MétaCan
Menu
← Back to cohort
Record W3126912406

Natural diagenesis in stromatolitic dolomite and chert from the late Palaeoproterozoic McLeary Formation

2021· article· en· W3126912406 on OpenAlexaboutno aff
Dominic Papineau

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsDiagenesisStromatoliteGeologyLithificationDolomitePrecambrianPyriteCarbonatePaleontologyMicrobial matGeochemistrySedimentary depositional environmentNatural (archaeology)Sedimentary rockPseudomorphOverprintingMineralogyDolostoneCarbonate rockQuartzMetamorphic rockChemistry
DOInot available

Abstract

fetched live from OpenAlex

Broad stromatolitic carbonate stages created during and after the Palaeoproterozoic Great Oxidation Occasion (GOE), which records a huge increment of oxygen in the environment and seas. Stromatolites interface natural and non-natural cycles through their minuscule organo-sedimentary designs that have the potential to give data about microbial and diagenetic measures that work during their arrangement. This investigation intends to report the mineralogy and natural geochemistry of tiny diagenetic structures in the incredibly protected late Palaeoproterozoic stromatolitic dolomite from the McLeary Formation of the Belcher Islands, in Nunavut, Canada. This is done to test the theory that artificially wavering responses can impact the arrangement of diagenetic spheroids, for example, rosettes, granules, solidifications, and botryoids; these responses happen over short timescales during diagenesis, for example prior to the lithification of the dregs. Decimetresize columnar stromatolites from the McLeary Formation contain centimeter-size pyrite solidifications, which themselves likewise contain framboids. Inside adjusted, dark chert solidifications and coarse quartz granules, there are filamentous microfossils made out of natural issue part of the way supplanted by pyrite. These perceptions are predictable with post-depositional oxidation–decrease responses including natural issue and sulfate. In examination, decimetre-size even bioherms of millimeter-to-centimeter size stromatolite sections contain minuscule dolomitic carbonate structures including circularly-concentric rosettes, drafted dolomite rhombs, and depression constructions of adjusted equidistant overlays, which are all layered with natural issue. All these diagenetic spheroids co-happen with circularly-concentric, equidistant and overlaid minerals related with debased natural issue or microfossils. The piece and math of these highlights are reliable with the nonbiological oxidation of natural carboxylic acids during diagenetic artificially swaying responses. Subsequently, both natural and non-organic cycles assume a significant part in the precipitation of diagenetic spheroids in McLeary stromatolites. Expanded plenitude of natural issue as microbial biomass, just as oxidized incandescent lamp also, sulfate, prompted far reaching natural disintegration in the Palaeoproterozoic McLeary Formation. At last, synthetically wavering responses after times of oxygenation probably assume a more critical part than already thought in the development of diagenetic spheroids inside stromatolitic dolomite.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation 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 score0.289
Threshold uncertainty score0.575

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.001
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.197
Teacher spread0.185 · 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 source (direct Gemma or distilled Codex), 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

Citations0
Published2021
Admission routes1
Has abstractyes

Explore more

Same topicPaleontology and Stratigraphy of Fossils→French-language works237,207→