The Dorotea Formation was first described by Katz in 1963. The formation comprises sandstones with frequent conglomerate lenses, concretionary levels and claystones. The Dorotea Formation includes calcareous sandstones with abundant marine invertebrate and fragmentary vertebrate fossils. Hervé et al. (2004) obtained a maximum radiometric age of 67.4 ± 1.5 Ma from detrital zircons contained in sandstones of the Dorotea Formation.[2] Near the top of the formation is an iridium anomaly, correlated with the Cretaceous–Paleogene boundary; this is the southernmost K–Pg boundary site known from South America.[3]
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^Püschel Hans P., Martinelli Agustin G., Soto-Acuña Sergio, Ortiz Héctor, Leppe Marcelo and Vargas Alexander O. 2025A subantarctic reigitheriid and the evolution of crushing teeth in these enigmatic Mesozoic mammalsProc. R. Soc. B.29220251056
http://doi.org/10.1098/rspb.2025.1056
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