Historie Mammalia: Fosilní Záznam

Total Page:16

File Type:pdf, Size:1020Kb

Historie Mammalia: Fosilní Záznam • Primární viscerokranium: Historie Mammalia: mandibulare- quadratum- Fosilní záznam hyomandibulare • Synapsida - nejstarší Amniota - od (stapes) středniho Karbonu (ca 320 My) • Dermální • Cotylosauria vs. Pelycosauria (nejhojnější skelet: skupina v permu a triasu) – Dentale, coronoideum, angulare, suprangulare, prearticulare 190 Pelycosauria 225 THERAPSIDA Non-Mammalian Caseasauria Synapsida 1 Synapsida • Autapomorphies of the main clades of synapsids • Michel Laurin and Robert R. Reisz The classification of synapsids may be summarized as follows: • =============================================================== Eothyrididae ==Caseasauria=| | =============================================================== Caseidae | | ============================================================ Varanopseidae | | | | ======================================================== Ophiacodontidae | | | | | | ==================================================== Edaphosauridae | | | | =====| | | | =================================== Haptodus garnettensis | | | | | ==Eupelycosauria=| | | | =============================== Palaeohatteria ==A=| | | | ==B=| | | =========================== Pantelosaurus ==Sphenacodontia=| | | ==C=| | ======================= Cutleria ==D=| | ==E=| === Sphenacodontidae ==Sphenacodontoidea=| === Therapsida This classification and the list of apomorphies given below is taken from recent studies by Reisz (1986), Hopson (1991), Reisz et al. (1992), Berman et al. (1995), and Laurin and Reisz (1996), to which the readers should refer for further information. • Caseasauria (eothyridids and caseids) exhibits the following autapomorphies: • A long external naris with an external narial shelf (Fig. 1A). Temporální jáma mezi • A pointed rostrum formed by the dorsal process of the premaxilla (Fig. 1A). squamosum, jugale, postorbitale, • • Click on an image to view larger version & data in a new window • • Figure 1. Synapsid skulls in lateral view. A, Cotylorhynchus, a Lower Permian caseid. B, Varanosaurus, a Lower Permian ophiacodontid. C, Dimetrodon, a Lower Permian sphenacodontid. D, Titanophoneus, an Upper Permian therapsid. Redrawn from B, Berman et al occipitale orientováno vertikálně . (1995); C, Romer and Price (1940), and D, Orlov (1958). Abbreviations: An, angular; Ar, articular; Bc, braincase; D, dentary; E, epipterygoid; F, frontal; J, jugal; L, lacrimal; M, maxilla; N, nasal; P, parietal; Pm, premaxilla; Po, postorbital; Pof, po stfrontal; Prf, prefrontal; Pt, pterygoid; Q, quadrate; Qj, quadratojugal; Sa, surangular; Sp, splenial; Sq, squamosal; St, supratemporal; T, tabular. Scale bars equal 1 cm. • The main autapomorphy of Eothyrididae (Eothyris and Casea) is as follows: • Large caniniform tooth is present in anterior part of the maxilla. • Ca sei d a e possesses the following autapomorphies: • A large, high external naris (Fig. 1A). The external naris of eothyridids is long, but it is more primitive in that it is relatively low (narrow). • Posterior marginal teeth bearing a longitudinal row of cusps. Similar teeth are found in many other herbivorous amniotes, such as herbivorous squamates (iguanas) and many groups of herbivorous dinosaurs. • Reduced phalangeal formula, ranging from 2-3-4-4-3 to 2-2-2-3-2. Primitively in synapsids, the phalangeal formula was 2-3-4- 5-3 in the hand and 2-3-4-5-4 in the foot. • • Click on an image to view larger version & data in a new window • • Figure 2. Synapsid skulls in dorsal view. A, Cotylorhynchus, a Lower Permian caseid. B, Varanosaurus, a Lower Permian ophiacodontid. C, Dimetrodon, a Lower Permian sphenacodontid. D, Titanophoneus, an Upper Permian therapsid. Redrawn from B, Berman et al. (1995); C, Romer and Price (1940), and