Synchrotron-Aided Reconstruction of the Conodont Feeding Apparatus and Implications for the Mouth of the first Vertebrates

Total Page:16

File Type:pdf, Size:1020Kb

Synchrotron-Aided Reconstruction of the Conodont Feeding Apparatus and Implications for the Mouth of the first Vertebrates Synchrotron-aided reconstruction of the conodont feeding apparatus and implications for the mouth of the first vertebrates Nicolas Goudemanda,1, Michael J. Orchardb, Séverine Urdya, Hugo Buchera, and Paul Tafforeauc aPalaeontological Institute and Museum, University of Zurich, CH-8006 Zürich, Switzerland; bGeological Survey of Canada, Vancouver, BC, Canada V6B 5J3; and cEuropean Synchrotron Radiation Facility, 38043 Grenoble Cedex, France Edited* by A. M. Celâl Sxengör, Istanbul Technical University, Istanbul, Turkey, and approved April 14, 2011 (received for review February 1, 2011) The origin of jaws remains largely an enigma that is best addressed siderations. Despite the absence of any preserved traces of oral by studying fossil and living jawless vertebrates. Conodonts were cartilages in the rare specimens of conodonts with partly pre- eel-shaped jawless animals, whose vertebrate affinity is still dis- served soft tissue (10), we show that partial reconstruction of the puted. The geometrical analysis of exceptional three-dimensionally conodont mouth is possible through biomechanical analysis. preserved clusters of oro-pharyngeal elements of the Early Triassic Novispathodus, imaged using propagation phase-contrast X-ray Results synchrotron microtomography, suggests the presence of a pul- We recently discovered several fused clusters (rare occurrences ley-shaped lingual cartilage similar to that of extant cyclostomes of exceptional preservation where several elements of the same within the feeding apparatus of euconodonts (“true” conodonts). animal were diagenetically cemented together) of the Early This would lend strong support to their interpretation as verte- Triassic conodont Novispathodus (11). One of these specimens brates and demonstrates that the presence of such cartilage is a (Fig. 2A), found in lowermost Spathian rocks of the Tsoteng plesiomorphic condition of crown vertebrates. section (Tiandong District, Guangxi Province, China) (12, 13), consists of four “grasping” elements (S1–4 elements). apical cartilage | conodont oral skeleton | early vertebrates | homology Fused clusters partially preserve the relative 3D positions and EVOLUTION orientations of the involved elements. However, they are very ow the transition from “agnathans” to gnathostomes small, fragile, tricky to manipulate, and if more than two or three H(“jawed” vertebrates) occurred is one of the most intriguing elements are involved, very complicated to analyze. One way to problems of evolutionary biology (1). Little is known about the circumvent this is to use a nondestructive imaging method such endoskeleton of fossil jawless vertebrates [e.g., fossil cyclostomes as X-ray microtomography. In our case, the required resolution (hagfishes and lampreys) and “ostracoderms”]. Although the view and contrast could not be achieved with conventional micro- is still debated (2), euconodonts would have possessed the very tomography. Hence, we scanned this Chinese cluster, as well as GEOLOGY first vertebrate mineralized skeleton in the form of their oral a complete set of isolated elements (catalog nos. PIMUZ 39841–9) denticles (3, 4). found in the same sample and belonging to the same multielement The general architecture of the conodont oral skeleton is species, at the European Synchrotron Radiation Facility, on the a bilaterally symmetrical array of usually 15 phosphatic elements, ID19 beamline, using submicron resolution propagation phase- which generally becomes disarticulated after the decay of the contrast X-ray synchrotron microtomography (PPC-SRμCT) (14) supporting tissues. Hence most conodonts are known only as (Methods). On the basis of refs. 6, 11, and 15, we reconstructed isolated elements. From the detailed study of hundreds of ar- avirtual3DapparatusofNovispathodus. The relative sizes of the “ ” ticulated natural assemblages and photographic simulation S1–4 elements were inferred from the cluster. The other relative of their collapse, Purnell and Donoghue (5) constructed a 3D sizes (M, S0,P1,P2 relative to S1–4) were derived from the few model of the Idiognathodus apparatus [presumably a template known Neogondolella natural assemblages (Fig. 2 B–C)(15,16). for all ozarkodinid