This document summarizes a study that discovered fossil wood related to mangrove environments in southern South America during the Late Miocene. The fossil, named Mangroveoxylon areniensis, was found in Entre Ríos, Argentina. It shares anatomical characteristics most similar to the genus Conocarpus, particularly Conocarpus erectus, a species associated with mangroves. This suggests mangrove ecosystems existed further south than previously thought during this time period. Associated fossils of oysters that attach to mangrove tree roots also support the presence of mangroves. This discovery provides the first evidence of a coastal marine environment in this region during the Late Miocene, indicating tropical conditions extended further south than today.