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Record W4414429402 · doi:10.1130/b38014.1

Fish tooth U-Pb dating reveals the late Miocene REY enrichment of the Clarion-Clipperton Fracture Zone

2025· article· en· W4414429402 on OpenAlexaff
Jieyun Chen, Yu Fu, Dengfeng Li, Pete Hollings, Jinzhou Peng, Xiaoming Sun

Bibliographic record

VenueGeological Society of America Bulletin · 2025
Typearticle
Languageen
FieldArts and Humanities
TopicForensic Anthropology and Bioarchaeology Studies
Canadian institutionsLakehead University
Fundersnot available
KeywordsSedimentary depositional environmentDeposition (geology)GeochronologyMineralFracture zoneFracture (geology)Sediment

Abstract

fetched live from OpenAlex

Abstract Deep-sea sediments enriched in rare earth elements and yttrium (REY) are promising mineral resources and are extensively developed in the Pacific Ocean. However, REY enrichment mechanisms of deep-sea sediments remain poorly constrained due to a lack of chronological constraints on associated geological events. We integrated bioapatite U-Pb geochronometry with geochemical data to elucidate the temporal evolution and genetic processes of REY-rich sediments located in the Clarion-Clipperton Fracture Zone (CCFZ) in the central North Pacific Ocean. Fish tooth specimens, separated from deep-sea sediments collected from core MG026, were subjected to in situ trace-element analysis and U-Pb dating on their enamel-protected dentin layers using laser ablation–inductively coupled plasma–mass spectrometry. The bioapatite samples exhibited higher enrichments in total REY (ΣREY) and uranium than bulk sediments, and a moderate positive correlation between ΣREY and uranium concentrations. These bioapatite samples yielded Tera-Wasserburg lower intercept ages ranging from 15.8 ± 1.2 Ma to 9.5 ± 1.4 Ma, robustly constraining the depositional age of the host sediments and revealing a pronounced REY enrichment episode from 12.0 Ma to 9.0 Ma. Our results demonstrate a mean sedimentation rate of ~0.48 m/m.y. for the REY-rich sediments in the CCFZ. Multivariate analysis of bulk geochemical data indicates that REY-enrichment in CCFZ sediments is controlled not only by slow deposition rate but also by REY-bearing mineral phases and depositional environment conditions (including redox conditions and biological productivity). The REY enrichment event (ca. 12.0–9.0 Ma) is characterized by a significant transition toward more oxygenated and higher productivity conditions, as documented by trace metal enrichment factors (EF) of MoEF, UEF, CuEF, and NiEF. This event coincided with the progressive closure of the Central American Seaway, which enhanced the advection of oxygen-enriched, nutrient-bearing bottom waters into the CCFZ, promoting extensive formation of Fe-Mn (oxyhydr)oxides and facilitating REY enrichment. Our study establishes a reliable geochronological framework for late Miocene REY enrichment and provides exploration strategies linking tectonic events to deep-sea REY mineralization in the CCFZ.

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)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.048
Threshold uncertainty score0.096

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.014
GPT teacher head0.238
Teacher spread0.223 · 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 designObservational
Domainnot available
GenreEmpirical

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

Citations1
Published2025
Admission routes1
Has abstractyes

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