The Ecomorphology of Facultative Bipedality in Lepidosauria: Implications for the Evolution of Reptilian Bipedality
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Comparative Locomotor Performance of Marsupial and Placental Mammals
J. Zool., Lond. (1988) 215, 505-522 Comparative locomotor performance of marsupial and placental mammals T. GARLAND,JR Department of Zoology, University of Wisconsin, Madison, WZ 53706, USA School of Biological Sciences, The Flinders University of South Australia, Bedford Park, Adelaide, 5042, South Australia (Accepted 13 October 1987) (With 6 figures in the text) Marsupials are often considered inferior to placental mammals in a number of physiological characters. Because locomotor performance is presumed to be an important component of fitness, we compared marsupials and placentals with regard to both maximal running speeds and maximal aerobic speeds (=speed at which the maximal rate of oxygen consumption, \jozmax, is attained). Maximal aerobic speed is related to an animal's maximal sustainable speed, and hence is a useful comparative index of stamina. Maximal running speeds of 1 I species of Australian marsupials, eight species of Australian murid rodents, two species of American didelphid marsupials, and two species of American rodents were measured in the laboratory and compared with data compiled from the literature. Our values are greater than, or equivalent to, those reported previously. Marsupials and placentals do not differ in maximal running speeds (nor do Australian rodents differ from non- Australian rodents). Within these groups, however, species and families may differ considerably. Some of the interspecific variation in maximal running speeds is related to differences in habitat: species inhabiting open habitats (e.g. deserts) tend to be faster than are species from habitats with more cover, or arboreal species. Maximal aerobic speeds (compiled from the literature) were higher in large species than in small species. -
Ischigualasto Formation. the Second Is a Sile- Diversity Or Abundance, but This Result Was Based on Only 19 of Saurid, Ignotosaurus Fragilis (Fig
This article was downloaded by: [University of Chicago Library] On: 10 October 2013, At: 10:52 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Vertebrate Paleontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ujvp20 Vertebrate succession in the Ischigualasto Formation Ricardo N. Martínez a , Cecilia Apaldetti a b , Oscar A. Alcober a , Carina E. Colombi a b , Paul C. Sereno c , Eliana Fernandez a b , Paula Santi Malnis a b , Gustavo A. Correa a b & Diego Abelin a a Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan , España 400 (norte), San Juan , Argentina , CP5400 b Consejo Nacional de Investigaciones Científicas y Técnicas , Buenos Aires , Argentina c Department of Organismal Biology and Anatomy, and Committee on Evolutionary Biology , University of Chicago , 1027 East 57th Street, Chicago , Illinois , 60637 , U.S.A. Published online: 08 Oct 2013. To cite this article: Ricardo N. Martínez , Cecilia Apaldetti , Oscar A. Alcober , Carina E. Colombi , Paul C. Sereno , Eliana Fernandez , Paula Santi Malnis , Gustavo A. Correa & Diego Abelin (2012) Vertebrate succession in the Ischigualasto Formation, Journal of Vertebrate Paleontology, 32:sup1, 10-30, DOI: 10.1080/02724634.2013.818546 To link to this article: http://dx.doi.org/10.1080/02724634.2013.818546 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. -
A New Subspecies of Jackyhosersaur Hoser, 2013 from North-West Australia
Australasian Journal of Herpetology 5 Australasian Journal of Herpetology 49:5-6. Published 6 August 2020. ISSN 1836-5698 (Print) ISSN 1836-5779 (Online) A new subspecies of Jackyhosersaur Hoser, 2013 from north-west Australia. LSIDURN:LSID:ZOOBANK.ORG:PUB:2877185D-E93C-4040-973C-89657DC512B1 RAYMOND T. HOSER LSID urn:lsid:zoobank.org:author:F9D74EB5-CFB5-49A0-8C7C-9F993B8504AE 488 Park Road, Park Orchards, Victoria, 3134, Australia. Phone: +61 3 9812 3322 Fax: 9812 3355 E-mail: snakeman (at) snakeman.com.au Received 10 February 2017, Accepted 17 January 2020, Published 6 August 2020. ABSTRACT As part of an ongoing audit of Australian reptiles, specimens of the endemic Western Australian dragon