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Protist shell

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There are also costs for protists that carry protective shells. The diagram on the right above shows some of the energetic costs coccolithophore incur from carrying coccoliths. In the diagram, the energetic costs are reported in percentage of total photosynthetic budget. (A) represents transport
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encased in elaborate globular shells (or "capsules"), usually made of silica and pierced with holes. Their name comes from the Latin for "radius". They catch prey by extending parts of their body through the holes. As with the silica frustules of diatoms, radiolarian shells can sink to the ocean
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organisms and greatly contribute to biogenic silica production. In the open ocean, however, diatoms have a reduced role in global annual silica production. Diatoms in North Atlantic and North Pacific subtropical gyres contribute only about 6% of global annual marine silica production, while the
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There are benefits for protists that carry protective shells. The diagram on the left below shows some benefits coccolithophore get from carrying coccoliths. In the diagram, (A) represents accelerated photosynthesis including carbon concentrating mechanisms (CCM) and enhanced light uptake via
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Most protists are too small to be seen with the naked eye. They are highly diverse organisms currently organised into 18 phyla, but are not easy to classify. Studies have shown high protist diversity exists in oceans, deep sea-vents and river sediments, suggesting large numbers of eukaryotic
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crystals. (C) Mechanical and structural processes account for the secretion of the completed coccoliths that are transported from their original position adjacent to the nucleus to the cell periphery, where they are transferred to the surface of the cell.
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In addition to protection and support, protist shells also serve scientists as a means of identification. By examining the characteristics of the shells, different species of protists can be identified and their ecology and evolution can be studied.
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Southern Ocean produces about one-third of the global marine biogenic silica. The Southern Ocean is referred to as having a "biogeochemical divide", since only minuscule amounts of silicon is transported out of this region.
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form a (disputed) phylum containing about 100,000 recognised species of mainly unicellular algae. Diatoms generate about 20 per cent of the oxygen produced on the planet each year, take in over 6.7 billion metric tons of
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Foraminifera: notes for a short course organized by M.A. Buzas and B.K. Sen Gupta: prepared for the short course on foraminifera sponsored by the Paleontological Society, held at New Orleans, Louisiana, October 17,
1017:. Availability of silicon appears crucial for diatom productivity, and as long as silicic acid is available for diatoms to utilize, the diatoms contribute other important nutrient concentrations in the deep ocean. 1183: 3754:
Monteiro, F.M., Bach, L.T., Brownlee, C., Bown, P., Rickaby, R.E., Poulton, A.J., Tyrrell, T., Beaufort, L., Dutkiewicz, S., Gibbs, S. and Gutowska, M.A. (2016) "Why marine phytoplankton calcify".
2167:. These cell coverings vary greatly in structure and composition and are used by taxonomists for classification purposes. Many choanoflagellates build complex basket-shaped "houses", called 3511:
De Tommasi, E., Congestri, R., Dardano, P., De Luca, A.C., ManagΓ², S., Rea, I. and De Stefano, M. (2018) "UV-shielding and wavelength conversion by centric diatom nanopatterned frustules".
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around the globe. The evolutionary causes for the generation of nano and microstructured silica by photosynthetic algae are not yet clear. However, in 2018 it was shown that absorption of
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Kuwata, A., Yamada, K., Ichinomiya, M., Yoshikawa, S., Tragin, M., Vaulot, D. and Lopes dos Santos, A. (2018) "Bolidophyceae, a sister picoplanktonic group of diatoms – a review".
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for short) are single-celled predatory protists, also protected with shells that have holes in them. Their name comes from the Latin for "hole bearers". Their shells, often called
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Gafar, N. A., Eyre, B. D. and Schulz, K. G. (2019) "A comparison of species specific sensitivities to changing light and carbonate chemistry in calcifying marine phytoplankton".
1941:, may be single-chambered or multi-chambered; multi-chambered forams add more chambers as they grow. The most famous of these are made of calcite, but tests may also be made of 1214: 1265:. "The microscopic structures of diatoms help them manipulate light, leading to hopes they could be used in new technologies for light detection, computing or robotics. 3639:
Kachovich, S., Sheng, J. and Aitchison, J. C., 2019. Adding a new dimension to investigations of early radiolarian evolution. Scientific reports, 9(1), pp. 1–10.