D, Orlov (1958). Abbreviations: Bc, braincase; F, frontal; J, jugal; L, lacrimal; M, maxilla; N, nasal; P, parietal; Pa, palatine; Pm, premaxilla; Po, postorbital; Pof, postfrontal; Pp, postparietal; Prf, prefrontal ; Qj, quadratojugal; Sq, squamosal; St, supratemporal; T, tabular. Scale bars equal 1 cm. • Au t ap o mo rp h i es o f Eupelycosauria: • A long, narrow supratemporal (Fig. 2B-D). The supratemporal of caseasaurs is almost as wide as long (length to width ratio less than two). • The frontal contributes to at least one third of the dorsal orbital margin (the orbital contribution of the frontal is narrower in caseasaurs) (Fig. 2B-D). • Au t ap o mo rp h i es o f Varanopseidae: • Marginal dentition composed of strongly curved, mediolaterally flattened teeth. • Occipital flange of squamosal reduced. • Narro w zy g o mat i c arch . • Autapomorphies of the clade including Ophiacodontidae, Edaphosauria, and Sphenacodontia (unnamed clade A in the above classification): • Nasal longer than parietal at midline (it is shorter in other synapsids) (Fig. 2B-D). • A narrow posterior process of the postorbital (this process is broad in other synapsids). • A long contribution of the jugal to the ventral edge of the skull (this contribution is narrow, if present, in other synapsids). • A contribution of the squamosal to the zygomatic arch (in other synapsids, this arch is composed exclusively of the jugal and the quadratojugal) (Fig. 1B-D). • Ectopterygoid teeth absent. • Au t ap o mo rp h i es o f Ophiacodontidae include: • Antorbital region of skull at least twice as long (Fig. 2B-D) as the postorbital region (it is shorter in other synapsids). • Nasal longer than frontal (it is shorter than the frontal in other synapsids). • Paroccipital process short, not extending to the cheek (it is longer and reaches the quadrate or the squamosal in other synapsids) (Fig. 3B). • Tabular not extending ventrally beyond the level of the supraoccipital (in other synapsids, it extends farther ventrally) (Fig. 3B). • • Click on an image to view larger version & data in a new window • • Figure 3. Synapsid skulls in occipital view. A, Cotylorhynchus, a Lower Permian caseid. B, Varanosaurus, a Lower Permian ophiacodontid. C, Dimetrodon, a Lower Permian sphenacodontid. D, Titanophoneus, an Upper Permian therapsid. Redrawn from B, Berman et al . (1 9 9 5 ); C, Ro mer an d P ri ce (1 9 4 0 ), an d D, Orl o v (1 9 5 8 ). Ab b rev i at i o n s: Bc, b rai n case; J, j u g al ; P , p ari et al ; P p , p o st p ari et al ; P s, p arasp h en o i d ; P t , p t ery g o i d ; Q, q u ad rat e; Qj , q u ad rat o j u g al ; S , st ap es; S q , sq u amo sal ; S t , su p rat emp o ral ; T , t ab u l ar. S c al e b ars eq u al 1 cm. • Au t ap o mo rp h i es o f Unnamed clade B (Edaphosauridae and Sephenacodontia) include: • Orbital process of frontal present (in other synapsids, the frontal may contribute to the orbit, but it does not extend farther laterally in this area than elsewhere) (Fig. 2C, D). • Lateral surface of postorbital recessed (it is flat in other synapsids). • Anteroventral process of quadratojugal absent (in other synapsids, the quadratojugal is much larger in lateral view because it has a long anteroventral process) (Fig. 1C, D). • Au t ap o mo rp h i es o f Edaphosauridae include: • Presence of lateral tubercles on neural spines. • Neural spines long and circular in cross section distal to a laterally compressed proximal section. • Cervical neural spines lean anteriorly, whereas posterior spines lean posteriorly. • These three autapomorphies contribute to the peculiar morphology of the sail of edaphosaurs. • Au t ap o mo rp h i es o f Sphenacodontia include: • Maxillary supracanine buttress present (this structure is a thickening of the maxilla visible on its internal surface, dorsal to the caniniform