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Timeline of glaciation - Wikipedia

https://en.wikipedia.org/wiki/Timeline_of_glaciation

Timeline of glaciation. Life timeline. view • discuss-4500 — –-4000 — –-3500 — –-3000 — – ... The second ice age, and possibly most severe, ...

Timeline of glaciation

From Wikipedia, the free encyclopedia

Life timeline

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Earliest Earth (−4540)

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Earliest sexual reproduction

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Axis scale: millions of years.
Orange labels: known ice ages.
Also see: Human timeline and Nature timeline

There have been five known ice ages in the Earth's history, with the Earth experiencing the Quaternary Ice Age during the present time. Within ice ages, there exist periods of more severe glacial conditions and more temperate referred to as glacial periods and interglacial periods, respectively. The Earth is currently in such an interglacial period of the Quaternary Ice Age, with the last glacial period of the Quaternary having ended approximately 11,700 years ago with the start of the Holocene epoch.^[1] Based on climate proxies, paleoclimatologists study the different climate states originating from glaciation.

Known ice ages

Name	Period (Ma)	Period	Era
Quaternary	2.58 – present	(Neogene and) Quaternary	Cenozoic
Karoo	360 – 260	Carboniferous and Permian	Paleozoic
Andean-Saharan	450 – 420	Ordovician and Silurian	Paleozoic
Cryogenian (or Sturtian-Varangian)	720 – 635^[2]	Cryogenian	Neoproterozoic
Huronian	2400 – 2100	Siderian and Rhyacian	Paleoproterozoic

Descriptions

The second ice age, and possibly most severe, is estimated to have occurred from 720 to 635 Ma (million years) ago,^[2] in the Neoproterozoic Era and it has been suggested that it produced a second^[3] "Snowball Earth" in which the earth iced over completely. It has been suggested also that the end of this second cold period^[3] was responsible for the subsequent Cambrian Explosion, a time of rapid diversification of multicelled life during the Cambrian Period. However, this hypothesis is still controversial,^[4]^[5] though is growing in popularity among researchers as evidence in its favor has mounted.^[who?]
A minor series of glaciations occurred from 460 Ma to 430 Ma. There were extensive glaciations from 350 to 250 Ma. The current ice age, called the Quaternary glaciation, has seen more or less extensive glaciation on 40,000 and later, 100,000 year cycles.

Nomenclature of Quaternary glacial cycles

500 million year record shows current and previous two major glacial periods

Originally, the glacial and interglacial periods of the Quaternary Ice Age were named after characteristic geological features, and these names varied from region to region. It is now more common for researchers to refer to the periods by their marine isotopic stage number.^[6] 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. Ice cores from continental ice accumulations also provide a complete record, but do not go as far back in time as marine data. Pollen data from lakes and bogs as well as loess profiles provided important land-based correlation data.^[7] The names system has not been completely filled out since the technical discussion moved to using marine isotopic stage numbers. For example, there are five Pleistocene glacial/interglacial cycles recorded in marine sediments during the last half million years, but only three classic interglacials were originally recognized on land during that period (Mindel, Riss and Würm).^[8]
Land-based evidence works acceptably well back as far as MIS 6, but it has been difficult to coordinate stages using just land-based evidence before that. Hence, the "names" system is incomplete and the land-based identifications of ice ages previous to that are somewhat conjectural. Nonetheless, land based data is essentially useful in discussing landforms, and correlating the known marine isotopic stage with them.^[7]
The last glacial and interglacial periods of the Quaternary are named, from most recent to most distant, as follows. Dates shown are in thousand years before present.

Land-based chronology of Quaternary glacial cycles

This section's factual accuracy is disputed. Please help to ensure that disputed statements are reliably sourced. See the relevant discussion on the talk page. (May 2008) (Learn how and when to remove this template message)

Backwards Glacial Index	Names					Inter/Glacial	Period (ka)	Marine isotope stage (MIS)	Epoch
Backwards Glacial Index	Alpine	N. American	N. European	Great Britain	S. American	Inter/Glacial	Period (ka)	Marine isotope stage (MIS)	Epoch
				Flandrian		interglacial	present – 12	1	Holocene
1st	Würm	Wisconsin	Weichselian	Devensian	Llanquihue^[9] or Mérida	glacial period	12 – 110	2-4 & 5a-d	Pleistocene
	Riss-Würm	Sangamonian	Eemian	Ipswichian	Valdivia^[10]	interglacial	115 – 130^[11]	5e
2nd	Riss	Illinoian	Saalian	Wolstonian or Gipping	Santa María^[9]	glacial period	130 – 200	6
	Mindel-Riss	Pre-Illinoian	Holstein	Hoxnian		interglacial(s)	374 – 424^[12]	11
3rd – 6th	Mindel	Pre-Illinoian	Elsterian	Anglian	Río Llico^[9]	glacial period(s)	424 – 478	12
	Günz-Mindel	Pre-Illinoian		Cromerian*		interglacial(s)	478 – 533 – 563	13-15
7th – 8th	Günz	Pre-Illinoian	Elbe or Menapian	Beestonian	Caracol^[9]	glacial period	621 – 676	16