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Treguer, P.; Nelson, D. M.; Van Bennekom, A. J.; Demaster, D. J.; Leynaert, A.; Queguiner, B. (1995). "The Silica Balance in the World Ocean: A Reestimate".
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Dodd, Matthew S.; Papineau, Dominic; Grenne, Tor; slack, John F.; Rittner, Martin; Pirajno, Franco; O'Neil, Jonathan; Little, Crispin T. S. (2 March 2017).
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In contrast to the cells of bacteria and archaea, the cells of protists and other eukaryotes are highly organised. Plants, animals and fungi are usually
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that are hard and protective, and serve as a barrier to prevent water loss. The shells have small pores that allow for gas exchange and nutrient uptake.
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Booth, B.C. and Marchant, H.J. (1987) "Parmales, a new order of marine chrysophytes, with descriptions of three new genera and seven new species".
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Diatom frustules have been accumulating for over 100 million years, leaving rich deposits of nano and microstructured silicon oxide in the form of
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Baines, Stephen B.; Twining, Benjamin S.; Brzezinski, Mark A.; Krause, Jeffrey W.; Vogt, Stefan; Assael, Dylan; McDaniel, Hannah (December 2012).
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The term protist came into use historically to refer to a group of biologically similar organisms; however, modern research has shown it to be a
733:. Although protists are typically very small, they are ubiquitous. Their numbers are such that their shells play a huge part in the formation of 420: 2246:. This sample consists of a mixture of centric (radially symmetric) and pennate (bilaterally symmetric) diatoms. Click 3 times to fully enlarge. 2190:                         3476:
Aguirre, L. E., Ouyang, L., Elfwing, A., Hedblom, M., Wulff, A. and InganΓ€s, O. (2018) "Diatom frustules protect DNA from ultraviolet light".
1681:, referring to their small size and the coccolith stones they carry. Under the right conditions they bloom, like other phytoplankton, and can 792:. Eukaryotes include organisms such as plants, animals, fungi and "protists". Protists are usually single-celled and microscopic. They can be 1504: 2619: 2391:
4.54 billion years ago. Nonetheless, life may have started even earlier, at nearly 4.5 billion years ago, as claimed by some researchers.
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scattering of scarce photons for deep-dwelling species. (B) represents protection from photodamage including sunshade protection from
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to be predominantly used in constructing these protective cell wall structures. Silicon enters the ocean in a dissolved form such as
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Arsenieff, L.; Simon, N.; Rigaut-Jalabert, F.; Le Gall, F.; Chaffron, S.; Corre, E.; Com, E.; Bigeard, E.; Baudoux, A.C. (2018).
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are minute unicellular photosynthetic protists with two flagella for locomotion. Most of them are protected by a shell called a
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Diatom productivity in the upper ocean contribute to the amount of silicon exported to the lower ocean. When diatom cells are
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Betts, Holly C.; Putick, Mark N.; Clark, James W.; Williams, Tom A.; Donoghue, Philip C.J.; Pisani, Davide (20 August 2018).
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Marinov, I.; Gnanadesikan, A.; Toggweiler, J. R.; Sarmiento, J. L. (June 2006). "The Southern Ocean biogeochemical divide".
2798:"Silicon-Induced Cell Wall Fortification of Rice Leaves: A Possible Cellular Mechanism of Enhanced Host Resistance to Blast" 1005:
in the upper ocean, their nutrients like, iron, zinc, and silicon, are brought to the lower ocean through a process called
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Protists shells are often tough, mineralised forms that resist degradation, and can survive the death of the protist as a
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and is not currently in formal scientific use. Nonetheless, the term continues to be used informally to refer to those
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Rost, B. and Riebesell, U. (2004) "Coccolithophores and the biological pump: responses to environmental changes". In:
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each year from the waters in which they live, and contribute nearly half of the organic material found in the oceans.
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Xu, K., Hutchins, D. and Gao, K. (2018) "Coccolith arrangement follows Eulerian mathematics in the coccolithophore
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that are generally between 0.001mm and 1 mm in size, the study of which requires the use of light or electron
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processes include the transport into the cell from the surrounding seawater of primary calcification substrates Ca
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microbial communities have yet to be discovered. As eukaryotes, protists possess within their cell at least one
2666:. Thomas W. Broadhead, Paleontological Society. : University of Tennessee, Dept. of Geological Sciences. 1982. 2145: 1826: 2251: 1650: 552: 547: 380: 181: 1749: 3817:
Pawlowski, Jan; Bolivar, Ignacio; Fahrni, Jose F.; Vargas, Colomban De; Bowser, Samuel S. (November 1999).
