Stable oxygen isotopic ratios in corals (d18Ocoral) are commonly utilized to reconstruct climate variability beyond the limit of instrumental observations. These measurements provide constraints on pa
Age given in calendar years. Coccosphere-unit: Conversion of coccoliths to hypothetical coccospheres by taking an average number of coccoliths per coccosphere.
DEPTH, sediment is given in mcd. At Site 184-1148, the Zone N12/N13 boundary is undecided, and the Zone N6/N7 boundary at 367 mcd is estimated to be ~18000 ka on the local FO of Globigerinatella insue
An almost complete Upper Cretaceous sedimentary sequence recently recovered on the Kerguelen Plateau (southern Indian Ocean) during ODP Leg 183 was analysed for planktonic foraminifera in order to ref
This dataset contains a compilation of planktic foraminiferal d18O from sediment cores spanning the last deglaciation in the Southern Ocean. The compilation includes 4610 data points from 64 individua
