Memory and the Anthropocene

The increase in carbon-dioxide emissions through the burning of fossil fuels and its effects of global warming has left a geological record, as shown by polar ice core samples that date from the mid-to-late-eighteenth century. This has prompted Paul J. Crutzen and Eugene F. Stoermer (in 2000 and 200...

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Bibliographic Details
Published in:Témoigner. Entre histoire et mémoire
Main Author: Crownshaw, Richard
Format: Article in Journal/Newspaper
Language:English
Published: Éditions du Centre d'études et de documentation Mémoire d'Auschwitz 2015
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Online Access:http://temoigner.revues.org/1492
Description
Summary:The increase in carbon-dioxide emissions through the burning of fossil fuels and its effects of global warming has left a geological record, as shown by polar ice core samples that date from the mid-to-late-eighteenth century. This has prompted Paul J. Crutzen and Eugene F. Stoermer (in 2000 and 2002) to identify the end of the previous geological epoch, the Holocene, the warmer period of 10-12 millennia that succeeded the ice age of the Pleistocene. Crutzen and Stoermer have identified the A.