Mandibular and Dental Characteristics of Late Triassic Mammaliaform
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April Isch Neander
February 2017 Curriculum Vitae April Isch Neander Scientific Illustrator University of Chicago Department of Organismal Biology and Anatomy 1027 E 57th Street Anatomy 306 Chicago, IL 60637 [email protected] 773.702.4715 Education M.S. Biomedical Visualization, University of Illinois at Chicago, 2012 Graduate Research Project: Visualizing the Parasagittal Step Cycle of Kryptobaatar dashzevegi, a Multituberculate with Transitional Shoulder Girdle. B.A. Biology, University of Vermont, 2010 Minor in Studio Art Publications Published Art and Illustrations Luo, Z. X., Schultz, J. A., & Ekdale, E. G. (2016). Evolution of the Middle and Inner Ears of Mammaliaforms: The Approach to Mammals. In Evolution of the Vertebrate Ear (pp. 139-174). Springer International Publishing. Brusatte, S., Luo, Z. X. (2016, June). Ascent of the Mammals. Scientific American, 30-35. Luo, Z. X., Gatesy, S. M., Jenkins, F. A., Amaral, W. W., & Shubin, N. H. (2015). Mandibular and dental characteristics of Late Triassic mammaliaform Haramiyavia and their ramifications for basal mammal evolution. Proceedings of the National Academy of Sciences, 112(51), E7101-E7109. Chang, Kenneth. (2015, November 16). Jawbone in Rock May Clear Up a Mammal Family Mystery. The New York Times. Hopson, James A. (2015). Fossils, Trackways, and Transitions in Locomotion. In Dial, Kenneth P., Neil Shubin, and Elizabeth L. Brainerd, eds. Great transformations in vertebrate evolution (pp. 125-141). University of Chicago Press. Luo, Z. X., Meng, Q. J., Ji, Q., Liu, D., Zhang, Y. G., & Neander, A. I. (2015). Evolutionary development in basal mammaliaforms as revealed by a docodontan. Science, 347(6223), 760-764. Meng, Q. J., Ji, Q., Zhang, Y. -
A Review of Palaeozoic and Mesozoic Tetrapods from Greenland
A review of Palaeozoic and Mesozoic tetrapods from Greenland MARCO MARZOLA, OCTÁVIO MATEUS, JESPER MILÀN & LARS B. CLEMMENSEN Marzola, M., Mateus, O., Milàn, J. & Clemmensen, L.B. 2018. A review of Palaeozoic and Mesozoic tetrapods from Greenland. © 2018 by Bulletin of the Geological Society of Denmark, Vol. 66, pp. 21–46. ISSN 2245-7070. (www.2dgf.dk/publikationer/bulletin). https://doi.org/10.37570/bgsd-2018-66-02 This article presents a synthesis of Palaeozoic and Mesozoic fossil tetrapods from Greenland, includ- ing an updated review of the holotypes and a new photographic record of the main specimens. All fossil tetrapods found are from East Greenland, with at least 30 different known taxa: five stem tetra- pods (Acanthostega gunnari, Ichthyostega eigili, I. stensioi, I. watsoni, and Ymeria denticulata) from the Late Received 1 December 2016 Devonian of the Aina Dal and Britta Dal Formations; four temnospondyl amphibians (Aquiloniferus Accepted in revised form kochi, Selenocara groenlandica, Stoschiosaurus nielseni, and Tupilakosaurus heilmani) from the Early Triassic 27 October 2017 of the Wordie Creek Group; two temnospondyls (Cyclotosaurus naraserluki and Gerrothorax cf. pulcher- Published online rimus), one testudinatan (cf. Proganochelys), two stagonolepids (Aetosaurus ferratus and Paratypothorax 3 March 2018 andressorum), the eudimorphodontid Arcticodactylus, undetermined archosaurs (phytosaurs and both sauropodomorph and theropod dinosaurs), the cynodont Mitredon cromptoni, and three mammals (Ha- ramiyavia clemmenseni, Kuehneotherium, and cf. ?Brachyzostrodon), from the Late Triassic of the Fleming Fjord Formation; one plesiosaur from the Early Jurassic of the Kap Stewart Formation; one plesiosaur and one ichthyosaur from the Late Jurassic of the Kap Leslie Formation, plus a previously unreported Late Jurassic plesiosaur from Kronprins Christian Land. -
Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna. -
A Non-Mammaliaform Cynodont from the Upper Triassic of South Africa: a Therapsid Lazarus Taxon?