apparatuses (6)] in which one pair of Both our Novispathodus cluster and the Neogondolella natural obliquely pointed M elements are located rostrally and, behind assemblages (15, 16) show that the cusps of the S1 and S2 ele- them, one unpaired S0 (subscript number indicates distance or- ments were oriented more caudally than those of the S0 and S3, 4 dering from the symmetry axis) element lying on the axis of bi- elements, a feature that Orchard and Rieber considered to be lateral symmetry and four pairs of elements (S1–4) located on unique to the “gondolellaceans” (15, p. 480). Its recurrence in all both sides of the S0 would have grasped food and, more caudally, known Triassic assemblages (17 and 18) independently of their two pairs of pectiniform elements (P1,P2) would have processed collapse angle suggests that it is not due to a taphonomic bias – this food by crushing and/or slicing (5, 7, 8) (Fig. 1 A B) (for (postmortem rotation of elements) and indeed records a config- “ ” standard orientation of single elements, see Fig. S1). Purnell uration that differs from the Idiognathodus reconstruction (5). ’ and Donoghue s reconstruction of a generalized resting (dead) Natural assemblages of Ozarkodina, the presumed rootstock of position is very well supported and in most aspects very convincing. the Ozarkodinida (19), indicate that this caudal orientation of It is therefore adopted here as a basis upon which we build our dynamic reconstruction of the feeding apparatus at work. How could these elements actually grasp or cut prey tissues? Author contributions: N.G. designed research; N.G. and S.U. performed research; P.T. Purnell and Donoghue’s functional model (section 6 of ref. 5) contributed new reagents/analytic tools; H.B. provided biostratigraphic and paleoenvir- was based chiefly on analogies with extant agnathans. Indeed, the onmental data; N.G., M.J.O., S.U., and H.B. analyzed data; and N.G. wrote the paper. “quite simple” geometry of the Idiognathodus elements does not The authors declare no conflict of interest. provide much indication of what motions are possible or not *This Direct Submission article had a prearranged editor. [except for uncommon natural assemblages (see below)]. Thus, Data deposition: The synchrotron data presented in this manuscript is available on the hypotheses were inferred from extant putative closest relatives. open access paleontological database of the ESRF at http://paleo.esrf.eu. In our view, the more “complicated” Novispathodus apparatus 1To whom correspondence should be addressed. E-mail: [email protected]. imposes additional constraints that enable us to reconstruct the This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10. movement of the elements independently of phylogenetic con- 1073/pnas.1101754108/-/DCSupplemental. www.pnas.org/cgi/doi/10.1073/pnas.1101754108 PNAS Early Edition | 1of5 Downloaded by guest on September 25, 2021 A P1 B dorsal A B P2 sinistral rostral caudal dextral S0 S4 S1 S2 S3 M M ventral Fig. 1. Anatomical notation and orientation. (A) Dorsal view of the recon- C D structed, closed apparatus of Novispathodus. Anatomical notation after Purnell et al. (9). (B) Orientation of the apparatus within the conodont’s head. the cusp of the S1 is not restricted to the Gondolelloideans (ref. 20, reinterpreted in ref. 6, fig. 13A; 21). Fused clusters involving only the two hindeodelliform S3 and S4 elements are relatively more frequent in our collections. This suggests that they were located close and subparallel to one another (their recurrent relative position in those clusters) and Fig. 3. Geometrical correspondences between elements. (A) The S1 ele- fi had probably a common motion within the living animal. In ments match the posterior process of the S0. Per de nition, the tip of the (ab)oral view, their respective posterior processes are substraight cusp points posteriorly. ant: anterior; post: posterior. (B) Closed arrangement posteriorly and outwardly deflected behind the cusp, and their of S elements. (C) Presumed growth position of the S2 (silver) as inferred by anterior processes are laterally bowed inward, which results in an geometrical correspondences with the S3 and S4 elements (gold). (D) Pro- fi posed movement of the S0 against the M elements (silver: start and end overall sitar-like pro le. – fi positions; gold: pinching position). (A D) c: caudal; d: dextral; do: dorsal; r: The shape of the S2 ts those of the S3 and S4 in the following rostral; s: sinistral; v: ventral; blue circles: