The 100,000–77,000-Year Old Middle Stone Age Micromammal Sequence from Blombos Cave, South Africa: Local Climatic Stability or a Tale of Predator Bias?

被引:0
作者
Turid Hillestad Nel
Christopher Stuart Henshilwood
机构
[1] University of Bergen,SFF Centre for Early Sapiens Behaviour (SapienCE)
[2] University of the Witwatersrand,Evolutionary Studies Institute
来源
African Archaeological Review | 2021年 / 38卷
关键词
Micromammals; Middle stone age; Palaeoenvironment; Blombos cave;
D O I
暂无
中图分类号
学科分类号
摘要
In this paper, we present a case study of the micromammal sequence from Marine Isotope Stage 5 (130,000–71,000 YBP) at Blombos Cave on the southern Cape coast of South Africa. Our analyses of the micromammal assemblage from 100,000 to 76,000 YBP shed light on micromammal taxonomic distributions, local palaeoenvironments, and site formation processes at this renowned Middle Stone Age site. Taphonomic analyses indicate that spotted eagle owls (Bubo africanus) were the main predator species responsible for accumulating the micromammals, but with contributions from barn owls (Tyto alba). In addition, the micromammal bones have been subjected to a range of post-depositional processes, some of which are associated with microbial actions likely resulting from human or animal activities in the cave. We have recorded three species in the archaeological assemblage that do not occur in the Blombos area today. These are the Hottentot golden mole (Amblysomus hottentotus), Duthie’s golden mole (Chlorotalpa duthieae), and Laminate vlei rat (Otomys laminatus). The biodiversity indices based on micromammal species suggest that local vegetation consisted of different habitats that could sustain a diverse small mammal population. During MIS 5c/5b, the diversity of species declined, but there was still a mosaic of vegetation habitats present in the local area. On a larger temporal scale, climate conditions were slightly more humid than at present, and winter rainfall was seemingly greater. The amount of winter rainfall would have been similar to locations currently c. 50–150 km further west of Blombos Cave. However, based on micromammal proxies, there were seemingly no major fluctuations visible in climate or vegetation composition during the entire 24,000-year period. We suggest that the explanation could be multifaceted, two potential factors being predator bias derived from the owls’ preference for generalist micromammal species or an actual reflection of local stable climatic and environmental conditions in the Blombos area.
引用
收藏
页码:443 / 476
页数:33
相关论文
共 302 条
[1]  
Andrews P(1983)Small mammal bone accumulations produced by mammalian carnivores Paleobiology 9 289-307
[2]  
Evans EN(1982)Micromammals as palaeoenvironmental indicators and an interpretation of the late Quaternary in the southern Cape Province, South Africa Annals of the South African Museum 85 183-377
[3]  
Avery D(1987)Late Pleistocene coastal environment of the Southern Cape province of South Africa: Micromammals from Klasies River Mouth Journal of Archaeological Science 14 405-421
[4]  
Avery DM(1992)Ecological data on micromammals collected by barn owls Tyto alba in the West Coast National Park, South Africa Israel Journal of Ecology and Evolution 38 385-397
[5]  
Avery DM(1992)Micromammals and the environment of early pastoralists at Spoeg River, western Cape Province, South Africa The South African Archaeological Bulletin 47 116-121
[6]  
Avery DM(2001)The Plio-Pleistocene vegetation and climate of Sterkfontein and Swartkrans, South Africa, based on micromammals Journal of Human Evolution 41 113-132
[7]  
Avery DM(2002)Taphonomy of micromammals from cave deposits at Kabwe (Broken Hill) and Twin Rivers in Central Zambia Journal of Archaeological Science 29 537-544
[8]  
Avery DM(2007)Micromammals as palaeoenvironmental indicators of the southern African Quaternary Transactions of the Royal Society of South Africa 62 17-23
[9]  
Avery DM(2005)Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli) Journal of Natural History 39 2047-2071
[10]  
Avery DM(2010)A high resolution and continuous isotopic speleothem record of paleoclimate and paleoenvironment from 90 to 53 ka from Pinnacle Point on the south coast of South Africa Quaternary Science Reviews 29 2131-2145