Stoermer's Anthropology: What Is The Anthropocene?

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The Anthropocene is a proposed epoch dating from the commencement of significant human impact on the Earth's geology and ecosystems, including, but not limited to, anthropogenic climate change., neither the International Commission on Stratigraphy nor the International Union of Geological Sciences has yet officially approved the term as a recognized subdivision of geological time,
Various different start dates for the Anthropocene have been proposed, ranging from the beginning of the Agricultural Revolution 12-15,000 years ago, to as recent as the Trinity test in 1945., the ratification process continues and thus a date remains to be decided definitively, but the latter date has been more favored than others.
The most recent period of the Anthropocene has been referred to by several authors as the Great Acceleration during which the socioeconomic and earth system trends are increasing dramatically, especially after the Second World War.
General
An early concept for the Anthropocene was the Noosphere by Vladimir Vernadsky, in 1938 he wrote of “scientific
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Ecologist Eugene F. Stoermer subsequently used "Anthropocene" with a different sense in the 1980s and the term was widely popularized in 2000 by atmospheric chemist Paul J. Crutzen, who regards the influence of human behavior on Earth's atmosphere in recent centuries as so significant as to constitute a new geological epoch.
In 2008, the Stratigraphy Commission of the Geological Society of London considered a proposal to make the Anthropocene a formal unit of geological epoch divisions. A majority of the commission decided the proposal had merit and should be examined further. Independent working groups of scientists from various geological societies have begun to determine whether the Anthropocene will be formally accepted into the Geological Time