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Record W90907268 · doi:10.4000/quaternaire.6019

Etude morphosédimentaire d’un remplissage endokarstique de la grotte du bois du clos (Charente, France) : contraintes géométriques et dynamiques hydrologiques

2011· article· fr· W90907268 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueQuaternaire · 2011
Typearticle
Languagefr
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsUniversité du Québec à Montréal
FundersAgence Nationale de la Recherche
KeywordsHumanitiesGeologyArt

Abstract

fetched live from OpenAlex

<p class="resume">Une coupe dans un remplissage détritique remarquable de plus de 5 m de hauteur, situé dans la grotte du Bois du Clos (karst de La Rochefoucauld, Charente) a permis une analyse morphosédimentaire d’une séquence discontinue et complexe. Trois grandes phases successives d’ennoyage/dénoyage de la cavité ont été mises en évidence par la combinaison d’une analyse granulométrique, des diagrammes de Passega, d’une analyse minéralogique des sables et des argiles et d’une analyse géochimique. Malgré l’absence de jalons chronologiques à l’intérieur de la séquence sédimentaire, une chronostratigraphie et un calage chronologique sont proposés grâce à une stalagmite qui scelle le remplissage et datée du stade isotopique marin 3. Les résultats sont corrélés avec des épisodes mis en évidence dans des sites voisins. Ils montrent dans notre cas le paléofonctionnement d’un système karstique d’abord ouvert et largement influencé par la fluctuation d’une grande nappe karstique (la Touvre) et par des écoulements proches (paléopertes), mais qui progressivement va se fermer. La question de l’interprétation paléoclimatique et paléoenvironnementale des sédiments est discutée. Les notions de piège karstique et de lacune sédimentaire sont développées. Les effets de site sur l’enregistrement sédimentaire des influences des variations climatiques sont ici mis en évidence. </p><p class="resume"><span xml:lang="en" lang="en">A section in a remarkable sequence of detrital deposits of more than 5 m high, filling in the cave of the Clos du Bois (La Rochefoucauld karst, Charente) allowed a morphosedimentary analysis of a discontinuous and complex sequence. </span>Three major phases of submergence / dewatering of the cave have been identified by the combination of a grain-size analysis, Passega diagrams, a mineralogical analysis of sands and clays, and a geochemical analysis. Despite the lack of chronological milestones within the sedimentary sequence, a chronostratigraphy and time setting are proposed following the study of a stalagmite that seals the filling and is dated from marine isotopic stage 3. The results are correlated with episodes highlighted in nearby sites. They show in our case the palaeofunctioning of an initially open karst system heavily influenced by the fluctuation of a large karst water table (the Touvre) and by nearby flows (palaeostreams and palaeovadose flows), but gradually closing down. The palaeoclimatic and palaeoenvironmental interpretation of the sediments is discussed. Notions of endokarstic trap and sedimentary gap are developed. The “site effects” on the sedimentary record of the influences of climate variability are shown.</p>

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.

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)0.003
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Insufficient 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 score0.023
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0030.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.000
Science and technology studies0.0010.002
Scholarly communication0.0000.001
Open science0.0010.000
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0060.001

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 head0.017
GPT teacher head0.249
Teacher spread0.232 · 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