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Record W4224262641 · doi:10.31223/x5kw6x

Exploring the depositional, diagenetic and carbon-oxygen isotope record of an evolving Ordovician carbonate system, Tarim Basin, China

2022· preprint· en· W4224262641 on OpenAlexafffund
Yuefeng Shen, Fritz Neuweiler, Adrian Immenhauser

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsUniversité LavalGeological Survey of Canada
FundersChina Scholarship CouncilHefei University of TechnologyHefei UniversityNational Natural Science Foundation of ChinaUniversité Laval
KeywordsGeologyOrdovicianDiagenesisPaleontologyCarbonateCarbonate platformFaciesδ18OSedimentary depositional environmentChemostratigraphyIsotopes of carbonGeochemistryTotal organic carbonStructural basinStable isotope ratio

Abstract

fetched live from OpenAlex

Bulk-rock based carbon-oxygen chemostratigraphy should be combined with a detailed understanding of depositional facies (mineralogy, porosity), its 2D-chronostratigraphic architecture, and diagenesis. The Ordovician of the western Tarim Basin recorded a peculiar litho-biostratigraphic succession. The Darriwilian Yijianfang Formation formed part of a carbonate ramp dominated by filter feeders. Toward its top, there is condensation succeeded by a multi-Myr hiatus. The hiatus correlative succession is a black-shale (Darriwilian to early Sandbian Saergan Formation) preserved in slope-to-basin settings. A marine red-bed interval (Sandbian Tumuxiuke Formation) diachronously succeeded toward a more basin-wide record. Finally, the late Sandbian to Katian Lianglitag Formation re-established a shallow-water carbonate factory (ramp-to-platform), but this time being highly productive and hosting a diversifying assemblage of benthic primary producers. By exploring diagenesis associated with a first component-specific data-set of δ13C - δ18O values and by integrating and filtering respective literature bulk-rock data, a synoptic chemo-chronostratigraphic sequence is presented. It displays segments lasting from tens of Myrs to several 100 kyrs. There is a long-term trend of increasing δ13C values culminating in the early Katian at 3.2 ‰ followed by a steady decrease. This tipping point is associated with a precursory baseline shift that interferes with the short-term Guttenberg carbon-isotope excursion presumably associated with a positive shift of δ18O values. The baseline shift was driven by regional effects of photosynthesis and a boosting (dasycladacean-related) production of aragonite along the Sandbian-Katian boundary interval. There is a medium-term (Darriwilian to earliest Sandbian) negative δ13C excursion coinciding with both a basal positive δ18O excursion and the demise of the Darriwilian carbonate ramp (Suecicus-Event, new term). It might represent the effects of volcanism/SO2-outgassing during the switch from a passive to an active continental arc. This event masquerades the elsewhere recorded middle Darriwilian carbon-isotope excursion. Caution is needed to consider the Tarim realm for global Ordovician chemostratigraphy.

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 score0.085
Threshold uncertainty score0.170

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 studies0.0000.000
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 head0.035
GPT teacher head0.221
Teacher spread0.187 · 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

Citations1
Published2022
Admission routes2
Has abstractyes

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