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Record W1982679949 · doi:10.2113/gsrocky.38.1.45

Stratigraphy and megaflora of a K-T boundary section in the eastern Denver Basin, Colorado

2003· article· en· W1982679949 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

VenueRocky Mountain geology · 2003
Typearticle
Languageen
FieldAgricultural and Biological Sciences
TopicPlant Diversity and Evolution
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyStratigraphySection (typography)Structural basinBoundary (topology)PaleontologyGeomorphologyTectonicsOperating system

Abstract

fetched live from OpenAlex

A 50-m-thick section of the Denver Formation (D1 sequence of Raynolds) exposed at the West Bijou Site of the Plains Conservation Center, Arapahoe County, Colorado, contains the first complete Cretaceous-Tertiary (K-T) boundary section in the Denver Basin. The 3-cm-thick boundary claystone coincides with a 21 percent palynological extinction, contains iridium and shocked-mineral anomalies, and is immediately overlain by a 7-cm-thick, fern-spore anomaly interval. The entire 50-m section is of reversed magnetic polarity and is interpreted to be subchron C29r because of paleontological data, the presence of a tuff with an 40 Ar/39 Ar date of 65.73 ± 0.13 Ma, and by correlation to the Kiowa cored well. A diagnostic basal Puercan (Pu1) mammal jaw was found 12 m above the boundry clay, and ceratopsian and hadrosaurian dinosaur fragments occur 4 m below the boundary clay. Estimates of the basin sedimentation rate derived from the duration of C29r based on marine cyclostratigraphy suggest that the 28 m of basal Paleocene strata represent approximately 200,000 years. Abundant fossil leaves found within the Paleocene sedimentary rocks at the West Bijou Site K-T boundary section allow assessment of early Paleocene patterns of plant diversity. Nine leaf localities at eight stratigraphic levels in the basal 22 m of the Paleocene section were sampled and analyzed to better understand the flora that survived the global K-T catastrophe. The Paleocene flora of this site is taxonomically dominated by dicotyledonous angiosperms (74%), with lesser numbers of monocotyledons (10%), ferns and allies (11%), and conifers (5%). By number of specimens, angiosperms comprise greater than 95 percent of the flora. Within the sampled section, there were no recognizable directional trends in diversity or abundance, suggesting that earliest Paleocene vegetation was stable, although not particularly diverse. The West Bijou Megaflora is strikingly similar in composition and relative abundance to basal Paleocene floras from the northern Great Plains. This K-T boundary disaster-recovery flora, also known as the FUI flora, is shown to have been widespread, ranging from central Colorado to southern Canada, a distance of at least 1,100 km. The West Bijou Site megaflora is markedly different from coeval floras along the western margin of the Denver Basin, supporting the hypothesis that orography and elevation provided greater influence on basal Paleocene floral composition and diversity than did latitude.

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 score0.023
Threshold uncertainty score0.472

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
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 head0.012
GPT teacher head0.183
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