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crystals. The completed coccolith (gray plate) is a complex structure of intricately arranged CAPs and CaCO
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with four nested spheres. The innermost sphere is highlighted red. Each segment is shown at the same scale.
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Exploded drawing of the shell, D = dorsal plate, G = girdle plate, S = shield plate and V = ventral plate.
3818: 2836: 1706: 1539: 375: 1677:. The coccoliths are made from calcium carbonate. The term coccolithophore derives from the Greek for a 4231: 3221: 2695: 1010: 662: 609: 1848:βˆ’ (black arrows) and the removal of the end product H+ from the cell (gray arrow). The transport of Ca 1516: 3889: 2380: 1105: 603: 262: 4107: 4236: 2383:, suggesting "an almost instantaneous emergence of life" (in a geological time-scale sense), after 1014: 819:
group that does not contain all descendants of a common ancestor. As such it does not constitute a
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floor when radiolarians die and become preserved as part of the ocean sediment. These remains, as
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in the algal cells, and this may be an evolutionary cause for the formation of the glass cages.
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TrΓ©guer, Paul J.; De La Rocha, Christina L. (3 January 2013). "The World Ocean Silica Cycle".
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The shells or skeletons of many protists survive over geological time scales as microfossils.
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Biodegradable glitter and pollution-eating microalgae: the new materials inspired by nature
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An Illustrated Guide to the Protozoa, Second Edition. Lawrence: Society of Protozoologists
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Blog of the Tectonics and Structural Geology Division of the European Geosciences Union.
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Exley, C. (1998). "Silicon in life:A bioinorganic solution to bioorganic essentiality".
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Corliss JO (1992). "Should there be a separate code of nomenclature for the protists?".
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Durkin, Colleen A.; Koester, Julie A.; Bender, Sara J.; Armbrust, E. Virginia (2016).
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Leadbeater BS, Kelly M (2001). "Evolution of animals choanoflagellates and sponges".
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as a structural material for their skeletons. In more advanced plants, the silica
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organisms that are not plants, animals, or fungi. They are typically microscopic
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Varea, C.; Aragon, J. L.; Barrio, R. A. (1999). "Turing patterns on a sphere".
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The role of protist shells depends on the type of protist. Protists such as
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Diatoms, major components of marine plankton, have silica skeletons called
991: 860: 844: 840: 832: 769: 761: 634: 311: 306: 288: 106: 3968:"Evidence for early life in Earth's oldest hydrothermal vent precipitates" 2555: 2520: 1910: 1413: 812:, meaning they produce their own food through a mixture of those methods. 4018: 3246: 2334: 2330: 2310: 2298: 2287: 2275: 2257: 1986: 1764: 1670: 1553: 1481: 1432: 1193: 1006: 894: 875: 809: 797: 730: 584: 569: 512: 426: 193: 125: 3995: 3333: 2660: 1691: 1673:. Coccospheres are covered with ornate circular plates or scales called 1577: 75: 3420:"Bio-manufacturing technology based on diatom micro- and nanostructure" 2346: 2283: 1974: 1861: 1661: 1404: 917: 785: 749: 164: 3311: 3042: 2620:"The molecular ecology of microbial eukaryotes unveils a hidden world" 2321:
is represented in the microfossil record, the most abundant forms are
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Zhang, D.; Wang, Y.; Cai, J.; Pan, J.; Jiang, X.; Jiang, Y. (2012).
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Protistan Skeletons: A Geologic History of Evolution and Constraint
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Silicified frustule of a pennate diatom with two overlapping halves
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Bidle, Kay D.; Manganelli, Maura; Azam, Farooq (6 December 2002).
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Also like diatoms, radiolarian shells are usually made of silicate
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Material was copied from this source, which is available under a
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Material was copied from this source, which is available under a
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Material was copied from this source, which is available under a
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Material was copied from this source, which is available under a
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Material was copied from this source, which is available under a
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Material was copied from this source, which is available under a
2322: 2279: 2243: 2003: 1954: 961: 883: 852: 796:, meaning they obtain nutrients by consuming other organisms, or 715: 490: 415: 336: 225: 111: 4023:"Scientists Say Canadian Bacteria Fossils May Be Earth's Oldest" 2309:, but also occur in brackish water, fresh water and terrestrial 967:
Diatoms are enclosed in protective silica (glass) shells called
4077:"Canadian bacteria-like fossils called oldest evidence of life" 2354: 2350: 2113: 1950: 1221: 1155: 1075: 956: 913: 788:(including modern bacteria and archaea) and later evolved into 753: 745: 707: 519: 3128:"Significant silicon accumulation by marine picocyanobacteria" 2796:
Kim, Sang Gyu; Kim, Ki Woo; Park, Eun Woo; Choi, Doil (2002).
