Early Triassic Trace Fossils of the Western United States and their Implications for Prolonged Environmental Stress from the End-Permian Mass Extinction
Bibliographic record
Abstract
Abstract The end-Permian mass extinction left an indelible mark on trace-fossil assemblages. This is evident during the lag phase of the biotic-recovery interval that occurred in the Early Triassic. Research on the Spathian Virgin Limestone Member of the Moenkopi Formation, western United States, has yielded a mixed carbonate–siliciclastic trace fossil assemblage. The presence of such traces as Thalassinoides, Laevicyclus, and Gyrochorte indicate that previously unreported metazoan behaviors had reappeared in equatorial regions by the close of the Early Triassic. Whereas diversity of trace-fossil assemblages increased from earliest to late Early Triassic time, persistent small size, low average ichnofabric index, low bedding-plane coverage, and reduced tiering point to prolonged stressful environmental conditions following the end-Permian mass extinction—conditions for which there is an abundance of global sedimentological evidence. This trace-fossil assemblage provides a record of soft-bodied organisms that might not otherwise be detected from the study of body fossils alone; it therefore acts as a constraint on the timing of the biotic recovery. This assemblage from the Virgin Limestone Member also serves as an indicator of environmental conditions that might not otherwise be gleaned, illustrating the utility of using trace fossils as environmental proxies during the lag phase of a biotic recovery. The presence of some of these traces (i.e., Thalassinoides) in lowermost Triassic strata of western Canada suggests that the recovery of trace-makers after the end-Permian mass extinction was asynchronous, and that northerly latitudes may have experienced a less-protracted biotic recovery than in equatorial regions.
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 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 | 0.001 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.002 | 0.002 |
| Science and technology studies | 0.001 | 0.000 |
| Scholarly communication | 0.001 | 0.000 |
| Open science | 0.000 | 0.001 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.002 | 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".