The Developmental Relationship Between Teeth and Dermal
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
A Unified Anatomy Ontology of the Vertebrate Skeletal System
A Unified Anatomy Ontology of the Vertebrate Skeletal System Wasila M. Dahdul1,2*, James P. Balhoff2,3, David C. Blackburn4, Alexander D. Diehl5, Melissa A. Haendel6, Brian K. Hall7, Hilmar Lapp2, John G. Lundberg8, Christopher J. Mungall9, Martin Ringwald10, Erik Segerdell6, Ceri E. Van Slyke11, Matthew K. Vickaryous12, Monte Westerfield11,13, Paula M. Mabee1 1 Department of Biology, University of South Dakota, Vermillion, South Dakota, United States of America, 2 National Evolutionary Synthesis Center, Durham, North Carolina, United States of America, 3 Department of Biology, University of North Carolina, Chapel Hill, North Carolina, United States of America, 4 Department of Vertebrate Zoology and Anthropology, California Academy of Sciences, San Francisco, California, United States of America, 5 The Jacobs Neurological Institute, University at Buffalo, Buffalo, New York, United States of America, 6 Oregon Health and Science University, Portland, Oregon, United States of America, 7 Department of Biology, Dalhousie University, Halifax, Nova Scotia, Canada, 8 Department of Ichthyology, The Academy of Natural Sciences, Philadelphia, Pennsylvania, United States of America, 9 Genomics Division, Lawrence Berkeley National Laboratory, Berkeley, California, United States of America, 10 The Jackson Laboratory, Bar Harbor, Maine, United States of America, 11 Zebrafish Information Network, University of Oregon, Eugene, Oregon, United States of America, 12 Department of Biomedical Sciences, Ontario Veterinary College, University of Guelph, Guelph, -
Comparative Bone Histology of the Turtle Shell (Carapace and Plastron)
Comparative bone histology of the turtle shell (carapace and plastron): implications for turtle systematics, functional morphology and turtle origins Dissertation zur Erlangung des Doktorgrades (Dr. rer. nat.) der Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität zu Bonn Vorgelegt von Dipl. Geol. Torsten Michael Scheyer aus Mannheim-Neckarau Bonn, 2007 Angefertigt mit Genehmigung der Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität Bonn 1 Referent: PD Dr. P. Martin Sander 2 Referent: Prof. Dr. Thomas Martin Tag der Promotion: 14. August 2007 Diese Dissertation ist 2007 auf dem Hochschulschriftenserver der ULB Bonn http://hss.ulb.uni-bonn.de/diss_online elektronisch publiziert. Rheinische Friedrich-Wilhelms-Universität Bonn, Januar 2007 Institut für Paläontologie Nussallee 8 53115 Bonn Dipl.-Geol. Torsten M. Scheyer Erklärung Hiermit erkläre ich an Eides statt, dass ich für meine Promotion keine anderen als die angegebenen Hilfsmittel benutzt habe, und dass die inhaltlich und wörtlich aus anderen Werken entnommenen Stellen und Zitate als solche gekennzeichnet sind. Torsten Scheyer Zusammenfassung—Die Knochenhistologie von Schildkrötenpanzern liefert wertvolle Ergebnisse zur Osteoderm- und Panzergenese, zur Rekonstruktion von fossilen Weichgeweben, zu phylogenetischen Hypothesen und zu funktionellen Aspekten des Schildkrötenpanzers, wobei Carapax und das Plastron generell ähnliche Ergebnisse zeigen. Neben intrinsischen, physiologischen Faktoren wird die -
The Integumentary Skeleton of Tetrapods: Origin, Evolution, and Development Matthew K
