The Cretaceous‐Tertiary extinction: Modeling carbon flux and ecological response

Abstract

It is widely recognized that a significant negative excursion in carbon isotopic (δ 13 C) differences between planktic and benthic foraminiferal tests occurred at the Cretaceous‐Tertiary (K‐T) boundary. We applied parametric and nonparametric breakpoint tests and statistical comparisons of different recovery models to assess the timing and pattern of recovery from this negative excursion at South Atlantic Deep Sea Drilling Project (DSDP) Site 528 and equatorial Pacific DSDP Site 577. Our results indicate a two‐stage recovery with an initial recovery to an intermediate state of planktic‐to‐benthic δ 13 C differences followed by a discontinuous shift to a final state with planktic‐to‐benthic δ 13 C differences similar to preextinction values. The final discontinuous shift in both the Pacific and Atlantic Ocean sites occurred several million years after the K‐T collapse of planktic‐to‐benthic δ 13 C differences. Both the first and second stages of recovery are best described by damped exponential relaxations. The pattern and timing of this carbon cycle recovery may have been contingent on the occurrence of key biological events.