hypocene

The Hypocene is a hypothetical geological epoch that follows the Anthropocene, a proposed epoch marked by significant human impact on Earth's geology and ecosystems. The concept of the Hypocene, while not formally recognized by geological societies, suggests a future period where the effects of human activities may continue to shape the planet's geological record. It is often envisioned as a time when the lasting consequences of the Anthropocene become evident in rock strata and landforms.

Discussions surrounding the Hypocene often touch upon long-term environmental changes such as altered climate patterns, the persistence of anthropogenic materials like plastics and concrete, and the potential for significant biodiversity shifts or extinctions. The term implies a continuation or evolution of the conditions established during the Anthropocene, with human influence being a dominant factor in geological processes.

The precise start date and characteristics of the Hypocene are subjects of speculation, as it lies in the future. However, the conceptualization of this epoch serves as a thought experiment to consider the deep-time implications of current human actions. It prompts reflection on the planet's enduring geological narrative and the potential legacy of the current era. The Hypocene remains a theoretical construct, awaiting potential future geological evidence to support its definition.