Tuesday, August 30, 2016

a new epoch

Humanity’s impact on the Earth is now so profound that a new geological epoch – the Anthropocene – needs to be declared, according to an official expert group who presented the recommendation to the International Geological Congress in Cape Town on Monday.

The new epoch should begin about 1950, the experts said, and is likely to be defined by the radioactive elements dispersed across the planet by nuclear bomb tests, although an array of other signals, including plastic pollution, soot from power stations, concrete, and even the bones left by the global proliferation of the domestic chicken are now under consideration.

The current epoch, the Holocene, is the 12,000 years of stable climate since the last ice age during which all human civilisation developed. But the striking acceleration since the mid-20th century of carbon dioxide emissions and sea level rise, the global mass extinction of species, and the transformation of land by deforestation and development mark the end of that slice of geological time, the experts argue. The Earth is so profoundly changed that the Holocene must give way to the Anthropocene.

Evidence of the Anthropocene

Human activity has:

Pushed extinction rates of animals and plants far above the long-term average. The Earth is now on course to see 75% of species become extinct in the next few centuries if current trends continue.

Increased levels of climate-warming CO2 in the atmosphere at the fastest rate for 66m years, with fossil-fuel burning pushing levels from 280 parts per million before the industrial revolution to 400ppm and rising today.

Put so much plastic in our waterways and oceans that microplastic particles are now virtually ubiquitous, and plastics will likely leave identifiable fossil records for future generations to discover.

Doubled the nitrogen and phosphorous in our soils in the past century with our fertiliser use. This is likely to be the largest impact on the nitrogen cycle in 2.5bn years.

Left a permanent layer of airborne particulates in sediment and glacial ice such as black carbon from fossil fuel burning.

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