hypothetical cartilage. aspects: (i) In the “cluster position” (see above) where the cusp of the S2 is subparallel to the posterior processes of the S3 and S4 elements, the outer profile (oral view) of the S2 is similar to the If we assume that the various elements moved along trajec- fi inner pro le of the S3, and the largest denticle of its antero- tories approximately parallel to the curvature of the cusp and lateral process is aligned with the cusps of the S3 and S4 (Figs. 2A denticles (5), then the movements of the S2–4 elements must have and 3B). (ii) In a presumed “growth position” where the re- included an opening/closing pivot motion around an axis parallel spective basal cavities (initial growth centers) of the S2–4 ele- to the posterior processes of the S3 and S4. Consequently, the
Recommended publications
  • Fish Identification
    FISH IDENTIFICATION Anurag Babu EWRG ,CES, IISc, Bangalore SUPER CLASS INFRAPHYLUM AGNATHA CYCLOSTOMAT A PHYLUM CHORDATA SUPER CLASS INFRAPHYLUM Incertae serdis GNATHOSTOMA SUPER CLASS OSTEICHTHYES CLASS CLASS CLASS MYXINI PETROMYZONTIDA CONODANTA CLASS CLASS CLASS CONDRICHTHYES PLACODERMI ACANTHODII CLASS CLASS ACTINOPTERYGII SARCOPTERYGII CLASS CLASS CLASS PTERASPIDOMORPHI THELODONTI ANASPIDA CLASS CEPHALASPIDOMORPHI So , What are the Steps FISH SAMPLING What is the purpose of our Sampling ? Use suitable gears Gears based on purpose Active Gear/ Sampling Passive Gear/ Sampling Fyke Net Cast Net Scoop Net Gill Net Angling FISH IDENTIFICATION ANATOMICAL BODY SHAPE Torpediform Dorso Ventrally Flattened Ribbon like Eel like Spheroid Laterally Flattened Arrow like COLOR & PATTERN ? Etroplus maculatus Scatophagus argus Etroplus suratensis MERISTIC FACIAL & CRANIAL BONES TYPE OF MOUTH Funneled Silver bellies Mouth Classification EYE Caranx latus EYE Caranx latus LEFT OR RIGHT Scophthalmus maximus Hippoglossus hippoglossus FINS DORSAL FINS CAUDAL FINS PECTORAL FIN PELVIC FIN ANAL FIN Caranx ignobilis Spiny Dorsal DORSAL FIN Rayed Dorsal Adipose Dorsal Spiny & Rayed Anal ANAl FIN Rayed Anal PECTORAL FINS PELVIC FINS Abdominal Thoracic CAUDAL FINS CAUDAL FINS What makes Spine & Ray Different ? GILL RAKERS SCALES LATERAL LINE CONTINUITY POSITION CURVE SCUTES IDENTIFICATION KEYS DICHOTOMOUS POLYTOMOUS FIN ( Neogobius melanostomus (Pallas, 1811).) FORMULAD1 VI (V-VII); D2 I + 14-16 (13-16); A I + 11-13 (11-14); P 18-19 (17-20). The anterior dorsal fin has 6 spines, ranging from 5-7 The posterior dorsal fin has one spine and 14-16 soft rays, ranging from 13-16 The anal fin has one spine, 11-13 soft rays, ranging from 11-14 The pectoral fins have 18-19 soft rays, ranging from 17-20 MORPHOMETRIC LET’S try Identifying A FISH !! FIN ( Neogobius melanostomus (Pallas, 1811).) FORMULAD1 VI (V-VII); D2 I + 14-16 (13-16); A I + 11-13 (11-14); P 18-19 (17-20).
    [Show full text]
  • New Genus of Eugaleaspidiforms Found in China 15 February 2012
    New genus of Eugaleaspidiforms found in China 15 February 2012 The new genus is most suggestive of Eugaleaspis of the Eugaleaspidae by the absence of inner corners, in addition to the diagnostic features of the family, such as only 3 pairs of lateral transverse canals from lateral dorsal canals, and the U-shaped trajectory of median dorsal canals. They differ in that the new genus possesses a pair of posteriorly extending corners, the breadth/length ratio of the shield smaller than 1.1, and the posterior end of median dorsal opening beyond the posterior margin of orbits. Dr. ZHU Min, lead author of the study, and his colleagues reexamined the type specimen of Eugaleaspis xiushanensis from the Wenlock Huixingshao Formation of Chongqing, and observed a pair of posteriorly extending lobate corners and three (instead of four in the original description) pairs of lateral transverse canals. Thus, they re-assigned it to Dunyu. The new species Fig.1: Cephalic shield of Dunyu longiforus gen. et sp. differs from Dunyu xiushanensis in its large nov. ( holotype IVPP V 17681). A. dorsal view; B. ventral cephalic shield which is longer than broad, spine- view; C. close-up view of the left corner; D. close-up shaped corners, anteriorly positioned orbits, the view to show the regional variation of polygonal length ratio between preorbital and postorbital tubercles, and minute spines on the inner surface of the portions of the shield less than 0.75, and large dermal rim encircling the median dorsal opening; E. polygonal, flat-topping tubercles exceeding 2.0 mm illustrative drawing in dorsal view.
