Enamel Microstructure of the Late Cretaceous Multituberculate Mammal Kogaionon
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Dome-Headed, Small-Brained Island Mammal from the Late Cretaceous of Romania
Dome-headed, small-brained island mammal from the Late Cretaceous of Romania Zoltán Csiki-Savaa,1, Mátyás Vremirb, Jin Mengc, Stephen L. Brusatted, and Mark A. Norellc aLaboratory of Paleontology, Faculty of Geology and Geophysics, University of Bucharest, 010041 Bucharest, Romania; bDepartment of Natural Sciences, Transylvanian Museum Society, 400009 Cluj-Napoca, Romania; cDivision of Paleontology, American Museum of Natural History, New York, NY 10024; and dSchool of GeoSciences, Grant Institute, University of Edinburgh, EH9 3FE Edinburgh, United Kingdom Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved March 26, 2018 (received for review January 20, 2018) The island effect is a well-known evolutionary phenomenon, in describe the anatomy of kogaionids in detail, include them in a which island-dwelling species isolated in a resource-limited envi- comprehensive phylogenetic analysis, estimate their body sizes, ronment often modify their size, anatomy, and behaviors compared and present a reconstruction of their brain and sense organs. with mainland relatives. This has been well documented in modern This species exhibits several features that we interpret as re- and Cenozoic mammals, but it remains unclear whether older, more lated to its insular habitat, most notably a brain that is sub- primitive Mesozoic mammals responded in similar ways to island stantially reduced in size compared with close relatives and habitats. We describe a reasonably complete and well-preserved skeleton of a kogaionid, an enigmatic radiation of Cretaceous island- mainland contemporaries, demonstrating that some Mesozoic dwelling multituberculate mammals previously represented by frag- mammals were susceptible to the island effect like in more mentary fossils. -
Enamel Ultrastructure of Multituberculate Mammals: an Investigation of Variability
CO?JTRIBI!TIONS FROM THE MUSEUM OF PALEOK.1-OLOCiY THE UNIVERSITY OF MICHIGAN VOL. 27. NO. 1, p. 1-50 April I, 1985 ENAMEL ULTRASTRUCTURE OF MULTITUBERCULATE MAMMALS: AN INVESTIGATION OF VARIABILITY BY SANDRA J. CARLSON and DAVID W. KRAUSE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRlBUTlONS FROM THE MUSEUM OF PALEON I OLOGY Philip D. Gingerich, Director Gerald R. Smith. Editor This series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan, 48109. VOLS. 11-XXVI. Parts of volumes may be obtained if available. Price lists available upon inquiry. CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN Vol . 27, no. 1, p. 1-50, pub1 ished April 1, 1985, Sandra J. Carlson and David W. Krause (Authors) ERRATA Page 11, Figure 4 caption, first line, should read "(1050X)," not "(750X)." ENAMEL ULTRASTRUCTURE OF MULTITUBERCULATE MAMMALS: AN INVESTIGATION OF VARIABILITY BY Sandra J. Carlsonl and David W. Krause' Abstract.-The nature and extent of enamel ultrastructural variation in mammals has not been thoroughly investigated. In this study we attempt to identify and evaluate the sources of variability in enamel ultrastructural patterns at a number of hierarchic levels within the extinct order Multituberculata. -
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. -
Mammals from the Mesozoic of Mongolia
Mammals from the Mesozoic of Mongolia Introduction and Simpson (1926) dcscrihed these as placental (eutherian) insectivores. 'l'he deltathcroids originally Mongolia produces one of the world's most extraordi- included with the insectivores, more recently have narily preserved assemblages of hlesozoic ma~nmals. t)een assigned to the Metatheria (Kielan-Jaworowska Unlike fossils at most Mesozoic sites, Inany of these and Nesov, 1990). For ahout 40 years these were the remains are skulls, and in some cases these are asso- only Mesozoic ~nanimalsknown from Mongolia. ciated with postcranial skeletons. Ry contrast, 'I'he next discoveries in Mongolia were made by the Mesozoic mammals at well-known sites in North Polish-Mongolian Palaeontological Expeditions America and other continents have produced less (1963-1971) initially led by Naydin Dovchin, then by complete material, usually incomplete jaws with den- Rinchen Barsbold on the Mongolian side, and Zofia titions, or isolated teeth. In addition to the rich Kielan-Jaworowska on the Polish side, Kazi~nierz samples of skulls and skeletons representing Late Koualski led the expedition in 1964. Late Cretaceous Cretaceous