Abstract
The fossil content of a limestone succession of the Cuautla Formation, from the central part of the State of Morelos, indicates a late Cenomanian age. Amongst the fossils that were identified, those that do not show reworking include the calcareous algae Permocalculus irenae, P. budaensis, Heteroporella lepina, Dissocladella sp. cf. D. undulata… in order to continue, download the full paper in PDF.
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