Holocenin

Holocenin is a hypothetical geological epoch that, if recognized, would follow the Holocene epoch. The term itself is a neologism, combining "Holo-" from Holocene and "-cenin" suggesting a future period. Currently, the Holocene epoch is still ongoing and its end has not been formally defined by geological bodies such as the International Commission on Stratigraphy.

The concept of a post-Holocene epoch arises from discussions about significant human-induced changes to Earth's systems, often referred to as the Anthropocene. Some geologists and scientists propose that the current epoch is already defined by these anthropogenic impacts. However, the formalization of the Anthropocene as a new epoch faces considerable debate regarding its starting point and defining markers.

If the Anthropocene is eventually designated as a distinct epoch, it would represent the current period of significant human influence. Whether a subsequent, separate epoch like the "Holocenin" would be recognized depends on future geological and environmental developments, and the long-term stability or transformation of Earth's systems. The scientific community continues to analyze geological records and environmental data to understand the past, present, and potential future trajectory of Earth's history. The naming and definition of future geological time intervals are subject to rigorous scientific consensus and evidence-based argumentation.