mam~nals,certain localities in Mongolia ma~nmalswere collected in three Gohi Desert regions: are also known for less well preserved, but important, Bayan Zag (Djadokhta Formation), Nenlegt and remains of Early Cretaceous mammals. The mammals Khulsan in the Nemegt Valley (Baruungoyot from hoth Early and Late Cretaceous intervals have Formation), and llcrmiin 'ISav, south-\vest of the increased our understanding of diversification and Neniegt Valley, in the Red beds of Hermiin 'rsav, morphologic variation in archaic mammals. which have heen regarded as a stratigraphic ecluivalent Potentially this new information has hearing on the of the Baruungoyot Formation (Gradzinslti r't crl., phylogenetic relationships among major branches of 1977). -
A Aardvark, 96 Abderites, 15, 162 Abderitidae, 11, 159, 200 Aboriginal, 15, 17 Adamantina, 79, 83 Africa, 79, 96, 116, 127, 130
Index A Antarctic Circumpolar Current (ACC), 126, Aardvark, 96 188, 210 Abderites, 15, 162 Antarctic Counter Current, 104 Abderitidae, 11, 159, 200 Antarctic Peninsula, 12, 80, 83, 97, 109, Aboriginal, 15, 17 113–116, 165, 187, 216 Adamantina, 79, 83 Antarctic Region, 113, 133 Africa, 79, 96, 116, 127, 130, 141 Antarctodonas, 110 Afrotemperate Region, 133 Antechinus, 56 Afrothere, 96 Aonken Sea, 139 Afrotheria, 96, 97 Aptian, 79, 98, 129 Alamitan, 83, 90, 95, 141, 211 Aquatic, 130 Alchornea, 113 Araceae, 113 Alcidedorbignia, 94 Araucaria, 130 Alisphenoid, 10, 11 Arboreal, 6, 12, 38, 58–61, 64, 65 Allen, 80 Archaeodolops, 195 Allenian, 211 Archaeohyracidae, 143 Allotherian, 212 Archaeonothos, 109 Allqokirus, 95, 214 Arctodictis, 166 Alphadelphian, 214 Arecaceae, 113 Altiplano, 127 Argentina, 13, 17, 19, 22, 61, 80, 83, 95, 107, Altricial, 203 112, 116, 130, 135, 136, 138, 157 Ameghinichnus, 140 Argentodites, 212 Ameridelphia, 157, 165, 166, 186, 192, 195 Argyrolagidae, 13, 158, 196, 220 Ameridelphian, 91, 95, 106, 107, 110, 157, Argyrolagoidea, 13, 143, 195, 201, 220 166, 200, 213, 215, 216 Argyrolagus, 158, 220 Amphidolops, 195, 200 Arid diagonal, 135, 136, 138 Anachlysictis, 23, 161 Arminiheringia, 166, 194 Andean Range, 133 A1 scenario, 138 Andean Region, 127, 132, 133, 135, 136 Ascending ramus, 170 Andes, 12, 127 Asia, 6, 127, 156, 202 Andinodelphys, 95, 157, 159 Astragalar, 10 Angiosperm, 114, 115, 129, 190 Astrapotheria, 3 Angular process, 10, 11, 171, 175 Atacama Desert, 130, 133, 136 Animalivore, 47 Atlantic Forest, 61, 130 Animalivorous, 47 Atlantic Ocean, 137 Ankle bone, 96, 107 Atlantogenata, 97 Antarctica, 8, 12, 79, 98–100, 104, 109, 112, Australasia, 218 115, 116, 126, 127, 133, 135, 137, 210, 220 © Springer Science+Business Media Dordrecht 2016 227 F.J. -
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. -
Continental Tertiary Basins and Associated Deposits of Aragón and Catalunya
CHAPTER16 CONTINENTAL TERTIARY BASINS AND ASSOCIATED DEPOSITS OF ARAGÓN AND CATALUNYA Aragonian type series (stratotype) behind the village of Villafeliche, near the Jiloca river. Élez, J. One of the main problems in stratigraphy and paleon- surrounded by orogens (overthrusted units of the tology is the correlation between the sediments and Pyrenees to the north, the Iberian Mountain Range to faunas of continental and marine origin, originated the south, and the Catalan-Coastal Mountain Range by the difficulty to establish a parallelism between to the east). It responds to a general compression gen- the respective biostratigraphic scales. That is why the erated as a consequence of the shortening between stratigraphy of the continental Tertiary basins and the the Iberian and European plates. In this basin there associated vertebrate deposits in Aragón and Cataluña is an important paleontological area forming a wide are of great international relevance. fringe parallel to the Catalan orogen and attached to the Catalan-Coastal Mountain Range. There are some The Lower Tertiary (Paleogene) continental series of other more scattered but less important areas in the Aragón and Cataluña, with good exposures and abun- interior, both of Cataluña and Aragón. dant deposits, are exceptional cases in the European framework as their biostratigraphy is correlatable to The other model of continental Tertiary sedimenta- marine sediments. In the Upper Tertiary (Neogene), its tion for these regions corresponds to the so called importance is even bigger, since unique stratigraphic intramontane basins, with smaller tectonic graben or series crop out with numerous deposits which allowed semigraben morphologies and filled faster. As a norm, a better accuracy in the continental time scales. -