teeth). • Premaxillary teeth in deep sockets. The teeth of other synapsids are implanted in shallow sockets. • Au t ap o mo rp h i es o f Haptodus garnettensis include: • The presence of a small facial exposure of the septomaxilla. In other synapsids, the septomaxilla is restricted to the external naris, except in most therapsids, where it has a large facial exposure. • Postcaniniform teeth robust, chisel- shaped. The shape of marginal teeth is quite variable in early synapsids, but their morphology in H. garnettensis is unique. • Teeth present on the palatal ramus of the premaxilla. In other synapsids, this bone only bears marginal teeth. • Au t ap o mo rp h i es o f unnamed clade C (Palaeohatteria, Pantelosaurus, Cutleria, and Sphenacodontoidea) include: • Presence of a reflected lamina of the angular (Fig. 1C, D). This ventral flange of the angular eventually became part of the tympanic annulus of mammals (the ring that supports the ear drum). • Au t ap o mo rp h i es o f Palaeohatteria longicaudata include: • A contact between the postorbital and the supratemporal. • Au t ap o mo rp h i es o f unnamed clade D (Pantelosaurus, Cutleria, and Sphenacodontoidea) include: • Jugal anterior process broad anteriorly (it is narrow in other synapsids) (Fig. 1C). • Only one autapomorphy was identified in Pantelosaurus saxonicus: • Posterior end of dentary well below the posterior edge of the jaw. In other synapsids, the posterior end of the dentary is near the dorsal edge of the jaw. • Au t ap o mo rp h i es o f unnamed clade E (Cutleria and Sphenacodontoidea) include: • Nasal longer than the frontal (the nasal is shorter in most other synapsids). A long nasal appeared convergently in ophiacodontids (Fig. 2B-D). • A deep notch on the parietal for the anterior tip of the supratemporal (this notch is shallow in other synapsids) (Fig. 3C). • Cutting edges on marginal teeth (these edges are absent in most other synapsids). • Au t ap o mo rp h i es o f Cutleria wilmarthi include: • An anteriorly
Recommended publications
  • A New Basal Sphenacodontid Synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany
    A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany JÖRG FRÖBISCH, RAINER R. SCHOCH, JOHANNES MÜLLER, THOMAS SCHINDLER, and DIETER SCHWEISS Fröbisch, J., Schoch, R.R., Müller, J., Schindler, T., and Schweiss, D. 2011. A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany. Acta Palaeontologica Polonica 56 (1): 113–120. A new basal sphenacodontid synapsid, represented by an anterior portion of a mandible, demonstrates for the first time the presence of amniotes in the largest European Permo−Carboniferous basin, the Saar−Nahe Basin. The new taxon, Cryptovenator hirschbergeri gen. et sp. nov., is autapomorphic in the extreme shortness and robustness of the lower jaw, with moderate heterodonty, including the absence of a greatly reduced first tooth and only a slight caniniform develop− ment of the second and third teeth. Cryptovenator shares with Dimetrodon, Sphenacodon, and Ctenospondylus, but nota− bly not with Secodontosaurus, enlarged canines and a characteristic teardrop outline of the marginal teeth in lateral view, possession of a deep symphyseal region, and a strongly concave dorsal margin of the dentary. The new find shows that sphenacodontids were present in the Saar−Nahe Basin by the latest Carboniferous, predating the record of sphenacodontid tracks from slightly younger sediments in this region. Key words: Synapsida, Sphenacodontidae, Carboniferous, Saar−Nahe Basin, Germany. Jörg Fröbisch [[email protected]], Department of Geology, The Field Museum, 1400 South Lake Shore Drive, Chicago, Illinois 60605, USA and [joerg.froebisch@mfn−berlin.de], Museum für Naturkunde Leibniz−Institut für Evolu− tions− und Biodiversitätsforschung an der Humboldt−Universität zu Berlin, Invalidenstr.
