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P a l é o n t o l o g i e f r a n ç a i s e . Terrains c r é t a c é s . Céphalopodes. texte 662 p. et atlas 148 p. ORBIGNY A. D' (1842-1851). , texte 642 p. et atlas 2 3 4 pl. Württ. f r a n ç a i s e . Terrains jurassiques. Paris, Masson. , I : Céphalopodes. Paris, Masson, ORBIGNY A. D' (1849-1852). — Cours é l é m e n t a i r e de P a l é o n t o l o g i e et de G é o l o g i e stratigraphiques. , tableaux. ORBIGNY A. — Prodrome de P a l é o n t o l o g i e stratigraphique universelle des animaux mollusques rayonnes.

Phys. , 1837 (1839), p. 4 9 . C. ( 1 9 0 9 ) . - Diastrophism as the ultimate basis of correlation. J. Geol. , 17, pp. 6 8 5 - 6 9 3 . DIENER C. — G r u n d z ü g e der Biostratigraphie. Leipzig, Vienne, F. , 4 0 fig. O. et RODGERS J. (1 9 5 7 ) . - Principles of Stratigraphy. New York, John Wiley and Sons, 356 p. FREBOLD H. — Die Palaeogeographische Analyse der epirogenen Bewegungen und ihre Bedeutung f ü r die Stratigraphie. Geol. , IV, pp. 2 2 3 - 2 4 0 . G. ( 1 9 0 4 ) . — On unconformities and Palaeontological Breaks in relation to geological time.

Ru/ GRENZEN DER BIOSTRATIGRAPHIE I M J U R A lösen sich jedoch die drei Arten G. crenosum, G. nimbatum eudoxus-Zone mit ihren H ä u f i g k e i t s m a x i m a mehrfach ab. und G. modestum während der acanthicum und Weder das H ä u f i g k e i t s m a x i m u m , noch das Vorkommen einer Art ü b e r h a u p t m ü s s e n also von Ort zu Ort zeitgleich sein. Es spricht sogar vieles d a f ü r , dass sie es nicht sein können. S e l b s t v e r s t ä n d l i c h sind die zeitlichel Unterschiede im Auftreten einer Art an zwei beliebigen Punkten nie g r ö s s e r als die Existenzdauer der Art.

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Colloque du Jurassique à Luxembourg 1967


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