2053:, together with nanofossils enclosed inside the shell hexagons 1444:, provide valuable information about past oceanic conditions. 3772: 3649: 3589: 3529: 3494: 3125: 2763:
Annual Review of Plant Physiology and Plant Molecular Biology
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Empty Foraminiferan test, showing multiple chambers and pores
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on a sphere closely replicate some radiolarian shell patterns
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also have hard protective shells, but the shells are made of
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build calcite skeletons important to the marine carbon cycle
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Leadbeater BS, Thomsen H (2000). "Order Choanoflagellida".
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Coccolithophores: From Molecular Processes to Global Impact
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Benefits in coccolithophore calcification – see text above
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Cutaway schematic diagram of a spherical radiolarian shell
3222:"Role of diatoms in regulating the ocean's silicon cycle" 1295: 4133: 3789: 1992:...and in life, showing pseudopodia streaming from pores 47:
and the relatively small but ubiquitous coccolithophore
3628:"Minds over Methods: Linking microfossils to tectonics" 2575:
Proceedings of the Royal Society B: Biological Sciences
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which account for 50% of the ocean's primary production
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that cannot be classified as plants, fungi or animals.
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Creative Commons Attribution 4.0 International License
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Creative Commons Attribution 4.0 International License
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Creative Commons Attribution 4.0 International License
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Creative Commons Attribution 4.0 International License
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Creative Commons Attribution 4.0 International License
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Creative Commons Attribution 4.0 International License
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and a drawing of its silicate shell, scale bar = 1 ΞΌm.
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Their protective shells (frustles) are made of silicon
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Dugdale, R. C.; Wilkerson, F. P. (30 December 2001).
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Foraminiferans are important unicellular zooplankton
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Although silicon is readily available in the form of
3900: 3898: 3790:Hemleben, C.; Anderson, O.R.; Spindler, M. (1989). 2961: 2617: 1497:
An animation of the diversity of radiolarian shells
