R Marine Isotope Substage 5e
Climatostratigraphic > SubstageStratigraphy Layers
EonPhanerozoic
EraCenozoic
PeriodQuaternary
EpochPleistocene
AgeLate Pleistocene
StageMarine Isotope Stage 5
Location Occurrences
Occurrences
VS | Scientific Name | Archipelago | Island | Location | Min/Max Age |
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Stratigraphy Data
Designation | Marine Isotope Substage 5e |
Status | Accepted |
Parent Strata | Marine Isotope Stage 5 |
Unit Type | Climatostratigraphic |
Rank | Substage |
Scope | Global |
Top - Base Age (Ma) | 0.1225 - 0.125 |
Chronostratigraphy - min/max age | Marine Isotope Substage 5e |
Stratigraphy verification status | Trusted |
Added by | Madeira, P. |
Added date | 2024-02-27 16:00:00 |
Updated by | Madeira, P. |
Update date | 2024-05-17 15:29:14 |
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.