Colobops: a Juvenile Rhynchocephalian Reptile (Lepidosauromorpha), Not a Diminutive Archosauromorph with an Unusually Strong Bite
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Macroevolutionary Patterns in Rhynchocephalia: Is the Tuatara (Sphenodon Punctatus) a Living Fossil? Palaeontology, 60(3), 319-328
Herrera Flores, J., Stubbs, T., & Benton, M. (2017). Macroevolutionary patterns in Rhynchocephalia: is the tuatara (Sphenodon punctatus) a living fossil? Palaeontology, 60(3), 319-328. DOI: 10.1111/pala.12284 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1111/pala.12284 Link to publication record in Explore Bristol Research PDF-document University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/pure/about/ebr-terms.html [Palaeontology, 2017, pp. 1–10] MACROEVOLUTIONARY PATTERNS IN RHYNCHOCEPHALIA: IS THE TUATARA (SPHENODON PUNCTATUS) A LIVING FOSSIL? by JORGEA.HERRERA-FLORES , THOMAS L. STUBBS and MICHAEL J. BENTON School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, UK; jorge.herrerafl[email protected], [email protected], [email protected] Typescript received 4 July 2016; accepted in revised form 19 January 2017 Abstract: The tuatara, Sphenodon punctatus, known from since the Triassic, rhynchocephalians had heterogeneous rates 32 small islands around New Zealand, has often been noted of morphological evolution and occupied wide mor- as a classic ‘living fossil’ because of its apparently close phospaces during the Triassic and Jurassic, and these then resemblance to its Mesozoic forebears and because of a long, declined in the Cretaceous. In particular, we demonstrate low-diversity history. This designation has been disputed that the extant tuatara underwent unusually slow lineage because of the wide diversity of Mesozoic forms and because evolution, and is morphologically conservative, being located of derived adaptations in living Sphenodon. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Two Kinds of Halo Gas Identified Small Companions for Early Dinosaurs
N~A~ru~~~v~0=L.~m~12~JMru~~AA~Y~I~~~ ___________________ NEWSANDVI8NS ____________________________________ 1=11 stars is observed are considerably different Galaxy structure from these expected for corotating gas. Evidently, these gas clouds have large peculiar velocities with respect to a co Two kinds of halo gas identified rotating halo. The data are qualitatively from Joel Bregman consistent with features of a corona that rotates more slowly than the disk and of ALTHOUGH most of the cool gas in our beyond a height of 3,000 light years. galactic fountain models. More data are galaxy lies in the galactic disk, it is not However, little neutral gas exists further needed before the various models can be entirely confined there and the study of gas than 6,000 light years from the disk. Albert tested critically and more studies along the above and below the disk (halo gas) has has added to our understanding by com lines of Albert's would be valuable. 0 been an especially vigorous area of research paring the difference in absorption for during the past few years. Unfortunately, it pairs of stars, one of which is just above the Joel Bregman is in the department ofphysics at has frequently been difficult to galactic disk and the other in the halo. She New York University. discriminate between disk and halo gas, for shows that the halo is rich in gas and it is not possible to determine distances to distinguishes between two types of neutral I. Mhort, C,E. Aslrophys. J. 271,509(1983). gas clouds and we can only look at the halo halo gas: a layer of gas similar to disk gas 2. -
The Terrestrial Fauna of the Late Triassic Pant-Y-Ffynnon Quarry Fissures, South Wales, UK and a New Species of Clevosaurus (Lepidosauria: Rhynchocephalia)
Keeble, E., Whiteside, D. I., & Benton, M. J. (2018). The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures, South Wales, UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia). Proceedings of the Geologists' Association. https://doi.org/10.1016/j.pgeola.2017.11.001 Peer reviewed version License (if available): Other Link to published version (if available): 10.1016/j.pgeola.2017.11.001 Link to publication record in Explore Bristol Research PDF-document This is the author accepted manuscript (AAM). The final published version (version of record) is available online via Elsevier at https://www.sciencedirect.com/science/article/pii/S0016787817301529?via%3Dihub#!. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ 1 The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures, South Wales, UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia) Emily Keeble, David I. Whiteside, Michael J. Benton* School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UK ABSTRACT Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. -