    [Show full text]
  • THE CLASSIFICATION and EVOLUTION of the HETEROSTRACI Since 1858, When Huxley Demonstrated That in the Histological Struc
    ACTA PALAEONT OLOGICA POLONICA Vol. VII 1 9 6 2 N os. 1-2 L. BEVERLY TARLO THE CLASSIFICATION AND EVOLUTION OF THE HETEROSTRACI Abstract. - An outline classification is given of the Hetero straci, with diagnoses . of th e following orders and suborders: Astraspidiformes, Eriptychiiformes, Cya­ thaspidiformes (Cyathaspidida, Poraspidida, Ctenaspidida), Psammosteiformes (Tes­ seraspidida, Psarnmosteida) , Traquairaspidiformes, Pteraspidiformes (Pte ras pidida, Doryaspidida), Cardipeltiformes and Amphiaspidiformes (Amphiaspidida, Hiber­ naspidida, Eglonaspidida). It is show n that the various orders fall into four m ain evolutionary lineages ~ cyathaspid, psammosteid, pteraspid and amphiaspid, and these are traced from primitive te ssellated forms. A tentative phylogeny is pro­ posed and alternatives are discussed. INTRODUCTION Since 1858, when Huxley demonstrated that in the histological struc­ ture of their dermal bone Cephalaspis and Pteraspis were quite different from one another, it has been recognized that there were two distinct groups of ostracoderms for which Lankester (1868-70) proposed the names Osteostraci and Heterostraci respectively. Although these groups are generally considered to be related to on e another, Lankester belie­ ved that "the Heterostraci are at present associated with the Osteostraci because they are found in the same beds, because they have, like Cepha­ laspis, a large head shield, and because there is nothing else with which to associate them". In 1889, Cop e united these two groups in the Ostracodermi which, together with the modern cyclostomes, he placed in the Class Agnatha, and although this proposal was at first opposed by Traquair (1899) and Woodward (1891b), subsequent work has shown that it was correct as both the Osteostraci and the Heterostraci were agnathous.
    [Show full text]
  • Two New Early Balognathid Conodont Genera from the Ordovician Of
    Two new early balognathid conodont genera from the Ordovician of Oman and comments on the early evolution of prioniodontid conodonts Miller, Giles; Heward, Alan; Mossoni, Angelo; Sansom, Ivan DOI: 10.1080/14772019.2017.1314985 License: Other (please specify with Rights Statement) Document Version Peer reviewed version Citation for published version (Harvard): Miller, G, Heward, A, Mossoni, A & Sansom, I 2017, 'Two new early balognathid conodont genera from the Ordovician of Oman and comments on the early evolution of prioniodontid conodonts', Journal of Systematic Palaeontology, pp. 1-23. https://doi.org/10.1080/14772019.2017.1314985 Link to publication on Research at Birmingham portal Publisher Rights Statement: This is an Accepted Manuscript of an article published by Taylor & Francis in Journal of Systematic Palaeontology on 05/05/2017, available online: http://www.tandfonline.com/10.1080/14772019.2017.1314985 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain.
    [Show full text]
  • The Nearshore Cradle of Early Vertebrate Diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan
    University of Birmingham The nearshore cradle of early vertebrate diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan DOI: 10.1126/science.aar3689 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Sallan, L, Friedman, M, Sansom, R, Bird, C & Sansom, I 2018, 'The nearshore cradle of early vertebrate diversification', Science, vol. 362, no. 6413, pp. 460-464. https://doi.org/10.1126/science.aar3689 Link to publication on Research at Birmingham portal Publisher Rights Statement: This is the author’s version of the work. It is posted here by permission of the AAAS for personal use, not for redistribution. The definitive version was published in Science on 26th October 2018. DOI: 10.1126/science.aar3689 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document.