882:are neither single-celled nor microscopic, such as 3605: 3603: 3276: 3027:"The evolution of silicon transporters in diatoms" 2379:that may be as old as 4.28 billion years old, the 3904: 3895: 3666: 1078:are one of the most common types of phytoplankton 16:Protective shell of a type of eukaryotic organism 4218: 3084: 2484: 1832:Energetic costs in coccolithophore calcification 1009:. Marine snow involves the downward transfer of 972: 3923: 3750: 3748: 3746: 3744: 3600: 3417: 2188:Testate amoebas: blobby, modest shell dwellers 2131:were constructed from limestone that contained 1441: 3472: 3470: 2913: 2795: 2084:streaming granular ectoplasm for catching food 1456:Like diatoms, radiolarians come in many shapes 1360:Diatoms: Tiny factories you can see from space 800:, meaning they produce their own food through 3633: 3505: 2569:Slapeta J, Moreira D, LΓ³pez-GarcΓ­a P (2005). 2218: 1020:In coastal zones, diatoms serve as the major 683: 40:Size comparison between the relatively large 4127: 4099: 4042: 4011: 3959: 3876:European Geosciences Union, 9 November 2020. 3741: 2837:The Air You're Breathing? A Diatom Made That 4068: 4051:"Earliest evidence of life on Earth 'found" 3467: 3365:"First Viruses Infecting the Marine Diatom 3270: 3219: 2238:made up of microfossils in the form of the 2533: 2066:section showing chambers of a spiral foram 1233:Different diatom frustule shapes and sizes 752:have intricate, glass-like shells made of 726:that live in water or moist environments. 690: 676: 4161: 3994: 3443: 3394: 3384: 3245: 3102: 3058: 2813: 2594: 2510: 2293:Microfossils are a common feature of the 1953:, or (rarely) of silica. Most forams are 986:) form, which is taken up by the silicon 3783: 3715:Te Ara - the Encyclopedia of New Zealand 3615:Te Ara - the Encyclopedia of New Zealand 2925:Te Ara - the Encyclopedia of New Zealand 2461:"Groups of Protists | Boundless Biology" 2222: 2144: 2044: 1492: 1372:How diatoms build their beautiful shells 1236: 1228: 1196:in the North Sea and the English Channel 898:A diatom, enclosed in a silica cell wall 893: 702:Many protists have protective shells or 2938:"King's College London - Lake Megachad" 2789: 2760: 1709:named after the BBC documentary series 1644: 1279:SEM images of pores in diatom frustules 889: 4219: 4074: 4017: 3823:The Journal of Eukaryotic Microbiology 3172: 2754: 2708: 2385:ocean formation 4.41 billion years ago 2368:, or microfossils, were discovered in 1637:Ernst Haeckel's radiolarian engravings 1294:by nanostructured silica protects the 1241:Structure of a centric diatom frustule 912:, very few organisms use it directly. 4182: 4105: 4048: 3173:Turner, Jefferson T. (January 2015). 3080: 3078: 2733: 2711:Studies in Natural Products Chemistry 1860:(white rectangles) that regulate the 3291:10.1146/annurev-marine-121211-172346 3220:Yool, Andrew; Tyrrell, Toby (2003). 2761:Epstein, Emanuel (1999). "SILICON". 2709:Rahman, Atta-ur- (2008). "Silicon". 1390:Radiolaria Β§ Radiolarian shells 3945:"Discovering Devonian Microfossils" 2487:"Kingdom protozoa and its 18 phyla" 1655: 1484:radiolarians have shells made from 784:Cellular life likely originated as 13: 3942: 3835:10.1111/j.1550-7408.1999.tb05137.x 3560:10.1111/j.1529-8817.1987.tb04132.x 3075: 2727: 2618:Moreira D, LΓ³pez-GarcΓ­a P (2002). 2485:Cavalier-Smith T (December 1993). 2159:is surrounded by a distinguishing 1957:, but about 40 living species are 1220:There are over 100,000 species of 1111:They come in many shapes and sizes 851:but can reproduce rapidly through 14: 4248: 2736:Journal of Inorganic Biochemistry 2112:forams of various sizes from the 2038:Foraminiferal networks and growth 1880: 1570:Turing and radiolarian morphology 3771: 3648: 3588: 3528: 3493: 2775:10.1146/annurev.arplant.50.1.641 2441: 2204: 2182: 2120: 2101: 2089: 2071: 2059: 2032: 2020: 1985: 1973: 1909: 1900: 1856:(CAPs – gray rectangles) by the 1825: 1802: 1763: 1748: 1719: 1699: 1690: 1631: 1619: 1588: 1583:Shell of a spherical radiolarian 1576: 1538: 1515: 1503: 1473: 1461: 1449: 1412: 1403: 1366: 1354: 1340:, a sister taxon to the diatoms. 