Spherule deposits in Cretaceous-Tertiary boundary sediments in Belize and Guatemala

TitleSpherule deposits in Cretaceous-Tertiary boundary sediments in Belize and Guatemala
Publication TypeJournal Article
Year of Publication2003
AuthorsKeller, G, Stinnesbeck, W, Adatte, T, Holland, B, Stüben, D, Harting, M, Leon, Cd., Cruz, Jd.
JournalJournal of the Geological Society
Volume160
Issue5
Pagination783 - 795
Date PublishedJan-09-2003
ISSN0016-7649
Abstract

Large spheroid deposits at Albion Island and Armenia in northern and central Belize and the spherule deposits of southern Belize and eastern Guatemala have the same glass origin based on the presence of almost pure Cheto smectite derived from alteration of impact glass from the Chicxulub impact on Yucatan, Mexico. The same origin has also been determined for altered glass spherules in Mexico, Haiti and the Caribbean. However, the spherule layers have variable ages as a result of erosion and redeposition, with an early Danian (Parvularugoglobigerina eugubina) zone Pla(1) age in southern Belize, Guatemala, Haiti, southern Mexico and the Caribbean, and a pre-K–T (Plummerita hantkeninoides) zone CF1 age of 65.27 ± 0.03 Ma in NE Mexico. A pre-K–T age for the Chicxulub impact has now also been determined from the new Yaxcopoil 1 core drilled in the impact crater. These data show that Chicxulub was not the K–T impact that caused the end-Cretaceous mass extinction, but an earlier impact event. A multiple impact hypothesis, volcanism and climate change appears the likely scenario for the end-Cretaceous mass extinction.  PDF

URLhttp://jgs.lyellcollection.org/cgi/doi/10.1144/0016-764902-119http://jgs.geoscienceworld.org/cgi/doi/10.1144/0016-764902-119
DOI10.1144/0016-764902-119
Short TitleJournal of the Geological Society