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Wyszukujesz frazę "Lockley, M. G." wg kryterium: Autor


Wyświetlanie 1-5 z 5
Tytuł:
New perspectives on morphological variation in tridactyl footprints: clues to widespread convergence in developmental dynamics
Autorzy:
Lockley, M. G.
Powiązania:
https://bibliotekanauki.pl/articles/2059254.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Opis:
It is well-known that the phalangeal formulae of the feet of dinosaurs and other vertebrates are relatively consistent within any given clade. Indeed, such similarities are part of the basis for alpha taxonomy (e.g., bird and non-avian theropod relation ships). Developmental studies of the vertebrate foot support the view that morphological similarity owes as much to intrinsic (formal) developmental dynamics as to exrinic (functional) influences. Thus, the morphologies of ornithopod, non-avian theropod and most bird feet are convergent (especially with respect to digits II–IV) despite significant differences in size and functional adaptation. Despite these "general" convergences, "detailed" variation in the morphology of tridactyl, mesaxonic, Triassic through recent non-avian dinosaur and bird tracks has allowed the diagnosis of hundreds of ichnotaxa, as well as the recogni ion of nearly continuous subtle variation in modern bird tracks. Several studies characterize this variation by measuring how far digit III projects anteriorly beyond lateral digit IV and medial digit II, creating an "anterior triangle" between the tips of digits II, III and IV (Weems, 1992). Differences in this projection of digit III highlight a polarity between strong mesaxony (strong central tendency) and weak mesaxony (weak central tendency). Early studies (Olsen, 1980) suggested that as theropod tracks in the Grallator–Eubrontes plexus increase in size, they shift from narrow to wide and from strongly to weakly mesaxonic. However, such polarities also reiterate (independent of size) among medium-sized and diminutive theropod tracks (e.g., Minisauripus). Such polarity also recurs among ornithopods, and is equally striking in extant birds (e.g., between passerines and members of the charadriiformes). Such "intrinsic" differences canonly be partially attributed to functional variation in digit divarication caused by foot-substrate interaction. Moreover, such polarities in foot morphology give important clues to whole limb and whole body proportions, and suggest an intrinsic "lawfulness" to patterns of convergence.
Źródło:
Geological Quarterly; 2009, 53, 4; 415-432
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Jurassic tetrapod footprint ichnofaunas and ichnofacies of the Western Interior, USA
Autorzy:
Lockley, M.
Gierlinski, G.
Powiązania:
https://bibliotekanauki.pl/articles/2077341.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Jurassic
footprints
ichnofacies
dinosaurs
pterosaurs
Western Interior
jura
ślady
dinozaury
Opis:
The Jurassic tetrapod track record of the Western Interior, USA, is one of the most diverse, complete and well-studied in the world, spanning a relatively continuous representation of Lower, Middle and Upper Jurassic formations. Although a few of these formations, notably the Morrison Formation, have yielded abundant body fossils, the majority lack abundant skeletal remains and, while trackrich, are in some cases completely barren of body fossils. Thus, the track record assumes great importance as the most complete and representative record of changing tetrapod faunas through time in a region where the body fossil record is often sparse or absent. In the Lower and Middle Jurassic, many distinctive assemblages are associated with eolian units (Wingate, Navajo and Entrada) that are almost devoid of body fossils. However, the former two units are rich in synapsid tracks characterized as the Brasilichnium ichnofacies. In the Middle Jurassic, fluctuating sea-levels exerted important controls on the distribution of theropod and pterosaur-dominated ichnofaunas associated with coastal plain and marginal marine settings. The Morrison ichnofauna is a reliable reflection of the body fossil record of that formation. Ongoing efforts to group and classify the various tetrapod ichnofaunas into tetrapod ichnofacies and tetrapod biochron categories have, in some cases, provoked stimulating, if sometimes inconclusive, debate.
