Fig. 1From: Evolution of a Late Oxfordian: early Kimmeridgian carbonate platform, French Jura Mountains a Geographical and b paleogeographical context at the Bimammatum/Planula boundary (Late Oxfordian), compiled after Cecca et al. (2005), Hug (2003), Jank et al. (2006a), and Cariou et al. (2014)Back to article page