species, Jackyhosersaur superba (Storr, 1974), known to most herpetologists as “Diporiphora superba Storr, 1974” were inspected from all parts of the known range. A population from the Manning Creek Gorge area of the Kimberley in Western Australia were found to be morphologically divergent and so are formally described herein as a new subspecies. Keywords: Lizards; taxonomy; nomenclature; Agamidae; Western Australia; Diporiphora; Jackyhosersaur; superba; newsubspecies; jackyhoserae. INTRODUCTION Jackyhosersaur superba (Storr, 1974) as currently recognized, As stated in the abstract, as part of an ongoing audit of even though all occur within close geographical proximity, being Australian reptiles, specimens of the endemic Western restricted to the high rainfall parts of the West Kimberley Region. Australian dragon species, Jackyhosersaur superba (Storr, Significant is that the species appears to be reasonably 1974) were inspected from all parts of the known range. A common and different populations are in close proximity to one population from the Manning Creek Gorge area of the Kimberley another without obvious biogeographical barriers stopping gene in Western Australia were found to be morphologically divergent flow between them. -
An Annotated Type Catalogue of the Dragon Lizards (Reptilia: Squamata: Agamidae) in the Collection of the Western Australian Museum Ryan J
RECORDS OF THE WESTERN AUSTRALIAN MUSEUM 34 115–132 (2019) DOI: 10.18195/issn.0312-3162.34(2).2019.115-132 An annotated type catalogue of the dragon lizards (Reptilia: Squamata: Agamidae) in the collection of the Western Australian Museum Ryan J. Ellis Department of Terrestrial Zoology, Western Australian Museum, Locked Bag 49, Welshpool DC, Western Australia 6986, Australia. Biologic Environmental Survey, 24–26 Wickham St, East Perth, Western Australia 6004, Australia. Email: [email protected] ABSTRACT – The Western Australian Museum holds a vast collection of specimens representing a large portion of the 106 currently recognised taxa of dragon lizards (family Agamidae) known to occur across Australia. While the museum’s collection is dominated by Western Australian species, it also contains a selection of specimens from localities in other Australian states and a small selection from outside of Australia. Currently the museum’s collection contains 18,914 agamid specimens representing 89 of the 106 currently recognised taxa from across Australia and 27 from outside of Australia. This includes 824 type specimens representing 45 currently recognised taxa and three synonymised taxa, comprising 43 holotypes, three syntypes and 779 paratypes. Of the paratypes, a total of 43 specimens have been gifted to other collections, disposed or could not be located and are considered lost. An annotated catalogue is provided for all agamid type material currently and previously maintained in the herpetological collection of the Western Australian Museum. KEYWORDS: type specimens, holotype, syntype, paratype, dragon lizard, nomenclature. INTRODUCTION Australia was named by John Edward Gray in 1825, The Agamidae, commonly referred to as dragon Clamydosaurus kingii Gray, 1825 [now Chlamydosaurus lizards, comprises over 480 taxa worldwide, occurring kingii (Gray, 1825)]. -
Rethinking the Evolution of the Human Foot: Insights from Experimental Research Nicholas B
© 2018. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2018) 221, jeb174425. doi:10.1242/jeb.174425 REVIEW Rethinking the evolution of the human foot: insights from experimental research Nicholas B. Holowka* and Daniel E. Lieberman* ABSTRACT presumably owing to their lack of arches and mobile midfoot joints Adaptive explanations for modern human foot anatomy have long for enhanced prehensility in arboreal locomotion (see Glossary; fascinated evolutionary biologists because of the dramatic differences Fig. 1B) (DeSilva, 2010; Elftman and Manter, 1935a). Other studies between our feet and those of our closest living relatives, the great have documented how great apes use their long toes, opposable apes. Morphological features, including hallucal opposability, toe halluces and mobile ankles for grasping arboreal supports (DeSilva, length and the longitudinal arch, have traditionally been used