Molecules, Morphology, and Ecology Indicate a Recent, Amphibious Ancestry for Echidnas

Total Page:16

File Type:pdf, Size:1020Kb

Molecules, Morphology, and Ecology Indicate a Recent, Amphibious Ancestry for Echidnas Molecules, morphology, and ecology indicate a recent, amphibious ancestry for echidnas Matthew J. Phillipsa,1, Thomas H. Bennetta, and Michael S. Y. Leeb,c aCentre for Macroevolution and Macroecology, Research School of Biology, Australian National University, Canberra, ACT 0200, Australia; bSchool of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5005, Australia; and cEarth Sciences Section, South Australian Museum, Adelaide, SA 5000, Australia Edited by David B. Wake, University of California, Berkeley, CA, and approved August 14, 2009 (received for review April 28, 2009) The semiaquatic platypus and terrestrial echidnas (spiny anteaters) Fossil echidnas do not appear until the mid-Miocene (Ϸ13 are the only living egg-laying mammals (monotremes). The fossil Ma) (13), despite excellent late Oligocene–Early Miocene mam- record has provided few clues as to their origins and the evolution mal fossil records in both northern and southern Australia. This of their ecological specializations; however, recent reassignment absence has tentatively been attributed in part to echidnas of the Early Cretaceous Teinolophos and Steropodon to the platy- lacking teeth (14), which are the most common fossil remains pus lineage implies that platypuses and echidnas diverged >112.5 from mammals. Alternatively, if the molecular dating studies million years ago, reinforcing the notion of monotremes as living that estimate the divergence of echidnas from platypuses at fossils. This placement is based primarily on characters related to 17–35 Ma (15–22) are correct, then characters that clearly ally a single feature, the enlarged mandibular canal, which supplies fossil taxa with echidnas would not be expected to have evolved blood vessels and dense electrosensory receptors to the platypus until even more recently. bill. Our reevaluation of the morphological data instead groups Molecular dating can play a pivotal role in inferring the platypus and echidnas to the exclusion of Teinolophos and Stero- evolutionary history of taxa with a sparse fossil record, such as podon and suggests that an enlarged mandibular canal is ancestral monotremes (14, 23, 24). Recent reassignment of the 112.5–121 Ϸ for monotremes (partly reversed in echidnas, in association with Ma Teinolophos and the 105 Ma Steropodon from outside of the monotreme crown group (platypuses and echidnas) specif- general mandibular reduction). A multigene evaluation of the EVOLUTION echidna–platypus divergence using both a relaxed molecular clock ically to the platypus lineage has profound implications (25). and direct fossil calibrations reveals a recent split of 19–48 million Teinolophos would be the oldest fossil unequivocally within any years ago. Platypus-like monotremes (Monotrematum) predate of the three mammalian crown groups (Monotremata, Marsu- this divergence, indicating that echidnas had aquatically foraging pialia, and Placentalia). The fundamental morphological and ancestors that reinvaded terrestrial ecosystems. This ecological ecological differences between platypuses and echidnas also would date back over 100 Ma, reinforcing the notion of shift and the associated radiation of echidnas represent a recent monotremes being ‘‘living fossils,’’ a term that Darwin (26) first expansion of niche space despite potential competition from mar- coined with reference to the platypus. Furthermore, it implies supials. Monotremes might have survived the invasion of marsu- slow molecular evolution within monotremes that challenges pials into Australasia by exploiting ecological niches in which current views of molecular evolutionary rates (25). marsupials are restricted by their reproductive mode. Morphology, Upon revising Luo and Wible’s (27) data set, Rowe et al. (25) ecology, and molecular biology together indicate that Teinolophos assigned Teinolophos to the platypus lineage, based primarily on and Steropodon are basal monotremes rather than platypus rela- characters related to the mandibular canal. In the platypus, tives, and that living monotremes are a relatively recent radiation. Teinolophos, and certain other fossil monotremes, the canal is enlarged; in the platypus it contains the hypertrophied mandib- ͉ ͉ ͉ ͉ calibration molecular dating Monotremata niche phylogeny ular branch of the trigeminal nerve, which supports an extensive mechanosensory–electrosensory