Table 1.
Paleohydroclimate records used in this study.
| Site number | Site name | Latitude (°N) | Longitude (°E) | Proxies | References |
|---|---|---|---|---|---|
| 1 | Lake Kaiike | 30.85 | 129.87 | Sediment δD | Soelen et al.22 |
| 2 | Mulyoungari Swamp | 33.37 | 126.68 | Pollen, diatom, δ13C, CN, TS | This study |
| 3 | Southern Okinawa Trough | 24.80 | 122.49 | Diatom | Li et al.75 |
| 4 | Dahu Lake | 24.75 | 121.70 | Pollen, diatom, grain size | Wang et al.68 |
| 5 | Tsuifong Lake | 24.50 | 121.60 | Diatom, δ15N, δ13C, magnetic susceptivility | Wang et al.67 |
| 6 | Lower Huai River and Yangtz River Basin | 32.36 | 117.84 | Historical documents | Man (2009)16 (as cited in ref. 25) |
| 7 | Jiang-Nan Area | 27.50 | 117.00 | Historical documents | Zheng et al.12 |
| 8 | Dongdao Island | 16.75 | 112.80 | Grain size | Yan et al.59 |
| 9 | Hainan Island | 19.30 | 110.67 | Coral δ13C and δ18O | Deng et al.76 |
| 10 | Huguangyan Maar Lake | 21.15 | 110.28 | TOC, TN, Sr | Zeng et al.19 |
| 11 | Lake San-No-Megata | 39.93 | 139.70 | Geochemical data, magnetic susceptibility | Yamada et al.18 |
| 12 | Xiaolongwan Lake | 42.30 | 126.35 | Sediment δ13C | Chu et al.15 |
| 13 | Maili Pond | 42.87 | 122.88 | Pollen | Ren (1998)11 |
| 14 | Kaiyuan Cave | 36.40 | 118.03 | Stalagmite δ18O | Wang et al.77 |
| 15 | Dali Lake | 43.26 | 116.60 | TOC | Xiao et al.54 |
| 16 | North China | 36.40 | 115.12 | Historical documents | Man (2009)16 (as cited in ref. 25) |
| 17 | Gonghai Lake | 38.90 | 112.23 | Geochemical data | Liu et al.20 |
| 18 | Heshang Cave | 30.45 | 110.42 | Stalagmite δ18O | Hu et al.51 |
| 19 | Dongge Cave | 25.28 | 108.08 | Stalagmite δ18O | Zhao et al.21 |
| 20 | Wanxiang Cave | 33.58 | 105.00 | Stalagmite δ18O | Zhang et al.14 |
| 21 | Longxi Area | 35.45 | 104.78 | Historical documents | Tan et al.13 |
Coastal sites showing the dry MCA/wet LIA pattern are indicated by bold numbers (1–10) while other sites are by italic numbers (11–21) (see Fig. 5 for the location of each site).