The Early Cretaceous carbonate carbon isotope stratigraphy established
in pelagic limestones is marked by several pronounced excursions towa
rds positive delta(13)C values, We investigated a biostratigraphically
and palaeomagnetically calibrated Aptian section to see whether C iso
tope stratigraphy could be recognized in shallow-water carbonates. The
chosen carbonate platform sections are located in southern Italy and
have been dated by biostratigraphy. Bulk samples, chosen from the Barr
emian-Albian part of the sequence, were analysed for their O and C iso
tope compositions. The C isotope curve established shows two major pos
itive excursions which can be correlated with the synchronous and glob
ally recognized Aptian C isotope events, The data provide evidence tha
t C isotope stratigraphy can be used as a powerful correlation tool be
tween pelagic and shallow-water limestone sequences.