{"title":"PhD Abstract","authors":"D. Witelson","doi":"10.1080/0067270x.2022.2156719","DOIUrl":null,"url":null,"abstract":"It has been proposed that the southernmost coast of South Africa was a uniquely important region in later human evolution, in part due to the abundance of nutritious and dense coastal resources. Yet, strong contrasts between its Middle Stone Age (MSA) and subsequent Later Stone Age (LSA) archaeological records cast uncertainty on the significance of shellfish utilisation for processes of human evolution. Furthermore, climatic shifts are frequently advanced as drivers of widespread technological change, but few climate proxy records correspond adequately to the archaeological evidence at a temporal or spatial level to allow them to be unambiguously linked to human cultural activity. This thesis presents a temporally and spatially distributed record of near-shore seasonal sea surface temperatures (SSTs) from serial δO shell measurements of archaeological Turbo sarmaticus opercula. In addition, the annual timing of shellfish harvesting captured in the temperature signal of the shells’ final few growth increments is indicative of hunter-gatherers’ scheduling of foraging behaviours and of their social organisation. A non-destructive method for evaluating the preservation of the original aragonitic shell carbonate using Fourier transform infrared spectrometry with an attenuated reflectance attachment is presented, allowing for robust SST reconstructions. Near-shore SST reconstructions are presented from the LSA levels of Nelson Bay Cave and Byneskranskop 1, along with new radiocarbon chronologies spanning the terminal Pleistocene and the Holocene, and from the MSA deposits at Pinnacle Point 5–6 and Klasies River Main site, dated to periods in Marine Isotope Stage (MIS) 5 and across the MIS5/4 transition. These reconstructions confirm the utility of near-shore SST records for terrestrial climate reconstructions, indicating shifts in summer rainfall during the Holocene and across MIS5/4. The annual timing of shellfish foraging is shown to be markedly different between the MSA and LSA, permitting more nuanced assessments of foraging behaviours within the MSA and LSA.","PeriodicalId":45689,"journal":{"name":"Azania-Archaeological Research in Africa","volume":null,"pages":null},"PeriodicalIF":1.1000,"publicationDate":"2022-12-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Azania-Archaeological Research in Africa","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/0067270x.2022.2156719","RegionNum":2,"RegionCategory":"历史学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"0","JCRName":"ARCHAEOLOGY","Score":null,"Total":0}
引用次数: 1
Abstract
It has been proposed that the southernmost coast of South Africa was a uniquely important region in later human evolution, in part due to the abundance of nutritious and dense coastal resources. Yet, strong contrasts between its Middle Stone Age (MSA) and subsequent Later Stone Age (LSA) archaeological records cast uncertainty on the significance of shellfish utilisation for processes of human evolution. Furthermore, climatic shifts are frequently advanced as drivers of widespread technological change, but few climate proxy records correspond adequately to the archaeological evidence at a temporal or spatial level to allow them to be unambiguously linked to human cultural activity. This thesis presents a temporally and spatially distributed record of near-shore seasonal sea surface temperatures (SSTs) from serial δO shell measurements of archaeological Turbo sarmaticus opercula. In addition, the annual timing of shellfish harvesting captured in the temperature signal of the shells’ final few growth increments is indicative of hunter-gatherers’ scheduling of foraging behaviours and of their social organisation. A non-destructive method for evaluating the preservation of the original aragonitic shell carbonate using Fourier transform infrared spectrometry with an attenuated reflectance attachment is presented, allowing for robust SST reconstructions. Near-shore SST reconstructions are presented from the LSA levels of Nelson Bay Cave and Byneskranskop 1, along with new radiocarbon chronologies spanning the terminal Pleistocene and the Holocene, and from the MSA deposits at Pinnacle Point 5–6 and Klasies River Main site, dated to periods in Marine Isotope Stage (MIS) 5 and across the MIS5/4 transition. These reconstructions confirm the utility of near-shore SST records for terrestrial climate reconstructions, indicating shifts in summer rainfall during the Holocene and across MIS5/4. The annual timing of shellfish foraging is shown to be markedly different between the MSA and LSA, permitting more nuanced assessments of foraging behaviours within the MSA and LSA.
有人提出,南非最南端的海岸在后来的人类进化中是一个独特的重要地区,部分原因是丰富的营养和密集的沿海资源。然而,其中石器时代(MSA)和随后的晚石器时代(LSA)考古记录之间的强烈对比,使人们对贝类利用对人类进化过程的重要性产生了不确定性。此外,气候变化经常被认为是广泛的技术变革的驱动因素,但很少有气候代理记录在时间或空间水平上与考古证据充分对应,从而使它们与人类文化活动明确联系起来。本文通过对古萨玛aticus opercula的δO壳序列测量,获得了近岸季节海表温度的时空分布记录。此外,贝壳最后几个生长增量的温度信号中捕获的贝类捕捞的年度时间指示了狩猎采集者的觅食行为和他们的社会组织安排。本文提出了一种非破坏性的方法来评估原始文石壳碳酸盐的保存情况,该方法使用带有衰减反射附加的傅里叶变换红外光谱法,允许稳健的海温重建。从Nelson Bay Cave和Byneskranskop 1的LSA水平重建近岸海表温度,以及跨越更新世和全新世的新放射性碳年代学,以及Pinnacle Point 5 - 6和Klasies River Main遗址的MSA沉积物,可追溯到海洋同位素阶段(MIS) 5和MIS5/4过渡时期。这些重建证实了近岸海温记录在陆地气候重建中的作用,表明了全新世和MIS5/4期间夏季降雨的变化。贝类的年度觅食时间在MSA和LSA之间有显著差异,这使得对MSA和LSA内的觅食行为进行更细致的评估成为可能。