Chapter 11 a PHYLOGENETIC REVISION of NORTH AMERICAN
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(Squamata: Mosasauridae) from the Late Cretaceous Of
C. R. Palevol 14 (2015) 483–493 Contents lists available at ScienceDirect Comptes Rendus Palevol www.sci encedirect.com General Palaeontology, Systematics and Evolution (Vertebrate Palaeontology) An halisaurine (Squamata: Mosasauridae) from the Late Cretaceous of Patagonia, with a preserved tympanic disc: Insights into the mosasaur middle ear Un halisauriné (Squamata : Mosasauridae) du Crétacé supérieur de Patagonie, à disque tympanique conservé : un aperc¸ u de l’oreille moyenne des mosasaures a,∗ b Marta S. Fernández , Marianella Talevi a CONICET - División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina b CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Isidro Lobo y Belgrano, 8332 General Roca, Río Negro, Argentina a b s t r a c t a r t i c l e i n f o Article history: Halisaurinae is a subfamily of enigmatic, small- to medium-sized mosasauroids, which Received 15 September 2014 retain a mosaic of primitive and derived features. The first record of a South American Hal- Accepted after revision 13 May 2015 isaurus with precise stratigraphic information includes a quadrate carrying a tympanic disc together with twelve vertebrae, collected in the Late Maastrichtian of Jagüel Formation Handled by Nathalie Bardet in northern Patagonia (Argentina). The preservation of a tympanic disc allows exploring and discussing the mechanisms of sound transmission in these mosasauroids. The loca- Keywords: tion of the tympanic disc resembles that one formed by the extracolumella of aquatic Halisaurus turtles and at least one extant lizard. Based on morphological comparison of the middle Patagonia ear we discuss previous hypotheses on the modification of the tympanic middle ear system Late Maastrichtian of mosasauroids for underwater hearing, in a manner similar to that observed in aquatic Cretaceous turtles. -
Three-Dimensionally Preserved Integument Reveals Hydrodynamic Adaptations in the Extinct Marine Lizard Ectenosaurus (Reptilia, Mosasauridae)
Fort Hays State University FHSU Scholars Repository Sternberg Museum of Natural History Faculty Publications Sternberg Museum of Natural History 12-1-2011 Three-Dimensionally Preserved Integument Reveals Hydrodynamic Adaptations in the Extinct Marine Lizard Ectenosaurus (Reptilia, Mosasauridae) Johan Lindgren Lunds Universitet Michael J. Everhart Fort Hays State University Michael W. Caldwell University of Alberta Follow this and additional works at: https://scholars.fhsu.edu/sternberg_facpubs Part of the Paleontology Commons Recommended Citation Lindgren, J., Everhart, M. J., & Caldwell, M. W. (2011). Three-Dimensionally Preserved Integument Reveals Hydrodynamic Adaptations in the Extinct Marine Lizard Ectenosaurus (Reptilia, Mosasauridae). PLOS ONE, 6(11), e27343. https://doi.org/10.1371/journal.pone.0027343 This Article is brought to you for free and open access by the Sternberg Museum of Natural History at FHSU Scholars Repository. It has been accepted for inclusion in Sternberg Museum of Natural History Faculty Publications by an authorized administrator of FHSU Scholars Repository. Three-Dimensionally Preserved Integument Reveals Hydrodynamic Adaptations in the Extinct Marine Lizard Ectenosaurus (Reptilia, Mosasauridae) Johan Lindgren1*, Michael J. Everhart2, Michael W. Caldwell3 1 Department of Earth and Ecosystem Sciences, Lund University, Lund, Sweden, 2 Sternberg Museum of Natural History, Fort Hays State University, Hays, Kansas, United States of America, 3 Department of Earth and Atmospheric Sciences, and Department of Biological -