J. Anat. (2009) 214, pp441–464 doi: 10.1111/j.1469-7580.2008.01043.x REVIEWBlackwell Publishing Ltd The integumentary skeleton of tetrapods: origin, evolution, and development Matthew K. Vickaryous1 and Jean-Yves Sire2 1Department of Biomedical Sciences, Ontario Veterinary College, University of Guelph, Canada 2Université Pierre et Marie Curie-Paris 6, UMR 7138-Systématique, Adaptation, Evolution, Paris, France Abstract Although often overlooked, the integument of many tetrapods is reinforced by a morphologically and structurally diverse assemblage of skeletal elements. These elements are widely understood to be derivatives of the once all-encompassing dermal skeleton of stem-gnathostomes but most details of their evolution and development remain confused and uncertain. Herein we re-evaluate the tetrapod integumentary skeleton by integrating comparative developmental and tissue structure data. Three types of tetrapod integumentary elements are recognized: (1) osteoderms, common to representatives of most major taxonomic lineages; (2) dermal scales, unique to gymnophionans; and (3) the lamina calcarea, an enigmatic tissue found only in some anurans. As presently understood, all are derivatives of the ancestral cosmoid scale and all originate from scleroblastic neural crest cells. Osteoderms are plesiomorphic for tetrapods but demonstrate considerable lineage-specific variability in size, shape, and tissue structure and composition. While metaplastic ossification often plays a role in osteoderm development, it is not the exclusive mode of skeletogenesis. All osteoderms share a common origin within the dermis (at or adjacent to the stratum superficiale) and are composed primarily (but not exclusively) of osseous tissue. These data support the notion that all osteoderms are derivatives of a neural crest-derived osteogenic cell population (with possible matrix contributions from the overlying epidermis) and share a deep homology associated with the skeletogenic competence of the dermis. -
Fotw Classification Detailed Version
1 Classification of fishes from Fishes of the World 5th Edition. Nelson, JS, Grande, TC, and Wilson, MVH. 2016. This is a more detailed version of the listing in the book’s Table of Contents. Order and Family numbers are in parentheses; the page number follows a comma; † indicates extinct taxon. If you spot errors, please let us know at [email protected]. Latest update January 11, 2018. PHYLUM CHORDATA, 13 SUBPHYLUM UROCHORDATA—tunicates, 15 Class ASCIDIACEA—ascidians, 15 Class THALIACEA—salps, 15 Order PYROSOMIDA, 15 Order DOLIOLIDA, 15 Order SALPIDA, 15 Class APPENDICULARIA, 15 SUBPHYLUM CEPHALOCHORDATA, 16 Order AMPHIOXIFORMES—lancelets, 16 Family BRANCHIOSTOMATIDAE, 16 Family EPIGONICHTHYIDAE, 16 †SUBPHYLUM CONODONTOPHORIDA—conodonts, 17 †Class CONODONTA, 17 SUBPHYLUM CRANIATA, 18 INFRAPHYLUM MYXINOMORPHI, 19 Class MYXINI, 20 Order MYXINIFORMES (1)—hagfishes, 20 Family MYXINIDAE (1)—hagfishes, 20 Subfamily Rubicundinae, 21 Subfamily Eptatretinae, 21 Subfamily Myxininae, 21 INFRAPHYLUM VERTEBRATA—vertebrates, 22 †Anatolepis, 22 Superclass PETROMYZONTOMORPHI, 23 Class PETROMYZONTIDA, 23 Order PETROMYZONTIFORMES (2)—lampreys, 23 †Family MAYOMYZONTIDAE, 24 Family PETROMYZONTIDAE (2)—northern lampreys, 24 Subfamily Petromyzontinae, 24 Subfamily Lampetrinae, 25 Family GEOTRIIDAE (3)—southern lampreys, 25 Family MORDACIIDAE (4)—southern topeyed lampreys, 26 †Superclass PTERASPIDOMORPHI, 26 †Class PTERASPIDOMORPHA, 26 Subclass ASTRASPIDA, 27 †Order ASTRASPIDIFORMES, 27 Subclass ARANDASPIDA, 27 †Order ARANDASPIDIFORMES, -
Early Gnathostome Phylogeny Revisited: Multiple Method Consensus
RESEARCH ARTICLE Early Gnathostome Phylogeny Revisited: Multiple Method Consensus Tuo Qiao1, Benedict King2, John A. Long2, Per E. Ahlberg3, Min Zhu1* 1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China, 2 School of Biological Sciences, Flinders University, Adelaide, South Australia, Australia, 3 Department of Organismal Biology, Evolutionary Biology Centre, Uppsala University, NorbyvaÈgen, Uppsala, Sweden * [email protected] a11111 Abstract A series of recent studies recovered consistent phylogenetic scenarios of jawed verte- brates, such as the paraphyly of placoderms with respect to crown gnathostomes, and anti- archs as the sister group of all other jawed vertebrates. However, some of the phylogenetic OPEN ACCESS relationships within the group have remained controversial, such as the positions of Ente- Citation: