Toward defining the Anthropocene onset using a rapid increase in anthropogenic fingerprints in global geological archives

One of the remaining issues regarding the Anthropocene is the lack of stratigraphic evidence indicating when the cumulative human pressure from the early Holocene began to fundamentally change the Earth system. Herein, we compile anthropogenic fingerprints from various high-precision-dated proxy rec...

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Published inProceedings of the National Academy of Sciences - PNAS Vol. 121; no. 41; p. e2313098121
Main Authors Kuwae, Michinobu, Yokoyama, Yusuke, Tims, Stephen, Froehlich, Michaela, Fifield, L. Keith, Aze, Takahiro, Tsugeki, Narumi, Doi, Hideyuki, Saito, Yoshiki
Format Journal Article
LanguageEnglish
Published United States National Academy of Sciences 08.10.2024
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Online AccessGet full text
ISSN0027-8424
1091-6490
1091-6490
DOI10.1073/pnas.2313098121

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Abstract One of the remaining issues regarding the Anthropocene is the lack of stratigraphic evidence indicating when the cumulative human pressure from the early Holocene began to fundamentally change the Earth system. Herein, we compile anthropogenic fingerprints from various high-precision-dated proxy records for 137 global sites to determine the age of the unprecedented surge in these records over the last 7700 y. The cumulative number of fingerprints revealed an unprecedented surge in diverse anthropogenic fingerprints starting in 1952 ± 3 CE, corresponding to the onset of the Great Acceleration. Notably, the period from 1953 to 1958 CE saw a nearly simultaneous surge in fingerprints across all regions, including Antarctica, the Arctic, East Asia, Europe, North America, and Oceania. This synchronous upsurge reflects the moment when human impacts led to rapid transformations in various natural processes and cycles, with humans becoming a geological force capable of inscribing abundant and diverse anthropogenic fingerprints in global strata. Following this global fingerprint explosion, profound planetary-scale changes, including deviations from the established natural climatic conditions, begin. This unprecedented surge in anthropogenic signals worldwide suggests that human influences started to match many natural forces controlling the processes and cycles and overwhelm some of the functioning of the Earth system around 1952.
AbstractList One of the remaining issues regarding the Anthropocene is the lack of stratigraphic evidence indicating when the cumulative human pressure from the early Holocene began to fundamentally change the Earth system. Herein, we compile anthropogenic fingerprints from various high-precision-dated proxy records for 137 global sites to determine the age of the unprecedented surge in these records over the last 7700 y. The cumulative number of fingerprints revealed an unprecedented surge in diverse anthropogenic fingerprints starting in 1952 ± 3 CE, corresponding to the onset of the Great Acceleration. Notably, the period from 1953 to 1958 CE saw a nearly simultaneous surge in fingerprints across all regions, including Antarctica, the Arctic, East Asia, Europe, North America, and Oceania. This synchronous upsurge reflects the moment when human impacts led to rapid transformations in various natural processes and cycles, with humans becoming a geological force capable of inscribing abundant and diverse anthropogenic fingerprints in global strata. Following this global fingerprint explosion, profound planetary-scale changes, including deviations from the established natural climatic conditions, begin. This unprecedented surge in anthropogenic signals worldwide suggests that human influences started to match many natural forces controlling the processes and cycles and overwhelm some of the functioning of the Earth system around 1952.
In the context of the Anthropocene, identifying the precise moment at which the consequences of fundamental human-induced changes in the Earth system first appear on the planet remains a long-standing challenge. This is due to the lack of a clear stratigraphic marker for the start date, as human impacts on Earth’s environments are significantly time-transgressive and spatiotemporally variable. Our study revealed that the number of anthropogenic fingerprints in global strata began to increase abruptly from 1952 ± 3 CE. This signal may reflect the onset of key human-induced changes in the Earth system, providing unambiguous stratigraphic evidence. This unprecedented synchronous increase has potential significance for defining the start of the Anthropocene in the future. One of the remaining issues regarding the Anthropocene is the lack of stratigraphic evidence indicating when the cumulative human pressure from the early Holocene began to fundamentally change the Earth system. Herein, we compile anthropogenic fingerprints from various high-precision-dated proxy records for 137 global sites to determine the age of the unprecedented surge in these records over the last 7700 y. The cumulative number of fingerprints revealed an unprecedented surge in diverse anthropogenic fingerprints starting in 1952 ± 3 CE, corresponding to the onset of the Great Acceleration. Notably, the period from 1953 to 1958 CE saw a nearly simultaneous surge in fingerprints across all regions, including Antarctica, the Arctic, East Asia, Europe, North America, and Oceania. This synchronous upsurge reflects the moment when human impacts led to rapid transformations in various natural processes and cycles, with humans becoming a geological force capable of inscribing abundant and diverse anthropogenic fingerprints in global strata. Following this global fingerprint explosion, profound planetary-scale changes, including deviations from the established natural climatic conditions, begin. This unprecedented surge in anthropogenic signals worldwide suggests that human influences started to match many natural forces controlling the processes and cycles and overwhelm some of the functioning of the Earth system around 1952.
