Williams, Mark; Zalasiewicz, Jan. 2009 Enter the Anthropocene : an epoch of time characterised by humans. Journal Open University Geological Society, 30 (2). 31-34.
Abstract
In the first years of the 21st century Earth was being influenced by forces greater than
our own and yet as vulnerable. With infinite complacency men and women went to and
fro over this globe about their affairs, serene in their assurance of their empire over
matter. And yet, across the vastness of time Earth viewed the actions of people with
increasing despair. And slowly, but surely, she drew her plans against us…..
We have borrowed these words, with some poetic licence, from H.G. Wells’ late
Victorian science fiction spectacular The War of Worlds. Wells’ carefully crafted opening
salvo to his novel contains words prescient in the early 21st century as we face the
prospect of rapid change to our climate, and warns us about complacency in the belief of
our dominion over nature. Already in the late 19th century many scientists were
commenting on the extent of human influence on planet Earth. The Italian geologist
Antonio Stoppani (1873) was perhaps the first to moot these ideas. Later, as the 19th
century drew to a close the Swede Arrhenius and the American Chamberlain worked out
the relationship between the amount of CO2 in the atmosphere and global warming.
Arrhenius suggested that future generations of humans would need to raise surface
temperatures to provide new areas of agricultural land and thus feed a growing
population. But he could not have conceived of the massive rate of human population
increase in the 20th century. In 2002 the Nobel Prize winning scientist Paul Crutzen
resurrected the concept of the Anthropocene to denote the ever increasing influence of
humans on Earth. The word has now entered the scientific literature as a vivid expression
of the degree of environmental change on planet Earth caused by humans (Zalasiewicz et
al. 2008 and references therein).
For the Anthropocene to become useful though, it needs some quantification.
How might an Anthropocene Epoch be unique relative to the Holocene or the Pleistocene epochs that preceded it? What criteria could we use to quantify when the Anthropocene
began, and how might future generations of geologists recognise its signal in the rock
record? More importantly though, does the term Anthropocene help us to understand the
influence of humans on our world and how that affects the environment of the near
future?
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