Prospects and pitfalls of an intrusive model for the Chatelperronian stone tool industry during the Middle to Upper Palaeolithic transition in France and northern Spain

Djakovic, I.; Soressi, M.; Roussel, M.

doi:10.1101/2023.07.14.549013

Home/Archive/bioRxiv

bioRxiv · 10.1101/2023.07.14.549013

Prospects and pitfalls of an intrusive model for the Chatelperronian stone tool industry during the Middle to Upper Palaeolithic transition in France and northern Spain

Djakovic, I.·Soressi, M.·Roussel, M.

View original source ↗Export metadata ↓

Abstract

The Middle to Upper Palaeolithic transition in France and northern Spain reflects the transition from Neandertals to Homo sapiens and the emergence of novel cultural entities and standardised laminar technologies between ~50 and 40 thousand years ago. The Chatelperronian stone tool industry sits at the centre of this period, and is commonly considered as representing a geographically isolated archaeological entity produced by late Neandertals. However, debate as to the makers and origin of this industry has long persisted. Fuel has recently been thrown onto this discussion through the formulation of a hypothesis in which the Chatelperronian directly originates from the Northern Early Ahmarian industry of the Levant. This model proposes that the Chatelperronian is in fact indicative of a direct migration of a population of Homo sapiens from the Levant to France around 44-40 thousand years ago - potentially via the crossing (or series of crossings) of the Mediterranean Sea. Such a scenario would have significant implications for how we interpret this key portion of recent human evolutionary history. In this paper, we highlight some of the prospects and pitfalls of an intrusive origin model for the emergence of the Chatelperronian industry in western Europe - taking into account technological, chronological, geographic, and stratigraphic perspectives. To frame this discussion, we review the state of understanding on the Chatelperronian and provide a detailed, synthetic review of Chatelperronian lithic technology. Our review reinforces the distinctive and fully Upper Palaeolithic character of this industry, and we subsequently suggest a few avenues of research which, in our opinion, may help shed progressively clearer light on the demographic and cultural processes operating during the Middle to Upper Palaeolithic transition in western Europe.

Explore related subjects

ecology Preprint

Keep this discovery

Explore connections, maps & timelines

BibTeX RIS

Djakovic, I., Soressi, M., Roussel, M.. 2023-07-14. Prospects and pitfalls of an intrusive model for the Chatelperronian stone tool industry during the Middle to Upper Palaeolithic transition in France and northern Spain. https://doi.org/10.1101/2023.07.14.549013

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related preprints

bioRxiv2026

A leaf-carbon economy model to explain the adaptive value of low vs. high leaf mass per area as a function of habitat productivity

Plant traits interact with environmental conditions to determine plant fitness. In particular, plant species with low leaf mass per area (LMA) are more common in high fertility soils and forest gaps, while plant species with high LMA are more common in low fertility soils and in shaded forest understories. It is not yet known why the adaptive value of LMA changes as a function of environmental productivity. We present a model for plant growth as a function of LMA and productivity. Our model relies on an empirically derived relationship between LMA and leaf lifespan. We are able to explain why species with lower LMA are successful in high productivity environments including environments with high availability of either light or soil nutrients, by showing that the LMA which maximizes growth rate decreases with increasing rate of carbon assimilation. We show that low LMA species are better at taking advantage of the 'high interest' environment of high productivity habitats by reinvesting assimilated carbon in new leaves and earning compound interest, while high LMA species grow more efficiently in the 'low interest' environment of low productivity habitats. This tradeoff sheds light on the adaptive value of LMA as it relates to environmental productivity.

ecology↗

bioRxiv2026

Species differentiate water uptake depths within a narrow vertical zone in temperate grasslands

Whether and under which conditions coexisting species in temperate grasslands differentiate their water uptake within the shallow soil layer they share is central to understanding hydrological niche differentiation in these ecosystems. In this field study, we quantified water uptake depth of 28 coexisting herbaceous species across 74 temperate grassland plots in three regions of Germany using oxygen stable isotopes and soil water content measured at multiple depths. Species consistently differed in water uptake depth across all regions, consistent with hydrological niche differentiation. This differentiation was largely confined to the upper 30 cm of soil and became stronger as overall soil moisture declined, with plants accessing water at greater depths in drier plots. In contrast, the vertical distribution of soil moisture was unrelated to either uptake depth or species differentiation. Despite pronounced species level variation, broad herbaceous functional classifications, including grasses versus forbs and fibrous versus taprooted species, showed substantial overlap in water uptake depth. Together, our results show that hydrological niche differentiation in temperate grasslands is expressed through fine scale differences among species within a shared shallow soil domain, becomes more pronounced under drier conditions, and is poorly captured by broad herbaceous functional classifications.

ecology↗

bioRxiv2026

Fungal-bacterial interactions enhance bacterial but constrain fungal resistance and recovery to extreme heat across soil moisture levels

Soil fungi and bacteria are key drivers of nutrient cycling and plant productivity in terrestrial ecosystems, yet their responses to climate extremes are rarely studied as interacting partners rather than in isolation. Moreover, it remains largely unknown how fungal-bacterial interactions regulate fungal and bacterial stability under climate extremes, particularly resistance (immediate responses to climate extremes) and recovery (responses after climate extremes cease). Here, we conducted a soil microcosm experiment with a bacterial species (Pseudomonas putida KT2440) paired with one of four Trichoderma species (T. hamatum, T. atroviride, T. koningiopsis, and T. harzianum). These fungal-bacterial pairs were then exposed to a 5-day heat event (40 {degrees}C/32 {degrees}C, day/night) followed by a 14-day recovery period (25 {degrees}C/17 {degrees}C, day/night), at two soil moisture levels (30% and 5% gravimetric water content). Our results show that fungal-bacterial interactions asymmetrically affect fungal and bacterial responses to extreme heat. Trichoderma species facilitated the resistance and recovery of P. putida density (CFUs) to extreme heat, whereas P. putida constrained the resistance and recovery of fungal biomass (ergosterol) to extreme heat, regardless of soil moisture conditions. Moreover, faster-growing Trichoderma species were associated with greater facilitation of bacterial resistance and recovery. Bacterial density also covaried positively with fungal biomass during heat stress under both soil moisture conditions, suggesting that net fungal facilitation enhances bacterial persistence under extreme heat. Together, our findings reveal that fungal-bacterial interactions can stabilize one microbial partner while increasing the vulnerability of the other, highlighting the contrasting consequences of biotic interactions under climate extremes.

ecology↗