Qiao T, King B, Long JA, Ahlberg PE, Zhu lognathus, ptyctodontids, and the Guiyu-lineage that comprises Guiyu, Psarolepis and M (2016) Early Gnathostome Phylogeny Revisited: Achoania. The revision of the dataset in a recent study reveals a modified phylogenetic Multiple Method Consensus. PLoS ONE 11(9): hypothesis, which shows that some of these phylogenetic conflicts were sourced from a e0163157. doi:10.1371/journal.pone.0163157 few inadvertent miscodings. The interrelationships of early gnathostomes are addressed Editor: Hector Escriva, Laboratoire Arago, FRANCE based on a combined new dataset with 103 taxa and 335 characters, which is the most Received: May 2, 2016 comprehensive morphological dataset constructed to date. This dataset is investigated in a Accepted: September 2, 2016 phylogenetic context using maximum parsimony (MP), Bayesian inference (BI) and maxi- Published: September 20, 2016 mum likelihood (ML) approaches in an attempt to explore the consensus and incongruence between the hypotheses of early gnathostome interrelationships recovered from different Copyright: 2016 Qiao et al. -
Morphology and Histology of Acanthodian Fin Spines from the Late Silurian Ramsasa E Locality, Skane, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E
Morphology and histology of acanthodian fin spines from the late Silurian Ramsasa E locality, Skane, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E. Ahlberg To cite this version: Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E. Ahlberg. Morphology and histology of acanthodian fin spines from the late Silurian Ramsasa E locality, Skane, Sweden. Palaeontologia Electronica, Coquina Press, 2017, 20 (3), pp.20.3.56A-1-20.3.56A-19. 10.26879/749. hal-02976007 HAL Id: hal-02976007 https://hal.archives-ouvertes.fr/hal-02976007 Submitted on 23 Oct 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. Palaeontologia Electronica palaeo-electronica.org Morphology and histology of acanthodian fin spines from the late Silurian Ramsåsa E locality, Skåne, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, and Per E. Ahlberg ABSTRACT Comparisons of acanthodians to extant gnathostomes are often hampered by the paucity of mineralized structures in their endoskeleton, which limits the potential pres- ervation of phylogenetically informative traits. Fin spines, mineralized dermal struc- tures that sit anterior to fins, are found on both stem- and crown-group gnathostomes, and represent an additional potential source of comparative data for studying acantho- dian relationships with the other groups of early gnathostomes. -
Development of the Turtle Plastron, the Order-Defining Skeletal Structure
Development of the turtle plastron, the order-defining skeletal structure Ritva Ricea,1, Aki Kallonenb, Judith Cebra-Thomasc,d, and Scott F. Gilberta,c,1 aDevelopmental Biology, Institute of Biotechnology, University of Helsinki, Helsinki 00014, Finland; bDepartment of Physics, University of Helsinki, Helsinki 00014, Finland; cDepartment of Biology, Swarthmore College, Swarthmore, PA 19081; and dDepartment of Biology, Millersville University, Millersville, PA 17551 Edited by Clifford J. Tabin, Harvard Medical School, Boston, MA, and approved March 30, 2016 (received for review January 19, 2016) The dorsal and ventral aspects of the turtle shell, the carapace and the fontanel at the midline of the plastron. Moreover, processes extend plastron, are developmentally different entities. The carapace con- dorsally from the hyoplastron and hypoplastron to form a bridge that tains axial endochondral skeletal elements and exoskeletal dermal connects the plastron with the ribs and the carapace. In some turtles bones. The exoskeletal plastron is found in all extant and extinct (especially ancient lineages), a further set of paired plastron bones, species of crown turtles found to date and is synaptomorphic of the the mesoplastra, lie between the hyoplastra and hypoplastra (7). order Testudines. However, paleontological reconstructed transition Although the anatomy of plastron bones has been known for forms lack a fully developed carapace and show a progression of centuries, and the homology of these bones to the skeletal structures bony elements ancestral to the plastron. To understand the evolu- of other reptilian clades has been debated almost as long (3, 4, 6, 8), tionary development of the plastron, it is essential to know how it has we still know very little about how these intramembranous bones formed. -
