The Genus Furo (Pisces, Halecomorphi) from the Upper Jurassic Plattenkalke of Germany

Total Page:16

File Type:pdf, Size:1020Kb

The Genus Furo (Pisces, Halecomorphi) from the Upper Jurassic Plattenkalke of Germany ORYCTOS,Vol. 1 :23-35,Octobre 1998 THEGENUS FURO (PISCES, HALECOMORPHI) FROMTHE UPPERJURASSIC PLATTENKALKE OF GERMANY Paul H. LAMBERS PaleontologischeWerkkamer, Biologisch Centrum RUG, Postbus 14,9750 AA Haren, the Netherlands. e-mail: phlambers@ biol.rug.nl Abstract : An overview of the speciesassigned to the genus Furo fowd in the German lithographic limestones of the Solnhofen-area(Bavaria) and Nusplingen (Baden-Wiirttemberg) is presentedand the monophyly of the Upper JurassicFuro is discussed.Six speciescan be recognized: 'F.' latim.anus,'F.' longiserratus, 'F.' microlepidotes, 'E' aldingeri, 'F.' angustus and'F.' miinsteri. Among these 'E' angustus and'F.' miinsteri form a monophyletic group, to which 'F.' aldingeri might be related as well. 'F.' longiserrarus might be closely related to the Ophiopsidae,whereas 'E' microlepidotes shows similarities with the Caturidae. The position of 'F.' latimanus remains to be determined. There are no indications of a monophyletic genusof Furo and the relationshipsof the Upper Jurassicfurids with the Lower Jurassicspecies of Furo remain to be examined. Key words: Eugnathus, Furo, Halecomorphi, phylogeny, Plattenknlke, Tithonian Le genreFuro (Pisces,Halecomorphi) du Jurassiquesupérieur d'Allemagne. Résumé : Les différentes espècesdu genre Furo enprovenancedes gisementsallemands à calcaireslithographiques des régions de Solnhofen (Bavière) et de Nusplingen (Bade-Wiirttemberg)sont présentéeset la monophylie du genre Furo du Jurassiquesupérieur est discutée.Six espècespeuvent être reconnues: '.8' Iatimanus, 'E longiserrattts, 'F.' microlepidotes,'F.'aldingeri, 'F.'angustuset 'F.'miinsteri.Parmi ces espèces,'F.' angustus et 'E'milnsteri consti- tuent un groupe monophylétique, auquel pourrait être rattaché 'E'aldingeri. 'F.'longiserratus se rapprocherait des Ophiopsidae et 'F.'microlepidotes montre des ressemblancesavec les Caturidae.La position de 'E' latimanus reste à être déterminée.Il n'existe aucuneindication sur la monophylie du genre Furo et les relations entre les furidés du Jurassiquesupérieur avec les espècesdu genre Furo du Jurassiqueinférieur doivent être étudiées. (traduit par la rédaction). Mots clés: Eugnathus,Furo, Halecomorphi, phylogénie, Plattenkalke, Tithonien INTRODUCTION England. The knowledge of the genus is mainly based on original descriptions from the 19th century The fossil fish genus Furo ( - Eugnathus,this and Woodwards Catalog of Fossil Fishes (1895a). F. name was preoccupiedby a genusof Coleoptera)is normandica, from the Toarcian of Normandy, des- known from the UpperTriassic of Lomb ardia(F. her- cribed by Wenz (1968), is the best known species. mesi, F. trottii. Alessandri,, 1910), severalspecies The monophyly of the genus has never been tested from the Lower Jurassic of England and France and it is therefore unknown whether all species assi- (Woodward, 1895a, b; Arambourg, 1935; Wenz, gned to Furo belong to this genus.The oldest known 1968)and the UpperJurassic of Cerin,France (Saint- representatives were originally described as belon- Seine,1949) and southernGermany. The type species ging to the genera Semionotus and Lepidotes and is F. orthostomus from the Lower Jurassic of referred to Furo by Allessandri (1910). 23 ORYCTOS,Vol. 1, 1998 I csgr q.n.d/^ Figure I a. Holotype of Furo longiserratus,specimen in the BayerischeStaatssammlung ftr Palâontologieund historischeGeologie, AS.Vil. I 136,Kelheim, Bavaria. b. Holotype of Furo latimanus,specimen in the BayerischeStaatssammlung ftir Palâontologieund historischeGeologie, AS.VII.262. Solnhofen.Bavaria. c. Holotype of Furo microlepidotes,specimen in the BayerischeStaatssammlung fùr Palâontologie und historischeGeologie, AS.V. I 1a,Eichstâtt, Bavaria. 