COURS STRATIGRAPHIE SEQUENTIELLE PDF

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In comparison to pre records of nonavian dinosaur remains from the Maastrichtian type strata, material collected during the past 20 years is both fairly common and diverse, consisting mostly of isolated cranial and post-cranial remains of hadrosaurids.

With the exception of the type specimen of Megalosaurus bredai Seeley, a fragmentary right femur, no theropod material is represented in collections screened by us. In the present contribution, specimens recognised in various collections subsequent to our last tabulation are illustrated and briefly discussed. Although we are fully aware that the material is too limited to draw meaningful conclusions from, the specimens are here tied-in with a preliminary sequence-stratigraphic interpretation of the type Maastrichtian, which is currently being refined by strontium-isotope studies of coleoid cephalopods.

To cite this article: J. Jagt, E. Mulder, A. Schulp, R. Dortangs, R. Fraaije, C. Palevol 2 Pour citer cet article : J. Journal page Archives Contents list. Article Article Outline. Access to the text HTML. Access to the PDF text. Recommend this article. Save as favorites. Access to the full text of this article requires a subscription. If you are a subscriber, please sign in 'My Account' at the top right of the screen. Dinosaurs from the Maastrichtian-type area southeastern Netherlands, northeastern Belgium.

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Stratigraphie séquentielle

Abdellah, H. Cretaceous Research, 16 5 : — Arthur, M. Palaeoceanographic controls on organic-matter production and preservation. Geological Society of London Special Publications, —

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In comparison to pre records of nonavian dinosaur remains from the Maastrichtian type strata, material collected during the past 20 years is both fairly common and diverse, consisting mostly of isolated cranial and post-cranial remains of hadrosaurids. With the exception of the type specimen of Megalosaurus bredai Seeley, a fragmentary right femur, no theropod material is represented in collections screened by us. In the present contribution, specimens recognised in various collections subsequent to our last tabulation are illustrated and briefly discussed. Although we are fully aware that the material is too limited to draw meaningful conclusions from, the specimens are here tied-in with a preliminary sequence-stratigraphic interpretation of the type Maastrichtian, which is currently being refined by strontium-isotope studies of coleoid cephalopods.

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