    [Show full text]
  • Pelycosauria Y Therapsida
    Pelycosauria y Therapsida Los amniotos pueden dividirse en dos líneas principales: Los synapsidos (de quienes provienen los mamíferos) y los Sauropsidos (de quienes provienen “rep;les” y aves). Los Synápsidos poseen una apertura (fenestra) en el cráneo, detrás del ojo, debajo de la unión entre los huesos postorbital y escamoso. Comparten un ancestro en común más reciente con un mamífero que con una lagar;ja. Filogené;camente, no pertenecen a rep;lia, pero a la mayoría se les conoce como “rep;les semejantes a mamíferos” Anapsida Synapsida Diapsida “Parapsida” o “Euryapsida” (Diapsida modificados) SYNAPSIDA: -COMPARTEN UN ACMR CON MAMÍFEROS QUE CON REPTILES -FENESTRA TEMPORAL, BAJO POSTORBITAL-ESCAMOSO -REGION OCCIPITAL POSTERIORMENTE INCLINADA (NO VERTICAL) -SUPRATEMPORAL SE CONECTA AL POSTORBITAL PETROLACOSAURUS ARCHAEOTHYRIS (synapsida) -CENTRALE MEDIAL (MC) BIEN DESARROLLADO EN EL TARSO -PRESENCIA DE DOS HUESOS CORONOIDES (LADO MEDIAL MANDÍBULA) Tradicionalmente se discuten cuatro “tipos fundamnetales” de synapsidos, que en efecto son grupos sucesivamente sucesivamente anidados “Pelycosaurios” (parafilético, se usa para hablar de synapsidos basales) Carbonífero Superior- Terápsidos. Pérmico-Triásico Pérmico. Muy “reptilianos” aún Modificaciones craneales y posturales importantes Cynodontes. Pérmico superior, Triásico Mamíferos. Triásico Muy similares a mamíferos Oído interno tres huesos Dinastías synapsidas Meg Dynasty 1: Pelicosaurios del Pérmico inferior Meg Dynasty 2: Terápsidos del Pérmico superior-Triásico inferior Meg Dynasty 3: Mamíferos del Cenozoico Los primeros synápsidos (basales) se conocen colectivamente como un grupo “parafilético”, los Pelycosaurios (P en la figura) que excluyen a sus descendientes Terápsidos. Los pelycosaurios presentan abundantes dientes en el paladar. Reconstruc;on of Pangaea showing anteosaurid dinocephalians and platyoposaurid temnospondyles during the Middle Permian. Probable dispersal routes are indicated by red arrows.
    [Show full text]
  • Exact Distribution of Divergence Times from Fossil Ages and Tree Topologies Gilles Didier, Michel Laurin
    Exact distribution of divergence times from fossil ages and tree topologies Gilles Didier, Michel Laurin To cite this version: Gilles Didier, Michel Laurin. Exact distribution of divergence times from fossil ages and tree topologies. Systematic Biology, Oxford University Press (OUP), 2020, 69 (6), pp.1068-1087. 10.1101/490003. hal-01952736 HAL Id: hal-01952736 https://hal.archives-ouvertes.fr/hal-01952736 Submitted on 18 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Exact distribution of divergence times from fossil ages and tree topologies Gilles Didier1 and Michel Laurin2 1IMAG, Univ Montpellier, CNRS, Montpellier, France 2CR2P (Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements; UMR 7207), CNRS/MNHN/UPMC, Sorbonne Université, Muséum National d'Histoire Naturelle, Paris, France April 17, 2020 Abstract Being given a phylogenetic tree of both extant and extinct taxa in which the fossil ages are the only temporal information (namely, in which divergence times are considered unknown), we provide a method to compute the exact probability distribution of any divergence time of the tree with regard to any speciation (cladogenesis), extinction and fossilization rates under the Fossilized-Birth-Death model.
