At the Roots of the Mammalian Family Tree
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FROM the EARLY CRETACEOUS (BARREMIAN) WESSEX FORMATION OFTHEISLEOFWIGHT,SOUTHERNBRITAIN by STEVEN C
[Palaeontology, Vol. 49, Part 4, 2006, pp. 889–897] A GOBICONODONTID (MAMMALIA, EUTRICONODONTA) FROM THE EARLY CRETACEOUS (BARREMIAN) WESSEX FORMATION OFTHEISLEOFWIGHT,SOUTHERNBRITAIN by STEVEN C. SWEETMAN School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth PO1 3QL, UK; e-mail: [email protected] Typescript received 16 June 2004; accepted in revised form 20 June 2005 Abstract: Bulk screening of Early Cretaceous (Barremian) gobiconodontid mammal in Early Cretaceous deposits of strata of the Wessex Formation, exposed in sections on Britain sheds further light on the palaeogeographical distri- the south-west and south-east coasts of the Isle of Wight, bution of an apparently successful clade of Early Creta- southern England, has resulted in the recovery of mammal ceous mammals and together with the occurrence of a remains, the first to be obtained from Wealden Group gobiconodontid in the earliest Cretaceous of North Africa strata since the early 1970s. The fauna comprises at least calls into question recent hypotheses concerning the area six taxa represented by isolated teeth and in addition, in of origin of the Gobiconodontidae and mechanisms of dis- the case of an as yet undescribed spalacotheriid, a partial persal therefrom. dentary. One of the teeth, a distal premolar, is of unique tricuspid, single-rooted morphology and represents the first Key words: Britain, Cretaceous, Gobiconodontidae, Mam- British record of the Gobiconodontidae. Discovery of a malia, palaeogeography, premolar. The Early Cretaceous (Barremian, Wealden Group) which may or may not be of mammalian origin (pers. Wessex Formation of the Isle of Wight, southern England obs. -
New Gobiconodontid (Eutriconodonta, Mammalia) from the Lower
第58卷 第1期 古 脊 椎 动 物 学 报 pp. 45–66 2020年1月 VERTEBRATA PALASIATICA figs. 1–5 DOI: 10.19615/j.cnki.1000-3118.190724 New gobiconodontid (Eutriconodonta, Mammalia) from the Lower Cretaceous Shahai and Fuxin formations, Liaoning, China KUSUHASHI Nao1 WANG Yuan-Qing2,3,4* LI Chuan-Kui2 JIN Xun2 (1 Department of Earth’s Evolution and Environment, Graduate School of Science and Engineering, Ehime University Matsuyama, Ehime 790-8577, Japan [email protected]) (2 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044, China * Corresponding author: [email protected]) (3 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044, China) (4 College of Earth and Planetary Sciences, University of Chinese Academy of Sciences Beijing 100049, China) Abstract Eutriconodontans are one of the key members of mammals to our understanding of the evolution and transition of mammalian fauna in Asia during the Cretaceous. Two gobiconodontid and two triconodontid species have previously been reported from the upper Lower Cretaceous Shahai and Fuxin formations. Here we describe two additional eutriconodontans from the formations, Fuxinoconodon changi gen. et sp. nov. and ?Gobiconodontidae gen. et sp. indet. This new species is attributed to the Gobiconodontidae, characterized by having an enlarged first lower incisor, reduction in the number of incisors and premolariforms, proportionally large cusps b and c being well distant from cusp a on the molariforms, presence of a labial cingulid, and a unique mixed combination of molariform characters seen on either the first or the second, but not both, generations of molariforms in Gobiconodon. -
Dual Origin of Tribosphenic Mammals
articles Dual origin of tribosphenic mammals Zhe-Xi Luo*, Richard L. Cifelli² & Zo®a Kielan-Jaworowska³ *Section of Vertebrate Paleontology, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania 15213, USA ² Oklahoma Museum of Natural History, 2401 Chautauqua, Norman, Oklahoma 73072, USA ³ Institute of Paleobiology, Polish Academy of Sciences, ulica Twarda 51/55, PL-00-818 Warszawa, Poland ............................................................................................................................................................................................................................................................................ Marsupials, placentals and their close therian relatives possess complex (tribosphenic) molars that are capable of versatile occlusal