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Wits Institutional Repository on DSPACE A non-mammaliaform cynodont from the Upper Triassic of South Africa: a therapsid Lazarus taxon? Fernando Abdala1*, Ross Damiani2, Adam Yates1 & Johann Neveling3 1Bernard Price Institute for Palaeontological Research, School of Geosciences, University of the Witwatersrand, Private Bag 3, WITS, 2050 South Africa 2Staatliches Museum für Naturkunde Stuttgart, Rosenstein 1, D-70191, Stuttgart, Germany 3Council for Geoscience, Private Bag X112, Pretoria, 0001 South Africa Received 20 January 2006. Accepted 10 January 2007 The tetrapod record of the ‘Stormberg Group’, including the Lower Elliot Formation, in the South African Karoo is widely dominated by archosaurian reptiles, contrasting with the therapsid dominion of the subjacent Beaufort Group. The only therapsids represented by skeletal remains in the Upper Triassic Lower Elliot Formation are the large traversodontid cynodont Scalenodontoides macrodontes and the recently described tritheledontid cynodont Elliotherium kersteni. Here we present a fragmentary lower jaw that provides evidence of a third type of cynodont for the Upper Triassic of South Africa. The fossil is tentatively assigned to the Diademodontidae. The latter representative of this family is known from the Late Anisian, and its tentative record in the Norian Lower Elliot Formation, if confirmed, will represent a case of Lazarus taxon. Thus, Diademodontidae apparently disappeared from the fossil record by the end of the Anisian and then reappeared in the Norian of South Africa, a stratigraphic interval of some 21 million years. This new cynodont record, together with the recently described Tritheledontidae, show that cynodonts are now the second most diverse tetrapod group in the Lower Elliot fauna. -
Triassic Lithostratigraphy of the Jameson Land Basin (Central East Greenland), with Emphasis on the New Fleming Fjord Group
BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK · VOL. 68 · 2020 Triassic lithostratigraphy of the Jameson Land Basin (central East Greenland), with emphasis on the new Fleming Fjord Group LARS B. CLEMMENSEN, DENNIS V. KENT, MALTE MAU, OCTÁVIO MATEUS & JESPER MILÀN Clemmensen, L.B., Kent, D.V., Mau, M., Mateus, O. & Milàn, J. 2020. Triassic lithostratigraphy of the Jameson Land basin (central East Greenland), with emphasis on the new Fleming Fjord Group. Bulletin of the Geological Society of Denmark, vol. 68, pp. 95–132. ISSN 2245-7070. https://doi.org/10.37570/bgsd-2020-68-05-rev File replaced 2021-05-08: Erroneous rotation directions in the original publication Geological Society of Denmark are now correct. https://2dgf.dk The lithostratigraphy of the Triassic deposits of the Jameson Land Basin in central East Received 26 August 2019 Greenland is revised. The new Scoresby Land Supergroup is now composed of the Wordie Accepted in revised form Creek, Pingo Dal, Gipsdalen and Fleming Fjord Groups. This paper only deals with the 23 April 2020 lithostratigraphy of the late Early-Late Triassic continental deposits of the latter three Published online groups with emphasis on the vertebrate-bearing Fleming Fjord Group. The new Pingo 05 June 2020 Dal Group consists of three new formations, the Rødstaken, Paradigmabjerg and Klitdal © 2020 the authors. Re-use of material is Formations (all elevated from members), the new Gipsdalen Group consists of three new permitted, provided this work is cited. formations, the Kolledalen, Solfaldsdal (with the new Gråklint Member) and Kap Seaforth Creative Commons License CC BY: Formations (all elevated from members), and the new Fleming Fjord Group is subdivided https://creativecommons.org/licenses/by/4.0/ into three new formations, the Edderfugledal, Malmros Klint and Ørsted Dal Formations (all elevated from members). -
213 a New Haramiyid Indicating a Complex Pattern of Evolution In
