Bischoff J L, Fitzpatrick J A, León L, Arsuagà J L, Falgueres C, Bahain J J, Bullen T
U.S. Geological Survery, Menlo Park, California 94025, USA.
J Hum Evol. 1997 Aug-Sep;33(2-3):129-54. doi: 10.1006/jhev.1997.0130.
Sediments of the Sima de los Huesos vary greatly over distances of a few meters. This is typical of interior cave facies, and caused by cycles of cut and fill. Mud breccias containing human bones, grading upwards to mud containing bear bones, fill an irregular surface cut into basal marks and sands. The lack of Bedding and the chaotic abundance of fragile speleothem clasts in the fossiliferous muds suggests that the deposit was originally a subterranean pond facies, and that after emplacement of the human remains, underwent vigorous post-depositional rotation and collapse and brecciation, caused by underlying bedrock dissolution and undermining. The fossiliferous deposits are capped by flowstone and guano-bearing muds which lack large-mammal fossils. U-series and radiocarbon dating indicates the capping flowstones formed from about 68 ka to about 25 ka. U-series analyses of speleothem clasts among the human fossils indicate that all are at, or close to, isotopic equilibrium (> 350 ka). The distribution of U-series dates for 25 bear bones (154 +/- 66 ka) and for 16 human bones (148 +/- 34 ka) is similar and rather broad. Because the human bones seem to be stratigraphically older than chose of the bears, the results would indicate that most of the bones have been accumulating uranium irregularly with time. Electron spin resonance (ESR) analyses of six selected bear bones indicates dates of 189 +/- 28 ka, for which each is cordant with their corresponding U-series date (181 +/- 41 ka). Combined ESR and U-series dates for these samples yielded 200 +/- 4 ka. Such agreement is highly suggestive that uranium uptake in these bones was close to the early-uptake (EU) model, and the dates are essentially correct. Another three selected samples yielded combined ESR U-series dates of 320 +/- 4 ka with a modeled intermediate-mode of uranium uptake. The dating results, therefore, seem to provide a firm minimum age of about 200 ka for the human entry: and suggestive evidence of entry before 320 ka.
休索斯洞穴沉积层在几米的范围内变化很大。这是洞穴内部相的典型特征,是由切割和填充循环造成的。含有人类骨骼的泥质角砾岩向上逐渐变为含有熊骨骼的泥质,填充在切入基底痕迹和砂岩的不规则表面中。含化石泥中缺乏层理以及易碎的洞穴沉积物碎屑的混乱堆积表明,该沉积物最初是地下池塘相,在人类遗骸安置之后,由于下伏基岩的溶解和侵蚀,经历了强烈的沉积后旋转、坍塌和角砾化过程。含化石沉积物被流石和含鸟粪的泥质覆盖,这些泥质中没有大型哺乳动物化石。铀系和放射性碳测年表明,覆盖层流石形成于约68千年前至约25千年前。对人类化石中的洞穴沉积物碎屑进行的铀系分析表明,所有碎屑都处于或接近同位素平衡状态(>350千年前)。25块熊骨(154±66千年前)和16块人类骨骼(148±34千年前)的铀系测年结果分布相似且范围较宽。由于人类骨骼在地层上似乎比熊的骨骼更古老,结果表明大多数骨骼随时间不规则地积累了铀。对六块选定的熊骨进行的电子自旋共振(ESR)分析得出的年代为189±28千年前,每一个都与其对应的铀系年代(181±41千年前)一致。这些样本的ESR和铀系联合年代为200±4千年前。这种一致性强烈表明这些骨骼中的铀吸收接近早期吸收(EU)模型,并且年代基本正确。另外三个选定样本的ESR铀系联合年代为320±4千年前,模拟的铀吸收模式为中间模式。因此,测年结果似乎为人类进入提供了一个确定的最小年龄约为200千年前:并暗示了在320千年前之前进入的证据。