system (28). The mandibular ore than 99% of the Ϸ5,400 extant mammal species are canal is narrower in echidnas than in other monotremes, al- Mtherian (marsupials and placentals) (1). Monotremes, the though still relatively larger than in most other mammals. But only egg-laying mammals, are their living sister group and whether the condition in echidnas is primitive for monotremes comprise just 5 extant species. One of these species is the or a partial reversal correlated with the reduction of the man- semiaquatic, invertebrate feeding platypus (Ornithorhynchus dible to little more than elongate splints of bone remains unclear. anatinus) of eastern and southern Australia; the others are the All support for the platypus affinities of Teinolophos derives terrestrial echidnas (Tachyglossidae), the short-beaked echidna from mandibular characters. This is surprising given that the or spiny anteater, Tachyglossus aculeatus of Australia and New initial description of Teinolophos (29), based largely on a man- Guinea, and three species of New Guinean long-beaked echidnas dible, aligned it with stem therians rather than with monotremes, (Zaglossus bruijni, Z. attenboroughi, and Z. bartoni), which feed let alone platypuses. Full exposure of the molar revealed on worms and arthropod larvae. Fossil monotremes, such as monotreme affinities (30) but suggested that Teinolophos was a Teinolophos trusleri and Steropodon galmani (2), along with their stem monotreme, diverging before the common ancestor of putative relatives, the insectivore-like ausktribosphenids (3–6), platypus and echidnas underwent a size increase and a dietary make up the bulk of the known Australian Cretaceous mammal shift that required relatively weaker bite forces. fauna. Known monotreme diversity then contracts to only platypus-like taxa, subsequent to the arrival of marsupials from Ϸ Author contributions: M.J.P. and M.S.Y.L. designed research; M.J.P., T.H.B., and M.S.Y.L. South America via Antarctica 71–54.6 million years ago (Ma) performed research; M.J.P. and M.S.Y.L. analyzed data; and M.J.P. and M.S.Y.L. wrote the (7, 8). Monotrematum sudamericanum (9, 10) from the Palaeo- paper. cene (Ϸ61 Ma) of South America is known from two platypus- The authors declare no conflict of interest. like distal femora and several molar teeth that closely match This article is a PNAS Direct Submission. those of the extinct Australian platypus, Obdurodon (11, 12). The 1To whom correspondence should be addressed. E-mail: [email protected]. Ϸ later appearance ( 25 Ma) of Obdurodon probably reflects the This article contains supporting information online at www.pnas.org/cgi/content/full/ sparseness of earlier Tertiary mammal-bearing sites in Australia. 0904649106/DCSupplemental. www.pnas.org͞cgi͞doi͞10.1073͞pnas.0904649106 PNAS Early Edition ͉ 1of6 Downloaded by guest on September 28, 2021 Table 1. Divergence age estimates from the BEAST analyses for dating studies, a practice that is problematic (37). An additional Monotremata (platypus vs. echidnas), Tachyglossidae (Zaglossus concern is that the upper estimate reported for Monotremata of vs. Tachyglossus), and Mammalia (Theria vs. Monotremata) 130.8 Ma (25) cannot be considered in isolation from the upper Median 95% HPD estimate of 322.8 Ma for the adjacent monotreme–therian divergence. There often is a strong correlation between credi- Monotremata bility intervals for adjacent nodes on trees (38), and the 322.4 Ma mtnuc14 32.1 18.5–47.8 upper estimate for crown mammals appears implausible, being nuc14 37.8 14.8–73.8 twice as old as the oldest unequivocal fossils (39) and predating mt88 27.7 13.3–47.1 even the earliest fully terrestrial vertebrates (amniotes). Tachyglossidae With a view to increasing the precision of molecular dating mt88 5.5 1.8–10.6 estimates for the echidna–platypus divergence, we add long Mammalia sequences from 2 other nuclear genes (Rag1 and apob) to make mtnuc14 186.5 160.8–216.9 a 7–nuclear gene data set (7,137 nucleotides) and analyze this nuc14 203.4 163.5–252.2 alongside complete mitochondrial (mt) genome sequences. We mt88 168.8 145.8–196.2 use relaxed-clock dating methods, including up to 20 prior distributions for calibrations derived directly from the fossil record. We first estimate the age of the echidna–platypus One concern with the morphological data set of Rowe et al. divergence with no age constraints on this node, then examine (25) is that one character (enlarged mandibular canal) overlaps how bounding the age of this node with Teinolophos (i.e., with others (hypertrophy of the mandibular canal; characters 425 assuming that it is a stem platypus) effects estimates of molecular and 440) and is also used to infer states for unfossilized char- evolutionary rates. acters (presence of a bill and electrosensory capability; charac- ters 423 and 424). We address this nonindependence issue by Results removing redundant characters and indirect inferences [see Molecular divergence dates were derived using relaxed clocks supporting information (SI) Text]. The support for grouping and three alternative calibration schemes. The discussion that Teinolophos and Steropodon with platypuses
