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The ‘La Celle interglacial’: a key-record of MIS 11c palaeoenvironments and palaeoclimate in NW Europe

2025· article· en· W4415763173 on OpenAlexaff
N. Limondin-Lozouet, Julie Dabkowski, Pierre Antoine, Jean‐Jacques Bahain, Pierre Voinchet, Kirsty Penkman, Dustin White, Marie‐Claude Jolly‐Saad, Patrick Auguste, Bassam Ghaleb

Bibliographic record

VenueQuaternary Science Reviews · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsUniversité du Québec à Montréal
FundersEuropean Research CouncilHorizon 2020 Framework ProgrammeCentre National de la Recherche ScientifiqueConseil National de la Recherche ScientifiqueH2020 European Research CouncilAgence Nationale de la Recherche
KeywordsPalynologyEcological successionMarine isotope stagePleistoceneInterglacialHippopotamusStromatoliteMediterranean climateQuaternary

Abstract

fetched live from OpenAlex

The La Celle calcareous tufa formation, located in the Seine valley (Paris Basin, France) provides an exceptional stratigraphic record (9 m thick), yielding a wide variety of palaeontological remains (molluscs, leaf prints, ostracods, mammals) as well as geochemical data allowing a detailed reconstruction of the environmental and climatic dynamics during the Marine Isotope Stage (MIS) 11c interglacial. The chronological assignment of the site is particularly well constrained by a number of methods (U-series, electron spin resonance, thermoluminescence). This review synthesises previously published data as well as new research on the formation of the deposit (stratigraphy, micromorphology), amino-acid geochronology, palaeobotany, and compares these results with those of European palynological references. Several important markers of the continental environments during MIS 11c are identified. The malacological succession is of particular importance for reconstructing the vegetation dynamics, reflecting the expansion of forest biotopes and their subsequent degradation and is closely linked to geochemical analyses, providing a reliable framework for the associated climatic conditions. The La Celle sequence yields the only complete record for the development of the “ Lyrodiscus fauna”, a characteristic biostratigraphic signature of MIS 11c in NW Europe. The long molluscan succession of La Celle is the relevant reference for the integration of shorter regional malacological series into the environmental dynamics of the interglacial. The occurrence of several Mediterranean trees, and mammal remains of Hippopotamus and Macaca are registered during the climatic optimum revealed by geochemistry. Together with isotopic data this set of thermophilic bioproxies indicates the warmest and wettest conditions ever recorded for late Middle Pleistocene interglacials in the region. Comparison of the reconstructed palaeoenvironmental and climatic succession with the nearest long pollen series demonstrates that the La Celle tufa deposit records almost the entire interglacial. Therefore, the “La Celle Interglacial” is proposed as a major reference for understanding the evolution of the MIS 11c continental landscapes and biodiversity in northwestern Europe. • Major record of continental MIS 11c climatic and environmental dynamics in NW Europe. • Coupled land snails and isotopes allow correlation with palynological references. • La Celle Interglacial is a key reference for NW European MIS 11c palaeobiodiversity.

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)0.003
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.055
Threshold uncertainty score0.645

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0030.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.002
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.017
GPT teacher head0.276
Teacher spread0.260 · 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.

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".

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Citations1
Published2025
Admission routes1
Has abstractyes

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