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First Remains of Diplocynodon Cf. Ratelii from the Early Miocene Sites of Ahníkov (Most Basin, Czech Republic)
First remains of Diplocynodon cf. ratelii from the early Miocene sites of Ahníkov (Most Basin, Czech Republic) Milan Chroust, Martin MazuCh, Martin ivanov, Boris Ekrt & ÀngEl h. luján Fossil crocodylians from the early Miocene (Eggenburgian, MN3a) sites of Ahníkov (Most Basin, Czech Republic) are described in this paper. The new material presented here includes over 200 remains (bones, teeth and osteoderms), and therefore constitutes the largest crocodylian sample known from the fossil record of the Czech Republic. Assignment of the specimens to the fossil alligatoroid taxon Diplocynodon cf. ratelii Pomel, 1847 (family Diplocynodontidae) is justified by the presence of several cranial and postcranial features. In the Czech Republic, this species has been previously reported only from the Tušimice site (MN3, Most Basin, Ohře/Eger Graben). The majority of the material reported from Ahníkov is composed of disarticulated juvenile individuals. Both sites are most likely attributable to the specific environment of swampy areas, where crocodile hatchlings would hide from predators. The presence of the genus Diplocynodon supports the assumption of rather warm climatic conditions in Central Europe during the early to middle Miocene, as well as a swampy depositional environment previously inferred for Ahníkov. However, some squamate taxa suggest the existence of additional, surrounding palaeoenvironment characterised by a more open landscape with slightly drier conditions. • Key words: fossil crocodiles, alligatoroid, Ahníkov, Ohře/Eger Graben, Eggenburgian. CHROUST, M., MAZUCH, M., IVANOV, M., EKRT, B. & LUJÁN, À.H. 2021. First remains of Diplocynodon cf. ratelii from the early Miocene sites of Ahníkov (Most Basin, Czech Republic). Bulletin of Geosciences 96(2), 123–138 (10 figures, 1 table). -
Genetic Diversity of False Gharial Tomistoma Schlegelii Based on Cytochrome B-Control Region (Cyt B-CR) Gene Analysis
Genetic Diversity of False Gharial Tomistoma schlegelii based on Cytochrome b-Control Region (cyt b-CR) Gene Analysis Muhamad Farhan Bin Badri (34975) Bachelor of Science with Honours (Aquatic Resource Science and Management) 2015 UNIVERSITJ MALAYSIASARAWAK Grade A- Please tick <V) Final Year Project Report Masters PhD DECIA RATJON OF ORIGINAL WORK This declaration is made on the... .;l... day of.. .. ;Jr.,-.v!y" year .....;;;,;;J].C;S: Stude nt's Declaration: I .. _ ~~_~!l.~_~.I? .f!J~_~~ __ . ~?.: ___~~e!: .. .J..3_ f:{~~ _./. £~... ____ .....-.---- ..----- ....-------.----......--.--..--- (PLEASE INDIC TE NAME. MATRIC NO. AND FACULTy) hereby declare that the work entitled. .~ft~ _ !l! ~~.'!.!J - f!~ - ~ b.':>!~.I-- !: --~~-~ ['JJ'.~! - .b.i.'.J--~:! ..~L~.":~B - ~ !.~.- ~ -~~?: is my original work. I have not copied from any other students' work or from any other sources with tbe exception where due reference or acknowledgement is made explicitly in th e text. nor has any part of the work been written for me by another person. r / 7 / :»')1 ~ MV~fI~AO F~IlH~'" p,Itv Il/!PlT G4'11S') Date submitted Name of the student (Mabic No.) Supervisor's Declaration: I,-- -OP,- - ~!!~~..~~!!.. !!~~_~ _ ...............__ .__ (SUPERVISOR'S NAME), herehy certify that the work entitled, q~~~-- ~.'".'!~~ - ~~~ - ~~~.~X: - ~~-~~i. ~}!lg-"'-- ~t_<;t ·~~jdTITLE ) was prepared by the aforementioned or above mentioned student, and was submitted to the "FACULTY' as a * partiaJJfuil fulfillment for the conferment of ._.¥h__J!~!.~..$.~~~_~L ~~A._ ~f!~~~- -