SKULL STRUCTURE and AFFINITIES of the M ULTITUBERCULATA (Plates I-V)
ZOFIA KIELAN -JAWOROWSKA SKULL STRUCTURE AND AFFINITIES OF THE M ULTITUBERCULATA (Plates I-V) Abstrac t. - The skull structure of two Upper Cretaceous multituberculate genera from the Gobi Desert, Mongo lia: Kamptobaatar KIELA N-JAWOROWSKAand Slo anbaatar KIELA N-JAWO ROWSKA is described in detail. The lateral wall of the braincase and the occipital region of multi tuberculat e skulls are described for the first time.The ant erior lamina of the petrosal in the mu ltitube rculates consists of two parts : the ventra l part and the ascend ing part. The ascending par t of the anterior lamina, previously unknown in the mult ituberculates, is present in Kamp tobaatar and it may be shown that the ascending part occup ies most of the lateral wall of the bra incase. The orbitosphenoid is large and not ent irely ossified, whilst the alisphenoid is reduced to a comp arat ively small, ventral element, which is, however, more extensive than that of the rnonotremes, The followin g reptilian element s: ectopterygoid, tabu lar and post-temporal fossa are found in the studied skulls. The multitubercula te bra incase is compared with tho se of the Docodonta (Morganucodon), Tr iconodonta and Monotremata and it is shown that the general pattern of the bra incase structure in these four orders is the same. However, the Multituberculata are more allied to the Mon otremata than they are to the Docodonta and the Triconodon ta. The opin ion that the Docodonta, Triconodonta, Multituberculata and Monotremata for m a subclass Prototheria, equi valent to the Theria , is supported. -
Multituberculate Mammals from the Cretaceous of Uzbekistan
Multituberculate mammals from the Cretaceous of Uzbekistan ZOFIA KIELAN- JAWOROWSKA and LEV A. NESSOV Kielan-Jaworowska, 2. & Nessov, L. A. 1992. Multituberculate mammals from the Cretaceous of Uzbelustan. Acta Palaeontologica Polonica 37, 1, 1- 17. The first western Asian multituberculates found in the Bissekty Formation (Co- niacian) of Uzbekistan are described on the basis of a lower premolar (p4), a fragment of a lower incisor, an edentulous dentary, a proximal part of the humerus and a proximal part of the femur. Uzbekbaatar kizylkumensis gen. et sp. n. is defined as having a low and arcuate p4. possibly without a posterobuccal cusp; it presumably had two lower premolars, as inferred from the presence of a triangular concavity at the upper part of the anterior wall of p4, and p3 less reduced in relation to p4 than in non-specialized Taeniolabidoidea and Ptilodontoidea. Uzbek- baatar is placed in the Cimolodonta without indicating family and infraorder. It might have originated from the Plagiaulacinae or Eobaatarinae. Key words : Multituberculata, Marnmalia, Cretaceous, Coniacian, Uzbekistan. Zofia Kielan-Jaworowska. Paleontologisk Museum, Universitetet i Oslo, Sars Gate 1, N-0562 Oslo, Norway. flec A. Hecoc, kf~cmumym3exnoiL Kopbl, Ca~~m-nemep6ypzc~uiiYnueepcumem, 199 034 Ca~~m-l7emep6ypz,Poccun (Lev A. Nessov, Institute of the Earth Crust, Sankt-Peters- burg University, 199 034 St. Petersburg. Russla]. Introduction The Multituberculata is the first mammalian order to have adapted to herbivorous niches, although many may have been omnivorous (Krause 1982). Known from the Late Triassic to the Early Oligocene (Hahn & Hahn 1983), this order of mammals was dominant throughout the Mesozoic in most of the local faunas studied. -
Teruel, Spain)
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/232388110 A systematic reassessment of Early Cretaceous multituberculates from Galve (Teruel, Spain) Article in Cretaceous Research · February 2011 DOI: 10.1016/j.cretres.2010.10.003 CITATIONS READS 12 34 3 authors: Ainara Badiola José Ignacio Canudo Universidad del País Vasco / Euskal Herriko… University of Zaragoza 15 PUBLICATIONS 109 CITATIONS 430 PUBLICATIONS 3,138 CITATIONS SEE PROFILE SEE PROFILE Gloria Cuenca-Bescós University of Zaragoza 300 PUBLICATIONS 4,166 CITATIONS SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: José Ignacio Canudo letting you access and read them immediately. Retrieved on: 29 July 2016 Author's personal copy Cretaceous Research 32 (2011) 45e57 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A systematic reassessment of Early Cretaceous multituberculates from Galve (Teruel, Spain) Ainara Badiola*, José Ignacio Canudo, Gloria Cuenca-Bescós Grupo Aragosaurus-IUCA,1 Paleontología, Facultad de Ciencias, Universidad de Zaragoza, Pedro Cerbuna 