Separating Sexual Dimorphism from Other Morphological Variation in a Specimen Complex of Fossil Marine Reptiles (Reptilia, Ichthyosauriformes, Chaohusaurus)
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Ichthyosaur Species Valid Taxa Acamptonectes Fischer Et Al., 2012: Acamptonectes Densus Fischer Et Al., 2012, Lower Cretaceous, Eng- Land, Germany
Ichthyosaur species Valid taxa Acamptonectes Fischer et al., 2012: Acamptonectes densus Fischer et al., 2012, Lower Cretaceous, Eng- land, Germany. Aegirosaurus Bardet and Fernández, 2000: Aegirosaurus leptospondylus (Wagner 1853), Upper Juras- sic–Lower Cretaceous?, Germany, Austria. Arthropterygius Maxwell, 2010: Arthropterygius chrisorum (Russell, 1993), Upper Jurassic, Canada, Ar- gentina?. Athabascasaurus Druckenmiller and Maxwell, 2010: Athabascasaurus bitumineus Druckenmiller and Maxwell, 2010, Lower Cretaceous, Canada. Barracudasauroides Maisch, 2010: Barracudasauroides panxianensis (Jiang et al., 2006), Middle Triassic, China. Besanosaurus Dal Sasso and Pinna, 1996: Besanosaurus leptorhynchus Dal Sasso and Pinna, 1996, Middle Triassic, Italy, Switzerland. Brachypterygius Huene, 1922: Brachypterygius extremus (Boulenger, 1904), Upper Jurassic, Engand; Brachypterygius mordax (McGowan, 1976), Upper Jurassic, England; Brachypterygius pseudoscythius (Efimov, 1998), Upper Jurassic, Russia; Brachypterygius alekseevi (Arkhangelsky, 2001), Upper Jurassic, Russia; Brachypterygius cantabridgiensis (Lydekker, 1888a), Lower Cretaceous, England. Californosaurus Kuhn, 1934: Californosaurus perrini (Merriam, 1902), Upper Triassic USA. Callawayia Maisch and Matzke, 2000: Callawayia neoscapularis (McGowan, 1994), Upper Triassic, Can- ada. Caypullisaurus Fernández, 1997: Caypullisaurus bonapartei Fernández, 1997, Upper Jurassic, Argentina. Chaohusaurus Young and Dong, 1972: Chaohusaurus geishanensis Young and Dong, 1972, Lower Trias- sic, China. -
Exceptional Vertebrate Biotas from the Triassic of China, and the Expansion of Marine Ecosystems After the Permo-Triassic Mass Extinction
Earth-Science Reviews 125 (2013) 199–243 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Exceptional vertebrate biotas from the Triassic of China, and the expansion of marine ecosystems after the Permo-Triassic mass extinction Michael J. Benton a,⁎, Qiyue Zhang b, Shixue Hu b, Zhong-Qiang Chen c, Wen Wen b, Jun Liu b, Jinyuan Huang b, Changyong Zhou b, Tao Xie b, Jinnan Tong c, Brian Choo d a School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK b Chengdu Center of China Geological Survey, Chengdu 610081, China c State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, China d Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China article info abstract Article history: The Triassic was a time of turmoil, as life recovered from the most devastating of all mass extinctions, the Received 11 February 2013 Permo-Triassic event 252 million years ago. The Triassic marine rock succession of southwest China provides Accepted 31 May 2013 unique documentation of the recovery of marine life through a series of well dated, exceptionally preserved Available online 20 June 2013 fossil assemblages in the Daye, Guanling, Zhuganpo, and Xiaowa formations. New work shows the richness of the faunas of fishes and reptiles, and that recovery of vertebrate faunas was delayed by harsh environmental Keywords: conditions and then occurred rapidly in the Anisian. The key faunas of fishes and reptiles come from a limited Triassic Recovery area in eastern Yunnan and western Guizhou provinces, and these may be dated relative to shared strati- Reptile graphic units, and their palaeoenvironments reconstructed. -
Preliminary Report on Ichthyopterygian Elements from the Early Triassic (Spathian) of Spitsbergen
