The concept of the 'Anthropocene' has gained traction among geologists as a proposed new geological epoch defined by significant human impact on Earth's geology and ecosystems. Unlike previous epochs, which were shaped by natural forces such as volcanic activity or asteroid impacts, the Anthropocene is characterized by anthropogenic markers including radioactive isotopes from nuclear tests, plastic pollution, and elevated carbon dioxide levels. However, the formal recognition of this epoch remains contentious. Some scholars argue that human influence, while pervasive, does not yet represent a distinct stratigraphic boundary comparable to those of the Pleistocene-Holocene transition. Others contend that the scale and irreversibility of changes, such as biodiversity loss and climate alteration, justify a new epoch. This debate underscores a broader challenge in stratigraphy: balancing geological precision with the need to communicate planetary-scale changes.