24 LAMBERS- THEGENUS FURO In the Upper Jurassiclithographic limestonesof to group the Upper JurassicFuro into a monophyle- Bavaria and Nusplingen in Germany and Cerin, tic assemblagetogether with the Lower Jurassictype France,the following speciesof Furo havebeen des- species,all Upper Jurassicforms will be designated cribed (following the definition of Furo by 'Fu,ro'. Woodward, 1895 a): Furo aldingeri (Nusplingen; Heimberg, 1949), Furo vetteri (Bavaria?, Nusplingen; Heineke, 1906) Furo longimanus ?URO'LONGISERRATUS (B avaria),F uro longi se rratus (Bavaria,Nusplingen), Furo microlepidotus(Bavaria, Nusplingen) andFuro 'Furo' longiserratzs(Agassiz) (Figs. la,2) praelongus (Cerin, see Saint-Seine, 1949). 1843Pholidophorus longiserratus Agassiz, vol. II, Woodward (1895a) thought that Pholidophorus pt. I, p. 277, p1.38,fig. 2 (1843)(in 1833-1843) angustus, Pholidophorus elongatus and 1863Pholidophorus longiserratu,s, Wagner, p.664 Pholidophorus miinsterl belonged to Furo as well. 1863Pholidophorus brevivelis,rù/agner, p.664 Zittel (1887) placed Furo longisercatus,Furo longi- 1887Isopholis longiserratus,Zittel, p.216 manus and Furo miinsteri in a separate genus 1887Isopholis brevivelis,Zittel, p.216 Isopholis. He also included Pholidophorusbrevivelis 1895aEugnathus longiserratus (Agassiz), describedby Wagner(1863) in this genus. \iloodward,p. 301 ?19 14 Eugnathus lon gise rcatus (Agassiz),Eastman, The purposeof this paperis to give a short over- p. 410,pl. LXN, figs. 1, 2 view of the speciesof Furo from the GermanUpper 1949Eugnathus longiserratus Agassiz, Heimberg, Jurassiclocalities, to discusssome salient anatomical p. 97, pl. VIII, fig. 2 featuresand their implications on the phylogeny of 1966Eugnathus longiserratus (Agassiz), Schultze, Furo. A more detaileddescription of the speciesand fig. 19b an elaboratephylogenetic discussion will be publi- 1994Furo longimanus,Frickhinger, p.206,frg.434 shedin the future. As it appearsthat it is not possible - Figure 2 Skull of Furo longiserratus,lateral P+Dpt view. specimenin the Jura-Museum,SOS 3123. I Tithonianof Zandt.Bavaria. I sop Sor lo N lop Ao Mtp ec San F o Pm Ang Den mc G 25 ORYCTOS.Vol. 1. 1998 Holotype : Specimen AS.VII.I 136, Bayerische margin is embayed or only slightly notched, with a Staatssammlung fiir Palâontologie und historische small posterior process ventrally. The shape of the Geologie. Kelheim, Bavaria. maxilla is similar to that of primitive halecomorphs 'Fttro' longiserratus was originally described as a such as Brachyichthys (Woodward, 1895a), Conodus pholidophorid. This species was classified with the (pers. obs., a.o. specimen P.3645 in the NHM, poorly defined genus Isopholis by Zittel (1887). London), Heterolepidotes (pers. obs., a.o. specimen 'Furo' longiserratus is a slender, fusifoffn fish, P.2008in the NHM, London), Ionoscopus (pers. obs., with elongate head, pointed snout, high back, rather a.o. specimen 1903.I.64 in the Bayerische long dorsal fin placed posteriorly to halfway the body Staatssammlung fiir Palâontologie und historische length, narrow caudal peduncle, deeply forked caudal Geologie), Ophiopsis (Bartrâffi, I9l5), Teoichtlrys fin, the ventral rim forming almost a straight line (Applegate, 1988), Macrepistius (Schaeffer, 1960) from the anterior trunk to the posterior end of the and Lower Jurassic Furo (Woodward, 1895a; V/efz, lower lobe of the caudal fin and a scale-coverconsis- 1968).Most conspicuousis the presenceof a sensory ting of rhombic scales with serrated posterior mar- canal that runs through the maxilla. This is so far only gins, but in the throat region the scales are circular. known in the ophiopsids Ophiopsis and Teoichthys Most specimensmeasure between 10 and 15 cm stan- (Bartrâffi, I975; Applegate, 1988). The supramaxilla dard length, but the largest specimen that probably is half-oval. There areat least 14 branchiostegalrays. belongs