Phylogeny Discovery

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Caroline Bowman, Seungmin Albanerpetontidae Kim, Logan Arneson, Benjamin Salzberg Mesozoic-Cenozoic salamander-like amphibians GEOL 204 The Fossil Record Discovery Spring 2019 Section 0101 Phylogeny https://en.wikipedia.org/wiki/Albanerpetontidae https://journals.plos.org/plosone/article?id=10.1371/journal.pone.01 89767#pone-0189767-g001 Origins -First record of Albanerpetontidae Originated 160 million years ago from the was found in East Asia, specifically Bathonian stage of the Middle Jurassic & Western Japan. lived until the beginning of the Pleistocene https://www.tandfonline.com/doi/pdf/10.1671/0272-4634%282002%29022%5B0012%3AMAIGRO%5D2.0.CO%3B2?needAccess=true -In 1997, fossils were found on the 2.13-2 million years ago² "Kaseki-Kabe" fossil cliff.³ Family -Genus: Albanerpeton -Approximately 10-20 known species -the changes in each taxa involved Model Clay Reconstruction of Skull -5 genera: Albanerpeton, Anoualerpeton, broadening of the head & strengthening of Celtedens, Shirerpeton & Wesserpeton the snout and jaws, both intended for Common Misconception improved feeding and burrowing² -The albanerpetontidae’s small size and specific body parts lead people to believe they are salamanders, which they AREN'T -Their skin was actually covered with bony scales, thus differentiating them from salamanders. https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0189767#pone-0189767-g001 There are 3 living orders of amphibians: Methods of reconstruction: -Only a small area of skull bone was exposed on the surface Anura Caudata Gymnophiona -The Tokyo Metropolitan Industrial (frogs) (salamanders) (caecilians) Technology Research Institute scanned the area using a CT scanner (Toscaner 30000 micro CN) https://slideplayer.com/slide/4693638/ -Features like foramina, tooth tips, https://slideplayer.com/slide/4693638/ http://www.pbs.org/wnet/nature/group/amphibians-reptile https://www.pictorem.com/80254/Salamander%20(Caudata)%20on%20a%20white%20backgrou https://en.wikipedia.org/wiki/Caecilian and fine edges were found. s/frog/ nd;%20Tarifa,%20Cadiz,%20Andalusia,%20Spain.html -These parts were segmented out The albanerpetontid family is recognized as from scanned area & 3D printed part of the clade/amphibian sub-class (Objet350 Connex) lissamphibians -Parts were pieced together using ★ Crown group of amphibians is lissamphibia. modeling clay to figure out the bone albanerpetontidaes are closely related to Not all amphibians are lissamphibians, but positions to reconstruct the skull³ frogs and salamanders, but not to caecilians.² all lissamphibians are amphibians¹.

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Szentesi Et Al.Indd
FRAGMENTA PALAEONTOLOGICA HUNGARICA Volume 32 Budapest, 2015 pp. 49–66 Albanerpetontidae from the late Pliocene (MN 16A) Csarnóta 3 locality (Villány Hills, South Hungary) in the collection of the Hungarian Natural History Museum Zoltán Szentesi1, Piroska Pazonyi2 & Lukács Mészáros3 1Department of Palaeontology and Geology, Hungarian Natural History Museum, H-1083 Budapest, Ludovika tér 2, Hungary. E-mail: [email protected] 2MTA–MTM–ELTE Research Group for Palaeontology H-1083 Budapest, Ludovika tér 2, Hungary. E-mail: [email protected] 3Department of Palaeontology, Eötvös Loránd University, H-1117 Budapest, Pázmány Péter sétány 1/C, Hungary. E-mail: [email protected] Abstract – Based on cranial and jaw elements, the presence of Albanerpeton pannonicum species (Allocaudata: Albanerpetontidae) was noticed from the late Pliocene Csarnóta 3 locality (Villány Hills). Since it is considered a poor fossil site, it had not been suffi ciently studied. Th ese fossils represent the geologically youngest record of the species from Hungary. Th ough, the Csarnóta 3 albanerpetontid assemblage is small the bones are well preserved, and all are informative on spe- cies or at least on genus level. Th e red coloured bone-bearing deposits and the preservation quality of bones are very similar to the uppermost strata (4–1) of the Csarnóta 2 palaeovertebrate locality. Th e study of small mammal fauna also suggests this correlation, as well as explains the age of the site. Th e studied vertebrate fauna forms a transition between the woodland and steppe wildlife. With 17 fi gures and 3 tables. Key words – Albanerpeton, Albanerpetontidae, late Pliocene, small mam mals, taphonomy, Vil- lány Hills INTRODUCTION Albanerpetontidae are a Middle Jurassic – late Pliocene clade of salaman- der-like lissamphibians that are closely related to anurans and salamanders (e.g.
