Knowledge (XXG)

Protist shell

Source πŸ“

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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.
1801:(UV) and photosynthetic active radiation (PAR) and energy dissipation under high-light conditions. (C) represents armour protection includes protection against viral/bacterial infections and grazing by selective and nonselective grazers. 1036:
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,
1028:. 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. 1473: 1485: 3765:
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".
2178:. 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 3522:
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
1863:+ through the cytoplasm to the coccolith vesicle (CV) is the dominant cost associated with calcification. (B) represents metabolic processes include the synthesis of coccolith-associated 1972:. They are widely researched with well established fossil records which allow scientists to infer a lot about past environments and climates. Some foraminifera lack tests altogether. 3582:
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".
1952:, 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 2071: 700: 2132: 1276:. "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. 3650:
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
744:. Although protists are typically very small, they are ubiquitous. Their numbers are such that their shells play a huge part in the formation of 2257:. This sample consists of a mixture of centric (radially symmetric) and pennate (bilaterally symmetric) diatoms. Click 3 times to fully enlarge. 2201:                         3487:
Aguirre, L. E., Ouyang, L., Elfwing, A., Hedblom, M., Wulff, A. and InganΓ€s, O. (2018) "Diatom frustules protect DNA from ultraviolet light".
1692:, referring to their small size and the coccolith stones they carry. Under the right conditions they bloom, like other phytoplankton, and can 803:. Eukaryotes include organisms such as plants, animals, fungi and "protists". Protists are usually single-celled and microscopic. They can be 3812: 2729: 2630: 2402:
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".
2809:"Silicon-Induced Cell Wall Fortification of Rice Leaves: A Possible Cellular Mechanism of Enhanced Host Resistance to Blast" 1016:
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
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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.
882: 585: 410: 3829: 2847: 1688:. The coccoliths are made from calcium carbonate. The term coccolithophore derives from the Greek for a 1556: 148: 3232: 2216: 1504: 1859:βˆ’ (black arrows) and the removal of the end product H+ from the cell (gray arrow). The transport of Ca 45: 3993: 3687: 3442: 3332: 3244: 3197: 3150: 2986: 2868: 2171: 859: 749: 734: 268: 180: 4118: 2394:, suggesting "an almost instantaneous emergence of life" (in a geological time-scale sense), after 875: 830:
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.
1897: 1876: 1798: 1742: 1693: 1568: 1496: 1302: 1240: 998: 776: 722: 640: 550: 219: 153: 78: 60: 3721: 943:(opal phytoliths) are rigid microscopic bodies occurring in the cell; some plants, including 4212: 4168: 4160: 4151: 4001: 3841: 3774: 3695: 3651: 3591: 3566: 3531: 3496: 3450: 3401: 3391: 3340: 3297: 3252: 3205: 3158: 3109: 3065: 3049: 2994: 2876: 2820: 2781: 2754: 2645: 2601: 2593: 2554: 2517: 2509: 2444: 2399: 2329: 2272: 2246: 2222: 2179: 2167: 2139: 1107: 932: 600: 590: 570: 192: 187: 107: 3470:
Biodegradable glitter and pollution-eating microalgae: the new materials inspired by nature
2582:"The extent of protist diversity: insights from molecular ecology of freshwater eukaryotes" 1317: 4061: 3918:
An Illustrated Guide to the Protozoa, Second Edition. Lawrence: Society of Protozoologists
2975:"Regulation of Oceanic Silicon and Carbon Preservation by Temperature Control on Bacteria" 2317: 1787: 1738: 1722: 1677: 1032: 990: 956: 936: 914: 768: 466: 256: 224: 52: 35: 3301: 3997: 3691: 3641:
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).
