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Fig. 5 | Swiss Journal of Geosciences

Fig. 5

From: Evidence for synsedimentary differential tectonic movements in a low-subsidence setting: Early Jurassic in northwestern Switzerland

Fig. 5

Early Jurassic biostratigraphy and lithostratigraphy of NW Switzerland and adjacent parts of SW Germany and E France as well as eustatic sea-level change during this period of time (compiled from Haq et al. 1988 and Reisdorf et al. 2011; modified). Note the stratigraphic range of the isopach maps. Due to the partly complex stratigraphic architecture of the Early Jurassic deposits in a few cases simplifications are required in the assignment of lithostratigraphic units: (i) despite of its wide chronostratigraphical range, the Weissenstein Member is included in only one isopach map; (ii) the thickness values for the Mt. Terri Member based on the biostratigraphic data available are incorporated into two isopach maps. B.Mb Belchen Member, E East of the Black Forest, FC France Comté, Fm. Formation, G. Gächlingen Bed, G.Bd. Gipf Bed?, Lum. Lumachelle, Mb. Member, Nor. Norian, Rhaet. Rhaetian, Schamb. Schambelen Member, Tabular J. Tabular Jura, URG Upper Rhine Graben, W West of the Black Forest, # = zones sensu Dean et al. (1961), sensu Bloos (1979) and sensu Schlegelmilch (1992); I = Psilonotenbank (e.g., Bloos et al. 2005; Etzold et al. 2010); II = Oolithenbank (e.g., Schloz 1972; Bloos et al. 2005; Schmid et al. 2008); III = Kupferfelsbank (e.g., LGRB 2004; Schmid et al. 2008); IV = Davoei-Bank (e.g., Schlatter 1991); V = Unterer Stein (e.g., Urlichs 1977; Röhl and Schmid-Röhl 2005)

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