Older periods of the Quaternary

Name	Inter/Glacial	Period (ka)	MIS	Epoch
Pastonian Stage	interglacial	600 – 800
Pre-Pastonian Stage	glacial period	800 – 1300
Bramertonian Stage	interglacial	1300 – 1550

**Table data is based on Gibbard Figure 22.1.^[6]

Ice core evidence of recent glaciation

Main article: Ice core

Ice cores are used to obtain a high resolution record of recent glaciation. It confirms the chronology of the marine isotopic stages. Ice core data shows that the last 400,000 years have consisted of short interglacials (10,000 to 30,000 years) about as warm as the present alternated with much longer (70,000 to 90,000 years) glacials substantially colder than present. The new EPICA Antarctic ice core has revealed that between 400,000 and 780,000 years ago, interglacials occupied a considerably larger proportion of each glacial/interglacial cycle, but were not as warm as subsequent interglacials.

References

Walker, M., Johnsen, S., Rasmussen, S. O., Popp, T., Steffensen, J.-P., Gibbard, P., Hoek, W., Lowe, J., Andrews, J., Bjo¨ rck, S., Cwynar, L. C., Hughen, K., Kershaw, P., Kromer, B., Litt, T., Lowe, D. J., Nakagawa, T., Newnham, R., and Schwander, J. 2009. Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records. J. Quaternary Sci., Vol. 24 pp. 3–17. ISSN 0267-8179.

Lisiecki, Lorraine E.; Raymo, Maureen E. (2005). "A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records". doi:10.1029/2004PA001071.

External links

Look up glaciation in Wiktionary, the free dictionary.

Aber, J.S. (2006). "Regional Glaciation of Kansas and Nebraska". Emporia KA: Emporia State University.
Work Group on Geospatial Analysis of Glaciated Environments (GAGE) (2000). "Pre-Wisconsin Glaciation of Central North America". Emporia KA: INQUA Commission on Glaciation, Emporia State University. Archived from the original on May 13, 2008.
Subcommission on Quaternary Stratigraphy (2011). "Global correlation tables for the Quaternary". Cambridge UK: Department of Geography, University of Cambridge.
Gibbard, P.L.; Boreham, S.; Cohen, K.M.; Moscariello, A. (2011). "Global chronostratigraphical correlation table for the last 2.7 million years v. 2011." (PDF). Cambridge UK: Subcommission on Quaternary Stratigraphy, Department of Geography, University of Cambridge.
Hambrey, M.J.; Harland, W.B., eds. (1981). Earth's pre-Pleistocene glacial record. Cambridge University Press. Archived from the original on October 11, 2006. 1004 + xv pp. (book downloadable as series of PDF files)
Silva, P.G.; Zazo,C; Bardají,T.; Baena, J.; Lario, J.; Rosas, A.; Van der Made (2009). "Tabla Cronoestratigráfica del Cuaternario AEQUA V.2" (PDF 3.6 Mb). Departamento de Geología, Universidad de Salamanca, Spain: Asociación Española para el Estudio del Cuaternario (AEQUA). (Correlation Chart of European Quaternary and cultural stages and fossils)

Categories:

"Chart". International Commission on Stratigraphy. Archived from the original on 2017-01-13. Retrieved 2017-02-14.

Miracle Planet: Snowball Earth, (2005) documentary, Canadian Film Board, rebroadcast 25 April 2009 on the Science Channel (HD)

van Andel, Tjeerd H. (1994). New Views on an Old Planet: A History of Global Change (2nd ed.). Cambridge UK: Cambridge University Press. ISBN 0-521-44755-0.

Rieu, Ruben; et al. (2007). "Climatic cycles during a Neoproterozoic "snowball" glacial epoch". Geology. 35 (4): 299–302. doi:10.1130/G23400A.1. Archived from the original on 2012-05-16.

Gibbard, P.; van Kolfschoten, T. (2004). "Chapter 22: The Pleistocene and Holocene Epochs" (PDF). In Gradstein, F. M.; Ogg, James G.; Smith, A. Gilbert. A Geologic Time Scale 2004. Cambridge: Cambridge University Press. ISBN 0-521-78142-6.

Davis, Owen K. "Non-Marine Records: Correlatiuons withe the Marine Sequence". Introduction to Quaternary Ecology. University of Arizona.

Kukla, George (August 2005). "Saalian supercycle, Mindel/Riss interglacial and Milankovitch's dating". Quaternary Science Reviews. 24 (14-15): 1573–83. doi:10.1016/j.quascirev.2004.08.023.

Porter, Stephen C. (1981). "Pleistocene Glaciation in the Southern Lake District of Chile". Quaternary Research. 16: 263–292.

Astorga, G. and Pino, M.. 2011. Fossil leaves from the last interglacial in Central-Southern Chile: Inferences regarding the vegetation and paleoclimate. Geologica Acta.

NEEM community members (2013). "Eemian interglacial reconstructed from a Greenland folded ice core". Nature. 493: 489–94. doi:10.1038/nature11789. PMID 23344358.

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