Recommended publications
  • Miocene Mammal Reveals a Mesozoic Ghost Lineage on Insular New Zealand, Southwest Pacific
    Miocene mammal reveals a Mesozoic ghost lineage on insular New Zealand, southwest Pacific Trevor H. Worthy*†, Alan J. D. Tennyson‡, Michael Archer§, Anne M. Musser¶, Suzanne J. Hand§, Craig Jonesʈ, Barry J. Douglas**, James A. McNamara††, and Robin M. D. Beck§ *School of Earth and Environmental Sciences, Darling Building DP 418, Adelaide University, North Terrace, Adelaide 5005, South Australia, Australia; ‡Museum of New Zealand Te Papa Tongarewa, P.O. Box 467, Wellington 6015, New Zealand; §School of Biological, Earth and Environmental Sciences, University of New South Wales, New South Wales 2052, Australia; ¶Australian Museum, 6-8 College Street, Sydney, New South Wales 2010, Australia; ʈInstitute of Geological and Nuclear Sciences, P.O. Box 30368, Lower Hutt 5040, New Zealand; **Douglas Geological Consultants, 14 Jubilee Street, Dunedin 9011, New Zealand; and ††South Australian Museum, Adelaide, South Australia 5000, Australia Edited by James P. Kennett, University of California, Santa Barbara, CA, and approved October 11, 2006 (sent for review July 8, 2006) New Zealand (NZ) has long been upheld as the archetypical Ma) dinosaur material (13) and isolated moa bones from marine example of a land where the biota evolved without nonvolant sediments up to 2.5 Ma (1, 14), the terrestrial record older than terrestrial mammals. Their absence before human arrival is mys- 1 Ma is extremely limited. Until now, there has been no direct terious, because NZ was still attached to East Antarctica in the Early evidence for the pre-Pleistocene presence in NZ of any of its Cretaceous when a variety of terrestrial mammals occupied the endemic vertebrate lineages, particularly any group of terrestrial adjacent Australian portion of Gondwana.
    [Show full text]
  • Versión Disponible En PDF
    nicolás r chimento, Federico L agnolin y Fernando e novas Museo Argentino de Ciencias Naturales Bernardino Rivadavia Necrolestes un mamífero patagónico que sobrevivió a la extinción de los dinosaurios Un descubrimiento patagónico desembocadura del río Santa Cruz, descubrieron esque- letos fósiles prácticamente completos del Necrolestes. El es- En 1891, Florentino Ameghino (1854-1911) dio a tudio de esos esqueletos llevó a pensar que se trataba de conocer unos restos fósiles encontrados por su hermano un mamífero muy arcaico en la historia de la evolución, Carlos (1865-1936) en las barrancas de Monte Obser- más que un ancestro de los topos, como había supuesto vación, en la provincia de Santa Cruz, en yacimientos Ameghino. Por determinados rasgos se pensó que podía de unos 17 millones de años de antigüedad. Determinó haber sido un marsupial, es decir, un pariente lejano de las que pertenecían a un pequeño –escasos 10cm de largo, comadrejas, los canguros y los coalas actuales. del hocico a la cola– y desconocido mamífero extin- Ciertos investigadores aceptaron esta última hipótesis guido. Estudió los diminutos huesos y consideró que de parentesco, pero otros se mostraron escépticos acerca el animal habría sido un pariente lejano de los topos de ella y se inclinaron por considerar inciertas las rela- africanos vivientes. Le dio el nombre científicoN ecrolestes ciones genealógicas del diminuto mamífero. Así, su po- patagonensis, es decir, ladrón de tumbas de la Patagonia, en sición en el árbol evolutivo de los mamíferos fue objeto alusión a sus hábitos excavadores. El hallazgo, publica- de debate durante gran parte del siglo XX. Para algunos, do por Ameghino en el número de la Revista Argentina de era pariente lejano de las mulitas; otros seguían pensan- Historia Natural citado entre las lecturas sugeridas, atrajo do que podía estar relacionado con los topos, y para un la atención del ámbito científico, ya que hasta ese mo- tercer grupo, sus vínculos eran con los marsupiales aus- mento en Sudamérica no se habían encontrado restos tralianos.
