Quaternary

Short description: Third and current period of the Cenozoic Era, from 2.58 million years ago to the present

Quaternary

2.58 – 0 Ma

PreЄ

A map of the world as it appeared during the Pleistocene epoch, c. 1 Ma

Chronology

Template:Quaternary graphical timeline

Etymology
Name formality| Formal
Usage information
Celestial body| Earth
Regional usage| Global (ICS)
Time scale(s) used| ICS Time Scale
Definition
Chronological unit| Period
Stratigraphic unit| System
Time span formality| Formal
Lower boundary definition|

* Base of magnetic polarity chronozone C2r (Matuyama)
* Extinction of the Haptophytes Discoaster pentaradiatus and Discoaster surculus

Lower boundary GSSP| Monte San Nicola Section, Gela, Sicily, Italy
[ ⚑ ] 37°08′49″N 14°12′13″E﻿ / ﻿37.1469°N 14.2035°E﻿ / 37.1469; 14.2035
GSSP ratified| 2009 (as base of Quaternary and Pleistocene)[1]
Upper boundary definition| Present day
Upper boundary GSSP| N/A
GSSP ratified| N/A
Atmospheric and climatic data
Mean atmospheric O2 content| c. 20.8 vol %
(104 % of modern)
Mean atmospheric CO2 content| c. 250 ppm
(1 times pre-industrial)
Mean surface temperature| c. 14 °C
(0 °C above modern)

The Quaternary (/kwəˈtɜːrnəri, ˈkwɒtərnɛri/ kwə-TUR-nə-ree, KWOT-ər-nerr-ee) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS).[2] It follows the Neogene Period and spans from 2.58 million years ago to the present.[3] As of 2023, the Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today); a third epoch, the Anthropocene, has recently been proposed, but it is not officially recognised by the ICS.

The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused.[4][5]

## Contents

* 1 Research history
* 2 Geology
* 3 Climate
* 4 Flora and Fauna
* 5 See also
* 6 References
* 7 External links

## Research history

In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" (Italian: quattro ordini).[6] The term "quaternary" was introduced by Jules Desnoyers in 1829 for sediments of France 's Seine Basin that clearly seemed to be younger than Tertiary Period rocks.[7][8][9]

The Quaternary Period follows the Neogene Period and extends to the present. The Quaternary covers the time span of glaciations classified as the Pleistocene, and includes the present interglacial time-period, the Holocene.

This places the start of the Quaternary at the onset of Northern Hemisphere glaciation approximately 2.6 million years ago (mya). Prior to 2009, the Pleistocene was defined to be from 1.805 million years ago to the present, so the current definition of the Pleistocene includes a portion of what was, prior to 2009, defined as the Pliocene.

Quaternary stratigraphers usually worked with regional subdivisions. From the 1970s, the International Commission on Stratigraphy (ICS) tried to make a single geologic time scale based on GSSP's, which could be used internationally. The Quaternary subdivisions were defined based on biostratigraphy instead of paleoclimate.

This led to the problem that the proposed base of the Pleistocene was at 1.805 million years ago, long after the start of the major glaciations of the northern hemisphere. The ICS then proposed to abolish use of the name Quaternary altogether, which appeared unacceptable to the International Union for Quaternary Research (INQUA).

In 2009, it was decided to make the Quaternary the youngest period of the Cenozoic Era with its base at 2.588 mya and including the Gelasian Stage, which was formerly considered part of the Neogene Period and Pliocene Epoch.[10] This was later revised to 2.58 mya.[3][11]

The Anthropocene has been proposed as a third epoch as a mark of the anthropogenic impact on the global environment starting with the Industrial Revolution, or about 200 years ago.[12] The Anthropocene is not officially designated by the ICS, but a working group has been working on a proposal for the creation of an epoch or sub-period.[13]

## Geology

Further information: Earth:Quaternary geology

The 2.58 million years of the Quaternary represents the time during which recognisable humans existed.[14] Over this geologically short time period there has been relatively little change in the distribution of the continents due to plate tectonics.

The Quaternary geological record is preserved in greater detail than that for earlier periods.

The major geographical changes during this time period included the emergence of the Strait of Bosphorus and Skagerrak during glacial epochs, which respectively turned the Black Sea and Baltic Sea into fresh water lakes, followed by their flooding (and return to salt water) by rising sea level;[15] the periodic filling of the English Channel, forming a land bridge between Britain and the European mainland; the periodic closing of the Bering Strait, forming the land bridge between Asia and North America; and the periodic flash flooding of Scablands of the American Northwest by glacial water.[16]

The current extent of Hudson Bay, the Great Lakes and other major lakes of North America are a consequence of the Canadian Shield's readjustment since the last ice age; different shorelines have existed over the course of Quaternary time.[17]

## Climate

Further information: Earth:Quaternary glaciation and Earth:Last Glacial Period

The climate was one of periodic glaciations with continental glaciers moving as far from the poles as 40 degrees latitude. Glaciation took place repeatedly during the Quaternary Ice age – a term coined by Schimper in 1839 that began with the start of the Quaternary about 2.58 Mya and continues to the present day.