A New Sphenodontian (Lepidosauria: Rhynchocephalia)
View metadata, citation and similar papersDownloaded at core.ac.uk from http://rspb.royalsocietypublishing.org/ on February 13, 2017 brought to you by CORE provided by CONICET Digital A new sphenodontian (Lepidosauria: Rhynchocephalia) from the Late Triassic of Argentina and the early origin of the herbivore opisthodontians rspb.royalsocietypublishing.org Ricardo N. Martı´nez1, Cecilia Apaldetti1,2, Carina E. Colombi1,2, Angel Praderio1, Eliana Fernandez1,2, Paula Santi Malnis1,2, 1,2 1 1 Research Gustavo A. Correa , Diego Abelin and Oscar Alcober 1Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan, Avenida Espan˜a 400 Norte, Cite this article: Martı´nez RN, Apaldetti C, 5400 San Juan, Argentina Colombi CE, Praderio A, Fernandez E, Malnis 2Consejo Nacional de Investigaciones Cientı´ficas y Te´cnicas, CONICET, Buenos Aires, Argentina PS, Correa GA, Abelin D, Alcober O. 2013 A new sphenodontian (Lepidosauria: Rhyncho- Sphenodontians were a successful group of rhynchocephalian reptiles that dominated the fossil record of Lepidosauria during the Triassic and Jurassic. cephalia) from the Late Triassic of Argentina Although evidence of extinction is seen at the end of the Laurasian Early and the early origin of the herbivore Cretaceous, they appeared to remain numerically abundant in South America opisthodontians. Proc R Soc B 280: 20132057. until the end of the period. Most of the known Late Cretaceous record in http://dx.doi.org/10.1098/rspb.2013.2057 South America is composed of opisthodontians, the herbivorous branch of Sphenodontia, whose oldest members were until recently reported to be from the Kimmeridgian–Tithonian (Late Jurassic). Here, we report a new sphenodontian, Sphenotitan leyesi gen. -
Testing the Relationship Between Marine Transgression and Evolving Island Palaeogeography Using 3D GIS: an Example from the Late Triassic of SW England
Downloaded from http://jgs.lyellcollection.org/ at University of Bristol Library on April 27, 2021 Research article Journal of the Geological Society https://doi.org/10.1144/jgs2020-158 | Vol. 178 | 2021 | jgs2020-158 Testing the relationship between marine transgression and evolving island palaeogeography using 3D GIS: an example from the Late Triassic of SW England Jack Lovegrove1, Andrew J. Newell2, David I. Whiteside1,3 and Michael J. Benton1* 1 School of Earth Sciences, University of Bristol, Bristol BS8 1TQ, UK 2 British Geological Survey, Maclean Building, Crowmarsh Gifford, Wallingford OX10 8BB, UK 3 The Natural History Museum, Cromwell Road, London SW7 5BD, UK DIW, 0000-0003-1619-747X; MJB, 0000-0002-4323-1824 * Correspondence: [email protected] Abstract: The Rhaetian transgression marked a major change in landscape. The Permian and Triassic had been a time of terrestrial conditions across Europe, including much of mainland UK, as well as the North Sea and Irish Sea, represented by red bed clastic successions. Seas flooded across Europe at 205.7 Ma and the shift from terrestrial to marine environments is marked in the UK by the switch from the red beds of the Mercia Mudstone Group to the black mudstones and shelly limestones and sandstones of the Penarth Group. The area around Bristol was marked by a complex landscape in which an archipelago of islands of Carboniferous limestone was formed in the new shallow seas. The application of new methods in geographical information systems allows a detailed exploration of a number of conformable surfaces, the unconformity between the underlying Paleozoic rocks and the overlying Mesozoic strata, as well as levels within the latest Triassic sediments, marking the advance of the sea and interactions with the coeval tectonics, which caused some islands to rise and some basins to descend. -
Vertebrates from the Late Triassic Thecodontosaurus-Bearing Rocks Of
Proceedings of the Geologists’ Association 125 (2014) 317–328 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola Vertebrates from the Late Triassic Thecodontosaurus-bearing rocks of Durdham Down, Clifton (Bristol, UK) Davide Foffa *, David I. Whiteside, Pedro A. Viegas, Michael J. Benton School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK A R T I C L E I N F O A B S T R A C T Article history: Since the discovery of the basal sauropodomorph dinosaur Thecodontosaurus in the 1830s, the associated Received 12 October 2013 fauna from the Triassic fissures at Durdham Down (Bristol, UK) has not been investigated, largely Received in revised form 3 February 2014 because the quarries are built over. Other fissure sites around the Bristol