Cryogenian

Short description: Second period of the Neoproterozoic Era, with major glaciation

Cryogenian

c. 720 – c. 635 Ma

Had'n

Archean

Proterozoic

Pha.

A map of the world as it appeared at the start of the Cryogenian, c. 720 Ma

Chronology

Template:Cryogenian graphical timeline

Etymology
Name formality| Formal
Name ratified| 1990
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| Defined chronometrically with an interim calibrated age of c. 720 Ma. GSSP is in progress.
Lower boundary definition candidates| The first appearance of widespread glaciation.[1]
Lower boundary GSSP candidate section(s)| To be determined
Upper boundary definition|

* Worldwide distinct cap carbonates.
* Beginning of a distinctive pattern of secular changes in carbon isotopes.

Upper boundary GSSP| Enorama Creek section, Flinders Ranges, South Australia
[ ⚑ ] 31°19′53″S 138°38′00″E﻿ / ﻿31.3314°S 138.6334°E﻿ / -31.3314; 138.6334
GSSP ratified| March 2004[2]
Atmospheric and climatic data
Mean atmospheric O2 content| c. 12 vol %
(60 % of modern)
Mean atmospheric CO2 content| c. 1300 ppm
(5 times pre-industrial)
Mean surface temperature| c. 5 °C
(-9 °C above modern)

Life timeline

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Primates

Earth (−4540)

Earliest water

Earliest life

Earliest oxygen

Atmospheric oxygen

Oxygen crisis

Sexual reproduction

Earliest plants

Ediacara biota

Cambrian explosion

Tetrapoda

Earliest apes

black;">Pongola

black;">Huronian

black;">Cryogenian

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black;">Quaternary

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Clickable

(million years ago)

(See also: Human timeline, and Nature timeline.)

The Cryogenian (from Ancient Greek:, meaning "cold" and γένεσις, romanized: génesis, meaning "birth") is a geologic period that lasted from 720 to 635 million years ago.[3] It forms the second geologic period of the Neoproterozoic Era, preceded by the Tonian Period and followed by the Ediacaran.

The Cryogenian was a time of drastic biosphere changes. After the previous Boring Billion years of stability, at the beginning of Cryogenian the severe Sturtian glaciation began, freezing the entire Earth in a planetary state known as a Snowball Earth. After 70 million years it ended, but was quickly followed by the Marinoan glaciation, which was also a global event. These events are the subject of much scientific controversy specifically over whether these glaciations covered the entire planet or a band of open sea survived near the equator (termed "slushball Earth").

## Contents

* 1 Ratification
* 2 Climate
* 3 Paleogeography
* 4 Cryogenian biota and fossils
* 5 See also
* 6 References
* 7 Further reading
* 8 External links

## Ratification

The Cryogenian Period was ratified in 1990 by the International Commission on Stratigraphy.[4] In contrast to most other time periods, the beginning of the Cryogenian is not linked to a globally observable and documented event. Instead, the base of the period is defined by a fixed rock age, that was originally set at 850 million years,[5] but changed in 2015 to 720 million years.[3]

This could cause ambiguity because estimates of rock ages are variable and are subject to laboratory error. For instance, the time scale of the Cambrian Period is not reckoned by rock younger than a given age (541 million years), but by the appearance of the worldwide Treptichnus pedum diagnostic trace fossil assemblages. This means that rocks can be recognized as Cambrian in the field, without extensive lab testing.

Currently, there is no consensus on what global event is a suitable candidate to mark the start of the Cryogenian Period, but a global glaciation would be a likely candidate.[5]

## Climate

The name of the geologic period refers to the very cold global climate of the Cryogenian.

Characteristic glacial deposits indicate that Earth suffered the most severe ice ages in its history during this period (Sturtian and Marinoan). According to Eyles and Young, "Late Proterozoic glaciogenic deposits are known from all the continents. They provide evidence of the most widespread and long-ranging glaciation on Earth." Several glacial periods are evident, interspersed with periods of relatively warm climate, with glaciers reaching sea level in low paleolatitudes.[6]

Glaciers extended and contracted in a series of rhythmic pulses, possibly reaching as far as the equator.[7]

Diamictite of the Elatina Formation in South Australia, formed during the Marinoan glaciation of the late Cryogenian

The Cryogenian is generally considered to be divisible into at least two major worldwide glaciations. The Sturtian glaciation persisted from 720 to 660 million years ago, and the Marinoan glaciation which ended approximately 635 Ma, at the end of the Cryogenian.[8] The deposits of glacial tillite also occur in places that were at low latitudes during the Cryogenian, a phenomenon which led to the hypothesis of deeply frozen planetary oceans called "Snowball Earth".[9] Between the Sturtian and Marinoan glaciations was a so-called "Cryogenian interglacial period" marked by relatively warm climate and anoxic oceans,[10] along with marine transgression.[11]

## Paleogeography

Before the start of the Cryogenian, around 750 Ma, the cratons that made up the supercontinent Rodinia started to rift apart. The superocean Mirovia began to close while the superocean Panthalassa began to form. The cratons (possibly) later assembled into another supercontinent called Pannotia, in the Ediacaran.

