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Record W4414415567 · doi:10.1016/j.jasrep.2025.105399

The palaeoenvironmental context of MIS 3 and the use of plants by Neanderthal groups in southern Italy: results from the Riparo l’Oscurusciuto site

2025· article· en· W4414415567 on OpenAlexafffund
Rosa M. Albert, Juan Ochando, Ivan Martini, Carlos Rondón, Jacopo Crezzini, Clarissa Dominici, Vincenzo Spagnolo, Paolo Boscato, Annamaria Ronchitelli, Francesco Boschin, Francesco Berna

Bibliographic record

VenueJournal of Archaeological Science Reports · 2025
Typearticle
Languageen
FieldSocial Sciences
TopicPleistocene-Era Hominins and Archaeology
Canadian institutionsSimon Fraser University
FundersSocial Sciences and Humanities Research CouncilMinisterio de Ciencia, Innovación y UniversidadesAgencia Estatal de InvestigaciónEuropean Regional Development FundSocial Sciences and Humanities Research Council of CanadaMinisterio de Ciencia e Innovación
KeywordsNeanderthalPhytolithContext (archaeology)TaphonomyVegetation (pathology)Marine isotope stagePaleoecologyMacrofossil

Abstract

fetched live from OpenAlex

• Phytolith and pollen allow reconstruction of vegetation over 12,200 ka. • Vegetation is shifting from forests to open areas along the studied sequence. • Siliceous aqueous microremains indicates moisture conditions within the site. • Use of Poaceae plants and ash scattering revealed by study of sediments and hearths. • High phytolith dissolution is due to calcium carbonate rich sediments. Neanderthal populations occupied caves and rockshelters across the Mediterranean, leaving behind evidence of their daily activities, including plant remains. By studying these remains, we can gain a better understanding of how these populations used plant resources and adapted to their environment. A critical period for studying Neanderthal behaviour is Marine Isotope Stage 3 (MIS 3) which was characterized in Europe by millennial-scale climatic instability involving fluctuations between warming and cooling events. These changes may have impacted the dispersal and dynamics of Neanderthal populations, prompting new behavioural, subsistence and settlement adaptations. A key site for studying Neanderthal groups in southern Italy during MIS 3 is Riparo l’Oscurusciuto in the Ginosa Ravine. The site’s long stratigraphic sequence and well-preserved faunal and material culture remains, including hearths, span the period from ∼55 ka to ∼42.8 ka BP. This makes the site central to our understanding of Neanderthal life and how they adapted to the environment until their disappearance from the region. Here, we present the results of a high-resolution study of plant microremains (phytoliths and pollen) and aquatic siliceous microremains (diatoms and chrysophyte cysts), alongside the mineralogical characterisation of their sedimentary contexts using Fourier Transform Infrared (FTIR) spectroscopy. The ∼12,200-year long reconstruction of the palaeoenvironment reveals a changing landscape starting with semi-open woodlands and forests at ∼55 ka and changing to more open woodland steppe environments starting sometime before ∼52 ka. The woody vegetation was composed of evergreen and deciduous oak woodlands with a continued presence of other mesophytes and Mediterranean woody taxa, including gymnosperms. The grasses (mostly C 3 Pooid), are associated with a wide range of herbaceous species, probably reflecting the opening up of the landscape. Neanderthals responded to these changes by adapting their activities to the surrounding vegetation, by for example using grasses for the hearths, the ashes of which were later spread around the site.

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)0.006
metaresearch head score (Gemma)0.003
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesScience and technology studies
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.017
Threshold uncertainty score0.985

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0060.003
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.018
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 head0.028
GPT teacher head0.271
Teacher spread0.243 · 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

Citations2
Published2025
Admission routes2
Has abstractyes

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