to this specieshas a standardlength of 29 cm (specimen SOS.2I78a/b in the Jura-Museum, Eichstâtt). ,FURO'LATIMANUS The skull anatomy is of the general halecomorph type, with large first infraorbital, a single infraorbital 'Furo'latimanus (Agassiz) (Figs. lb, 3) behind the orbit, a broad, plate-like maxilla, with straight dentigerous border and which is expanded 1838-1843 Pholidophorus latimanus Agassiz, vol. dorsally in its posterior part with the dorsal margin II, pt I, 280(1843), pl. 43 (1838),(in 1833-1843) directed obliquely ventro-dorsally. The posterior 1863Pholidophorus latimanus, Wagner, p. 665 Figure 3 N Prn lol Skull of Furo latimanus, dorsalview, specimenin the Jura-Museum,SOS 2814. l.ryrI ..\. Tithonian t::::,, of Dollnstein. 'i! . '-.II:. Enp t-, \\ Bavaria. :r,!. \t I .:i'iJj . ' \l I Sm i I Enp I Ang \t So tl _- soc 'i O Sor Sy Pop /l Hyo r I ( ll 26 LAMBERS - THE GENUS FURO 1881 Pholidophorus latimanus, Vetter, p. 58 the short, weekly forked caudal fin are unique for this 1887 Pholidophorus latimanus, Zittel, p.216 form. 1895a Eugnathus latimanlts, Agassiz, Woodward, p. 302 ,FURO' 1966 Eugnathus latimanus (Agassiz), Schultze, fig. MICROLEPIDOTES 26 1994 Furo vetteri, Frickhinger, p. 206, fig. 435 'Furo'microlepidotes (Agassiz) (Figs. lc, 4,,5) Holotype: Specimen AS.VII .262, Bayerische 1833Uraeus microlepidotes, Agassiz, vol II, pt. I, p. Staatssammlung fiir Palâontologie und historische 12 (in 1833-1843) Geologie. Solnhofen, Bavaria. 1839-1843 Eugnathusmicrolepidotes, Agassiz, vol. IV p. 118 (1839),vol. II, pt. II, p. I04, (1843),(in 'Furo' latimanus was originally described as a 1833-1843) pholidophorid. It is a small (standard length up to 10 1863Eugnathus microlepidotes, Wagner, p. 673 cm) fish, with a round dorsal profile, a short skull 1895a Eugnathus microlepidotes, Agassiz, with a rounded or blunt snout, a triangular dorsal fin Woodward,p. 300 situated posteriorly to halfway the body-length, 1906Eugnathus
Recommended publications
  • Cryptoclidid Plesiosaurs (Sauropterygia, Plesiosauria) from the Upper Jurassic of the Atacama Desert
    Journal of Vertebrate Paleontology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/ujvp20 Cryptoclidid plesiosaurs (Sauropterygia, Plesiosauria) from the Upper Jurassic of the Atacama Desert Rodrigo A. Otero , Jhonatan Alarcón-Muñoz , Sergio Soto-Acuña , Jennyfer Rojas , Osvaldo Rojas & Héctor Ortíz To cite this article: Rodrigo A. Otero , Jhonatan Alarcón-Muñoz , Sergio Soto-Acuña , Jennyfer Rojas , Osvaldo Rojas & Héctor Ortíz (2020): Cryptoclidid plesiosaurs (Sauropterygia, Plesiosauria) from the Upper Jurassic of the Atacama Desert, Journal of Vertebrate Paleontology, DOI: 10.1080/02724634.2020.1764573 To link to this article: https://doi.org/10.1080/02724634.2020.1764573 View supplementary material Published online: 17 Jul 2020. Submit your article to this journal Article views: 153 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ujvp20 Journal of Vertebrate Paleontology e1764573 (14 pages) © by the Society of Vertebrate Paleontology DOI: 10.1080/02724634.2020.1764573 ARTICLE CRYPTOCLIDID PLESIOSAURS (SAUROPTERYGIA, PLESIOSAURIA) FROM THE UPPER JURASSIC OF THE ATACAMA DESERT RODRIGO A. OTERO,*,1,2,3 JHONATAN ALARCÓN-MUÑOZ,1 SERGIO SOTO-ACUÑA,1 JENNYFER ROJAS,3 OSVALDO ROJAS,3 and HÉCTOR ORTÍZ4 1Red Paleontológica Universidad de Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Santiago, Chile, [email protected]; 2Consultora Paleosuchus Ltda., Huelén 165, Oficina C, Providencia, Santiago, Chile; 3Museo de Historia Natural y Cultural del Desierto de Atacama. Interior Parque El Loa s/n, Calama, Región de Antofagasta, Chile; 4Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Barrio Universitario, Concepción, Región del Bío Bío, Chile ABSTRACT—This study presents the first plesiosaurs recovered from the Jurassic of the Atacama Desert that are informative at the genus level.