Eyles and Young state, "Most Neoproterozoic glacial deposits accumulated as glacially influenced marine strata along rifted continental margins or interiors." Worldwide deposition of dolomite might have reduced atmospheric carbon dioxide. The break up along the margins of Laurentia at about 750 Ma occurs at about the same time as the deposition of the Rapitan Group in North America, contemporaneously with the Sturtian in Australia. A similar period of rifting at about 650 Ma occurred with the deposition of the Ice Brook Formation in North America, contemporaneously with the Marinoan in Australia.[6] The Sturtian and Marinoan are local divisions within the Adelaide Rift Complex.

## Cryogenian biota and fossils

Between the Sturtian and Marinoan glaciations, global biodiversity was very low.[10]

Fossils of testate amoeba (or Arcellinida) first appear during the Cryogenian Period.[12] Since 2009, some researchers have argued that during the Cryogenian Period, potentially the oldest known fossils of sponges, and therefore animals, were formed.[13][14][15] However, it is unclear whether these fossils actually belong to sponges, though the authors do not rule out the possibility of such fossils to represent proto-sponges or complex microbial precursors to sponge-grade organisms.[16] The issue of whether or not biology was impacted by this event has not been settled, for example Porter (2000) suggests that new groups of life evolved during this period, including the red algae and green algae, stramenopiles, ciliates, dinoflagellates, and testate amoeba.[17]

The end of the period also saw the origin of heterotrophic plankton, which would feed on unicellular algae and prokaryotes, ending the bacterial dominance of the oceans.[18]

## See also

* Earth:Timeline of glaciation - Chronology of the major ice ages of the Earth

## References

1. ↑ Shields-Zhou, Graham A.; Porter, Susannah; Halverson, Galen P. (2016). "A new rock-based definition for the Cryogenian Period (circa 720 – 635 Ma)". Episodes 39 (1): 3–8. doi:10.18814/epiiugs/2016/v39i1/89231. ISSN 0705-3797. https://discovery.ucl.ac.uk/id/eprint/1496826/1/Shields-Zhou et al (2016) Cryogenian Period.pdf.
2. ↑ Knoll, Andrew H.; Walter, Malcolm R.; Narbonne, Guy M.; Christie-Black, Nicholas (3 March 2006). "The Ediacaran Period: a new addition to the geologic time scale". Lethaia 39: 13–30. doi:10.1080/00241160500409223. https://stratigraphy.org/gssps/files/ediacaran.pdf. Retrieved 6 December 2020.
3. ↑ 3.0 3.1 "Chart". International Commission on Stratigraphy. http://www.stratigraphy.org/index.php/ics-chart-timescale.
4. ↑ Plumb, Kenneth A. (1991). "New Precambrian time scale". Episodes. 2 14 (2): 134–140. doi:10.18814/epiiugs/1991/v14i2/005. http://www.stratigraphy.org/bak/Precambrian.pdf. Retrieved 7 September 2013.
5. ↑ 5.0 5.1 "GSSP Table - Precambrian". Geologic Timescale Foundation. https://engineering.purdue.edu/Stratigraphy/gssp/index.php?parentid=181.
6. ↑ 6.0 6.1 Eyles, Nicholas; Young, Grant (1994). Deynoux, M.; Miller, J.M.G.; Domack, E.W. et al.. eds. Geodynamic controls on glaciation in Earth history, in Earth's Glacial Record. Cambridge: Cambridge University Press. pp. 5–10. ISBN 0521548039. https://archive.org/details/earthsglacialrec0000unse/page/5.
7. ↑ Dave Lawrence (2003). "Microfossil lineages support sloshy snowball Earth". Geotimes. http://www.agiweb.org/geotimes/apr03/WebExtra041803.html.
8. ↑ Shields, G. A. (2008). "Palaeoclimate: Marinoan meltdown". Nature Geoscience 1 (6): 351–353. doi:10.1038/ngeo214. Bibcode: 2008NatGe...1..351S.
9. ↑ Hoffman, P.F. 2001. Snowball Earth theory
10. ↑ 10.0 10.1 Xu, Lingang; Frank, Anja B.; Lehmann, Bernd; Zhu, Jianming; Mao, Jingwen; Ju, Yongze; Frei, Robert (21 October 2019). "Subtle Cr isotope signals track the variably anoxic Cryogenian interglacial period with voluminous manganese accumulation and decrease in biodiversity" (in en). Scientific Reports 9 (1): 15056. doi:10.1038/s41598-019-51495-0. ISSN 2045-2322. PMID 31636318.
11. ↑ Freitas, B.T.; Rudnitzki, I.D.; Morais, L.; Campos, M.D.R.; Almeida, R.P.; Warren, L.V.; Boggiani, P.C.; Caetano-Filho, S. et al. (30 August 2021). "Cryogenian glaciostatic and eustatic fluctuations and massive Marinoan-related deposition of Fe and Mn in the Urucum District, Brazil" (in en). Geology 49 (12): 1478–1483. doi:10.1130/G49134.1. ISSN 0091-7613. https://pubs.geoscienceworld.org/geology/article/49/12/1478/607268/Cryogenian-glaciostatic-and-eustatic-fluctuations. Retrieved 11 September 2023.
12. ↑ Porter, S.A.; Knoll, A.H. (2000). "Testate amoeba in the Neoproterozoic Era: evidence from vase-shaped microfossils in the Chuar Group, Grand Canyon". Paleobiology 26 (3): 360–385. doi:10.1666/0094-8373(2000)026<0360:TAITNE>2.0.CO;2. ISSN 0094-8373. http://nrs.harvard.edu/urn-3:HUL.InstRepos:3708936.
13. ↑ LoveExpression error: Unrecognized word "etal". (2009). "Fossil steroids record the appearance of Demospongiae during the Cryogenian period". Nature 457 (7230): 718–721. doi:10.1038/nature07673. PMID 19194449. Bibcode: 2009Natur.457..718L. http://eaps.mit.edu/geobiology/recent pubs/Love et al 2009.pdf. Retrieved 2009-04-15.
14. ↑ Maloof, Adam C.; Rose, Catherine V.; Beach, Robert; Samuels, Bradley M.; Calmet, Claire C.; Erwin, Douglas H.; Poirier, Gerald R.; Yao, Nan et al. (17 August 2010). "Possible animal-body fossils in pre-Marinoan limestones from South Australia". Nature Geoscience 3 (9): 653–659. doi:10.1038/ngeo934. Bibcode: 2010NatGe...3..653M.
15. ↑ "Discovery of possible earliest animal life pushes back fossil record". 2010-08-17. http://www.physorg.com/news201273825.html.
16. ↑ Wallace, M.W.; Hood, A.v.S.; Woon, E.M.S.; Hoffman, K.-H.; Reed, C.P. (2014). "Enigmatic chambered structures in Cryogenian reefs: The oldest sponge-grade organisms?". Precambrian Research 255: 653–659. doi:10.1016/j.precamres.2014.09.020.
17. ↑ "Palaeos Proterozoic: Neoproterozoic: Cryogenian". http://palaeos.com/proterozoic/neoproterozoic/cryogenian/cryogenian2.html.
18. ↑ Fossil fats reveal how complex life kicked off after Snowball Earth phase

