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Record W4412949165 · doi:10.1002/dep2.70033

The Cenomanian–Turonian boundary interval in the Western Canada Foreland Basin: Stratigraphy, geochemistry, geochronology and sea‐level changes recorded in expanded and condensed clastic successions

2025· article· en· W4412949165 on OpenAlexafffundabout
A. Guy Plint, Darren R. Gröcke, David Selby, Ireneusz Walaszczyk, Sandra L. Kamo, Ian Jarvis, João Trabucho‐Alexandre, Jessica A. Flynn, Fred J. Longstaffe, Kienan P. Marion, B. L. Varban, Alice D.C. Du Vivier, David Uličný

Bibliographic record

VenueThe Depositional Record · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsImperial Oil (Canada)University of TorontoWestern University
FundersNatural Environment Research CouncilNatural Sciences and Engineering Research Council of Canada
KeywordsGeochronologyCenomanianGeologyClastic rockForeland basinStratigraphyPaleontologyStructural basinGeochemistryTectonics

Abstract

fetched live from OpenAlex

Abstract A 300 m thick section at Nini Hill in the proximal foredeep of the Western Canada Foreland Basin is dominated by shallow‐marine mudstone that spans the Cenomanian–Turonian boundary (CTB). The section preserves a 185 m thick record of OAE2, characterised by an ornate positive excursion in the organic carbon‐isotope profile. Osmium‐isotopes show the characteristic shift to unradiogenic ratios 21 m below the onset of OAE2. Carbon‐isotope events (CIE) at Nini Hill are correlated with both the Chalk reference section at Eastbourne, UK and the well‐dated SH#1 core in Utah, the latter permitting correlation to other sections in the southern USA. However, only the ~450 m thick, deep‐water CTB section in the Saku Formation, Japan, appears to match the CIE detail at Nini Hill. High‐resolution correlation utilising CIEs allows, for the first time, sea‐level changes, mapped in the poorly fossiliferous strata of Western Canada, to be correlated with coeval events in the USA and Europe. The globally‐recognised sub‐plenus unconformity that underlies OAE2 in many passive‐margin sections spanning the North Atlantic region is correlative with up to six high‐frequency sequences preserved in the highly expanded foredeep. Various studies have inferred sea‐level change of 10–40 m for this event, suggesting that thermo‐ and aquifer‐eustasy may have been supplemented by glacio‐eustasy. Other sea‐level changes of ~10–30 m recognised in Canada correlate with coeval events in the USA and Europe. Lower‐amplitude sea‐level cycles of ~5–10 m, form a persistent signal throughout the Canadian CTB interval. Strata thin dramatically from foredeep to forebulge due to condensation and lap out, hiatuses being represented by cryptic mud‐on‐mud disconformities. Without knowledge of physical stratigraphy, interpretation of carbon‐ and osmium‐isotope profiles in attenuated successions is prone to misinterpretation. Osmium data show that the influence of a large igneous province diminished markedly northward within the Western Interior Seaway.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.752
Threshold uncertainty score0.761

Codex and Gemma teacher scores by category

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

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 head0.013
GPT teacher head0.227
Teacher spread0.214 · 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.

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

Citations3
Published2025
Admission routes3
Has abstractyes

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