to 2009; Holowka et al., 2017a; Morton, 1924). These observations dichotomize human and great ape feet as being adapted for bipedal underlie what has become a consensus model of human foot walking and arboreal locomotion, respectively. However, recent evolution: that selection for bipedal walking came at the expense of biomechanical models of human foot function and experimental arboreal locomotor capabilities, resulting in a dichotomy between investigations of great ape locomotion have undermined this simple human and great ape foot anatomy and function. According to this dichotomy. Here, we review this research, focusing on the way of thinking, anatomical features of the foot characteristic of biomechanics of foot strike, push-off and elastic energy storage in great apes are assumed to represent adaptations for arboreal the foot, and show that humans and great apes share some behavior, and those unique to humans are assumed to be related underappreciated, surprising similarities in foot function, such as to bipedal walking. -
Late Triassic) Adrian P
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/56 Definition and correlation of the Lamyan: A new biochronological unit for the nonmarine Late Carnian (Late Triassic) Adrian P. Hunt, Spencer G. Lucas, and Andrew B. Heckert, 2005, pp. 357-366 in: Geology of the Chama Basin, Lucas, Spencer G.; Zeigler, Kate E.; Lueth, Virgil W.; Owen, Donald E.; [eds.], New Mexico Geological Society 56th Annual Fall Field Conference Guidebook, 456 p. This is one of many related papers that were included in the 2005 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. -
KENNETH A. NAGY PUBLICATIONS up to JUNE 2016
KENNETH A. NAGY PUBLICATIONS Up to JUNE 2016 For Open Access pdf, click link. For copyrighted reprint pdfs, please email your request to Ken Nagy at [email protected]. I will be happy to share a copy of the article with individual colleagues, when permissible under copyright law. 2016 Nagy, K.A., G. Kuchling, L.S. Hillard, and B.T. Henen. (2016) Weather and sex ratios of head-started Agassiz’s desert tortoise Gopherus agassizii juveniles hatched in natural habitat enclosures. Endangered Species Research 30:145- 155. (Research article) (Link to pdf) Ellsworth, E., M.R. Boudreau, K. Nagy, J.L. Rachlow, and D.L. Murray. (2016). Differential sex-related winter energetics in free-ranging snowshoe hAres (Lepus americanus). Canadian Journal of Zoology 94:115-121. (Research article) (link to pdf) 2015 Nagy, K.A., S.Hillard, S. Dickson, and D.J. Morafka. (2015). Effects of artificial rain on survivorship, body condition, and growth of head-started desert tortoises (Gopherus agassizii) released to the open desert. Herpetological Conservation and Biology 10:535-549. (Research article) (Link to pdf) Nagy, K.A., L.S. Hillard, M.W. Tuma, and D.J. Morafka. (2015). Head-started desert tortoises (Gopherus agassizii): Movements, survivorship and mortality causes following their release. Herpetological Conservation and Biology 10:203-215. (Research article) (link to pdf) 2014 Gienger, C.M., C.R. Tracy, and K.A. Nagy. (2014). Life in the slow lane: GilA Monsters have low rates of energy use and water flux. Copeia 2014:279-287. (Research article) (email Nagy for pdf) 2012 Nagy, K.A., and G.G. -
Origin of Tropical American Burrowing Reptiles by Transatlantic Rafting
Biol. Lett. in conjunction with head movements to widen their doi:10.1098/rsbl.2007.0531 burrows (Gans 1978). Published online Amphisbaenians (approx. 165 species) provide an Phylogeny ideal subject for biogeographic analysis because they are limbless (small front limbs are present in three species) and fossorial, presumably limiting dispersal, Origin of tropical American yet they are widely distributed on both sides of the Atlantic Ocean (Kearney 2003). Three of the five burrowing reptiles by extant families have restricted geographical ranges and contain only a single genus: the Rhineuridae (genus transatlantic rafting Rhineura, one species, Florida); the Bipedidae (genus Nicolas Vidal1,2,*, Anna Azvolinsky2, Bipes, three species, Baja California and mainland Corinne Cruaud3 and S. Blair Hedges2 Mexico); and the Blanidae (genus Blanus, four species, Mediterranean region; Kearney & Stuart 2004). 