Titlebook: Quantitative Geology of Late Jurassic Epicontinental Sediments in the Jura Mountains of Switzerland; Reinhart A. Gygi Book 2012 Springer B

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zwei Prinzi­ pien, die vom Herausgeber als wesentlich erachtet werden: 1. Die Qualität der praktischen Medizin ist abhängig vom Verständnis medi­ zinisch-wissenschaftlicher Grundlagen, denn Fortschritte in der klinischen Medi­ zin basieren fast immer auf wissenschaftlicher Grundlage. 2. Krankheiten oder Stör978-3-642-68415-9

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Quantitative Geology of Late Jurassic Epicontinental Sediments in the Jura Mountains of Switzerland

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Sedimentation,RG 340 in a quarry at La Rasse south of Porrentruy in Canton Jura (. 2000a, Pl. 17). Bed no. 23 of this section is a sediment of probably the . Chron from very shallow water in the lower Reuchenette Formation. Very fine-grained, light-green glauconite was found in a thin-section of limestone bed no.

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Hermatypic Coral Assemblages: Growth Form, Spatial Distribution, and Paleobathymetry, Growth of coral assemblages at the basinward margin of the carbonate platform of the St-Ursanne Formation was uninterrupted from base to top. The growth form of these coral assemblages was probably a biostrome at all stages of growth. The best place to see this is section RG 404 in the gorge of the