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Aretz et al_2011.pdf - ORBi - Université de Liège

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Kölner Forum Geol. P<strong>al</strong>äont., 19 (2011)<br />

M. ARETZ, S. DELCULÉE, J. DENAYER & E. POTY (Eds.)<br />

Abstracts, 11th Symposium on Fossil Cnidaria and Sponges, <strong>Liège</strong>, August 19-29, 2011<br />

_________________________________________________________________________________________________________<br />

similarity to the type materi<strong>al</strong> (FOMICHEV 1953) <strong>al</strong>lows to establish the species range from the latest<br />

Myachkovian to the sagitt<strong>al</strong>is zone of the Kasimovian. B. timanoi<strong>de</strong>s timanoi<strong>de</strong>s FEDOROWSKI 1975, Ambigua<br />

Lm., Sv<strong>al</strong>bard <strong>al</strong>so bears the rather simple axi<strong>al</strong> structure, but shows shorter minor septa (FEDOROWSKI<br />

1975: 61, fig.8). The group of cor<strong>al</strong>s possessing simplified features is different from the topotypes of B.<br />

conicum <strong>de</strong>monstrating well <strong>de</strong>veloped axi<strong>al</strong> structures. The typic<strong>al</strong> B. conicum is similar with the specimen<br />

assigned to a new Bothrophyllum species d<strong>et</strong>ermined in the Donskaya Luka at the bas<strong>al</strong> Kasimovian (in its<br />

tradition<strong>al</strong> meaning).<br />

Siedleckia FEDOROWSKI 1975 is another abundant genus among the caninomorph cor<strong>al</strong>s of the transition<strong>al</strong><br />

interv<strong>al</strong>. It appeared in the Moscovian (the type species S. mutafii (GORSKY 1978) and it <strong>al</strong>so occurs in the<br />

lowermost Kasimovian in the Donskaya Luka and is known from the Kasimovian of the Ambigua Lm. and<br />

the Ur<strong>al</strong>s (GREK 1936).<br />

The specific ontogen<strong>et</strong>ic <strong>de</strong>velopment of the specimens from the Donskaya Luka seems to be a strong<br />

reason to propose a new genus. It shows the long duration of the primitive amplexoid neanic stage. By the<br />

short minor septa, gener<strong>al</strong> caninomorph habitus of the mature stage the new genus is similar with<br />

Caninophyllum domheri FOMICHEV 1953, forma b. The long counter septum brings it tog<strong>et</strong>her with B.<br />

timanicum timanicum (FEDOROWSKI 1975) and some Timania species, but the difference in ontogeny<br />

contradicts the typic<strong>al</strong> succession of the evolution stages of both genera. Pseudotimania DORBOLYUBOVA &<br />

KABAKOVICH 1948 bearing caninomorph features at the mature stages has long cardin<strong>al</strong> septa at the early<br />

stages and more or less visible <strong>al</strong>ar fossules. In the Ur<strong>al</strong>s P. kasimovi was found in the Podolskian and P.<br />

irregularis - in the Myachkovian. Pseudotimania is typic<strong>al</strong> for the Myachkovian in the Moscow Basin (P.<br />

mosquensis, P. kasimovi) and occurs at the base of the Kasimovian in Donskaya Luka (P. kasimovi).<br />

This study is supported by RFBR grant 09-05-00101-а.<br />

ALEKSEEV, A. & GOREVA, N. (Eds.) (2009): Type and Reference Carboniferous sections in the South part of the Moscow<br />

basin. - Field trip gui<strong>de</strong>book of the I.U.G.S. Subcommission on Carboniferous stratigraphy, Moscow, 1-148.<br />

BAMBER, E.W. & FEDOROWSKI, J. (1998): Biostratigraphy and systematics of Upper Carboniferous crerioid rugose cor<strong>al</strong>s,<br />

Ellesmere Island, Arctic Canada. - Geologic<strong>al</strong> Survey of Canada, Bull<strong>et</strong>in, 511: 127 p.<br />

FEDOROWSKI, J. (1975): On some Upper Carboniferous Coelenterata from Bjørnøya and Spitsbergen. - Acta Geologica<br />