Recent Mosasaur Discoveries from New Jersey and Delaware, USA: Stratigraphy, Taphonomy and Implications for Mosasaur Extinction
r fs| Netherlands Journal of Geosciences — Geologie en Mijnbouw | 84 - 3 | 241 - 245 | 2005 Recent mosasaur discoveries from New Jersey and Delaware, USA: stratigraphy, taphonomy and implications for mosasaur extinction W.B. Gallagher1' 1 Bureau of Natural History, New Jersey State Museum, Trenton, NJ 08625-0530, USA. Email: [email protected] 2 Department of Geological Sciences, Rutgers University, Piscataway, NJ 08855, USA. Manuscript received: December 2004; accepted: January 2005 Abstract The Upper Cretaceous deposits of New Jersey and Delaware produced the first mosasaur specimens collected in North America. Recent recovery of mosasaur specimens from streambank exposures and new excavation sites has increased our knowledge of the stratigraphic distribution of these animals in the northern Atlantic coastal plain. Reassessment of the source and age of mosasaur specimens from the Big Brook site and other localities in Monmouth County (NJ) has greatly increased the number of known Campanian mosasaur specimens from this region. Two main taphonomic occurrence modes are noted: 1 - single, worn and broken bones and isolated teeth in mixed faunal deposits probably accumulated due to current action in nearshore environments; 2 - partial skeletons, skulls and single bones in deeper-water settings were the aftermath of biological modification of carcasses and deadfalls. The mosasaurs of the New Egypt Formation represent some of the last (i.e., stratigraphically highest) mosasaur fossils in North America. Mosasaur extinction was due to the collapse of the rich Late Cretaceous marine food web at the K/T boundary. Subsequently in the early Paleocene, with the disappearance of the mosasaurs, crocodilians became the apical predators of the marine environment in this area. -
Allometric Growth in the Skull of Tylosaurus Proriger (Squamata: Mosasauridae) and Its Taxonomic Implications Robert F
Vertebrate Anatomy Morphology Palaeontology 6:75–90 75 ISSN 2292-1389 Allometric growth in the skull of Tylosaurus proriger (Squamata: Mosasauridae) and its taxonomic implications Robert F. Stewart1 and Jordan C. Mallon2,* 1Department of Earth Sciences, Carleton University, Ottawa, Ontario, Canada, K1S 5B6; [email protected] 2Palaeobiology, Canadian Museum of Nature, PO Box 3223, Station D, Ottawa, Ontario, Canada, K1P 6P4; [email protected] Abstract: Ontogeny—the growth and development of an organism—is among the more poorly understood aspects of the life history of mosasaurs, largely owing to a dearth of fossil material from young individuals. We describe the par- tial and nearly complete skulls of two subadult individuals of the mosasaurid Tylosaurus proriger from the upper Smoky Hills Chalk Member of the Niobrara Formation (upper Santonian) in Kansas. We include the more complete of the two specimens in an allometric analysis to better understand proportional changes in the skull through growth. Although our small sample size produces several instances of ‘soft isometry’, we recover the length of the edentulous rostrum as significantly negatively allometric, and quadrate height as significantly positively allometric. In light of our findings, we consider the question of whether T. kansasensis represents an immature ontogimorph of T. nepaeolicus, and find substan- tive evidence to reject this hypothesis. INTRODUCTION Seaway of North America (Williston 1898; Russell 1967; Everhart 2017). These are among the smallest skulls known Mosasauridae is a clade of carnivorous, mostly marine for the species, and they help to elucidate the allometric reptiles known from Upper Cretaceous deposits world- changes undergone by T. proriger through life. -
