(Table T1) Stable carbon and oxygen isotope ratios of benthic foraminifera in the Late Pliocene-Pleistocene section of ODP Site 181-1123 in the Southwest Pacific

• Main Author: Harris, Sara E
• Format: Dataset
• Language: English
• Published: PANGAEA 2002
• Subjects: 181-1123; Cibicides cicatricosus; δ13C; δ18O; Cibicides corpulentus; Cibicides kullenbergi; Cibicides pachyderma; Cibicides robertsonianus; Cibicides sp.; Cibicides wuellerstorfi; Comment; COMPCORE; Composite Core; Depth; composite; composite revised; sediment/rock; DSDP/ODP/IODP sample designation; Joides Resolution; Leg181; Mass spectrometer Finnigan MAT 252; Nuttallides umbonifera; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean; Uvigerina hispida; Southern Ocean; Pacific; North Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.700860; https://doi.org/10.1594/PANGAEA.700860

Stable isotope records were generated for a late Pliocene-early Pleistocene interval from Ocean Drilling Program (ODP) Site 1123 in the southwest Pacific (41°47 S, 171°30 W; 3290 m water depth). Based on these data, new revisions were made to the shipboard splice and composite section. The isotope records will be used to evaluate the influence of North Atlantic and Southern Ocean deepwater masses on water entering the Pacific in the Deep Western Boundary Current. Three holes were cored at Site 1123, yielding a complete composite section over approximately the last 4.7 m.y. A representative spliced record (“the splice”) was developed aboard ship based on magnetic susceptibility, gamma ray attenuation bulk density, and percent reflectance data from the three adjacent holes (Carter, McCave, Richter, Carter, et al., 1999, doi:10.2973/odp.proc.ir.181.2000). No gaps in the sedimentary record were detected for the multiple-cored section of Site 1123. In addition to the isotope data, postcruise revisions to the splice and composite section based on stable isotope data are described here.