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- W2091645035 abstract "The availability of CaCO3 and ³He content results for core TT 13-72 from 4.3 km depth in the equatorial Pacific [Marcantonio et al., 1996] allows the magnitude of the excess (i.e., over ambient) CaCO3 dissolution at the onset of marine glacial stages 10, 8, and 6 to be estimated. These three events are remarkably similar; during each an integrated loss of about 28 g CaCO3 per cm² occurred. While the magnitude of this loss is consistent with that expected from the interglacial to glacial pH shifts reconstructed based on boron isotope measurements on benthic foraminifera [Sanyal et al., 1995], measurements at a number of other locations and water depths will be required before this approach can be used to evaluate the global toll of these dissolution events." @default.
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- W2091645035 date "1997-08-01" @default.
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- W2091645035 title "Magnitude of the CaCO3dissolution events marking the onset of times of glaciation" @default.
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- W2091645035 doi "https://doi.org/10.1029/97pa01020" @default.
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