Edwards Tara R, Armstrong Brian J, Birkett-Rees Jessie, Blackwood Alexander F, Herries Andy I R, Penzo-Kajewski Paul, Pickering Robyn, Adams Justin W
The Australian Archaeomagnetism Laboratory, Department of Archaeology and History, La Trobe University, Melbourne, Victoria, Australia.
Centre for Ancient Cultures, Faculty of Arts, Monash University, Clayton, Melbourne, Victoria, Australia.
PeerJ. 2019 Jan 14;7:e6202. doi: 10.7717/peerj.6202. eCollection 2019.
Bolt's Farm is a Plio-Pleistocene fossil site located within the southwestern corner of the UNESCO Hominid Fossil Sites of South Africa World Heritage Site. The site is a complex of active caves and more than 20 palaeokarst deposits or pits, many of which were exposed through the action of lime mining in the early 20th century. The pits represent heavily eroded cave systems, and as such associating the palaeocave sediments within and between the pits is difficult, especially as little geochronological data exists. These pits and the associated lime miner's rubble were first explored by palaeoanthropologists in the late 1930s, but as yet no hominin material has been recovered. The first systematic mapping was undertaken by Frank Peabody as part of the University of California Africa Expedition (UCAE) in 1947-1948. A redrawn version of the map was not published until 1991 by Basil Cooke and this has subsequently been used and modified by recent researchers. Renewed work in the 2000s used Cooke's map to try and relocate the original fossil deposits. However, Peabody's map does not include all the pits and caves, and thus in some cases this was successful, while in others previously sampled pits were inadvertently given new names. This was compounded by the fact that new fossil bearing deposits were discovered in this new phase, causing confusion in associating the 1940s fossils with the deposits from which they originated; as well as associating them with the recently excavated material. To address this, we have used a Geographic Information System (GIS) to compare Peabody's original map with subsequently published maps. This highlighted transcription errors between maps, most notably the location of Pit 23, an important palaeontological deposit given the recovery of well-preserved primate crania (, ) and partial skeletons of the extinct felid . We conducted the first drone and Differential Global Positioning System (DGPS) survey of Bolt's Farm. Using legacy data, high-resolution aerial imagery, accurate DGPS survey and GIS, we relocate the original fossil deposits and propose a definitive and transparent naming strategy for Bolt's Farm, based on the original UCAE Pit numbers. We provide datum points and a new comprehensive, georectified map to facilitate spatially accurate fossil collection for all future work. Additionally, we have collated recently published faunal data with historic fossil data to evaluate the biochronological potential of the various deposits. This suggests that the palaeocave deposits in different pits formed at different times with the occurrence of in some pits implying ages of <2.3 Ma, whereas more primitive suids () hint at a terminal Pliocene age for other deposits. This study highlights that Bolt's Farm contains rare South African terminal Pliocene fossil deposits and creates a framework for future studies of the deposits and previously excavated material.
博尔特农场是一个上新世 - 更新世化石遗址,位于南非世界遗产地联合国教科文组织人类化石遗址的西南角。该遗址是一个由活跃洞穴和20多个古岩溶沉积物或矿坑组成的复合体,其中许多是在20世纪初因石灰开采活动而暴露出来的。这些矿坑代表了严重侵蚀的洞穴系统,因此很难将矿坑内部和之间的古洞穴沉积物联系起来,尤其是因为几乎没有地质年代数据。这些矿坑和相关的石灰矿工碎石在20世纪30年代末首次被古人类学家探索,但至今尚未发现人类化石材料。第一次系统测绘是由弗兰克·皮博迪在1947 - 1948年作为加利福尼亚大学非洲探险队(UCAE)的一部分进行的。直到1991年,巴西尔·库克才出版了该地图的重新绘制版本,随后的研究人员对其进行了使用和修改。21世纪初的重新工作使用了库克的地图来尝试重新定位原始化石沉积物。然而,皮博迪的地图并没有包括所有的矿坑和洞穴,因此在某些情况下这是成功的,而在其他情况下,之前采样的矿坑被无意中赋予了新的名称。此外,在这个新阶段发现了新的含化石沉积物,这使得将20世纪40年代的化石与其来源的沉积物联系起来变得困难,同时也难以将它们与最近挖掘的材料联系起来。为了解决这个问题,我们使用了地理信息系统(GIS)来比较皮博迪的原始地图和随后出版的地图。这突出了地图之间的转录错误,最明显的是23号矿坑的位置,鉴于保存完好的灵长类颅骨( , )和已灭绝猫科动物的部分骨骼的发现,23号矿坑是一个重要的古生物学沉积物。我们对博尔特农场进行了首次无人机和差分全球定位系统(DGPS)测量。利用遗留数据、高分辨率航空图像、精确的DGPS测量和GIS,我们重新定位了原始化石沉积物,并基于原始UCAE矿坑编号为博尔特农场提出了一个明确且透明的命名策略。我们提供了基准点和一张新的全面的、地理校正地图,以便为未来所有工作进行空间精确的化石采集。此外,我们整理了最近发表的动物群数据和历史化石数据,以评估各种沉积物的生物年代学潜力。这表明不同矿坑中的古洞穴沉积物在不同时间形成,一些矿坑中出现的 意味着年龄小于230万年,而其他沉积物中更原始的猪科动物( )则暗示了上新世末期的年龄。这项研究强调博尔特农场包含罕见的南非上新世末期化石沉积物,并为该沉积物和先前挖掘材料的未来研究创建了一个框架。