NORWEGIAN JOURNAL OF GEOLOGY Vol 98 Nr. 2 https://dx.doi.org/10.17850/njg98-2-07 Preliminary report on ichthyopterygian elements from the Early Triassic (Spathian) of Spitsbergen Christina Pokriefke Ekeheien1, Lene Liebe Delsett1, Aubrey Jane Roberts2 & Jørn Harald Hurum1 1Natural History Museum, University of Oslo, Pb.1172 Blindern, N–0318 Oslo, Norway. 2Natural History Museum, London, United Kingdom. E-mail corresponding author (Lene Liebe Delsett): [email protected] Jaw elements of Omphalosaurus sp. are described from the Early Triassic (Spathian) of Marmierfjellet, Spitsbergen. The elements are from the Grippia and the Lower Saurian niveaus in the Vendomdalen Member of the Vikinghøgda Formation. In the Grippia niveau a bonebed was excavated in 2014–15 and a large number of ichthyopterygian elements were recovered. Together with the omphalosaurian jaw elements a collection of large vertebral centra were recognized as different from the smaller Grippia centra and more than 200 large vertebral centra are referred to Ichthyopterygia indet. and tentatively assigned to regions of the vertebral column. We refrain from further assignment due to the systematic position and the difficulty of defining criteria for recognizing postcranial elements of Omphalosaurus. Keywords: Ichthyopterygia; Spitsbergen; Triassic; Omphalosaurus; Grippia bonebed Electronic Supplement A: Supplementary Material Received 23. November 2017 / Accepted 21. August 2018 / Published online 4. October 2018 Introduction The skull material is referred to Omphalosaurus based on the distinct tooth enamel, dome-shaped teeth and The Early Triassic deposits of Svalbard contain large an overall similar morphology to other specimens amounts of fish, amphibian and reptilian fossils from the of the genus (Sander & Faber, 2003). -
Now, on to Mesozoic Marine Reptiles
Now, on to Mesozoic Marine Reptiles NOT DINOSAURS! • They are reptiles, but some have adopted different skull fenestration • “Euryapsid” and “Anapsid” conditions are likely modified Diapsids • First reptiles returned to the sea in the Permian (Mesosaurus) How they are related: Sauropterygia Mosasauridae Thalattosuchia Dinosauria Phytosauria Lepidosauromorpha Crurotarsi Prolacertiformes Archosauromorpha Thalattosauriformes? Ichthyosauromorpha Sauria Claudiosaurus Neodiapsida Morphology • 4 basic body plans (Baupläne): (a) Thunniform advanced ichthyosaur (b) Long neck/small head plesiosaur (elasmosaur) (c) Short neck/big head pliosaur (d) Undulatory mosasaur (and basal ichthyosaur) • + “functional group 3” after Robert L. Carroll (“swimming lizards”) Morphological Trends • Limbs become rigid, often with hyperphalangy (many phalanges) • Polydactyly in ichthyosaurs Morphological Trends • (A) Merriamia (basal ichthyosaur) manus • (B) Opthalmosaurus (Jurassic ichthyosaur) manus • (C) Elasmosaurus (Cretaceous plesiosaur) manus • (D) Nothosaur pes • (E) Mosasaur pes Morphological Trends • Thoracic stiffening a usual trend • Lateral flexion directed posteriorly, or propulsion moved paraxially Carrier’s Constraint • Because of their sprawling gait, *GASP!* reptiles cannot breathe and run at the same time Ahhh… • Same applies to marine reptiles with lateral flexion (they breathe air!) *GASP!* • Solved by moving propulsion posteriorly, stiffening thorax, or moving limbs independently of spine Triassic Seas • Pangea beginning to break up • Marine -
Terrestrial Origin of Viviparity in Mesozoic Marine Reptiles Indicated by Early Triassic Embryonic Fossils
Terrestrial Origin of Viviparity in Mesozoic Marine Reptiles Indicated by Early Triassic Embryonic Fossils Ryosuke Motani1, Da-yong Jiang2,3*, Andrea Tintori4, Olivier Rieppel5, Guan-bao Chen6 1 Department of Earth and Planetary Sciences, University of California, Davis, Davis, California, United States of America, 2 Laboratory of Orogenic Belt and Crustal Evolution, Ministry of Education, Department of Geology and Geological Museum, Peking University, Beijing, People’s Republic of China, 3 State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences), Nanjing, Jiangsu Province, People’s Republic of China, 4 Dipartimento di Scienze della Terra, Universita` degli Studi di Milano, Via Mangiagalli, Milano, Italy, 5 Center of Integrative Research, The Field Museum, Chicago, Illinois, United States of America, 6 Department of Research, Anhui Geological Museum, Hefei, Anhui Province, People’s Republic of China Abstract Viviparity in Mesozoic