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Record W153958331

Новые сведения по биостратиграфии и фораминиферам турона Западной Сибири

2012· article· ru· W153958331 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
KeywordsBoreholeGeologyHorizonPaleontologyGeometry
DOInot available

Abstract

fetched live from OpenAlex

The previous studies on numerous borehole sections of Western Siberia have proved that the Kuznetsovskian Horizon is assigned to the Turonian and encloses two foraminiferal zones: the Gaudryinopsis angustus Zone (the Lower Turonian) and the Pseudoclavulina hastata Zone (the Upper Turonian). The systematic composition and distribution of the Turonian assemblages along the lateral and in the sections of Western Siberia were previously reported by the present author [1, 2, 3, 4, 9]. In the top of the Kuznetsovskian Horizon, numbers of the zonal species Gaudryinopsis angustus Podobina are reduced, while the quantity of the Pseudoclavulina hastata (Cushman) Species increases in the upper zone of the Turonian. Simultaneously, the content of Reophax and Haplophragmiidea in this zone grows, the species Ammoscalaria antis Podobina, Textularia anceps Reuss, Trochammina arguta Podobina appear. In the northern district of Western Siberia (northwards the lateral flow of the Ob River) several holes were first bored within the Van-Eganskaya area. Of them, in sections of boreholes 1002 and 2031 the deposits of the Kuznetsovskian Horizon were studied, in which the clearly defined Late Turonian Pseudoclavulina hastata Zone was established. In the bottom of the horizon the Lower Turonian Gaudryinopsis angustus Zone was established within the section of borehole 2031 (depth interval 936.5-934.9 m). In borehole 1002 (depth interval 942.0-938.5 m) beds with Hedbergella loetterlei, with the planktonic foraminifers dominant in the assemblage, correspond to the above stated zone. The sections of these two boreholes are illustrated in figures 1 and 2, where the data are combined on the lithological structure, zones, beds and characteristic species of the assemblages. The analysis of the systematic composition of the Turonian foraminiferal assemblages of Western Siberia, Northern Alaska and Canada entering the Arctic Paleozoogeographic Realm demonstrated their great similarity not only at the generic level, but also at the specific one. Among the compared assemblages, the common species, geographical subspecies and vicariants were distinguished. The Gaudryina (Gaudryinopsis) irenensis Stelck et Wall Species is the vicariant for the West Siberian zonal species Gaudryinopsis angustus Podobina. In a number of Canadian provinces, the Pelagic zone enclosing the planktonic foraminifers seems to correspond to West Siberian Lower Turonian beds with Hedbergella loetterlei. The new factual material on the Turonian foraminifers of the northern district of Western Siberia allowed to compare their systematic composition with that of the coeval species from both the other districts of Western Siberia and more remote regions: Northern Alaska and Canada. Four palaeontological plates illustrate the Turonian characteristic species of the northern district of Western Siberia (boreholes 1002, 2031 of the Van-Eganskaya area).

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, 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 score0.474
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.002
Science and technology studies0.0020.001
Scholarly communication0.0000.003
Open science0.0020.001
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0230.017

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