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Record W18865127

Early Cambrian tidal sedimentary environments, western Victoria Island, Arctic Canada

2014· article· en· W18865127 on OpenAlexaboutno aff
Andrew M. Durbano

Bibliographic record

VenuePediatria de las Americas · 2014
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsGeologySedimentary rockArcticOceanographyPhysical geographyPaleontologyEarth scienceGeography
DOInot available

Abstract

fetched live from OpenAlex

The currently unnamed early Cambrian (Series 2, Stage 4) sandstone unit is exposed in the Minto Inlier of western Victoria Island, Canadian Arctic Islands, and forms the base of the Phanerozoic succession. Coeval with other sandstones of this age in Laurentia, it was deposited in a shallow-marine embayment on the passive margin during the initial phase of the early Paleozoic transgression. Four facies associations are recognized: (1) outer embayment sand dune complex characterized by laterally continuous, planar cross-stratified, medium- to coarse-grained sandstone; (2) inner embayment sand flat consisting dominantly of fine- to medium-grained bioturbated sandstone and fine- to medium-grained sandstone interbedded with laminated mudstone; (3) coastal lagoon characterized by laterally continuous, medium-grained oolitic ironstone and fine- to medium-grained bioturbated sandstone; and (4) offshore muddy shelf consisting dominantly of laminated mudstone with discontinuous seams of medium- to coarse sand. Bioturbation in the form of a typical early Cambrian suite of shallow-subtidal ichnofossils predominated in the inner embayment and coastal lagoon settings, representing a low-diversity Cruziana ichnofacies. Oolitic ironstone horizons in the coastal lagoon setting mark periods of low sedimentation rates when iron became concentrated and calcite was the primary cementing agent. Dunes are, for the most part, non-bioturbated or contain just a few individual burrows belonging to Skolithos, representing the Skolithos ichnofacies. The dominantly tabular, sheet-like geometry of the sandstones characterizes a comparatively lower energy regime than what has been found in typical complex dune geometries in modern and ancient examples and is attributed to sediment deposition under essentially uniform current speeds at consistent water depth conditions on a low-gradient shelf. Paleocurrent measurements and thickness variation suggest that deposition was affected by undulating topography on the Proterozoic basement within facies association 1 and 2, as well as by syndepositional faulting in some areas. The coastline is envisaged as a complex of bays and lagoons. The embayment opened to the northwest where sandbars developed offshore; stratigraphic thinning towards both the south and northeast indicates the direction of the paleoshoreline. Approximately shoreline orthogonal paleocurrents are considered indicative of a tidal origin. The lack of hummocky cross-stratification suggests there was no influence of major storms in this region.

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 score0.026
Threshold uncertainty score0.189

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.006
Science and technology studies0.0070.001
Scholarly communication0.0020.001
Open science0.0010.002
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0030.000

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 head0.007
GPT teacher head0.178
Teacher spread0.172 · 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
Published2014
Admission routes1
Has abstractno

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