Fig. 2From: Bentho-planktonic evidence from the Austrian Alps for a decline in sea-surface carbonate production at the end of the TriassicNorth-South transect of the Late Norian to Rhaetian facies of the northern Calcareous Alps (modified after Kuerschner et al. 2007) and palaeogeographical setting of the Schlossgraben, Eiberg and Tiefengraben sections within the Eiberg BasinBack to article page