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A New Microvertebrate Assemblage from the Mussentuchit
A new microvertebrate assemblage from the Mussentuchit Member, Cedar Mountain Formation: insights into the paleobiodiversity and paleobiogeography of early Late Cretaceous ecosystems in western North America Haviv M. Avrahami1,2,3, Terry A. Gates1, Andrew B. Heckert3, Peter J. Makovicky4 and Lindsay E. Zanno1,2 1 Department of Biological Sciences, North Carolina State University, Raleigh, NC, USA 2 North Carolina Museum of Natural Sciences, Raleigh, NC, USA 3 Department of Geological and Environmental Sciences, Appalachian State University, Boone, NC, USA 4 Field Museum of Natural History, Chicago, IL, USA ABSTRACT The vertebrate fauna of the Late Cretaceous Mussentuchit Member of the Cedar Mountain Formation has been studied for nearly three decades, yet the fossil-rich unit continues to produce new information about life in western North America approximately 97 million years ago. Here we report on the composition of the Cliffs of Insanity (COI) microvertebrate locality, a newly sampled site containing perhaps one of the densest concentrations of microvertebrate fossils yet discovered in the Mussentuchit Member. The COI locality preserves osteichthyan, lissamphibian, testudinatan, mesoeucrocodylian, dinosaurian, metatherian, and trace fossil remains and is among the most taxonomically rich microvertebrate localities in the Mussentuchit Submitted 30 May 2018 fi fi Accepted 8 October 2018 Member. To better re ne taxonomic identi cations of isolated theropod dinosaur Published 16 November 2018 teeth, we used quantitative analyses of taxonomically comprehensive databases of Corresponding authors theropod tooth measurements, adding new data on theropod tooth morphodiversity in Haviv M. Avrahami, this poorly understood interval. We further provide the first descriptions of [email protected] tyrannosauroid premaxillary teeth and document the earliest North American record of Lindsay E.
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Early Cretaceous) Wessex Formation of the Isle of Wight, Southern England
A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wessex Formation of the Isle of Wight, southern England STEVEN C. SWEETMAN and JAMES D. GARDNER Sweetman, S.C. and Gardner, J.D. 2013. A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wes− sex Formation of the Isle of Wight, southern England. Acta Palaeontologica Polonica 58 (2): 295–324. A new albanerpetontid, Wesserpeton evansae gen. et sp. nov., from the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England, is described. Wesserpeton is established on the basis of a unique combination of primitive and derived characters relating to the frontals and jaws which render it distinct from currently recognized albanerpetontid genera: Albanerpeton (Late Cretaceous to Pliocene of Europe, Early Cretaceous to Paleocene of North America and Late Cretaceous of Asia); Celtedens (Late Jurassic to Early Cretaceous of Europe); and Anoualerpeton (Middle Jurassic of Europe and Early Cretaceous of North Africa). Although Wesserpeton exhibits considerable intraspecific variation in characters pertaining to the jaws and, to a lesser extent, frontals, the new taxon differs from Celtedens in the shape of the internasal process and gross morphology of the frontals in dorsal or ventral view. It differs from Anoualerpeton in the lack of pronounced heterodonty of dentary and maxillary teeth; and in the more medial loca− tion and direction of opening of the suprapalatal pit. The new taxon cannot be referred to Albanerpeton on the basis of the morphology of the frontals. Wesserpeton currently represents the youngest record of Albanerpetontidae in Britain. Key words: Lissamphibia, Albanerpetontidae, microvertebrates, Cretaceous, Britain. Steven C.
