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   <subfield code="u">Geologisch-Paläontologisches Institut und Museum, Forschungsstelle für Korallenpaläozoologie, Pferdegasse 3, D-4400, Münster</subfield>
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   <subfield code="a">Paleoecology of Upper Eifelian and Lower Givetian coral limestones in the northwestern Sauerland (Devonian; Rhenish Massif)</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Andreas May]</subfield>
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   <subfield code="a">Summary: The prevailing sandy/silty lower part of the Middle Devonian in the northwestern Sauerland includes two coral limestone horizons, which contain a rich fauna of corals, stromatoporoids, and calcareous algae. The Ihmert-Formation is subdvided into three parts. The older coral limestone horizon is the Grünewiese-Member of the Ihmert-Formation (uppermost Eifelian), the younger is in the Bredenbruch-Member of the Unterhonsel-Formation (lower Lower Givetian). Conclusions about the environmental constraints are drawn from the sedimentology and the fossil content of the coral limestones. Predominant biostromes are built between storm wave base and normal wave base. Only the few bioherms grew above the normal wave base. These coral limestones were deposited in a tropical or subtropical normal marine environment in the shallow euphotic zone. Among the reef-builders epoecism is very frequent, and until now this phenomenon has not been investigated in detail. Fragile rugose and tabulate corals lived as commensals with stromatoporoids. Some other aspects of paleoecology are concisely presented.</subfield>
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   <subfield code="a">Institut für Palaentologie, Universitat Erlangen, 1992</subfield>
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   <subfield code="a">Reefs</subfield>
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   <subfield code="a">Rhenish Massif (Sauerland, Germany)</subfield>
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   <subfield code="a">Devonian (Upper Eifelian, Lower Givetian)</subfield>
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