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In 2016, the Anthropocene Working Group confirmed that the Anthropocene is different from the Holocene, and it began in the year 1950 with the Great Acceleration. Stratospheric ozone depletion – The stratospheric ozone layer in the atmosphere filters out ultraviolet (UV) radiation from the sun.
Possible negative impacts may include changing regional weather patterns — creating or shifting areas of drought or regions that receive extreme precipitation — or altering tropospheric chemistry and ocean circulation patterns. Partially blocking the sun’s rays could interfere with normal plant processes and reduce agricultural yields.
These include climate change, biosphere integrity (functional and generic), land-system change, freshwater use, biogeochemical flows (nitrogen and phosphorus), oceanacidification, atmospheric aerosol pollution, stratospheric ozone depletion, and the release of novel chemicals. tar sand oil pipelines on October 11, 2016.
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