Fig. 5From: Bentho-planktonic evidence from the Austrian Alps for a decline in sea-surface carbonate production at the end of the TriassicEiberg section. a High-resolution Geochemistry. Carbonate, total organic carbon (TOC), organic carbon isotope (δ13Corg), and C and O isotopic composition of carbonate (δ13Ccarb, and δ18O). b Relative abundance (in %) of calcareous nannofossils. Calcareous nannofossil assemblages as in Fig. 4 Back to article page