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Record W2521527611 · doi:10.2110/jsr.2016.47

Living On the Edge: Evaluating the Impact of Stress Factors On Animal–Sediment Interactions In Subenvironments of A Shelf-Margin Delta, the Mayaro Formation, Trinidad

2016· article· en· W2521527611 on OpenAlexaff
Sudipta Dasgupta, Luís A. Buatois, M. Gabriela Mángano

Bibliographic record

VenueJournal of Sedimentary Research · 2016
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsUniversity of Saskatchewan
Fundersnot available
KeywordsGeologyMargin (machine learning)DeltaSedimentOceanographyPaleontology

Abstract

fetched live from OpenAlex

Abstract: Integrating sedimentological and ichnological characteristics of the Gelasian Mayaro Formation along the SE coast of Trinidad allows recognition of a river-dominated and wave-influenced shelf-edge deltaic succession of the paleo–Orinoco River developed under strong slope instability. Four main sedimentary settings and twelve subenvironments developed on and beyond the outer shelf (i.e., at the shelf margin) have been identified. Extreme paleoenvironmental conditions make the succession rarely and sporadically colonized. Ichnologic evidence suggests that shelf-edge deltas are among the most stressful marine environments, due to a combination of physicochemical factors in response to the intrinsic sedimentary processes and the relative hierarchy of their influences specific to every subenvironment. Within any particular subenvironment, the relative dominance of the fluvial feeder system, the action of waves (and rare influence of tides), and slope instability determine the combinations and ranking of stress factors. River-dominated shelf-edge delta subenvironments demonstrate the extreme influence of stress factors related to channel activity (e.g., salinity changes, high sedimentation and erosion rates, flocculation of mud, seasonal variations of fluvial flux), whereas subenvironments dominated by waves, storms, and oceanic swells away from the axial feeder(s) are mostly influenced by barform morphodynamics and its effects on local physiography. The paleo–Orinoco delta is represented not only by the delta lobe(s) developed at the shelf edge but by delta lobe(s) formed on the outer shelf as well. Outer shelf deltaic subenvironments manifest typical ichno-sedimentological signatures of a “normal” (wave-influenced in this case) inner-shelf delta. Being susceptible to extensive gravitational instabilities, the delta system suffered from canyonization (and smaller gullying) and subsequent filling (N.B. Hereafter we use the term canyon for both canyons and smaller gullies). The shelf-edge delta system was also associated with “shelf-attached” mass-transport systems. Such depositional subenvironments dominated by slope instability and sediment-gravity-flows appear to be the most unconducive for benthic colonization, resulting in almost complete absence of bioturbation. Characterization of the stress factors, as the functions of parameters arising from specific sedimentary and/or oceanographic processes, chemical conditions, and preservational constraints specific to each subenvironment, leads to the construction of a comprehensive ichnological and depositional analog model for shelf-edge deltas in general, and for the accommodation-driven low-latitude shelf-edge deltas at an active oblique foreland setting in particular.

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)0.004
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.015
Threshold uncertainty score0.997

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0040.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0040.000

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 head0.126
GPT teacher head0.388
Teacher spread0.262 · 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.

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

Citations56
Published2016
Admission routes1
Has abstractyes

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