(Table 3) Aragonite content, stable oxygen isotopes of Globigerinoides ruber, and age of ODP Site 166-1006 sediments

Sediment depth is given in mcd. For the creation of the age model, ODP Site 166-1006 oxygen isotope record was correlated to the Site 130-806 profile as provided by Berger et al. (1993, doi:10.2973/odp.proc.sr.130.023.1993) to facilitate low-latitude Atlantic-Pacific comparisons. The stable isotope record of ODP Site 130-806 was tuned by using the obliquity cycles apparent in the record (Berger et al., 1993, doi:10.2973/odp.proc.sr.130.023.1993).