marine reptiles has traditionally been considered an aquatic adaptation. We report a new fossil specimen that strongly contradicts this traditional interpretation. The new specimen contains the oldest fossil embryos of Mesozoic marine reptile that are about 10 million years older than previous such records. The fossil belongs to Chaohusaurus (Reptilia, Ichthyopterygia), which is the oldest of Mesozoic marine reptiles (ca. 248 million years ago, Early Triassic). This exceptional specimen captures an articulated embryo in birth position, with its skull just emerged from the maternal pelvis. Its headfirst birth posture, which is unlikely to be a breech condition, strongly indicates a terrestrial origin of viviparity, in contrast to the traditional view. The tail-first birth posture in derived ichthyopterygians, convergent with the conditions in whales and sea cows, therefore is a secondary feature. -
Supplementary Information Phylogeny of the Ichthyopterygia Incorporating
Supplementary Information Phylogeny of the Ichthyopterygia incorporating the recent discoveries from South China CHENG JI,1,2 DA-YONG JIANG,*, 2, 3 RYOSUKE MOTANI,4 OLIVIER RIEPPEL,5 WEI-CHENG HAO,2 and ZUO-YU SUN2 1Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, People’s Republic of China, [email protected]; 2Laboratory of Orogenic Belt and Crustal Evolution, Ministry of Education; Department of Geology and Geological Museum, Peking University, Beijing 100871, People’s Republic of China, [email protected]; 3State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, People’s Republic of China; 4Department of Geology, University of California, Davis, California 95616, U.S.A., [email protected]; 5Section of Earth Sciences, Integrative Research Center, The Field Museum, Chicago, Illinois 60605-2496, U.S.A., [email protected] RH: JI ET AL.—PHYLOGENY OF THE ICHTHYOPTERYGIA *Corresponding author INGROUP TAXA SELECTION We aim at conducting a comprehensive phylogengetic analysis incorporating the recent discoveries during the past fifteen years. However, some genera are known from only partial skeleton and many characters are coded as “?” (Table 1S). Therefore, we provide two analyses in the text based on different combinations of ingroup taxa. In the first analysis, all the taxa in Table 1S are included and results in many polytomies. In the second analysis, the taxa which can not be coded for more than 1/3 (54.3 characters) are removed and the topology is highly resolved. Table S1. -
Effects of Body Plan Evolution on the Hydrodynamic Drag And
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Birmingham Research Portal University of Birmingham Effects of body plan evolution on the hydrodynamic drag and energy requirements of swimming in ichthyosaurs Gutarra, Susana; Moon, Benjamin; Rahman, Imran; Palmer, Colin; Lautenschlager, Stephan; Brimacombe, Alison; Benton, Michael DOI: 10.1098/rspb.2018.2786 License: Creative Commons: Attribution (CC BY) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Gutarra, S, Moon, B, Rahman, I, Palmer, C, Lautenschlager, S, Brimacombe, A & Benton, M 2019, 'Effects of body plan evolution on the hydrodynamic drag and energy requirements of swimming in ichthyosaurs', Royal Society of London. Proceedings B. Biological Sciences, vol. 286, no. 1898, 286. https://doi.org/10.1098/rspb.2018.2786 Link to publication on Research at Birmingham portal 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. -
Resetting the Evolution of Marine Reptiles at the Triassic-Jurassic Boundary
