Sample number | Core | Depth (cm) | Material | Conventional radiocarbon age (yrBP) | Calibrated age (2σ) cal BP | δ13C (‰) |
---|---|---|---|---|---|---|
1 | NM2 | 30–32 | Organic sediment | 1910 ± 30 | 1920–1815 | − 27.2 |
2 | NM8 | 25–27 | Organic sediment | 2100 ± 30 | 2150–1995 | − 27.0 |
3 | NM-D | 35–37 | Organic sediment | 1740 ± 30 | 1715–1565 | − 27.6 |
4 | NM12 | 30–32 | Organic sediment | 2030 ± 30 | 2055–1900 | − 24.4 |
5 | NM-F | 17–19 | Organic sediment | 1910 ± 30 | 1920–1815 | − 26.9 |
6 | NM13 | 48–50 | Organic sediment | 2610 ± 30 | 2765–2730 | − 24.1 |
7 | NM-H | 21–23 | Organic sediment | 1940 ± 30 | 1945–1825 | − 27.6 |
8 | NM15 | 48–50 | Organic sediment | 2170 ± 30 | 2305–2070 | − 27.6 |
9 | NM-I | 41–43 | Organic sediment | 2000 ± 30 | 2000–1885 | − 27.3 |
10 | NM16 | 42–44 | Organic sediment | 2070 ± 30 | 2120–1950 | − 26.8 |
11 | NM17 | 50–52 | Organic sediment | 2000 ± 30 | 2000–1885 | − 26.8 |
12 | NM-K | 18–20 | Organic sediment | 1300 ± 30 | 1290–1180 | − 27.4 |
13 | NM-K | 30–32 | Organic sediment | 2050 ± 30 | 2115–1930 | − 26.6 |
14 | NM-K | 34–36 | Organic sediment | 2100 ± 30 | 2150–1995 | − 26.5 |
15 | NM-K | 40–42 | Organic sediment | 2170 ± 30 | 2305–2070 | − 26.2 |
16 | NM-K | 44–45 | Organic sediment | 2190 ± 30 | 2310–2120 | − 24.3 |
17 | NM-K | 51–53 | Organic sediment | 2480 ± 30 | 2720–2385 | − 25.2 |
18 | NM-K | 54–55 | Organic sediment | 2570 ± 30 | 2750–2710 | − 26.6 |
19 | NM18 | 25–27 | Organic sediment | 2150 ± 30 | 2300–2055 | − 26.9 |
20 | NM19 | 41–43 | Organic sediment | 2160 ± 30 | 2305–2065 | − 24.7 |