Chert
Sedimentary rock | |
Composition | |
---|---|
Microcrystalline or cryptocrystalline quartz |
Chert (/ˈtʃɜːrt/) is a hard, fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline quartz,[1] the mineral form of silicon dioxide (SiO2).[2] Chert is characteristically of biological origin, but may also occur inorganically as a chemical precipitate or a diagenetic replacement, as in petrified wood.[3]
Chert is typically composed of the petrified remains of siliceous ooze, the biogenic sediment that covers large areas of the deep ocean floor, and which contains the silicon skeletal remains of diatoms, silicoflagellates, and radiolarians.[4] Precambrian cherts are notable for the presence of fossil cyanobacteria.[5] In addition to microfossils,[4] chert occasionally contains macrofossils.[6][7] However, some chert is devoid of any fossils.[8]
Chert varies greatly in color, from white to black, but is most often found as gray, brown, grayish brown and light green to rusty red[9][10] and occasionally as dark green.[11] Its color is an expression of trace elements present in the rock. Both red and green are most often related to traces of iron in its oxidized and reduced forms, respectively.[4][12]
Description
In
The
Chert is found in settings as diverse as
Bedded chert
Bedded chert, also known as ribbon chert, takes the form of thinly
Seawater typically contains between 0.01 and 11
The skeletons of these organisms are composed of opal-A, an amorphous form of silica, lacking long-range crystal structure. This is gradually transformed to opal-CT, a microcrystalline form of silica composed mostly of bladed crystals of cristobalite and tridymite.[29] Much opal-CT takes the form of lepispheres, which are clusters of bladed crystals about 10 microns in diameter.[30] Opal-CT in turn transforms to microquartz. In deep ocean water, the transition to opal-CT occurs at a temperature of about 45 °C (113 °F) while the transition to microquartz occurs at a temperature of about 80 °C (176 °F). However, the transition temperature varies considerably, and the transition is hastened by the presence of magnesium hydroxide, which provides a nucleus for the recrystallization. Megaquartz forms at elevated temperatures typical of metamorphism.[29]
There is evidence that the variety of chert called
Subvarieties
Bedded cherts can be further subdivided by the kinds of organisms that produced the silica skeletons.[23]
Diatomaceous chert consists of beds and lenses of
Spicularite is chert composed of spicules of glass sponges and other invertebrates. When densely cemented, it is known as spicular chert. They are found in association with
Some bedded cherts appear devoid of fossils even under close microscopic examination. Their origin is uncertain, but they may form from fossil remains that are completely dissolved in fluids that then migrate to precipitate their silica load in a nearby bed.[35][36] Eolian quartz has also been suggested as a source of silica for chert beds.[37] Precambrian bedded cherts are common, making up 15% of middle Precambrian sedimentary rock,[21] and may have been deposited nonbiologically in oceans more saturated in silica than the modern ocean. The high degree of silica saturation was due either to intense volcanic activity or to the lack of modern organisms that remove silica from seawater.[38]
Nodular chert
Nodular chert is most common in limestone but may also be found in
Nodular chert is often dark in color with a white weathering rind.[25]
Most chert nodules have textures suggesting they were formed by diagenetic replacement, where silica was deposited in place of calcium carbonate or clay minerals.[8] This may have taken place where meteoric water (water derived from snow or rain) mixed with saltwater in the sediment beds, where carbon dioxide was trapped, producing an environment supersaturated with silica and undersaturated with calcium carbonate.[1] Nodular chert is particularly common in continental shelf environments.[38] In the Permian Basin (North America), chert nodules and chertified fossils are abundant in basin limestones, but there is little in the carbonate buildup zone itself. This may reflect dissolution of opal where carbonate is being actively deposited, a lack of siliceous organisms in these environments, or removal of siliceous skeletons by strong currents that redeposit the siliceous material in the deep basin.[39]
The silica in nodular chert likely precipitates as opal-A, based on internal banding in nodules,[39] and may recrystallize directly to microquartz without first recrystallizing to opal-CT.[38] Some nodular chert may precipitate directly as microquartz, due to low levels of supersaturation of silica.[25]
Other occurrences
The banded iron formations of Precambrian age are composed of alternating layers of chert and iron oxides.[40][41]
Nonmarine cherts may form in saline alkaline lakes as thin lenses or nodules showing sedimentary structures suggestive of
Chert may also form from replacement of
Fossils
The cryptocrystalline nature of chert, combined with its above average ability to resist weathering, recrystallization and metamorphism has made it an ideal rock for preservation of early life forms.[45]
For example:
- The 3.2
- The Gunflint Chert of western Ontario (1.9 to 2.3 Ga) preserves not only bacteria and cyanobacteria but also organisms believed to be ammonia-consuming and some that resemble green algae and fungus-like organisms.[48][49]
- The
- The Bitter Springs Formation of the Amadeus Basin, Central Australia, preserves 850 Ma cyanobacteria and algae.[53][54][55]
- The Rhynie chert (410 Ma) of Scotland has remains of a Devonian land flora and fauna with preservation so perfect that it allows cellular studies of the fossils.[56]
Prehistoric and historic uses
Chert is of only modest economic importance today as a source of silica (quartz sand being much more important.) However, chert deposits may be associated with valuable deposits of iron, uranium, manganese, phosphorite, and petroleum.[57]
Tools
In prehistoric times, chert was often used as a raw material for the construction of
When a chert stone is struck against an iron-bearing surface, sparks result. This makes chert an excellent tool for starting fires, and both flint and common chert were used in various types of fire-starting tools, such as
Construction
Cherts are subject to problems when used as concrete aggregates. Deeply weathered chert develops surface pop-outs when used in concrete that undergoes freezing and thawing because of the high porosity of weathered chert. The other concern is that certain cherts undergo an alkali-silica reaction with high-alkali cements. This reaction leads to cracking and expansion of concrete and ultimately to failure of the material.[60]
Varieties
There are numerous varieties of chert, classified based on their visible, microscopic and physical characteristics.[9][10] Some of the more common varieties are:
- silica. Commonly found as nodules, this variety was often used in past times to make bladed tools. Today, some geologists refer to any dark gray to black chert as flint.[61][62][63] The dark color is from inclusions of organic matter.[21] Among non-geologists, the distinction between "flint" and "chert" is often one of quality – chert being lower quality than flint. This usage of the terminology is particularly prevalent in Great Britain where most true flint (found in chalk formations) was of better quality than "common chert" (from limestone formations).[64]
- "Common chert" is a variety of chert which forms in limestone formations by replacement of calcium carbonate with silica. This is the most abundantly found variety of chert. It is generally considered to be less attractive for producing gem stones and bladed tools than flint.
