae, Triassico superiore, Prealpi Carniche. Abstract - The decapod crustaceans from the Upper Triassic (Norian) of the Dolomia di Forni Formation were reported by Garassino et al. (1996). The recent discovery of a small sample from this Formation between Seazza and Rovadia brooks allowed updating the decapod assemblages from the Norian of Carnic Pre-Alps.
    [Show full text]
  • First Record of Dromia Neogenica Müller, 1979 (Decapoda, Brachyura, Dromiidae) from Neogene Strata in the Southern North Sea Basin
    FIRST RECORD OF DROMIA NEOGENICA MÜLLER, 1979 (DECAPODA, BRACHYURA, DROMIIDAE) FROM NEOGENE STRATA IN THE SOUTHERN NORTH SEA BASIN BY RENÉ H.B. FRAAIJE1,4), BARRY W.M. VAN BAKEL1,2,5) and JOHN W.M. JAGT3,6) 1) Oertijdmuseum De Groene Poort, Bosscheweg 80, NL-5283 Boxtel, The Netherlands 2) Nederlands Centrum voor Biodiversiteit (Naturalis), P.O. Box 9517, NL-2300 RA Leiden, The Netherlands 3) Natuurhistorisch Museum Maastricht, de Bosquetplein 6-7, NL-6211 KJ Maastricht, The Netherlands ABSTRACT The sponge crab Dromia neogenica Müller, 1979 (Dromiidae) is recorded for the first time from strata of Neogene (late Miocene-early Pliocene) age in the southern North Sea Basin, on the basis of two concretion-preserved carapaces from Bemmel (north of Nijmegen, province of Gelderland, The Netherlands). The presence of this species, which was previously known from the middle-upper Miocene of Hungary and Algeria, suggests relatively higher seawater temperatures in the North Sea during the late Miocene-early Pliocene. Morphological differences (extraorbital and anterolateral teeth, development of cervical and branchiocardiac grooves) between D. neogenica and extant D. personata (Linnaeus, 1758) are relatively minor. This observation, coupled with the absence of the former species in mid-Pliocene and younger strata, and with the robust record of the latter in the mid-Pliocene to upper Pleistocene of Italy, would indicate that D. neogenica and D. personata are closely related, and probably represent the same lineage. RÉSUMÉ La dromie éponge Dromia neogenica Müller, 1979 (Dromiidae) est signalée pour la premiére fois dans les strates du Néogène (fin du Miocène-début du Pliocène) du sud du bassin de la mer du Nord.
    [Show full text]
  • An Exceptionally Preserved Arthropod Cardiovascular System from the Early Cambrian
    ARTICLE Received 20 Dec 2013 | Accepted 4 Mar 2014 | Published 7 Apr 2014 DOI: 10.1038/ncomms4560 An exceptionally preserved arthropod cardiovascular system from the early Cambrian Xiaoya Ma1,2, Peiyun Cong1, Xianguang Hou1, Gregory D. Edgecombe2 & Nicholas J. Strausfeld3 The assumption that amongst internal organs of early arthropods only the digestive system withstands fossilization is challenged by the identification of brain and ganglia in early Cambrian fuxianhuiids and megacheirans from southwest China. Here we document in the 520-million-year-old Chengjiang arthropod Fuxianhuia protensa an exceptionally preserved bilaterally symmetrical organ system corresponding to the vascular system of extant arthropods. Preserved primarily as carbon, this system includes a broad dorsal vessel extending through the thorax to the brain where anastomosing branches overlap brain seg- ments and supply the eyes and antennae. The dorsal vessel provides segmentally paired branches to lateral vessels, an arthropod ground pattern character, and extends into the anterior part of the abdomen. The addition of its vascular system to documented digestive and nervous systems resolves the internal organization of F. protensa as the most completely understood of any Cambrian arthropod, emphasizing complexity that had evolved by the early Cambrian. 1 Yunnan Key Laboratory for Palaeobiology, Yunnan University, Kunming 650091, China. 2 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK. 3 Department of Neuroscience and Center for Insect Science, University of Arizona, Tucson, Arizona 85721, USA. Correspondence and requests for materials should be addressed to X.H. (email: [email protected]) or to N.J.S. (email: fl[email protected]).
