Hsandagolian

The Hsandagolian age is a period of geologic time (33.9 – 23.03 Ma) within the Oligocene epoch of the Paleogene used more specifically with Asian Land Mammal Ages. ^[1]

9 relations: Aquitanian (stage), Asian land mammal age, Geologic time scale, Kekeamuan, Oligocene, Paleogene, Rupelian, Tabenbulakian, Year.

Aquitanian (stage)

The Aquitanian is, in the ICS' geologic timescale, the oldest age or lowest stage in the Miocene.

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The Asian land mammal ages, acronym ALMA, establish a geologic timescale for prehistoric Asian fauna beginning 58.7 Mya during the Paleogene and continuing through to the Miocene (Aquitanian) (23.03 Ma).

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Geologic time scale

The geologic time scale (GTS) is a system of chronological dating that relates geological strata (stratigraphy) to time.

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Kekeamuan

The Kekeamuan age is a period of geologic time (33.9—28.4 Ma) within the Early Oligocene Epoch of the Paleogene Period.

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Oligocene

The Oligocene is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present (to). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain.

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Paleogene

The Paleogene (also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the beginning of the Neogene Period Mya.

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Rupelian

The Rupelian is, in the geologic timescale, the older of two ages or the lower of two stages of the Oligocene epoch/series.

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Tabenbulakian

The Tabenbulakian age is a period of geologic time (28.4—23.03 Ma) within the Oligocene Epoch of the late Paleogene Period and Miocene Epoch of the early Neogene Period, used more specifically with Asian Land Mammal Ages.

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Year

A year is the orbital period of the Earth moving in its orbit around the Sun.

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References

[1] https://en.wikipedia.org/wiki/Hsandagolian

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