| Publication: | ||
| Miura, Hideki and Maemoku, Hideaki and Seto, Koji and Moriwaki, Kiichi and others Late Quaternary East Antarctic melting event in the Soya Coast region based on stratigraphy and oxygen isotopic ratio of fossil molluscs Polar Geoscience, 1998 DOI: None |
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| The following sites appear in this publication: | |
| Langhovde-N. Kominato E-trench (7 samples) | |
| Langhovde-S. Yatude terrace (1 samples) | |
| Yatude Valley (6 samples) | |
| Yukidori Valley (1 samples) | |
| Skarvsness Kizahasi Beach (12 samples) | |
| The following samples appear in this publication: | |||||||
| ID | Latitude | Longitude | Past sea level (m) | What | Constraint type | C14 age | |
| 1 | -69.19 | 39.65 | 12.2 ± 2.0 | Shell in-situ | 1 | 4920.0 ± 60.0 | |
| 2 | -69.19 | 39.65 | 12.1 ± 2.0 | Shell in-situ | 1 | 4850.0 ± 60.0 | |
| 3 | -69.19 | 39.65 | 12.2 ± 2.0 | Shell in-situ | 1 | 5270.0 ± 60.0 | |
| 4 | -69.19 | 39.65 | 12.1 ± 2.0 | Shell in-situ | 1 | 4350.0 ± 70.0 | |
| 5 | -69.19 | 39.65 | 12.1 ± 2.0 | Shell in-situ | 1 | 4900.0 ± 60.0 | |
| 6 | -69.19 | 39.65 | 12.0 ± 2.0 | Shell in-situ | 1 | 5000.0 ± 50.0 | |
| 7 | -69.19 | 39.65 | 11.8 ± 2.0 | Shell in-situ | 1 | 5070.0 ± 50.0 | |
| 8 | -69.26 | 39.65 | 19.0 ± 2.0 | Shell in-situ | 1 | 6810.0 ± 60.0 | |
| 9 | -69.26 | 39.65 | 7.4 ± 2.0 | Shell in-situ | 1 | 4180.0 ± 50.0 | |
| 10 | -69.26 | 39.65 | 7.0 ± 2.0 | Shell in-situ | 1 | 5820.0 ± 80.0 | |
| 11 | -69.26 | 39.65 | 4.7 ± 2.0 | Shell in-situ | 1 | 4780.0 ± 60.0 | |
| 12 | -69.26 | 39.65 | 3.1 ± 2.0 | Shell in-situ | 1 | 3170.0 ± 70.0 | |
| 13 | -69.26 | 39.65 | 3.2 ± 2.0 | Shell in-situ | 1 | 3440.0 ± 50.0 | |
| 14 | -69.26 | 39.65 | 3.0 ± 2.0 | Shell in-situ | 1 | 3890.0 ± 50.0 | |
| 15 | -69.26 | 39.65 | 12.0 ± 2.0 | Shell in-situ | 1 | 4280.0 ± 90.0 | |
| 16 | -69.47 | 39.57 | 5.7 ± 2.0 | Shell in-situ | 1 | 4260.0 ± 60.0 | |
| 17 | -69.47 | 39.57 | 6.8 ± 2.0 | Shell in-situ | 1 | 4060.0 ± 60.0 | |
| 18 | -69.47 | 39.57 | 7.4 ± 2.0 | Shell in-situ | 1 | 4400.0 ± 70.0 | |
| 19 | -69.47 | 39.57 | 7.5 ± 2.0 | Shell in-situ | 1 | 4380.0 ± 50.0 | |
| 20 | -69.47 | 39.57 | 8.0 ± 2.0 | Shell in-situ | 1 | 4430.0 ± 60.0 | |
| 21 | -69.47 | 39.57 | 7.9 ± 2.0 | Shell in-situ | 1 | 4560.0 ± 60.0 | |
| 22 | -69.47 | 39.57 | 10.0 ± 2.0 | Shell in-situ | 1 | 4670.0 ± 60.0 | |
| 23 | -69.47 | 39.57 | 10.7 ± 2.0 | Shell in-situ | 1 | 4860.0 ± 60.0 | |
| 24 | -69.47 | 39.57 | 11.8 ± 2.0 | Shell in-situ | 1 | 4910.0 ± 50.0 | |
| 25 | -69.47 | 39.57 | 11.8 ± 2.0 | Shell in-situ | 1 | 5190.0 ± 60.0 | |
| 26 | -69.47 | 39.57 | 14.3 ± 2.0 | Shell in-situ | 1 | 5290.0 ± 70.0 | |
| 27 | -69.47 | 39.57 | 18.0 ± 2.0 | Shell in-situ | 1 | 7170.0 ± 60.0 | |