Phylogenetic Taphonomy: a Statistical and Phylogenetic
Drumheller and Brochu | 1 1 PHYLOGENETIC TAPHONOMY: A STATISTICAL AND PHYLOGENETIC 2 APPROACH FOR EXPLORING TAPHONOMIC PATTERNS IN THE FOSSIL 3 RECORD USING CROCODYLIANS 4 STEPHANIE K. DRUMHELLER1, CHRISTOPHER A. BROCHU2 5 1. Department of Earth and Planetary Sciences, The University of Tennessee, Knoxville, 6 Tennessee, 37996, U.S.A. 7 2. Department of Earth and Environmental Sciences, The University of Iowa, Iowa City, Iowa, 8 52242, U.S.A. 9 email: [email protected] 10 RRH: CROCODYLIAN BITE MARKS IN PHYLOGENETIC CONTEXT 11 LRH: DRUMHELLER AND BROCHU Drumheller and Brochu | 2 12 ABSTRACT 13 Actualistic observations form the basis of many taphonomic studies in paleontology. 14However, surveys limited by environment or taxon may not be applicable far beyond the bounds 15of the initial observations. Even when multiple studies exploring the potential variety within a 16taphonomic process exist, quantitative methods for comparing these datasets in order to identify 17larger scale patterns have been understudied. This research uses modern bite marks collected 18from 21 of the 23 generally recognized species of extant Crocodylia to explore statistical and 19phylogenetic methods of synthesizing taphonomic datasets. Bite marks were identified, and 20specimens were then coded for presence or absence of different mark morphotypes. Attempts to 21find statistical correlation between trace types, marking animal vital statistics, and sample 22collection protocol were unsuccessful. Mapping bite mark character states on a eusuchian 23phylogeny successfully predicted the presence of known diagnostic, bisected marks in extinct 24taxa. Predictions for clades that may have created multiple subscores, striated marks, and 25extensive crushing were also generated. Inclusion of fossil bite marks which have been positively 26associated with extinct species allow this method to be projected beyond the crown group. -
An Eocene Tomistomine from Peninsular Thailand Jérémy Martin, Komsorn Lauprasert, Haiyan Tong, Varavudh Suteethorn, Eric Buffetaut
An Eocene tomistomine from peninsular Thailand Jérémy Martin, Komsorn Lauprasert, Haiyan Tong, Varavudh Suteethorn, Eric Buffetaut To cite this version: Jérémy Martin, Komsorn Lauprasert, Haiyan Tong, Varavudh Suteethorn, Eric Buffetaut. An Eocene tomistomine from peninsular Thailand. Annales de Paléontologie, Elsevier Masson, 2019, 10.1016/j.annpal.2019.03.002. hal-02121886 HAL Id: hal-02121886 https://hal.archives-ouvertes.fr/hal-02121886 Submitted on 6 May 2019 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. An Eocene tomistomine from peninsular Thailand Un tomistominé éocène de la peninsule Thaïlandaise Jeremy E. Martin1, Komsorn Lauprasert2, Haiyan Tong2, Varavudh Suteethorn2 and Eric Buffetaut3 1Laboratoire de Géologie de Lyon: Terre, Planète et Environnement, UMR CNRS 5276 (CNRS, ENS, Université Lyon 1), Ecole Normale Supérieure de Lyon, 69364 Lyon Cedex 07, France, email: [email protected] 2Palaeontological Research and Education Centre, Mahasarakham University, Khamrieng, 44150 Thailand 3Laboratoire de Géologie de l’Ecole Normale Supérieure, CNRS (UMR 8538), 24 rue Lhomond, Paris Cedex 05, 75231, France Abstract Skull and mandibular elements of a tomistomine crocodilian are described from the late Eocene to early Oligocene lignite seams of Krabi, peninsular Thailand. -
Phylogenetic Position of the Crocodylian Megadontosuchus Arduini and Tomistomine Palaeobiogeography