- Jasper is a variety of chert formed as primary deposits, found in or in connection with magmatic formations which owes its red color to hematite inclusions. Jasper frequently also occurs in black, yellow or even green (depending on the type of iron it contains). Jasper is usually opaque to near opaque.[65] Jasper is also present in banded iron formation, where it is described as jaspilite.[8]
- Radiolarite is a variety of chert formed as primary deposits and containing
- Chalcedony is a microfibrous quartz.[16]
- Magadi-type chert is a variety that forms from a sodium silicate precursor in highly alkaline lakes such as Lake Magadi in Kenya.[68]
- Novaculite is a very dense, fine-grained, and uniform form of very pure white chert with a high content of extracrystalline water.[21] It is most common in the mid-Paleozoic rocks of Texas, Oklahoma, and Arkansas in the south-central United States, where it has undergone some metamorphism.[8]
- Porcelanite is a term used for fine-grained siliceous rocks with a texture and a fracture resembling those of unglazed porcelain. It likely forms in shallow water and is composed mostly of opal-CT.[69]
- Tripolitic chert (or tripoli) is a light-colored porous friable siliceous (largely chalcedonic) sedimentary rock, which results from the weathering (decalcification) of chert or siliceous limestone.[70]
- Siliceous sinter is porous, low-density, light-colored siliceous rock deposited by waters of hot springs and geysers.[8]
- Mozarkite a varicolored, easily polished Ordovician chert that takes a high polish. It is the state rock of Missouri.[71]
Other lesser used archaic terms for chert are firestone and silex.[72]
See also
- Petrology – Branch of geology that studies the formation, composition, distribution and structure of rocks
- Eolith – Knapped flint nodule
- Nodule (geology) – Small mass of a mineral with a contrasting composition to the enclosing sediment or rock not to be confused with Concretion
- Obsidian – Naturally occurring volcanic glass
- Opal – Hydrated amorphous form of silica
- Whinstone – Quarrying term for any hard dark-coloured rock
- Archaeology – Study of human activity via material culture
- Clovis Points – New World prehistoric projectileClovis culture in New Mexico, archaeological artefacts of the
- Piatra Tomii – late Jurassic limestone outcrop , a prehistoric chert mine in Alba County, Romania
References
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- ^ Blatt, Middleton & Murray 1980, p. 572.
- ^ Blatt & Tracy 1996, pp. 336–338.
- ^ Blatt, Middleton & Murray 1980, p. 575.
- ^ Blatt & Tracy 1996, pp. 339.
- ^ a b c d e f Blatt, Middleton & Murray 1980, p. 571.
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- ^ a b Boggs 2006, p. 208, 211-213.
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- ^ Blatt & Tracy 1996, pp. 336–337.
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- ^ Smith, Gary A.; Huckell, Bruce B. (2005). "The geological and geoarchaeological significance of Cerro Pedernal, Rio Arriba County, New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 56: 427. Retrieved 10 July 2021.
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- ^ Gunflint chert Archived 2005-06-12 at the Wayback Machine
- ^ Biogenicity of Microfossils in the Apex Chert
- ^ "Portion Of Ancient Australian Chert Microstructures Definitively Pseudo-Fossils". Carnegie Science. Carnegie Institution for Science. 16 February 2016. Retrieved 10 July 2021.
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- ^ Barbara E. Luedtke, "The Identification of Sources of Chert Artifacts", American Antiquity, Vol. 44, No.4 (Oct., 1979), 744–57.
- ISBN 0-917956-75-3. Retrieved 8 October 2020.
- ^ Bates & Jackson 1984, "Jasper".
- ISBN 047157452X.
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- ^ Bates & Jackson 1984, "Tripoli".
- ^ Bates & Jackson 1984, "Mozarkite".
- ^ Bates & Jackson 1984.
External links
- Photo & note re: Fig Tree Formation
- Microphotographs of Fig Tree fossils
- Schopf, J.W. (1999) Cradle of Life: The Discovery of Earth's Earliest Fossils, Princeton University Press, 336 p. ISBN 0-691-00230-4
- An Archaeological Guide To Chert Types Of East-Central Illinois