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Wyszukujesz frazę "ammonite" wg kryterium: Temat


Wyświetlanie 1-6 z 6
Tytuł:
Lower and Middle Cenomanian ammonites from the Morondava Basin, Madagascar
Autorzy:
Kennedy, W. J.
Walaszczyk, I.
Gale, A. S.
Dembicz, K.
Praszkier, T.
Powiązania:
https://bibliotekanauki.pl/articles/139375.pdf
Data publikacji:
2013
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Madagascar
Morondava Basin
cenomanian
ammonite succession
ammonite zonation
chronostratigraphy
Madagaskar
dorzecze
cenoman
amonit
sukcesja
podział na strefy
chronostratygrafia
Opis:
Lower and Middle Cenomanian ammonite assemblages have been collected on a bed-by-bed basis from localities at Vohipaly and Mahaboboka, Madagascar, as well as from outcrops around Berekata, all in the Morondava Basin, southwest Madagascar. These collections demonstrate the presence of the upper Lower Cenomanian Mantelliceras dixoni Zone and the lower Middle Cenomanian Cunningtoniceras inerme Zone of the north-western European standard sequence. These records indicate that the striking anomalies in the zonal assemblages of the classic divisions of the Madagascan Cenomanian are based on mixed assemblages, rather than a succession that differs radically from that elsewhere in the world. The dixoni Zone fauna is: Desmoceras cf. latidorsatum (Michelin, 1838), Pachydesmoceras kossmati Matsumoto, 1987, Forbesiceras sp., F. baylissiWright & Kennedy, 1984, F. largilliertianum (d'Orbigny, 1841), Mantelliceras cantianum Spath, 1926a, M. dixoni Spath, 1926b, M. mantelli (J. Sowerby, 1814), M. picteti Hyatt, 1903, M. saxbii (Sharpe, 1857), Sharpeiceras sp., S. falloti (Collignon, 1931), S. mocambiquense (Choffat, 1903), S. cf. florencae Spath, 1925, Acompsoceras renevieri (Sharpe, 1857), A. tenue Collignon, 1964, Calycoceras sp., Mrhiliceras lapparenti (Pervinquičre, 1907), Mariella (Mariella) stolizcai (Collignon, 1964), Hypoturrilites taxyfabreae (Collignon, 1964), Turrilites scheuchzerianus Bosc, 1801, Sciponoceras cucullatum Collignon, 1964, and Sciponoceras antanimangaensis (Collignon, 1964). The presence of Calycoceras in a Lower Cenomanian association represents a precocious appearance of a genus typically Middle and Upper Cenomanian in occurrence, and matches records from Tunisia. The inerme Zone yields a more restricted assemblage: Pachydesmoceras kossmati, Forbesiceras baylissi, Acanthoceras sp. juv., Cunningtoniceras cunningtoni (Sharpe, 1855) and Hypoturrilites taxyfabreae.
Źródło:
Acta Geologica Polonica; 2013, 63, 4; 625-655
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The lower and middle Berriasian in Central Tunisia: Integrated ammonite and calpionellid biostratigraphy of the Sidi Kralif Formation
Autorzy:
Maalaoui, K.
Zargouni, F.
Powiązania:
https://bibliotekanauki.pl/articles/138976.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
ammonite
calpionellids
Berriasian
bioevents
biostratigraphy
Tunisia
amonit
kalpionellidy
berias
biostratygrafia
Tunezja
Opis:
The lower and middle Berriasian sedimentary succession of the Sidi Kralif Formation has been a subject of biostratigraphic study in two key sections in Central Tunisia. Our contribution is an attempt to better define the basal Berriasian interval, between the Berriasella jacobi Zone and the Subthurmannia occitanica Zone. Zonal schemes are established using ammonites and calpionellids, and these permit correlation with other regions of Mediterranean Tethys and beyond. The use of biomarkers afforded by microfossil groups has allowed characterization and direct correlation with four widely accepted calpionellid sub-zones, namely Calpionella alpina, Remaniella, Calpionella elliptica and Tintinopsella longa. The two ammonite zones of Berriasella jacobi and of Subthurmannia occitanica are recognised on the basis of their index species. The parallel ammonite and calpionellid zonations are useful as a tool for correlation and calibration in time and space, thus allowing a better definition of a J/K boundary. The presence of four Berriasian calpionellid bioevents is recognised: (1) the ‘explosion’ of Calpionella alpina, (2) the first occurrence of Remaniella, (3) the first occurrence of Calpionella elliptica and (4) the first occurrence of Tintinopsella longa. The last is here documented as coeval with the presence of Subthurmannia occitanica, which marks the lower/middle Berriasian boundary.
