Jason W. Eleson, Timothy J. Bralower; Evidence of changes in surface water temperature and productivity at the Cenomanian/Turonian Boundary. Micropaleontology ; 51 (4): 319–332. doi: https://doi.org/10.2113/gsmicropal.51.4.319
Calcareous nannofossil assemblages were investigated across the Oceanic Anoxic Event (OAE) at the Cenomanian/Turonian Boundary (CTB) in a section from the Western Interior Basin and a borehole from the New Jersey coastal plain. The objective was to determine the surface-water response to environmental perturbations during the OAE. A decrease in surface water fertility at the two localities is suggested by an increase in relative abundances of taxa with oligotrophic affinities and a concomitant decrease in taxa with mesotrophic or eutrophic affinities. Oligotrophy and anoxia at both localities are likely responses to increased water-column stratification associated with the incursion of warmer waters from lower latitudes.