Fig. 27

Detailed section of the Early Jurassic strata at Courtemautruy (JU). α = no indications for disturbances caused by postjurassic tectonic processes or landslides could be detected in this sedimentary succession (section established by Reisdorf 2005); β = compare Buxtorf (1910); γ = loosely collected Angulaticeras angulatoides (Qu.); δ = ostracods (own data, det. E. Beher 2004): Bairdia fortis, Isobythocypris tatei, Ledahia sp., Ogmoconcha sp.; ε = loosely collected Arietites sp., Arietites s.l.; ζ = loosely collected Paracoroniceras s.l.; η ostracods (own data, det. E. Beher 2004): Bairdia molesta, Cardobairdia liasica, Ledahia sp., Pseudohealdia? sp.; λ = Beaniceras sp.; π = ostracods (own data, det. E. Beher 2004): Bairdia fortis; χ = Coroniceras sp.; ψ = ostracods (own data, det. E. Beher 2004): Bairdia molesta, Cardobairdia liasica, Isobythocypris tatei; ω = ostracods (own data, det. E. Beher 2004): Bairdia fortis, Bairdia molesta, Bairdia michelseni?, Bairdiacypris anisica brevis, Bythocypris postera, Cardobairdia sp. 3, Cardobairdia liasica, Isobythocypris tatei, Ledahia sp., Ogmoconcha sp., Ostracode E, Paracypris? redcarensis (Beher 2004)