    [Show full text]
  • From the Crato Formation (Lower Cretaceous)
    ORYCTOS.Vol. 3 : 3 - 8. Décembre2000 FIRSTRECORD OT CALAMOPLEU RUS (ACTINOPTERYGII:HALECOMORPHI: AMIIDAE) FROMTHE CRATO FORMATION (LOWER CRETACEOUS) OF NORTH-EAST BRAZTL David M. MARTILL' and Paulo M. BRITO'z 'School of Earth, Environmentaland PhysicalSciences, University of Portsmouth,Portsmouth, POl 3QL UK. 2Departmentode Biologia Animal e Vegetal,Universidade do Estadode Rio de Janeiro, rua SâoFrancisco Xavier 524. Rio de Janeiro.Brazll. Abstract : A partial skeleton representsthe first occurrenceof the amiid (Actinopterygii: Halecomorphi: Amiidae) Calamopleurus from the Nova Olinda Member of the Crato Formation (Aptian) of north east Brazil. The new spe- cimen is further evidencethat the Crato Formation ichthyofauna is similar to that of the slightly younger Romualdo Member of the Santana Formation of the same sedimentary basin. The extended temporal range, ?Aptian to ?Cenomanian,for this genus rules out its usefulnessas a biostratigraphic indicator for the Araripe Basin. Key words: Amiidae, Calamopleurus,Early Cretaceous,Brazil Première mention de Calamopleurus (Actinopterygii: Halecomorphi: Amiidae) dans la Formation Crato (Crétacé inférieur), nord est du Brésil Résumé : la première mention dans le Membre Nova Olinda de la Formation Crato (Aptien ; nord-est du Brésil) de I'amiidé (Actinopterygii: Halecomorphi: Amiidae) Calamopleurus est basée sur la découverted'un squelettepar- tiel. Le nouveau spécimen est un élément supplémentaireindiquant que I'ichtyofaune de la Formation Crato est similaire à celle du Membre Romualdo de la Formation Santana, située dans le même bassin sédimentaire. L'extension temporelle de ce genre (?Aptien à ?Cénomanien)ne permet pas de le considérer comme un indicateur biostratigraphiquepour le bassin de l'Araripe. Mots clés : Amiidae, Calamopleurus, Crétacé inférieu4 Brésil INTRODUCTION Araripina and at Mina Pedra Branca, near Nova Olinda where cf.
    [Show full text]
  • 35-51 New Data on Pleuropholis Decastroi (Teleostei, Pleuropholidae)
    Geo-Eco-Trop., 2019, 43, 1 : 35-51 New data on Pleuropholis decastroi (Teleostei, Pleuropholidae), a “pholidophoriform” fish from the Lower Cretaceous of the Eurafrican Mesogea Nouvelles données sur Pleuropholis decastroi (Teleostei, Pleuropholidae), un poisson “pholidophoriforme” du Crétacé inférieur de la Mésogée eurafricaine Louis TAVERNE 1 & Luigi CAPASSO 2 Résumé: Le crâne et le corps de Pleuropholis decastroi, un poisson fossile de l’Albien (Crétacé inférieur) du sud de l’Italie, sont redécrits en détails. P. decastroi diffère des autres espèces du genre par ses deux nasaux en contact médian et qui séparent complètement le dermethmoïde ( = rostral) des frontaux. Avec son maxillaire extrêmement élargi qui couvre la mâchoire inférieure et son supramaxillaire fortement réduit, P. decastroi semble plus nettement apparenté avec Pleuropholis cisnerosorum, du Jurassique supérieur du Mexique, qu’avec les autres espèces du genre. Par ses mâchoires raccourcies et ses nombreux os orbitaires, Pleuropholis apparaît également comme le genre le plus spécialisé de la famille. La position systématique des Pleuropholidae au sein du groupe des « pholidophoriformes » est discutée. Mots-clés: Pleuropholis decastroi, Albien, Italie du sud, Pleuropholis, Pleuropholidae, “Pholidophoriformes”, ostéologie, position systématique. Abstract: The skull and the body of Pleuropholis decastroi, a fossil fish from the marine Albian (Lower Cretaceous) of southern Italy, are re-described in details. P. decastroi differs from the other species of the genus by their two nasals that are in contact along the mid-line, completely separating the dermethmoid (= rostral) from the frontals. With its extremely broadened maxilla that covers the lower jaw and its strongly reduced supramaxilla, P. decastroi seems more closely related to Pleuropholis cisnerosorum, from the Upper Jurassic of Mexico, than to the other species of the genus.