Vol.27 No.4 2013 Science Watch A New Haramiyid Indicating a Complex Pattern of Evolution in Mesozoic Mammals Earth Science major unsolved problem in mammalian evolution is University reported a new haramiyid from the Jurassic period the origin of Allotheria, including Multituberculata of China, Arboroharamiya jenkinsi, a partial skeleton with A and Haramiyida. Multituberculates are the most both mandibles associated with teeth and isolated upper teeth. diverse and best known Mesozoic era mammals and This largest known haramiyid reveals additional mammalian ecologically resemble rodents, but haramiyids are known features of this group, and helps to identify other haramiyids mainly from isolated teeth, hampering our search for their represented by isolated teeth, indicating a complex pattern phylogenetic relationships. Researchers from the Institute of evolution involving many convergences and/or reversals of Vertebrate Paleontology and Paleoanthropology (IVPP), existed in Mesozoic mammals, as reported August 8 in CAS, the Shandong Tianyu Museum of Nature and the Linyi Nature. Reconstruction of Arboroharamiya jenkinsi. (Image by BI Shundong) Bulletin of the Chinese Academy of Sciences 213 BCAS Vol.27 No.4 2013 The new specimen was unearthed from the Middle–Late Jurassic Tiaojishan Formation in the town of Mutoudeng, Qinglong County, Hebei Province, China, dated about 160 million years. Researchers said it is the largest known haramiyid with a body mass estimated at 354 grams. Arboroharamiya, as with other mammals, has body Earth Science hair (preserved as impressions), a single-boned (dentary) mandible that implies a three-boned middle ear. The dentition is differentiated into incisors and multi-rooted premolars and molars, with the canine presumably lost. -
Lower Triassic Postcanine Teeth with Allotherian-Like Crowns
Research Letters South African Journal of Science 103, May/June 2007 245 Lower Triassic postcanine teeth with allotherian-like crowns F. Abdala*‡, H. Mocke*§ and P.J. Hancox* The Allotheria are fossil mammals with upper and lower post- canines usually showing two longitudinal rows of cusps separated by a central valley. The group comprises the poorly known haramiyids, mostly represented by isolated teeth, and the notably diverse and long-lived multituberculates; its monophyly is uncer- tain. The oldest records of this particular group are the Late Triassic (Norian–Rhaetian) haramiyids. We present here postcanines with haramiyid-like crowns that were recovered from the Lower Triassic of South Africa. A distinguishing feature of the new teeth is that they are single-rooted. This is the oldest record of mammal-like teeth with crowns having parallel rows of cusps, representing a temporal extension of some 43 million years from similar crown patterns of haramiyids and tritylodontids. This finding reinforces evidence of the remarkable faunal turnover of therapsids in the Early/Middle Triassic, at which time an explosive origin followed by a rapid early diversification of herbivorous/omnivorous forms with occluding expanded postcanines took place. Introduction The Beaufort Group of the South African Karoo shows an abundance and diversity of non-mammalian synapsids, which have allowed for biostratigraphic subdivisions ranging from Middle Permian to Middle Triassic.1 The youngest of these Fig. 1.Allotherian-like teeth.A, Occlusal and lateral views of BP/1/6515 (Pattern 1); B, occlusal and lateral views of BP/1/6516 (Pattern 2). biozones, the Cynognathus Assemblage Zone (AZ), comprises the full extent of the Burgersdorp Formation of the Tarkastad Sub- found to be most parsimonious from an unconstrained search, group (J. -
Osteohistology of Late Triassic Prozostrodontian Cynodonts from Brazil
Osteohistology of Late Triassic prozostrodontian cynodonts from Brazil Jennifer Botha-Brink1,2, Marina Bento Soares3 and Agustín G. Martinelli3 1 Department of Karoo Palaeontology, National Museum, Bloemfontein, South Africa 2 Department of Zoology and Entomology, University of the Free State, Bloemfontein, South Africa 3 Departamento de Paleontologia e Estratigrafia, Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil ABSTRACT The Prozostrodontia includes a group of Late Triassic-Early Cretaceous eucynodonts plus the clade Mammaliaformes, in which Mammalia is nested. Analysing their growth patterns is thus important for understanding the evolution of mammalian life histories. Obtaining material for osteohistological analysis is difficult due to the rare and delicate nature of most of the prozostrodontian taxa, much of which comprises mostly of crania or sometimes even only teeth. Here we present a rare opportunity to observe the osteohistology of several postcranial elements of the basal prozostrodontid Prozostrodon brasiliensis, the tritheledontid Irajatherium hernandezi, and the brasilodontids Brasilodon quadrangularis and Brasilitherium riograndensis from the Late Triassic of Brazil (Santa Maria Supersequence). Prozostrodon and Irajatherium reveal similar growth patterns of rapid early growth with annual interruptions later in ontogeny. These interruptions are associated with wide zones of slow growing bone tissue. Brasilodon and Brasilitherium exhibit a mixture of woven-fibered bone tissue and slower growing parallel-fibered and lamellar bone. The slower growing bone tissues are present even during early ontogeny. The relatively slower growth in Brasilodon and Brasilitherium may be related to their small body size compared to Prozostrodon and Irajatherium. These brasilodontids also exhibit osteohistological similarities with the Late Triassic/Early Jurassic mammaliaform Morganucodon and the Late Cretaceous multituberculate mammals Kryptobaatar and Nemegtbaatar. -