    [Show full text]
  • A New Groenlandaspidid Arthrodire (Vertebrata: Placodermi) from the Famennian of Belgium
    GEOLOGICA BELGICA (2005) 8/1-2: 51-67 A NEW GROENLANDASPIDID ARTHRODIRE (VERTEBRATA: PLACODERMI) FROM THE FAMENNIAN OF BELGIUM Philippe JANVIER1-2 and Gaël CLÉMENT1 1. UMR 5143 du CNRS, Département «Histoire de la Terre», Muséum National d ’Histoire Naturelle, 8 rue Buffon, 75005 Paris, France. [email protected] 2. Toe Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom (9 figures, 1 table and 2 plates) ABSTRACT. A new species of the arthrodire genus Groenlandaspis is described from the upper part of the Evieux Formation (Upper Famennian), based on several specimens collected from quarries at Modave and Villers-le-Temple, Liège Province, Belgium. It is the first occurrence of this widespread genus in continental Europe. This new species is characterized by an almost smooth dermal armour, except for some scattered tubercles on its skull roof, median dorsal and spinal plates. Its median dorsal plate is triangular in shape and almost perfectly equilateral in lateral aspect and bears large, spiniform denticles on its posterior edge. All these Groenlandaspis remains occur in micaceous, dolomitic claystones or siltstones probably deposited in a subtidal environment. Outcrops of the same area have yielded other vertebrate remains, such as the placoderms Phyllolepis and Bothriolepis, acanthodians, various piscine sarcopterygians (Holoptychius , dipnoans, a rhizodontid, Megalichthys, Eusthenodon and a large tristichopterid), and a tetrapod that is probably close to Ichthyostega. The biogeographical history of the genus Groenlandaspis
    [Show full text]
  • The Pharynx of the Stem-Chondrichthyan Ptomacanthus and the Early Evolution of the Gnathostome Gill Skeleton
    ARTICLE https://doi.org/10.1038/s41467-019-10032-3 OPEN The pharynx of the stem-chondrichthyan Ptomacanthus and the early evolution of the gnathostome gill skeleton Richard P. Dearden 1, Christopher Stockey1,2 & Martin D. Brazeau1,3 The gill apparatus of gnathostomes (jawed vertebrates) is fundamental to feeding and ventilation and a focal point of classic hypotheses on the origin of jaws and paired appen- 1234567890():,; dages. The gill skeletons of chondrichthyans (sharks, batoids, chimaeras) have often been assumed to reflect ancestral states. However, only a handful of early chondrichthyan gill skeletons are known and palaeontological work is increasingly challenging other pre- supposed shark-like aspects of ancestral gnathostomes. Here we use computed tomography scanning to image the three-dimensionally preserved branchial apparatus in Ptomacanthus,a 415 million year old stem-chondrichthyan. Ptomacanthus had an osteichthyan-like compact pharynx with a bony operculum helping constrain the origin of an elongate elasmobranch-like pharynx to the chondrichthyan stem-group, rather than it representing an ancestral condition of the crown-group. A mixture of chondrichthyan-like and plesiomorphic pharyngeal pat- terning in Ptomacanthus challenges the idea that the ancestral gnathostome pharynx con- formed to a morphologically complete ancestral type. 1 Department of Life Sciences, Imperial College London, Silwood Park Campus, Buckhurst Road, Ascot SL5 7PY, UK. 2 Centre for Palaeobiology Research, School of Geography, Geology and the Environment, University of Leicester, University Road, Leicester LE1 7RH, UK. 3 Department of Earth Sciences, Natural History Museum, London SW7 5BD, UK. Correspondence and requests for materials should be addressed to M.D.B.