## Further reading

* "Cryogenian Period". GeoWhen Database. http://www.stratigraphy.org/geowhen/stages/Cryogenian.html.
* James G. Ogg (2004). "Status on Divisions of the International Geologic Time Scale". Lethaia 37 (2): 183-199. doi:10.1080/00241160410006492.
* Brain, C. K.; Prave, A. R.; Hoffmann, K. H.; Fallick, A. E.; Herd, D. A.; Sturrock, C.; Young, I.; Condon, D. J. et al. (2012). "The first animals: ca. 760-million-year-old sponge-like fossils from Namibia". South African Journal of Science 108: 1–8. doi:10.4102/sajs.v108i1/2.658. https://repository.up.ac.za/bitstream/2263/18222/1/Brain_First(2012).pdf.
* Hoffman, Paul F.Expression error: Unrecognized word "et". (November 8, 2017). "Snowball Earth climate dynamics and Cryogenian geology-geobiology". Science Advances (American Association for the Advancement of Science) 3 (11): e1600983. doi:10.1126/sciadv.1600983. PMID 29134193. Bibcode: 2017SciA....3E0983H.

## External links

* The Time Travellers Guide to Australia (2012) on IMDb
* Miracle Planet : Snowball Earth on YouTube (2010s) BBC/CBC/NHK

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Ice ages

Quaternary /
Late Cenozoic|

| Quaternary|

* Antarctica
* Greenland
* Penultimate Glacial Period
* Last Glacial Period (Last Glacial Maximum)
* 1st: Würm, Wisconsin, Weichselian, Devensian/Midlandian, Pinedale/Fraser, Merida, Llanquihue
* 2nd: Riss, Illinoian, Saale, Wolstonian, Santa María
* 3rd–6th: Mindel, Pre-Illinoian, Elster, Anglian, Rio Llico
* 7th–8th: Günz, Pre-Illinoian, Elbe or Menapian, Beestonian, Caracol (2.5 to 0 Mya)

|

Pliocene
Miocene
Oligocene|

* Antarctic (34 to 2.5 Mya)

Carboniferous–Permian|

* Late Paleozoic icehouse (360 Mya to 260 Mya)

Late Ordovician glaciation|

* Andean-Saharan (460 Mya to 430 Mya)

Ediacaran|

* Gaskiers (579.88 to 579.63 Mya)
* Baykonurian (547 to 541.5 Mya)

Cryogenian|

* Sturtian (717 to 660 Mya); Marinoan (650 to 635 Mya)

Paleoproterozoic|

* Huronian (2.4 to 2.1 Gya)

Mesoarchean|

* Pongola (2.9 to 2.78 Gya)

Related topics|

* Greenhouse and icehouse Earth
* Great Oxygenation Event
* Snowball Earth
* Interglacial
* Milankovitch cycles
* Stadial

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