    [Show full text]
  • Callibrachion and Datheosaurus, Two Historical and Previously Mistaken Basal Caseasaurian Synapsids from Europe
    Callibrachion and Datheosaurus, two historical and previously mistaken basal caseasaurian synapsids from Europe FREDERIK SPINDLER, JOCELYN FALCONNET, and JÖRG FRÖBISCH Spindler, F., Falconnet, J., and Fröbisch, J. 2016. Callibrachion and Datheosaurus, two historical and previously mis- taken basal caseasaurian synapsids from Europe. Acta Palaeontologica Polonica 61 (3): 597–616. This study represents a re-investigation of two historical fossil discoveries, Callibrachion gaudryi (Artinskian of France) and Datheosaurus macrourus (Gzhelian of Poland), that were originally classified as haptodontine-grade sphenaco- dontians and have been lately treated as nomina dubia. Both taxa are here identified as basal caseasaurs based on their overall proportions as well as dental and osteological characteristics that differentiate them from any other major syn- apsid subclade. As a result of poor preservation, no distinct autapomorphies can be recognized. However, our detailed investigations of the virtually complete skeletons in the light of recent progress in basal synapsid research allow a novel interpretation of their phylogenetic positions. Datheosaurus might represent an eothyridid or basal caseid. Callibrachion shares some similarities with the more derived North American genus Casea. These new observations on Datheosaurus and Callibrachion provide new insights into the early diversification of caseasaurs, reflecting an evolutionary stage that lacks spatulate teeth and broadened phalanges that are typical for other caseid species. Along with Eocasea, the former ghost lineage to the Late Pennsylvanian origin of Caseasauria is further closed. For the first time, the presence of basal caseasaurs in Europe is documented. Key words: Synapsida, Caseasauria, Carboniferous, Permian, Autun Basin, France, Intra-Sudetic Basin, Poland. Frederik Spindler [[email protected]], Dinosaurier-Park Altmühltal, Dinopark 1, 85095 Denkendorf, Germany.
    [Show full text]
  • The Cranial Anatomy and Relationships of the Synapsid Varanosaurus (Eupelycosauria: Ophiacodontidae) from the Early Permian of Texas and Oklahoma
    ANNALS OF CARNEGIE MUSEUM VOL 64, NUM~. 2, ..... 99-133 12 MAy 1995 THE CRANIAL ANATOMY AND RELATIONSHIPS OF THE SYNAPSID VARANOSAURUS (EUPELYCOSAURIA: OPHIACODONTIDAE) FROM THE EARLY PERMIAN OF TEXAS AND OKLAHOMA DAVID S BERMAN Curator, Section of Vertebrate Paleontology ROBERT R. REISZI JOHN R. BoLT2 DIANE ScoTTI ABsTRACT The cranial anatomy of the Early Permian synapsid Varanosaurus is restudied on the basis of preY iously described specimens from Texas, most importantly the holotype of the type species V. aCUlirostris. and a recently discovered, excellently preserved specimen from Oklahoma. Cladistic analysis of the Eupelycosauria, using a data matrix 0(95 characters, provides the following hYPOthesis of relationships of VaraIJosaurus: I) VaraIJosaurus is a member of the family Ophiacodontidae; 2) of the ophiacodonlid genera included in the analysis, Varanosaurus and OpniacodOIJ share a more recent common ancestor than either does with the more primitive Arcna('()tnyris; and 3) a clade containing the progressively more derived taxa Edaphosauridae, H aplodus. and Sphenacodontoidea (Sphena- . codontidae plus Therapsida), together with Varanopseidae and Caseasauria, are progressively more distant outgroups or sister taxa to Ophiacodontidae. A revised diagnosis is given for VaralJosQurus. INTRODUCTION Published accounts of the Early Permian synapsid Varanosaurus have been limited almost entirely to rather brief descriptions based on a few poorly preserved andlor incomplete skeletons collected from the Lower Permian of north-central Texas. The holotype of the type species Varanosaurus acutirostris was described originally by Broili (1904) and consists of an incomplete articulated skeleton (BSPHM 1901 XV 20), including most importantly the greater portion of the skull, collected from the Arroyo Formation, Clear Fork Group.