    [Show full text]
  • Decapod Crustaceans from the Middle Jurassic Opalinus Clay of Northern Switzerland, with Comments on Crustacean Taphonomy
    0012-9402/04/030381-12 Eclogae geol. Helv. 97 (2004) 381–392 DOI 10.1007/s00015-004-1137-2 Birkhäuser Verlag, Basel, 2004 Decapod crustaceans from the Middle Jurassic Opalinus Clay of northern Switzerland, with comments on crustacean taphonomy WALTER ETTER Key words: Decapoda, Peracarida, Jurassic, Switzerland, ecology, crustacean taphonomy ABSTRACT ZUSAMMENFASSUNG Four species of decapod crustaceans from the Middle Jurassic Opalinus Clay Aus dem Opalinuston (Mittlerer Jura, Aalenian) der Nordschweiz werden vier (Aalenian) of Northern Switzerland are described. Of these, Mecochirus cf. Arten von decapoden Krebsen beschrieben. Von Aeger sp., Eryma cf. bedelta eckerti is the most common one, while Eryma cf. bedelta, Glyphea sp. and und Glyphaea sp. wurden nur ganz wenige Exemplaren gefunden, während Aeger sp. were present as individuals, or only a few specimens. The preserva- Mecochirus cf. eckerti etwas häufiger ist. Die Erhaltungsbedingungen waren tion of these crustaceans ranges from moderate to excellent, reflecting the während der Ablagerung des Opalinustones günstig, was sich in einer geringen favourable taphonomic conditions of the depositional environment. An inter- Disartikulations- und Fragmentationsrate der Krebse widerspiegelt. Ein in- esting aspect of the taphocoenosis in the Opalinus Clay is that the decapod teressanter Aspekt der Taphocoenose ist die deutliche Dominanz der Klein- crustaceans are by far outnumbered by small peracarid crustaceans (isopods krebse (Peracarida: Isopoden und Tanaidaceen). Dies dürfte die Zahlenver- and tanaids). This is interpreted as reflecting the original differences in abun- hältnisse der ehemaligen Lebensgemeinschaft widerspiegeln. In den meisten dance. Yet this distribution is not frequently encountered in sedimentary se- Ablagerungen dominieren jedoch die decapoden Krebse, wogegen Peracarida quences where decapods (although rare) are far more common than isopods äusserst selten sind.
    [Show full text]
  • Rediscovery of the Type Material of Eryon Cuvieri Desmarest, 1817 (Crustacea, Decapoda, Eryonidae) and Nomenclatural Consequences
    Rediscovery of the type material of Eryon cuvieri Desmarest, 1817 (Crustacea, Decapoda, Eryonidae) and nomenclatural consequences Sylvain CHARBONNIER Muséum national d’Histoire naturelle, Département Histoire de la Terre, UMR 7207 CNRS, Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements, case postale 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France) [email protected] Alessandro GARASSINO Museo di Storia Naturale di Milano, Sezione di Paleontologia, Corso Venezia 55, I-20121 Milano (Italy) [email protected] Jean-Michel PACAUD Muséum national d’Histoire naturelle, Département Histoire de la Terre, UMR 7207 CNRS, Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements, case postale 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France) [email protected] Günter SCHWEIGERT Staatliches Museum für Naturkunde, Rosenstein 1, D-70911 Stuttgart (Germany) [email protected] Charbonnier S., Garassino A., Pacaud J.-M. & Schweigert G. 2012. — Rediscovery of the type material of Eryon cuvieri Desmarest, 1817 (Crustacea, Decapoda, Eryonidae) and nomen- clatural consequences. Geodiversitas 34 (4): 849-855. http://dx.doi.org/10.5252/g2012n4a7 ABSTRACT In 1817, Desmarest erected Eryon cuvieri, a new crustacean from the Late Jurassic of Bavaria (southern Germany). Later, the same taxon was described as Macrourites arctiformis by von Schlotheim (1820). Subsequently, numerous authors, probably KEY WORDS unaware of Desmarest’s first paper, referred to this taxon as Eryon arctiformis (von Crustacea, Schlotheim, 1820). Following the Principle of Priority, the original name must be Decapoda, Eryonidae, used and Macrourites arctiformis von Schlotheim, 1820 is here considered to be a Eryon, more recent, subjective synonym. Moreover, two specimens of the type series of Lectotype, Eryon cuvieri Desmarest, 1817, from Faujas de Saint-Fond’s Cabinet of Natural Jurassic, Germany, History, have recently been traced in the Collection de Géologie of the Muséum Solnhofen.
