From Wikipedia, the free encyclopedia

The Cambrian is a major division of the geologic timescale that begins about 542 ± 1.0 Ma (million years ago) at the end of the Proterozoic eon and ended about 488.3 ± 1.7 Ma with the beginning of the Ordovician period (ICS, 2004)^[2]. It is the first period of the Paleozoic era of the Phanerozoic eon. The Cambrian takes its name from Cambria, the classical name for Wales, the area where rocks from this time period were first studied.

The Cambrian is the earliest period in whose rocks are found numerous large, distinctly fossilizable multicellular organisms that are more complex than sponges or medusoids. This sudden appearance of hard body fossils is referred to as the Cambrian explosion.

Contents 1 Cambrian subdivisions 1.1 Cambrian dating 2 Cambrian paleogeography 3 Cambrian fauna 3.1 Cambrian flora 4 See also 5 References 6 External links

The Cambrian period follows after the Neoproterozoic and is followed by the Ordovician period. The Cambrian is divided into three epochs — the Early Cambrian (Caerfai or Waucoban), Middle Cambrian (St Davids or Albertian) and Furongian (also known as Late Cambrian, Merioneth or Croixan). Rocks of these epochs are referred to as belonging to the Lower, Middle, or Upper Cambrian.

Each of the epochs are divided into two faunal stages. Only one, the Paibian, has been recognized by the International Commission on Stratigraphy, and others are still unnamed. However, the Cambrian is divided into several regional faunal stages:

	Chinese	North American	Russian-Kazakhian	Australian	Regional
Furongian		Ibexian (part)	Ayusokkanian	Idamean	Dolgellian
		Sunwaptan	Sakian	Mindyallan	Festiniogian
		Steptoan	Aksayan	Payntonian	Maentwrogian
		Marjuman	Batyrbayan
Middle Cambrian	Maozhangian		Mayan	Boomerangian
	Zuzhuangian	Delamaran	Amgan	Undillian
	Zhungxian			Florian
				Templetonian
		Dyeran		Ordian
Early Cambrian	Longwangmioan		Toyonian		Lenian
	Changlangpuan	Montezuman	Botomian
	Qungzusian		Atdabanian
	Meishuchuan		Tommotian
			Nemakit-Daldynian

The time range for the Cambrian has classically been thought to have been from about 500 mya to about 570 mya. The lower boundary of the Cambrian was traditionally set at the earliest appearance of early arthropods known as trilobites and of primitive reef-forming animals known as archeocyathids.

The end of the period was eventually set at a fairly definite faunal change now identified as an extinction event. Fossil discoveries and radioactive dating in the last quarter of the 20th century have called these dates into question. Date inconsistencies as large as 20 Ma are common between authors. Framing dates of ca. () 545 to 490 mya were proposed by the International Subcommission on Global Stratigraphy as recently as 2002.

A radiometric date from New Brunswick puts the end of the first stage of the Cambrian around 511 mya. This leaves 21 Ma for the other two stages of the Cambrian.

A more precise date of 542 ± 0.3 mya for the extinction event at the beginning of the Cambrian has recently been submitted.^[1] The rationale for this precise dating is interesting in itself as an example of paleological deductive reasoning. Exactly at the Cambrian boundary there is a marked fall in the abundance of carbon-13, a "reverse spike" that paleontologists call an excursion. It is so widespread that it is the best indicator of the position of the Precambrian-Cambrian boundary in stratigraphic sequences of roughly this age. One of the places that this well-established carbon-13 excursion occurs is in Oman. Amthor (2003) describes evidence from Oman that indicates the carbon-isotope excursion relates to a mass extinction: the disappearance of distinctive fossils from the Precambrian coincides exactly with the carbon-13 anomaly. Fortunately, in the Oman sequence, so too does a volcanic ash horizon from which zircons provide a very precise age of 542 ± 0.3 Ma (calculated on the decay rate of uranium to lead). This new and precise date tallies with the less precise dates for the carbon-13 anomaly, derived from sequences in Siberia and Namibia. It is presented here as likely to become accepted as the definitive age for the start of the Phanerozoic eon, and thus the start of the Paleozoic era and the Cambrian period.