Cranial Anatomy of a Maastrichtian (Upper Cretaceous) Mosasaur (Squamata, Mosasauridae) from North-East Mexico
Revista Mexicana de Ciencias Geológicas,Cranial anatomy v. 24, núm.of a Maastrichtian 1, 2007, p. 89-103 mosasaur from north-east Mexico 89 Cranial anatomy of a Maastrichtian (Upper Cretaceous) mosasaur (Squamata, Mosasauridae) from north-east Mexico Marie-Céline Buchy1,*, Eberhard Frey2, Wolfgang Stinnesbeck3, and José Guadalupe López-Oliva4 1 Universität Karlsruhe, Geologisches Institut, Postfach 6980, D-76128 Karlsruhe, Germany. Current address: Museo del Desierto, Apartado Postal 307, 25000 Saltillo, Coahuila, Mexico. 2 Geowissenschaftliche Abteilung, Staatliches Museum für Naturkunde, Erbprinzenstrasse 13, D-76133 Karlsruhe, Germany. 3 Universität Karlsruhe, Geologisches Institut, Postfach 6980, D-76128 Karlsruhe, Germany. 4 Universidad Autónoma de Nuevo León, Facultad de Ciencias de la Tierra, Apartado Postal 104, 67700 Linares, N.L., Mexico. * [email protected] ABSTRACT We here describe the first mosasaur from Mexico known by significant cranial remains, from the late Early Maastrichtian Méndez Formation of Nuevo León, north-east Mexico. The specimen comprises a fragmentary skull and parts of the mandibles. Some anatomical features suggest a juvenile animal. The skull possesses a rostral tuberosity on the premaxilla, as well as a combination of features known from different mosasaur genera, like its frontopremaxillary suture situated caudal to the external naris, its prefrontal and postorbitofrontal being in contact lateral to the orbit, associated with the supra- and infrastapedial processes of its quadrate which almost contact one another. Despite being clearly distinct from any hitherto described mosasaur, the affinities of this specimen with other mosasaurs remain obscure, not only because of incompleteness, but also because of the poorly understood biological significance of the characters used for the classification of Mosasauridae. -
A Tyrannosauroid Metatarsus from the Merchantville Formation of Delaware Increases the Diversity of Non-Tyrannosaurid Tyrannosauroids on Appalachia
A tyrannosauroid metatarsus from the Merchantville Formation of Delaware increases the diversity of non-tyrannosaurid tyrannosauroids on Appalachia Chase D. Brownstein Collections and Exhibitions, Stamford Museum & Nature Center, Stamford, CT, USA ABSTRACT During the Late Cretaceous, the continent of North America was divided into two sections: Laramidia in the west and Appalachia in the east. Although the sediments of Appalachia recorded only a sparse fossil record of dinosaurs, the dinosaur faunas of this landmass were different in composition from those of Laramidia. Represented by at least two taxa (Appalachiosaurus montgomeriensis and Dryptosaurus aquilunguis), partial and fragmentary skeletons, and isolated bones, the non-tyrannosaurid tyrannosauroids of the landmass have attracted some attention. Unfortunately, these eastern tyrants are poorly known compared to their western contemporaries. Here, one specimen, the partial metatarsus of a tyrannosauroid from the Campanian Merchantville Formation of Delaware, is described in detail. The specimen can be distinguished from A. montgomeriensis and D. aquilunguis by several morphological features. As such, the specimen represents a potentially previously unrecognized taxon of tyrannosauroid from Appalachia, increasing the diversity of the clade on the landmass. Phylogenetic analysis and the morphology of the bones suggest the Merchantville specimen is a tyrannosauroid of “intermediate” grade, thus supporting the notion that Appalachia was a refugium Submitted 18 July 2017 for relict dinosaur -
A Mosasaur from the Lewis Shale