Phylogenetic position of the crocodylian Megadontosuchus arduini and tomistomine palaeobiogeography PAOLO PIRAS, MASSIMO DELFINO, LETIZIA DEL FAVERO, and TASSOS KOTSAKIS Piras, P., Delfino, M., Del Favero, L., and Kotsakis, T. 2007. Phylogenetic position of the crocodylian Megadontosuchus arduini and tomistomine palaeobiogeography. Acta Palaeontologica Polonica 52 (2): 315–328. A cladistic analysis of Megadontosuchus arduini from the middle Eocene of Monte Duello (NE Italy) confirms its tomistomine relationships, but the low number of scorable characters determines a low resolution within the tomistomine clade. However, Megadontosuchus is clearly distinct from the other Eocene European or North African tomistomines, in having a moderate elongated but robust rostrum, massive maxillary and dentary teeth and large supratemporal fenestrae. The rostrum and teeth characteristics could indicate that M. arduini had a degree of feeding specialization intermediate between Maroccosuchus zennaroi and the Eocene European tomistomines. A summary of tomistomine palaeobiogeo− graphy suggests that despite only one species with a rather restricted range survives at present, such a clade had a glorious past with a world wide distribution documented by a conspicuous fossil record that starts at least in the early Eocene. At present, a detailed knowledge of tomistomine palaeobiogeography is hindered by the lack of modern taxonomic revisions of some fossil remains and therefore by the poor understanding of phylogenetic relationships. Key words: Crocodylidae, -
The Serrated Teeth Ofsebecus and the Iberoccitanian Crocodile. A
STVDIA GEOLÓGICA SALMANTICENSIA, XXIX, 127-144 (1994) THE SERRATED TEETH OF SEBECUS AND THE IBEROCCITANIAN CROCODILE, A MORPHOLOGICAL AND ULTRASTRUCTURAL COMPARISON O. LEGASA (*) A. D. BUSCALIONI (*) Z. GASPARINI (**) RESUMEN:- Se compara la morfología y ultraestructura del esmalte de dientes aserrados de cocodrilos. La muestra está compuesta por coronas aisladas atribuidas a la forma iberoccitana (Eoceno de la cuenca del Duero) y Sebecus (S. ?huilensis y S. icaeorhinus del Mioceno medio de Colombia y Eoceno inferior de Argentina). Se examinaron caracteres cuantitativos y cualitativos de la corona y sus márgenes aserrados. En este sentido, se han explorado todas las variables que caracterizan la simetría de la corona dentaria, diferenciando los dientes más grandes de Sebecus ?huilensis de los de la forma iberoccitana. El análisis de la ultraestructura evidencia una organización pseudoprismática del esmalte de Sebecus ?huilensis, contrastando con el modelo aprismático del cocodrilo iberoccitano. En este artículo se definen los dientes aserrados como aquellos que poseen carenas con dentículos aislados. Un dentículo aislado es una unidad morfológica discreta. Esta definición excluye los dientes con carenas crenulados formadas por crestas anastomosadas convergentes, que proceden de la ornamentación del esmalte. También, se evalúan aspectos funcionales de los dientes considerando los microdesgastes observados en los dentículos aislados. ABSTRACT:- The morphology and enamel ultrastructure of serrated teeth of crocodiles is compared. The sample is composed by isolated teeth attributed to the iberoccitanian form (Eocene of the Duero basin, Spain) and Sebecus (S. ?huilensis and (*): Unidad de Paleontología. Dpto. Biología. Universidad Autónoma, Cantoblanco 28049 Madrid, Spain. (**): Museo de La Plata, Paseo del Bosque s/n. 1900 La Plata. -
On a New Melanosuchus Species (Alligatoroidea: Caimaninae) from Solimões Formation (Eocene-Pliocene), Northern Brazil, and Evolution of Caimaninae
