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Record W2059652977 · doi:10.4138/1048

The Cretaceous age of the Vinegar Hill silica sand deposit, southern New Brunswick: evidence from palynology and paleobotany

2003· article· en· W2059652977 on OpenAlexafffundvenueabout
Howard J. Falcon‐Lang, Robert A. Fensome, D. V. Venugopal

Bibliographic record

VenueAtlantic Geology · 2003
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsGovernment of New BrunswickUniversity of New BrunswickBedford Institute of OceanographyGeological Survey of CanadaNatural Resources Canada
FundersKillam TrustsDalhousie University
KeywordsGeologyOutcropCretaceousPalynologyFossil woodPaleontologyMesozoicCarboniferousMolasseSubtropicsPollenStructural basin

Abstract

fetched live from OpenAlex

A small outcrop of quartz (silica) sand has been recognized at Vinegar Hill, near Cassidy Lake south of Sussex, New Brunswick, since the 1980s and extracted for commercial purposes. The deposit overlies Carboniferous rocks and underlies glacial deposits, and its setting is very similar to comparable, confirmed Cretaceous deposits in Nova Scotia. The age of the Vinegar Hill deposit, which appears to be of fluvial origin, has been unconfirmed until the present study. In this study, a general Mesozoic-early Tertiary age is indicated by the identity of a fossil araucarian wood specimen that occurs within the sand, and palynomorphs suggest a late Early Cretaceous, probably Albian, age. The absence of true growth rings in the wood implies a humid subtropical climate characterized by high temperatures, a conclusion consistent with a Cretaceous age because such climates are predicted for that age in the region by global paleoclimate reconstructions. The Vinegar Hill deposit represents the only known outcrop of Cretaceous strata in New Brunswick, but given its economic and scientific interest, a search for similar basins in the province would be worthwhile. RÉSUMÉ Un petit affleurement de sable quartzeux (silice) a été repéré sur la colline Vinegar, près du lac Cassidy, au sud de Sussex, Nouveau-Brunswick, au cours des années 80 et il a fait l'objet d'extraction à des fins commerciales. Le gîte recouvre des roches du Carbonifère et se trouve sous des dépôts glaciaires, dans un cadre semblable aux gîtes crétacés confirmés comparables de la Nouvelle-Écosse. L'âge du gîte de la colline Vinegar, qui semble d'origine fluviatile, n'avait pas été confirmé avant la présente étude. L'étude le situe d'une façon générale au Mésozoïque-Tertiaire inférieur en s'appuyant sur l'identité d'un spécimen de bois araucarien fossile présent à l'intérieur du sable; les palynomorphes laissent supposer qu'il remonterait à la fin du Crétacé inférieur, probablement l'Albien. L'absence de cernes réels dans le bois permet de supposer un climat subtropical humide caractérisé par des températures élevées, une conclusion qui est compatible avec un âge le situant au Crétacé parce qu'on peut déterminer la présence de tels climats dans la région à cette époque au moyen de reconstructions paléoclimatiques planétaires. Le gîte de la colline Vinegar représente le seul affleurement connu de strates du Crétacé au Nouveau-Brunswick, mais vu son intérêt économique et scientifique, il serait intéressant de rechercher des bassins semblables dans la province.

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 score0.293
Threshold uncertainty score0.590

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.000
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 head0.016
GPT teacher head0.219
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

Citations14
Published2003
Admission routes4
Has abstractyes

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