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Record W4413819008 · doi:10.2110/jsr.2025.002

Early Cretaceous continental-scale sediment dispersal: towards resolving the McMurray Conundrum

2025· article· en· W4413819008 on OpenAlexaffabout
Abdullah M. Wahabi, B. L. Varban

Bibliographic record

VenueJournal of Sedimentary Research · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsImperial Oil (Canada)
Fundersnot available
KeywordsGeologyCretaceousBiological dispersalSedimentPaleontologyScale (ratio)OceanographyEarth scienceGeographyCartography

Abstract

fetched live from OpenAlex

ABSTRACT Alternative interpretations of Early Cretaceous McMurray Formation environments of deposition in the Western Canada Sedimentary Basin of Alberta have been referred to as the McMurray Conundrum because they have been debated for more than a decade. Recent empirically grounded research has continued to support long-held views that favor both fluvial and estuarine depositional models, but have provided no further resolution of the controversy. Here, we use multiple quantitative macro-, meso- and micro-scale approaches to further advance discussion of the McMurray Conundrum. First, we present published results of a recent paleogeographical reconstruction of the McMurray river system paleodrainage basin area, which places McMurray deposition within the context of a continental-scale system. We then use a high-density McMurray subsurface dataset, including published 3-D seismic observations, to test for downstream morphological and sedimentary transformations that indicate a paleogeographic position in the normal flow reach, perhaps extending into the backwater reach, which indicate that McMurray environments of deposition were terrestrial, and formed far upstream from marine influence. Last, we deploy oxygen and carbon isotope analyses of unaltered mollusk shells in the McMurray, which indicate freshwater conditions during and shortly after deposition, and provide no evidence of brackish-water marine conditions. Our results from three types of data therefore converge on the following characteristics for the McMurray system: a) the McMurray, in the Alberta foreland, represents the axial river of a south-to-north-flowing continental-scale fluvial system that drained much of North America, serving as the Amazon River or the Mississippi River of its time, b) data collected in the Alberta foreland basin over a downstream distance of > 400 km, from the Cold Lake to Athabasca Oil Sands areas, shows no evidence of downstream morphological and sedimentary transformations that are characteristic of rivers in their backwater reach, indicating that the axial McMurray river system was characterized by normal flow, and was likely > 1000 km upstream (to the south) from a coeval shoreline, and c) the recently published carbon and oxygen isotope analyses from unrecrystalized mollusk shells (Hasiuk et al. 2024) show that McMurray deposition took place in a fully freshwater continental environment, significantly upstream from the influences of saltwater penetration or tidal processes that would indicate marine proximity and influence.

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)0.004
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 score0.154
Threshold uncertainty score0.662

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0040.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.001
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 head0.031
GPT teacher head0.314
Teacher spread0.282 · 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

Citations1
Published2025
Admission routes2
Has abstractyes

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