    [Show full text]
  • The Scales of Mesozoic Actinopterygians
    Mesozoic Fishes – Systematics and Paleoecology, G. Arratia & G. Viohl (eds.): pp. 83-93, 6 figs. © 1996 by Verlag Dr. Friedrich Pfeil, München, Germany – ISBN 3-923871–90-2 The scales of Mesozoic actinopterygians Hans-Peter SCHULTZE Abstract Cycloid scales (elasmoid scales with circuli) are a unique character of teleosts above the level of Pholidophorus and Pholidophoroides. Cycloid scales have two layers. A bony layer, usually acellular, is superimposed on a basal plate composed of partially mineralized layers of plywoodlike laminated collagen fibres. The tissue of the basal layer is refered to here as elasmodin. Basal teleosts (sensu PATTERSON 1973) possess rhombic scales with a bony base overlain by ganoin (lepidosteoid ganoid scale). Amioid scales (elasmoid scales with longitudinally to radially arranged ridges or rods on the overlapped field) are found within halecomorphs. This scale type evolved more than once within primitive actinopterygians and other osteichthyan fishes. It may have even developed twice within halecomorphs, in Caturidae and Amiidae, from rhombic scales of lepidosteoid type. Some basal genera of halecomorphs show remains of a dentine layer between ganoin and bone that is characteristic of actinopterygians below the halecostome level. The Semionotidae placed at the base of the Halecostomi, exhibit scale histology transitional between the palaeoniscoid and lepidosteoid scale type. Introduction Actinopterygians, from primitive Coccolepididae to advanced teleosts, are represented in the Solnhofen lithographic limestone. These are fishes with rhombic and round scales. Ganoid scales of the lepidosteoid type are found in the following fishes: semionotid Lepidotes and Heterostrophus, macrosemiids Histionotus, Macrosemius, Notagogus and Propterus, ophiopsid Ophiopsis, caturids Furo and Brachyichthys, aspido- rhynchid Belonostomus, pleuropholid Pleuropholis, and pholidophorid Pholidophorus.
    [Show full text]
  • Vertebrate Remains Are Relatively Well Known in Late Jurassic Deposits of Western Cuba. the Fossil Specimens That Have Been Coll
    Paleontología Mexicana, 3 (65): 24-39 (versión impresa), 4: 24-39 (versión electrónica) Catalogue of late jurassiC VerteBrate (pisCes, reptilian) speCiMens froM western CuBa Manuel Iturralde-Vinent ¹, *, Yasmani Ceballos Izquierdo ² A BSTRACT Vertebrate remains are relatively well known in Late Jurassic deposits of western Cuba. The fossil specimens that have been collected so far are dispersed in museum collections around the world and some have been lost throughout the years. A reas- sessment of the fossil material stored in some of these museums’ collections has generated new data about the fossil-bearing lo- calities and greatly increased the number of formally identified specimens. The identified bone elements and taxa suggest a high vertebrate diversity dominated by actinopterygians and reptiles, including: long-necked plesiosaurs, pliosaurs, metriorhynchid crocodilians, pleurodiran turtles, ichthyosaurs, pterosaurs, and sauropod dinosaurs. This assemblage is commonly associated with unidentified remains of terrestrial plants and rare microor- ganisms, as well as numerous marine invertebrates such as am- monites, belemnites, pelecypods, brachiopods, and ostracods. This fossil assemblage is particularly valuable because it includes the most complete marine reptile record of a chronostratigraphic interval, which is poor in vertebrate remains elsewhere. In this contribution, the current status of the available vertebrate fossil specimens from the Late Jurassic of western Cuba is provided, along with a brief description of the fossil materials. Key words: Late Jurassic, Oxfordian, dinosaur, marine reptiles, fish, western Cuba. I NTRODUCTION Since the early 20th century, different groups of collectors have discovered 1 Retired curator, Museo a relatively rich and diverse vertebrate assemblage in the Late Jurassic stra- Nacional de Historia Natural, ta of western Cuba, which has been only partially investigated (Brown and Havana, Cuba.
