The concept of the 'Anthropocene' has gained significant traction in geological and environmental circles, yet its formal recognition as a new geological epoch remains contentious. Proponents argue that human activities have left indelible marks on the planet, such as radioactive isotopes from nuclear tests and ubiquitous microplastics, which justify a distinct stratigraphic boundary. Conversely, skeptics contend that the term is more cultural than geological, noting that human impacts, while profound, have not yet produced a globally synchronous and clearly defined marker in the rock record. This debate underscores a fundamental tension: whether geology should reflect purely physical evidence or also accommodate the socio-political dimensions of planetary change.