Resetting the evolution of marine reptiles at the Triassic-Jurassic boundary Philippa M. Thorne, Marcello Ruta, and Michael J. Benton1 School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, United Kingdom Edited by Neil Shubin, University of Chicago, Chicago, IL, and accepted by the Editorial Board March 30, 2011 (received for review December 18, 2010) Ichthyosaurs were important marine predators in the Early Jurassic, life, swimming with lateral undulations of the tail and steering and an abundant and diverse component of Mesozoic marine with elongate fore paddles and producing live young at sea. ecosystems. Despite their ecological importance, however, the After the Tr-J bottleneck, ichthyosaurs apparently did not Early Jurassic species represent a reduced remnant of their former achieve such diversity of form but nonetheless recovered suffi- significance in the Triassic. Ichthyosaurs passed through an evolu- ciently to be the dominant marine predators of the Early Ju- tionary bottleneck at, or close to, the Triassic-Jurassic boundary, rassic, after which they dwindled in diversity through the Middle which reduced their diversity to as few as three or four lineages. and Late Jurassic and much of the Cretaceous until they dis- Diversity bounced back to some extent in the aftermath of the appeared at the end of the Cenomanian, ∼100 Ma, after having end-Triassic mass extinction, but disparity remained at less than had a significant role in Mesozoic seas for 150 Myr. one-tenth of pre-extinction levels, and never recovered. The group In this study, we concentrate on disparity (morphological fi remained at low diversity and disparity for its nal 100 Myr. -
Repeated Evolution of Durophagy During Ichthyosaur Radiation After
www.nature.com/scientificreports OPEN Repeated evolution of durophagy during ichthyosaur radiation after mass extinction indicated by hidden dentition Jian-dong Huang1, Ryosuke Motani2 ✉ , Da-yong Jiang3,4, Xin-xin Ren1, Andrea Tintori5, Olivier Rieppel6, Min Zhou3, Yuan-chao Hu1 & Rong Zhang1 Marine tetrapods quickly diversifed and were established as marine top predators after the end- Permian Mass extinction (EPME). Ichthyosaurs were the forerunner of this rapid radiation but the main drivers of the diversifcation are poorly understood. Cartorhynchus lenticarpus is a basal ichthyosauriform with the least degree of aquatic adaptation, holding a key to identifying such a driver. The unique specimen appeared edentulous based on what was exposed but a CT scanning revealed that the species indeed had rounded teeth that are nearly perpendicular to the jaw rami, and thus completely concealed in lateral view. There are three dental rows per jaw ramus, and the root lacks infoldings of the dentine typical of ichthyopterygians. The well-developed and worn molariform dentition with three tooth rows supports the previous inference that the specimen is not of a juvenile. The premaxilla and the corresponding part of the dentary are edentulous. Molariform dentition evolved three to fve times independently within Ichthyosauriformes in the Early and Middle Triassic. Convergent exploitation of hard-shelled invertebrates by diferent subclades of ichthyosauriforms likely fueled the rapid taxonomic diversifcation of the group after EPME. Many components of the modern ecosystem emerged in the Triassic, afer the EPME. One of them is marine tetrapods, air-breathing vertebrates that invaded the sea from land, such as marine mammals and reptiles1. -
A Detailed Lower Triassic Conodont Biostratigraphy and Its Implications for the GSSP Candidate of the Induan–Olenekian Boundary in Chaohu, Anhui Province
Available online at www.sciencedirect.com Progress in Natural Science 18 (2008) 79–90 A detailed Lower Triassic conodont biostratigraphy and its implications for the GSSP candidate of the Induan–Olenekian boundary in Chaohu, Anhui Province Laishi Zhao a,*, Jinnan Tong a, Zhiming Sun a,b, Michael J. Orchard c a State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China b Institute of Geomechanics, Chinese Academy of Geological Science, Beijing 100081, China c Geological Survey of Canada, 101-605 Robson Street, Vancouver, Canada V6B5J3 Received 26 February 2007; received in revised form 24 April 2007; accepted 4 July 2007 Abstract Chaohu is located in a deep part of carbonate ramp on the Lower Yangtze Block, which belonged to the low-latitude eastern Tethyan archipelago during the Early Triassic. Fossils were very rich in the Lower Triassic of Chaohu. Bivalves, ammonoids, conodonts were very common throughout the Lower Triassic, while fish fossils were generally rich in some beds of the upper part. It is one of the most typical sections for