    [Show full text]
  • 0 Introduction
    Cambridge University Press 978-0-521-78117-6 - Evolution of Tertiary Mammals of North America, Volume 2: Small Mammals, Xenarthrans, and Marine Mammals Christine M. Janis, Gregg F. Gunnell and Mark D. Uhen Excerpt More information 0 Introduction christine m. janis,1 gregg f. gunnell2 and mark d. uhen3 1Brown University, Providence, RI, USA 2Museum of Paleontology, University of Michigan, Ann Arbor, MI, USA 3Smithsonian Institution, Washington, DC, USA AIMS OF VOLUME 2 the chapter are presented according to a standardized format, and the institutional abbreviations have also been standardized and are This enterprise was originally conceived of as a single volume. How- listed in an appendix (Appendix III). ever, after a span of 10 years from its original conception, the current senior editor (Christine Janis), and the then junior editors (Kathleen Scott and Louis Jacobs) realized that it would be more realistic THE STANDARDIZED LAYOUT OF EACH CHAPTER to proceed with chapters then in hand, which could more or less be assembled into the conceptually useful, if taxonomically para- The chapters are laid out in a similar fashion to those in Volume 1. phyletic, rubric of “Terrestrial Carnivores and Ungulates” (Janis, The contributors were requested to adhere to a common layout for Scott, and Jacobs, 1998). This in part reflected the chapters that had each chapter, in order to provide uniform information throughout been assembled to date, although it should be noted that some of the book. The “Introduction” for each chapter introduces the group. the chapters in this current volume, most notably those by Darryl The “Defining features” section lays out the basic cranial, dental, Domning on sirenians and desmostylians, were among the first ones and postcranial features of the taxon.
    [Show full text]
  • Like Globin Genes in Monotremes and Therian Mammals
    Genomic evidence for independent origins of ␤-like globin genes in monotremes and therian mammals Juan C. Opazo*, Federico G. Hoffmann, and Jay F. Storz† School of Biological Sciences, University of Nebraska, Lincoln, NE 68588 Edited by Morris Goodman, Wayne State University School of Medicine, Detroit, MI, and approved December 13, 2007 (received for review November 5, 2007) Phylogenetic reconstructions of the ␤-globin gene family in ver- embryonic ␤-globin gene is exclusively expressed in primitive tebrates have revealed that developmentally regulated systems of erythroid cells derived from the yolk sac. However, the ‘‘␧- hemoglobin synthesis have been reinvented multiple times in globin’’ gene in birds is not orthologous to the ␧-globin gene in independent lineages. For example, the functional differentiation mammals (2, 12), because they are independently derived from of embryonic and adult ␤-like globin genes occurred independently lineage-specific duplications of a proto ␤-globin gene. in birds and mammals. In both taxa, the embryonic ␤-globin gene In placental mammals (subclass Eutheria), the ␤-globin gene is exclusively expressed in primitive erythroid cells derived from cluster includes a linked set of three early expressed (prenatal) the yolk sac. However, the ‘‘␧-globin’’ gene in birds is not ortholo- genes, ␧-␥-␩,atthe5Ј end of the cluster, and a pair of late gous to the ␧-globin gene in mammals, because they are indepen- expressed (adult) genes, ␦ and ␤,atthe3Ј end. There is extensive dently derived from lineage-specific duplications of a proto variation in the copy number of these different paralogs among ␤-globin gene. Here, we report evidence that the early and late species, and in a number of placental mammal lineages, the ␩- expressed ␤-like globin genes in monotremes and therian mam- and ␦-globin genes have been inactivated or deleted (13–15).
