Cambrian (geology): Difference between revisions
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'''Establishing the beginning of the Cambrian strata.''' | '''Establishing the beginning of the Cambrian strata.''' | ||
Overtime, research uncovered a growing number of immediately sub-Cambrian strata. In 1952, '''Boris Sokolov''' proposed the name '''Vendian''' to label a discrete system of siliciclastic rocks.<ref>Sokolov, B.S., 1952, On the age of the old sedimentary cover of the Russian Platform: Izvestiya Akademii Nauk SSSR, ''Seriya geologicheskaya, v. 5,'' p. 21-31.</ref> The Vendian underlay the '''Lower Cambrian''' strata in a geological formation known as the '''Russian Platform''' in the '''Ural Mountains'''. Sokolov later expanded the '''Vendian System''' to encompass the '''Laplandian glacial level''' exposed in the Ural Mountains <ref>summarized in | Overtime, research uncovered a growing number of immediately sub-Cambrian strata. In 1952, '''Boris Sokolov''' proposed the name '''Vendian''' to label a discrete system of siliciclastic rocks.<ref>Sokolov, B.S., 1952, On the age of the old sedimentary cover of the Russian Platform: Izvestiya Akademii Nauk SSSR, ''Seriya geologicheskaya, v. 5,'' p. 21-31.</ref> The Vendian underlay the '''Lower Cambrian''' strata in a geological formation known as the '''Russian Platform''' in the '''Ural Mountains'''. Sokolov later expanded the '''Vendian System''' to encompass the '''Laplandian glacial level''' exposed in the Ural Mountains.<ref>summarized in | ||
*Sokolov, B.S., (1984). ''The Vendian System and its position in the stratigrahi scale: Proceedings of the 27th International Geological Congress (Stratigraphy), v. 1,'' p. 241-269. Cited in Andrew H. Knoll et al (2004) | *Sokolov, B.S., (1984). ''The Vendian System and its position in the stratigrahi scale: Proceedings of the 27th International Geological Congress (Stratigraphy), v. 1,'' p. 241-269. Cited in Andrew H. Knoll et al (2004) | ||
*Sokolov, B.S., (1997). ''Essays on the Establishment of the Vendian System.'' Moscow, KMK | *Sokolov, B.S., (1997). ''Essays on the Establishment of the Vendian System.'' Moscow, KMK | ||
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In 1960, '''Termier and Termier''' proposed that there was an unrecorded global '''Ediacarien interval''' that immediately preceeded the Cambrian strata (i.e. indicated immediate pre-Cambrian time).<ref>Termier, H., and Termier, G., (1960) L’Ediacarien, premier etage paleontologique. ''Revue Gen. Sci. Pure Appliquées et Bull. Assoc. France Avanc. Sci., v. 67'', p. 79-87. Cited in Andrew H. Knoll et al (2004)</ref> In addition, as suggested by Darwin, the interval contained fossils of simple animals. | In 1960, '''Termier and Termier''' proposed that there was an unrecorded global '''Ediacarien interval''' that immediately preceeded the Cambrian strata (i.e. indicated immediate pre-Cambrian time).<ref>Termier, H., and Termier, G., (1960) L’Ediacarien, premier etage paleontologique. ''Revue Gen. Sci. Pure Appliquées et Bull. Assoc. France Avanc. Sci., v. 67'', p. 79-87. Cited in Andrew H. Knoll et al (2004)</ref> In addition, as suggested by Darwin, the interval contained fossils of simple animals. | ||
By the 1960s, two significant factors were known to be manifest on a global scale: There was strong evidence of '''continental glaciation''' <ref> Harland, W.B., Armstrong, R.L., Cox, A.V., Graig, L.E., Smith, A.G., and Smith, D.G., (1989). ''A Geologic Time Scale 1989.'' Cambridge, Cambridge University Press, p. 263 Cited in Andrew H. Knoll et al (2004)</ref> and '''Ediacaran fossils''' <ref> Glaessner, M.F., 1966, Precambrian paleontology. ''Earth-Science Reviews, v.1,'' p. 29-50. Cited in Andrew H. Knoll et al (2004)</ref> | By the 1960s, two significant factors were known to be manifest on a global scale: There was strong evidence of '''continental glaciation''' <ref> Harland, W.B., Armstrong, R.L., Cox, A.V., Graig, L.E., Smith, A.G., and Smith, D.G., (1989). ''A Geologic Time Scale 1989.'' Cambridge, Cambridge University Press, p. 263 Cited in Andrew H. Knoll et al (2004)</ref> and '''Ediacaran fossils'''.<ref> Glaessner, M.F., 1966, Precambrian paleontology. ''Earth-Science Reviews, v.1,'' p. 29-50. Cited in Andrew H. Knoll et al (2004)</ref> These both had a major impact on attempts to correlated research findings regionally and globally. | ||
