dc.contributor.author
Zalasiewicz, Jan
dc.contributor.author
Head, Martin J.
dc.contributor.author
Waters, Colin N.
dc.contributor.author
Summerhayes, Colin
dc.contributor.author
Turner, Simon
dc.contributor.author
Wagreich, Michael
dc.contributor.author
Aquilina, Luc
dc.contributor.author
Cearreta, Alejandro
dc.contributor.author
Chakraborty, Abhik
dc.contributor.author
Leinfelder, Reinhold
dc.date.accessioned
2025-10-27T09:53:37Z
dc.date.available
2025-10-27T09:53:37Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/50025
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-49750
dc.description.abstract
The Anthropocene was introduced to denote a dramatic, ongoing, planetary shift from prolonged relative Holocene stability, driving the Earth system into a new functional state outside its natural variability. Now stratigraphically-grounded, the Anthropocene is de facto a new epoch, not the subjective filtering of all anthropogenic impacts in Earth history.
en
dc.format.extent
5 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject
Anthropocene
en
dc.subject
Great Acceleration
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::550 Geowissenschaften
dc.title
Reply to Edgeworth et al. (2024): The Anthropocene Is a Time Interval, and More Besides
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.articlenumber
e2024EF005612
dcterms.bibliographicCitation.doi
10.1029/2024EF005612
dcterms.bibliographicCitation.journaltitle
Earth's Future
dcterms.bibliographicCitation.number
9
dcterms.bibliographicCitation.volume
13
dcterms.bibliographicCitation.url
https://doi.org/10.1029/2024EF005612
refubium.affiliation
Geowissenschaften
refubium.affiliation.other
Institut für Geologische Wissenschaften / Fachrichtung Paläontologie
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.eissn
2328-4277
refubium.resourceType.provider
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