2974: 2758: 2649: 2522: 2497: 1702: 1588: 889:. Most protists are single-celled and microscopic, but there are exceptions, and some 86: 4231: 3935:
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
3979:"Evidence for early life in Earth's oldest hydrothermal vent precipitates" 2566: 2531: 823:, meaning they produce their own food through a mixture of those methods. 4123: 4065: 3257: 2313: 2250: 1969: 1344: 1273: 1170: 1157: 1006: 979: 920: 506: 496: 312: 231: 214: 4006: 3344: 2671: 1684:. Coccospheres are covered with ornate circular plates or scales called 4091: 3783: 3660: 3600: 3540: 3505: 3431:"Bio-manufacturing technology based on diatom micro- and nanostructure" 2453: 2333: 2290: 2254: 2014: 1965: 972: 894: 863: 726: 501: 426: 347: 236: 122: 3053: 2631:"The molecular ecology of microbial eukaryotes unveils a hidden world" 2332:
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
807:, meaning they obtain nutrients by consuming other organisms, or 4034:"Scientists Say Canadian Bacteria Fossils May Be Earth's Oldest" 2320:, but also occur in brackish water, fresh water and terrestrial 978:
Diatoms are enclosed in protective silica (glass) shells called
944: 364: 303: 4088:"Canadian bacteria-like fossils called oldest evidence of life" 799:(including modern bacteria and archaea) and later evolved into 3139:"Significant silicon accumulation by marine picocyanobacteria" 2807:
Kim, Sang Gyu; Kim, Ki Woo; Park, Eun Woo; Choi, Doil (2002).
2064:, together with nanofossils enclosed inside the shell hexagons 1455:, provide valuable information about past oceanic conditions. 1306: 2774:
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
3233:"Role of diatoms in regulating the ocean's silicon cycle" 2003:...and in life, showing pseudopodia streaming from pores 58:
and the relatively small but ubiquitous coccolithophore
3639:"Minds over Methods: Linking microfossils to tectonics" 2586:
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
3911: 3909: 3801:Hemleben, C.; Anderson, O.R.; Spindler, M. (1989). 2187: 2025: 1624: 1508:
An animation of the diversity of radiolarian shells
1359: 893:are neither single-celled nor microscopic, such as 3616: 3614: 3038:"The evolution of silicon transporters in diatoms" 2390:that may be as old as 4.28 billion years old, the 1089:are one of the most common types of phytoplankton 27:Protective shell of a type of eukaryotic organism 1843:Energetic costs in coccolithophore calcification 1020:. Marine snow involves the downward transfer of 983: 3761: 3759: 3757: 3755: 2199:Testate amoebas: blobby, modest shell dwellers 2142:were constructed from limestone that contained 1452: 3483: 3481: 2095:streaming granular ectoplasm for catching food 1467:Like diatoms, radiolarians come in many shapes 1371:Diatoms: Tiny factories you can see from space 811:, meaning they produce their own food through 2580:Slapeta J, Moreira D, LΓ³pez-GarcΓ­a P (2005). 1031:In coastal zones, diatoms serve as the major 694: 51:Size comparison between the relatively large 8: 3887:European Geosciences Union, 9 November 2020. 2848:The Air You're Breathing? A Diatom Made That 4062:"Earliest evidence of life on Earth 'found" 3376:"First Viruses Infecting the Marine Diatom 2249:made up of microfossils in the form of the 2077:section showing chambers of a spiral foram 1244:Different diatom frustule shapes and sizes 763:have intricate, glass-like shells made of 737:that live in water or moist environments. 