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Record W4406140189 · doi:10.1177/03091333241310742

A conceptual and statistical framework for delineating the timing of a stratigraphic transition: Holocene-Anthropocene boundary as a case study

2025· article· en· W4406140189 on OpenAlexaboutno aff
Z. Bora Ön, Mustafa Ateş, Jérôme Kaiser

Bibliographic record

VenueProgress in Physical Geography Earth and Environment · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsAnthropoceneStratotypeGlobal Boundary Stratotype Section and PointGeologyPopulationOrbital forcingTephraHoloceneBoundary (topology)PaleontologyVolcanoGlacial periodBiostratigraphyDemographyStage (stratigraphy)

Abstract

fetched live from OpenAlex

The AWG (Anthropocene Working Group) proposed 1952 CE as the onset of the Anthropocene, marked by the detonation of the first hydrogen bomb, and designates Crawford Lake’s sediments in Canada as the potential stratotype. While the proposal for the Anthropocene as an epoch has been rejected by the SQS (Subcommision on Quaternary Stratigraphy), ongoing discussions regarding this debate remain unresolved. Here, we explore the possible biases and pitfalls of selecting the onset date from a singular site as the GSSP (Global boundary Stratotype Section and Point) for a chronostratigraphic boundary, using the potential Holocene-Anthropocene boundary as an example. We address the challenges of identifying changes in anthropogenic markers, along with the inherent measurement and age uncertainties, by employing a multilevel Bayesian change point analysis integrated with an errors-in-variables approach applied to proxy data. Our analysis utilizes plutonium isotopes ( (239+240) Pu), SCPs (spheroidal carbonaceous fly-ash particles), and radiocarbon (F 14 C) records from multiple locations established to evidence global anthropogenic imprints. Key findings include the identification of a population-level change point for (239+240) Pu at 1953 CE (1951.5–1954.5). While the standard practice for defining the onset date of a stratigraphic boundary typically involves selecting the date from the stratotype, our results suggest that 1953 CE should be the preferred date to define the onset of a potential Anthropocene Epoch. However, 1952 CE, which coincides with the first H-bomb test, cannot be statistically rejected as an alternative. Geographical clustering of SCPs data highlights regional variations in proxy signatures, while F 14 C results emphasize a lag of 5.5–9 years corresponding to carbon residence time. Our research contributes to discussions surrounding the delineation of a potential boundary between the Holocene and Anthropocene Epochs. Additionally, it provides methodological insights into identifying change points in multiple datasets and temporal lags in the environmental impacts of human activities.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.035
metaresearch head score (Gemma)0.078
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Theoretical or conceptual · Consensus signal: Theoretical or conceptual
GenreCandidate signal: Methods · Consensus signal: Methods
Teacher disagreement score0.035
Threshold uncertainty score0.187

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0350.078
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.002
Bibliometrics0.0080.008
Science and technology studies0.0020.010
Scholarly communication0.0070.006
Open science0.0040.003
Research integrity0.0020.003
Insufficient payload (model declined to judge)0.0030.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.019
GPT teacher head0.297
Teacher spread0.278 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designTheoretical or conceptual
Domainnot available
GenreMethods

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations7
Published2025
Admission routes1
Has abstractyes

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