Family-Group Names of Fossil Fishes
European Journal of Taxonomy 466: 1–167 ISSN 2118-9773 https://doi.org/10.5852/ejt.2018.466 www.europeanjournaloftaxonomy.eu 2018 · Van der Laan R. This work is licensed under a Creative Commons Attribution 3.0 License. Monograph urn:lsid:zoobank.org:pub:1F74D019-D13C-426F-835A-24A9A1126C55 Family-group names of fossil fishes Richard VAN DER LAAN Grasmeent 80, 1357JJ Almere, The Netherlands. Email: [email protected] urn:lsid:zoobank.org:author:55EA63EE-63FD-49E6-A216-A6D2BEB91B82 Abstract. The family-group names of animals (superfamily, family, subfamily, supertribe, tribe and subtribe) are regulated by the International Code of Zoological Nomenclature. Particularly, the family names are very important, because they are among the most widely used of all technical animal names. A uniform name and spelling are essential for the location of information. To facilitate this, a list of family- group names for fossil fishes has been compiled. I use the concept ‘Fishes’ in the usual sense, i.e., starting with the Agnatha up to the †Osteolepidiformes. All the family-group names proposed for fossil fishes found to date are listed, together with their author(s) and year of publication. The main goal of the list is to contribute to the usage of the correct family-group names for fossil fishes with a uniform spelling and to list the author(s) and date of those names. No valid family-group name description could be located for the following family-group names currently in usage: †Brindabellaspidae, †Diabolepididae, †Dorsetichthyidae, †Erichalcidae, †Holodipteridae, †Kentuckiidae, †Lepidaspididae, †Loganelliidae and †Pituriaspididae. Keywords. Nomenclature, ICZN, Vertebrata, Agnatha, Gnathostomata. -
Scale Morphology and Squamation Pattern of Guiyu Oneiros Provide
www.nature.com/scientificreports OPEN Scale morphology and squamation pattern of Guiyu oneiros provide new insights into Received: 8 June 2018 Accepted: 7 January 2019 early osteichthyan body plan Published: xx xx xxxx Xindong Cui1,2,3, Tuo Qiao1,2 & Min Zhu1,2,3 Scale morphology and squamation play an important role in the study of fsh phylogeny and classifcation. However, as the scales of the earliest osteichthyans or bony fshes are usually found in a disarticulated state, research into squamation patterns and phylogeny has been limited. Here we quantitatively describe the scale morphology of the oldest articulated osteichthyan, the 425-million- year-old Guiyu oneiros, based on geometric morphometrics and high-resolution computed tomography. Based on the cluster analysis of the scales in the articulated specimens, we present a squamation pattern of Guiyu oneiros, which divides the body scales into 4 main belts, comprising 16 areas. The new pattern reveals that the squamation of early osteichthyans is more complicated than previously known, and demonstrates that the taxa near the crown osteichthyan node in late Silurian had a greater degree of squamation zonation compared to more advanced forms. This study ofers an important reference for the classifcation of detached scales of early osteichthyans, provides new insights into the early evolution of osteichthyan scales, and adds to our understanding of the early osteichthyan body plan. Research of the scale morphology and squamation of both fossil1–7 and extant osteichthyans8–14 provides valuable information for the fsh systematics and phylogeny. Previous descriptive works on early osteichthyan scale-based taxa were based on qualitative descriptions, or simple quantitative descriptions, lacking any systematic morpho- metric data2,15–20. -