the Early Triassic chronostratigraphy in the world. Although various fossils had been studied in the 1980s and 1990s, recent studies based upon new and more detailed collections from the Lower Triassic of Chaohu showed that the conodont zonation needs revision. We collected Lower Triassic conodont fossils from continuous sections of the West Pingdingshan, North Pingdingshan and South Majiashan, Chaohu, Anhui Province, and updated zonations were made for each section. Eight conodont zones have been dis- tinguished. They are, in ascending order, Hindeodus typicalis zone, Neogondolella krystyni zone, Neospathodus kummeli zone, Neospath- odus dieneri zone, Neospathodus waageni zone, Neospathodus pingdingshanensis zone, Neospathodus homeri zone, and Neospathodus anhuinensis zone. -
A New Lower Triassic Ichthyopterygian Assemblage from Fossil Hill, Nevada
A peer-reviewed version of this preprint was published in PeerJ on 26 January 2016. View the peer-reviewed version (peerj.com/articles/1626), which is the preferred citable publication unless you specifically need to cite this preprint. Kelley NP, Motani R, Embree P, Orchard MJ. 2016. A new Lower Triassic ichthyopterygian assemblage from Fossil Hill, Nevada. PeerJ 4:e1626 https://doi.org/10.7717/peerj.1626 A new Lower Triassic ichthyopterygian assemblage from Fossil Hill, Nevada Neil P Kelley, Ryosuke Motani, Patrick Embree, Michael J Orchard We report a new ichthyopterygian assemblage from Lower Triassic horizons of the Prida Formation at Fossil Hill in central Nevada. Although fragmentary, the specimens collected so far document a diverse fauna. One partial jaw exhibits isodont dentition with blunt tipped, mesiodistally compressed crowns and striated enamel. These features are shared with the Early Triassic genus Utatsusaurus known from coeval deposits in Japan and British Columbia. An additional specimen exhibits a different dentition characterized by relatively small, rounded posterior teeth resembling other Early Triassic ichthyopterygians particularly Grippia. This Nevada assemblage marks a southward latitudinal extension for Early Triassic ichthyopterygians along the eastern margin of Panthalassa and indicates repeated circum-oceanic dispersal events in Early Triassic ichthyopterygians. PeerJ PrePrints | https://dx.doi.org/10.7287/peerj.preprints.1447v1 | CC-BY 4.0 Open Access | rec: 23 Oct 2015, publ: 23 Oct 2015 1 A new Lower -
No. 208,5Tuttgrrr
i Rirnrr Italiana di Paleonrologir e Stratiqraiia rolunìe I lO no- pp. +79-+92 l I I July 200.{ FIRST RECORD OF THE RARE MARINE REPTILE THOLODUS SCHMIDI FROM THE MIDDLE TRIASSIC OF THE SOUTHERN ALPS FABIO MARCO DALLA VECCHIA' Rceì*d ,ll,trcb 27, 2Aú; n(elted August 13, 2A03 Kq tt.ords: Tholodu: trxonomic ,rflinin rrnd rangc. Ichrhl'c> saurii. denrition. A bstract . Tholodn s schnizli. r rrre nnrine reptile of dcÌltcd affinity rnd rvith a pcculiar durophagors dcntirio, is tor the firsr rimc recordcd outsidc the l\'luschelkalk B:rs;n ot Cenrrrl Europe. Parts ofa rnandibular rxnrus and a nlixille, borh bearing rcerh rnd nearly uncrushcd. have bcen found in the upper Anisinn (B.rl:rronicus Subzone) ol northcastern ftalr'. Thc toorh inrplantation is reìatirclv complcx. *ìth borh "alvcolate" and "rnk\'losed" tcc!h. Disùnicul,ìred posrcrinìrìl boncs of an ichthyosnur Plan Coces l hrre been found cÌo* ro, btrr nor in arriculrr rssociarion rith. rhe den- a_. rigerrrus boncs oi Tholodr:. -fhe humerus lcscmbìes rhat oi immaturc Cuel d. Rinch ' .{f individurls of rhe Chinese genrs Chaahwdul'us. This associrtion, rnd .1 sorne feÀturcs of teeth rnd dcntigerous bones, suggests ùr Tholo,lts nighr be r grippiid ichrhlosrur. Rias:unto. Thokxlus scbridt, un rrro rettìle nr.rrino di discuss.r aiiiniti tassononrìca c con uniì denrarurr durofrg:r peculi:rrc', è sccna- lato pcr la prìnrir volrr al di fuorj del Bacino del Muschelkrlk dell'l-u- ropr Ccntmle. È st.rro rinvenuto ncll'Anisico superiore (Sottozon:r a ( Balarcnicus) dcll ltalir nordorienr.rle rd è r:rppresentrro dr un rrnro mandibol:rre incompleto e da un nrascelliìre, enrrenlbi denrigeri e poco Udine ./ Rt ar complessi.