    [Show full text]
  • The Carpus and Tarsus of the Early Permian Synapsid Sphenacodon Ferox (Eupelycosauria: Sphenacodontidae)
    Lucas, S.G. and Zeigler, K.E., eds., 2005, The Nonmarine Permian, New Mexico Museum of Natural History and Science Bulletin No. 30. 106 THE CARPUS AND TARSUS OF THE EARLY PERMIAN SYNAPSID SPHENACODON FEROX (EUPELYCOSAURIA: SPHENACODONTIDAE) AMY C. HENRICI1, DAVID S BERMAN1, SPENCER G. LUCAS2, ANDREW B. HECKERT2, LARRY F. RINEHART2, AND KATE E. ZEIGLER3 1Section of Vertebrate Paleontology, Carnegie Museum of Natural History, 4400 Forbes Avenue, Pittsburgh, PA 15213-4080; 2New Mexico Museum of Natural History & Science, 1801 Mountain Road, NW, Albuquerque, NM 87104; 3Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131 Abstract—The carpus and tarsus of the sphenacodontid synapsid Sphenacodon ferox are described in detail for the first time on the basis of nearly complete, loosely articulated examples from an incomplete, partially articu- lated skeleton from the Lower Permian El Cobre Canyon Formation of the Cutler Group of north-central New Mexico. On the one hand, the carpus and tarsus of S. ferox are compared to those of the more derived Dimetrodon and only member of Sphenacodontidae in which these structures are otherwise known adequately, and, on the other, to Haptodus, the sole member of the sister taxon of Sphenacodontoidea (Sphenacodontidae plus Therapsida). In order to recognize possible morphological trends in the carpus and tarsus within the combined clades of Haptodus and Sphenacodontidae, members of the sister clades Ophiacodontidae and Varanopseidae are utilized for outgroup comparison. INTRODUCTION the Lower Permian of New Mexico (Romer and Price, 1940; Eberth, 1985). The Late Pennsylvanian to Early Permian pelycosaurian-grade Weight of the matrix-encased specimens and the remoteness of or basal synapsid amniotes include seven genera of Sphenacodontidae, the Cardillo Quarry necessitated that the three specimens be removed some of which became a common component of Early Permian assem- as two plaster-jacketed blocks.
    [Show full text]
  • 622-2014Lectureweek3
    BIOLOGY 622 – FALL 2014 BASAL AMNIOTA - STRUCTURE AND PHYLOGENY WEEK – 3 EUPELYCOSAURIA S. S. SUMIDA INTRODUCTION Recall the Synapsida is one of the two great groups of the Amniota sensu stricto (the other being Reptilia). Within Synapsida, two subgroups are known, the Caseasauria and the Eupelycosauria. The term “Eupelycosauria” has been adopted in part as a reaction to the realization that “Pelycosauria” is technically a polyphyletic group, as it does not include all members of the group derived from it. So, notably, Eupelycosauria technically includes all therapsids and mammals as well. We are focusing only the basal-most members. As stated earlier, the familial designations of Romer and Price (1940) have in many cases held up, however, the interrelationships of those families have been subject to some change. MODERN INTERPRETATIONS OF PHYLOGENETIC RELATIONSHIPS OF BASAL SYNAPSIDS (I.E “PELYCOSAURS”) The work of Reisz (1980, 1986), Reisz et al (1992), and Berman et al (1995) have confirmed the validity pelycosaurian families, and placed them in two distinct groups: SYNAPSIDA Caseasauria Family Eothyrididae Family Caseidae Eupelycosauria Family Varanopseidae Family Ophiacodontidae Family Edaphosauridae Sphenacodontia Haptodus Palaeohatteria 1 Pantelosaurus Cutleria Sphenacodontoidea Family Sphenacodontidae Therpasida (leading to mammals) EUPLEYCOSAURIA: DEFINITION Eupelycosauria is defined as those taxa bearing all basal synapsid synapomorphies with the following unique features: (1) a long, narrow supratemporal. (2) The frontal contributes to at least one third of the dorsal orbital margin. Haptodus, Palaeohatteria, Pantelosaurus, and Cutleria are all genera that used to be placed in a distinct group known as the “Haptodontidae” or Haptodontinae”; but that has been shown to be a structural grade as opposed to a monophyletic family or subfamily.
