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Record W2254192784

Palynological dating of the upper part of the De Geerdalen Formation on central parts of Spitsbergen and Hopen

2013· dissertation· en· W2254192784 on OpenAlexaboutno aff
Marianne Ask

Bibliographic record

VenueBergen Open Research Archive (BORA) (University of Bergen) · 2013
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsPalynologyGeologyPaleontologyArchaeologyPhysical geographyGeographyPollenBiology
DOInot available

Abstract

fetched live from OpenAlex

The Late Triassic is the most problematic period in terms of resolution and age control. The period spans about 36 million years and consists of three stages - Carnian, Norian and Rhaetian. Only four clusters of radiometric age constrain the Triassic time scale (Ogg et al., 2012), and macrofossil data are scarce, hampering exact age determination and biostratigraphic correlation. Additional knowledge on the stratigraphy and geographic ranges of different fossil groups are therefore crucial to build a better framework and thereby contribute in increasing the database. In the Barents Sea area, a huge delta complex reached Eastern Svalbard and Hopen by the end of Late Carnian, and by the end of Late Triassic the paralic deposits had prograded over the northwestern part of the Svalbard Archipelago. Shales, siltstones and sandstones of various thicknesses alternate in the De Geerdalen, Flatsalen and Svenskøya formations, reflecting the deltaic sediments deposited during this period (Riis et al., 2008). Previous studies regarding age datings from Hopen have been conflicting, and a lot of uncertainty is related to the location of the prograding deltafront at any time during this period. Palynological work from two sections, located at Lyngefjellet northeast on Hopen, and from Deltaneset, Central Spitsbergen, resulted in recognition of three assemblages of Late Carnian to ?Middle Norian age. The palynological assemblages are based on spores, pollen, acritarchs and other palynomorphs, and correlation to published records from the Barents Sea area and Arctic Canada have been used for age determination. The lower part of the De Geerdalen Formation section on Hopen is assigned a Late Carnian age based on palynological assemblages similar to the palynofloras recorded in the Barents Sea area and Arctic Canada, and is believed deposited in a deltaic setting reflected in a palynoflora from typical wetland plants. For the upper part of the formation, Early Norian has been suggested based on resemblances to assemblages from the overlying ammonite dated (Korchinskaya, 1982) Flatsalen Formation. The upper section of the De Geerdalen Formation belongs to the Hopen member (Solvi, 2013), herein documented to be equivalent to the Isfjorden Member on Deltaneset, Central Spitsbergen. A coastal environment, probably a delta setting, is suggested for these sections. Svenskøya Formation overlays the Flatsalen Formation and an Early to Middle Norian age is suggested based on the stratigraphically limited taxa, and a delta-setting environment is proposed.

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)0.001
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 score0.144
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.061
GPT teacher head0.265
Teacher spread0.204 · 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

Citations6
Published2013
Admission routes1
Has abstractyes

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