Artist's impression of Earth during the Last Glacial Maximum

In 1821, a Switzerland engineer, Ignaz Venetz, presented an article in which he suggested the presence of traces of the passage of a glacier at a considerable distance from the Alps. This idea was initially disputed by another Swiss scientist, Louis Agassiz, but when he undertook to disprove it, he ended up affirming his colleague's hypothesis. A year later, Agassiz raised the hypothesis of a great glacial period that would have had long-reaching general effects. This idea gained him international fame and led to the establishment of the Glacial Theory.

In time, thanks to the refinement of geology, it has been demonstrated that there were several periods of glacial advance and retreat and that past temperatures on Earth were very different from today. In particular, the Milankovitch cycles of Milutin Milankovitch are based on the premise that variations in incoming solar radiation are a fundamental factor controlling Earth's climate.

During this time, substantial glaciers advanced and retreated over much of North America and Europe, parts of South America and Asia, and all of Antarctica.

## Flora and Fauna

There was a major extinction of large mammals in Northern areas at the end of the Pleistocene Epoch. Many forms such as sabre-toothed cats, mammoths, mastodons, glyptodonts, etc., became extinct worldwide. Others, including horses, camels and American cheetahs became extinct in North America.[18][19]

The Great Lakes formed and giant mammals thrived in parts of North America and Eurasia not covered in ice. These mammals became extinct when the glacial period ended about 11,700 years ago. Modern humans evolved about 315,000 years ago. During the Quaternary Period, mammals, flowering plants, and insects dominated the land. [citation needed]