functions. This functional complex is widely thought to be a key to the early diversi®cation and evolutionary success of extant therians and their close relatives (tribosphenidans). Long thought to have arisen on northern continents, tribosphenic mammals have recently been reported from southern landmasses. The great age and advanced morphology of these new mammals has led to the alternative suggestion of a Gondwanan origin for the group. Implicit in both biogeographic hypotheses is the assumption that tribosphenic molars evolved only once in mammalian evolutionary history. Phylogenetic and morphometric analyses including these newly discovered taxa suggest a different interpretation: that mammals with tribosphenic molars are not monophyletic. Tribosphenic -
Aspects of the Microvertebrate Fauna of the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, Southern England
ASPECTS OF THE MICROVERTEBRATE FAUNA OF THE EARLY CRETACEOUS (BARREMIAN) WESSEX FORMATION OF THE ISLE OF WIGHT, SOUTHERN ENGLAND By STEVEN CHARLES SWEETMAN M.A. (Oxon.) 1980 F.G.S. A thesis submitted in partial fulfilment of the requirements for the award of the degree of Doctor of Philosophy of the University of Portsmouth School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth, PO1 3QL, U.K. April, 2007 0 Disclaimer Whilst registered for this degree, I have not registered for any other award. No part of this work has been submitted for any other academic award. 1 Acknowledgements At inception of this project there was a significant risk that the Wessex Formation would not yield a microvertebrate fauna. I would, therefore, like to express special thanks to Dave Martill (University of Portsmouth) for his initial support and for securing the research scholarship which made this study possible. I would also like to thank him for his supervision, generous support, encouragement and advice thereafter. Special thanks also to Susan Evans (UCL) for her enthusiastic help and advice on all matters relating to microvertebrates in general, and lizards in particular, and to Jerry Hooker (NHM) for everything relating to mammals; also to Brian Gasson for his support in the field and for the generous donation of many exceptional specimens from his private collection. The broad scope of this study has engendered the help, support and advice of many others and I am grateful to all. At the University -
Diversity of Triconodont Mammals from the Early Cretaceous of North Africa - Affinities of the Amphilestids
DIVERSITY OF TRICONODONT MAMMALS FROM THE EARLY CRETACEOUS OF NORTH AFRICA - AFFINITIES OF THE AMPHILESTIDS by Denise SIGOGNEAU-RUSSELL* SUMMARY Page Abstract, Resume 28 Introduction ........ , .................. , .............. , ....................... 28 Systematic palaeontology .................. , ............ , ......... , ........... 29 Relationships of 'amphilestids' ....... , ........ , , , .......... , , ... , ............. , .. 46 Ackno\vledgtnents ......................... , , ..................... , ............ 52 References ................................................... , ............... 52 Plate 1 55 '" 20 Bd de I'H6pital, 75005 Paris, France. email: dS.dr@freeJr Key~words: teeth, triconodonts, amphilestines, gobiconodontines, North Africa, Early Cretaceous. Motswcles: dents, triconodontes, amphilcstines, gobiconodontines, Afrique du Nord, Cretacc infericur. Palaeovertebrata, Montpellier, 32 (I); 27-55, 13 fig., I pI. (Re~u le 27 Juin 2003, acccpte le JO Scptembrc 2003, publie le 15 Octobrc 2003) ABSTRACT The mammalian fauna (represented only by isolated teeth) from the carly Cretaceous of Morocco includes a number of l1on-'therian' specimens, characterized by the antero-posterior alignement of the main molar cusps. This assemblage is very heterogenous, including forms (among them GobicOIIOdoll pa/aias sp. nov,) that can be related to Laurasian triconodonts, and several forms so far known only in this part of Gondwana (among them Kl}'ptotherium po/ysphel1os gen. et sp. nov.). The latter, in particular, exemplifies -
The Miocene Mammal Necrolestes Demonstrates the Survival of a Mesozoic Nontherian Lineage Into the Late Cenozoic of South America
