Fig. 3From: Evolution of a Late Oxfordian: early Kimmeridgian carbonate platform, French Jura MountainsCorrelation of sections and depositional sequences. The numbered medium-scale sequences (SI–SVII) are interpreted to correspond to the 100-kyr eccentricity cycle. Sequence boundaries Ox6′ to Kim 3 according to Hardenbol et al. (1998). Geographical coordinates of sections are in Fig. 2 Back to article page