(Table 3) Th230 excess content and calcite accumulation rates in the eastern equatorial Pacific
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Age dating of sediment intervals is based on oxygen isotope stratigraphy and identification of 4 intervals, or boundaries: postdeglacial, MIS 1/2, MIS 2.2, and MIS 2/3. Data are averaged for intervals defined by these boundaries for presentation in Figures 3 and 12.
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2025-11-21
