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Record W4408295827 · doi:10.1144/jgs2024-123

Constraining the relative positions of island arc terranes in the Canadian Cordillera using conodont oxygen isotope thermometry

2025· article· en· W4408295827 on OpenAlexaffabout
Martyn L. Golding, James R. Wheeley, Yadong Sun, Michael J. Orchard, Ivan J. Sansom

Bibliographic record

VenueJournal of the Geological Society · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsGeological Survey of Canada
Fundersnot available
KeywordsConodontGeologyTerraneIsotopes of oxygenPaleontologyIsotopeArc (geometry)GeochemistryBiostratigraphyTectonicsGeometry

Abstract

fetched live from OpenAlex

The Canadian Cordillera is a composite of crustal terranes with various stratigraphic and tectonic histories. The relationships between these terranes, and their relative positions throughout the late Paleozoic and Mesozoic, remain contentious. In British Columbia and southern Yukon, the oceanic Cache Creek terrane is structurally juxtaposed between the Stikine and Quesnel island arc terranes; the exotic Wrangell island arc terrane lies further to the west. Multivariate statistical analyses of Late Triassic (late Carnian–early Norian) conodont faunas from the Stikine and Quesnel terranes and the North American margin have previously suggested that the terranes were likely situated to the south of their present location relative to the North American margin prior to accretion in the latest Triassic to Mid-Jurassic. An independent test of this hypothesis can be provided by oxygen isotope ( δ 18 O) analysis of conodont phosphate. Changes in δ 18 O seawater were likely minor in open, well-ventilated oceans, therefore analysis of δ 18 O preserved in Late Triassic (early Norian) conodonts of the Quesnel, Stikine and Wrangell terranes, as well as the northern part of the North American margin, may allow the relative seawater temperatures at the time of deposition of each of these tectonic entities to be determined for this time interval. Previous studies of the δ 18 O of conodonts have suggested that the seawater temperature of the Wrangell terrane was warmer than that of the North American margin during the early Norian. The present study expands on these preliminary results by extending the geographical range of the dataset. In addition to confirming higher seawater temperatures for the Wrangell terrane, the δ 18 O ratios of early Norian elements of the conodont genus Ancyrogondolella from both the Stikine and Quesnel terranes are notably lower than those of the same genus from the North American margin. If the salinity was consistent across the tectonic entities, then this may imply that the seawater temperatures of both the Stikine and Quesnel terranes were also warmer than that of the North American margin in the early Norian and suggests that these terranes, similar to the Wrangell terrane, were either located to the south of their present location in equatorial latitudes or oceanic currents were bringing warm water north at this time. A southern location for the terranes would be consistent with the results of the previous multivariate statistical analyses.

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)0.001
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 score0.011
Threshold uncertainty score0.073

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0030.003
Science and technology studies0.0020.000
Scholarly communication0.0010.000
Open science0.0010.001
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 head0.024
GPT teacher head0.228
Teacher spread0.204 · 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

Citations0
Published2025
Admission routes2
Has abstractyes

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