Table 1.
Sample ID | Site | Layer | Age (kcal BP) | Stage | 87Sr/86Sr | 2SE± | 2SE± (%) |
SF-4 | Melikane | 1 | 0.3–0.15 | Late Holocene | 0.713080 | 0.000017 | 0.0023 |
SF-10 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.713242 | 0.000016 | 0.0016 |
SF-13 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.714967 | 0.000016 | 0.0016 |
SF-20 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.717149 | 0.000014 | 0.0020 |
SF-29 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.715892 | 0.000014 | 0.0020 |
SF-43 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.715753 | 0.000014 | 0.0019 |
SF-48 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.714822 | 0.000013 | 0.0018 |
SF-56 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.713849 | 0.000012 | 0.0017 |
SF-70 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.719894 | 0.000019 | 0.0026 |
SF-87 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.713054 | 0.000015 | 0.0021 |
SF-90 | Melikane | 2 | 3.3–0.15 | Late Holocene | 0.716775 | 0.000014 | 0.0019 |
SF-86 | Sehonghong | DC | 1.26–0.98 | Late Holocene | 0.715509 | 0.000013 | 0.0018 |
SF-101 | Sehonghong | DC | 1.26–0.98 | Late Holocene | 0.713296 | 0.000013 | 0.0017 |
J12-11B | Sehonghong | DC | 1.26–0.98 | Late Holocene | 0.714032 | 0.000012 | 0.0016 |
J12-11C | Sehonghong | DC | 1.26–0.98 | Late Holocene | 0.713137 | 0.000014 | 0.0019 |
SF-691 | Sehonghong | DC | 1.26–0.98 | Late Holocene | 0.714276 | 0.000014 | 0.0020 |
SF-174 | Sehonghong | ALP | 8.3–7.67 | Early Holocene | 0.716115 | 0.000012 | 0.0018 |
SF-231 | Sehonghong | ALP | 8.3–7.67 | Early Holocene | 0.714180 | 0.000013 | 0.0019 |
SF-265 | Sehonghong | ALP | 8.3–7.67 | Early Holocene | 0.714251 | 0.000014 | 0.0020 |
SF-267 | Sehonghong | ALP | 8.3–7.67 | Early Holocene | 0.715159 | 0.000018 | 0.0025 |
SF-751 | Sehonghong | ALP | 8.3–7.67 | Early Holocene | 0.716321 | 0.000014 | 0.0020 |
SF-430 | Sehonghong | BARF | 13.4–12.6 | Late Pleistocene | 0.755539 | 0.000012 | 0.0016 |
SF-430 replicate | Sehonghong | BARF | 13.4–12.6 | Late Pleistocene | 0.755541 | 0.000021 | 0.0028 |
SF-1090 | Sehonghong | RF | 15–13.7 | Late Pleistocene | 0.715643 | 0.000015 | 0.0021 |
SF-1091 | Sehonghong | RF | 15–13.7 | Late Pleistocene | 0.714490 | 0.000014 | 0.0020 |
SF-1092 | Sehonghong | RF | 15–13.7 | Late Pleistocene | 0.716109 | 0.000012 | 0.0017 |
SF-392 | Sehonghong | RBL-CRBLF | 15.7–15.2 | Late Pleistocene | 0.712252 | 0.000015 | 0.0021 |
I13-170 | Sehonghong | n/a | 33.7–31.9 | Late Pleistocene | 0.718649 | 0.000013 | 0.0018 |
Mean value for the Sr standard NBS 987: 87Sr/86Sr = 0.710250 ± 0.000016 (n = 16) Finnigan MAT 262; 87Sr/86Sr = 0.710245 ± 0.000014 (n = 11) Thermo Scientific Triton Plus. Accepted value of McArthur et al. (75) = 0.710248. n/a, not applicable (layers currently unassigned as this portion of the Sehonghong sequence remains under excavation).