The concept of the 'Anthropocene' has gained significant traction in geological and environmental circles, though its formal recognition as a new epoch remains a subject of debate. Proponents argue that human activities, particularly since the mid-20th century, have left unmistakable markers in the stratigraphic record, such as radioactive isotopes from nuclear tests, microplastics, and elevated carbon dioxide levels. These markers, they contend, justify a distinct geological boundary. Conversely, skeptics point out that the term lacks the temporal depth of formal geological epochs, which typically span millions of years. They also question whether human impacts are truly global and synchronous, noting that geological boundaries require a clear, worldwide signal. Despite these disagreements, the Anthropocene concept has proven valuable as a heuristic device, prompting interdisciplinary research into human-environment interactions and fostering a broader dialogue about sustainability and planetary stewardship.