前处理与测试条件差异对化石牙釉质羟磷灰石稳定同位素数据的影响：以步氏巨猿动物群为例
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姜曲怡, 赵凌霞, 胡耀武
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Isotopic (C, O) variations of fossil enamel bioapatite caused by different preparation and measurement protocols: a case study of Gigantopithecus fauna
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JIANG Qu-Yi, ZHAO Ling-Xia, HU Yao-Wu
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Table 1 Results of δ13C and δ18O values in Zhao et al. (2011), Nelson (2014) and this study (VPDB, ‰)
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| Number | Number (original) | Species | δ13C (our study) | δ13C (Nelson, 2014) | δ13C (Zhao et al., 2011) | δ18O (Nelson, 2014) | δ18O (our study) | | 1 | 1 | Leptobos sp. | -15.4 | -14.4 | -15.8 | -9.7 | -9.9 | | 2 | 2 | Leptobos sp. | -15.2 | -14.5 | -15.4 | -9.3 | -9.6 | | 3 | 3 | Leptobos sp. | -16.7 | -15.8 | -17.1 | -9.3 | -9.6 | | 4 | 4 | Leptobos sp. | -15.0 | -14.3 | -15.3 | -7.2 | -7.2 | | 5 | 5 | Cervus sp. | -16.5 | -15.5 | -16.8 | -5.7 | -5.7 | | 6 | 6 | Cervus sp. | -17.4 | -16.5 | -17.8 | -7.6 | -7.7 | | 7 | 7 | Cervus sp. | -14.9 | -14.1 | -15.5 | -6.4 | -6.2 | | 8 | 8 | Tapirus sinensis | -15.9 | -15.0 | -16.6 | -10.4 | -10.1 | | 9 | 9 | Tapirus sinensis | -17.1 | -16.2 | -17.7 | -10.9 | -10.8 | | 10 | 10 | Tapirus sinensis | -15.6 | -15.1 | -16.3 | -9.2 | -9.4 | | 11 | 11 | Tapirus sinensis | -15.8 | -15.7 | -16.1 | -12.2 | -11.3 | | 12 | 12 | Rhinoceros sinensis | -14.0 | -13.8 | -14.4 | -9.7 | -10.0 | | 13 | 13 | Rhinoceros sinensis | -15.6 | -15.3 | -15.8 | -10.0 | -10.4 | | 14 | 14 | Rhinoceros sinensis | -14.6 | -14.1 | -14.9 | -6.4 | -6.1 | | 15 | 15 | Rhinoceros sinensis | -15.5 | -15.2 | -15.8 | -9.4 | -9.1 | | 16 | 16 | Pachycrocuta licenti | -13.8 | -13.7 | -14.1 | -9.8 | -9.1 | | 17 | 18 | Ailuropoda wulingshanensis | -17.9 | -16.7 | -18.3 | -7.7 | -7.2 | | 18 | 23 | Gigantopithecus blacki | -16.7 | -15.6 | -17.2 | -9.4 | -9.5 | | 19 | 24 | Gigantopithecus blacki | -15.4 | -15.4 | -15.9 | -9.2 | -9.2 | | 20 | 25 | Gigantopithecus blacki | -17.4 | -16.6 | -18.2 | -8.1 | -8.7 | | 21 | 26 | Gigantopithecus blacki | -13.7 | -12.1 | -14.2 | -10.5 | -9.5 |
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