The Info List - Precambrian

The Precambrian
(or Pre-Cambrian, sometimes abbreviated pЄ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic
Eon. The Precambrian
is so named because it preceded the Cambrian, the first period of the Phanerozoic
eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian
accounts for 88% of the Earth's geologic time. The Precambrian
(colored green in the timeline figure) is an informal unit of geologic time,[1] subdivided into three eons (Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago (Ga) to the beginning of the Cambrian
Period, about 541 million years ago (Ma), when hard-shelled creatures first appeared in abundance.


1 Overview 2 Life forms 3 Planetary environment and the oxygen catastrophe 4 Subdivisions 5 Precambrian
supercontinents 6 See also 7 References 8 Further reading 9 External links

Overview[edit] Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian
fossil record is poorer than that of the succeeding Phanerozoic, and fossils from the Precambrian
(e.g. stromatolites) are of limited biostratigraphic use.[2] This is because many Precambrian rocks have been heavily metamorphosed, obscuring their origins, while others have been destroyed by erosion, or remain deeply buried beneath Phanerozoic
strata.[2][3][4] It is thought that the Earth coalesced from material in orbit around the Sun at roughly 4,543 Ma, and may have been struck by a very large (Mars-sized) planetesimal shortly after it formed, splitting off material that formed the Moon
(see Giant impact hypothesis). A stable crust was apparently in place by 4,433 Ma, since zircon crystals from Western Australia
Western Australia
have been dated at 4,404 ± 8 Ma.[5] The term "Precambrian" is recognized by the International Commission on Stratigraphy as the only "supereon" in geologic time;[citation needed] it is so called because it includes the Hadean
(~4.6—4 billion), Archean
(4—2.5 billion), and Proterozoic
(2.5 billion—541 million) eons. (There is only one other eon: the Phanerozoic, 541 million-present.)[6] "Precambrian" is still used by geologists and paleontologists for general discussions not requiring the more specific eon names. As of 2010[update], the United States Geological Survey
United States Geological Survey
considers the term informal, lacking a stratigraphic rank.[7]

Life forms[edit] Further information: Origin of life
Origin of life
and Earliest known life forms Landmass positions near the end of the Precambrian A specific date for the origin of life has not been determined. Carbon found in 3.8 billion-year-old rocks ( Archean
eon) from islands off western Greenland
may be of organic origin. Well-preserved microscopic fossils of bacteria older than 3.46 billion years have been found in Western Australia.[8] Probable fossils 100 million years older have been found in the same area. However, there is evidence that life could have evolved over 4.280 billion years ago.[9][10][11][12] There is a fairly solid record of bacterial life throughout the remainder (Proterozoic eon) of the Precambrian. Excluding a few contested reports of much older forms from North America and India, the first complex multicellular life forms seem to have appeared at roughly 1500 Ma, in the Mesoproterozoic era of the Proterozoic
eon.[citation needed] Fossil evidence from the later Ediacaran
period of such complex life comes from the Lantian formation, at least 580 million years ago. A very diverse collection of soft-bodied forms is found in a variety of locations worldwide and date to between 635 and 542 Ma. These are referred to as Ediacaran
or Vendian biota. Hard-shelled creatures appeared toward the end of that time span, marking the beginning of the Phanerozoic
eon. By the middle of the following Cambrian
period, a very diverse fauna is recorded in the Burgess Shale, including some which may represent stem groups of modern taxa. The increase in diversity of lifeforms during the early Cambrian
is called the Cambrian
explosion of life.[13][14] While land seems to have been devoid of plants and animals, cyanobacteria and other microbes formed prokaryotic mats that covered terrestrial areas.[15] Tracks from an animal with leg like appendages have been found in what was mud 551 million years ago.[16]