Channel show that dinosaurs Accepted 7 February 2014 represented a minor part of the fauna of the Late Triassic archipelago. Here we present data on Available online 16 April 2014 microvertebrates from the original Durdham Down fissure rocks, which considerably expand the taxonomic diversity of the island fauna, revealing that it was dominated by the sphenodontian Keywords: Diphydontosaurus, and that archosauromorphs, including sphenosuchian crocodylomorphs, coelophy- Late Triassic soid theropods, and the basal sauropodomorph Thecodontosaurus, were diverse. Importantly, a few fish Fissure fills Archosaurs teeth provide new information about the debated age of the fissure deposit, which is identified as lower Sphenodontians Rhaetian. Thecodontosaurus had been assigned an age range over 20–25 Myr of the Late Triassic, so this Durdham Down narrower age determination (209.5–204 Myr) is important for studies of early dinosaurian evolution. -
Is the Tuatara (Sphenodon Punctatus) a Living Fossil? Palaeontology, 60(3), 319-328
Herrera Flores, J., Stubbs, T., & Benton, M. (2017). Macroevolutionary patterns in Rhynchocephalia: is the tuatara (Sphenodon punctatus) a living fossil? Palaeontology, 60(3), 319-328. https://doi.org/10.1111/pala.12284 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1111/pala.12284 Link to publication record in Explore Bristol Research PDF-document University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ [Palaeontology, 2017, pp. 1–10] MACROEVOLUTIONARY PATTERNS IN RHYNCHOCEPHALIA: IS THE TUATARA (SPHENODON PUNCTATUS) A LIVING FOSSIL? by JORGEA.HERRERA-FLORES , THOMAS L. STUBBS and MICHAEL J. BENTON School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, UK; jorge.herrerafl[email protected], [email protected], [email protected] Typescript received 4 July 2016; accepted in revised form 19 January 2017 Abstract: The tuatara, Sphenodon punctatus, known from since the Triassic, rhynchocephalians had heterogeneous rates 32 small islands around New Zealand, has often been noted of morphological evolution and occupied wide mor- as a classic ‘living fossil’ because of its apparently close phospaces during the Triassic and Jurassic, and these then resemblance to its Mesozoic forebears and because of a long, declined in the Cretaceous. In particular, we demonstrate low-diversity history. This designation has been disputed that the extant tuatara underwent unusually slow lineage because of the wide diversity of Mesozoic forms and because evolution, and is morphologically conservative, being located of derived adaptations in living Sphenodon. -
(Lepidosauria: Rhynchocephalia) From
Proceedings of the Geologists’ Association 126 (2015) 402–416 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola A distinctive Late Triassic microvertebrate fissure fauna and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia) from Woodleaze Quarry, Gloucestershire, UK Catherine G. Klein *, David I. Whiteside, Victor Selles de Lucas, Pedro A. Viegas, Michael J. Benton School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK A R T I C L E I N F O A B S T R A C T Article history: During the Late Triassic and Early Jurassic, diverse terrestrial vertebrates were preserved in fissures Received 13 November 2014 formed in Carboniferous Limestone on an island archipelago spanning from the south of Wales to the Received in revised form 25 April 2015 north and south of Bristol. Here we report the faunas of two new fissures in Woodleaze quarry, near to Accepted 3 May 2015 Tytherington quarry, where the vertebrate fauna is already well known. The new site extends the lateral Available online 3 June 2015 distribution of fissures in this vicinity to over 900 m, and fissures sampled along that transect show a southerly change in the dominant species and a reduction in diversity. The Woodleaze fissure fauna is Keywords: nearly monofaunal, comprising >98% of a new Clevosaurus species, as well as some Diphydontosaurus Late Triassic fragments, a possible undescribed lepidosaur and a few fish fossils. The new clevosaur is distinguished Fissure fills Sphenodontians from the type species Clevosaurus hudsoni by its dentition, and by being smaller (average long bones are Clevosaurus 40–80% the length of C. -
IS the TUATARA (SPHENODON PUNCTATUS) a LIVING FOSSIL? by JORGEA.HERRERA-FLORES , THOMAS L
