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Record W57800897

Новые сведения по фораминиферам и биостратиграфии верхнего сеномана северного района Западной Сибири

2012· article· ru· W57800897 on OpenAlex
Подобина Вера Михайловна

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

VenueVestnik Tomskogo gosudarstvennogo universiteta Filologiya · 2012
Typearticle
Languageru
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyLithologyFaciesCenomanianBoreholeHorizonMarine transgressionPaleontologyBiostratigraphyBiozoneCretaceousStructural basin
DOInot available

Abstract

fetched live from OpenAlex

Foraminifers and biostratigraphy of the Upper Cenomanian of the northern district of Western Siberia were first studied with the use of materials from seven newly bored holes on the territory of the Van-Yeganskaya area. Two foraminiferal zones (the Lower Saccammina micra Ammomarginulina sibirica and the Upper Trochammina wetteri tumida Verneuilinoides kansasensis) were established in the Upper Cenomanian by the change in the species composition of the foraminiferal assemblages and the lithology of the enclosing rocks of seven studied borehole sections. The beds with Gaudryinopsis nanushukensis elongatus were traced within the lower part of the upper zone. The change in the species composition and the rocks lithology results from the depth variations in the spread of the advancing Boreal transgression. The significant difference of facies (the alternation of the relatively deep-water and shallow facies) is observed not only within the section of the Uvatskian Horizon (the Upper Cenomanian), but also laterally, especially in its uppermost strata. Hence, in some borehole sections of the Van-Yeganskaya area, in the upper strata of the Uvatskian Horizon, the marine facies of dark-gray clays were distinguished, to which the well-preserved foraminiferal assemblages of the upper zone were assigned. The similar well-preserved assemblages had previously been distinguished from the dark-grey, almost black clays of the top of the Uvatskian Horizon within the borehole sections of the Tazovskaya and Purpeyskaya areas. In the lower deposits of the Uvatskian Horizon, within the investigated seven borehole sections of the Van-Yeganskaya area, the foraminiferal tests, not sufficiently well preserved, were discovered having principally coarse-grained quartz-siliceous wall. The comparison of the Late Cenomanian foraminiferal assemblages from the West Siberian and Canadian provinces was made within the whole Arctic paleobiogeographical Realm. Thereby, the common species, vicariants and geographical subspecies were established. Owing to this comparison, the detailed correlation and refinement of the age of West-Siberian foraminiferal zones and beds of the Upper Cenomanian stratons were performed. In the present paper, ten species are described, eight of them are new. They are assigned to the following orders: Ammodiscida (the superfamily Haplophragmiidea the families Haplophragmoididae and Haplophragmiidae), Textulariida (the family Textulariidae). All the described species are illustrated on three paleontological plates. These taxa are of great importance for the subsequent determinative works for the study of foraminifers and biostratigraphy of the Cenomanian deposits of Western Siberia.

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)0.002
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, Research integrity, Insufficient payload (model declined to judge)
Consensus categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.465
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.000
Meta-epidemiology (narrow)0.0020.001
Meta-epidemiology (broad)0.0020.001
Bibliometrics0.0010.002
Science and technology studies0.0020.001
Scholarly communication0.0000.003
Open science0.0020.001
Research integrity0.0010.002
Insufficient payload (model declined to judge)0.0220.017

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 head0.030
GPT teacher head0.198
Teacher spread0.168 · 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