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- W2048424103 abstract "Dissolution of calcareous tests in waters undersaturated with respect to calcium carbonate causes postmortem changes to assemblages of modern benthic foraminifera. Comparison of the percentage of agglutinated tests in the living and dead assemblages from the same sample enables the amount of dissolution to be quantified. Re-examination of data from the continental shelf off New York and the estuarine Chezzetcook Inlet, Canada, reveals major dissolution losses which lead to dead assemblages rich in agglutinated tests. It is probable that partial dissolution of the calcareous component of modern assemblages is more widespread than has been recognised." @default.
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- W2048424103 title "Syndepositional dissolution of calcareous foraminifera in modern shallow-water sediments" @default.
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