Planetary environment and the oxygen catastrophe[edit] Weathered Precambrian
pillow lava in the Temagami Greenstone Belt
Temagami Greenstone Belt
of the Canadian Shield Evidence of the details of plate motions and other tectonic activity in the Precambrian
has been poorly preserved. It is generally believed that small proto-continents existed prior to 4280 Ma, and that most of the Earth's landmasses collected into a single supercontinent around 1130 Ma. The supercontinent, known as Rodinia, broke up around 750 Ma. A number of glacial periods have been identified going as far back as the Huronian epoch, roughly 2400–2100 Ma. One of the best studied is the Sturtian-Varangian glaciation, around 850–635 Ma, which may have brought glacial conditions all the way to the equator, resulting in a "Snowball Earth". The atmosphere of the early Earth is not well understood. Most geologists believe it was composed primarily of nitrogen, carbon dioxide, and other relatively inert gases, and was lacking in free oxygen. There is, however, evidence that an oxygen-rich atmosphere existed since the early Archean.[17] At present, it is still believed that molecular oxygen was not a significant fraction of Earth's atmosphere
Earth's atmosphere
until after photosynthetic life forms evolved and began to produce it in large quantities as a byproduct of their metabolism. This radical shift from a chemically inert to an oxidizing atmosphere caused an ecological crisis, sometimes called the oxygen catastrophe. At first, oxygen would have quickly combined with other elements in Earth's crust, primarily iron, removing it from the atmosphere. After the supply of oxidizable surfaces ran out, oxygen would have begun to accumulate in the atmosphere, and the modern high-oxygen atmosphere would have developed. Evidence for this lies in older rocks that contain massive banded iron formations that were laid down as iron oxides.

Subdivisions[edit] Main article: Timetable of the Precambrian Life timelineThis box: viewtalkedit-4500 —–-4000 —–-3500 —–-3000 —–-2500 —–-2000 —–-1500 —–-1000 —–-500 —–0 —waterSingle-celled lifephotosynthesisEukaryotesMulticellular lifeArthropods and MolluscsPlantsDinosaursMammalsFlowersBirdsPrimates           ←Earth (−4540)←Earliest water←Earliest life←Earliest oxygen←Atmospheric oxygen← Oxygen
crisis←Sexual reproduction←Earliest plants← Ediacaran
biota←Cambrian explosion←Tetrapoda←Earliest apesPhanerozoicProterozoicArcheanHadeanPongolaHuronianCryogenianAndeanPaleozoicQuaternaryIce AgesAxis scale: million years (See also: Human timeline, and Nature timeline.)

A terminology has evolved covering the early years of the Earth's existence, as radiometric dating has allowed real dates to be assigned to specific formations and features.[18] The Precambrian
is divided into three eons: the Hadean
(4600–4000 Ma), Archean (4000-2500 Ma) and Proterozoic
(2500-541 Ma). See Timetable of the Precambrian.

Proterozoic: this eon refers to the time from the lower Cambrian boundary, 541 Ma, back through 2500 Ma. As originally used, it was a synonym for "Precambrian" and hence included everything prior to the Cambrian
boundary. The Proterozoic
eon is divided into three eras: the Neoproterozoic, Mesoproterozoic and Paleoproterozoic. Neoproterozoic: The youngest geologic era of the Proterozoic
Eon, from the Cambrian
Period lower boundary (541 Ma) back to 1000 Ma. The Neoproterozoic corresponds to Precambrian
Z rocks of older North American geology. Ediacaran: The youngest geologic period within the Neoproterozoic Era. The "2012 Geologic Time Scale" dates it from 541 to 635 Ma. In this period the Ediacaran
fauna appeared. Cryogenian: The middle period in the Neoproterozoic Era: 635-720 Ma. Tonian: the earliest period of the Neoproterozoic Era: 720-1000 Ma. Mesoproterozoic: the middle era of the Proterozoic
Eon, 1000-1600 Ma. Corresponds to " Precambrian
Y" rocks of older North American geology. Paleoproterozoic: oldest era of the Proterozoic
Eon, 1600-2500 Ma. Corresponds to " Precambrian
X" rocks of older North American geology. Archean
Eon: 2500-4000 Ma. Hadean
Eon: 4000–4600 Ma. This term was intended originally to cover the time before any preserved rocks were deposited, although some zircon crystals from about 4400 Ma demonstrate the existence of crust in the Hadean
Eon. Other records from Hadean
time come from the moon and meteorites.[19] It has been proposed that the Precambrian
should be divided into eons and eras that reflect stages of planetary evolution, rather than the current scheme based upon numerical ages. Such a system could rely on events in the stratigraphic record and be demarcated by GSSPs. The Precambrian
could be divided into five "natural" eons, characterized as follows:[20]