1De´partement Syste´matique et Evolution, UMR 7138, Syste´matique, Evolution, Adaptation, Case Postale 26, Muse´um National d’Histoire Species in the Trogonophidae (four genera and six Naturelle, 57 rue Cuvier, 75231 Paris Cedex 05, France species) are sand specialists found in the Middle East, 2Department of Biology, 208 Mueller Laboratory, Pennsylvania State North Africa and the island of Socotra, while the University, University Park, PA 16802-5301, USA largest and most diverse family, the Amphisbaenidae 3Centre national de se´quenc¸age, Genoscope, 2 rue Gaston-Cre´mieux, CP5706, 91057 Evry Cedex, France (approx. 150 species), is found on both sides of the *Author and address for correspondence: De´partment Syste´matique et Atlantic, in sub-Saharan Africa, South America and Evolution, UMR 7138, Syste´matique, Evolution, Adoptation, Case the Caribbean (Kearney & Stuart 2004). -
And Early Jurassic Sediments, and Patterns of the Triassic-Jurassic
and Early Jurassic sediments, and patterns of the Triassic-Jurassic PAUL E. OLSEN AND tetrapod transition HANS-DIETER SUES Introduction parent answer was that the supposed mass extinc- The Late Triassic-Early Jurassic boundary is fre- tions in the tetrapod record were largely an artifact quently cited as one of the thirteen or so episodes of incorrect or questionable biostratigraphic corre- of major extinctions that punctuate Phanerozoic his- lations. On reexamining the problem, we have come tory (Colbert 1958; Newell 1967; Hallam 1981; Raup to realize that the kinds of patterns revealed by look- and Sepkoski 1982, 1984). These times of apparent ing at the change in taxonomic composition through decimation stand out as one class of the great events time also profoundly depend on the taxonomic levels in the history of life. and the sampling intervals examined. We address Renewed interest in the pattern of mass ex- those problems in this chapter. We have now found tinctions through time has stimulated novel and com- that there does indeed appear to be some sort of prehensive attempts to relate these patterns to other extinction event, but it cannot be examined at the terrestrial and extraterrestrial phenomena (see usual coarse levels of resolution. It requires new fine- Chapter 24). The Triassic-Jurassic boundary takes scaled documentation of specific faunal and floral on special significance in this light. First, the faunal transitions. transitions have been cited as even greater in mag- Stratigraphic correlation of geographically dis- nitude than those of the Cretaceous or the Permian junct rocks and assemblages predetermines our per- (Colbert 1958; Hallam 1981; see also Chapter 24). -
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HAMADRYAD Vol. 27. No. 2. August, 2003 Date of issue: 31 August, 2003 ISSN 0972-205X CONTENTS T. -M. LEONG,L.L.GRISMER &MUMPUNI. Preliminary checklists of the herpetofauna of the Anambas and Natuna Islands (South China Sea) ..................................................165–174 T.-M. LEONG & C-F. LIM. The tadpole of Rana miopus Boulenger, 1918 from Peninsular Malaysia ...............175–178 N. D. RATHNAYAKE,N.D.HERATH,K.K.HEWAMATHES &S.JAYALATH. The thermal behaviour, diurnal activity pattern and body temperature of Varanus salvator in central Sri Lanka .........................179–184 B. TRIPATHY,B.PANDAV &R.C.PANIGRAHY. Hatching success and orientation in Lepidochelys olivacea (Eschscholtz, 1829) at Rushikulya Rookery, Orissa, India ......................................185–192 L. QUYET &T.ZIEGLER. First record of the Chinese crocodile lizard from outside of China: report on a population of Shinisaurus crocodilurus Ahl, 1930 from north-eastern Vietnam ..................193–199 O. S. G. PAUWELS,V.MAMONEKENE,P.DUMONT,W.R.BRANCH,M.BURGER &S.LAVOUÉ. Diet records for Crocodylus cataphractus (Reptilia: Crocodylidae) at Lake Divangui, Ogooué-Maritime Province, south-western Gabon......................................................200–204 A. M. BAUER. On the status of the name Oligodon taeniolatus (Jerdon, 1853) and its long-ignored senior synonym and secondary homonym, Oligodon taeniolatus (Daudin, 1803) ........................205–213 W. P. MCCORD,O.S.G.PAUWELS,R.BOUR,F.CHÉROT,J.IVERSON,P.C.H.PRITCHARD,K.THIRAKHUPT, W. KITIMASAK &T.BUNDHITWONGRUT. Chitra burmanica sensu Jaruthanin, 2002 (Testudines: Trionychidae): an unavailable name ............................................................214–216 V. GIRI,A.M.BAUER &N.CHATURVEDI. Notes on the distribution, natural history and variation of Hemidactylus giganteus Stoliczka, 1871 ................................................217–221 V. WALLACH. -
