Figure F2. Stratigraphy of the Cretaceous section cored in Hole 1149B and correlation with the Capriolo section in the Southern Alps (Bralower, 1987; Channell and Erba, 1992). Calcareous nannofossil (CN Zones according to Bralower et al., 1995) and radiolarian bioevents (UAZ = Unitarian Association Zones; Baumgartner et al., 1995) are indicated and correlated with the chemostratigraphic data of delta13C (A. Bartolini, pers. comm., 2001). The pink pattern underlines the interval of relatively high abundance of the calcareous nannofossil species Diazomatolithus lehmanii. TD = total depth.

Figure F2. Stratigraphy of the Cretaceous section cored in Hole 1149B and correlation with the Capriolo section in the Southern Alps (Bralower, 1987; Channell and Erba, 1992). Calcareous nannofossil (CN Zones according to Bralower et al., 1995) and radiolarian bioevents (UAZ = Unitarian Association Zones; Baumgartner et al., 1995) are indicated and correlated with the chemostratigraphic data of

¹³C (A. Bartolini, pers. comm., 2001). The pink pattern underlines the interval of relatively high abundance of the calcareous nannofossil species Diazomatolithus lehmanii. TD = total depth.