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Record W7023664345

Palynological dating of low-grade metamorphosed rocks: applications to Early Paleozoic rocks of the Central Maine/Aroostook-Matapedia basin and Fredericton trough (Northern Appalachians) in Eastern and East-Central Maine, USA

2020· article· en· W7023664345 on OpenAlex

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

VenueSapientia (Algarve University) · 2020
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsFaciesSedimentologyTrough (economics)Structural basinOrdovicianPaleozoicLaurentiaAcritarchSedimentary rockTerrane
DOInot available

Abstract

fetched live from OpenAlex

Identification of spores, acritarchs, and chitinozoans in weakly metamorphosed (>= 300 degrees C) turbidites demonstrates the usefulness of palynological dating for hitherto unfossiliferous strata that underlie much of the Gander terrane in Maine. Combined with sparse macrofossil ages and geochronologic data from detrital zircons, volcanic horizons, and plutons, the fossils constrain the ages of strata in the Central Maine/Aroostook-Matapedia (CMAM) basin and Fredericton trough and help to resolve paleogeographic and tectonic problems. Ages for the provisional Brewer (Upper Ordovician to Llandovery) and Bangor (Wenlock) formations in the Bangor area fill the last remaining gap in CMAM basin stratigraphy and permit correlation across the entire basin, from western Maine to the New Brunswick border. Resulting lithofacies patterns document basinward facies changes from both eastern and western external sources, and also indicate internal sources within the basin. A progressive decrease in carbonate sediment in the CMAM basin toward the south suggests interaction between axial and basinward currents in which micrite transported by axial currents from the Matapedia platform in northern New Brunswick was progressively overwhelmed to the south by clastic sedimentation from flanking highland sources. Middle to late Silurian age ranges for the Flume Ridge Formation, the most extensive unit in the Fredericton trough, and the newly named County Road Formation permit correlation with rocks in similar structural positions in New Brunswick. Recent geologic mapping, the new age control, and improved understanding of facies relationships show that the CMAM basin was perhaps as wide as 800 to 1000 km prior to deformation; developed on continental crust after mid-Ordovician plate accretion; contained a body of deep water with anoxic bottom conditions and mostly pelagic organisms; and contains a series of overlapping submarine fans derived from multiple sources.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.017
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
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 head0.014
GPT teacher head0.184
Teacher spread0.169 · 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