Cambrian continents are thought to have resulted from the breakup of a Neoproterozoic supercontinent called Pannotia. The waters of the Cambrian period appear to have been widespread and shallow. Gondwana remained the largest supercontinent after the breakup of Pannotia. It is thought that Cambrian climates were significantly warmer than those of preceding times that experienced extensive ice ages discussed as the Varanger glaciation. Also there was no glaciation at the poles. Continental drift rates in the Cambrian may have been anomalously high. Laurentia, Baltica and Siberia remained independent continents since the break-up of the supercontinent of Pannotia. Gondwana started to drift towards the South Pole. Panthalassa covered most of the southern hemisphere, and minor oceans included the Proto-Tethys Ocean, Iapetus Ocean, and Khanty Ocean, all of which expanded by this time.

Of those modern animal phyla that fossilize easily, all save the bryozoans appear to have representatives in the Cambrian, and of these most (except the considerably older sponges) seem to have originated near the start of the period. Many extinct phyla and odd animals that have unclear relationships to other animals also appear in the Cambrian. The apparent "sudden" appearance of very diverse faunas over a period of no more than a few tens of millions of years is referred to as the "Cambrian Explosion". Also, the first possible tracks on land, such as Protichnites and Climactichnites, dating to about 530 mya and found in Ontario, Canada, and northern United States, appeared at this time. The conodonts, small predatory primitive chordates known from their fossilised teeth, also appeared during the Furongian epoch of the Cambrian period. The conodonts thrived throughout the Paleozoic and the early Mesozoic until they completely disappeared during the Late Triassic period when the first mammals were evolving.

The best studied sites where the soft parts of organisms have fossilized are in the Burgess shale of British Columbia. They represent strata from the Middle Cambrian and provide us with a wealth of information on early animal diversity. Similar faunas have subsequently been found in a number of other places — most importantly in very early Cambrian shales in the People's Republic of China's Yunnan Province (see Maotianshan shales). Fairly extensive Precambrian Ediacaran faunas have been identified in the past 50 years, but their relationships to Cambrian forms are quite obscure.

Generally it is accepted that there were no land plants at this time although molecular dating suggests that land plant ancestors diverged from the algae much earlier, in the Neoproterozoic about 700 ma^{[citation needed]}, and that fungi diverged from the animals about 1 billion years ago^{[citation needed]}. The land at this time was barren, mostly desert and badlands.^{[citation needed]}

• List of fossil sites (with link directory)

• Gould, Stephen Jay; Wonderful Life: the Burgess Shale and the Nature of Life (New York: Norton, 1989)
• Amthor, J. E.; and others (2003). "Extinction of Cloudina and Namacalathus at the Precambrian-Cambrian boundary in Oman". Geology 31: pp 431–434. doi:10.1130/0091-7613(2003)031<0431:EOCANA>2.0.CO;2 10.1130/0091-7613(2003)031<0431:EOCANA>2.0.CO;2 . 
• Ogg, Jim; June, 2004, Overview of Global Boundary Stratotype Sections and Points (GSSP's) http://www.stratigraphy.org/gssp.htm Accessed April 30, 2006.

• Weird Life on the Mats
• Photos of Cambrian trace fossils and stranded jellyfish
• Dr. Sam Gon's trilobite pages (contains numerous Cambrian trilobites)
  • Biostratigraphy - includes information on Cambrian trilobite biostratigraphy
• Report on the web on Amthor and others from Geology vol. 31
• Paleomap Project
• Examples of Cambrian Fossils

Cambrian period
Early Cambrian	Middle Cambrian	Furongian
Stage 1 | Stage 2	Stage 3 | Stage 4 | Stage 5 Stage 6 | Stage 7	Paibian | Stage 9 Stage 10

Paleozoic era
Cambrian	Ordovician	Silurian	Devonian	Carboniferous	Permian