The Miocene mammal Necrolestes demonstrates the survival of a Mesozoic nontherian lineage into the late Cenozoic of South America Guillermo W. Rougiera,b,1, John R. Wibleb, Robin M. D. Beckc, and Sebastian Apesteguíad,e aDepartment of Anatomical Sciences and Neurobiology, University of Louisville, Louisville, KY 40202; bSection of Mammals, Carnegie Museum of Natural History, Pittsburgh, PA 15206; cSchool of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, Australia; dCEBBAD–Fundación de Historia Natural ‘Félix de Azara’, Universidad Maimónides, 1405 Buenos Aires, Argentina; and eConsejo Nacional de Investigaciones Científicas y Técnicas de Argentina, C1033AAJ Buenos Aires, Argentina Edited by Richard L. Cifelli, University of Oklahoma, Norman, OK, and accepted by the Editorial Board October 18, 2012 (received for review July 27, 2012) The early Miocene mammal Necrolestes patagonensis from Pata- not referable to either Metatheria or Eutheria, but did not discuss gonia, Argentina, was described in 1891 as the only known extinct the evidence for this interpretation, nor did they identify the placental “insectivore” from South America (SA). Since then, and specific therian lineages they considered to be potential relatives despite the discovery of additional well-preserved material, the of Necrolestes. Starting in 2007, we oversaw additional prepara- systematic status of Necrolestes has remained in flux, with earlier tion of Necrolestes specimens that comprise the best-preserved studies leaning toward placental affinities and more recent ones material currently available, including skulls, jaws, and some iso- endorsing either therian or specifically metatherian relationships. We lated postcranial bones; as a result, many phylogenetically signif- have further prepared the best-preserved specimens of Necrolestes icant features have been revealed for the first time. -
Jaw Shape and Mechanical Advantage Are Indicative of Diet in Mesozoic Mammals ✉ Nuria Melisa Morales-García 1 , Pamela G
ARTICLE https://doi.org/10.1038/s42003-021-01757-3 OPEN Jaw shape and mechanical advantage are indicative of diet in Mesozoic mammals ✉ Nuria Melisa Morales-García 1 , Pamela G. Gill1,2, Christine M. Janis 1,3 & Emily J. Rayfield 1 Jaw morphology is closely linked to both diet and biomechanical performance, and jaws are one of the most common Mesozoic mammal fossil elements. Knowledge of the dietary and functional diversity of early mammals informs on the ecological structure of palaeo- communities throughout the longest era of mammalian evolution: the Mesozoic. Here, we analyse how jaw shape and mechanical advantage of the masseter (MAM) and temporalis (MAT) muscles relate to diet in 70 extant and 45 extinct mammals spanning the Late 1234567890():,; Triassic-Late Cretaceous. In extant mammals, jaw shape discriminates well between dietary groups: insectivores have long jaws, carnivores intermediate to short jaws, and herbivores have short jaws. Insectivores have low MAM and MAT, carnivores have low MAM and high MAT, and herbivores have high MAM and MAT. These traits are also informative of diet among Mesozoic mammals (based on previous independent determinations of diet) and set the basis for future ecomorphological studies. 1 School of Earth Sciences, Wills Memorial Building, University of Bristol, Bristol, UK. 2 Department of Earth Sciences, Natural History Museum, London, UK. ✉ 3 Department of Ecology and Evolutionary Biology, Brown University, Providence, RI, USA. email: [email protected] COMMUNICATIONS BIOLOGY | (2021) 4:242 | https://doi.org/10.1038/s42003-021-01757-3 | www.nature.com/commsbio 1 ARTICLE COMMUNICATIONS BIOLOGY | https://doi.org/10.1038/s42003-021-01757-3 ur understanding of Mesozoic mammals has dramatically metric) has been used as a proxy for prey choice and feeding improved in the past three decades. -
Morphological Evidence Supports Dryolestoid Affinities for the Living Australian Marsupial Mole Notoryctes
