Content area
Abstract
Spero et al report experimental measurements on living symbiotic and non-symbiotic plankton foraminifera showing that the 13C/12C and 18O/16O ratios of the calcite shells decrease with increasing seawater.
You might have access to more details...
Try and log in through your library or institution to see if they have access.
Spero et al report experimental measurements on living symbiotic and non-symbiotic plankton foraminifera showing that the 13C/12C and 18O/16O ratios of the calcite shells decrease with increasing seawater.