In 2008, a distinguished group of scholars supported Crutzen’s theory by announcing that sufficient evidence of stratigraphically significant change had emerged for recognition of the Anthropocene as a new geological epoch, and the concept should be considered for formalization by international discussion. According to Christian and McNeill, what distinguishes the Anthropocene from the preceding epoch, the Holocene, is the fact that humans have begun—without understanding what they are doing—to transform the chemistry of the atmosphere; the range, variety and distribution of plant and animals species; the nature of the water cycle; and fundamental processes of erosion and sedimentation.
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