    [Show full text]
  • The Strawberry Bank Lagerstätte Reveals Insights Into Early Jurassic Lifematt Williams, Michael J
    XXX10.1144/jgs2014-144M. Williams et al.Early Jurassic Strawberry Bank Lagerstätte 2015 Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 2014-144review-articleReview focus10.1144/jgs2014-144The Strawberry Bank Lagerstätte reveals insights into Early Jurassic lifeMatt Williams, Michael J. Benton &, Andrew Ross Review focus Journal of the Geological Society Published Online First doi:10.1144/jgs2014-144 The Strawberry Bank Lagerstätte reveals insights into Early Jurassic life Matt Williams1, Michael J. Benton2* & Andrew Ross3 1 Bath Royal Literary and Scientific Institution, 16–18 Queen Square, Bath BA1 2HN, UK 2 School of Earth Sciences, University of Bristol, Bristol BS8 2BU, UK 3 National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK * Correspondence: [email protected] Abstract: The Strawberry Bank Lagerstätte provides a rich insight into Early Jurassic marine vertebrate life, revealing exquisite anatomical detail of marine reptiles and large pachycormid fishes thanks to exceptional preservation, and especially the uncrushed, 3D nature of the fossils. The site documents a fauna of Early Jurassic nektonic marine animals (five species of fishes, one species of marine crocodilian, two species of ichthyosaurs, cephalopods and crustaceans), but also over 20 spe- cies of insects. Unlike other fossil sites of similar age, the 3D preservation at Strawberry Bank provides unique evidence on palatal and braincase structures in the fishes and reptiles. The age of the site is important, documenting a marine ecosystem during recovery from the end-Triassic mass extinction, but also exactly coincident with the height of the Toarcian Oceanic Anoxic Event, a further time of turmoil in evolution.
    [Show full text]
  • A Middle Triassic Kyphosichthyiform from Yunnan, China, and Phylogenetic Reassessment of Early Ginglymodians
    SUPPLEMENTARY DATA A Middle Triassic kyphosichthyiform from Yunnan, China, and phylogenetic reassessment of early ginglymodians XU Guang-Hui1,2 MA Xin-Ying1,2,3 WU Fei-Xiang1,2 REN Yi1,2,3 (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 [email protected]) (2 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044) (3 University of Chinese Academy of Sciences Beijing 100049) Part A Material examined and references Amia calva and Solnhofenamia elongata (Grande and Bemis, 1998); Araripelepidotes temnurus (Maisey, 1991; Thies, 1996); Asialepidotus shingyiensis (Xu and Ma, 2018); Atractosteus spatula, Cuneatus wileyi, Dentilepisosteus laevis, Lepisosteus osseus, Masillosteus janeae, and Obaichthys decoratus (Grande, 2010); Caturus furcatus (Patterson, 1975; Lambers, 1992; Grande and Bemis, 1998; FMNH UC2057); Dorsetichthys (‘Pholidophorus’) bechei (Patterson, 1975; Grande and Bemis, 1998; Arratia, 2013); Elops hawaiensis (Forey, 1973); Fuyuanichthys wangi (Xu et al., 2018); Ichthyokentema purbeckensis (Griffith and Patterson, 1963); Ionoscopus cyprinoides (Grande and Bemis, 1998; Maisey, 1999; FMNH P15472); Isanichthys palustris (Cavin and Suteethorn, 2006); Kyphosichthys grandei (Xu and Wu, 2012; Sun and Ni, 2018); Lashanichthys (‘Sangiorgioichthys’) sui (López-Arbarello et al., 2011); Lashanichthys (‘Sangiorgioichthys’) yangjuanensis (Chen et al, 2014); Lepidotes gigas (Thies,
    [Show full text]
  • Figura 33: Consenso Estrito Das Cinco Árvores Mais Parcimoniosas
    98 Figura 33: Consenso estrito das cinco árvores mais parcimoniosas. 99 Figura 34: C onsenso de maioria das cinco árvores mais parcimoniosas. 100 3 DISCUSSÃO 3.1 Nomenclatura 3.1.1 Série orbital A descrição da série orbital da presente dissertação foi baseada, principalmente, na nomenclatura utilizada por Daget (1964), Patterson (1973) e Grande & Bemis (1998). Daget (1964) definiu os ossos da série infraorbital como sendo os ossos que se dispõem ao longo do canal infraorbital (canal que segue da região nasal, passa abaixo das narinas e dos olhos e segue para trás pelo dermopterótico, chegando ao extraescapular e encontrando o canal da linha lateral), à frente do pterótico e anexados à margem da órbita. Expôs que podiam ser designados por número de ordem, da parte mais anterior para a mais posterior (e.g., infraorbital 1, infraorbital 2, infraorbital 3) ou por posição em relação a órbita (e.g., antorbital, suborbital e postorbital). O autor adotou a designação por ordem. Expôs ainda que é comum a denominação do último infraorbial como dermoesfenótico, osso no qual muitas vezes ocorre a anastomose do canal infraorbital com o canal supraorbital (canal que passa no nasal e no frontal). Para os ossos sem canal da série orbital, os quais Daget tratou como puramente membranosos, ele definiu como supraorbitais os ossos anexados ao longo da borda antero-lateral do frontal e como adenasal (= antorbital para outros autores) o osso entre o nasal e o primeiro infraorbital (Daget, 1964: fig. 38). Patterson (1973), da mesma forma que Daget (1964), denominou de infraorbitais os ossos anexados à margem inferior da órbita pelos quais passava o canal infraorbital e de supraorbitais os ossos anexados à margem superior da órbita e ao frontal.