Zootaxa 4894 (4): 561–593 ISSN 1175-5326 (print edition) https://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2020 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4894.4.5 http://zoobank.org/urn:lsid:zoobank.org:pub:19BD5D89-5C9C-4111-A271-98E819A03D8E On a new Melanosuchus species (Alligatoroidea: Caimaninae) from Solimões Formation (Eocene-Pliocene), Northern Brazil, and evolution of Caimaninae JONAS PEREIRA DE SOUZA-FILHO1,2*, EDSON GUILHERME1,3, PETER MANN DE TOLEDO5, ISMAR DE SOUZA CARVALHO6, FRANCISCO RICARDO NEGRI7, ANDRÉA APARECIDA DA ROCHA MACIENTE1,4, GIOVANNE M. CIDADE8, MAURO BRUNO DA SILVA LACERDA9 & LUCY GOMES DE SOUZA10* 1Laboratório de Pesquisas Paleontológicas (LPP), Centro de Ciências Biológicas e da Natureza, Universidade Federal do Acre, BR 364, Km 04, 69.920-900, Rio Branco, Acre, Brazil. 2 �[email protected]; https://orcid.org/0000-0003-0481-3204 3 �[email protected]; https://orcid.org/0000-0001-8322-1770 4 �[email protected]; https://orcid.org/0000-0003-3504-1833 5INPE—Instituto Nacional de Pesquisas Espaciais, MCT, São José dos Campos, São Paulo, Brazil. �[email protected]; https://orcid.org/0000-0003-4265-2624 6Departamento de Geologia, CCMN–IGEO, Universidade Federal do Rio de Janeiro, 21.910-200, Cidade Universitária—Ilha do Fundão, Rio de Janeiro, Rio de Janeiro, Brazil. �[email protected]; https://orcid.org/0000-0002-1811-0588 7Laboratório de Paleontologia, Universidade Federal do Acre—Campus Floresta, 69895-000, Cruzeiro do Sul, Acre, Brazil. �[email protected]; https://orcid.org/0000-0001-9292-7871 8Laboratório de Estudos Paleobiológicos, Departamento de Biologia, Universidade Federal de São Carlos—Campus Sorocaba, 18052–780, Sorocaba, São Paulo, Brazil. -
Pleistocene Ziphodont Crocodilians of Queensland
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Molnar, R. E. 1982. Pleistocene ziphodont crocodilians of Queensland. Records of the Australian Museum 33(19): 803–834, October 1981. [Published January 1982]. http://dx.doi.org/10.3853/j.0067-1975.33.1981.198 ISSN 0067-1975 Published by the Australian Museum, Sydney. nature culture discover Australian Museum science is freely accessible online at www.australianmuseum.net.au/Scientific-Publications 6 College Street, Sydney NSW 2010, Australia PLEISTOCENE ZIPHODONT CROCODllIANS OF QUEENSLAND R. E. MOLNAR Queensland Museum Fortitude Valley, Qld. 4006 SUMMARY The rostral portion of a crocodilian skull, from the Pleistocene cave deposits of Tea Tree Cave, near Chillagoe, north Queensland, is described as the type of the new genus and species, Quinkana fortirostrum. The form of the alveoli suggests that a ziphodont dentition was present. A second specimen, referred to Quinkana sp. from the Pleistocene cave deposits of Texas Caves, south Queensland, confirms the presence of ziphodont teeth. Isolated ziphodont teeth have also been found in eastern Queensland from central Cape York Peninsula in the north to Toowoomba in the south. Quinkana fortirostrum is a eusuchian, probably related to Pristichampsus. The environments of deposition of the beds yielding ziphodont crocodilians do not provide any evidence for (or against) a fully terrestrial habitat for these creatures. The somewhat problematic Chinese Hsisosuchus chungkingensis shows three apomorphic sebe.cosuchian character states, and is thus considered a sebecosuchian. INTRODUCTION The term ziphodont crocodilian refers to those crocodilians possessing a particular adaptation in which a relatively deep, steep sided snout is combined with laterally flattened, serrate teeth (Langston, 1975). -
Phylogenetic Analysis of a New Morphological Dataset Elucidates the Evolutionary History of Crocodylia and Resolves the Long-Standing Gharial Problem
