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- The Core Concept: The Anthropocene, or "Age of Man," is a proposed geological epoch positing that human activity has superseded natural forces to become the primary driver of Earth's geological and ecological systems.
- Key Distinction/Mechanism: Unlike the Holocene—the stable epoch of the last 11,700 years that fostered human civilization—the Anthropocene represents a fundamental rupture in Earth's history where humanity operates as a geological force rather than merely a biological one. It is characterized by the human-driven alteration of the atmosphere, hydrosphere, cryosphere, and biosphere, shifting the planet into a volatile and unstable interval.
- Origin/History: The term was popularized by atmospheric chemist Paul Crutzen at the turn of the millennium (c. 2000) to describe the profound impact of humanity on the planet.
Major Frameworks/Components
- A Diachronous "Event": The scientific community increasingly views the Anthropocene not strictly as a defined epoch with a singular start date (a "golden spike"), but as an unfolding, diachronous geological event comparable to the Great Oxidation Event.
- Planetary Health Indicators: The framework highlights critical shifts such as the disruption of nitrogen and phosphorus cycles, rapid ocean acidification, and accelerating species extinction.
- Stratigraphic Alteration: The concept suggests that humanity has fundamentally altered the physical stratigraphic record of the Earth.
- Why It Matters: The Anthropocene redefines the current environmental crisis not as a series of isolated issues, but as a systemic transformation of the Earth caused by a single species. It serves as the dominant conceptual framework for understanding planetary instability and signals that the conditions necessary for known civilization are ending.





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