Reviewing Manuscript Morphological Evidence supports Dryolestoid affinities for the living Australian Marsupial Mole Notoryctes Federico Agnolin, Nicolas Roberto Chimento Recent discoveries demonstrated that the southern continents were a cradle for the evolutionary radiation of dryolestoid mammals at the end of the Cretaceous. Moreover, it becomes evident that some of these early mammals surpassed the K/T boundary in South America, at least. Notoryctes is a poorly known living mammal, currently distributed in the s t deserts of central Australia. Due to its extreme modifications to fossoriality and peculiar n i anatomy, the phylogenetic relationships of this genus were debated in the past, but most r P recent authors agree in its marsupial affinities. A comparative survey of the anatomy of e Notoryctes reveals the poorly sustained marsupial affinities for the genus and striking r P plesiomorphies for a living mammal. Surprisingly, Notoryctes exhibits similarities with dryolestoids. Dryolestoids were a diverse and mainly mesozoic mammalian group phylogenetically nested between the egg-lying monotremes and derived therians. In particular, Notoryctes share a number of shared features with the extinct dryolestoid Necrolestes, from the Miocene of Patagonia. Both taxa conform a clade of burrowing and animalivorous dryolestoids that survived other members of their lineage probably due to their peculiar habits. Accordingly, Notoryctes constitutes a “living-fossil” from the supposedly extinct dryolestoid radiation, extending the biochron of the group more than 20 million years to the present day. The intermediate phylogenetic position of Notoryctes has the pivotal potential to shed light on crucial anatomical, physiological, ecological, and evolutionary topics in the deep transformation from egg-lying to placental mammals. -
Molar Occlusion and Jaw Roll in Early Crown Mammals Kai R
www.nature.com/scientificreports OPEN Molar occlusion and jaw roll in early crown mammals Kai R. K. Jäger1*, Richard L. Cifelli2 & Thomas Martin1 Triconodontidae are considered the frst carnivorous crown mammals. A virtual reconstruction of the masticatory cycle in the Late Jurassic Priacodon showed that triconodontid dental function is characterized by precise cutting on elongated crests. The combination of traits linked to both carnivorous diets (e.g. fore-aft cutting edges) and insectivorous diets (transverse crests and lobes) suggests a varied faunivorous diet appropriate to the small body size of most triconodontids. Total length of molar shear decreased with wear, suggesting a dietary shift during ontogeny. Embrasure occlusion is confrmed for P. fruitaensis as indicated by premolar positioning, facet orientation, and collision areas. Embrasure occlusion is considered a general feature of all Eutriconodonta, whereas the previously assumed Morganucodon-like pattern is limited to few early mammaliaforms. Unlike modern carnivores, signifcant roll of around 10° of the active hemimandible occurred during the power stroke. Roll was likely passive in Triconodontidae in contrast to active roll described for extant therians. The triconodontid molar series was highly uniform and adapted to a precise ft, with self-sharpening lower molar cusps. Whereas the uniformity ensured good cutting capabilities, it likely put the dentition under greater constraints, conserving the highly stereotyped nature of triconodontid molars for 60–85 Ma. Triconodontids are a clade of the eutriconodontans 1,2, which is a clade of early crown mammals with a fossil record from the Late Jurassic through the Late Cretaceous 3–8. It has been well established that stem mammalia- forms with triconodont-like molars, such as Morganucodon, are phylogenetically distinct and separated from the eutriconodontans9 by many derived features of the latter groups, including tooth wear characteristics 10. -
In Quest for a Phylogeny of Mesozoic Mammals
In quest for a phylogeny of Mesozoic mammals ZHE−XI LUO, ZOFIA KIELAN−JAWOROWSKA, and RICHARD L. CIFELLI Luo, Z.−X., Kielan−Jaworowska, Z., and Cifelli, R.L. 2002. In quest for a phylogeny of Mesozoic mammals. Acta Palaeontologica Polonica 47 (1): 1–78. We propose a phylogeny of all major groups of Mesozoic mammals based on phylogenetic analyses of 46 taxa and 275 osteological and dental characters, using parsimony methods (Swofford 2000). Mammalia sensu lato (Mammaliaformes of some authors) are monophyletic. Within mammals, Sinoconodon is the most primitive taxon. Sinoconodon, morganu− codontids, docodonts, and Hadrocodium lie outside the mammalian crown group (crown therians + Monotremata) and are, successively, more closely related to the crown group. Within the mammalian crown group, we recognize a funda− mental division into australosphenidan (Gondwana) and boreosphenidan (Laurasia) clades, possibly with vicariant geo− graphic distributions during the Jurassic and Early Cretaceous. We provide additional derived characters supporting these two ancient clades, and we present two