Zhu Zhao-Yu, Dennell Robin, Huang Wei-Wen, Wu Yi, Rao Zhi-Guo, Qiu Shi-Fan, Xie Jiu-Bing, Liu Wu, Fu Shu-Qing, Han Jiang-Wei, Zhou Hou-Yun, Ou Yang Ting-Ping, Li Hua-Mei
Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China.
Department of Archaeology, University of Exeter, Exeter, United Kingdom.
J Hum Evol. 2015 Jan;78:144-57. doi: 10.1016/j.jhevol.2014.10.001. Epub 2014 Nov 20.
The Homo erectus cranium from Gongwangling, Lantian County, Shaanxi Province is the oldest fossil hominin specimen from North China. It was found in 1964 in a layer below the Jaramillo subchron and was attributed to loess (L) L15 in the Chinese loess-palaeosol sequence, with an estimated age of ca. 1.15 Ma (millions of years ago). Here, we demonstrate that there is a stratigraphical hiatus in the Gongwangling section immediately below loess 15, and the cranium in fact lies in palaeosol (S) S22 or S23, the age of which is ca. 1.54-1.65 Ma. Closely spaced palaeomagnetic sampling at two sections at Gongwangling and one at Jiacun, 10 km to the north, indicate that the fossil layer at Gongwangling and a similar fossil horizon at Jiacun were deposited shortly before a short period of normal polarity above the Olduvai subchron. This is attributed to the Gilsa Event that has been dated elsewhere to ca. 1.62 Ma. Our investigations thus demonstrate that the Gongwangling cranium is slightly older than ca. 1.62 Ma, probably ca. 1.63 Ma, and significantly older than previously supposed. This re-dating now makes Gongwangling the second oldest site outside Africa (after Dmanisi) with cranial remains, and causes substantial re-adjustment in the early fossil hominin record in Eurasia.
陕西省蓝田县公王岭的直立人头骨是华北地区最古老的古人类化石标本。它于1964年在贾拉米洛亚时层之下的一层中被发现,并被归入中国黄土 - 古土壤序列中的黄土(L)L15,估计年龄约为115万年(百万年前)。在此,我们证明在公王岭剖面中,紧挨着黄土15之下存在地层间断,实际上该头骨位于古土壤(S)S22或S23层中,其年龄约为154 - 165万年。在公王岭的两个剖面以及向北10公里处的家村的一个剖面进行的密集古地磁采样表明,公王岭的化石层和家村的一个类似化石层位是在奥杜威亚时层之上的一段短暂正极性期之前不久沉积的。这归因于吉尔萨事件,在其他地方测定该事件的年代约为162万年。我们的研究因此表明,公王岭头骨比约162万年稍早,可能约为163万年,且比之前认为的要古老得多。这次重新测定年代现在使公王岭成为非洲以外(仅次于德马尼西)第二个有头骨化石的最古老遗址,并导致欧亚大陆早期古人类化石记录的大幅重新调整。