Phylogenetic analysis of a new morphological dataset elucidates the evolutionary history of Crocodylia and resolves the long-standing gharial problem Jonathan P. Rio1 and Philip D. Mannion2* 1Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London, SW7 2AZ, UK 2Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK *Corresponding author (email address: [email protected]) ABSTRACT First appearing in the latest Cretaceous, Crocodylia is a clade of mostly semi-aquatic, predatory reptiles, defined by the last common ancestor of extant alligators, caimans, crocodiles, and gharials. Despite large strides in resolving extant and fossil crocodylian interrelationships over the last three decades, several outstanding problems persist in crocodylian systematics. Most notably, there has been persistent discordance between morphological and molecular datasets surrounding the affinities of the extant gharials, Gavialis gangeticus and Tomistoma schlegelii. Whereas molecular data consistently support a sister relationship between the extant gharials, which appear to be more closely related to crocodylids than to alligatorids, morphological data indicate that Gavialis is the sister taxon to all other extant crocodylians. Here we present a new morphological dataset for Crocodylia, based on a critical reappraisal of published crocodylian character data matrices and extensive first-hand observations of a global sample of crocodylians. This comprises the most taxonomically comprehensive crocodylian dataset to date (144 OTUs scored for 330 characters) and includes a new, illustrated character list with modifications to the construction and scoring of characters, and 46 novel characters. Under a maximum parsimony framework, our analyses robustly recover Gavialis as more closely related to Tomistoma than to other extant crocodylians for the first time based on morphology alone. -
Old African Fossils Provide New Evidence for the Origin of the American Crocodiles Massimo Delfno1,2*, Dawid A
www.nature.com/scientificreports OPEN Old African fossils provide new evidence for the origin of the American crocodiles Massimo Delfno1,2*, Dawid A. Iurino3,4*, Bruno Mercurio3, Paolo Piras5,6, Lorenzo Rook7 & Rafaele Sardella3,8 Molecular and morphological phylogenies concur in indicating that the African lineages formerly referred to Crocodylus niloticus are the sister taxon the four Neotropical crocodiles (Crocodylus intermedius, C. moreleti, C. acutus and C. rhombifer), implying a transoceanic dispersal from Africa to America. So far the fossil record did not contribute to identify a possible African forerunner of the Neotropical species but, curiously, the oldest remains referred to the African C. niloticus are Quaternary in age, whereas the oldest American fossils of Crocodylus are older, being dated to the early Pliocene, suggesting that another species could be involved. We re-described, also thanks to CT imaging, the only well-preserved topotipic skull of Crocodylus checchiai Maccagno, 1947 from the late Miocene (Messinian) African site of As Sahabi in Libya. As previously suggested on the basis of late Miocene material from Tanzania, C. checchiai is a valid, diagnosable species. According to our phylogenetic analyses, C. checchiai is related to the Neotropical taxa and could be even located at the base of their radiation, therefore representing the missing link between the African and the American lineages. Extant crocodylians are represented by 25 species grouped into 9 genera 1. Te most speciose and widespread genus is Crocodylus Laurenti, 1768 that hosts 12 species inhabiting a longitudinally very broad intertropical belt ranging from Australia to South Asia, to Africa and then America. -
Leidyosuchus (Crocodylia: Alligatoroidea) from the Upper Cretaceous Kaiparowits Formation (Late Campanian) of Utah, USA
