Geology & Geochemistry Cluster, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands.
CLUE+, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands.
Rapid Commun Mass Spectrom. 2022 May 30;36(10):e9277. doi: 10.1002/rcm.9277.
Strontium isotope ( Sr/ Sr) analysis of skeletal remains has become a powerful tool in archaeological studies of human migration and mobility. Owing to its resistance to post-mortem alteration, dental enamel is the preferred sampling material used for Sr/ Sr analysis in bioarchaeological provenance research, although recent studies have demonstrated that cremated bone is also generally resistant to diagenesis. This paper presents the results of a pilot study exploring the potential of unburnt petrous bone (pars petrosa) as a reservoir of biogenic (diagenetically unaltered) strontium, as the otic capsule or bony labyrinth within the petrous bone is extremely dense and is thought to be unable to remodel after early childhood, potentially providing an alternative for dental enamel.
From an individual from a colonial-era (18th century) site on the island of Saba in the Caribbean for whom previous enamel Sr/ Sr results had indicated non-local origins, multiple locations (n = 4) on the petrous were sampled and measured for strontium isotope composition. Saba (13 km ) has been extensively mapped for baseline strontium isotopes (n = 50) with Sr/ Sr varying from ca 0.7065 to 0.7090, whereas enamel Sr/ Sr (n = 3) ranged from 0.7104 to 0.7112.
All four petrous Sr/ Sr ratios (0.7111-0.7122) are consistently and considerably higher than the local bioavailable range, and very similar to the enamel Sr/ Sr. These results provide initial evidence that unburnt petrous bones may preserve biogenic strontium, at least in this specific burial context.
While more research in diverse burial conditions is needed to validate this observation, if confirmed, it would have broader implications for sample selection strategies in bioarchaeological studies using the strontium isotope method.
骨骼锶同位素(Sr/Sr)分析已成为考古学研究人类迁移和流动性的有力工具。由于其耐死后变化,牙釉质是生物考古学起源研究中用于 Sr/Sr 分析的首选采样材料,尽管最近的研究表明,火化后的骨骼通常也不易发生变化。本文介绍了一项探索未燃烧的岩骨(岩骨部分)作为生物成因(未发生变化的)锶储层潜力的初步研究结果,因为岩骨内的耳骨或骨迷路非常密集,并且据认为在幼儿期后无法重塑,这可能为牙釉质提供了一种替代物。
从加勒比地区萨巴岛(Saba)一个殖民时期(18 世纪)遗址的个体身上采集了多个岩骨部位(n=4)进行锶同位素组成测量,该个体的牙釉质 Sr/Sr 先前的结果表明其起源于非本地。萨巴岛(13 公里)已经对基线锶同位素进行了广泛的测绘(n=50),Sr/Sr 从 ca 0.7065 到 0.7090 不等,而牙釉质 Sr/Sr(n=3)范围从 0.7104 到 0.7112。
所有四个岩骨 Sr/Sr 比值(0.7111-0.7122)都明显且一致地高于当地生物可利用范围,且与牙釉质 Sr/Sr 非常相似。这些结果初步证明未燃烧的岩骨可能保留生物成因的锶,至少在这种特定的埋葬环境中是如此。
虽然需要在更多的多样化埋葬条件下进行研究来验证这一观察结果,但如果得到证实,这将对使用锶同位素方法的生物考古学研究中的样本选择策略产生更广泛的影响。