E. Fourcade et al., AGE OF THE GUATEMALA BRECCIAS AROUND THE CRETACEOUS-TERTIARY BOUNDARY- RELATIONSHIPS WITH THE ASTEROID IMPACT ON THE YUCATAN, Comptes rendus de l'Academie des sciences. Serie 2. Sciences de la terre et des planetes, 327(1), 1998, pp. 47-53
The upper part of the near K/T boundary limestone breccia deposits whi
ch crop out in Guatemala near 16 degrees N contains impact remains: al
tered glass spherules (tektites) and elevated concentrations of iridiu
m. This suggests that these deposits could result from the impact of t
he K/T boundary asteroid on the Yucatan. However, their matrix contain
s foraminifers of the Eugubina Zone and calcareous nannofossils of the
CP1a Zone, an association characterizing Early (but not the earliest)
Danian. This unusual assemblage of K/T and Danian components suggests
that the upper part of the breccia was reworked several thousands of
years after the K/T event. ((C) Academie des sciences / Elsevier, Pari
s.)