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Yaksha Perettii
Yaksha perettii Yaksha perettii is an extinct species of albanerpetontid amphibian, and the only species in the genus Yaksha. It is known from three Yaksha perettii specimens found in Cenomanian aged Burmese amber from Temporal range: Early Cenomanian Myanmar. The remains of Yaksha perettii are the best preserved of 99 Ma all albanerpetontids, which usually consist of isolated fragments or ↓ crushed flat, and have provided significant insights in the PreꞒ Ꞓ O S D C P T J K PgN morphology and lifestyle of the group. Contents Etymology Discovery Description Phylogeny Holotype skull of Yaksha perettii, dark References grey represents preserved soft tissue Scientific classification Etymology Kingdom: Animalia Phylum: Chordata The generic epithet is named after the Yaksha, a class of nature Class: Amphibia and guardian spirits in Indian religions, while the specific epithet honors Dr. Adolf Peretti, who provided some of the specimens, Order: †Allocaudata including the holotype.[1] Family: †Albanerpetontidae Discovery Genus: †Yaksha Daza et al, 2020 The paratype specimen was originally described in 2016 amongst Species: †Y. perettii a collection of fossil lizard species from Burmese amber, and was initially identified as a stem-chameleon.[2] However Professor Binomial name Susan E. Evans, a researcher who has extensively worked on †Yaksha perettii albanerpetontids, recognised the specimen as belonging to the Daza et al, 2020 group.[3] Subsequently, another specimen was discovered in the collection of gemologist Dr. Adolf Peretti, which would later become the holotype specimen.[4] The paper describing Yaksha perettii was published in November 2020 in the journal Science.[1] Description The species is known from three specimens, the small juvenile skeleton described in the 2016 paper (JZC Bu154), a complete adult skull and lower jaws (GRS-Ref-060829), and a partial adult postcranium (GRSRef- 27746).
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Early Tetrapod Relationships Revisited
Biol. Rev. (2003), 78, pp. 251–345. f Cambridge Philosophical Society 251 DOI: 10.1017/S1464793102006103 Printed in the United Kingdom Early tetrapod relationships revisited MARCELLO RUTA1*, MICHAEL I. COATES1 and DONALD L. J. QUICKE2 1 The Department of Organismal Biology and Anatomy, The University of Chicago, 1027 East 57th Street, Chicago, IL 60637-1508, USA ([email protected]; [email protected]) 2 Department of Biology, Imperial College at Silwood Park, Ascot, Berkshire SL57PY, UK and Department of Entomology, The Natural History Museum, Cromwell Road, London SW75BD, UK ([email protected]) (Received 29 November 2001; revised 28 August 2002; accepted 2 September 2002) ABSTRACT In an attempt to investigate differences between the most widely discussed hypotheses of early tetrapod relation- ships, we assembled a new data matrix including 90 taxa coded for 319 cranial and postcranial characters. We have incorporated, where possible, original observations of numerous taxa spread throughout the major tetrapod clades. A stem-based (total-group) definition of Tetrapoda is preferred over apomorphy- and node-based (crown-group) definitions. This definition is operational, since it is based on a formal character analysis. A PAUP* search using a recently implemented version of the parsimony ratchet method yields 64 shortest trees. Differ- ences between these trees concern: (1) the internal relationships of aı¨stopods, the three selected species of which form a trichotomy; (2) the internal relationships of embolomeres, with Archeria
