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Record W2732821000

Integrated, high-resolution allostratigraphic, biostratigraphic and carbon-isotope correlation of Coniacian Strata (Upper Cretaceous), Western Alberta and Northern Montana

2017· book-chapter· en· W2732821000 on OpenAlex
A. Guy Plint, Elizabeth A. Hooper, Grifi, Ireneusz Walaszczyk, Neil H. Landman, Darren R. Gröcke, Ian Jarvis

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueDurham Research Online (Durham University) · 2017
Typebook-chapter
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsAmmoniteGeologyPaleontologyCretaceousForeland basinBorealFaunaStructural basinEcology
DOInot available

Abstract

fetched live from OpenAlex

Inoceramid bivalves are the dominant invertebrate fauna of the Coniacian and basal Santonian of
\nthe Western Canada Foreland Basin in western Alberta. In the upper lower Coniacian through to basal
\nSantonian, six successive faunas are recognized, which provide the basis for corresponding, formally
\ndefined inoceramid zones. From bottom upward these are the zones of: Cremnoceramus crassus crassus
\n/C. deformis deformis, Inoceramus gibbosus, Volviceramus koeneni, Volviceramus involutus, Sphenoceramus
\nsubcardissoides, and Sphenoceramus ex gr. pachti. Particular faunas represent assemblages known
\nwidely from the Euramerican biogeographic region, although they characterize mostly its northern,
\nboreal area. The inoceramid-based biostratigraphic scheme allows correlation with other parts of the
\nNorth American Western Interior and with parts of the Euramerican biogeographic region.
\nThe studied succession provides a good record of the Inoceramus gibbosus Zone, which characterizes
\nthe topmost lower Coniacian. This zone, first recognized from northern Germany, is usually
\nabsent, both in Europe and in North America, due to a stratigraphic gap resulting from a eustatic
\nlowstand. The base of the middle Coniacian is marked by the abrupt appearance of the taxonomically
\nvariable Volviceramus fauna (V. koeneni (Müller), V. exogyroides (Meek and Hayden)), with associated
\nInoceramus undabundus Meek and Hayden and Volviceramus cardinalensis, newly described
\nherein. Scaphites (Scaphites) ventricosus Meek and Hayden, the ammonite marker of the base of the
\nmiddle Coniacian first appears in the late early Coniacian. The base of the upper Coniacian marks
\nthe first appearance of the characteristic northern inoceramid species Sphenoceramus subcardissoides
\n(Schlüter), the appearance of which coincides with Scaphites (Scaphites) depressus Reeside, the
\nammonite marker of this boundary. Close to this boundary Volviceramus stotti also appears, which
\nis newly described from the Canadian sections. The base of the Santonian corresponds to the abrupt
\nappearance of Sphenoceramus ex gr. pachti (Arkhangelsky).
\nThe studied sections demonstrate that the appearance of new inoceramid faunas (lowest occurrence
\nof Cremnoceramus crassus crassus (Petrascheck), of various species of Volviceramus, Sphenoceramus
\nsubcardissoides (Schlüter) and of S. ex gr. pachti) takes place immediately above major
\nmarine flooding surfaces, suggesting a close correspondence between evolutionary and/or migration
\nevents and episodes of relative sea-level rise.

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.

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), Science and technology studies
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.673
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0020.000
Science and technology studies0.0010.003
Scholarly communication0.0000.001
Open science0.0010.000
Research integrity0.0010.002
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 head0.031
GPT teacher head0.244
Teacher spread0.213 · 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