(Appendix A) Age model of ODP Hole 120-747A

• Main Authors: Verducci, Marina, Foresi, L M, Scott, George H, Sprovieri, Mario, Lirer, Fabrizio, Pelosi, Nicola
• Format: Dataset
• Language: English
• Published: PANGAEA 2009
• Subjects: 120-747A; Age model; DEPTH; sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg120; Ocean Drilling Program; ODP; Sample code/label; South Indian Ridge; South Indian Ocean; Southern Ocean
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.775985; https://doi.org/10.1594/PANGAEA.775985

Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Indian Ocean) contain abundant, well-preserved and diverse planktonic foraminiferal assemblages. A detailed study of the climatic and hydrographic changes that occurred in this region during the Middle Miocene Climatic Transition led to the identification of an intense cooling phase (the Middle Miocene Shift). Abundance fluctuations of planktonic foraminiferal species with different paleoclimatic affinities, and oxygen and carbon stable isotopes have been integrated in a multi-proxy approach. Reconstruction of changes in foraminiferal faunal composition and diversity through time were the basis for identification of three foraminiferal biofacies. The most prominent faunal change took place at 13.8 Ma, when a fauna with warm-water affinity (marked by high abundance of Globorotalia miozea group and Globoturborotalita woodi plexus) was replaced by an oligotypic, opportunistic fauna with typical polar characters and dominated by neogloboquadrinids. This faunal change is interpreted as the result of foraminiferal migration from adjacent bioprovinces, caused by modifications in climate and hydrography. A positive 2.0 per mil shift in d18O (interpreted as the Mi3 event) and a related positive 1.0 per mil shift in d13C (corresponding to the CM6 event) accompanied this faunal turnover. These are interpreted to reflect substantial reorganization of Southern Ocean waters, the northward migration of the Polar Front and a strong increase in primary productivity. The second faunal change took place at 12.9 Ma and was characterized by the gradual decrease in abundance of the neogloboquadrinids and the recovery of Globorotalia praescitula/scitula group and Globigerinita glutinata. A positive 1.5 per mil shift in d18O (interpreted as the Mi4 event) and a concurrent gradual negative shift in d13C accompanied this faunal change, witnessing further modifications of the climate/ocean system. Variations in sea surface temperature, ...