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A New Genus and Species of Basal Salamanders from the Middle Jurassic of Western Siberia, Russia P.P
Proceedings of the Zoological Institute RAS Vol. 315, No. 2, 2011, рр. 167–175 УДК 57.072:551.762.2 A NEW GENUS AND SPECIES OF BASAL SALAMANDERS FROM THE MIDDLE JURASSIC OF WESTERN SIBERIA, RUSSIA P.P. Skutschas1* and S.A. Krasnolutskii2 1Saint Petersburg State University, Universitetskaya Emb. 7/9, 199034 Saint Petersburg, Russia; e-mail: [email protected] 2Sharypovo Regional Museum, 2nd microrayon 10, Sharypovo, 662311 Krasnoyarsk Territory, Russia; e-mail: [email protected] ABSTRACT A new basal stem salamander, Urupia monstrosa gen. et sp. nov., is described based on an atlantal centrum (holotype), fragments of trunk vertebrae, and some associated elements (fragmentary dentaries and a femur) from the Middle Jurassic (Bathonian) Itat Formation of Krasnoyarsk Territory in Western Siberia, Russia. The new taxon is characterized by the following combination of characters: lack of the spinal nerve foramina in the atlas, presence atlantal transverse processes and a deep depression on the ventral surface of the atlas; lateral surface of anterior part of the dentary is sculptured by oval and rounded pits; very short diaphyseal part of femur. The absence of intercotylar tubercle on the atlas and presence of atlantal transverse processes support for neotenic nature of Urupia monstrosa gen. et sp. nov. Large size, presence of sculpture on vertebrae, and the absence of spinal nerve foramina in the atlas suggest that Urupia monstrosa gen. et sp. nov. is a stem group salamander. The phylogenetic relationships of Urupia monstrosa gen. et sp. nov. with other stem group salamanders cannot be established on the available material. Key words: Caudata, Itat Formation, Jurassic, Russia НОВЫЙ РОД И ВИД БАЗАЛЬНЫХ ХВОСТАТЫХ АМФИБИЙ ИЗ СРЕДНЕЙ ЮРЫ ЗАПАДНОЙ СИБИРИ, РОССИЯ П.П.
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Fossils Importance Bibliography
GEOL 204 The Fossil Record Las Hoyas Spring 2020 Section 0101 Daniel Boyarsky, Noor Nabulsi, Alyssa Pryputniewicz & Elijah WeBB Fossils Geological Layout This Lagerstätten site has exceptionally preserved fossils. Some of these fossils include Microbial mats: responsible for the preservation of soft tissue in many fossils The iron structures that are rarely found in the fossil record, such as soft tissues, patterns of carbonate depositions, as a result from bacterial metabolism which covered the dinosaur's crest coloring, nerviation, and gut tracts (Buscalioni, A.D.). Below are some of the other animals increased the preservation of those soft tissues. Evidence of these mats comes from the studies that researchers have found fossils of. on microfacies and the fossils themselves. Albanerpeton (amphibian) Europejara (pterosaur) Crusafontia (mammal) Abruption: Notable in the formation, due to the presence of complex specimens. From studies on several different organisms it can be estimated that the burial of most entities was quick. Stagnation: Millions of years with the lack of external forces on the site created an untouched site of easily accessible fossils. 20 mm 35 cm 5 cm Fig. 1: Tamura, N. (Albanerpeton); Fig. 2: “Euro” Fig. 3: “Crusafontia” Venczel, M. Fig. 6: “Crusafontia” Http://Gomeslab.weebly.com/Uploads/1/0/9/2/10 Https://d1k5w7mbrh6vq5.Cloudfront.net/Images/ 9219815/Published/Img-1803- Cache/0d/34/7d/0d347d1e06f219283da2064b963 Importance 2.Jpg?1503670391, 5b420.Jpg,mages.app.goo.gl/qTGBW7NvY4X9v The Las Hoyas site has recorded a wide array of species of diverse plant and animal taxa. At images.app.goo.gl/C2zWPTU1rVD9VzoR7. 6HU8. present, the biodiversity count comprises 118 families and 201 species.
