MORPHOLOGIC AND ISOTOPIC INVESTIGATION OF THE NEOGENE PLANKTONIC FORAMINIFERAL SUBGENUS GLOBOROTALIA (TRUNCOROTALIA)
This study tracks the persistence of those morphotypes temporally, concentrating on speciation events in the lineage. Some of these morphologic characters retain their correlation with coiling direction and are persistent through time and appear to be consistent with the “genetic species” found in studies of Gr. truncatulinoides. Coiling direction in Gr. truncatulinoides is known to correlate locally with the Pleistocene glacial/inter-glacial cycles. Ancestral species of the plexus also show changes in coiling direction related to oceanographic change. Additionally, the truncorotalid lineage shows a higher occurrence of kummerform specimens during times of environmental stress.
Stable light isotope analysis of individual chambers shows a difference in depth preference between the coiling types within species and between species of the lineage. This supports the idea that that the dextral and sinistral populations have different depth preferences and/or timing of the annual reproductive cycle, providing a mechanism for genetic isolation in the lineage and within each species. The significance of stable light isotopic variation among kummerform and normalform specimens will also be presented.