evolutionary hypotheses as to how the molars of early monotremes could have evolved. We consider two alternative placements of allotherians (haramiyids + multituberculates). The first, supported by strict consensus of most parsimonious trees, suggests that multituberculates (but not other alllotherians) are closely re− lated to a clade including spalacotheriids + crown therians (Trechnotheria as redefined herein). Alternatively, allotherians can be placed outside the mammalian crown group by a constrained search that reflects the traditional emphasis on the uniqueness of the multituberculate dentition. Given our dataset, these alternative topologies differ in tree−length by only ~0.6% of the total tree length; statistical tests show that these positions do not differ significantly from one another. -
Cuenca-Bescós,G.And Canudo,J.I.2003.A New
A new gobiconodontid mammal from the Early Cretaceous of Spain and its palaeogeographic implications GLORIA CUENCA−BESCÓS and JOSÉ I. CANUDO Cuenca−Bescós, G. and Canudo, J.I. 2003. A new gobiconodontid mammal from the Early Cretaceous of Spain and its palaeogeographic implications. Acta Paleontologica Polonica 48 (4): 575–582. A new gobiconodontid from Vallipón (Teruel, Spain) represents the first record of this family in Europe. The site has a di− verse fossil assemblage mainly composed of isolated bones and teeth probably accumulated by tidal action and water streams in an ancient beach of upper Barremian, in the transitional marine−continental sediments of the Artoles Forma− tion. The new gobiconodontid consist of an isolated upper molar, smaller in size than that element in other gobi− conodontids, with a robust cusp A, characterised by lateral bulges on each mesial and distal flanges of that cusp, and a dis− continuous cingulum raised at the lingual side. The occlusal outline is smooth compared with Gobiconodon borissiaki, Gobiconodon hoburensis,orGobiconodon ostromi. The Gobiconodontidae record is exclusively Laurasiatic. The oldest gobiconodontid fossil remains are Hauterivian; though their probable origin has to be found at the Late Jurassic in Central Asia (as inferred from derived character of the first gobiconodontids as well as phylogenetic relationships). At the end of the Early Cretaceous they expanded throughout Laurasia as indicated by findings in Asia, North America, and Spain. Two dispersion events spread gobiconodontids: to the West (Europe) in the Barremian and to the East (North America) during the Aptian/Albian. Key words: Cretaceous, Barremian, Mammalia, Gobiconodontidae, Europe, palaeogeography. -
Supplemental Data
Supplementary Information Diversity Data The Paleobiology Database [1] was used as the principal source for taxonomic ranges of the early mammalian genera. Much of the data in the Paleobiology Database came from Kielan- Jaworowska et al. [2], Lofgren [3], Clemens [4], Archibald [5], Hartman [6], Fox [7], Eaton and Cifelli [8], Montellano [9], Pearson et al. [10], and Lillegraven and McKenna [11]. Dental Functional Types For our purposes, triconodont refers to a molar with three primary cusps in a linear or obtuse- angled arrangement, such as in eutriconodontans, amphilestids, and morganucodontans. Symmetrodont molars are those with three primary cusps in a triangular arrangement and no talonid. Tribosphenic molars have dual-function trigonids and talonids such as in true tribosphenic eutherians, metatherians, and stem boreosphenidans, as well as pseudo-tribosphenic australosphenidans. Upper molars of plagiaulacoid multituberculates possess two rows of cusps and upper molars of cimolodont multituberculates have three rows, although the two dental types are also distinguished by number of incisors and premolars [2]. See Kielan-Jaworowska et al. [2] for descriptions of gondwanatherians, haramiyids, eupantotherians, and docodonts. One of the most contentious assignments for dental functional type involves the triconodonts (in the most general usage of the term) (see [71]). It should be noted, however, that even if alternative dental functional types were chosen for triconodont genera (e.g., if amphilestids were included with symmetrodonts instead of triconodontans), the overall diversity patterns of tribosphenic mammals and multituberculates relative to other dental types in the Cretaceous (the main focus of this portion of the study) would not be altered (figure 1).