Evidence of large Anacardiaceae trees from the Oligocene-early Miocene Santiago Formation, Azuero, Panama

We have poor knowledge of the plants that inhabited Central America during the Cenozoic. One of the families with a rich fossil record worldwide, especially for the Oligocene and Miocene epochs is Anacardiaceae. Llanodelacruzoxylon sandovalii gen. et sp. nov. is the first formal record of a fossil w...

Descripción completa

Detalles Bibliográficos
Autores: Oris Rodríguez-Reyes, Emilio Estrada-Ruiz, Peter Gasson
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2020
País:México
Institución:Instituto Politécnico Nacional
Repositorio:Redalyc-IPN
OAI Identifier:oai:redalyc.org:94366150006
Acceso en línea:https://www.redalyc.org/articulo.oa?id=94366150006
https://www.redalyc.org/journal/943/94366150006/
https://www.redalyc.org/journal/943/94366150006/html/
https://www.redalyc.org/journal/943/94366150006/94366150006.epub
https://www.redalyc.org/journal/943/94366150006/movil
Access Level:acceso abierto
Palabra clave:Ciencias de la Tierra
Panama
Miocene
Oligocene
fossil wood
Anacarcadiaceae
Descripción
Sumario:We have poor knowledge of the plants that inhabited Central America during the Cenozoic. One of the families with a rich fossil record worldwide, especially for the Oligocene and Miocene epochs is Anacardiaceae. Llanodelacruzoxylon sandovalii gen. et sp. nov. is the first formal record of a fossil wood of Anacardiaceae found in Panama and Central America to date. We collected the fossil woods in the Oligocene-Miocene Santiago Formation, in the Azuero Peninsula, Panama. Among the samples collected we have described and identified this new fossil genus of Anacardiaceae, using wood anatomical characters and extensive comparisons with fossil and extant material. These two specimens share diagnostic features with several Anacardiaceae woods, such as: large vessels (>200 µm), simple vessel-ray pitting and rays mostly uniseriate with large crystals. The occurrence of these Anacardiaceae in Panama by the Oligocene to Miocene adds to the understanding of the historical biogeography of the family and supports Central America (including Mexico) being a divergence center of the Anacardiaceae.