    [Show full text]
  • The Oldest Platypus and Its Bearing on Divergence Timing of the Platypus and Echidna Clades
    The oldest platypus and its bearing on divergence timing of the platypus and echidna clades Timothy Rowe*†, Thomas H. Rich‡§, Patricia Vickers-Rich§, Mark Springer¶, and Michael O. Woodburneʈ *Jackson School of Geosciences, University of Texas, C1100, Austin, TX 78712; ‡Museum Victoria, PO Box 666, Melbourne, Victoria 3001, Australia; §School of Geosciences, PO Box 28E, Monash University, Victoria 3800, Australia; ¶Department of Biology, University of California, Riverside, CA 92521; and ʈDepartment of Geology, Museum of Northern Arizona, Flagstaff, AZ 86001 Edited by David B. Wake, University of California, Berkeley, CA, and approved October 31, 2007 (received for review July 7, 2007) Monotremes have left a poor fossil record, and paleontology has broadly affect our understanding of early mammalian history, been virtually mute during two decades of discussion about with special implications for molecular clock estimates of basal molecular clock estimates of the timing of divergence between the divergence times. platypus and echidna clades. We describe evidence from high- Monotremata today comprises five species that form two resolution x-ray computed tomography indicating that Teinolo- distinct clades (16). The echidna clade includes one short-beaked phos, an Early Cretaceous fossil from Australia’s Flat Rocks locality species (Tachyglossus aculeatus; Australia and surrounding is- (121–112.5 Ma), lies within the crown clade Monotremata, as a lands) and three long-beaked species (Zaglossus bruijni, Z. basal platypus. Strict molecular clock estimates of the divergence bartoni, and Z. attenboroughi, all from New Guinea). The between platypus and echidnas range from 17 to 80 Ma, but platypus clade includes only Ornithorhynchus anatinus (Austra- Teinolophos suggests that the two monotreme clades were al- lia, Tasmania).
    [Show full text]
  • 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.
    [Show full text]
  • Early Cretaceous Amphilestid ('Triconodont') Mammals from Mongolia
    Early Cretaceous amphilestid ('triconodont') mammals from Mongolia ZOFIAKIELAN-JAWOROWSKA and DEMBERLYIN DASHZEVEG Kielan-Jaworowską Z. &Daslueveg, D. 1998. Early Cretaceous amphilestid (.tricono- dont') mammals from Mongotia. - Acta Pal.aeontol.ogicaPolonica,43,3, 413438. Asmall collection of ?Aptianor ?Albian amphilestid('triconodont') mammals consisting of incomplete dentaries and maxillae with teeth, from the Khoboor localiĘ Guchin Us counĘ in Mongolia, is described. Grchinodon Troftmov' 1978 is regarded a junior subjective synonym of GobiconodonTroftmov, 1978. Heavier wear of the molariforms M3 andM4than of themore anteriorone-M2 in Gobiconodonborissiaki gives indirect evidence formolariformreplacement in this taxon. The interlocking mechanismbetween lower molariforms n Gobiconodon is of the pattern seen in Kuchneotherium and Ttnodon. The ińterlocking mechanism and the type of occlusion ally Amphilestidae with Kuehneotheriidae, from which they differ in having lower molariforms with main cusps aligned and the dentary-squamosal jaw joint (double jaw joint in Kuehneotheńdae). The main cusps in upper molariforms M3-M5 of Gobiconodon, however, show incipient tńangular arrangement. The paper gives some support to Mills' idea on the therian affinities of the Amphilestidae, although it cannot be excluded that the characters that unite the two groups developed in parallel. Because of scanty material and arnbiguĘ we assign the Amphilestidae to order incertae sedis. Key words : Mammali4 .triconodonts', Amphilestidae, Kuehneotheriidae, Early Cretaceous, Mongolia. Zofia Kiel,an-Jaworowska [zkielnn@twarda,pan.pl], InsĘtut Paleobiologii PAN, ul. Twarda 5 I /5 5, PL-00-8 I 8 Warszawa, Poland. DemberĘin Dash7eveg, Geological Institute, Mongolian Academy of Sciences, Ulan Bator, Mongolia. Introduction Beliajeva et al. (1974) reportedthe discovery of Early Cretaceous mammals at the Khoboor locality (referred to also sometimes as Khovboor), in the Guchin Us Soinon (County), Gobi Desert, Mongolia.