(1974)recently reported a number of ammo- nites and other invertebratesfrom the Lewis A mosasaurfrom the Lewis Shale Shale along the easternedge of the San Juan Basin. UNM-V-070 is southeastof their lo- (UpperGretaceous), northwestern cality D4l5l and northeastof their locality D5067. Both D4l5l and D5087 are strati- graphically higher in the Lewis Shale than NewMexico Uf.ftU-V-OZOand are placed by Cobban and History,Yale University' others (1974) in the Late Campanian Didy- by'NewHaven,CT,andPeterK.Reser,OiiartmentotAnthropology,University0fNewMexico,Albuquerque,NMSpencer G Lucas,Department of Geology and Geophysics and Peabody Museum of Natural mocerascheyennense ammonite zone. Prob- ably UNM-V-070 is Late Campanianin age (no older strata are known in the Lewis Shale) Mosasaursare an extinct group of giant The following abbreviationsare usedin the (Cobban and others, 1974)and older than the a marinelizards that flourishedduring the Late text: AMNH-Department of VertebratePa- D. cheyennense zone. Unfortunately, out- Cretaceous. Their fossilized remains are leontology, American Museum of Natural diligent searchof the limited Lewis Shale yielded un- known from all the continentsexcept Antarc- History, New York; UNM-Department of crops around UNM-V-070 only tica; the largestand best known collections Geology,University of New Mexico, Albu- diagnostic fragments of inoceramid shells; precisely come from the Niobrara Formation in Kan- querque;YPM-Peabody Museumof Natural hence,its age cannot be more deter- sas. Although marine sediments of Late History,Yale University, New Haven. mined. cretaceousage are exposedthroughout large areas of New Mexico, only three mosasaur LewisShale and its fauna specimenshave previously been reported from The Lewis Shale was named by Cross and the state. -
I Exploring the Relationship Between Paleobiogeography, Deep-Diving
Exploring the Relationship between Paleobiogeography, Deep-Diving Behavior, and Size Variation of the Parietal Eye in Mosasaurs By Andrew M. Connolly Submitted to the graduate degree program in Geology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Arts. __________________________________ Stephen T. Hasiotis, Chairperson __________________________________ Rafe M. Brown __________________________________ Jennifer A. Roberts Date Defended: March 25, 2016 i The Thesis Committee for Andrew M. Connolly certifies that this is the approved version of the following thesis: Exploring the Relationship between Paleobiogeography, Deep-Diving Behavior, and Size Variation of the Parietal Eye in Mosasaurs __________________________________ Stephen T. Hasiotis, Chairperson Date Approved: March 25, 2016 ii ABSTRACT Andrew M. Connolly, M.S. Department of Geology, March 2015 University of Kansas The parietal eye (PE) in modern squamates (Reptilia) plays a major role in regulating body temperature, maintaining circadian rhythms, and orientation via the solar axis. This study is the first to determine the role, if any, of the PE in an extinct group of lizards. We analyzed variation in relative size of the parietal foramen (PF) of five mosasaur genera to explore the relationship between PF size and paleolatitudinal distribution. We also surveyed the same specimens for the presence of avascular necrosis—a result of deep- diving behavior—in the vertebrae. Plioplatecarpus had the largest PF followed by Platecarpus, Tylosaurus, Mosasaurus, and Clidastes. A weak relationship exists between paleolatitudinal distribution and PF size among genera, as Plioplatecarpus had the highest paleolatitudinal distribution (~78°N) and the largest PF among genera. -
Giant Mosasaurus Hoffmanni (Squamata, Mosasauridae) from the Late Cretaceous (Maastrichtian) of Penza, Russia
