Nouvelle biostratigraphie ammonitique du Barrémien (pro parte) du Sud-Est de la France
Identifieur interne : 000F42 ( Main/Exploration ); précédent : 000F41; suivant : 000F43Nouvelle biostratigraphie ammonitique du Barrémien (pro parte) du Sud-Est de la France
Auteurs : Jean Vermeulen [France]Source :
- Comptes Rendus de l'Academie des Sciences Series IIA Earth and Planetary Science [ 1251-8050 ] ; 1998.
English descriptors
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Abstract
Abstract: Since the Digne conference (South-Eastern France) the ammonite zonation of the Barremian has been considerably modified to produce a more accurate stratigraphical framework than those previously used. In South-Eastern France, from the lowermost A. hugii zone to the G. sartousiana zone, the Barremian is now divided up into nine zones and one sub-zone. Bed by bed collecting, in many sections, both in platform or basin domains, allowed the location of 11 additional horizons characterised by a wide species distribution area spreading over South-Eastern France. These horizons are defined, either by the bed where the species used truly appears, or by the lower bed marking the start of the acmeic phase. This research, which is directed towards the preparation of global stratigraphic sections and points, led to the proposal of a whole succession with twenty-one ammonite horizons, from the A. hugii zone to the G. sartousiana zone (Vermeulen, 1995b).
Url:
DOI: 10.1016/S1251-8050(99)80116-5
Affiliations:
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Le document en format XML
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<front><div type="abstract" xml:lang="en">Abstract: Since the Digne conference (South-Eastern France) the ammonite zonation of the Barremian has been considerably modified to produce a more accurate stratigraphical framework than those previously used. In South-Eastern France, from the lowermost A. hugii zone to the G. sartousiana zone, the Barremian is now divided up into nine zones and one sub-zone. Bed by bed collecting, in many sections, both in platform or basin domains, allowed the location of 11 additional horizons characterised by a wide species distribution area spreading over South-Eastern France. These horizons are defined, either by the bed where the species used truly appears, or by the lower bed marking the start of the acmeic phase. This research, which is directed towards the preparation of global stratigraphic sections and points, led to the proposal of a whole succession with twenty-one ammonite horizons, from the A. hugii zone to the G. sartousiana zone (Vermeulen, 1995b).</div>
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