Fig. 14From: New biostratigraphical data (calcareous nannofossils, ammonites) and Early to Late Barremian transition in the Urgonien Jaune facies and Marnes de la Russille complex of the Swiss Jura Mountainsa, b La Sarraz–Les Buis quarry Sect. (8/3/2020), channel infill of Marnes de la Russille (MRu) with LSBMRu0-9 samples positioned (red star and circles), the transitional change of colour between LSBMRu4 and LSBMRu5 indicates the Early/Late Barremian boundary. c, d Eclépens quarry Sect. (24/6/2018), transition of the highest Marnes de la Russille (MRu) between Urgonien Jaune (UJ) and Urgonien Blanc (UB) facies, with coloured marls partly rubefied (d, sample ECMRu10). e, f La Sarraz–Les Buis quarry Sect. (8/3/2020), paleokarst with Late Eocene infilling of red clays and marls (Siderolithic deposits) in the lower part of the massive UB limestones. Scale: hammer (red frame in c, e) = 31.5 cm longBack to article page