The Osteoderm Microstructure in Doswelliids and Proterochampsids and Its Implications for Palaeobiology of Stem Archosaurs
The osteoderm microstructure in doswelliids and proterochampsids and its implications for palaeobiology of stem archosaurs DENIS A. PONCE, IGNACIO A. CERDA, JULIA B. DESOJO, and STERLING J. NESBITT Ponce, D.A., Cerda, I.A., Desojo, J.B., and Nesbitt, S.J. 2017. The osteoderm microstructure in doswelliids and proter- ochampsids and its implications for palaeobiology of stem archosaurs. Acta Palaeontologica Polonica 62 (4): 819–831. Osteoderms are common in most archosauriform lineages, including basal forms, such as doswelliids and proterochamp- sids. In this survey, osteoderms of the doswelliids Doswellia kaltenbachi and Vancleavea campi, and proterochampsid Chanaresuchus bonapartei are examined to infer their palaeobiology, such as histogenesis, age estimation at death, development of external sculpturing, and palaeoecology. Doswelliid osteoderms have a trilaminar structure: two corti- ces of compact bone (external and basal) that enclose an internal core of cancellous bone. In contrast, Chanaresuchus bonapartei osteoderms are composed of entirely compact bone. The external ornamentation of Doswellia kaltenbachi is primarily formed and maintained by preferential bone growth. Conversely, a complex pattern of resorption and redepo- sition process is inferred in Archeopelta arborensis and Tarjadia ruthae. Vancleavea campi exhibits the highest degree of variation among doswelliids in its histogenesis (metaplasia), density and arrangement of vascularization and lack of sculpturing. The relatively high degree of compactness in the osteoderms of all the examined taxa is congruent with an aquatic or semi-aquatic lifestyle. In general, the osteoderm histology of doswelliids more closely resembles that of phytosaurs and pseudosuchians than that of proterochampsids. Key words: Archosauria, Doswelliidae, Protero champ sidae, palaeoecology, microanatomy, histology, Triassic, USA. -
Aetosaurs (Archosauria: Stagonolepididae) from the Upper Triassic (Revueltian) Snyder Quarry, New Mexico
Zeigler, K.E., Heckert, A.B., and Lucas, S.G., eds., 2003, Paleontology and Geology of the Snyder Quarry, New Mexico Museum of Natural History and Science Bulletin No. 24. 115 AETOSAURS (ARCHOSAURIA: STAGONOLEPIDIDAE) FROM THE UPPER TRIASSIC (REVUELTIAN) SNYDER QUARRY, NEW MEXICO ANDREW B. HECKERT, KATE E. ZEIGLER and SPENCER G. LUCAS New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, NM 87104-1375 Abstract—Two species of aetosaurs are known from the Snyder quarry (NMMNH locality 3845): Typothorax coccinarum Cope and Desmatosuchus chamaensis Zeigler, Heckert, and Lucas. Both are represented entirely by postcrania, principally osteoderms (scutes), but also by isolated limb bones. Aetosaur fossils at the Snyder quarry are, like most of the vertebrates found there, not articulated. However, clusters of scutes, presumably each from a single carapace, are associated. Typothorax coccinarum is an index fossil of the Revueltian land- vertebrate faunachron (lvf) and its presence was expected at the Snyder quarry, as it is known from correlative strata throughout the Chama basin locally and the southwestern U.S.A. regionally. The Snyder quarry is the type locality of D. chamaensis, which is considerably less common than T. coccinarum, and presently known from only one other locality. Some specimens we tentatively assign to D. chamaensis resemble lateral scutes of Paratypothorax, but we have not found any paramedian scutes of Paratypothorax at the Snyder quarry, so we refrain from identifying them as Paratypothorax. Specimens of both Typothorax and Desmatosuchus from the Snyder quarry yield insight into the anatomy of these taxa. Desmatosuchus chamaensis is clearly a species of Desmatosuchus, but is also one of the most distinctive aetosaurs known.