One of the remaining issues regarding the Anthropocene is the lack of stratigraphic evidence indicating when the cumulative human pressure from the early Holocene began to fundamentally change the Earth system. Herein, we compile anthropogenic fingerprints from various high-precision-dated proxy records for 137 global sites to determine the age of the unprecedented surge in these records over the last 7700 y. The cumulative number of fingerprints revealed an unprecedented surge in diverse anthropogenic fingerprints starting in 1952 ± 3 CE, corresponding to the onset of the Great Acceleration. Notably, the period from 1953 to 1958 CE saw a nearly simultaneous surge in fingerprints across all regions, including Antarctica, the Arctic, East Asia, Europe, North America, and Oceania. This synchronous upsurge reflects the moment when human impacts led to rapid transformations in various natural processes and cycles, with humans becoming a geological force capable of inscribing abundant and diverse anthropogenic fingerprints in global strata. Following this global fingerprint explosion, profound planetary-scale changes, including deviations from the established natural climatic conditions, begin. This unprecedented surge in anthropogenic signals worldwide suggests that human influences started to match many natural forces controlling the processes and cycles and overwhelm some of the functioning of the Earth system around 1952.One of the remaining issues regarding the Anthropocene is the lack of stratigraphic evidence indicating when the cumulative human pressure from the early Holocene began to fundamentally change the Earth system. Herein, we compile anthropogenic fingerprints from various high-precision-dated proxy records for 137 global sites to determine the age of the unprecedented surge in these records over the last 7700 y. The cumulative number of fingerprints revealed an unprecedented surge in diverse anthropogenic fingerprints starting in 1952 ± 3 CE, corresponding to the onset of the Great Acceleration. Notably, the period from 1953 to 1958 CE saw a nearly simultaneous surge in fingerprints across all regions, including Antarctica, the Arctic, East Asia, Europe, North America, and Oceania. This synchronous upsurge reflects the moment when human impacts led to rapid transformations in various natural processes and cycles, with humans becoming a geological force capable of inscribing abundant and diverse anthropogenic fingerprints in global strata. Following this global fingerprint explosion, profound planetary-scale changes, including deviations from the established natural climatic conditions, begin. This unprecedented surge in anthropogenic signals worldwide suggests that human influences started to match many natural forces controlling the processes and cycles and overwhelm some of the functioning of the Earth system around 1952.
Author Doi, Hideyuki
Aze, Takahiro
Tsugeki, Narumi
Fifield, L. Keith
Saito, Yoshiki
Kuwae, Michinobu
Tims, Stephen
Yokoyama, Yusuke
Froehlich, Michaela
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Copyright Copyright National Academy of Sciences Oct 8, 2024
Copyright © 2024 the Author(s). Published by PNAS. 2024
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Issue 41
Keywords anthropogenic fingerprints
great acceleration
anthropocene
plutonium
technosphere
Language English
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Edited by Carl Folke, Kungliga Vetenskapsakademien, Stockholm, Sweden; received August 15, 2023; accepted August 2, 2024
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Snippet One of the remaining issues regarding the Anthropocene is the lack of stratigraphic evidence indicating when the cumulative human pressure from the early...
In the context of the Anthropocene, identifying the precise moment at which the consequences of fundamental human-induced changes in the Earth system first...
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StartPage e2313098121
SubjectTerms Anthropocene
Anthropogenic Effects
Anthropogenic factors
Archives
Archives & records
Climatic conditions
Earth
Earth, Planet
Fingerprints
Geology
Holocene
Human influences
Humans
Physical Sciences
Social Sciences
Stratigraphy
Title Toward defining the Anthropocene onset using a rapid increase in anthropogenic fingerprints in global geological archives
URI https://www.ncbi.nlm.nih.gov/pubmed/39312679
https://www.proquest.com/docview/3116711425
https://www.proquest.com/docview/3108763602
https://pubmed.ncbi.nlm.nih.gov/PMC11474069
Volume 121
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