The detrital record of Cretaceous to Pliocene sandstones across the NE South American margin
Bibliographic record
Abstract
The Cretaceous to Pliocene erosional history of the NE South American margin depicts the increasing influence of the uplifting Caribbean Mountain belt. Petrographic analyses of 59 Cretaceous to Late Pliocene sandstone samples derived from across the islands of Trinidad and Barbados, demonstrate systematic mineralogical changes whereby Early Cretaceous arkosic arenites gave way to mature quartz arenites by the Late Cretaceous and Caribbean Mountain-derived lithic-rich arenites during the Neogene. Changes in the framework compositions are accompanied by changes in textural attributes, with Caribbean Mountain detritus being notably finer grained than cratonic input. Silica cements predominate in quartzose sandstones and sericitic and clay cements within litharenites. The changing mineralogical compositions record the gradual deformation of the northern South American passive margin and initiation of the Andean–Caribbean Mountain foreland basin system, with incipient orogenic detritus evident from the latest Eocene and unambiguous orogenic input by the Late Oligocene. The preponderance of finer grain sizes within deltaic Pliocene sandstones records the later fill of an established foredeep with sediments sourced primarily from erosion of the Andean hinterland. These interpretations agree with heavy mineral compositional changes and the timing of uplift from geo- and thermo-chronological data across the margin. Supplementary material: Qualitative descriptions, sample coordinates and raw point counts are available at https://doi.org/10.6084/m9.figshare.c.3659381
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot 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.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.001 | 0.001 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.001 | 0.000 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".