    [Show full text]
  • A Synopsis of the Vertebrate Fossils of the English Chalk
    A. S. WOODWARD ON FOSSILS OF THE ENGLI SH CHALK. 273 Portion of tooth of Mosasallrus, from the Upper Chalk of Norwich, exhibited hy Mr. B. B. W OODWARD, F.G.S. R ecent Conglomeratic Boulder (pebbles in clay), from the Isle of Wight, exhibited by Mr. E . LITCIIFIELD. A SYNOPSIS 0 .. THE VERTEBRATE FOSSILS OF THE ENGLISH CIIALK. By A. SMITH WOODWARD, F .G.S., F .Z.S., of the British Museum tNatural History). I. INTRODUCTION. Since the publication of the revised edition of Dixon's ' Geology and Fossils of Sussex,' in 1878, no synoptical review of the ver­ tebrate fossils of the English Chalk appears to have been at­ tempted; and with the exception of the elaborate (though not critical) synopsis of genera in Mr. Etheridge's new edition of Phillips' 'Manual,' students of Cretaceous pal reontology can still find no other concise treatise on the subject. Much advance, how­ ever, has been made within the last ten years in our knowledge of later Mesozoic life; and I propose in the present communication to offer a brief epit ome of the facts in regard to the Vertebrata of the period, yielded by th e well-known uppermost division of the Meso­ zoic strata in Western Europe. Th e' Proceedings' of th e Asso­ ciation afford a most appropriate medium for the publication of such a review, so many of th e Members being interested in the treasures continually disinterred from th e numerous chalk pits of the South of England. And I have fortunately been able to compare with all that has been written th e unrivalled series of original specimens in the British Museum, and th e collection of Henry Willett, Esq., F .G.S., of Brighton, besides many othe r fossils in th e Museum of Practical Geology, Jermyn Street, the W oodwardian Museum, Cambridge, and the private cabinets of Mr.
    [Show full text]
  • Marine Early Triassic Osteichthyes from Spiti, Indian Himalayas
    Swiss J Palaeontol (2016) 135:275–294 DOI 10.1007/s13358-015-0098-6 Marine Early Triassic Osteichthyes from Spiti, Indian Himalayas 1 1 1 1 Carlo Romano • David Ware • Thomas Bru¨hwiler • Hugo Bucher • Winand Brinkmann1 Received: 12 March 2015 / Accepted: 11 August 2015 / Published online: 28 September 2015 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2015 Abstract A new, marine osteichthyan (bony fish) fauna strata of other localities. The study of Early Triassic fish from the Early Triassic of northern India is presented. The assemblages, including the presented one, is fundamental material was collected in situ at localities within Pin Valley for our understanding of the great osteichthyan diversifi- (Lahaul and Spiti District, Himachal Pradesh, India) and is cation after the Late Permian mass extinction event. dated as middle-late Dienerian (one specimen possibly earliest Smithian). The new ichthyofauna includes a lower Keywords Neotethys Á Northern Indian Margin Á jaw of the predatory basal ray-finned fish Saurichthys,a Gondwana Á Anoxia Á Biotic recovery Á Urohyal nearly complete specimen of a parasemionotid neoptery- gian (cf. Watsonulus cf. eugnathoides), as well as further Abbreviations articulated and disarticulated remains (Actinopterygii CMNFV Canadian Museum of Nature (Fossil indet., Actinistia indet.), and thus comprises the most Vertebrate), Ottawa, Canada complete Triassic fish fossils known from the Indian sub- MNHN.F Muse´um National d’Histoire Naturelle, Paris, continent. Saurichthys is known from many Triassic France localities and reached a global distribution rapidly after the PIMUZ Pala¨ontologisches Institut und Museum, Late Permian mass extinction event. Parasemionotidae, a Universita¨tZu¨rich, Zu¨rich, Schweiz species-rich family restricted to the Early Triassic, also achieved widespread distribution during this epoch.