    [Show full text]
  • The Many Faces of Synapsid Cranial Allometry
    Paleobiology, 45(4), 2019, pp. 531–545 DOI: 10.1017/pab.2019.26 Article The many faces of synapsid cranial allometry Isaac W. Krone , Christian F. Kammerer, and Kenneth D. Angielczyk Abstract.—Previous studies of cranial shape have established a consistent interspecific allometric pattern relating the relative lengths of the face and braincase regions of the skull within multiple families of mam- mals. In this interspecific allometry, the facial region of the skull is proportionally longer than the braincase in larger species. The regularity and broad taxonomic occurrence of this allometric pattern suggests that it may have an origin near the base of crown Mammalia, or even deeper in the synapsid or amniote forerun- ners of mammals. To investigate the possible origins of this allometric pattern, we used geometric morpho- metric techniques to analyze cranial shape in 194 species of nonmammalian synapsids, which constitute a set of successive outgroups to Mammalia. We recovered a much greater diversity of allometric patterns within nonmammalian synapsids than has been observed in mammals, including several instances similar to the mammalian pattern. However, we found no evidence of the mammalian pattern within Theroce- phalia and nonmammalian Cynodontia, the synapsids most closely related to mammals. This suggests that the mammalian allometric pattern arose somewhere within Mammaliaformes, rather than within nonmammalian synapsids. Further investigation using an ontogenetic series of the anomodont Diictodon feliceps shows that the pattern of interspecific allometry within anomodonts parallels the ontogenetic trajectory of Diictodon. This indicates that in at least some synapsids, allometric patterns associated with ontogeny may provide a “path of least resistance” for interspecific variation, a mechanism that we suggest produces the interspecific allometric pattern observed in mammals.
    [Show full text]
  • The University of Chicago Forelimb Shape, Disparity
    THE UNIVERSITY OF CHICAGO FORELIMB SHAPE, DISPARITY, AND FUNCTIONAL MORPHOLOGY IN THE DEEP EVOLUTIONARY HISTORY OF SYNAPSIDA A DISSERTATION SUBMITTED TO THE FACULTY OF THE DIVISION OF THE BIOLOGICAL SCIENCES AND THE PRITZKER SCHOOL OF MEDICINE IN CANDIDACY FOR THE DEGREE OF DOCTOR OF PHILOSOPHY GRADUATE PROGRAM IN INTEGRATIVE BIOLOGY BY JACQUELINE K LUNGMUS CHICAGO, ILLINOIS DECEMBER 2020 To all the animals I’ve called family. You have never failed to fascinate me, inspire me, and love me. It has always been about you. Max (Canis l. familiaris) Shy (Terrapene ornata) Speedy (Terrapene ornata) Augie (Canis l. familiaris) Sonic (Atelerix albiventris) Dahli (Equus f. caballus) Seymour (Canis l. familiaris) Gunther (Canis l. familaris) Juniper (Canis l. familiaris) TABLE OF CONTENTS LIST OF FIGURES ...................................................................................................................... v LIST OF TABLES ...................................................................................................................... vii ACKNOWLEDGMENTS ......................................................................................................... viii ABSTRACT .................................................................................................................................. xi CHAPTER 1 INRODUCTION .................................................................................................... 1 CHAPTER 2 ANTIQUITY OF FORELIMB ECOMORPHOLOGICAL DIVERSITY IN THE MAMMALIAN STEM LINEAGE (SYNAPSIDA)
    [Show full text]
  • ©2018 by the Society of Vertebrate Paleontology
    Poster Session IV (Saturday, October 20, 2018, 4:15 – 6:15 PM) vertebrates and present in amniote embryos, developmentally contributes to the adult vertebral column of mammals as the nucleus pulposus (NP) which is the internal part of PELYCOSAURIAN “LINEAGES”: A META-ANALYSIS OF THREE DECADES the intervertebral disk of mammals (intervertebral disk proper), but not present in birds. OF PHYLOGENETIC RESEARCH The NP has large cartilage cells of notochordal origin and is surrounded by the annulus WILSON, Winston M., New York City, NY, United States of America; ANGIELCZYK, fibrosus which consists of fibrocartilage. The intervertebral disk is situated between the Kenneth D., Field Museum, Chicago, IL, United States of America; PEECOOK, Brandon, cartilaginous endplates of the vertebral centra and is encased by ligaments connecting the Field Museum, Seattle, WA, United States of America; LLOYD, Graeme T., Macquarie vertebrae. University, Macquarie University, Australia Conventional wisdom holds that reptiles cannot have an intervertebral disk. However, Pelycosaur-grade synapsids comprise the first major radiation of Synapsida, and their based on histology and morphology, we posit that the intervertebral disk proper is not a phylogenetic relationships have been the subject of over three decades of research in a mammalian autapomorphy and show that an intervertebral disk is present in many fossil cladistic framework. In this time three major “lineages” of shared character-taxon matrices and a few recent reptile clades. On the one hand, we found soft tissue preservation in the have been created, each with distinct sets of characters and taxa which have been analyzed intervertebral spaces in the articulated anterior dorsal vertebral column of a Jurassic using different tree-construction methods.