1320: 1305: 1272: 1254: 1213: 1201: 1182: 1170: 1139: 1125: 1104: 1095: 1083: 1068: 1046: 1037: 657: 656: 74: 33: 3936: 3917: 3879: 3865: 3810: 3720: 3703: 3660: 3620: 3565: 3540: 3452: 3411: 3356: 3305: 3279:Annual Review of Marine Science 3213: 3166: 3119: 3018: 2955: 2930: 2892: 2841: 2830: 2140: 1383: 421:microbial calcite precipitation 4049:Ghosh, Pallab (1 March 2017). 3892:. Retrieved: 18 November 2019. 3886:Foraminifera: History of Study 3793:Modern Planktonic Foraminifera 2702: 2653: 2611: 2562: 2527: 2503:10.1128/mmbr.57.4.953-994.1993 2478: 2453: 2418: 2381:oldest record of life on Earth 1: 4075:Dunham, Will (1 March 2017). 2815:10.1094/PHYTO.2002.92.10.1095 2748:10.1016/S0162-0134(97)10010-1 2713:. Vol. 35. p. 856. 2639:10.1016/S0966-842X(01)02257-0 2411: 2252:Protists in the fossil record 1999: 1651:Marine biogenic calcification 1436: 772:and move around more easily. 381:marine biogenic calcification 3717:. Accessed: 2 November 2019. 3617:. Accessed: 2 November 2019. 3611:"Plankton - Animal plankton" 3226:Global Biogeochemical Cycles 3199:10.1016/j.pocean.2014.08.005 2927:. Accessed: 2 November 2019. 2870:10.1126/science.268.5209.375 2548:10.1016/0303-2647(92)90003-H 2406:Particulate inorganic matter 978:Diatoms uses silicon in the 7: 3926:Water and Atmosphere Online 3573:Frontiers in Marine Science 3104:10.3989/scimar.2001.65s2141 2921:"Plankton - Plant plankton" 2394: 1192:, a diatom responsible for 779: 741:of elements and nutrients. 610:Biomineralising polychaetes 376:amorphous calcium carbonate 62:Part of a series related to 10: 4253: 3730:, pages 99–125, Springer. 3645:10.1038/s41598-019-42771-0 3525:10.1038/s41598-018-34651-w 3490:10.1038/s41598-018-21810-2 2438:10.1038/s41598-019-38661-0 2305:. They are most common in 2255: 2249: 2219:Microfossils and sediments 2194:Journey to the Microcosmos 2096:Group of planktonic forams 1884: 1683:turn the ocean milky white 1659: 1648: 1435:are unicellular predatory 1387: 1376:Journey to the Microcosmos 1011:particulate organic matter 949: 943: 939: 901: 642:Burgess Shale preservation 4154:10.1038/s41559-018-0644-x 3890:University College London 3709:Wassilieff, Maggy (2006) 3609:Wassilieff, Maggy (2006) 3445:10.1007/s11434-012-5410-x 3373:Frontiers in Microbiology 2919:Wassilieff, Maggy (2006) 2465:courses.lumenlearning.com 2387:, and not long after the 2181: 2176: 2031: 2019: 2014: 1796:Benefits of having shells 1630: 1618: 1613: 1365: 1353: 1348: 786:single-celled prokaryotes 604:Cupriavidus metallidurans 4106:Staff (20 August 2018). 3689:10.1103/PhysRevE.60.4588 3626:Kachovich, Sarah (2018) 3585:10.3389/fmars.2018.00370 3424:Chinese Science Bulletin 3386:10.3389/fmicb.2018.03235 3179:Progress in Oceanography 2900:"Engineering with algae" 2242:(shells) of single cell 1601:Computer simulations of 1015:dissolved organic matter 325:Teeth, scales, tusks etc 4206:10.1126/science.aaa7378 3947:. Iowa State University 2988:10.1126/science.1076076 2491:Microbiological Reviews 1550:Triplococcus acanthicus 863:) may reproduce either 790:more complex eukaryotes 718:are a diverse group of 386:calcareous nannofossils 182:Choanoflagellate lorica 45:Scyphosphaera apsteinii 3768:10.1126/sciadv.1501822 2694:: CS1 maint: others ( 2627:Trends in Microbiology 2587:10.1098/rspb.2005.3195 2389:formation of the Earth 2313:deposits. While every 2247: 2155:The cell body of many 2152: 2054: 1819:Costs of having shells 1498: 1242: 1234: 1013:by vertical mixing of 899: 575:Magnetotactic bacteria 400:oolitic aragonite sand 