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Widespread shallow-marine anoxia in Late Ordovician epicratonic seas of eastern Laurentia: Evidence from lithological and geochemical proxies

2025· article· en· W4410198348 on OpenAlexafffundabout
Dan Atasiei, Jisuo Jin, Karem Azmy, Cameron J. Tsujita, F R Brunton

Bibliographic record

VenueMarine and Petroleum Geology · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsGeological Survey of CanadaMemorial University of NewfoundlandWestern University
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsLaurentiaGeologyOrdovicianPaleontologyOceanographyGeochemistry

Abstract

fetched live from OpenAlex

ABSTRACT The Late Ordovician experienced dramatic episodes of globally widespread accumulation of organic-rich marine sediments as represented by black shales and their carbonate equivalents, often associated with ocean anoxia. During the mid-Katian, a widespread lithofacies of black, laminated, organic-rich marlstones referred to as BLORMs (new term ) in eastern Laurentia contain abundant benthic shelly fossils, such as brachiopods and large trilobites that are incompatible with anoxic water conditions previously suggested for the facies. Here, we present lithological, paleontological, and geochemical data to demonstrate that the BLORM facies accumulated in shallow epicratonic seas under predominantly suboxic conditions punctuated by frequent intervals of anoxia. Organic-rich laminae were the result of frequent eutrophication events associated with nutrient enrichment from weathering inputs enhanced by Taconic orogenic phases, and cool-water upwelling from the Appalachian Foreland Basin. The transitions from the normal-marine limestone of the Cobourg Formation to the Collingwood BLORM facies, and then to clay shale of the Blue Mountain Formation in southern Ontario represented oceanographic signals or changes resulting in widespread shallow-marine anoxia and a regional collapse of the carbonate factory in eastern Laurentia. The drastic increase in clay influx and decrease in TOC contents in the clay shale of the middle-upper Blue Mountain Formation mark the end of BLORM depositional conditions. The variations in the weathering (Rb/Sr, Al/Ti, ∑REE), redox (Cr, V, Mo, U, Th/U) and primary productivity (TOC, δ 15 N, Zn, P) proxies reflect the fluctuations of sea level and the influence of the Taconic orogenic pulses on siliciclastic inputs into the marine environment. The TOC, δ 15 N and P org profiles show distinct shifts that peak at a stratigraphic level correlated with the base of the Blue Mountain Formation and a significant increase in siliciclastic inputs as reflected by the climbing Rb/Sr, Al/Ti and ∑REE profiles, which is consistent with sedimentological evidence.

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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)0.000
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 score0.169
Threshold uncertainty score0.994

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.001
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 head0.011
GPT teacher head0.226
Teacher spread0.216 · 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

Citations2
Published2025
Admission routes3
Has abstractyes

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