Polonica, 25 (1): 27-78.<br />

FOMICHEV, V.D. (1953): Rugosa cor<strong>al</strong>s and the stratigraphy of the Middle-and Upper Carboniferous and Permian<br />

<strong>de</strong>posits of the Don<strong>et</strong>s basin. – In: GORSKY, I.I. (Ed.), Transaction of All-Union scientific Research geologic<strong>al</strong> Institute<br />

of the Ministry of Geology, State Publishing House of the Geologic<strong>al</strong> literature: 1-614 (in Russian).<br />

GOREVA, N., ALEKSEEV, A., ISAKOVA, T. & KOSSOVAYA, O. (2009): Biostratigraphic an<strong>al</strong>ysis of the Moscovian–Kasimovian<br />

transition at the neostratotype of Kasimovian Stage (Afanasievo section, Moscow Basin, Russia). - P<strong>al</strong>aeoworld, 18<br />

(2-3): 102-113.<br />

GRECK, N. (1936): The representatives of the Caninia genus from the limestones of the Verkhnie-Chussovskyie Gorodki,<br />

Colva-Vischera district and Yfa plateau. - Transaction of the oil - prospering geologic<strong>al</strong> institute, ser.B, 61: 1-22 (in<br />

Russian).<br />

KOSSOVAYA, O., L. (1989): New data on the morphogenesis and phylogeny of some Late Carboniferous and Early<br />

Permian rugose cor<strong>al</strong>s. - Memoir Association of Austr<strong>al</strong>asian P<strong>al</strong>aeontologists, 8: 109-113.<br />

KOSSOVAYA, O. L. (1997): Biostratigraphic<strong>al</strong> subdivisions of the zon<strong>al</strong> type on the rugose cor<strong>al</strong>s. In: carboniferous and<br />

Permian key sections of the Northern Timan. – KASHIK, D.S. (Ed.), Transaction of ISC, Sankt-P<strong>et</strong>ersburg, “Nauka”,<br />

24: 205-219 (in Russian).<br />

KOSSOVAYA, O. (1998): Evolution trend in Middle Casrboniferous P<strong>et</strong><strong>al</strong>axidae (Rugosa). - Geodiversitas, 20 (4): 663-685.<br />

KOSSOVAYA, O.L., GOREVA N.V., ISAKOVA T.A. & LEONTIEV D.I. (2011): The influence of the Middle-Late Pennsylvanian<br />

event on the rugose evolution in the shelf sea of the East-European Platform. - Exten<strong>de</strong>d abstracts of the LVII<br />

session of the P<strong>al</strong>eontologic<strong>al</strong> soci<strong>et</strong>y, Saint P<strong>et</strong>ersburg: 67-79. (in Russian).<br />

OGAR’, V.V. (2009): Bothrophyllum conicum (Fischer, 1837) (Rugosa) from the Middle and Upper Carboniferous of the<br />

Don<strong>et</strong>s Basin. – In: Fossil flora and fauna of Ukraine: P<strong>al</strong>eontologic<strong>al</strong> and stratigraphic<strong>al</strong> aspects. Proceedings of the<br />

Institute of Geologic<strong>al</strong> Sciense of the NAS of Ukraina. Kiev: 61-68 (in Ukrainian).<br />

SOMERVILLE, I.D. (1997): Biostratigraphy and biofacies of Upper Carboniferous - Lower Permian rugose assemblages<br />

from the Isfjore<strong>de</strong>n area, centr<strong>al</strong> Spitsbergen. - Bol<strong>et</strong>ín <strong>de</strong> la Re<strong>al</strong> Sociedad Espanola <strong>de</strong> Historia Natur<strong>al</strong> (Sección<br />

Geológica), 92 (1-4): 365-380.<br />

VASILJUK, N.P. & KOZYREVA, T.A. (1981): Attempt of correlation on cor<strong>al</strong>s of the upper pat of the middle Carboniferous<br />

of the Moscow syncline, Don<strong>et</strong>s basin and Northern Spain. - Bull<strong>et</strong>in of the Moscow soci<strong>et</strong>y of Natur<strong>al</strong>ists,<br />

geologic<strong>al</strong> series, 56 (5): 109-117 (in Russian).<br />

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