258:scaly-foot snail shell 2226: 2148: 2049:Benthic foraminifera 2048: 1660:Further information: 1546:X-ray microtomography 1523:Cladococcus abietinus 1496: 1388:Further information: 1240: 1232: 897: 724:unicellular organisms 3548:Journal of Phycology 3367:Guinardia delicatula 3247:10.1029/2002GB002018 3031:Journal of Phycology 2364:In 2017, fossilized 2161:extracellular matrix 1949:sediment particles, 1894:Foraminiferan shapes 1645:Calcium-based shells 1625:Radiolarian geometry 1190:Guinardia delicatula 890:Silicon-based shells 859:; others (including 847:. Many protists are 706:, usually made from 3996:10.1038/nature21377 3987:2017Natur.543...60D 3796:. Springer-Verlag. 3711:"A coccolithophore" 3681:1999PhRvE..60.4588V 3436:2012ChSBu..57.3836Z 3334:10.1038/nature04883 3326:2006Natur.441..964M 3238:2003GBioC..17.1103Y 3191:2015PrOce.130..205T 3144:2012NatGe...5..886B 2980:2002Sci...298.1980B 2974:(5600): 1980–1984. 2862:1995Sci...268..375T 1929:Like radiolarians, 1755:Have plates called 1679:seed carrying stone 302:Vertebrate skeleton 92:Mineralized tissues 4183:Further references 4028:The New York Times 3513:Scientific Reports 3478:Scientific reports 2426:Scientific Reports 2266:Diatomaceous earth 2248: 2228:Diatomaceous earth 2153: 2055: 1532:Fossil radiolarian 1499: 1397:Radiolarian shapes 1288:diatomaceous earth 1243: 1235: 952:diatomaceous earth 900: 874:and are typically 466:diatomaceous earth 432:Great Calcite Belt 349:Scale microfossils 342:otolithic membrane 253:small shelly fauna 226:echinoderm stereom 102:Biocrystallization 4232:Biomineralization 4190:Emiliania huxleyi 4148:(10): 1556–1562. 3943:Drewes, Charlie. 3873:Favulina hexagona 3803:978-3-540-96815-3 3669:Physical Review E 3430:(30): 3836–3849. 3320:(7096): 964–967. 3132:Nature Geoscience 3043:10.1111/jpy.12441 2720:978-0-444-53181-0 2581:(1576): 2073–81. 2377:Nuvvuagittuq Belt 2370:hydrothermal vent 2295:geological record 2200: 2199: 2157:choanoflagellates 2129:Egyptian pyramids 2051:Favulina hexagona 2043: 2042: 1887:foraminifera test 1788:ultraviolet light 1732:Emiliania huxleyi 1642: 1641: 1595:Shell micrographs 1558:Middle Ordovician 1486:strontium sulfate 1381: 1380: 1292:ultraviolet light 988:transport protein 922:siliceous sponges 766:calcium carbonate 712:calcium carbonate 700: 699: 630:permineralization 615:Mineral nutrients 540:Mineral evolution 209:foraminifera test 68:Biomineralization 50:Emiliania huxleyi 4244: 4176: 4175: 4165: 4131: 4125: 4124: 4122: 4120: 4103: 4097: 4096: 4094: 4092: 4083:. Archived from 4072: 4066: 4065: 4063: 4061: 4046: 4040: 4039: 4037: 4035: 4021:(1 March 2017). 4015: 4009: 4008: 3998: 3972: 3963: 3957: 3956: 3954: 3952: 3940: 3934: 3933: 3921: 3915: 3914: 3902: 3893: 3883: 3877: 3869: 3863: 3862: 3814: 3808: 3807: 3787: 3781: 3775: 3756:Science Advances 3752: 3739: 3724: 3718: 3707: 3701: 3700: 3675:(4): 4588–4592. 3664: 3658: 3652: 3637: 3631: 3624: 3618: 3607: 3598: 3592: 3569: 3563: 3544: 3538: 3532: 3509: 3503: 3497: 3474: 3465: 3456: 3450: 3449: 3447: 3415: 3409: 3408: 3398: 3388: 3360: 3354: 3353: 3309: 3303: 3302: 3274: 3268: 3267: 3249: 3217: 3211: 3210: 3170: 3164: 3163: 3152:10.1038/ngeo1641 3123: 3117: 3116: 3106: 3082: 3073: 3072: 3062: 3022: 3016: 3015: 2959: 2953: 2952: 2950: 2948: 2934: 2928: 2917: 2911: 2896: 2890: 2889: 2845: 2839: 2834: 2828: 2827: 2817: 2808:(10): 1095–103. 