Accretion and differentiation: a period of planetary formation until giant Moon-forming impact event. Hadean: dominated by heavy bombardment from about 4.51 Ga (possibly including a Cool Early Earth period) to the end of the Late Heavy Bombardment period. Archean: a period defined by the first crustal formations (the Isua greenstone belt) until the deposition of banded iron formations due to increasing atmospheric oxygen content. Transition: a period of continued iron banded formation until the first continental red beds. Proterozoic: a period of modern plate tectonics until the first animals. Precambrian
supercontinents[edit] The movement of Earth's plates has caused the formation and break-up of continents over time, including occasional formation of a supercontinent containing most or all of the landmass. The earliest known supercontinent was Vaalbara. It formed from proto-continents and was a supercontinent 3.636 billion years ago. Vaalbara
broke up c. 2.845–2.803 Ga ago. The supercontinent Kenorland was formed c. 2.72 Ga ago and then broke sometime after 2.45–2.1 Ga into the proto-continent cratons called Laurentia, Baltica, Yilgarn craton, and Kalahari. The supercontinent Columbia or Nuna formed 2.06–1.82 billion years ago and broke up about 1.5–1.35 billion years ago.[21][22][not in citation given] The supercontinent Rodinia
is thought to have formed about 1.13–1.071 billion years ago, to have embodied most or all of Earth's continents and to have broken up into eight continents around 750–600 million years ago.

See also[edit]

portal Phanerozoic – Fourth and current eon of the geological timescale Paleozoic – First era of the Phanerozoic
Eon Mesozoic – Second era of the Phanerozoic
Eon, also known as Age of Reptiles Cenozoic – Third and current era of the Phanerozoic
Eon References[edit]

^ Gradstein, F.M.; Ogg, J.G.; Schmitz, M.D.; Ogg, G.M. (editors) (2012). The Geologic Timescale 2012 (volume 1). Elsevier. p. 301. ISBN 978-0-44-459390-0.CS1 maint: Multiple names: authors list (link) CS1 maint: Extra text: authors list (link).mw-parser-output cite.citation font-style:inherit .mw-parser-output .citation q quotes:"""""""'""'" .mw-parser-output .citation .cs1-lock-free a background:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center .mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration a background:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center .mw-parser-output .citation .cs1-lock-subscription a background:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center .mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration color:#555 .mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration span border-bottom:1px dotted;cursor:help .mw-parser-output .cs1-ws-icon a background:url("//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/12px-Wikisource-logo.svg.png")no-repeat;background-position:right .1em center .mw-parser-output code.cs1-code color:inherit;background:inherit;border:inherit;padding:inherit .mw-parser-output .cs1-hidden-error display:none;font-size:100% .mw-parser-output .cs1-visible-error font-size:100% .mw-parser-output .cs1-maint display:none;color:#33aa33;margin-left:0.3em .mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-format font-size:95% .mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-left padding-left:0.2em .mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-right padding-right:0.2em

^ a b Monroe, James S.; Wicander, Reed (1997). The Changing Earth: Exploring Geology and Evolution (2nd ed.). Belmont: Wadsworth Publishing Company. p. 492. ISBN 9781285981383.

^ Levin, Harold L. (25 October 2005). "The Earliest Earth: 2,100,000,000 years of the Archean
Eon". In Gore, Pamela J.W. (ed.). The Earth Through Time. p. 1.

^ Davis, C.M. (1964). "The Precambrian
Era". Readings in the Geography of Michigan. Michigan State University.

^ "Zircons are Forever". Department of Geoscience. 2005. Retrieved 28 April 2007.

^ Fan, Junxuan; Hou, Xudong (February 2017). "Chart". International Commission on Stratigraphy. International Chronostratigraphic Chart. Retrieved 10 May 2018.

^ U.S. Geological Survey Geologic Names Committee (2010), "Divisions of geologic time—major chronostratigraphic and geochronologic units", U.S. Geological Survey Fact Sheet 2010–3059, United States Geological Survey, p. 2, retrieved 20 June 2018

^ Brun, Yves; Shimkets, Lawrence J. (January 2000). Prokaryotic development. ASM Press. p. 114. ISBN 978-1-55581-158-7.

^ Dodd, Matthew S.; Papineau, Dominic; Grenne, Tor; slack, John F.; Rittner, Martin; Pirajno, Franco; O'Neil, Jonathan; Little, Crispin T. S. (2 March 2017). "Evidence for early life in Earth's oldest hydrothermal vent precipitates". Nature. 543 (7643): 60–64. Bibcode:2017Natur.543...60D. doi:10.1038/nature21377. PMID 28252057. Archived from the original on 10 February 2017. Retrieved 2 March 2017.

^ Zimmer, Carl (1 March 2017). "Scientists Say Canadian Bacteria Fossils May Be Earth's Oldest". The New York Times. Retrieved 2 March 2017.