In 1991, the International Commission on Stratigraphy did ratify a series of '''Proterozoic periods''' but the time interval immediately prior to the Cambrian (the terminal Proterozoic period) was left undefined. The '''ICS Subcommission on the Terminal Proterozoic Period''' eventually voted a definition of initial GSSP for the Ediacaran Period, the terminal Proterozoic period, originally proposed by '''Cloud and Glaessner'''.<ref> Cloud, P.E., and Glaessner, M.F., (1982) The Ediacarian Period and System: Metazoa inherit the | In 1991, the International Commission on Stratigraphy did ratify a series of '''Proterozoic periods''' but the time interval immediately prior to the Cambrian (the terminal Proterozoic period) was left undefined. The '''ICS Subcommission on the Terminal Proterozoic Period''' eventually voted to recommend a definition of initial GSSP for the Ediacaran Period, the terminal Proterozoic period, originally proposed by '''Cloud and Glaessner'''.<ref> Cloud, P.E., and Glaessner, M.F., (1982) The Ediacarian Period and System: Metazoa inherit the | ||
Earth. ''Science, v. 217,'' p. 783-792. Cited in Andrew H. Knoll et al (2004)</ref> | Earth. ''Science, v. 217,'' p. 783-792. Cited in Andrew H. Knoll et al (2004)</ref><ref name=Knolletal-2004>[http://www.stratigraphy.org/ediacaran/Knoll_et_al_2004a.pdf The Ediacaran Period: A New Addition to the Geologic Time Scale] Andrew H. Knoll, Malcolm Walter, Guy Narbonne, and Nicholas Christie-Blick (2004). Submissions to the Terminal Proterozoic Subcommission of the International Commission on Stratigraphy</ref> | ||
==Characteristics of the Cambrian == | |||
===The time before the Cambrian Period=== | |||
The | |||
The Ediacaran Period immediately before the Cambrian Period began with the termination of the last great global glaciation when continental glaciers reached sea level in tropical latitudes (appropriately, the name of the preceding period, the '''Cryogenian''', basically means “genesis of ice”). The end of the period (marked by the initial GSSP of the Cambrian Period) is characterized by the fossils of animals who had a '''bilateral anatomic structure'''—a symmetrical left and right side as is prevalent today.<ref name=Knolletal-2004/> | |||
==Sources== | ==Sources== | ||
Revision as of 19:11, 26 April 2007
The Cambrian is both a system of strata and a period of time. The name refers to a chronostatrigraphic or a geochronological unit of geological measure. The Cambrian is roughly the period between 543 to 490 million years ago in the Paleozoic Era of the Phanerozoic Eon. It encompasses four chronostatrigraphic series and ten epochs and correspondingly, four geochronological stages and ten ages.
| Erathem/Era | System/Period | Series/Epoch | Stage/Age |
|---|---|---|---|
| Paleozoic | Cambrian | Furongian | Unnamed |
| Unnamed | |||
| Paibian | |||
| Unnamed | Unnamed | ||
| Drumian | |||
| Unnamed | |||
| Unnamed | Unnamed | ||
| Unnamed | |||
| Unnamed | Unnamed | ||
| Unnamed |
The name is derived from Cambria, the Roman word for Wales, the area where the rocks of the Cambrian was first studied.[1]
(See main article Geologic ages of earth history)
Boundaries
Geochronologically, the Cambrian Period is recognized by the ICS as the period from 542 million years ago (with an error factor plus or minus 1.0 mya) to 488.3 (plus or minus 1.7 mya).[2]
Stratigraphically, the Cambrian System (collective groups of layers or strata) is distinctive for a large increase in the fossil record indicating a significant increase in plant and animal life during that time (also referred to as the "Cambrian Explosion") [3]The lower boundry[4] is characterised by trace fossils, the lowest occurrence of Treptichnus (Phycodes) pedum and a near base of negative carbon-isotope excursion. The end or lower boundry is characterised by Conodont fossils, and the lowest occurrence of Iapetognathus fluctivagus; just above the base of Cordylodus lindstromi conodont Zone, and just below lowest occurrence of planktonic graptolites.