    [Show full text]
  • Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal)
    Alexandre Renaud Daniel Guillaume Licenciatura em Biologia celular Mestrado em Sistemática, Evolução, e Paleobiodiversidade Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal) Dissertação para obtenção do Grau de Mestre em Paleontologia Orientador: Miguel Moreno-Azanza, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Co-orientador: Octávio Mateus, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Júri: Presidente: Prof. Doutor Paulo Alexandre Rodrigues Roque Legoinha (FCT-UNL) Arguente: Doutor Hughes-Alexandres Blain (IPHES) Vogal: Doutor Miguel Moreno-Azanza (FCT-UNL) Júri: Dezembro 2018 MICROVERTEBRATES OF THE LOURINHÃ FORMATION (LATE JURASSIC, PORTUGAL) © Alexandre Renaud Daniel Guillaume, FCT/UNL e UNL A Faculdade de Ciências e Tecnologia e a Universidade Nova de Lisboa tem o direito, perpétuo e sem limites geográficos, de arquivar e publicar esta dissertação através de exemplares impressos reproduzidos em papel ou de forma digital, ou por qualquer outro meio conhecido ou que venha a ser inventado, e de a divulgar através de repositórios científicos e de admitir a sua cópia e distribuição com objetivos educacionais ou de investigação, não comerciais, desde que seja dado crédito ao autor e editor. ACKNOWLEDGMENTS First of all, I would like to dedicate this thesis to my late grandfather “Papi Joël”, who wanted to tie me to a tree when I first start my journey to paleontology six years ago, in Paris. And yet, he never failed to support me at any cost, even if he did not always understand what I was doing and why I was doing it. He is always in my mind. Merci papi ! This master thesis has been one-year long project during which one there were highs and lows.
    [Show full text]
  • Article (PDF, 1844
    Fossil Record 10(1) (2007), 17–37 / DOI 10.1002/mmng.200600016 Eurycormus –– Eurypoma, two Jurassic actinopterygian genera with mixed identity Gloria Arratia* & Hans-Peter Schultze** The University of Kansas, Biodiversity Research Center and Department of Ecology and Evolutionary Biology, 1345 Jayhawk Blvd., Lawrence, KS 66045-7561. U.S.A. Received 1 August 2006, accepted 31 August 2006 Published online 30 January 2007 With 14 figures Key words: actinopterygian fishes, Upper Jurassic, southern Germany, morphology, systematics. Abstract Three Late Jurassic actinopterygian species are commonly placed in the genus Eurycormus: E. egertoni, E. grandis and E. spe- ciosus. A detailed comparison supports an earlier assignment to two different genera, Eurycormus Wagner, 1863 (speciosus) and Eurypoma Huxley, 1866 (E. egertoni and E. grande). Systematically, the two genera are only distantly related; Eurycormus belongs to the Teleosteomorpha, whereas Eurypoma is a halecomorph closely related to or a member of the Caturoidea with- in the Amiiformes. Schlu¨ sselwo¨ rter: Actinopterygii, Oberer Jura, Su¨ ddeutschland, Morphologie, Systematik. Zusammenfassung Drei oberjurassische Actinopterygier-Arten, egertoni, grandis und speciosus, werden gewo¨ hnlich zur Gattung Eurycormus ge- stellt. Ein detaillierter Vergleich der drei Arten besta¨tigt eine fru¨ here Zuordnung zu zwei verschiedenen Gattungen, Eurycor- mus Wagner, 1863 (speciosus) und Eurypoma Huxley, 1866 (E. egertoni und E. grande), die zwei ho¨ heren Taxa innerhalb der Neopterygii zugeordnet werden: Eurycormus zu den Teleosteomorpha und Eurypoma zu den Amiiformes innerhalb der Hale- comorphi, mo¨ glicherweise nahe oder innerhalb der Caturoidea. # 2007 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim Introduction cies, E. grandis (see Fig. 2A), from the Upper Jur- assic of Cambridgeshire, England, within this Agassiz (1843) named a Late Jurassic fish from genus.
    [Show full text]