    [Show full text]
  • Fossil Crustacea Atlantic and Gulf Coastal Plain
    LIBRARY VJUSHMAN LABORATORY GE0WG1UAL UOVlkilk Ot AMERICA SPECIAL PAPERS NUMBER 2 FOSSIL CRUSTACEA OF THE ATLANTIC AND GULF COASTAL PLAIN BY MARY J. RATHBUN INVERTEBRATE \ ZOOLOGY % jDrustacea C | B R ft R-Y Wmi V CftUSTAOE* V PUBLISHED BY THE SOCIETY 14)35 COUNCIL, 1935 President: NEVIN M. FENNEMAN, Cincinnati, Ohio Past President: W. EL COLLINS, Ottawa, Canada Vice-Presidents: EDSON S. BASTIN, Chicago, 111. JOHN B. REESIDE, JR., Washington, D. C. DONNEL F. HEWETT, Washington, D. C. AUSTIN F. ROGERS, Stanford University, Cal. Secretary: CHARLES P. BERKEY, 419 W. 117th Street, New York, N. Y. Treasurer: EDWARD B. MATHEWS, Johns Hopkins University, Baltimore, Md. Councilors: (Term expires 1935) FRANK F. GROUT, Minneapolis, Minn. W. 0. HOTCHKISS, Houghton, Mich. JOSEPH STANLEY-BROWN, Kew Gardens, N. Y. (Term expires 1936) F. W. DEWOLF, Urbana, 111. D. H. MCLAUGHLIN, Cambridge, Mass. ADOLPH KNOPF, New Haven, Conn. (Term expires 1937) WALTER H. BUCHER, Cincinnati, Ohio RUSSELL S. KNAPPEN, Tulsa, Okla. E. L. BRUCE, Kingston, Ont., Canada GEOLOGICAL SOCIETY OF AMERICA SPECIAL PAPERS NUMBER 2 FOSSIL CRUSTACEA OF THE ATLANTIC AND GULF COASTAL PLAIN BY MARY J. RATHBUN L I B R a R Y pep^ Of O^UcTtkUEA ilDBRAT L ZOOLOGY Crustacea PUBLISHED BY THE SOCIETY 1935 WAVERLY PRESS, INC. BALTIMORE, MD. The Special Papers of The Geological Society of America are made possible through the bequest of Richard Alexander Fullerton Penrose, Jr. CONTENTS INTRODUCTION Statement of the Problem Sources of Material Unusual Extensions of Range Mingling of Cretaceous with Eocene Correlation with European Forms New Additions LIST OF SPECIES AND DISTRIBUTION DETAILED DESCRIPTION OF GENERA AND SPECIES.
    [Show full text]
  • (Marmara Sea) and Ecological Characteristics of Their Habitats
    RESEARCH ARTICLE Eur J Biol 2017; 76(1): 20-5 Decapod Crustaceans in the Marmara Island (Marmara Sea) and Ecological Characteristics of Their Habitats Begum Ayfer, Husamettin Balkis, Aysegul Mulayim* Istanbul University, Faculty of Science, Department of Biology, Istanbul, Turkey Please cite this article as: Ayfer B, Balkis H, Mulayim A. Decapod Crustaceans in the Marmara Island (Marmara Sea) and Ecological Characteristics of Their Habitats. Eur J Biol 2017; 76(1): 20-5. ABSTRACT We have performed series of analyses to identify decapod crustaceans inhabiting the littoral zone of the Marmara Island and to study specific ecological characteristics of the habitat. Samples of decapod crustaceans species were collected from 12 stations (6 onshore, 6 offshore) on May 12-17, 2008 and November 17-22, 2008. A total of 17 species and 1199 specimens of decapod crustaceans were recorded. Eigth species (A. lacazei, N. norvegicus, P. bluteli, P. longimana, P. platycheles, D. pugilator, D. personata and L. vernalis) have been reported in the littoral zone of Marmara Island for the first time in this study. Also our study also sheds light on some ecological properties (temperature, salinity, dissolved oxygen) of the habitats of the species from the littoral zone of the Marmara Island. Keywords: Ecology, decapoda, crustacea, Marmara Island, The Sea of Marmara INTRODUCTION The first study at the island was carried out by Ostrou- moff (3,4) followed by studies by Okuş (5), Yüksek (6) The Archipelago in the Sea of Marmara consisting of and Balkıs (7). small and large islands located southwest of the Sea of Marmara and the northwest of the Kapıdağ Peninsula MATERIALS AND METHODS are referred to as the Islands of Marmara.
    [Show full text]