Table 1. Data used to construct the age model of the sediment core investigated in this study, M40/4_SL71 (reproduced from [29]), and to adjust the age model of the comparative core M51/3_SL110 [10].
| Core | Depth (cm) | Age (cal ka BP) | Datum |
|---|---|---|---|
| SL71 | 0.00 | 0.000 | sediment surface |
| SL71 | 2.50 | 0.2 | δ18O record |
| SL71 | 4.75 | 1.935 ± 0.165 | AMS 14C |
| SL71 | 13.25 | 6.865 ± 0.165 | AMS 14C |
| SL71 | 15.00 | 7.8 | δ18O record |
| SL71 | 20.25 | 10.825 ± 0.265 | AMS 14C |
| SL71 | 35.00 | 17.9 | δ18O record |
| SL71 | 36.25 | 18.790 ± 0.120 | AMS 14C |
| SL71 | 50.25 | 25.540 ± 0.390 | AMS 14C |
| SL71 | 84.00 | 39.280 ± 0.110 | Top Y5 –Tephra |
| SL71 | 88.00 | 39.280 ± 0.110 | Base Y5—Tephra |
| SL71 | 100.00 | 50.2 | δ18O record |
| SL71 | 127.50 | 56.1 | δ18O record |
| SL71 | 147.50 | 67.2 | δ18O record |
| SL71 | 157.50 | 70.7 | δ18O record |
| SL71 | 177.50 | 77.5 | δ18O record |
| SL71 | 192.50 | 86.5 | δ18O record |
| SL71 | 215.50 | 96.4 | δ18O record |
| SL71 | 227.50 | 103.3 | δ18O record |
| SL71 | 239.50 | 114.3 | δ18O record |
| SL71 | 270.34 | 124.0 | δ18O record |
| SL71 | 286.80 | 130.0 | δ18O record |
| SL71 | 291.73 | 135.1 | δ18O record |
| SL71 | 305.55 | 139.9 | δ18O record |
| SL71 | 346.79 | 153.0 | δ18O record |
| SL71 | 366.48 | 155.9 | δ18O record |
| SL71 | 388.83 | 167.0 | δ18O record |
| SL71 | 414.47 | 174.0 | δ18O record |
| SL71 | 425.08 | 185.0 | δ18O record |
| SL71 | 465.49 | 192.0 | δ18O record |
| SL110 | 0.00 | 0.000 | Sediment surface |
| SL110 | 34.50 | 6.43 | AMS14C |
| SL110 | 64.50 | 11.53 | AMS14C |
| SL110 | 113.50 | 17.8 | δ18O record |
| SL110 | 150.50 | 24.4 | AMS14C |
| SL110 | 234.50 | 33.9 | AMS14C |
| SL110 | 464.50 | 66.0 | δ18O record |
| SL110 | 529.50 | 86.9 | δ18O record |
| SL110 | 579.00 | 108.9 | δ18O record |
| SL110 | 598.00 | 115.0 | Hiatus end |
| SL110 | 598.00 | 121.7 | Hiatus start |
| SL110 | 603.00 | 124.0 | Base S5 |
| SL110 | 629.50 | 134.9 | δ18O record |