Calcification in Ancient and Modern Coccolithophores
Cubillos, J.C., Henderiks, J., Beaufort, L., Howard, W.R. and Hallegraeff, G.M. 2012. Reconstructing calcification in ancient coccolithophores: Individual coccolith weight and morphology of Coccolithus pelagicus (sensu lato). Marine Micropaleontology 92-93: 29-39.
Cubillos et al., therefore, set out to adapt "an existing method to estimate coccolith calcite weight using birefringence (Beaufort, 2005)," which they felt was needed "to suit the large coccoliths of Coccolithus pelagicus," focusing "only on the central area, which is the thickest and most robust part of the coccolith," and applying the result "to fossil and sediment trap material from the South Tasman Rise area of the Southern Ocean, based on three sediment samples each from the Last Glacial Maximum, the Holocene and the Transition between the two periods, as well as modern-day trap samples. So what did they find?
"Most strikingly," as the five researchers report, "it appears that modern Coccolithus populations in the Southern Ocean are, on average, more heavily calcified than their fossil counterparts," which most all would agree is a very positive and encouraging finding. Cubillos et al. also remark that their work reveals "substantial non-linearity and independency of variations (plasticity) in coccolith size, shape and volumetric weight between the investigated time intervals," which phenomena they say they hope to study "in more detail" in order to "unravel what environmental conditions are related to intra-specific phenotypic variability in ancient and modern coccolithophores."
Beaufort, L. 2005. Weight estimates of coccoliths using the optical properties (birefringence) of calcite. Micropaleontology 51: 289-297.
Siegenthaler, U., Monnin, E., Kawamura, K., Spahni, R., Schwander, J., Stauffer, B., Stocker, T.F., Barnola, J.M. and Fischer, H. 2005. Supporting evidence from the EPICA Dronning Maud Land ice core for atmospheric CO2 changes during the past millennium. Tellus Series B: Chemical and Physical Meteorology 57: 51-57.