Celestite solubility appears to be an important control on interstitial water Sr concentrations in these sites, and it must be considered when constructing Sr mass balance models of calcite recrystallization. Calcite Sr/Ca ratios (range 1-2 mmol/mol) are similar from site to site when plotted vs. age, with a pattern comparable to that for well-preserved foraminifer tests over the past 40 Ma. Interstitial water Mg and Ca gradients appear to reflect basement character and the intensity of alteration. -from Authors
CITATION STYLE
Delaney, M. L., & Linn, L. J. (1993). Interstitial water and bulk calcite chemistry, Leg 130, and calcite recrystallization. Proc., Scientific Results, ODP, Leg 130, Ontong Java Plateau, 561–572. https://doi.org/10.2973/odp.proc.sr.130.038.1993
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