Historically it has been subdivided into three epochs (not recognized by the ICS)
- Early Cambrian (542 - 513 mya)
- Middle Cambrian (513 - 501 mya)
- Late Cambrian (501 - 488.3 mya)
Regional variations are also in use. An example of the Laurentian Timescale from the Geological Society of America:
Laurential Regional Designations[5]
- D Epoch
- Sunwaptan (495 – 490 mya)
- Steptoean (500 – 545 mya)
- C Epoch
- Marjuman (506 – 500 mya)
- Delamaran (512 – 516 mya)
- B Epoch
- Dyeran (516 – 512 mya)
- Montezuman (520 – 516 mya)
- A Epoch (543 – 520 mya)
Currently the Furongian Series (or Epoch) and the Paibian and Drumian Stages (or Ages) are defined and designated by name. [6] The earliest undefined series (unamed) encompasses the as yet unamed Stage 1 and Stage 2 (earliest to latest). Series 2 extends from 521 mya to 510 mya with two stages. Series 3 (from 510 to 501 mya) is composed of Stage 5, the Drumian Stage (or Age). and Stage 7. The final and last series to be created in the Cambrian, the Furongian, encompasses the Paibian Stage, Stage 9 and Stage 10 [7][8][9][10]
| System/Period | Series/Epoch | Stage/Age | Span in millions of years ago |
|---|---|---|---|
| Cambrian | Furongian | ||
| Unnamed | |||
| 492 to 488.3 mya | |||
| 496 to 492 mya | |||
| Unnamed | |||
| Paibian | |||
| 501 to 496 mya |
| System/Period | Series/Epoch | Stage/Age | Span in millions of years ago |
|---|---|---|---|
| Cambrian | Series 3 | ||
| Stage 7 | |||
| 503 to 501 mya | |||
| 506 to 503 mya | |||
| Drumian | |||
| Stage 5 | |||
| 510 to 506 mya |
| System/Period | Series/Epoch | Stage/Age | Span in millions of years ago |
|---|---|---|---|
| Cambrian | Series 2 | ||
| Stage 4 | |||
| 517 to 510 mya | |||
| 521 to 517 mya | |||
| Stage 3 |
| System/Period | Series/Epoch | Stage/Age | Span in millions of years ago |
|---|---|---|---|
| Cambrian | Series 1 | ||
| Stage 2 | |||
| 534.6 to 531 mya | |||
| 542 to 534.6 mya | |||
| Stage 1 |
GSSP
In accordance with ICS rules, a period is defined by an event recorded in rock formations termed the global stratotype section and point (GSSP). The GSSP is the reference point that defines the international “standard” for recognition of the base, or lower boundary, of the period. The initial GSSP of the beginning of the Cambrian Period is in Newfoundland, Canada.[11]
Defining the Cambrian Period
Developing the parameters of the Cambrian
Originally the Cambrian was an undefined period noted for the apparently sudden and unexplained appearance of complex animals. Charles Darwin referred to this as the stratigraphic product of massive record failure. [12]
In 1914, Charles Doolittle Walcott later expanded on Darwin’s view, defining a Lipalian Interval as “the unrecorded period of time reflected in the unconformity between lowermost Cambrian strata and the (commonly deformed) rocks that lay beneath them.” In other words, the beginning of the Cambrian period was not clearly marked. However, there were other stratigraphers at that time who knew there were successive Cambrian layers in various regions that lay atop distinctive, that is to say, discernable sedimentary layers up to thousands of meters in thickness. Wolcott and Darwin did not have a complete picture from which to work.
Establishing the beginning of the Cambrian strata.
Overtime, research uncovered a growing number of immediately sub-Cambrian strata. In 1952, Boris Sokolov proposed the name Vendian to label a discrete system of siliciclastic rocks.[13] The Vendian underlay the Lower Cambrian strata in a geological formation known as the Russian Platform in the Ural Mountains. Sokolov later expanded the Vendian System to encompass the Laplandian glacial level exposed in the Ural Mountains.[14]
In 1960, Termier and Termier proposed that there was an unrecorded global Ediacarien interval that immediately preceeded the Cambrian strata (i.e. indicated immediate pre-Cambrian time).[15] In addition, as suggested by Darwin, the interval contained fossils of simple animals.
By the 1960s, two significant factors were known to be manifest on a global scale: There was strong evidence of continental glaciation [16] and Ediacaran fossils.[17] These both had a major impact on attempts to correlated research findings regionally and globally.
In 1991, the International Commission on Stratigraphy did ratify a series of Proterozoic periods but the time interval immediately prior to the Cambrian (the terminal Proterozoic period) was left undefined. The ICS Subcommission on the Terminal Proterozoic Period eventually voted to recommend a definition of initial GSSP for the Ediacaran Period, the terminal Proterozoic period, originally proposed by Cloud and Glaessner.[18][19]
Characteristics of the Cambrian
The time before the Cambrian Period
The Ediacaran Period immediately before the Cambrian Period began with the termination of the last great global glaciation when continental glaciers reached sea level in tropical latitudes (appropriately, the name of the preceding period, the Cryogenian, basically means “genesis of ice”). The end of the period (marked by the initial GSSP of the Cambrian Period) is characterized by the fossils of animals who had a bilateral anatomic structure—a symmetrical left and right side as is prevalent today.[19]
Sources
- Proposed Global Standard Stratotype-Section and Point for the Paibian Stage and Furongian Series (Upper Cambrian) International Subcommission on Cambrian Stratigraphy, International Commission on Stratigraphy (ICS), International Union of Geological Sciences (IUGS).
