Institute for Human Evolution, University of the Witwatersrand, WITS 2050, Johannesburg, South Africa.
J Hum Evol. 2009 Dec;57(6):688-96. doi: 10.1016/j.jhevol.2009.05.014. Epub 2009 Aug 15.
We report on new research at Swartkrans Cave, South Africa, that provides evidence of two previously unrealized artifact- and fossil-bearing deposits. These deposits underlie a speleothem dated by the uranium-thorium disequilibrium technique to 110,000+/-1,980 years old, the first tightly constrained, geochronological date available for the site. Recovered fauna from the two underlying deposits-including, prominently, the dental remains of Paranthropus (Australopithecus) robustus from the uppermost layer (Talus Cone Deposit)-indicate a significantly older, late Pliocene or early Pleistocene age for these units. The lowest unit (LB East Extension) is inferred to be an eastward extension of the well-known Lower Bank of Member 1, the earliest surviving infill represented at the site. The date acquired from the speleothem also sets the maximum age of a rich Middle Stone Age lithic assemblage.
我们报告了南非斯瓦特克朗斯洞穴的新研究成果,该研究提供了两个以前未被发现的含有文物和化石的矿床的证据。这些矿床位于一个由铀-钍不平衡技术测定的年龄为 110,000+/-1,980 年的钟乳石之下,这是该遗址提供的第一个严格约束的地质年代日期。从两个下部矿床中回收的动物群——特别是最上层(塔勒斯圆锥体矿床)的粗壮南方古猿(南方古猿)的牙齿遗骸——表明这些地层的年龄要早得多,属于上新世晚期或更新世早期。最底层单元(LB 东延伸)被推断为著名的 1 号成员下岸的向东延伸部分,这是该遗址最早幸存的填充物。从钟乳石中获得的日期也确定了丰富的中石器时代石器组合的最大年龄。