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dc.contributor.authorSyvitski, Jaia
dc.contributor.authorWaters, Colin N.
dc.contributor.authorDay, John
dc.contributor.authorMilliman, John D.
dc.contributor.authorSummerhayes, Colin P.
dc.contributor.authorSteffen, Will
dc.contributor.authorZalasiewicz, Jan
dc.contributor.authorCearreta Bilbao, Alejandro
dc.contributor.authorGaluszka, Agnieszka
dc.contributor.authorHajdas, Irka
dc.contributor.authorHead, Martin J.
dc.contributor.authorLeinfelder, Reinhold
dc.contributor.authorMcNeill, J. R.
dc.contributor.authorPoirier, Clement
dc.contributor.authorRose, Neil L.
dc.contributor.authorShotyk, William
dc.contributor.authorWagreich, Michael
dc.contributor.authorWilliams, Mark
dc.date.accessioned2021-06-18T08:03:10Z
dc.date.available2021-06-18T08:03:10Z
dc.date.issued2020-10-16
dc.identifier.citationCommunications Earth & Environment 1(1) : (2020) // Article ID 32es_ES
dc.identifier.issn2662-4435
dc.identifier.urihttp://hdl.handle.net/10810/51932
dc.description.abstractGrowth in fundamental drivers-energy use, economic productivity and population-can provide quantitative indications of the proposed boundary between the Holocene Epoch and the Anthropocene. Human energy expenditure in the Anthropocene, similar to 22 zetajoules (ZJ), exceeds that across the prior 11,700 years of the Holocene (similar to 14.6 ZJ), largely through combustion of fossil fuels. The global warming effect during the Anthropocene is more than an order of magnitude greater still. Global human population, their productivity and energy consumption, and most changes impacting the global environment, are highly correlated. This extraordinary outburst of consumption and productivity demonstrates how the Earth System has departed from its Holocene state since similar to 1950 CE, forcing abrupt physical, chemical and biological changes to the Earth's stratigraphic record that can be used to justify the proposal for naming a new epoch-the Anthropocene. Human energy consumption and productivity have steeply risen around 1950 CE, leading to a departure from the Earth's Holocene state into the Anthropocene, suggests a quantitative analysis of humanity's influence on the Earth system.es_ES
dc.language.isoenges_ES
dc.publisherSpringeres_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es/*
dc.subjectglobal phosphorus cyclees_ES
dc.subjectsea-leveles_ES
dc.subjectquaternary system/periodes_ES
dc.subjectpleistocene series/epoches_ES
dc.subjectanthropogenic emissionses_ES
dc.subjectsediment fluxes_ES
dc.subjectrecent trendses_ES
dc.subjectnitrogenes_ES
dc.subjectclimatees_ES
dc.subjecttransformationes_ES
dc.titleExtraordinary Human Energy Consumption and Resultant Geological Impacts Beginning Around 1950 CE Initiated the Proposed Anthropocene Epoches_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holderThis article is licensed under a Creative Commons Attribution 4.0 International License (CC BY)es_ES
dc.rights.holderAtribución 3.0 España*
dc.relation.publisherversionhttps://www.nature.com/articles/s43247-020-00029-yes_ES
dc.identifier.doi10.1038/s43247-020-00029-y
dc.departamentoesGeologíaes_ES
dc.departamentoeuGeologiaes_ES


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This article is licensed under a Creative Commons Attribution 4.0 International License (CC BY)
Except where otherwise noted, this item's license is described as This article is licensed under a Creative Commons Attribution 4.0 International License (CC BY)