Foraminiferal response to mid-Cenomanian (Upper Cretaceous) palaeoceanographic events in the Anglo-Paris Basin (Northwest Europe)

1998 ◽  
Vol 137 (1-2) ◽  
pp. 103-125 ◽  
Author(s):  
S.F. Mitchell ◽  
I.T. Carr
Keyword(s):  
Upper Cretaceous ◽  
Paris Basin ◽  
Northwest Europe

scholarly journals Reconstruction of the Upper Cretaceous chalks removed by dissolution during the Cenozoic in the western Paris Basin

1999 ◽  
Vol 88 (3) ◽  
pp. 467-474 ◽  
Author(s):  
B. Laignel ◽  
F. Quesnel ◽  
R. Meyer ◽  
C. Bourdillon
Keyword(s):  
Upper Cretaceous ◽  
Paris Basin

Le groupe des ganopristines

1940 ◽  
Vol S5-X (3-6) ◽  
pp. 127-147 ◽  
Author(s):  
Camille Arambourg
Keyword(s):  
North America ◽  
North Africa ◽  
Upper Cretaceous ◽  
Paris Basin

Abstract Characterizes and classifies the Ganopristinae (including Ctenopristis nougareti n.g. n.sp.), a group of selachian fishes from the upper Cretaceous of Syria, north Africa, the Paris basin, and North America. Possibly some forms occur in the Eocene.

Sur la signification de la craie a tubulures de Meudon [with discussion]

1945 ◽  
Vol S5-XV (7-8) ◽  
pp. 497-507
Author(s):  
Francois Ellenberger
Keyword(s):  
Upper Cretaceous ◽  
Tubular Structures ◽  
Paris Basin

Abstract Concludes that the indurated chalk bed containing numerous tubular structures which underlies the pisolitic limestone in the Meudon area, Paris basin, France, is a hard ground of submarine origin which was formed during a break in sedimentation, rather than in a period of emergence, probably in the upper Cretaceous.

scholarly journals Dinocyst distributions and stratigraphy of two Cenomanian–Turonian boundary (Upper Cretaceous) sections from the western Anglo-Paris Basin

1995 ◽  
Vol 14 (2) ◽  
pp. 97-105 ◽  
Author(s):  
Bruce A. Tocher ◽  
Ian Jarvis
Keyword(s):  
Upper Cretaceous ◽  
Paris Basin ◽  
Dinoflagellate Cyst ◽  
Northern France ◽  
Abundance And Diversity

Abstract. The dinoflagellate cyst distributions and stratigraphies of two representative Cenomanian/Turonian (C/T) boundary sections from the Maine and Normandy regions of northern France are described. Siliciclastic-rich sediments which characterize the Upper Cenomanian in Maine, contrast with the coeval nodular chalk and hardground lithofacies of Normandy. Both areas display a transition to marly chalks in the Lower Turonian. Dinocyst assemblages are characterized by low diversities (38 taxa) and low overall abundances, and relatively few stratigraphically significant species. The continued occurrence of Epelidosphaeridia spinosa (Cookson & Hughes) Davey in the Upper Cenomanian of Maine is noted. Results are compared and contrasted with those from coeval sections elsewhere in the Anglo-Paris Basin. A major decline in cyst abundance and diversity is typical of the C/T boundary interval, which is characterized by a dominance of tolerant cosmopolitan forms such as Circulodinium distinctum (Deflandre & Cookson) Jansonius, Hystrichosphaeridium bowerbankii Davey & Williams, Oligosphaeridium complex (White) Davey & Williams, Odontochitina costata Alberti; emend. Clarke & Verdier and O. operculata (O. Wetzel) Deflandre & Cookson.

Stratigraphy and stage boundaries in reference sections of the Upper Cretaceous Chalk in the east of the Paris Basin: the “Craie 700” Provins boreholes

2005 ◽  
Vol 26 (2) ◽  
pp. 157-169 ◽  
Author(s):  
Francis Robaszynski ◽  
Bernard Pomerol ◽  
Edwige Masure ◽  
Jean-Pierre Bellier ◽  
Jean-François Deconinck
Keyword(s):  
Upper Cretaceous ◽  
Paris Basin ◽  
Reference Sections ◽  
Stage Boundaries
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