PaleoBios 30(3):72–88, January 31, 2014 © 2014 University of California Museum of Paleontology Leidyosuchus (Crocodylia: Alligatoroidea) from the Upper Cretaceous Kaiparowits Formation (late Campanian) of Utah, USA ANDREW A. FARKE,1* MADISON M. HENN,2 SAMUEL J. WOODWARD,2 and HEENDONG A. XU2 1Raymond M. Alf Museum of Paleontology, 1175 West Baseline Road, Claremont, CA 91711 USA; email: afarke@ webb.org. 2The Webb Schools, 1175 West Baseline Road, Claremont, CA 91711 USA Several crocodyliform lineages inhabited the Western Interior Basin of North America during the late Campanian (Late Cretaceous), with alligatoroids in the Kaiparowits Formation of southern Utah exhibiting exceptional diversity within this setting. A partial skeleton of a previously unknown alligatoroid taxon from the Kaiparowits Formation may represent the fifth alligatoroid and sixth crocodyliform lineage from this unit. The fossil includes the lower jaws, numerous osteoderms, vertebrae, ribs, and a humerus. The lower jaw is generally long and slender, and the dentary features 22 alveoli with conical, non-globidont teeth. The splenial contributes to the posterior quarter of the mandibu- lar symphysis, which extends posteriorly to the level of alveolus 8, and the dorsal process of the surangular is forked around the terminal alveolus. Dorsal midline osteoderms are square. This combination of character states identifies the Kaiparowits taxon as the sister taxon of the early alligatoroid Leidyosuchus canadensis from the Late Cretaceous of Alberta, the first verified report of theLeidyosuchus (sensu stricto) lineage from the southern Western Interior Basin. This phylogenetic placement is consistent with at least occasional faunal exchanges between northern and southern parts of the Western Interior Basin during the late Campanian, as noted for other reptile clades. -
UC Berkeley Paleobios
UC Berkeley PaleoBios Title Leidyosuchus (Crocodylia: Alligatoroidea) from the Upper Cretaceous Kaiparowits Formation (late Campanian) of Utah, USA Permalink https://escholarship.org/uc/item/0q11x9vs Journal PaleoBios, 30(3) ISSN 0031-0298 Authors Farke, Andrew A. Henn, Madison M. Woodward, Samuel J. et al. Publication Date 2014-01-30 DOI 10.5070/P9303016247 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 30(3):72–88, January 31, 2014 © 2014 University of California Museum of Paleontology Leidyosuchus (Crocodylia: Alligatoroidea) from the Upper Cretaceous Kaiparowits Formation (late Campanian) of Utah, USA ANDREW A. FARKE,1* MADISON M. HENN,2 SAMUEL J. WOODWARD,2 and HEENDONG A. XU2 1Raymond M. Alf Museum of Paleontology, 1175 West Baseline Road, Claremont, CA 91711 USA; email: afarke@ webb.org. 2The Webb Schools, 1175 West Baseline Road, Claremont, CA 91711 USA Several crocodyliform lineages inhabited the Western Interior Basin of North America during the late Campanian (Late Cretaceous), with alligatoroids in the Kaiparowits Formation of southern Utah exhibiting exceptional diversity within this setting. A partial skeleton of a previously unknown alligatoroid taxon from the Kaiparowits Formation may represent the fifth alligatoroid and sixth crocodyliform lineage from this unit. The fossil includes the lower jaws, numerous osteoderms, vertebrae, ribs, and a humerus. The lower jaw is generally long and slender, and the dentary features 22 alveoli with conical, non-globidont teeth. The splenial contributes to the posterior quarter of the mandibu- lar symphysis, which extends posteriorly to the level of alveolus 8, and the dorsal process of the surangular is forked around the terminal alveolus.