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Record W2050093939 · doi:10.1134/s0031030114070016

Fusulinids (Foraminifera), lithofacies and biofacies of the Upper Moscovian (Carboniferous) of the southern Moscow Basin and Oka-Tsna Swell

2014· article· en· W2050093939 on OpenAlexaff
Daria V. Baranova, Pavel Kabanov, A. S. Alekseev

Bibliographic record

VenuePaleontological Journal · 2014
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsGeological Survey of CanadaUniversity of Calgary
Fundersnot available
KeywordsCyclothemsPaleontologyGeologyFaciesForaminiferaPennsylvanianGenusCarboniferousBiozoneBiostratigraphyStructural basinOceanographyEcologyBiology

Abstract

fetched live from OpenAlex

Twenty-nine fusulinid species of 14 genera are determined in the Podolskian and Myachkovian substages (Pennsylvanian) of the southern Moscow Basin. All test sections are determined to genus level, except for the genera Schubertella and Fusiella . Since it is impossible to distinguish between these two genera in oblique test sections, they are identified to the family Schubertellidae. The stratigraphic distribution of fusulinid species put on a new sequence-stratigraphic framework (succession of cyclothems) reveals nonsimultaneous appearance of zonal assemblages in different localities. Sporadical occurrence of index species below and above their designated zones attest for shortage of reliable biostratigraphic markers within the Upper Moscovian interval. The legacy acmezones Fusulinella bocki and Fusulina cylindrica appear to be the most robust divisions in the regional fusulinid zonation. The Podolskian-Myachkovian stratigraphic interval is characterized by progressive decline of Neostaffella , whereas representatives of Fusulina show inverse development. The genus Fusulina changes its facies preference from normal marine subtidal facies in the Podolskian to shoal peloidal-bioclastic grainstones in the upper half of the Myachkovian. Fusulinid genera tend to be distributed patchy and within a broad facies range. It is confirmed that the staffellid genera Reitlingerina and Parastaffelloides are good indicators of shallow-water normal marine euphotic conditions. The genus Hemifusuina occasionally masses in mud-dominated tempestitic limestones of shallowing-upward (regressive) parts of cyclothems. Schubertellids were the most tolerant group as seen from their steady presence in the entire spectrum of marine facies of the studied basin. Five fusulinid biofacies are recognized in the Upper Moscovian: (1) Fusulinella-Ozawainella , (2) Staffellida, (3) Staffellida- Fusulina , (4) impoverished Schubertellidae, and (5) Hemifusulina . These paleo-biofacies are based on mean densities of fusulinids in thin sections (tests per cm 2 ), data departure criteria of these mean densities, the Shannon diversity index H , and Berger-Parker index of dominance d . Degree of differentiation of fusulinid biofacies is notably low, which is explained by unsteady benthic environments affected by frequent storm dispersals of benthic organisms and geologically rapid eustatic sea level changes. The relation of fusulinid, conodont, and general biofacies is discussed. Three general biofacies are recognized: staffellid-syphonean (photozoan and transitional heterophotozoan), bryonoderm extended (heterozoan), and Meekella - Ortonella (assemblages of stressed shallowlagoon to tidal-flat habitats).

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 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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.031
Threshold uncertainty score0.568

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.002
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 head0.202
Teacher spread0.189 · 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 teacher head, 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

Citations10
Published2014
Admission routes1
Has abstractyes

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