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(Figure 2) Stable oxygen isotopes, Mg/Ca ratios, and intermediate-water temperatures of sediment core GeoB6007-2
depth, sediment/rock, age, hyalinea balthica, δ18o, magnesium/calcium ratio, temperature, water, gravity corer (kiel type), mass spectrometer finnigan mat 251, measured from h. balthica with icpms in solution (rosenthal et al. 1999)
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