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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Éditions du Centre d'études et de documentation Mémoire d'Auschwitz
2015
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Online Access: | https://doi.org/10.4000/temoigner.1492 http://journals.openedition.org/temoigner/1492 |
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fttriple:oai:gotriple.eu:dps2E6gTVJ7jrQP0DTwT5 2023-05-15T16:38:55+02:00 Memory and the Anthropocene Crownshaw, Richard 2015-01-01 https://doi.org/10.4000/temoigner.1492 http://journals.openedition.org/temoigner/1492 en eng Éditions du Centre d'études et de documentation Mémoire d'Auschwitz Éditions Kimé Témoigner. Entre histoire et mémoire Éditions du Centre d'études et de documentation de l'ASBL Mémoire d'Auschwitz urn:doi:10.4000/temoigner.1492 doi:10.4000/temoigner.1492 http://journals.openedition.org/temoigner/1492 other undefined Témoigner. Entre histoire et mémoire envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.4000/temoigner.1492 2023-01-22T18:07:46Z 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. Article in Journal/Newspaper ice core Unknown Témoigner. Entre histoire et mémoire 119 175 |
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envir geo Crownshaw, Richard Memory and the Anthropocene |
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description |
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. |
format |
Article in Journal/Newspaper |
author |
Crownshaw, Richard |
author_facet |
Crownshaw, Richard |
author_sort |
Crownshaw, Richard |
title |
Memory and the Anthropocene |
title_short |
Memory and the Anthropocene |
title_full |
Memory and the Anthropocene |
title_fullStr |
Memory and the Anthropocene |
title_full_unstemmed |
Memory and the Anthropocene |
title_sort |
memory and the anthropocene |
publisher |
Éditions du Centre d'études et de documentation Mémoire d'Auschwitz |
publishDate |
2015 |
url |
https://doi.org/10.4000/temoigner.1492 http://journals.openedition.org/temoigner/1492 |
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ice core |
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ice core |
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Témoigner. Entre histoire et mémoire |
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urn:doi:10.4000/temoigner.1492 doi:10.4000/temoigner.1492 http://journals.openedition.org/temoigner/1492 |
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https://doi.org/10.4000/temoigner.1492 |
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Témoigner. Entre histoire et mémoire |
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119 |
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175 |
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