    [Show full text]
  • (Chondrichthyes) from the Burtnieki Regional Stage, Middle Devonian of Estonia
    Estonian Journal of Earth Sciences, 2008, 57, 4, 219–230 doi:10.3176/earth.2008.4.02 Karksilepis parva gen. et sp. nov. (Chondrichthyes) from the Burtnieki Regional Stage, Middle Devonian of Estonia Tiiu Märss, Anne Kleesment, and Moonika Niit Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; [email protected], [email protected] Received 13 August 2008, accepted 30 September 2008 Abstract. Dermal scales of a new chondrichthyan were discovered in four levels in sandstones of the Härma Beds (lower part of the Burtnieki Regional Stage, Middle Devonian) in the Karksi outcrop of South Estonia. The classification of Karksilepis parva gen. et sp. nov. Märss is still uncertain. Key words: Chondrichthyes, Burtnieki Regional Stage, Middle Devonian, Estonia. INTRODUCTION list of chondrichthyan and putative chondrichthyan taxa from the Lochkovian of the Mackenzie Mountains Chondrichthyan scales are rare in Lower–Middle Palaeo- (MOTH locality), Canada, includes Kathemacanthus, zoic rocks. Chondrichthyan-like scales, however, were Altholepis, Seretolepis, Polymerolepis species, and five described by Sansom et al. (1996) from the Ordovician unnamed taxa (Hanke & Wilson 1997, 1998; Wilson & of Colorado, USA, and by Young (1997) from central Hanke 1998; Wilson et al. 2000). Ellesmereia are found Australia. The earliest Elasmobranchii gen. nov. has in the Lochkovian of the Canadian Arctic (Vieth 1980). been listed from the Early Llandovery (Early Silurian) Scales of Arauzia, Lunalepis, and Iberolepis are known of the Siberian Platform, Russia (Karatajūtė-Talimaa & from the Lower Devonian, Lower Gedinnian (Lochkovian) Predtechenskyj 1995). Niualepis and Elegestolepis conica of Spain (Mader 1986). Pamyrolepis nom. nud. Karatajūtė- have been identified in the Middle Llandovery of South Talimaa scales have been briefly described from the Yakutia and the Bratsk Region, Siberian Platform Emsian of the Eastern Pamyrs (Karatajūtė-Talimaa 1992; (Novitskaya & Karatajūtė-Talimaa 1986; Karatajūtė- Leleshus et al.
    [Show full text]
  • The Nearshore Cradle of Early Vertebrate Diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Birmingham Research Portal The nearshore cradle of early vertebrate diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan DOI: 10.1126/science.aar3689 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Sallan, L, Friedman, M, Sansom, R, Bird, C & Sansom, I 2018, 'The nearshore cradle of early vertebrate diversification', Science, vol. 362, no. 6413, pp. 460-464. https://doi.org/10.1126/science.aar3689 Link to publication on Research at Birmingham portal Publisher Rights Statement: This is the author’s version of the work. It is posted here by permission of the AAAS for personal use, not for redistribution. The definitive version was published in Science on 26th October 2018. DOI: 10.1126/science.aar3689 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain.
    [Show full text]
  • Exceptionally Preserved Conodont Apparatuses with Giant Elements from the Middle Ordovician Winneshiek Konservat-Lagerstätte, Iowa, USA
    Journal of Paleontology, 91(3), 2017, p. 493–511 Copyright © 2017, The Paleontological Society 0022-3360/16/0088-0906 doi: 10.1017/jpa.2016.155 Exceptionally preserved conodont apparatuses with giant elements from the Middle Ordovician Winneshiek Konservat-Lagerstätte, Iowa, USA Huaibao P. Liu,1 Stig M. Bergström,2 Brian J. Witzke,3 Derek E. G. Briggs,4 Robert M. McKay,1 and Annalisa Ferretti5 1Iowa Geological Survey, IIHR-Hydroscience & Engineering, University of Iowa, 340 Trowbridge Hall, Iowa City, IA 52242, USA 〈[email protected]〉; 〈[email protected]〉 2School of Earth Sciences, Division of Earth History, The Ohio State University, 125 S. Oval Mall, Columbus, Ohio 43210, USA 〈[email protected]〉 3Department of Earth and Environmental Sciences, University of Iowa, 115 Trowbridge Hall, Iowa City, IA 52242, USA 〈[email protected]〉 4Department of Geology and Geophysics, and Yale Peabody Museum of Natural History, Yale University, New Haven, CT 06520, USA 〈[email protected]〉 5Dipartimento di Scienze Chimiche e Geologiche, Università degli Studi di Modena e Reggio Emilia, via Campi 103, I-41125 Modena, Italy 〈[email protected]〉 Abstract.—Considerable numbers of exceptionally preserved conodont apparatuses with hyaline elements are present in the middle-upper Darriwilian (Middle Ordovician, Whiterockian) Winneshiek Konservat-Lagerstätte in northeastern Iowa. These fossils, which are associated with a restricted biota including other conodonts, occur in fine-grained clastic sediments deposited in a meteorite impact crater. Among these conodont apparatuses, the com- mon ones are identified as Archeognathus primus Cullison, 1938 and Iowagnathus grandis new genus new species. The 6-element apparatus of A.