2793: 2787: 2786: 2758: 2752: 2751: 2731: 2725: 2724: 2706: 2700: 2699: 2693: 2685: 2657: 2651: 2650: 2624: 2615: 2609: 2608: 2598: 2566: 2560: 2559: 2531: 2525: 2524: 2514: 2482: 2476: 2475: 2473: 2471: 2457: 2451: 2445: 2422: 2349:, together with 2307:marine sediments 2262:Pelagic sediment 2236:sedimentary rock 2212:Choanoflagellate 2208: 2191: 2186: 2185: 2174: 2173: 2124: 2105: 2093: 2075: 2063: 2036: 2035: 2024: 2023: 2012: 2011: 1989: 1977: 1913: 1904: 1829: 1806: 1777:Coccolithophores 1767: 1752: 1742:Coccolithophores 1723: 1707:Coccolithophores 1703: 1694: 1667:Coccolithophores 1656:Coccolithophores 1635: 1634: 1623: 1622: 1611: 1610: 1592: 1580: 1542: 1519: 1507: 1477: 1465: 1453: 1416: 1407: 1370: 1369: 1358: 1357: 1346: 1345: 1324: 1309: 1276: 1258: 1217: 1205: 1186: 1174: 1143: 1129: 1108: 1099: 1087: 1072: 1050: 1041: 973:half a mile deep 758:Coccolithophores 692: 685: 678: 665: 660: 659: 580:Magnetoreception 560:Ballast minerals 155:Cephalopod shell 150:Brachiopod shell 97:Remineralisation 78: 59: 58: 37: 4252: 4251: 4247: 4246: 4245: 4243: 4242: 4241: 4237:Skeletal system 4217: 4216: 4185: 4180: 4179: 4132: 4128: 4118: 4116: 4104: 4100: 4090: 4088: 4087:on 2 March 2017 4073: 4069: 4059: 4057: 4047: 4043: 4033: 4031: 4016: 4012: 3981:(7643): 60–64. 3970: 3964: 3960: 3950: 3948: 3941: 3937: 3922: 3918: 3903: 3896: 3884: 3880: 3870: 3866: 3815: 3811: 3804: 3788: 3784: 3762:(7): e1501822. 3753: 3742: 3725: 3721: 3708: 3704: 3665: 3661: 3638: 3634: 3625: 3621: 3608: 3601: 3570: 3566: 3545: 3541: 3510: 3506: 3475: 3468: 3457: 3453: 3416: 3412: 3361: 3357: 3310: 3306: 3275: 3271: 3218: 3214: 3171: 3167: 3138:(12): 886–891. 3124: 3120: 3097:(S2): 141–152. 3091:Scientia Marina 3083: 3076: 3023: 3019: 2960: 2956: 2946: 2944: 2936: 2935: 2931: 2918: 2914: 2897: 2893: 2856:(5209): 375–9. 2846: 2842: 2835: 2831: 2794: 2790: 2759: 2755: 2732: 2728: 2721: 2707: 2703: 2687: 2686: 2674: 2659: 2658: 2654: 2622: 2616: 2612: 2567: 2563: 2532: 2528: 2483: 2479: 2469: 2467: 2459: 2458: 2454: 2423: 2419: 2414: 2397: 2359:vascular plants 2272: 2254: 2221: 2214: 2209: 2189: 2183: 2177:External videos 2143: 2136: 2125: 2116: 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1316: 1313:Triparma laevis 1310: 1284: 1283: 1282: 1281: 1280: 1277: 1268: 1267: 1266: 1259: 1250: 1249: 1225: 1218: 1209: 1206: 1197: 1187: 1178: 1175: 1166: 1165: 1164: 1163: 1154:Diatoms have a 1151: 1150: 1149: 1144: 1136: 1135: 1130: 1121: 1120: 1112: 1109: 1100: 1091: 1088: 1079: 1073: 1064: 1063: 1062: 1061: 1053: 1052: 1051: 1043: 1042: 1033: 1032: 1022:phytoplanktonic 985: 980:biogenic silica 954: 948: 946:diatom frustule 942: 926:biogenic silica 906: 904:Biogenic silica 892: 880:marine protists 782: 735:ocean sediments 696: 655: 648: 647: 646: 534: 526: 525: 524: 480: 472: 471: 470: 456:biogenic silica 450: 440: 439: 438: 423: 411: 390: 370: 360: 359: 358: 326: 318: 317: 316: 296: 281: 280: 279: 246:gastropod shell 214:testate amoebae 204:diatom frustule 129: 118: 117: 116: 86: 57: 56: 55: 54: 53: 42:coccolithophore 38: 29: 28: 25:Coccolithophore 17: 12: 11: 5: 4250: 4240: 4239: 4234: 4229: 4215: 4214: 4209: 4184: 4181: 4178: 4177: 4126: 4098: 4067: 4041: 4010: 3958: 3935: 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Index

Coccolithophore

coccolithophore
Emiliania huxleyi
Biomineralization

Mineralized tissues
Remineralisation
Biocrystallization
Biointerface
Biofilm
Exoskeletons
exoskeleton
cuticle
Brachiopod shell
Cephalopod shell
cirrate shell
cuttlebone
gladius
Lorica
Choanoflagellate lorica
Protist shell
coccosphere
coccolith
diatom frustule
foraminifera test
testate amoebae
Seashell
echinoderm stereom
mollusc shell

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