## See also

* List of Quaternary volcanic eruptions

## References

1. ↑ Gibbard, Philip; Head, Martin (September 2010). "The newly-ratified definition of the Quaternary System/Period and redefinition of the Pleistocene Series/Epoch, and comparison of proposals advanced prior to formal ratification". Episodes 33 (3): 152–158. doi:10.18814/epiiugs/2010/v33i3/002. https://stratigraphy.org/gssps/files/quaternary-pleistocene.pdf. Retrieved 8 December 2020.
2. ↑ Cohen, K.M.; Finney, S.C.; Gibbard, P.L.; Fan, J.-X.. "International Chronostratigraphic Chart 2013". ICS. http://www.stratigraphy.org/icschart/chronostratchart2013-01.pdf.
3. ↑ 3.0 3.1 "Stratigraphic Chart 2022". International Stratigraphic Commission. February 2022. https://stratigraphy.org/ICSchart/ChronostratChart2022-02.pdf.
4. ↑ Denton, G.H.; Anderson, R.F.; Toggweiler, J.R.; Edwards, R.L.; Schaefer, J.M.; Putnam, A.E. (2010). "The Last Glacial Termination". Science 328 (5986): 1652–1656. doi:10.1126/science.1184119. PMID 20576882. Bibcode: 2010Sci...328.1652D.
5. ↑ Lowe, J.J.; Walker, M.J.C. (1997). Reconstructing Quaternary Environments. Routledge. ISBN 978-0582101661.
6. ↑ See:
* Arduino, Giovanni (1760). "Lettera Segonda di Giovanni Arduino … sopra varie sue osservazioni fatte in diverse parti del territorio di Vicenza, ed altrove, apparenenti alla Teoria terrestre, ed alla Mineralogia" (in it). Nuova Raccolta d'Opuscoli Scientifici e Filologici [New collection of scientific and philogical pamphlets] 6: 133 (cxxxiii)–180(clxxx). Available at: Museo Galileo (Florence (Firenze), Italy) From p. 158 (clviii): "Per quanto ho potuto sinora osservavare, la serie di questi strati, che compongono la corteccia visibile della terra, mi pare distinta in quattro ordini generali, e successivi, senza considerarvi il mare." (As far as I have been able to observe, the series of these layers that compose the visible crust of the earth seems to me distinct in four general orders, and successive, not considering the sea.)
* English translation: Ell, Theodore (2012). "Two letters of Signor Giovanni Arduino, concerning his natural observations: first full English translation. Part 2.". Earth Sciences History 31 (2): 168–192. doi:10.17704/eshi.31.2.c2q4076006wn7751.
7. ↑ Desnoyers, J. (1829). "Observations sur un ensemble de dépôts marins plus récents que les terrains tertiaires du bassin de la Seine, et constituant une formation géologique distincte; précédées d'un aperçu de la nonsimultanéité des bassins tertiares" (in fr). Annales des Sciences Naturelles 16: 171–214, 402–491. https://www.biodiversitylibrary.org/item/29350#page/177/mode/1up. From p. 193: "Ce que je désirerais … dont il faut également les distinguer." (What I would desire to prove above all is that the series of tertiary deposits continued – and even began in the more recent basins – for a long time, perhaps after that of the Seine had been completely filled, and that these later formations – Quaternary (1), so to say – should not retain the name of alluvial deposits any more than the true and ancient tertiary deposits, from which they must also be distinguished.) However, on the very same page, Desnoyers abandoned the use of the term "quaternary" because the distinction between quaternary and tertiary deposits wasn't clear. From p. 193: "La crainte de voir mal comprise … que ceux du bassin de la Seine." (The fear of seeing my opinion in this regard be misunderstood or exaggerated, has made me abandon the word "quaternary", which at first I had wanted to apply to all deposits more recent than those of the Seine basin.)
8. ↑ "Late Quaternary Fluvial and Coastal Sequences Chapter 1: Introduction". http://shodhganga.inflibnet.ac.in/bitstream/10603/77123/8/08_chapter 1.pdf.
9. ↑ Wiz Science™ (28 September 2015), Quaternary - Video Learning, https://www.youtube.com/watch?v=Io7vhansU1o, retrieved 26 March 2017
10. ↑ "See the 2009 version of the ICS geologic time scale". http://www.quaternary.stratigraphy.org.uk/correlation/GSAchron09.jpg.
11. ↑ "International Chronostratigraphic Chart ChangeLog for 2012-2022". International Chronostratigraphic Chart. International Commission on Stratigraphy. February 2022. https://stratigraphy.org/ICSchart/ChangeLog2012-2022.txt. Retrieved 4 June 2022.
12. ↑ Zalasiewicz, J.; Williams, M.; Haywood, A.; Ellis, M. (2011). "The Anthropocene: a new epoch of geological time?". Philosophical Transactions of the Royal Society A 369 (1938): 835–841. doi:10.1098/rsta.2010.0339. PMID 21282149. Bibcode: 2011RSPTA.369..835Z. http://nora.nerc.ac.uk/id/eprint/14867/1/Anthropocene_overview.pdf.
13. ↑ "Working Group on the 'Anthropocene'". http://quaternary.stratigraphy.org/workinggroups/anthropocene/.
14. ↑ Ghosh, Pallab (4 March 2015). "'First human' discovered in Ethiopia". BBC News (London). https://www.bbc.com/news/science-environment-31718336.
15. ↑ Ryan, William B.F.; Pitman, Walter C.; Major, Candace O.; Shimkus, Kazimieras; Moskalenko, Vladamir; Jones, Glenn A.; Dimitrov, Petko; Gorür, Naci et al. (April 1997). "An abrupt drowning of the Black Sea shelf". Marine Geology 138 (1–2): 119–126. doi:10.1016/s0025-3227(97)00007-8. Bibcode: 1997MGeol.138..119R.
16. ↑ Balbas, A.M., Barth, A.M., Clark, P.U., Clark, J., Caffee, M., O'Connor, J., Baker, V.R., Konrad, K. and Bjornstad, B., 2017. 10Be dating of late Pleistocene megafloods and Cordilleran Ice Sheet retreat in the northwestern United States. Geology, 45(7), pp. 583-586.
17. ↑ Dyke, Arthur S. (2004). "An outline of North American deglaciation with emphasis on central and northern Canada". Developments in Quaternary Sciences 2: 373–424. doi:10.1016/S1571-0866(04)80209-4. ISBN 9780444515926.
18. ↑ Haynes. "Stanford Camelops". http://www.unr.edu/cla/anthro/people/faculty/haynes/download Haynes+StanfordCamelops.pdf.
19. ↑ "Extinct American Cheetah Fact Sheet". http://library.sandiegozoo.org/factsheets/_extinct/cheetah1_american/cheetah1_american.html.