    [Show full text]
  • A Database of Triassic Conodonts from a Comprehensive Revision of Literature
    SPANISH JOURNAL OF PALAEONTOLOGY A database of Triassic conodonts from a comprehensive revision of literature Pablo PLASENCIA1,2*, Ana MÁRQUEZ-ALIAGA2 & Jingeng SHA1 1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology (CAS), Nanjing, 39 East Beijing Road, Nanjing, 210008, People’s Republic of China; [email protected]; [email protected] 2 Departamento de Geología, Universitat de Valencia, Dr. Moliner, 50, 46100 Burjassot, Valencia, Spain; [email protected] * Corresponding author Plasencia, P., Márquez-Aliaga, A. & Sha, J. 2013. A data base of Triassic conodonts from a comprehensive revision of literature. [Una base de datos de conodontos triásicos a partir de una completa revisión de la literatura]. Spanish Journal of Palaeontology, 28 (2), 215-226. Manuscript received 08 September 2012 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 19 December 2012 ABSTRACT RESUMEN The revision of a comprehensive amount of bibliography La revisión de una amplia cantidad de bibliografía ha hecho has made possible the development of a database containing posible el desarrollo de una base de datos en la que fi guran los the stratigraphic ranges of the conodont species from the rangos estratigráfi cos de las especies de conodontos presentes uppermost Permian and the Triassic, with a total of 336 species desde el Pérmico superior y el Triásico, con un total de 336 in 52 genera. This database is aimed at biostratigraphy and especies y 52 géneros. Esta base de datos está dirigida a la studies related to biological, evolutional and palaeodiversity bioestratigrafía y a estudios relacionados con las dinámicas dynamics.
    [Show full text]
  • Fossils, Histology, and Phylogeny: Why Conodonts Are Not Vertebrates
    234 by Alain Blieck1, Susan Turner2,3, Carole J. Burrow3, Hans-Peter Schultze4, Carl B. Rexroad5, Pierre Bultynck6 and Godfrey S. Nowlan7 Fossils, histology, and phylogeny: Why conodonts are not vertebrates 1Université Lille 1: Sciences de la Terre, FRE 3298 du CNRS «Géosystèmes», F-59655 Villeneuve d’Ascq cedex, France. E-mail: [email protected] 2Monash University, Geosciences, Box 28E, Victoria 3800, Australia 3Queensland Museum, Geosciences, 122 Gerler Road, Hendra, Queensland 4011, Australia 4Kansas University, Biodiversity Institute & Natural History Museum, 1345 Jayhawk Blvd., Lawrence, KS 66045-7593, USA 5Indiana Geological Survey, 611 North Walnut Grove, Bloomington, IN 47405-2208, USA 6Institut Royal des Sciences Naturelles de Belgique, Département de Paléontologie, Rue Vautier, 29, B-1000 Bruxelles, Belgium 7Geological Survey of Canada, 3303 – 33rd Street NW, Calgary, AB T2L 2A7, Canada The term vertebrate is generally viewed by help resolve the phylogenetic relationships of conodonts systematists in two contexts, either as Craniata and chordates, the analysis should be extended to (myxinoids or hagfishes + vertebrates s.s., i.e. basically, include non-chordate taxa. animals possessing a stiff backbone) or as Vertebrata (lampreys + other vertebrae-bearing animals, which Historical background we propose to call here Euvertebrata). Craniates are characterized by a skull; vertebrates by vertebrae A recent paper by Sweet and Cooper (2008), within the classic paper series of Episodes, drew our attention and prompted this (arcualia); euvertebrates are vertebrates with hard response. Their paper concerned the discovery and the concept of phosphatised tissues in the skeleton. The earliest conodonts by Christian Heinrich Pander (1856). He was the first known possible craniate is Myllokunmingia (syn.
    [Show full text]