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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 />

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associated with F. limitata and F. micrastraea. To the north of the Vesdre Massif, in the Streupas outlier, this<br />

biostrom<strong>al</strong> level is 19 m thick and contains F. micrastraea and Phillipsastrea ananas in its upper part.<br />

Frechastraea n. sp. A is <strong>al</strong>so well known at the base of the Aisemont Formation, in the Namur<br />

Synclinorium, at Huccorgne on its north si<strong>de</strong> and in different loc<strong>al</strong>ities from its south si<strong>de</strong> such as Presles,<br />

Strud and Huy or even Lan<strong>de</strong>lies in the outlier of La Tombe. In La M<strong>al</strong>lieue quarry at Engis located at the<br />

eastern end from the south si<strong>de</strong> of the Namur Synclinorium and <strong>de</strong>scribed by COEN-AUBERT & LACROIX<br />

(1979) and POTY & CHEVALIER (2007), the first limestone level of the Aisemont Formation is again thicker<br />

and very rich in massive rugose cor<strong>al</strong>s. In the main part of this biostrome, there are numerous colonies of<br />

Frechastraea n. sp. A accompanied by a few specimens of F. limitata and even F. phillipsastraeiformis at the<br />

base. However, in the last 2.5 m of this reef<strong>al</strong> level, the fauna is different with the occurrence of F. cf. bore<strong>al</strong>is<br />

and F. micrastraea.<br />

In conclusion, it appears that Frechastraea n.sp. A is a remarkable marker for the base of the Late<br />

Frasnian in various areas of Belgium. This study confirms <strong>al</strong>so the well known diachronism of the bases of<br />

the Neuville and Aisemont Formations from the south to north, in the direction of the transgression. This<br />

diachronism emphasized recently by POTY & CHEVALIER (2007) is based on the distribution of the<br />

conodonts and the massive rugose cor<strong>al</strong>s. It culminates in the more northern sections such as Embourg,<br />

Streupas and Engis where the first limestone level of the Aisemont Formation is more <strong>de</strong>veloped and<br />

typic<strong>al</strong>ly cor<strong>al</strong>liferous. Therefore, the species F. micrastraea and Phillipsastrea ananas appear in the upper part<br />

of this biostrome, above Frechastraea n. sp. A, just as it is the case in the upper part from the much thicker<br />

lenses of red marble belonging to the P<strong>et</strong>it-Mont Member in the Philippeville Massif<br />

BOULVAIN, F., BULTYNCK, P., COEN, M., COEN-AUBERT, M., LACROIX, D., LALOUX, M., CASIER, J.G., DEJONGHE, L., DUMOULIN,<br />

V., GHYSEL, P., GODEFROID, J., HELSEN, S., MOURAVIEFF, N.A., SARTENAER, P., TOURNEUR, F. & VANGUSTAINE, M. (1999):<br />

Les formations du Frasnien <strong>de</strong> la Belgique. - Memoirs of the Geologic<strong>al</strong> Survey of Belgium, 44: 1-125.<br />

COEN, M., COEN-AUBERT, M. & CORNET, P. (1977): Distribution <strong>et</strong> extension stratigraphique <strong>de</strong>s récifs à "Phillipsastrea"<br />

dans le Frasnien <strong>de</strong> l'Ar<strong>de</strong>nne. - Ann<strong>al</strong>es <strong>de</strong> la Société Géologique du Nord, 96: 325-331.<br />

COEN-AUBERT, M. (1974a): Représentants <strong>de</strong>s genres Phillipsastrea D'ORBIGNY, A., 1849, Billingsastraea GRABAU, A.W.<br />

1917 <strong>et</strong> Iowaphyllum STUMM, E.C. 1949 du Frasnien du Massif <strong>de</strong> la Vesdre <strong>et</strong> <strong>de</strong> la bordure orient<strong>al</strong>e du Bassin <strong>de</strong><br />

Dinant. - Bull<strong>et</strong>in <strong>de</strong> l'Institut roy<strong>al</strong> <strong>de</strong>s Sciences naturelles <strong>de</strong> Belgique, Sciences <strong>de</strong> la Terre, 49/8: 1-38.<br />

COEN-AUBERT, M. (1974b): Le Giv<strong>et</strong>ien <strong>et</strong> le Frasnien du Massif <strong>de</strong> la Vesdre. Stratigraphie <strong>et</strong> p<strong>al</strong>éogéographie. -<br />

Mémoires in quarto <strong>de</strong> la Classe <strong>de</strong>s Sciences <strong>de</strong> l'Académie Roy<strong>al</strong>e <strong>de</strong> Belgique, 2e série, 18/2: 1-146.<br />

COEN-AUBERT, M. (1994): Stratigraphie <strong>et</strong> systématique <strong>de</strong>s Rugueux <strong>de</strong> la partie moyenne du Frasnien <strong>de</strong> Frasnes-lez-<br />

Couvin (Belgique). - Bull<strong>et</strong>in <strong>de</strong> l'Institut roy<strong>al</strong> <strong>de</strong>s Sciences naturelles <strong>de</strong> Belgique, Sciences <strong>de</strong> la Terre, 64: 21-56.<br />

COEN-AUBERT, M. (2000): Annotations to the Devonian Correlation Table, B142dm00-B142ds00: Stratigraphic distribution<br />

of the Middle Devonian and Frasnian rugose cor<strong>al</strong>s from Belgium. - Senckenbergiana l<strong>et</strong>haea, 80: 743-745.<br />

COEN-AUBERT, M. & COEN, M. (1975): Le Giv<strong>et</strong>ien <strong>et</strong> le Frasnien dans la v<strong>al</strong>lée <strong>de</strong> la Meuse <strong>de</strong> Tailfer à Yvoir (bord nord<br />

du Bassin <strong>de</strong> Dinant). - Ann<strong>al</strong>es <strong>de</strong> la Société Géologique <strong>de</strong> Belgique, 97: 499-524.<br />

COEN-AUBERT, M. & LACROIX, D. (1979): Le Frasnien dans la partie orient<strong>al</strong>e du bord sud du Synclinorium <strong>de</strong> Namur. -<br />

Ann<strong>al</strong>es <strong>de</strong> la Société Géologique <strong>de</strong> Belgique, 101: 269-279.<br />

POTY, E. & CHEVALIER, E. (2007): Late Frasnian phillipsastreid biostromes in Belgium. - Geologic<strong>al</strong> In ÁLVARO, J.J., ARETZ,<br />

M. BOULVAIN, F., MUNNECKE, A., VACHARD, D. & VENNIN, E. (Eds.), P<strong>al</strong>aeozoic Reefs and Bioaccumulations: Climatic<br />

and Evolutionary Controls. Geologic<strong>al</strong> Soci<strong>et</strong>y, London, Speci<strong>al</strong> Publications 275: 143-161.<br />

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