Timeline of glaciation
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There have been four major periods of glaciation in the Earth's past. The first, and possibly most severe, may have occurred from 800 Ma to 600 Ma (million years ago, the late Proterozoic Age) and it has been suggested that it produced a "Snowball Earth" in which the earth iced over completely. It has been suggested also that the end of this cold period was responsible for the subsequent Cambrian Explosion, a time of rapid diversification of multicelled life during the Cambrian era. However, this theory is recent and controversial.
A minor series of glaciations occurred from 460 Ma to 430 Ma. There were extensive glaciations from 350 to 250 Ma. The present Pleistocene ice age has seen more or less extensive glaciation on 40,000 and later, 100,000 year cycles. The last glacial period ended about 10,000 years ago.
Pleistocene glacial cycles
Originally, the periods were named after characteristic geological features, and these names vary from region to region. It is now perhaps more common (before the previous interglacial to the current (Holocene) one, the Eemian) to refer to periods by their Marine isotopic stage number. The marine record preserves all the past glaciations; the land-based evidence is less complete because successive glaciations may wipe out evidence of their predecessors. Hence the "names" system is incomplete: the Pastonian glaciation is MIS63, i.e., the 30th interglacial before present.
The last glacial and interglacial phases of the Pleistocene are named, from most recent to most distant, as follows. Dates shown are in thousand years BCE.
| Backwards Glacial Index | Name Alpine | Name N. American | Name N. European | Name Great Britain | Inter/Glacial | Period (ka) | MIS | Epoch |
|---|---|---|---|---|---|---|---|---|
| Flandrian | interglacial | present – 12 | MIS1 | Holocene | ||||
| 1st | Würm | Wisconsinan | Weichsel or Vistula | Devensian | glacial period | 15 – 70 | MIS2-4 & 5a-d | Pleistocene |
| Riss-Würm | Sangamon | Eemian | Ipswichian | interglacial | 110 – 130 | MIS5e | ||
| 2nd | Riss | Illinoian | Saale | Wolstonian or Gipping | glacial period | 125 – 200 | MIS6 | |
| Mindel-Riss | Yarmouth | Holstein | Hoxnian | interglacial(s) | 200 – 425 | MIS7 | ||
| 3rd – 6th | Mindel | Kansan | Elster | Anglian | glacial period(s) | 240 – 455 | ||
| Günz-Mindel | Aftonian | Cromerian | interglacial(s) | 455 – 620 | ||||
| 7th | Günz | Nebraskan | Menapian | Beestonian | glacial period | 620 – 680 |
Other older periods of the Pleistocene
| Name | Inter/Glacial | Period (ka) | MIS | Epoch |
|---|---|---|---|---|
| Waalian | interglacial | 470 – 540 | Pleistocene | |
| Donau II | glacial period | 540 – 550 | ||
| Tiglian | interglacial | 550 – 585 | ||
| Donau I | glacial period | 585 – 600 | ||
| Pastonian interglacial | interglacial | 600 – 800 | MIS63 | |
| Pre-Pastonian glaciation | glacial period | 800 – 1300 | ||
| Bramertonian Interglacial | interglacial | 1300 – 1550 |
The Brunhes-Matuyama reversal occurred 780,000 years ago, approximately coincident with MIS19, the "Cromerian Complex" interglacial I, and can be used to date sediment cores.
Major glacial periods
| Name | Period (Ma) | Period | Era |
|---|---|---|---|
| 30 - present | Neogene | Cenozoic | |
| Karoo | 360 - 260 | Carboniferous and Permian | Paleozoic |
| Andean-Saharan | 450 - 420 | Ordovician and Silurian | Paleozoic |
| Cryogenian (or Sturtian-Varangian)
| 800 - 635 | Cryogenian | Neoproterozoic |
| Huronian
| 2100 - 2400 | Siderian and Rhyacian | Paleoproterozoic |
References
- http://www-qpg.geog.cam.ac.uk/people/gibbard/GTS2004Quat.pdf (fig 22.1)
See also
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