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Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal)
Alexandre Renaud Daniel Guillaume Licenciatura em Biologia celular Mestrado em Sistemática, Evolução, e Paleobiodiversidade Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal) Dissertação para obtenção do Grau de Mestre em Paleontologia Orientador: Miguel Moreno-Azanza, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Co-orientador: Octávio Mateus, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Júri: Presidente: Prof. Doutor Paulo Alexandre Rodrigues Roque Legoinha (FCT-UNL) Arguente: Doutor Hughes-Alexandres Blain (IPHES) Vogal: Doutor Miguel Moreno-Azanza (FCT-UNL) Júri: Dezembro 2018 MICROVERTEBRATES OF THE LOURINHÃ FORMATION (LATE JURASSIC, PORTUGAL) © Alexandre Renaud Daniel Guillaume, FCT/UNL e UNL A Faculdade de Ciências e Tecnologia e a Universidade Nova de Lisboa tem o direito, perpétuo e sem limites geográficos, de arquivar e publicar esta dissertação através de exemplares impressos reproduzidos em papel ou de forma digital, ou por qualquer outro meio conhecido ou que venha a ser inventado, e de a divulgar através de repositórios científicos e de admitir a sua cópia e distribuição com objetivos educacionais ou de investigação, não comerciais, desde que seja dado crédito ao autor e editor. ACKNOWLEDGMENTS First of all, I would like to dedicate this thesis to my late grandfather “Papi Joël”, who wanted to tie me to a tree when I first start my journey to paleontology six years ago, in Paris. And yet, he never failed to support me at any cost, even if he did not always understand what I was doing and why I was doing it. He is always in my mind. Merci papi ! This master thesis has been one-year long project during which one there were highs and lows.
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La Cantalera: an Exceptional Window Onto the Vertebrate Biodiversity of the Hauterivian-Barremian Transition in the Iberian Peninsula
ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es/info/estratig/journal.htm Journal of Iberian Geology 36 (2) 2010: 205-224 doi:10.5209/rev_JIGE.2010.v36.n2.8 La Cantalera: an exceptional window onto the vertebrate biodiversity of the Hauterivian-Barremian transition in the Iberian Peninsula La Cantalera: una excepcional ventana a la biodiversidad del tránsito Hauteriviense- Barremiense en la Península Ibérica J.I. Canudo1, J.M. Gasca1, M. Aurell2, A. Badiola1, H.-A. Blain3, P. Cruzado-Caballero1, D. Gómez- Fernández1, M. Moreno-Azanza1, J. Parrilla1, R. Rabal-Garcés1, J. I. Ruiz-Omeñaca1,4 1Grupo Aragosaurus (http://www.aragosaurus.com). Universidad de Zaragoza. 50009 Zaragoza, Spain. [email protected], [email protected], [email protected], [email protected], [email protected], [email protected], [email protected] 2Estratigrafía. Universidad de Zaragoza. 50009 Zaragoza. Spain. [email protected] 3Institut Català de Paleoecologia Humana y Evolució Social (Unitat asociada al CSIC). Universitat Rovira i Virgili. 43005 Tarragona. Spain. [email protected] 4Museo del Jurásico de Asturias (MUJA). 33328 Colunga. Asturias. Spain. [email protected] Received: 15/11/09 / Accepted: 30/06/10 Abstract La Cantalera is an accumulation site for fossil vertebrates consisting mainly of teeth and isolated postcranial remains. It has the greatest vertebrate biodiversity of any site from the Hauterivian-Barremian transition in the Iberian Peninsula. Up to now, 31 vertebrate taxa have been recognized: an osteichthyan (Teleostei indet.), two amphibians (Albanerpetonidae indet. and Discoglos- sidae indet.), a chelonian (Pleurosternidae? indet.), a lizard (Paramacellodidae? indet.), four crocodylomorphs (cf. Theriosuchus sp., Bernissartiidae indet., Goniopholididae indet., cf.