Proceedings of the Zoological Institute RAS Vol. 318, No. 2, 2014, рр. 148–167 УДК 568.113.3 GIANT MOSASAURUS HOFFMANNI (SQUAMATA, MOSASAURIDAE) FROM THE LATE CRETACEOUS (MAASTRICHTIAN) OF PENZA, RUSSIA D.V. Grigoriev Saint Petersburg State University, Universitetskaya Emb. 7-9, 199034 Saint Petersburg, Russia; e-mail: [email protected] ABSTRACT This study provides a morphological description of the fragmentary skull of a mosasaur discovered in 1927 in the Upper Cretaceous (Maastrichtian) deposits in the city of Penza (Russia). Some bones from the original material had been lost since their discovery; their description is based on plaster casts. The Penza mosasaur displays characteristic features of Mosasaurus hoffmanni such as the posterior carina that shifts from a somewhat lateral position in the anterior teeth to a posterior position further along the tooth row, a frontal with convex lateral margins, and a powerfully built dentary. This is the first unequivocal record of this taxon from Russia. M. hoffmanni from the Penza is one of the largest mosasaurs ever known with an overall length of the body about 17 m. Key words: Maastrichtian, Cretaceous, Penza, Mosasaurus hoffmanni, Mosasauridae ГИГАНТСКИЙ MOSASAURUS HOFFMANNI (SQUAMATA, MOSASAURIDAE) ИЗ ПОЗДНЕГО МЕЛА (МААСТРИХТА) ПЕНЗЫ, РОССИЯ Д.В. Григорьев Санкт-Петербургский Государственный Университет, Университетская наб. 7-9, 199034 Санкт-Петербург, Россия; e-mail: [email protected] РЕЗЮМЕ Приведено детальное морфологическое описание фрагментарного черепа мозазавра, найденного в 1927 г. в верхнемеловых отложениях (маастрихт) г. Пенза, Россия. Часть оригинальных костей была впоследствии утрачена; их описание выполнено по сохранившимся гипсовым слепкам. На основании изменения положе- ния зубной карины от передних к задним зубам, лобной кости с выгнутыми боковыми сторонами и массив- ных зубных костей пензенская особь отнесена к Mosasaurus hoffmanni. -
Dale Alan Russell (1937-2019): Voyageur of a Vanished World
Canadian Journal of Earth Sciences Dale Alan Russell (1937-2019): Voyageur of a Vanished World Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2020-0163.R1 Manuscript Type: Tribute Date Submitted by the 26-Nov-2020 Author: Complete List of Authors: Cumbaa, Stephen L.; Canadian Museum of Nature, Currie, Philip J.; University of Alberta, Biological Sciences Dodson, Peter; University of Pennsylvania School of Veterinary Medicine, Department of Biomedical Sciences; University of Pennsylvania, DepartmentDraft of Biomedical Sciences Mallon, Jordan; Canadian Museum of Nature Keyword: Dale Alan Russell, biography, dinosaurs, mosasaurs, extinction, evolution Is the invited manuscript for consideration in a Special Tribute to Dale Russell Issue? : © The Author(s) or their Institution(s) Page 1 of 37 Canadian Journal of Earth Sciences 1 Dale Alan Russell (1937-2019): Voyageur of a Vanished World 2 Stephen L. Cumbaa1, Philip J. Currie2, Peter Dodson3,4, Jordan C. Mallon1,5,* 3 4 1Beaty Centre for Species Discovery and Palaeobiology Section, Canadian Museum of Nature, 5 P.O. Box 3443, Station D, Ottawa, ON K1P 6P4, Canada 6 2University of Alberta, CW 405, Biological Sciences Building, Edmonton, AB T6G 2E9, Canada 7 3Department of Biomedical Sciences, University of Pennsylvania School of Veterinary 8 Medicine, Philadelphia, PA 19104, USA 9 4Department of Earth and EnvironmentalDraft Science, School of Arts and Sciences, University of 10 Pennsylvania, Philadelphia, PA 19104, USA 11 5Department of Earth Sciences, Carleton University, 2115 Herzberg Laboratories, 1125 Colonel 12 By Drive, Ottawa, ON K1S 5B6, Canada 13 14 *Corresponding author 15 1 © The Author(s) or their Institution(s) Canadian Journal of Earth Sciences Page 2 of 37 16 Abstract 17 We review the distinguished and varied career of our friend and colleague, 18 palaeontologist Dr. -
