Faculty of Archaeology, Leiden University, 2300 RA, Leiden, The Netherlands.
Proc Natl Acad Sci U S A. 2012 Feb 7;109(6):1889-94. doi: 10.1073/pnas.1112261109. Epub 2012 Jan 23.
The use of manganese and iron oxides by late Neandertals is well documented in Europe, especially for the period 60-40 kya. Such finds often have been interpreted as pigments even though their exact function is largely unknown. Here we report significantly older iron oxide finds that constitute the earliest documented use of red ochre by Neandertals. These finds were small concentrates of red material retrieved during excavations at Maastricht-Belvédère, The Netherlands. The excavations exposed a series of well-preserved flint artifact (and occasionally bone) scatters, formed in a river valley setting during a late Middle Pleistocene full interglacial period. Samples of the reddish material were submitted to various forms of analyses to study their physical properties. All analyses identified the red material as hematite. This is a nonlocal material that was imported to the site, possibly over dozens of kilometers. Identification of the Maastricht-Belvédère finds as hematite pushes the use of red ochre by (early) Neandertals back in time significantly, to minimally 200-250 kya (i.e., to the same time range as the early ochre use in the African record).
欧洲有大量关于晚期尼安德特人使用锰和氧化铁的记录,尤其是在 60-40 千年前。这些发现通常被解释为颜料,尽管其确切用途在很大程度上仍是未知的。在这里,我们报告了更早的氧化铁发现,这些发现构成了尼安德特人最早有记录的使用赤铁矿的证据。这些发现是在荷兰贝尔维德雷的马斯特里赫特遗址挖掘过程中,从红色物质的小浓缩物中提取的。这些挖掘暴露了一系列保存完好的燧石文物(偶尔还有骨头)的散布物,它们是在晚更新世全间冰期的河谷环境中形成的。对红色物质的样本进行了各种形式的分析,以研究其物理性质。所有分析都将红色物质鉴定为赤铁矿。这是一种非本地材料,可能是从几十公里以外的地方带到该遗址的。马斯特里赫特-贝尔维德雷遗址的发现被鉴定为赤铁矿,这使得(早期)尼安德特人使用赤铁矿的时间大大提前,至少可以追溯到 20 万至 25 万年前(即与非洲记录中早期使用赤铁矿的时间范围相同)。