A New Mammaliaform from the Early Jurassic and Evolution Of
R EPORTS tary trough with a shelflike dorsal medial ridge, and all other nonmammalian mamma- A New Mammaliaform from the liaforms have a medial concavity on the man- dibular angle (8–14, 23), as in nonmamma- Early Jurassic and Evolution of liaform cynodonts (9, 14, 24–27). The post- dentary trough and the medial concavity on Mammalian Characteristics the mandibular angle respectively accommo- dated the prearticular/surangular and the re- Zhe-Xi Luo,1* Alfred W. Crompton,2 Ai-Lin Sun3 flected lamina of the angular (9, 25–27) that are the homologs to the mammalian middle A fossil from the Early Jurassic (Sinemurian, ϳ195 million years ago) represents ear bones (9, 14, 16–21, 23, 26). The absence a new lineage of mammaliaforms, the extinct groups more closely related to of these structures indicates that the postden- the living mammals than to nonmammaliaform cynodonts. It has an enlarged tary bones (“middle ear ossicles”) must have cranial cavity, but no postdentary trough on the mandible, indicating separation been separated from the mandible (Fig. 3). of the middle ear bones from the mandible. This extends the earliest record of Hadrocodium lacks the primitive meckelian these crucial mammalian features by some 45 million years and suggests that sulcus of the mandible typical of all nonmam- separation of the middle ear bones from the mandible and the expanded brain maliaform cynodonts (24–27), stem groups vault could be correlated. It shows that several key mammalian evolutionary of mammaliaforms (8, 9, 14, 23, 26, 27), innovations in the ear region, the temporomandibular joint, and the brain vault triconodontids (28, 29), and nontribosphenic evolved incrementally through mammaliaform evolution and long before the therian mammals (30). -
Does the Jurassic Agilodocodon (Mammaliaformes, Docodonta) Have Any Exudativorous Dental Features?
DOES THE JURASSIC AGILODOCODON (MAMMALIAFORMES, DOCODONTA) HAVE ANY EXUDATIVOROUS DENTAL FEATURES? JOHN R. WIBLE and ANNE M. BURROWS Wible, J.R. and Burrows, A.M. 2016. Does the Jurassic Agilodocodon (Mammaliaformes, Docodonta) have any exudativorous dental features? Palaeontologia Polonica 67, 289–299. Obligate exudativory, including active wounding of bark to acquire gum and/or sap, is rare among extant mammals and does not show a consistent dental signature. A recently de- scribed Middle Jurassic docodont Agilodocodon was reconstructed as an exudativore based on proposed similarities of its lower anterior dentition to some extant New World monkeys, specifically marmosets, spider monkeys, and howler monkeys. Oddly enough, of these, only marmosets are exudate-feeders. In our reinvestigation, we did not find any significant resemblance in the lower (and upper) anterior dentition between the Middle Jurassic fossil and these extant New World monkeys. The marmosets, the only obligate platyrrhine exuda- tivores, have lower and upper incisors that are distinguished from Agilodocodon and other New World monkeys by having enamel restricted to the labial surface. Differential wear between the enamel and softer dentine maintains a chisel-like tooth that marmosets use in gouging bark. Additional comparisons of the anterior dentition of Agilodocodon and other extant mammals were conducted. The lower and upper anterior teeth of Agilodocodon were found to be most similar to some elephant shrews and South American marsupials, which have a primarily insectivorous diet. Agilodocodon does not show any dental adaptations found in extant mammals for exudativory. Key words: Docodonta, Agilodocodon, marmosets, exudativory, incisors, gums. John R. Wible [[email protected]], Section of Mammals, Carnegie Museum of Natural History, 5800 Baum Boulevard, Pittsburgh, PA 15206, USA. -
Parental Care Or Opportunism in South African Triassic Cynodonts?