The Largest Silurian Vertebrate and Its Palaeoecological Implications
OPEN The largest Silurian vertebrate and its SUBJECT AREAS: palaeoecological implications PALAEONTOLOGY Brian Choo1,2, Min Zhu1, Wenjin Zhao1, Liaotao Jia1 & You’an Zhu1 PALAEOCLIMATE 1Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology 2 Received and Paleoanthropology, Chinese Academy of Sciences, PO Box 643, Beijing 100044, China, School of Biological Sciences, 10 January 2014 Flinders University, GPO Box 2100, Adelaide 5001, South Australia. Accepted 23 May 2014 An apparent absence of Silurian fishes more than half-a-metre in length has been viewed as evidence that gnathostomes were restricted in size and diversity prior to the Devonian. Here we describe the largest Published pre-Devonian vertebrate (Megamastax amblyodus gen. et sp. nov.), a predatory marine osteichthyan from 12 June 2014 the Silurian Kuanti Formation (late Ludlow, ,423 million years ago) of Yunnan, China, with an estimated length of about 1 meter. The unusual dentition of the new form suggests a durophagous diet which, combined with its large size, indicates a considerable degree of trophic specialisation among early osteichthyans. The lack of large Silurian vertebrates has recently been used as constraint in Correspondence and palaeoatmospheric modelling, with purported lower oxygen levels imposing a physiological size limit. requests for materials Regardless of the exact causal relationship between oxygen availability and evolutionary success, this finding should be addressed to refutes the assumption that pre-Emsian vertebrates were restricted to small body sizes. M.Z. (zhumin@ivpp. ac.cn) he Devonian Period has been considered to mark a major transition in the size and diversity of early gnathostomes (jawed vertebrates), including the earliest appearance of large vertebrate predators1. -
SCIENCE CHINA Cranial Morphology of the Silurian Sarcopterygian Guiyu Oneiros (Gnathostomata: Osteichthyes)
SCIENCE CHINA Earth Sciences • RESEARCH PAPER • December 2010 Vol.53 No.12: 1836–1848 doi: 10.1007/s11430-010-4089-6 Cranial morphology of the Silurian sarcopterygian Guiyu oneiros (Gnathostomata: Osteichthyes) QIAO Tuo1,2 & ZHU Min1* 1 Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China; 2 Graduate School of Chinese Academy of Sciences, Beijing 100049, China Received April 6, 2010; accepted July 13, 2010 Cranial morphological features of the stem-group sarcopterygian Guiyu oneiros Zhu et al., 2009 provided here include the dermal bone pattern and anatomical details of the ethmosphenoid. Based on those features, we restored, for the first time, the skull roof bone pattern in the Guiyu clade that comprises Psarolepis and Achoania. Comparisons with Onychodus, Achoania, coelacanths, and actinopterygians show that the posterior nostril enclosed by the preorbital or the preorbital process is shared by actinopterygians and sarcopterygians, and the lachrymals in sarcopterygians and actinopterygians are not homologous. The endocranium closely resembles that of Psarolepis, Achoania and Onychodus; however, the attachment area of the vomer pos- sesses irregular ridges and grooves as in Youngolepis and Diabolepis. The orbito-nasal canal is positioned mesial to the nasal capsule as in Youngolepis and porolepiforms. The position of the hypophysial canal at the same level or slightly anterior to the ethmoid articulation represents a synapmorphy of the Guiyu clade. The large attachment area of the basicranial muscle indi- cates the presence of a well-developed intracranial joint in Guiyu. Sarcopterygii, Osteichthyes, Cranial morphology, homology, Silurian, China Citation: Qiao T, Zhu M.