## External links

* Subcommission on Quaternary Stratigraphy
* Stratigraphical charts for the Quaternary
* Version history of the global Quaternary chronostratigraphical charts (from 2004b)
* Silva, P.G. C. Zazo, T. Bardají, J. Baena, J. Lario, A. Rosas, J. Van der Made. 2009, "Tabla Cronoestratigrafíca del Cuaternario en la Península Ibérica - V.2". [Versión PDF, 3.6 Mb]. Asociación Española para el Estudio del Cuaternario (AEQUA), Departamento de Geología, Universidad de Salamanca, Spain. (Correlation chart of European Quaternary and cultural stages and fossils)
* Welcome to the XVIII INQUA-Congress, Bern, 2011
* Quaternary (chronostratigraphy scale)

* v
* t
* e

Quaternary Period

| Pleistocene Epoch| Holocene Epoch

|

* Early
* Middle
* Late

* Meghalayan
* Northgrippian
* Greenlandian
* Preboreal
* Boreal
* Atlantic
* Subboreal
* Subatlantic

* v
* t
* e

Geological history of Earth

Cenozoic era
(present–66.0 Mya)|

| Quaternary (present–2.588 Mya)|

* Holocene (present–11.784 kya)
* Pleistocene (11.784 kya–2.588 Mya)

|

Neogene (2.588–23.03 Mya)|

* Pliocene (2.588–5.333 Mya)
* Miocene (5.333–23.03 Mya)

Paleogene (23.03–66.0 Mya)|

* Oligocene (23.03–33.9 Mya)
* Eocene (33.9–56.0 Mya)
* Paleocene (56.0–66.0 Mya)

Mesozoic era
(66.0–251.902 Mya)|

| Cretaceous (66.0–145.0 Mya)|

* Late (66.0–100.5 Mya)
* Early (100.5–145.0 Mya)

|

Jurassic (145.0–201.3 Mya)|

* Late (145.0–163.5 Mya)
* Middle (163.5–174.1 Mya)
* Early (174.1–201.3 Mya)

Triassic (201.3–251.902 Mya)|

* Late (201.3–237 Mya)
* Middle (237–247.2 Mya)
* Early (247.2–251.902 Mya)

Paleozoic era
(251.902–541.0 Mya)|

| Permian (251.902–298.9 Mya)|

* Lopingian (251.902–259.8 Mya)
* Guadalupian (259.8–272.3 Mya)
* Cisuralian (272.3–298.9 Mya)

|

Carboniferous (298.9–358.9 Mya)|

* Pennsylvanian (298.9–323.2 Mya)
* Mississippian (323.2–358.9 Mya)

Devonian (358.9–419.2 Mya)|

* Late (358.9–382.7 Mya)
* Middle (382.7–393.3 Mya)
* Early (393.3–419.2 Mya)

Silurian (419.2–443.8 Mya)|

* Pridoli (419.2–423.0 Mya)
* Ludlow (423.0–427.4 Mya)
* Wenlock (427.4–433.4 Mya)
* Llandovery (433.4–443.8 Mya)

Ordovician (443.8–485.4 Mya)|

* Late (443.8–458.4 Mya)
* Middle (458.4–470.0 Mya)
* Early (470.0–485.4 Mya)

Cambrian (485.4–541.0 Mya)|

* Furongian (485.4–497 Mya)
* Miaolingian (497–509 Mya)
* Series 2 (509–521 Mya)
* Terreneuvian (521–541.0 Mya)

Proterozoic eon
(541.0 Mya–2.5 Gya)|

| Neoproterozoic (541.0 Mya–1 Gya)|

* Ediacaran (541.0–~635 Mya)
* Cryogenian (~635–~720 Mya)
* Tonian (~720 Mya–1 Gya)

|

Mesoproterozoic (1–1.6 Gya)|

* Stenian (1–1.2 Gya)
* Ectasian (1.2–1.4 Gya)
* Calymmian (1.4–1.6 Gya)

Paleoproterozoic (1.6–2.5 Gya)|

* Statherian (1.6–1.8 Gya)
* Orosirian (1.8–2.05 Gya)
* Rhyacian (2.05–2.3 Gya)
* Siderian (2.3–2.5 Gya)

Archean eon (2.5–4 Gya)|

| Eras|

* Neoarchean (2.5–2.8 Gya)
* Mesoarchean (2.8–3.2 Gya)
* Paleoarchean (3.2–3.6 Gya)
* Eoarchean (3.6–4 Gya)

|

Hadean eon (4–4.6 Gya)|

|  |

|

kya = thousands years ago. Mya = millions years ago. Gya = billions years ago.
See also: Geologic time scale

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* Atmospheric science / Meteorology
* Biogeography / Phytogeography
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* Coastal geography / Oceanography
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* Geobiology
* Geology
* Geomorphology
* Geostatistics
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* [[Earth:HydrologHydrology / Limnology
* Landscape ecology
* Quaternary science

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