Parental care or opportunism in South African AUTHOR: Triassic cynodonts? Julien Benoit1 AFFILIATION: In a paper published in Nature in 2018, Hoffman and Rowe1 describe the discovery of an adult tritylodontid cynodont, 1Evolutionary Studies Institute, Kayentatherium, from the Jurassic of the Kayenta Formation (Arizona, USA), accompanied by at least 38 perinatal School of Geosciences, University juveniles, all at the same very early stage of development. Such a high number of juveniles in one clutch is found of the Witwatersrand, Johannesburg, only in a handful of oviparous reptiles, and never in viviparous or ovoviviparous species1, suggesting that these South Africa cynodonts laid eggs. As tritylodontids are amongst the closest relatives to Mammaliaformes, and sometimes even reconstructed as their sister clade2, this textbook changing discovery implies that all non-mammaliaform CORRESPONDENCE TO: synapsids had an essentially reptilian-like reproductive biology1. Julien Benoit Hoffman and Rowe’s1 discovery forces a reappraisal of the interpretation of the rich fossil record of parental care EMAIL: in South African non-mammaliaform cynodonts3. [email protected] First, the implications of Hoffman and Rowe’s1 discovery for the evolution of parental care and lactation need to be discussed. With at least 38 hatchlings to feed, it can be safely assumed that lactation was not the main source of HOW TO CITE: Benoit J. Parental care or nutrients in Kayentatherium neonates (nor, by extension, in all more basal non-mammaliaform synapsids). Instead, opportunism in South African perinatal juveniles of Kayentatherium already had functional teeth despite their early age, which (1) impedes Triassic cynodonts? S Afr J Sci. -
Variability of the Parietal Foramen and the Evolution of the Pineal Eye in South African Permo-Triassic Eutheriodont Therapsids
The sixth sense in mammalian forerunners: Variability of the parietal foramen and the evolution of the pineal eye in South African Permo-Triassic eutheriodont therapsids JULIEN BENOIT, FERNANDO ABDALA, PAUL R. MANGER, and BRUCE S. RUBIDGE Benoit, J., Abdala, F., Manger, P.R., and Rubidge, B.S. 2016. The sixth sense in mammalian forerunners: Variability of the parietal foramen and the evolution of the pineal eye in South African Permo-Triassic eutheriodont therapsids. Acta Palaeontologica Polonica 61 (4): 777–789. In some extant ectotherms, the third eye (or pineal eye) is a photosensitive organ located in the parietal foramen on the midline of the skull roof. The pineal eye sends information regarding exposure to sunlight to the pineal complex, a region of the brain devoted to the regulation of body temperature, reproductive synchrony, and biological rhythms. The parietal foramen is absent in mammals but present in most of the closest extinct relatives of mammals, the Therapsida. A broad ranging survey of the occurrence and size of the parietal foramen in different South African therapsid taxa demonstrates that through time the parietal foramen tends, in a convergent manner, to become smaller and is absent more frequently in eutherocephalians (Akidnognathiidae, Whaitsiidae, and Baurioidea) and non-mammaliaform eucynodonts. Among the latter, the Probainognathia, the lineage leading to mammaliaforms, are the only one to achieve the complete loss of the parietal foramen. These results suggest a gradual and convergent loss of the photoreceptive function of the pineal organ and degeneration of the third eye. Given the role of the pineal organ to achieve fine-tuned thermoregulation in ecto- therms (i.e., “cold-blooded” vertebrates), the gradual loss of the parietal foramen through time in the Karoo stratigraphic succession may be correlated with the transition from a mesothermic metabolism to a high metabolic rate (endothermy) in mammalian ancestry.