    [Show full text]
  • Eutheria (Placental Mammals)
    Eutheria (Placental Introductory article Mammals) Article Contents . Introduction J David Archibald, San Diego State University, San Diego, California, USA . Basic Design . Taxonomic and Ecological Diversity Eutheria includes one of three major clades of mammals, the extant members of which are . Fossil History and Distribution referred to as placentals. Phylogeny Introduction have supernumerary teeth (e.g. some whales, armadillos, Eutheria (or Placentalia) is the most taxonomically diverse etc.), in extant placentals the number of teeth is at most of three branches or clades of mammals, the other two three upper and lower incisors, one upper and lower being Metatheria (or Marsupialia) and Prototheria (or canine, four upper and lower premolars, and three upper Monotremata). When named by Gill in 1872, Eutheria and lower molars. Except for one fewer upper molar, a included both marsupials and placentals. It was Huxley in domestic dog retains this pattern. Compared to reptiles, 1880 that recognized Eutheria basically as used today to mammals have fewer skull bones through fusion and loss, include only placentals. McKenna and Bell in their although bones are variously emphasized in each of the Classification of Mammals, published in 1997, chose to three major mammalian taxa. use Placentalia rather than Eutheria to avoid the confusion Physiologically, mammals are all endotherms of varying of what taxa should be included in Eutheria. Others such as degrees of efficiency. They are also homeothermic with a Rougier have used Eutheria and Placentalia in the sense relatively high resting temperature. These characteristics used here. Placentalia includes all extant placentals and are also found in birds, but because of anatomical their most recent common ancestor.
    [Show full text]
  • SUPPLEMENTARY INFORMATION: Tables, Figures and References
    Samuels et al. Evolution of the patellar sesamoid bone in mammals SUPPLEMENTARY INFORMATION: Tables, Figures and References Supplementary Table S1: Mammals$ Higher taxa Genus sp. Estimated. age of Patellar Comments# (partial) specimen, location state 0/1/2 (absent/ ‘patelloid’/ present) Sinoconodonta Sinoconodon Jurassic 0 Patellar groove absent, suggests no rigneyi (Kielan- patella Jaworowska, Cifelli & Luo, Sinoconodon is included on our 2004) phylogeny within tritylodontids. Morganucodonta Megazostrodon Late Triassic, southern 0 rudnerae (Jenkins Africa & Parrington, 1976) Morganucodonta Eozostrodon sp. Late Triassic, Wales 0 Asymmetric patellar groove, (Jenkins et al., specimens disarticulated so it is hard 1976) to assess the patella but appears absent Docodonta Castorocauda 164 Mya, mid-Jurassic, 0 Semi-aquatic adaptations lutrasimilis (Ji, China Luo, Yuan et al., 2006) Docodonta Agilodocodon 164 Mya, mid-Jurassic, 0 scansorius China (Meng, Ji, Zhang et al., 2015) Docodonta Docofossor 160 Mya 0 brachydactylus (Luo, Meng, Ji et al., 2015) Docodonta Haldanodon 150-155 Mya, Late 0 Shallow patellar groove exspectatus Jurassic, Portugal (Martin, 2005b) Australosphenida Asfaltomylos Mid-Jurassic, South ? Postcranial material absent patagonicus America (Martin, 2005a) Australosphenida Ornithorhynchus Extant 2 Platypus, genome sequenced Monotremata anatinus (Warren, Hillier, Marshall Graves et (Herzmark, 1938; al., 2008) Rowe, 1988) Samuels et al. Australosphenida Tachyglossus + Extant 2 Echidnas Monotremata Zaglossus spp. (Herzmark, 1938; Rowe, 1988) Mammaliaformes Fruitafossor 150 Mya, Late Jurassic, 0 Phylogenetic status uncertain indet. windscheffeli (Luo Colorado & Wible, 2005) Mammaliaformes Volaticotherium Late Jurassic/Early ? Hindlimb material incomplete indet. antiquus (Meng, Cretaceous Hu, Wang et al., 2006) Eutriconodonta Jeholodens 120-125 Mya, Early 0 Poorly developed patellar groove jenkinsi (Ji, Luo Cretaceous, China & Ji, 1999) Eutriconodonta Gobiconodon spp.