- Subcommission on Neoproterozoic Stratigraphy International Commission on Stratigraphy (ICS), International Union of Geological Sciences (IUGS).
- EarthTime
References
- ↑ Glossary Illinois State Geological Survey
- ↑ All ICS chronological data are given with boundaries of plus or minus millions of years ago (mya).
- ↑ Geologists seek to put an end to blind dates Tom Clarke (2003) Nature|Vol 425: 9 October. Reprinted from www.nature.com/nature
- ↑ At the upper most boundary of the Ediacaran system/period in the Neoproterozoic Erathem/Era in the Proterozoic Eonothem/Era of the Precambrian
- ↑ 1999 Geologic Time Scale The Geological Society of America. Compilers: A. R. Palmer, John Geissman. Note: Only a few internationally defined ages have been established. These are regional (Laurentian) only. Limits (referred to a "Boundary Picks") were based on dating techniques and fossil records current in 1999. Sources for nomenclature and ages:
- Primarily from Gradstein, F., and Ogg, J., 1996, Episodes, v. 19, nos. 1 & 2; Gradstein, F., et al., 1995,
- SEPM Special Pub. 54, p. 95–128; Berggren, W. A., et al., 1995,
- SEPM Special Pub. 54, p. 129–212; Cambrian and basal Ordovician ages adapted from Landing, E., 1998, Canadian Journal of Earth Sciences, v. 35, p. 329–338; *Davidek, K., et al., 1998, Geological Magazine, v. 135, p. 305–309.
- Cambrian age names from Palmer, A. R., 1998, Canadian Journal of Earth Sciences, v. 35, p. 323–328.
- ↑ Note: All other series and stages are as yet unmamed and referred to simply as "Series" or "Stage", by the ICS.
- ↑ Cambrian Period GeoWhen
- ↑ International Stratigraphic Chart International Commission on Stratigraphy (ICS), International Union of Geological Sciences (IUGS).
- ↑ Subcommission on Neoproterozoic Stratigraphy International Commission on Stratigraphy (ICS), International Union of Geological Sciences (IUGS)
- ↑ Evolving Time Scale EarthTime
- ↑ A new period for a geological time scale Andrew H. Knoll, Malcolm R.Walter, Guy M. Narbonne, Nicholas Christie-Blick (2004) Science. vol. 305, July
- ↑ The Origin of Species, Charles Darwin (1859). Cited in Andrew H. Knoll et al (2004)
- ↑ Sokolov, B.S., 1952, On the age of the old sedimentary cover of the Russian Platform: Izvestiya Akademii Nauk SSSR, Seriya geologicheskaya, v. 5, p. 21-31.
- ↑ summarized in
- Sokolov, B.S., (1984). The Vendian System and its position in the stratigrahi scale: Proceedings of the 27th International Geological Congress (Stratigraphy), v. 1, p. 241-269. Cited in Andrew H. Knoll et al (2004)
- Sokolov, B.S., (1997). Essays on the Establishment of the Vendian System. Moscow, KMK
- ↑ Termier, H., and Termier, G., (1960) L’Ediacarien, premier etage paleontologique. Revue Gen. Sci. Pure Appliquées et Bull. Assoc. France Avanc. Sci., v. 67, p. 79-87. Cited in Andrew H. Knoll et al (2004)
- ↑ Harland, W.B., Armstrong, R.L., Cox, A.V., Graig, L.E., Smith, A.G., and Smith, D.G., (1989). A Geologic Time Scale 1989. Cambridge, Cambridge University Press, p. 263 Cited in Andrew H. Knoll et al (2004)
- ↑ Glaessner, M.F., 1966, Precambrian paleontology. Earth-Science Reviews, v.1, p. 29-50. Cited in Andrew H. Knoll et al (2004)
- ↑ Cloud, P.E., and Glaessner, M.F., (1982) The Ediacarian Period and System: Metazoa inherit the Earth. Science, v. 217, p. 783-792. Cited in Andrew H. Knoll et al (2004)
- ↑ 19.0 19.1 The Ediacaran Period: A New Addition to the Geologic Time Scale Andrew H. Knoll, Malcolm Walter, Guy Narbonne, and Nicholas Christie-Blick (2004). Submissions to the Terminal Proterozoic Subcommission of the International Commission on Stratigraphy