Aix Marseille Univ, CNRS, Minist. Culture, LAMPEA, Aix-en-Provence, France.
Grupo de Investigación en Prehistoria IT-1223-19 (UPV-EHU)/IKERBASQUE-Basque Foundation for Science, Vitoria, Spain.
Am J Phys Anthropol. 2020 Oct;173(2):218-235. doi: 10.1002/ajpa.24089. Epub 2020 Jun 18.
The aims of this research are to explore the diet, mobility, social organization, and environmental exploitation patterns of early Mediterranean farmers, particularly the role of marine and plant resources in these foodways. In addition, this work strives to document possible gendered patterns of behavior linked to the neolithization of this ecologically rich area. To achieve this, a set of multiproxy analyses (isotopic analyses, dental calculus, microremains analysis, ancient DNA) were performed on an exceptional deposit (n = 61) of human remains from the Les Bréguières site (France), dating to the transition of the sixth to the fifth millennium BCE.
The samples used in this study were excavated from the Les Bréguières site (Mougins, Alpes-Maritimes, France), located along the southeastern Mediterranean coastline of France. Stable isotope analyses (C, N) on bone collagen (17 coxal bones, 35 craniofacial elements) were performed as a means to infer protein intake during tissue development. Sulfur isotope ratios were used as indicators of geographical and environmental points of origin. The study of ancient dental calculus helped document the consumption of plants. Strontium isotope analysis on tooth enamel (n = 56) was conducted to infer human provenance and territorial mobility. Finally, ancient DNA analysis was performed to study maternal versus paternal diversity within this Neolithic group (n = 30).
Stable isotope ratios for human bones range from -20.3 to -18.1‰ for C, from 8.9 to 11.1‰ for N and from 6.4 to 15‰ for S. Domestic animal data range from -22.0 to -20.2‰ for C, from 4.1 to 6.9‰ for N, and from 10.2 to 12.5‰ for S. Human enamel Sr/ Sr range from 0.7081 to 0.7102, slightly wider than the animal range (between 0.7087 and 0.7096). Starch and phytolith microremains were recovered as well as other types of remains (e.g., hairs, diatoms, fungal spores). Starch grains include Triticeae type and phytolith includes dicotyledons and monocot types as panicoid grasses. Mitochondrial DNA characterized eight different maternal lineages: H1, H3, HV (5.26%), J (10.53%), J1, K, T (5.2%), and U5 (10.53%) but no sample yielded reproducible Y chromosome SNPs, preventing paternal lineage characterization.
Carbon and nitrogen stable isotope ratios indicate a consumption of protein by humans mainly focused on terrestrial animals and possible exploitation of marine resources for one male and one undetermined adult. Sulfur stable isotope ratios allowed distinguishing groups with different geographical origins, including two females possibly more exposed to the sea spray effect. While strontium isotope data do not indicate different origins for the individuals, mitochondrial lineage diversity from petrous bone DNA suggests the burial includes genetically differentiated groups or a group practicing patrilocality. Moreover, the diversity of plant microremains recorded in dental calculus provide the first evidence that the groups of Les Bréguières consumed a wide breadth of plant foods (as cereals and wild taxa) that required access to diverse environments. This transdisciplinary research paves the way for new perspectives and highlights the relevance for novel research of contexts (whether recently discovered or in museum collections) excavated near shorelines, due to the richness of the biodiversity and the wide range of edible resources available.
本研究旨在探索早期地中海农民的饮食、流动性、社会组织和环境开发模式,特别是海洋和植物资源在这些饮食方式中的作用。此外,这项工作还旨在记录与该生态丰富地区新石器化相关的可能的性别行为模式。为了实现这一目标,对来自法国滨海阿尔卑斯省莫让(Mougins)Les Bréguières 遗址(法国)的一个特殊人类遗骸(n=61)进行了一组多指标分析(同位素分析、牙垢、微体分析、古 DNA),这些遗骸可追溯到公元前 6 世纪到 5 世纪的过渡期。
本研究使用的样本来自法国滨海阿尔卑斯省莫让的 Les Bréguières 遗址(Mougins,法国),位于法国东南部地中海海岸线沿线。对骨胶原(17 块骨盆骨,35 块颅面骨)进行稳定同位素(C、N)分析,以推断组织发育过程中的蛋白质摄入量。硫同位素比值可作为地理和环境起源的指标。牙垢中植物的研究有助于记录植物的消费情况。对牙釉质中的锶同位素(n=56)进行分析,以推断人类的起源和地域流动性。最后,通过古 DNA 分析研究新石器时代群体中的母系和父系多样性(n=30)。
人类骨骼的稳定同位素比值范围为 C 的-20.3 至-18.1‰,N 的 8.9 至 11.1‰,S 的 6.4 至 15‰。家养动物的数据范围为 C 的-22.0 至-20.2‰,N 的 4.1 至 6.9‰,S 的 10.2 至 12.5‰。人类牙釉质的 Sr/Sr 范围为 0.7081 至 0.7102,略宽于动物范围(0.7087 至 0.7096)。还回收了淀粉和植硅体微体以及其他类型的遗骸(如毛发、硅藻、真菌孢子)。淀粉粒包括三碳作物类型,植硅体包括双子叶植物和单子叶植物,如panicoid 草。线粒体 DNA 鉴定了八个不同的母系谱系:H1、H3、HV(5.26%)、J(10.53%)、J1、K、T(5.2%)和 U5(10.53%),但没有一个样本产生可重复的 Y 染色体 SNP,从而阻止了父系谱系的鉴定。
碳和氮稳定同位素比值表明人类主要通过食用陆地动物来获取蛋白质,并且可能会利用海洋资源,其中包括一名男性和一名未确定的成年人。硫稳定同位素比值允许区分来自不同地理起源的群体,其中包括两名可能更多地暴露在海雾效应中的女性。尽管锶同位素数据表明个体没有不同的起源,但来自耳骨的线粒体谱系多样性表明,埋葬包括遗传上有区别的群体或一个实行父居制的群体。此外,牙垢中记录的植物微体残留物首次表明,Les Bréguières 群体食用了广泛的植物性食物(如谷物和野生类群),这些食物需要接触不同的环境。这项跨学科研究为新的研究提供了新的视角,并强调了在沿海地区挖掘的背景(无论是最近发现的还是在博物馆收藏中)进行新研究的相关性,因为这些背景的生物多样性和可食用资源的广泛范围提供了丰富的研究价值。