Źródło:
Volumina Jurassica; 2014, 12, 2; 133-150
1896-7876
1731-3708
Pojawia się w:
Volumina Jurassica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
First report on dinosaur tracks from the Burro Canyon Formation, San Juan County, Utah, USA : evidence of a diverse, hitherto unknown Lower Cretaceous dinosaur fauna
Autorzy:
Milàn, J.
Chiappe, L. M.
Loope, D. B.
Kirkland, J. I.
Lockley, M. G.
Powiązania:
https://bibliotekanauki.pl/articles/191615.pdf
Data publikacji:
2015
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
dinosaur tracks
Lower Cretaceous
Barremian
Utah
pathology
dinosaur fauna
Opis:
The newly discovered White Mesa tracksite in the Burro Canyon Formation represents a snapshot of a diverse, Lower Cretaceous dinosaur fauna from south-eastern Utah. The tracks were found at a construction site where the sandstone had been bulldozed and broken up. All tracks were found as deep, well-preserved natural casts on the underside of the sandstone slabs. Individual theropod tracks are 19–57 cm in length; one peculiar track shows evidence of a possible pathological swelling in the middle of digit III and an apparently didactyl track is tentatively assigned to a dromaeosaurid. Individual sauropod tracks are found with pes lengths of 36–72 cm, and interestingly, three distinct shapes of manus tracks, ranging from wide banana shaped to rounded and hoof-like. Ornithopods are represented with individual tracks 18–37 cm in length; a sin gle track can possibly be attributed to the thyreophoran ichnogenus Deltapodus. Zircon U-Pb dating places the track-bearing layer in the Barremian, contemporary to the lower Yellow Cat Member of the Cedar Mountain Formation, which has a similar faunal composition based on both tracks and body fossils. This new track-fauna demonstrates the existence of a diverse dinosaurian assemblage in the lower part of the Burro Canyon Formation, which hitherto is not known to yield skeletalre mains.
Źródło:
Annales Societatis Geologorum Poloniae; 2015, 85, 3; 515-525
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A Grallator-dominated tracksite from the Chinle Group (Late Triassic), Moab, Utah
Autorzy:
Lockley, M. G.
Gierlinski, G. D.
Powiązania:
https://bibliotekanauki.pl/articles/2059243.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Utah
Moab
Chinle Group
footprints
theropod dinosaurs
Grallator
Opis:
Two roadside localities on the northern fringes of Moab, Grand County, Utah yield previously un-described Upper Triassic vertebrate tracks from the Chinle Group (Rock Point Formation). The first locality, designated the high way 191 site, yields dozens of small theropod dinosaur tracks (Grallator) preserved on a single, fallen slab. The tracks form a monospecific assemblage preserved as natural casts. The assemblage is representative of what has been referred to as Rhaetic assemblage II which is dominated by small Grallator tracks. In situ Grallator tracks are also described from a nearby locality, referred to as the Matrimony Spring site, where they are found in association with the ichnogenus Brachychirotherium. Many other sites with similar, often more-diverse, Late Triassic ichnofaunas are known from the region.
Źródło:
Geological Quarterly; 2009, 53, 4; 433-440
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A distinctive crouching theropod trace from the Lower Jurassic of Poland
Autorzy:
Gierliński, G. D.
Lockley, M. G.
Niedźwiedzki, G.
Powiązania:
https://bibliotekanauki.pl/articles/2059247.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polska
Holy Cross Mountains
Lower Jurassic
dinosaur crouching trace
Opis:
A well-preserved, essentially complete and distinctive trace fossil of a crouching, medium-sized theropod dinosaur is reported from the northern slope of the Holy Cross Mountains, Poland. Crouching theropod traces are rare, and currently known from only six specimens from the Jurassic of North America and Asia. Thus, this new specimen adds a seventh specimen to the dinosaur track record. The specimen was found in the Early Jurassic (Late Pliensbachian) sandstones mined in the Szydłówek quarry, in the vicinity of Szydłowiec.
Źródło:
Geological Quarterly; 2009, 53, 4; 471-476
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-5 z 5

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