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- W2891673493 abstract "Chronostratigraphically the middle Cretaceous is located at the transition from lower Cretaceous to upper Cretaceous. It concerns the Vraconian and the Cenomanian. However, the scarcity of macrofauna collected presents serious obstacles for the correct stamping of Foraminifera or Ostracoda scales, and for connecting these to the Ammonites zonation. Moreover, the distinctions of these zones which supplied the distribution chart for the inner part of middle Cretaceous are readily accessible, but difficult to chart. The marine transgression which ends the lower Cretaceous coincides in the aquitaine region with the beginning of a distension phase during the Vraconian. These phenomena show a recasting of sedimentary spaces, a redistribution of facies and a new adaptation of biological activity. This explains the diversity of areas of sedimentation which spread from tidal to basin environment. This is illustrated by tables and Vraconian and Cenomanian paleogeographic maps. recasting of sedimentary spaces, a redistribution of facies and a new adaptation of biological activity. This explains the diver¬ sity of areas of sedimentation which spread from tidal to basin environment. This is illustrated by tables and Vraconian and Cenomanian paleogeographic maps." @default.
- W2891673493 created "2018-09-27" @default.
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- W2891673493 date "1978-01-01" @default.
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- W2891673493 title "Histoire géologique du Crétacé moyen en Aquitaine (France S.W.)" @default.
- W2891673493 doi "https://doi.org/10.3406/geolm.1978.1028" @default.
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