12, E-50009 Zaragoza, Spain article info abstract Article history: This paper includes a systematic reassessment of the Early Cretaceous (late Hauterivianeearly Barre- Received 19 April 2010 mian) multituberculate fossils of Galve (Teruel, Spain), previously studied by Crusafont-Pairó and Adr- Accepted in revised form 1 October 2010 over, and Crusafont-Pairó and Gibert in 1966 and 1976, respectively, as well the study of other Available online 4 November 2010 unpublished specimens found in the revised collection of Institut Català de Paleontologia (ICP). We here include for the first time the emended descriptions and comparisons as well as the SEM photographs of Keywords: all the specimens found in the collection and update the biostratigraphic data that they have provided. -
The Earliest Mammal of the European Paleocene: the Multituberculate Hainina
J. Paleont., 74(4), 2000, pp. 701–711 Copyright ᭧ 2000, The Paleontological Society 0022-3360/00/0074-0701$03.00 THE EARLIEST MAMMAL OF THE EUROPEAN PALEOCENE: THE MULTITUBERCULATE HAININA P. PELA´ EZ-CAMPOMANES,1 N. LO´ PEZ-MARTI´NEZ,2 M.A. A´ LVAREZ-SIERRA,2 R. DAAMS3 1Department Paleobiologı´a,Museo Nacional de Ciencias Naturales, Gutie´rrez Abascal 2, 28006 Madrid, Spain, Ͻ[email protected]Ͼ, and 2Department-UEI Paleontologı´a, Facultad C. Geolo´gicas-Instit. Geologı´a Econo´mica,Universidad Complutense-CSIC, 28040 Madrid, Spain ABSTRACT—A new species of multituberculate mammal, Hainina pyrenaica n. sp. is described from Fontllonga-3 (Tremp Basin, Southern Pyrenees, Spain), correlated to the later part of chron C29r just above the K/T boundary. This taxon represents the earliest European Tertiary mammal recovered so far, and is related to other Hainina species from the European Paleocene. A revision of the species of Hainina allows recognition of a new species, H. vianeyae n. sp. from the Late Paleocene of Cernay (France). The genus is included in the family Kogaionidae Ra˜dulescu and Samson, 1996 from the Late Cretaceous of Romania on the basis of unique dental characters. The Kogaionidae had a peculiar masticatory system with a large, blade-like lower p4, similar to that of advanced Ptilodon- toidea, but occluding against two small upper premolars, interpreted as P4 and P5, instead of a large upper P4. The endemic European Kogaionidae derive from an Early Cretaceous group with five premolars, and evolved during the Late Cretaceous and Paleocene. The genus Hainina represents a European multituberculate family that survived the K/T boundary mass extinction event. -
Masticatory Musculature of Asian Taeniolabidoid Multituberculate Mammals
Masticatory musculature of Asian taeniolabidoid multituberculate mammals PETR P. GAMBARYAN & ZOFIA KIELAN-JAWOROWSKA* Gambaryan, P.P. & Kielan-Jaworowska, 2. 1995. Masticatory musculature of Asian taeniolabidoid multituberculate mammals. Acta Palaeontologica Polonica 40, 1, 45-108. The backward chewing stroke in multituberculates (unique for mammals) resulted in a more anterior insertion of the masticatory muscles than in any other mammal group, including rodents. Multituberculates differ from tritylodontids in details of the masticatory musculature, but share with them the backward masticatory power stroke and retractory horizontal components of the resultant force of all the masticatory muscles (protractory in Theria). The Taeniolabididae differ from the Eucosmodontidae in having a more powerful masticatory musculature, expressed by the higher zygomatic arch with relatively larger anterior and middle zygomatic ridges and higher coronoid process. It is speculated that the bicuspid, or pointed upper incisors, and semi-procumbent, pointed lower ones, characteristic of non- taeniolabidoid mdtitliberculates were used for picking-up and killing insects or other prey. In relation to the backward power stroke the low position of the condylar process was advantageous for most multituberculates. In extreme cases (Sloanbaataridae and Taeniolabididae), the adaptation for crushing hard seeds, worked against the benefit of the low position of the condylar process and a high condylar process developed. Five new multituberculate autapomorphies are rec- ognized: anterior and intermediate zygomatic ridges: glenoid fossa large, flat and sloping backwards (forwards in rodents), arranged anterolateral and standing out from the braincase; semicircular posterior margin of the dentary with condylar process forming at least a part of it; anterior position of the coronoid process; and anterior position of the masseteric fossa.