    [Show full text]
  • Phylogeny of Paleozoic Limbed Vertebrates Reassessed Through Revision and Expansion of the Largest Published Relevant Data Matrix
    Phylogeny of Paleozoic limbed vertebrates reassessed through revision and expansion of the largest published relevant data matrix David Marjanovic1 and Michel Laurin2 1 Science Programme “Evolution and Geoprocesses”, Museum für Naturkunde—Leibniz Institute for Evolutionary and Biodiversity Research, Berlin, Germany 2 Centre de Recherches sur la Paléobiologie et les Paléoenvironnements (CR2P), Centre national de la Recherche scientifique (CNRS)/Muséum national d’Histoire naturelle (MNHN)/Sorbonne Université, Paris, France ABSTRACT The largest published phylogenetic analysis of early limbed vertebrates (Ruta M, Coates MI. 2007. Journal of Systematic Palaeontology 5:69–122) recovered, for example, Seymouriamorpha, Diadectomorpha and (in some trees) Caudata as paraphyletic and found the “temnospondyl hypothesis” on the origin of Lissamphibia (TH) to be more parsimonious than the “lepospondyl hypothesis” (LH)—though only, as we show, by one step. We report 4,200 misscored cells, over half of them due to typographic and similar accidental errors. Further, some characters were duplicated; some had only one described state; for one, most taxa were scored after presumed relatives. Even potentially continuous characters were unordered, the effects of ontogeny were not sufficiently taken into account, and data published after 2001 were mostly excluded. After these issues are improved— we document and justify all changes to the matrix—but no characters are added, we find (Analysis R1) much longer trees with, for example, monophyletic Caudata, Diadectomorpha and (in some trees) Seymouriamorpha; Ichthyostega either crownward or rootward of Acanthostega; and Anthracosauria either crownward or Submitted 16 January 2016 Accepted 12 August 2018 rootward of Temnospondyli. The LH is nine steps shorter than the TH (R2; Published 4 January 2019 constrained) and 12 steps shorter than the “polyphyly hypothesis” (PH—R3; Corresponding author constrained).
    [Show full text]
  • And Its Phylogenetic Affinities
    Palaeontologia Electronica palaeo-electronica.org New material of Alierasaurus ronchii (Synapsida, Caseidae) from the Permian of Sardinia (Italy), and its phylogenetic affinities Marco Romano, Ausonio Ronchi, Simone Maganuco, and Umberto Nicosia ABSTRACT New characters of the giant caseid Alierasaurus ronchii are described here based on material recovered from the type locality in the Permian deposits of Cala del Vino Formation (Sardinia NW) and additional preparation of the previously collected mate- rial. All new described osteological elements are characterized by the same state of preservation and, given the absence of double elements and the total compatibility in absolute size, the new material can be attributed without doubt to the holotypic individ- ual of A. ronchii. Highly diagnostic material includes a caudal neural spine with a broad bifid distal termination. This represents a synapomorphy characterizing the more derived caseids, thus fully confirming the attribution of the Sardinian specimen to Caseidae. Also the other vertebral material and newly collected ribs show a typical caseid structure, fully consistent with the previously published material. Despite the highly partial nature of Alierasaurus, the taxon was included in a recent phylogenetic analysis of caseids to investigate its phylogenetic position within the monophyletic Caseasauria. Alierasaurus falls as the sister taxon of Cotylorhynchus, and is autapo- morphic in the general construction of MT-IV and proximal phalanx IV-I. The absolute size of the newly recovered material confirms a gigantic body size for Alierasaurus, comparable, if not greater, to that of the huge North American species Cotylorhynchus hancocki (up to 6 m in length). Such gigantic adult body size, closely correlated to its herbivorous lifestyle, must have been selected during evolution of caseids, leading to substantial advantages in terms of fitness.
    [Show full text]