Late Maastrichtian paleobiogeography of M. murus indicates major sea-surface currents.
Global correlation of the calcareous nannofossil expression of Deccan warming.
Cyclostratigraphy shows Maastrichtian C29r encompasses 15 to 19 precession cycles.
Drop in nannofossil species richness during the Deccan warming.
Return to high species richness in the last 100/140 kyr before K-PgB.