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The Making of Calibration Sausage Exemplified by Recalibrating the Transcriptomic Timetree of Jawed Vertebrates
bioRxiv preprint doi: https://doi.org/10.1101/2019.12.19.882829; this version posted November 30, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-ND 4.0 International license. The making of calibration sausage exemplified by recalibrating the transcriptomic timetree of jawed vertebrates 1 David Marjanović 2 Department of Evolutionary Morphology, Science Programme “Evolution and Geoprocesses”, 3 Museum für Naturkunde – Leibniz Institute for Evolutionary and Biodiversity Research, Berlin, 4 Germany 5 ORCID: 0000-0001-9720-7726 6 Correspondence: 7 David Marjanović 8 [email protected] 9 Keywords: timetree, calibration, divergence date, Gnathostomata, Vertebrata 10 Abstract 11 Molecular divergence dating has the potential to overcome the incompleteness of the fossil record in 12 inferring when cladogenetic events (splits, divergences) happened, but needs to be calibrated by the 13 fossil record. Ideally but unrealistically, this would require practitioners to be specialists in molecular 14 evolution, in the phylogeny and the fossil record of all sampled taxa, and in the chronostratigraphy of 15 the sites the fossils were found in. Paleontologists have therefore tried to help by publishing 16 compendia of recommended calibrations, and molecular biologists unfamiliar with the fossil record 17 have made heavy use of such works (in addition to using scattered primary sources
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Vertebrate Paleontology of the Cloverly Formation (Lower Cretaceous), II: Paleoecology Author(S): Matthew T
Vertebrate Paleontology of the Cloverly Formation (Lower Cretaceous), II: Paleoecology Author(s): Matthew T. Carrano , Matthew P. J. Oreska , and Rowan Lockwood Source: Journal of Vertebrate Paleontology, 36(2) Published By: The Society of Vertebrate Paleontology URL: http://www.bioone.org/doi/full/10.1080/02724634.2015.1071265 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Journal of Vertebrate Paleontology e1071265 (12 pages) Ó by the Society of Vertebrate Paleontology DOI: 10.1080/02724634.2015.1071265 ARTICLE VERTEBRATE PALEONTOLOGY OF THE CLOVERLY FORMATION (LOWER CRETACEOUS), II: PALEOECOLOGY MATTHEW T. CARRANO,*,1 MATTHEW P. J. ORESKA,1,2 and ROWAN LOCKWOOD3 1Department of Paleobiology, Smithsonian Institution, P.O. Box 37012, MRC 121, Washington, DC 20013-7012, U.S.A., [email protected]; 2Department of Environmental Sciences, University of Virginia, Clark Hall, 291 McCormick Road, P.O.
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ESTADO DE LAS INVESTIGACIONES SOBRE LOS VERTEBRADOS DEL JURASICO SUPERIOR Y CRETACICO INFERIOR DE GALVE (TERUEL)L J
Estudios Geol., 60: 179-202 (2004) ESTADO DE LAS INVESTIGACIONES SOBRE LOS VERTEBRADOS DEL JURASICO SUPERIOR y CRETACICO INFERIOR DE GALVE (TERUEL)l J. 1. Ruiz-Omeñaca*, J. 1. Canudo*, M. Aurell**, B. Bádenas**, J. L. Barco***, G. Cuenca-Bescós* y J. Ipas** RESUMEN En Galve (Teruel) hay más de 50 localidades con restos de vertebrados continentales en las Formaciones Higueruelas (Titónico), Villar del Arzobispo (Titónico superior-Berriasien se medio), El Castellar (Hauteriviense terminal-Barremiense basal) y Camarillas (Barre miense inferior). Por tanto, «Galve» no es un único yacimiento de vertebrados mesozoicos, sino una localidad con numerosos yacimientos de vertebrados del intervalo Titónico-Barre• miense, que geológicamente pertenecen a la Cuenca cretácica inferior del Maestrazgo (Cor dillera Ibérica Central), Subcuenca de Galve. La mayor parte de los yacimientos contienen restos óseos, pero también son abundantes los yacimientos paleoicnológicos y paleoológi• coso Los vertebrados mejor conocidos son los mamíferos y dinosaurios, aunque también hay estudios sobre los tiburones, peces óseos, anfibios, escamosos y cocodrilos. Algunos grupos, como tortugas y pterosaurios, permanencen prácticamente sin estudiar. Galve es la localidad tipo de varios taxones de vertebrados: el tiburón Lonchidion microselachos, el anfibio Gal verpeton ibericum, el dinosaurio Aragosaurus ischiaticus, los mamíferos Galveodon nan nothus, Lavocatia alfambrensis, Eobaatar hispanicus, Parendotherium herreroi, Spalacot herium henkeli y Pocamus pepelui, y la cáscara de huevo de dinosaurio Macroolithus turo lensis. Es este trabajo se revisa el estado de conocimientos sobre los vertebrados de Galve, y se actualiza la lista faunística de sus yacimientos, siendo la primera vez que se realiza teniendo en cuenta la distribución estratigráfica de los taxones.
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