[Palaeontology, 2017, pp. 1–10] MACROEVOLUTIONARY PATTERNS IN RHYNCHOCEPHALIA: IS THE TUATARA (SPHENODON PUNCTATUS) A LIVING FOSSIL? by JORGEA.HERRERA-FLORES , THOMAS L. STUBBS and MICHAEL J. BENTON School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, UK; jorge.herrerafl[email protected], [email protected], [email protected] Typescript received 4 July 2016; accepted in revised form 19 January 2017 Abstract: The tuatara, Sphenodon punctatus, known from since the Triassic, rhynchocephalians had heterogeneous rates 32 small islands around New Zealand, has often been noted of morphological evolution and occupied wide mor- as a classic ‘living fossil’ because of its apparently close phospaces during the Triassic and Jurassic, and these then resemblance to its Mesozoic forebears and because of a long, declined in the Cretaceous. In particular, we demonstrate low-diversity history. This designation has been disputed that the extant tuatara underwent unusually slow lineage because of the wide diversity of Mesozoic forms and because evolution, and is morphologically conservative, being located of derived adaptations in living Sphenodon. We provide a near the centre of the morphospace for all Rhynchocephalia. testable definition for ‘living fossils’ based on a slow rate of lineage evolution and a morphology close to the centroid of Key words: Rhynchocephalia, Sphenodontia, rates of evolu- clade morphospace. We show that through their history tion, living fossils, morphospace. T HE Rhynchocephalia is an ancient group of reptiles that geological time between the modern form and the young- emerged during the Early or Middle Triassic (Jones et al. est fossil forms, in the Miocene, Paleocene and Creta- 2013). -
A New Rhynchocephalian from the Late Jurassic of Germany with a Dentition That Is Unique Amongst Tetrapods
A New Rhynchocephalian from the Late Jurassic of Germany with a Dentition That Is Unique amongst Tetrapods Oliver W. M. Rauhut1,2*, Alexander M. Heyng2, Adriana Lo´ pez-Arbarello1, Andreas Hecker3 1 Bayerische Staatssammlung fu¨r Pala¨ontologie und Geologie and Department of Earth and Environmental Sciences, Ludwig Maximilians University, Munich, Germany, 2 GeoBioCenter, Ludwig Maximilians University, Munich, Germany, 3 Max-Planck-Gesellschaft, Generalverwaltung, Munich, Germany Abstract Background: Rhynchocephalians, the sister group of squamates (lizards and snakes), are only represented by the single genus Sphenodon today. This taxon is often considered to represent a very conservative lineage. However, rhynchocephalians were common during the late Triassic to latest Jurassic periods, but rapidly declined afterwards, which is generally attributed to their supposedly adaptive inferiority to squamates and/or Mesozoic mammals, which radiated at that time. New finds of Mesozoic rhynchocephalians can thus provide important new information on the evolutionary history of the group. Principle Findings: A new fossil relative of Sphenodon from the latest Jurassic of southern Germany, Oenosaurus muehlheimensis gen. et sp. nov., presents a dentition that is unique amongst tetrapods. The dentition of this taxon consists of massive, continuously growing tooth plates, probably indicating a crushing dentition, thus representing a previously unknown trophic adaptation in rhynchocephalians. Conclusions/Significance: The evolution of the extraordinary -
A Distinctive Late Triassic Microvertebrate Fissure Fauna and A
Proceedings of the Geologists’ Association 126 (2015) 402–416 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola A distinctive Late Triassic microvertebrate fissure fauna and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia) from Woodleaze Quarry, Gloucestershire, UK Catherine G. Klein *, David I. Whiteside, Victor Selles de Lucas, Pedro A. Viegas, Michael J. Benton School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK A R T I C L E I N F O A B S T R A C T Article history: During the Late Triassic and Early Jurassic, diverse terrestrial vertebrates were preserved in fissures Received 13 November 2014 formed in Carboniferous Limestone on an island archipelago spanning from the south of Wales to the Received in revised form 25 April 2015 north and south of Bristol. Here we report the faunas of two new fissures in Woodleaze quarry, near to Accepted 3 May 2015 Tytherington quarry, where the vertebrate fauna is already well known. The new site extends the lateral Available online 3 June 2015 distribution of fissures in this vicinity to over 900 m, and fissures sampled along that transect show a southerly change in the dominant species and a reduction in diversity. The Woodleaze fissure fauna is Keywords: nearly monofaunal, comprising >98% of a new Clevosaurus species, as well as some Diphydontosaurus Late Triassic fragments, a possible undescribed lepidosaur and a few fish fossils. The new clevosaur is distinguished Fissure fills Sphenodontians from the type species Clevosaurus hudsoni by its dentition, and by being smaller (average long bones are Clevosaurus 40–80% the length of C.