Department of Biology, College of Arts and Sciences, Howard University, Washington, D.C, 20059, USA.
W. Montague Cobb Research Laboratory, College of Arts and Sciences, Howard University, Washington, D.C., 20059, USA.
Sci Rep. 2019 Dec 12;9(1):18976. doi: 10.1038/s41598-019-55125-7.
The New York African Burial Ground (NYABG) is the country's oldest and largest burial site of free and enslaved Africans. Re-discovered in 1991, this site provided evidence of the biological and cultural existence of a 17 and 18 Century historic population viewing their skeletal remains. However, the skeletal remains were reburied in October 2003 and are unavailable for further investigation. The analysis of grave soil samples with modern technology allows for the assessment of trace metal presence. Portable X-ray fluorescence (pXRF) spectrometry provides a semi-quantitative and non-destructive method to identify trace metals of this population and in the surrounding environment. Sixty-five NYABG soil samples were analyzed on a handheld Bruker Tracer III- SD XRF with 40 kV of voltage and a 30μA current. Presence of As, Cu, and Zn can potentially decipher the influence of the local 18 Century pottery factories. Elevated levels of Sr validate the assumed heavy vegetative diets of poor and enslaved Africans of the time. Decreased levels of Ca may be due in part to the proximity of the Collect Pond, the existing water table until the early 19 Century, and Manhattan's rising sea level causing an elevated water table washing away the leached Ca from human remains. These data help us reconstruct the lives of these early Americans in what became New York City.
纽约非洲裔公墓(NYABG)是美国历史最悠久、最大的自由和被奴役的非洲人墓地。该墓地于 1991 年重新被发现,其出土的骨骼遗骸为人们了解 17 至 18 世纪的历史人口的生物和文化存在提供了证据。然而,这些骨骼遗骸已于 2003 年 10 月重新被埋葬,无法进行进一步的调查。利用现代技术分析墓地土壤样本,可以评估痕量金属的存在。便携式 X 射线荧光(pXRF)光谱分析提供了一种半定量和非破坏性的方法,可以识别该人群和周围环境中的痕量金属。使用 Bruker Tracer III-SD XRF 手持设备对 65 个 NYABG 土壤样本进行了分析,仪器的电压为 40kV,电流为 30μA。As、Cu 和 Zn 的存在可能可以揭示当地 18 世纪陶瓷厂的影响。Sr 的升高水平验证了当时贫穷和被奴役的非洲人大量食用植物性食物的假设。Ca 的减少可能部分是由于集水池的存在,该集水池一直是当时的地下水位,直到 19 世纪早期,以及曼哈顿不断上升的海平面导致水位升高,冲走了从人类遗骸中浸出的 Ca。这些数据帮助我们重建了这些早期美国人在后来成为纽约市的地方的生活。