    [Show full text]
  • Two New Species of Gobiconodon (Mammalia, Eutriconodonta, Gobiconodontidae) from the Lower Cretaceous Shahai and Fuxin Formations, Northeastern China
    Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: http://www.tandfonline.com/loi/ghbi20 Two new species of Gobiconodon (Mammalia, Eutriconodonta, Gobiconodontidae) from the Lower Cretaceous Shahai and Fuxin formations, northeastern China Nao Kusuhashi, Yuan-Qing Wang, Chuan-Kui Li & Xun Jin To cite this article: Nao Kusuhashi, Yuan-Qing Wang, Chuan-Kui Li & Xun Jin (2016) Two new species of Gobiconodon (Mammalia, Eutriconodonta, Gobiconodontidae) from the Lower Cretaceous Shahai and Fuxin formations, northeastern China, Historical Biology, 28:1-2, 14-26 To link to this article: http://dx.doi.org/10.1080/08912963.2014.977881 Published online: 01 Oct 2015. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Download by: [University of Sussex Library] Date: 01 October 2015, At: 18:24 Historical Biology, 2016 Vol. 28, Nos. 1–2, 14–26, http://dx.doi.org/10.1080/08912963.2014.977881 Two new species of Gobiconodon (Mammalia, Eutriconodonta, Gobiconodontidae) from the Lower Cretaceous Shahai and Fuxin formations, northeastern China Nao Kusuhashia*, Yuan-Qing Wangb, Chuan-Kui Lib and Xun Jinb aDepartment of Earth’s Evolution and Environment, Graduate School of Science and Engineering, Ehime University, Ehime 790-8577, Japan; bKey Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, P.R. China (Received 29 July 2014; accepted 14 October 2014) Two new gobiconodontid mammals, Gobiconodon tomidai sp.
    [Show full text]
  • Short Beaked Echidna Final SAVEM
    The Short-beaked ECHIDNA Bac-yard Echidna All photos: Echidna diggings in Mallee In5ured Bea- Rachel ,estcott Species The Short-bea-ed Echidna (Tachyglossus aculeatus) is a usually solitary living monotreme found in all climatic conditions in the Australian bioregion. Echidnas can swim and climb, with home ranges up to or above 250 hectares (3 . Complete AVA SA Wildlife Admission Form. Place in SAME NA3CRA9 1IS3ARDE.. Admission and smooth plastic tub at least 50 cm in height & add handling shredded paper or straw. Restrain using (1 towels/ Echidna numbers cannot be esti- gloves to lift whole animal (2 lift gently beneath mated by numbers of diggings. ventrum without gloves (3 suspend by hind feet & Echidnas can enter torpor at any limbs'this is more stressful for the animal. time of year. Echidna —trains are Examination A conscious echidna wraps into a ball when part of courtship behaviour. touched, so complete e)amination requires chemical Breeding season is between $une restraint (see below (Schultz, pers. comm. 2012 . and September. ,eigh, assess body condition, wounds, fractures, condition of spines and bea-. Cloacal temp is 2.-320 C, 1R 2110 bpm, RR 2 10/min. Se) by everting penis. Spurs on hind limbs are not confined to males. 1ealthy animals should be released as soon as possible to the location of collection. Blood Sample from cephalic, 5ugular (near thoracic inlet), femoral or brachycephalic veins. Some clinicians Collection sample from the bea- sinus, but with great care. Anesthesia & 6asting is not required, but avoid anesthesia 6at storage in Panniculus adiposus beneath immediately after eating.
    [Show full text]
  • 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.
    [Show full text]