R Marine Isotope Stage 6
Climatostratigraphic > StageOccurrences
| VS | Scientific Name | Archipelago | Island | Location | Min/Max Age |
|---|
Stratigraphy Data
| Designation | Marine Isotope Stage 6 |
| Status | Accepted |
| Parent Strata | Late Pleistocene |
| Unit Type | Climatostratigraphic |
| Rank | Stage |
| Scope | Global |
| Top - Base Age (Ma) | 0.13 - 0.19 |
| Chronostratigraphy - min/max age | Marine Isotope Stage 6 |
| Stratigraphy verification status | Trusted |
| Added by | Madeira, P. |
| Added date | 2024-05-17 15:00:00 |
References
Age Reference
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore, T. C., & Shackleton, N. J. (1987). Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year Chronostratigraphy. 1–29. Quaternary research. 27. 1. https://doi.org/10.1016/0033-5894(87)90046-9.
Stratigraphy After
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore, T. C., & Shackleton, N. J. (1987). Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year Chronostratigraphy. 1–29. Quaternary research. 27. 1. https://doi.org/10.1016/0033-5894(87)90046-9.
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore, T. C., & Shackleton, N. J. (1987). Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year Chronostratigraphy. 1–29. Quaternary research. 27. 1. https://doi.org/10.1016/0033-5894(87)90046-9.
Stratigraphy After
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore, T. C., & Shackleton, N. J. (1987). Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year Chronostratigraphy. 1–29. Quaternary research. 27. 1. https://doi.org/10.1016/0033-5894(87)90046-9.