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Scale and diversity of the physical technosphere: A geological perspective

dc.contributor.authorZalasiewicz, J
dc.contributor.authorWilliams, Mark
dc.contributor.authorWaters, Colin
dc.contributor.authorBarnosky, Anthony D.
dc.contributor.authorPalmesino, John
dc.contributor.authorRönnskog, Ann-Sofi
dc.contributor.authorEdgeworth, Matt
dc.contributor.authorNeal, Cath
dc.contributor.authorCearreta, Alejandro
dc.contributor.authorEllis, Erle C.
dc.contributor.authorGrinevald, Jacques
dc.contributor.authorHaff, Peter K
dc.contributor.authorIvar do Sul, Juliana
dc.contributor.authorJeandel, Catherine
dc.contributor.authorLeinfelder, Reinhold
dc.contributor.authorMcNeill, John R
dc.contributor.authorOdada, Eric O
dc.contributor.authorOreskes, Naomi
dc.contributor.authorPrice, Simon James
dc.contributor.authorRevkin, Andrew
dc.contributor.authorSteffen, Will
dc.contributor.authorSummerhayes, Colin
dc.contributor.authorVidas, Davor
dc.contributor.authorWing, Scott
dc.contributor.authorWolfe, Alexander P.
dc.date.accessioned2021-09-14T03:21:59Z
dc.date.issued2017
dc.date.updated2020-11-23T11:05:28Z
dc.description.abstractWe assess the scale and extent of the physical technosphere, defined here as the summed material output of the contemporary human enterprise. It includes active urban, agricultural and marine components, used to sustain energy and material flow for current human life, and a growing residue layer, currently only in small part recycled back into the active component. Preliminary estimates suggest a technosphere mass of approximately 30 trillion tonnes (Tt), which helps support a human biomass that, despite recent growth, is ~5 orders of magnitude smaller. The physical technosphere includes a large, rapidly growing diversity of complex objects that are potential trace fossils or ‘technofossils’. If assessed on palaeontological criteria, technofossil diversity already exceeds known estimates of biological diversity as measured by richness, far exceeds recognized fossil diversity, and may exceed total biological diversity through Earth’s history. The rapid transformation of much of Earth’s surface mass into the technosphere and its myriad components underscores the novelty of the current planetary transformation.en_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn2053-0196en_AU
dc.identifier.urihttp://hdl.handle.net/1885/247855
dc.language.isoen_AUen_AU
dc.publisherSage Journalsen_AU
dc.rights© The Author(s) 2016en_AU
dc.sourceThe Anthropocene Reviewen_AU
dc.subjectAnthropoceneen_AU
dc.subjectanthroposphereen_AU
dc.subjectartefactsen_AU
dc.subjectstratigraphyen_AU
dc.subjecttechnologyen_AU
dc.subjecttechnosphereen_AU
dc.titleScale and diversity of the physical technosphere: A geological perspectiveen_AU
dc.typeJournal articleen_AU
local.bibliographicCitation.issue1en_AU
local.bibliographicCitation.lastpage22en_AU
local.bibliographicCitation.startpage9en_AU
local.contributor.affiliationZalasiewicz, J, Leicester Universityen_AU
local.contributor.affiliationWilliams, Mark, Leicester Universityen_AU
local.contributor.affiliationWaters, Colin, British Geological Surveyen_AU
local.contributor.affiliationBarnosky, Anthony D., Stanford Universityen_AU
local.contributor.affiliationPalmesino, John, Architectural Association School of Architectureen_AU
local.contributor.affiliationRönnskog, Ann-Sofi, Oslo Centre for Urban and Landscape Studiesen_AU
local.contributor.affiliationEdgeworth, Matt, University of Leicesteren_AU
local.contributor.affiliationNeal, Cath, University of Yorken_AU
local.contributor.affiliationCearreta, Alejandro, Univeridad del Pais Vascoen_AU
local.contributor.affiliationEllis, Erle C., University of Marylanden_AU
local.contributor.affiliationGrinevald, Jacques, University of Genevaen_AU
local.contributor.affiliationHaff, Peter K, Duke Universityen_AU
local.contributor.affiliationIvar do Sul, Juliana, Federal University of Rio Grandeen_AU
local.contributor.affiliationJeandel, Catherine, Universite Paul Sabatieren_AU
local.contributor.affiliationLeinfelder, Reinhold, Freie Universitaten_AU
local.contributor.affiliationMcNeill, John R, Georgetown Universityen_AU
local.contributor.affiliationOdada, Eric O, University of Nairobien_AU
local.contributor.affiliationOreskes, Naomi, Harvard Universityen_AU
local.contributor.affiliationPrice, Simon James, University of Cambridgeen_AU
local.contributor.affiliationRevkin, Andrew, Pace Universityen_AU
local.contributor.affiliationSteffen, Will, College of Science, ANUen_AU
local.contributor.affiliationSummerhayes, Colin, Cambridge Universityen_AU
local.contributor.affiliationVidas, Davor, The Fridtjof Nansen Instituteen_AU
local.contributor.affiliationWing, Scott, Smithsonian Institutionen_AU
local.contributor.affiliationWolfe, Alexander P., University of Albertaen_AU
local.contributor.authoruidSteffen, Will, u4279891en_AU
local.description.embargo2099-12-31
local.description.notesImported from ARIESen_AU
local.identifier.absfor040311 - Stratigraphy (incl. Biostratigraphy and Sequence Stratigraphy)en_AU
local.identifier.absseo960300 - CLIMATE AND CLIMATE CHANGEen_AU
local.identifier.ariespublicationa383154xPUB5868en_AU
local.identifier.citationvolume4en_AU
local.identifier.doi10.1177/2053019616677743en_AU
local.identifier.scopusID2-s2.0-85018776185
local.publisher.urlhttp://www.uk.sagepub.com/home.naven_AU
local.type.statusPublished Versionen_AU

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