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Record W4322211011 · doi:10.5194/egusphere-egu23-15131

Depositional environment of coal and amber during the PETM and ETM-2 hyperthermal events in northern highlatitudes (Canadian Arctic)

2023· preprint· en· W4322211011 on OpenAlexaffabout
Andreas Lückge, Lutz Reinhardt, Werner von Gosen, Martin Blumenberg, Jennifer M. Galloway

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsGeological Survey of Canada
Fundersnot available
KeywordsGeologySedimentary depositional environmentPaleontologyUnconformitySedimentary rockClastic rockFjordArcticDetritusPaleogeneStructural basinOceanography

Abstract

fetched live from OpenAlex

High-latitude terrestrial records of Paleogene hyperthermal events can help to calibrate global climate models seeking a refined understanding of extreme warming events; however, such high-latitude records are rare. The Margaret Formation at Stenkul Fiord, southern Ellesmere Island, preserves a record of the early Eocene hyperthermal events. This late Paleocene to early Eocene sedimentary archive is composed of fluvially derived clastic sediments and amber-bearing coals. However, as the Eurekan deformation event caused major synsedimentary tectonic movement, resulting in substantial unconformities, the development of a reliable stratigraphic framework for Stenkul Fiord has proved challenging thus far. Field mapping and satellite image interpretation were used to identify unconformities and other tectonic structures in a section at Stenkul Fiord. In combination with a previously dated ash layer (U-Pb zircon age of 53.7 Ma, ID-TIMS) and biostratigraphic association (Graybullian, NALMA) of rare vertebrate fossils, both the PETM and ETM-2 hyperthermal events were identified. In addition, samples for new carbon isotope data of bulk coal, organic-rich sediments and ubiquitous occurring amber were collected. Using this refined stratigraphic framework the average sedimentation rates were calculated, and stratigraphic completeness of the section was evaluated. It was determined that the amount of clastic sediment deposited at Stenkul Fiord increased near the end stages of the PETM and ETM-2 hyperthermal events. This is interpreted as a response of the fluvial depositional system to an intensified hydrological cycle during the hyperthermals. This probably resulted also in discharge events, in which amber was enriched in layers due its lower density and thus their preferential mobilization and re-deposition during water flooding the swamp forest environment. Whereas amber in general shows less depleted isotope values compared to coals, this process may explain the larger offsets between the istopic composition of coals and ambers observed in some layers, respectively. This late Paleocene to early Eocene deposits at Stenkul Fiord offer further possibilities to study the effects of global warming events on terrestrial northern highlatitude depositional systems.

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 score0.040
Threshold uncertainty score0.080

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 studies0.0010.000
Scholarly communication0.0010.000
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 head0.021
GPT teacher head0.183
Teacher spread0.162 · 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

Citations0
Published2023
Admission routes2
Has abstractyes

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