Official Journal of the Asia Oceania Geosciences Society (AOGS)
Sample no. | Labo no. | Sample position | Grid no. | Depth (m) | Material | δ13C (‰) | Conventional 14C age (yrBP) | Calibrated age (2σ) (calBP) | Remark |
---|---|---|---|---|---|---|---|---|---|
1 | IAAA-143084 | Above E3 | S-1.95 | 0.35–0.36 | Organic sediments | −24.63 ± 0.24 | 450 ± 20 | 530–490 (95.4%) | |
2 | IAAA-143085 | Above E3 | S-1.95 | 0.38–0.39 | Organic sediments | −23.94 ± 0.26 | 460 ± 20 | 530–490 (95.4%) | |
3 | IAAA-140938 | Above E3 | S-1.95 | 0.41–0.42 | Organic sediments | −23.22 ± 0.4 | 480 ± 20 | 540–500 (95.4%) | |
4a | IAAA-143086 | Below E3 | E-11.75 | 0.30–0.31 | Organic sediments | −25.6 ± 0.25 | 700 ± 20 | 690–650 (89.8), 590–570 (5.6%) | |
5a | IAAA-143087 | Below E3 | E-11.75 | 0.32–0.33 | Organic sediments | −24.29 ± 0.26 | 760 ± 20 | 730–660 (95.4%) | |
6a | IAAA-143088 | Below E3 | E-11.75 | 0.34–0.35 | Organic sediments | −26.5 ± 0.25 | 840 ± 20 | 790–700 (95.4%) | |
7 | IAAA-143089 | Above E4 | E-11.75 | 0.53–0.54 | Organic sediments | −25.45 ± 0.3 | 1270 ± 20 | 1270–1180 (95.4%) | |
8 | IAAA-143090 | Above E4 | E-11.75 | 0.56–0.57 | Organic sediments | −25.78 ± 0.25 | 1240 ± 20 | 1270–1170 (72.4%), 1160–1080 (23.0%) | |
9 | IAAA-140592 | Above E4 | E-11.75 | 0.59–0.60 | Organic sediments | −26.77 ± 0.61 | 1260 ± 20 | 1280–1170 (95.4%) | |
10a | IAAA-131321 | Below E4 | E-11.75 | 0.74–0.76 | Organic sediments | −25.78 ± 0.54 | 1420 ± 20 | 1350–1290 (95.4%) | Ishimura and Miyauchi (2015) |
11 | IAAA-143091 | Below E4 | E-11.75 | 0.78–0.79 | Organic sediments | −24.82 ± 0.38 | 1560 ± 20 | 1530–1400 (95.4%) | |
12a | IAAA-140939 | Below E7 | E-11.75 | 1.23–1.24 | Organic sediments | −24.16 ± 0.53 | 2570 ± 30 | 2760–2690 (77.5%), 2640–2610 (5.2%), 2590–2500 (12.7%) | |
13 | IAAA-140593 | Above E8 | E-11.75 | 1.31–1.32 | Organic sediments | −23.54 ± 0.58 | 2800 ± 30 | 2980–2840 (91.4%), 2830–2790 (4.0%) | |
14a | IAAA-140940 | Below E8 | E-11.75 | 1.35–1.36 | Organic sediments | −24.7 ± 0.44 | 2730 ± 30 | 2880–2760 (95.4%) | |
15a | IAAA-140594 | Below E3 | W-2.75 | 0.40–0.42 | Organic sediments | −26.51 ± 0.54 | 580 ± 20 | 650–580 (64.8%), 570–530 (30.6%) | |
16a | IAAA-140595 | E3/E4 | W-2.75 | 0.70–0.71 | Organic sediments | −29.54 ± 0.51 | 1060 ± 20 | 1050–1020 (6.9%), 990–920 (88.5%) | |
17 | IAAA-140596 | Above E4 | W-2.75 | 0.85–0.86 | Organic sediments | −28.6 ± 0.63 | 1500 ± 20 | 1480–1460 (0.5%), 1420–1330 (94.9%) | |
18a | IAAA-140941 | Below E4 | W-2.75 | 0.95–0.96 | Organic sediments | −21.66 ± 0.41 | 1600 ± 20 | 1550–1410 (95.4%) | |
19 | IAAA-140597 | Above E5 | W-2.75 | 1.11–1.12 | Organic sediments | −24.99 ± 0.51 | 1810 ± 20 | 1820–1690 (94.8%), 1650–1630 (0.6%) | |
20a | IAAA-140942 | Below E5 | W-2.75 | 1.19–1.20 | Organic sediments | −22.3 ± 0.61 | 1780 ± 20 | 1810–1610 (95.4%) | |
21 | IAAA-140598 | Above E6 | W-2.75 | 1.30–1.31 | Organic sediments | −26.58 ± 0.56 | 2040 ± 30 | 2120–2080 (6.9%), 2070–1920 (88.1%), 1910–1900 (0.4%) | |
22a | IAAA-140943 | Below E6 | W-2.75 | 1.39-1.40 | Organic sediments | −24.14 ± 0.54 | 2240 ± 20 | 2340–2290 (23.5%), 2270–2150 (71.9%) | |
23 | IAAA-140599 | Above E7 | W-2.75 | 1.46–1.47 | Organic sediments | −26.26 ± 0.59 | 2430 ± 30 | 2700–2630 (19.6%), 2620–580 (6.6%), 2540–2350 (69.2%) | |
24 | IAAA-140600 | Above E9 | W-2.75 | 1.66–1.67 | Organic sediments | −27.29 ± 0.36 | 2910 ± 30 | 3160–2960 (95.4%) | |
25a | IAAA-140944 | Below E9 | W-2.75 | 1.73–1.74 | Organic sediments | −26.94 ± 0.53 | 3040 ± 30 | 3350–3160 (95.4%) | |
26 | IAAA-140601 | Above E10 | W-2.75 | 1.87–1.88 | Organic sediments | −26.72 ± 0.36 | 3270 ± 30 | 3580–3440 (92.7%), 3430–3400 (2.7%) | |
27a | IAAA-140945 | Below E10 | W-2.75 | 1.92–1.93 | Organic sediments | −25.92 ± 0.55 | 3180 ± 30 | 3460–3350 (95.4%) | |
28 | IAAA-131669 | Above E11 | W-2.75 | 2.16–2.17 | Organic sediments | −23.53 ± 0.27 | 3500 ± 30 | 3860–3690 (95.4%) | Ishimura and Miyauchi (2015) |
29a | IAAA-140946 | Below E11 | W-2.75 | 2.25–2.26 | Organic sediments | −28.71 ± 0.52 | 3590 ± 30 | 3980–3830 (95.4%) |