Palaeontological signatures of the Anthropocene are distinct from those of previous epochs

The “Great Acceleration” beginning in the mid-20th century provides the causal mechanism of the Anthropocene, which has been proposed as a new epoch of geological time beginning in 1952 CE. Here we identify key parameters and their diagnostic palaeontological signals of the Anthropocene, including t...

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Detalles Bibliográficos
Autores: Williams, Mark, Zalasiewicz, Jan, Barnosky, Anthony D., Leinfelder, Reinhold, Head, Martin J., Waters, Colin N., McCarthy, Francine M.G., Cearreta Bilbao, Alejandro, Aldridge, David C., McGann, Mary, Hamilton, Paul B., Summerhayes, Colin P., Syvitski, Jaia, Zinke, Jens, Cundy, Andrew B., Fiałkiewicz-Kozieł, Barbara, McNeill, John R., Kuwae, Michinobu, Rose, Neil L., Turner, Simon D., Saito, Yoshiki, Wagreich, Michael, Stegner, M. Allison, Yasuhara, Moriaki, Han, Yongming, Wrisdale, Amy, Holmes, Rachael, Berrio, Juan Carlos
Tipo de recurso: artículo
Fecha de publicación:2024
País:España
Institución:Universidad del País Vasco
Repositorio:Addi. Archivo Digital para la Docencia y la Investigación
OAI Identifier:oai:addi.ehu.eus:10810/72853
Acceso en línea:http://hdl.handle.net/10810/72853
Access Level:acceso abierto
Palabra clave:Anthropocene
Great Acceleration
stratigraphy
palaeontology
biosphere change
Descripción
Sumario:The “Great Acceleration” beginning in the mid-20th century provides the causal mechanism of the Anthropocene, which has been proposed as a new epoch of geological time beginning in 1952 CE. Here we identify key parameters and their diagnostic palaeontological signals of the Anthropocene, including the rapid breakdown of discrete biogeographical ranges for marine and terrestrial species, rapid changes to ecologies resulting from climate change and ecological degradation, the spread of exotic foodstuffs beyond their ecological range, and the accumulation of reconfigured forest materials such as medium density fibreboard (MDF) all being symptoms of the Great Acceleration. We show: 1) how Anthropocene successions in North America, South America, Africa, Oceania, Europe, and Asia can be correlated using palaeontological signatures of highly invasive species and changes to ecologies that demonstrate the growing interconnectivity of human systems; 2) how the unique depositional settings of landfills may concentrate the remains of organisms far beyond their geographical range of environmental tolerance; and 3) how a range of settings may preserve a long-lived, unique palaeontological record within post-mid-20th century deposits. Collectively these changes provide a global palaeontological signature that is distinct from all past records of deep-time biotic change, including those of the Holocene.

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