MétaCan
Menu
Back to cohort
Record W4413202287 · doi:10.1029/2024gc012151

Disentangling Impact Ejecta Dynamics Using Micro–X‐Ray Fluorescence (μ‐XRF): A Case Study From the Terrestrial Cretaceous‐Paleogene (K‐Pg) Boundary

2025· article· en· W4413202287 on OpenAlexaff
Pim Kaskes, Roald Tagle, Mariia Rey, Steven Goderis, Sophie Decrée, Jan Smit, Philippe Claeys

Bibliographic record

VenueGeochemistry Geophysics Geosystems · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of British Columbia
FundersFonds Wetenschappelijk OnderzoekBelgian Federal Science Policy Office
KeywordsEjectaGeologyPetrographyPaleogeneGeochemistryTrace elementChemostratigraphyPaleontologyMineralogyCretaceousIsotopes of carbonIsotope

Abstract

fetched live from OpenAlex

Abstract This study presents a non‐destructive geochemical and petrographic workflow to generate high‐resolution chemostratigraphic records across key stratigraphic intervals, exemplified by a terrestrial Cretaceous‐Paleogene (K‐Pg) boundary sequence preserved at Starkville South (Raton Basin, Colorado, USA). To fingerprint specific Chicxulub impact ejecta and to unravel their mode and timing of deposition, we combined high‐resolution (25 μm) micro‐X‐ray fluorescence (μ‐XRF) mapping and quantitative integrated‐area linescans with scanning electron microscopy. A complex microstratigraphy is observed at Starkville South in which additional sublayers are identified in contrast to the classic “dual‐layer” succession described in the literature for US Western Interior K‐Pg sites. First, a basal claystone occurs with abundant glassy impact spherules that were altered over time to kaolinite and jarosite due to acidic and reducing conditions in a local swamp. This first lithology is followed by a carbonaceous shale rich in ejected quartz grains. These two ejecta intervals are interpreted to have formed primarily by ballistic transport from the Chicxulub impact structure and were likely emplaced within ∼1 hr after impact at Starkville South. In the overlying lignite, pronounced enrichment in zirconium and chromium are detected, hinting at an ejecta sequence containing three distinct sublayers with a large part of the siderophile element anomaly being likely preserved at the base of this coaly interval, including the famous iridium anomaly. These enrichments are attributed to fine‐grained impact dust composed of pulverized granitoid basement (Zr) and an admixture of meteoritic material (Cr, Ni, and likely Ir), probably deposited <20 years after impact following slow atmospheric settling.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.880
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0010.000

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 head0.012
GPT teacher head0.240
Teacher spread0.228 · 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 teacher head, not a consensus.

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

Citations4
Published2025
Admission routes1
Has abstractyes

Explore more

Same venueGeochemistry Geophysics GeosystemsSame topicGeological and Geochemical AnalysisFrench-language works237,207