Late Triassic (Rhaetian) conodonts and ichthyoliths from Chile

Research output: Contribution to journalArticlepeer-review

1 Citation (Scopus)
236 Downloads (Pure)


The Late Triassic of the back arc Domeyko Basin, Chile is characterized by the onset of marine sedimentation that persisted throughout the rest of the Mesozoic. Carbonate bulk samples from the Punta del Viento Limestone Formation have yielded a numerically small, but apparently widespread, conodont fauna including Epigondolella mosheri, Epigondolella englandi and Neogondolella steinbergensis. These specimens indicate a Rhaetian (Epigondolella mosheri conodont Biozone roughly equivalent to the Paracochloceras amoenum ammonoid Biozone) age for this unit. Their recovery represents the first record of conodonts from Chile, and also indicates a considerable potential for use in correlating sequence stratigraphic events within the Mesozoic Marginal Sea in Colombia, Peru and Chile.
Original languageEnglish
Pages (from-to)129-135
Number of pages7
JournalGeological Magazine
Issue number2
Publication statusPublished - 1 Mar 2000


Dive into the research topics of 'Late Triassic (Rhaetian) conodonts and ichthyoliths from Chile'. Together they form a unique fingerprint.

Cite this