Zooarchaeological perspectives on the Chinese Early and Late Paleolithic from the Ma’anshan site (Guizhou, South China)
Introduction
The Chinese Paleolithic has been divided into two cultural stages, the Early and Late Paleolithic. This terminology contrasts with those commonly used in western Eurasia and Africa. The boundary between these periods in China conventionally is drawn at about 30–27 ka BP, based on the appearance in the latter of blade and microblade technology, formal bone tools, ornaments (Gao and Norton, 2002), or a combination of these. This study examines whether differences in the faunal assemblages from Ma’anshan Cave differ between the Chinese Early and Late Paleolithic as determined by the artifactual record. Zooarchaeological and taphonomic studies of Chinese Paleolithic sites are still few in number (e.g., Norton and Gao, 2008, Prendergast et al., 2009). Usually, only a species list is provided for the faunal assemblages, and there is little or no information on relative species abundance, frequencies of skeletal parts, prey mortality patterns or bone surface modification (e.g., Pei, 1940, Zhang, 1988). It has been almost impossible to distinguish between the Chinese early and late Paleolithic game use from such limited criteria.
Some of the Pleistocene bone collections for which species lists are available are housed in the Institute of Vertebrate Palaeontology and Paleoanthropology (IVPP) in Beijing. Of these, the Ma’anshan collections are very suitable for re-examination because of the recovery of all specimens, including microfauna and long bone mid-shaft fragments of large animals. The cave of Ma’anshan yielded thousands of bone fragments (the ratio of NISP to non-identified specimens is 4358/40,000) and artifacts. The ages of the assemblages range from 15 to 53 ka BP (Zhang, 1988, Zhang, 2001, Long, 1992). Though excavated under conditions that would not be considered optimal today, these collections nonetheless provide an important opportunity to examine whether differences exist between the faunal assemblages of the Chinese late Early Paleolithic and the Late Paleolithic at one location.
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Background
Ma’anshan Cave is located 2 km southeast of Tongzi County, northwest Guizhou Province (Fig. 1). The cave lies at an altitude of 960 m above modern sea level, and 40 m above the nearby Tianmen River. Its interior is 24 m long and narrows towards the back. The entrance faces northeast and is the widest part of the cave at 21 m across (Fig. 2).
Ma’anshan Cave was systematically excavated in 1986 and 1990 by the IVPP under the direction of Professor Zhang Senshui and Long Fengxiang. An area of 25 m2
Materials and methods
The Ma’anshan faunal assemblage contains roughly 40,000 faunal specimens. Only those specimens that could be identified to species and/or skeletal element are included in this study. Of the total macromammal NISP (4358), 2892 specimens are from the upper cultural layer and 1466 from the lower layer. About 17% of the identifiable remains from the upper layer are dental specimens (NISP 487), and 13% are dental specimens in the lower layer (NISP 189).
Four groups of observations were recorded for
Taphonomy and assemblage formation history
In the Ma’anshan site, the surfaces of some bones were destroyed by biological erosion, manganese or weathering. Most of the bone specimens have biological erosion marks (93.76% in the upper layer, 89.82% in the lower layer), with a dendritic pattern indicative of root action (Andrews and Cook, 1985, Binford, 1981). The marks are unevenly distributed among specimens, ranging from mild to severe. Heavy root damage is more common in the upper layer (80%) than in the lower layer (64%).
About 95% of
Prey species abundance
Fifteen large mammal genera (>10 kg) were identified, mainly from diagnostic teeth and antler specimens (Table 4). C. unicolor is the most common mammal in the upper layer. This species is also present in the lower cultural layer, but the much larger ungulate, Bubalus sp., dominates the assemblage. There therefore is a significant decrease in the mean body size of the mammals from the earlier to the later cultural period.
To explore differences in the relative importance of large, medium-sized,
Skeletal element representation
In order to compare the patterns of skeletal element representation among mammal body size classes in the two layers, bone elements are classified according to minimum anatomical units (MAU) and standardized as percentages of the most common element (Table 6, Fig. 8) following Binford (1978; see also review by Lyman, 1994). There are both similarities and differences between the skeletal element profiles of the upper and the lower layers. First, teeth generally are more common in both layers,
Mortality patterns
The most common technique for estimating a mammal’s age at death uses eruption and wear observations for deciduous and permanent teeth. In this study, occlusal wear is measured as the crown height, corrected for individual differences in tooth breadth, and by following standard wear stages (Brown and Chapman, 1991, Grimsdell, 1973, Hillman-Smith et al., 1986, Haynes, 1987, Haynes, 1991; reviewed by Hillson, 1986:205–256). Unfortunately, all the teeth from Ma’anshan are isolated from the jaws.
Concluding discussion
The analyses of species abundance, skeletal element representation, cut marks, and mortality patterns indicate that the occupants of the upper layer in Ma’anshan Cave hunted mainly medium-sized ungulate prey. The hunters brought meaty parts of their prey back to a base camp, where they defleshed both limbs and ribs with equal energy, and probably were more likely to roast these parts than the earlier hominids. To the extent that ribs are present in the lower layer, defleshing efforts were
Acknowledgments
We are grateful to Zhang Senshui, Long Fengxiang, An Jiayuan, Wang Xinjin and Cai Huiyang who excavated the Ma’anshan site in 1986 and 1990, appreciate the help from Qi Guoqin, Zhang Zhaoqun, Deng Tao, Tong Haowen and Liu Jinyi in identifying the bones, and also thank Christopher J. Norton, who provided the model of the Access data base. Supported by National Basic Research Program of China (Grant No. 2006CB806400), International Cooperation Program of MST of China (Grant No. 2007DFB20330), and
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