A Late Cretaceous Mosasaur from North-Central New Mexico
New Mexico Geological Society Guidebook, 46th Field Conference, Geology of the Santa Fe Region, 1995 257 A LATE CRETACEOUS MOSASAUR FROM NORTH-CENTRAL NEW MEXICO SPENCER G. LUCASl, ANDREW B. HECKERT2 and BARRY S. KUES2 New Mexico Museum of Natural History and Science, 1801 Mountain Road N.W., Albuquerque, New Mexico 87104; 2Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87l31-1116 Abstract-We describe a partial vertebral column of a mosasaur identified as cf. Tylosaurus sp. from the lower Niobrara interval of the Mancos Shale south of Galisteo in Santa Fe County, New Mexico. Invertebrate fossils collected from the same horizon include the inoceramids cf. Inoceramus (Cremnoceramus) deformis and cf. Inoceramus (Platyceramus ) platinus and dense growths of the oyster Pseudoperna congesta. They suggest a Coniacian age. This is the oldest documented mosasaur from New Mexico. INTRODUCTION more, comparison of NMMNH P-22142 to Williston's (1898) plates Mosasaurs were marine lizards of the Late Cretaceous that first ap shows that in Tylosaurus the rib articulations on the dorsal vertebrae are peared during the Cenomanian (Russell, 1967, 1993). Although marine large, dorsally positioned and circular in cross section. NMMNH P-22142 Upper Cretaceous strata are widely exposed in New Mexico, the fossil is also very similar to specimens of Tylosaurus proriger illustrated by record of mosasaurs from the state is limited to a handful of documented Williston (1898, pIs. 62, 65, 72) in that no traces of a zygosphene occurrences (Lucas and Reser, 1981; Hunt and Lucas, 1993). Here, we zygantrum articulation can be seen on any of the vertebrae, and the neu add to this limited record notice of incomplete remains of a mosasaur ral spines are very long antero-posteriorly so that their edges almost meet. -
Post-Gondwana Africa and the Vertebrate History of the Angolan Atlantic Coast
Memoirs of Museum Victoria 74: 343–362 (2016) Published 2016 ISSN 1447-2546 (Print) 1447-2554 (On-line) http://museumvictoria.com.au/about/books-and-journals/journals/memoirs-of-museum-victoria/ Post-Gondwana Africa and the vertebrate history of the Angolan Atlantic Coast LOUIS L. JACOBS1,*, MICHAEL J. POLCYN1, OCTÁVIO MATEUS2, ANNE S. SCHUlp3, ANTÓNIO OLÍmpIO GONÇALVES4 AND MARIA LUÍSA MORAIS4 1 Roy M. Huffington Department of Earth Sciences, Southern Methodist University, Dallas, Texas 75275, United States ([email protected]; [email protected]) 2 GeoBioTec, Faculdade de Ciências e Tecnologia, Universidade Nova de Lisboa, and Museu da Lourinhã, Rua João Luis de Moura, 2530-157, Lourinhã, Portugal ([email protected]) 3 Naturalis Biodiversity Center, P.O. Box 9517, NL-2300 RA Leiden, The Netherlands; Natuurhistorisch Museum Maastricht, de Bosquetplein 6-7, NL-6211 KJ Maastricht, The Netherlands; Faculty of Earth and Life Sciences, VU University Amsterdam, de Boelelaan 1085, NL-1081 HV Amsterdam, The Netherlands ([email protected]) 4 Departamento de Geologia, Faculdade de Ciências, Universidade Agostinho Neto, Avenida 4 de Fevereiro 7, Luanda, Angola ([email protected]; [email protected]) * To whom correspondence should be addressed. E-mail: [email protected] Abstract Jacobs, L.L., Polcyn, M.J., Mateus, O., Schulp, A.S., Gonçalves, A.O. and Morais M.L. 2016. Post-Gondwana Africa and the vertebrate history of the Angolan Atlantic Coast. Memoirs of Museum Victoria 74: 343–362. The separation of Africa from South America and the growth of the South Atlantic are recorded in rocks exposed along the coast of Angola. Tectonic processes that led to the formation of Africa as a continent also controlled sedimentary basins that preserve fossils.