Źródło:
Acta Geologica Polonica; 2016, 66, 1; 43-58
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mosasauroid predation on an ammonite – Pseudaspidoceras – from the Early Turonian of south-eastern Morocco
Autorzy:
Gale, A. S.
Kennedy, W. J.
Martill, D.
Powiązania:
https://bibliotekanauki.pl/articles/138610.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
predation
ammonite
mosasauroidae
Cretaceous
Turonian
Morocco
drapieżnictwo
amonit
mozazaury
kreda
turon
Maroko
Opis:
A juvenile specimen of the ammonite Pseudaspidoceras from the Early Turonian of the Goulmima area in the Province of Er-Rachida in south-eastern Morocco shows clear evidence of predation by a tooth-bearing verte-brate. Most of the body chamber is missing, as a result of post-burial compactional crushing. The adapertural part of the shell on the left flank of the surviving fragment of body chamber bears six circular punctuations; the right flank four. These are interpreted as the product of a single bite by a mosasauroid, probably a Tethysaurus. The taxonomy of the Goulmima Pseudaspidoceras is discuused in an appendix.
Źródło:
Acta Geologica Polonica; 2017, 67, 1; 31-46
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
In his own words
Autorzy:
Cobban, W. A.
Powiązania:
https://bibliotekanauki.pl/articles/139103.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
interview
biography
ammonite
geology
palaeontology
Cobban William
wywiad
biografia
amonit
geologia
paleontologia
Opis:
Bill Cobban in conversation with Kirk Johnson and Dave Baysinger, 19 February, 2010.
Źródło:
Acta Geologica Polonica; 2016, 66, 4; III-XIII
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The ammonite genus Prionocycloceras Spath, 1926, from the Coniacian of KwaZulu-Natal, South Africa
Autorzy:
Klinger, H. C.
Kennedy, W. J.
Powiązania:
https://bibliotekanauki.pl/articles/138691.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Cretaceous
coniacian
ammonite
prionocycloceras
KwaZulu-Natal
South Africa
kreda
koniak
amonit
Prionocycloceras
Afryka Południowa
Opis:
Subprionocyclus latiumbilicatus Van Hoepen, 1968, and Subprionocyclus obesus Van Hoepen, 1968, are revised, and referred to Prionocycloceras Spath, 1926, a genus not previously recognised from the South African Cretaceous. The material comes from the Middle and Upper Coniacian St Lucia Formation of northern KwaZulu-Natal.
Źródło:
Acta Geologica Polonica; 2016, 66, 4; 663-669
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A unique fossil record from neptunian sills: the worlds most extreme example of stratigraphic condensation (Jurassic, western Sicily)
Autorzy:
Wendt, J.
Powiązania:
https://bibliotekanauki.pl/articles/139227.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Sicily
Jurassic
biostratigraphy
synsedimentary tectonics
Neptunian sills
condensation
ammonite fauna
sea level
Sycylia
jura
biostratygrafia
tektonika synsedymentacyjna
kondensacja
amonity
poziom morza
Opis:
Neptunian sills at Rocca Busambra, a fragment of the Trapanese/Saccense Domain in western Sicily, host the most abundant ammonite and gastropod fauna which has ever been recorded from the Jurassic of the western Tethys. The fauna is dominated by parautochthonous organisms which were swept into the sills by gentle transport. Ammonites are characterized by perfect preservation and small size, a feature which is due to the predominance of microconchs but also of stunting. The most complete sill is 0.7 m thick and could be separated into 17 levels which range in age from the early Toarcian into the late Kimmeridgian, thus representing the most extreme case of palaeontologically and depositionally documented stratigraphic condensation in Earth history. The unique feature of the Rocca Busambra sills is due to the interaction of three processes: extreme stratigraphic condensation on the sea floor, weak tectonic fracturing of the host rock and repeated reopening on top of already existing sills. Contrasting percentages of gastropods in individual levels reflect sea-level oscillations which correspond to long known low- and highstands during the Jurassic of the western Tethys. Comparisons with other ammonite-bearing sill faunas reveal several similarities, but represent only short-timed phases of tectonic pulses and deposition.
Źródło:
Acta Geologica Polonica; 2017, 67, 2; 163-199, [6]
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-6 z 6

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