Aretz et al_2011.pdf - ORBi - Université de Liège
Aretz et al_2011.pdf - ORBi - Université de Liège
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 />
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mosquensis STUCKENBERG. Similar cha<strong>et</strong><strong>et</strong>id biostromes are <strong>de</strong>scribed in similar stratigraphic levels in the<br />
Moscow region and the USA (WEST & CLARK 1984).<br />
An Upper Carboniferous (Gzhelian) bioherme was earlier <strong>de</strong>scribed in the same section. It is <strong>al</strong>g<strong>al</strong><br />
buildup up to 5,2 m in size that is associated with limestone О6 1 .<br />
Thus, our data show that the formation of buildups occurred at various stages during the <strong>de</strong>velopment<br />
of the Don<strong>et</strong>s p<strong>al</strong>eobasins. However, the compositions of bioconstructors have changed over time. In<br />
gener<strong>al</strong>, the appearance of the Carboniferous buildups in the Don<strong>et</strong>s Basin corresponds to the periods of<br />
maximum diversity of various marine organisms.<br />
122<br />
Fig. 1: Distribution of the Carboniferous buildups in the<br />
Don<strong>et</strong>s Basin; 1: limestone; 2: marl; 3: <strong>al</strong>ternation of<br />
sandstones, siltstone, sh<strong>al</strong>e and co<strong>al</strong>s; 4: limestone with<br />
buildups.<br />
ARETZ, M. & WEBB, G.E. (2007): Western European and eastern Austr<strong>al</strong>ian Missisipian sh<strong>al</strong>low water reefs: a<br />
comparasion. – Proceedings of the XV th Internation<strong>al</strong> Congress on Carboniferous and Permian Stratigraphy: 433–<br />
442.<br />
KUZNEZOV, V.G. & ANTOSHKINA, A.I. (2006): Late Visean-Serpukhovian Stage in P<strong>al</strong>eozoic Reeff Formation. –<br />
Stratigraphy and Geologic<strong>al</strong> Correlation, 13 (4): 223.<br />
OGAR, V.V. (2007): Pro biohermnu prirody <strong>de</strong>jakych vapnjakiv moskovskogo jarusu Donezkogo basejnu [On bioherm<strong>al</strong><br />
genesis some moscovian limestones of the Don<strong>et</strong>s Basin]. - Ukrainian Geologist: 32-37 [in Ukrainian].<br />
POLJAKOVA, V.E. (1986): Beregovye rify verchneserpuchovskogo podjarusa Donezkogo basejna [The Upper<br />
Serpukhovian ringing reefs of the Don<strong>et</strong>s Basin]. – Fanerozojskie rify i kor<strong>al</strong>ly SSSR. Nauka: 174-179 [in Russian].<br />
SOMERVILLE, I. D COZAR, P. & RODRÍGUEZ, S. (2003): Late Viséan rugose cor<strong>al</strong> faunas from South-Eastern Ireland:<br />
composition, <strong>de</strong>position<strong>al</strong> s<strong>et</strong>ting and p<strong>al</strong>aeoecology of Siphono<strong>de</strong>ndron biostromes. – In: HUBMANN, B. & PILLER,<br />
W.E. (Eds.), Fossil Cor<strong>al</strong>s and Sponges, Proceedings of the 9th Internation<strong>al</strong> Symposium on Fossil Cnidaria and<br />
Porifera, Graz, 2003. Austrian Aca<strong>de</strong>my of Sciences, Schriftenreihe <strong>de</strong>r Erdwissenschaftlichen Kommissionen, 17:<br />
307–328.<br />
WEST, R.R. & CLARK, G.R. (1984): P<strong>al</strong>aeobiolodgy and biologic<strong>al</strong> affinities of P<strong>al</strong>aeozoic cha<strong>et</strong><strong>et</strong>ids. – P<strong>al</strong>aeontographica<br />
Americana, 54: 337-348.