^ Ghosh, Pallab (1 March 2017). "Earliest evidence of life on Earth 'found'". BBC News. Retrieved 2 March 2017.

^ Dunham, Will (1 March 2017). "Canadian bacteria-like fossils called oldest evidence of life". Reuters. Retrieved 1 March 2017.

^ Fedonkin, Mikhail A.; Gehling, James G.; Grey, Kathleen; Narbonne, Guy M.; Vickers-Rich, Patricia (2007). The Rise of Animals: Evolution and Diversification of the Kingdom Animalia. JHU Press. p. 326. doi:10.1086/598305. ISBN 9780801886799.

^ Dawkins, Richard; Wong, Yan (2005). The Ancestor's Tale: A Pilgrimage to the Dawn of Evolution. Houghton Mifflin Harcourt. p. 673. ISBN 9780618619160.

^ Selden, Paul A. (2005). "Terrestrialization (Precambrian-Devonian)" (PDF). Terrestrialization (Precambrian–Devonian). Encyclopedia of Life Sciences. John Wiley & Sons, Ltd. doi:10.1038/npg.els.0004145. ISBN 978-0470016176.

^ Scientists discover 'oldest footprints on Earth' in southern China dating back 550 million years The Independent

^ Clemmey, Harry; Badham, Nick (1982). " Oxygen
in the Precambrian Atmosphere". Geology. 10 (3): 141–146. Bibcode:1982Geo....10..141C. doi:10.1130/0091-7613(1982)10<141:OITPAA>2.0.CO;2.

^ Geological Society of America's "2009 GSA Geologic Time Scale."

^ "Archived copy". Archived from the original on 2012-05-10. Retrieved 2011-03-27.CS1 maint: Archived copy as title (link)

^ Bleeker, W. (2004) [2004]. "Toward a "natural" Precambrian
time scale". In Felix M. Gradstein; James G. Ogg; Alan G. Smith (eds.). A Geologic Time Scale 2004. Cambridge University Press. ISBN 978-0-521-78673-7. also available at Stratigraphy.org: Precambrian

^ Zhao, Guochun; Cawood, Peter A.; Wilde, Simon A.; Sun, M. (2002). "Review of global 2.1–1.8 Ga orogens: implications for a pre-Rodinia super-continent". Earth-Science Reviews. 59 (1): 125–162. Bibcode:2002ESRv...59..125Z. doi:10.1016/S0012-8252(02)00073-9.

^ Zhao, Guochun; Sun, M.; Wilde, Simon A.; Li, S.Z. (2004). "A Paleo- Mesoproterozoic super-continent: assembly, growth and breakup". Earth-Science Reviews (Submitted manuscript). 67 (1): 91–123. Bibcode:2004ESRv...67...91Z. doi:10.1016/j.earscirev.2004.02.003.

Further reading[edit] Valley, John W., William H. Peck, Elizabeth M. King (1999) Zircons Are Forever, The Outcrop for 1999, University of Wisconsin-Madison Wgeology.wisc.edu – Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago Accessed Jan. 10, 2006 Wilde, S. A.; Valley, J. W.; Peck, W. H.; Graham, C. M. (2001). "Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago". Nature. 409 (6817): 175–178. doi:10.1038/35051550. PMID 11196637. Wyche, S.; Nelson, D. R.; Riganti, A. (2004). "4350–3130 Ma detrital zircons in the Southern Cross Granite–Greenstone Terrane, Western Australia: implications for the early evolution of the Yilgarn Craton". Australian Journal of Earth Sciences. 51 (1): 31–45. Bibcode:2004AuJES..51...31W. doi:10.1046/j.1400-0952.2003.01042.x.

Wikimedia Commons has media related to Precambrian. External links[edit] Late Precambrian
and Ice House World from the Paleomap Project

vteGeological history of EarthCenozoic era'"`UNIQ--templatestyles-00000031-QINU`"'(present–66.0 Mya) Quaternary
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(5.333–23.03 Mya) Paleogene (23.03–66.0 Mya) Oligocene
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(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
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(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 era (541.0 Mya–1 Gya) Ediacaran
(541.0–~635 Mya) Cryogenian (~635–~720 Mya) Tonian (~720 Mya–1 Gya) Mesoproterozoic era (1–1.6 Gya) Stenian (1–1.2 Gya) Ectasian (1.2–1.4 Gya) Calymmian (1.4–1.6 Gya) Paleoproterozoic era (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, Geology Portal Authority control GND: 4046985