Ziegler R, Dean D
Staatliches Museum für Naturkunde, Stuttgart, Germany.
J Hum Evol. 1998 May;34(5):469-84. doi: 10.1006/jhev.1998.0213.
In 1978 three well-preserved pieces of a fossil human cranium (i.e., fused parietals, occipital and temporal) were found in a gravel pit near the southwest German town of Reilingen. It was recovered, with an accompanying mammalian fauna, as a side-product of commercial gravel mining. The sample was sorted from the dredgings of a boat-mounted crane reaching to a depth of 28 m below the surface. Here we present the mammalian fauna and discuss its biostratigraphical relevance. The fauna represents a mixture of Holstein interglacial to Würm glacial species. The occurrence of Holsteinian faunal components is indicated by presence of the extinct beaver, Trogontherium. Given the good preservation of specimens found at the lowest levels we can rule out reworking. The accompanying fauna indicates a Holstein to Würm time span bracketing the fossil hominid population.
1978年,在德国西南部小镇赖林根附近的一个砾石坑中发现了三块保存完好的人类颅骨化石(即融合的顶骨、枕骨和颞骨)。它是在商业砾石开采的副产品中与伴生的哺乳动物群一起被发现的。该样本是从一艘船用起重机挖掘到地表以下28米深处的疏浚物中挑选出来的。在此,我们展示该哺乳动物群并讨论其生物地层学意义。该动物群代表了霍尔斯坦间冰期到武木冰期物种的混合。已灭绝的河狸——巨河狸的存在表明了霍尔斯坦动物群成分的出现。鉴于在最低层发现的标本保存完好,我们可以排除再沉积的可能性。伴生的动物群表明化石人类种群的时间跨度为霍尔斯坦期到武木期。