R Marine Isotope Stage 6
Climatostratigraphic > EstadioResources
Resources
Ocurrencias
| VS | Nombre Científico | Archipiélago | Isla | Lugar | Edad Min/Max |
|---|
Datos Estratigráficos
| Designación | Marine Isotope Stage 6 |
| Estatus | Aceptado |
| Estrato Padre | Late Pleistocene |
| Tipo de unidad | Climatoestratigrafía |
| Categoría | Estadio |
| Ámbito | Global |
| Top - Base Age (Ma) | 0.13 - 0.19 |
| Cronoestratigrafía- edad min/max | Estadio isotópico marino 6 |
| Estado de verificación de estratigrafía | Confiable |
| Añadido por | Madeira, P. |
| Añadido a | 2024-05-17 15:00:00 |
Referencias
Referencia de edad
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.