701: 687: 69: 4172: 4005: 3454: 3405: 3395: 3256: 3113: 3069: 2824: 2605: 2521: 2304:Microfossils are a common feature of the 1964:, or (rarely) of silica. Most forams are 997:) form, which is taken up by the silicon 3726:Te Ara - the Encyclopedia of New Zealand 3626:Te Ara - the Encyclopedia of New Zealand 2936:Te Ara - the Encyclopedia of New Zealand 2472:"Groups of Protists | Boundless Biology" 1383:How diatoms build their beautiful shells 1207:in the North Sea and the English Channel 909:A diatom, enclosed in a silica cell wall 713:Many protists have protective shells or 2949:"King's College London - Lake Megachad" 2428: 2212: 2067: 1720:named after the BBC documentary series 1698: 1511: 1457: 1290:SEM images of pores in diatom frustules 1178: 1076: 77: 3834:The Journal of Eukaryotic Microbiology 2698: 2396:ocean formation 4.41 billion years ago 2379:, or microfossils, were discovered in 2184: 2022: 1648:Ernst Haeckel's radiolarian engravings 1621: 1356: 1305:by nanostructured silica protects the 1252:Structure of a centric diatom frustule 923:, very few organisms use it directly. 3184:Turner, Jefferson T. (January 2015). 3091: 3089: 2722:Studies in Natural Products Chemistry 1871:(white rectangles) that regulate the 7: 3302:10.1146/annurev-marine-121211-172346 3231:Yool, Andrew; Tyrrell, Toby (2003). 2772:Epstein, Emanuel (1999). "SILICON". 2720:Rahman, Atta-ur- (2008). "Silicon". 1401:Radiolaria Β§ Radiolarian shells 3956:"Discovering Devonian Microfossils" 2498:"Kingdom protozoa and its 18 phyla" 1495:radiolarians have shells made from 795:Cellular life likely originated as 3846:10.1111/j.1550-7408.1999.tb05137.x 3571:10.1111/j.1529-8817.1987.tb04132.x 2629:Moreira D, LΓ³pez-GarcΓ­a P (2002). 2496:Cavalier-Smith T (December 1993). 2170:is surrounded by a distinguishing 1968:, but about 40 living species are 1231:There are over 100,000 species of 1122:They come in many shapes and sizes 862:but can reproduce rapidly through 25: 2747:Journal of Inorganic Biochemistry 2123:forams of various sizes from the 2049:Foraminiferal networks and growth 1581:Turing and radiolarian morphology 3782: 3659: 3599: 3539: 3504: 2786:10.1146/annurev.arplant.50.1.641 2452: 2215: 2193: 2131: 2112: 2100: 2082: 2070: 2043: 2031: 1996: 1984: 1920: 1911: 1867:(CAPs – gray rectangles) by the 1836: 1813: 1774: 1759: 1730: 1710: 1701: 1642: 1630: 1599: 1594:Shell of a spherical radiolarian 1587: 1549: 1526: 1514: 1484: 1472: 1460: 1423: 1414: 1377: 1365: 1351:, a sister taxon to the diatoms. 1331: 1316: 1283: 1265: 1224: 1212: 1193: 1181: 1150: 1136: 1115: 1106: 1094: 1079: 1057: 1048: 668: 667: 85: 44: 3290:Annual Review of Marine Science 432:microbial calcite precipitation 4060:Ghosh, Pallab (1 March 2017). 3903:. Retrieved: 18 November 2019. 3897:Foraminifera: History of Study 3804:Modern Planktonic Foraminifera 2514:10.1128/mmbr.57.4.953-994.1993 2392:oldest record of life on Earth 1: 4086:Dunham, Will (1 March 2017). 2826:10.1094/PHYTO.2002.92.10.1095 2759:10.1016/S0162-0134(97)10010-1 2724:. Vol. 35. p. 856. 2650:10.1016/S0966-842X(01)02257-0 2263:Protists in the fossil record 2010: 1662:Marine biogenic calcification 1447: 783:and move around more easily. 392:marine biogenic calcification 3728:. Accessed: 2 November 2019. 3628:. Accessed: 2 November 2019. 3622:"Plankton - Animal plankton" 3237:Global Biogeochemical Cycles 3210:10.1016/j.pocean.2014.08.005 2938:. Accessed: 2 November 2019. 2881:10.1126/science.268.5209.375 2559:10.1016/0303-2647(92)90003-H 2417:Particulate inorganic matter 989:Diatoms uses silicon in the 3937:Water and Atmosphere Online 3584:Frontiers in Marine Science 3115:10.3989/scimar.2001.65s2141 2932:"Plankton - Plant plankton" 1203:, a diatom responsible for 752:of elements and nutrients. 621:Biomineralising polychaetes 387:amorphous calcium carbonate 73:Part of a series related to 4264: 3741:, pages 99–125, Springer. 3656:10.1038/s41598-019-42771-0 3536:10.1038/s41598-018-34651-w 3501:10.1038/s41598-018-21810-2 2449:10.1038/s41598-019-38661-0 2316:. They are most common in 2266: 2260: 2230:Microfossils and sediments 2205:Journey to the Microcosmos 2107:Group of planktonic forams 1895: 1694:turn the ocean milky white 1670: 1659: 1446:are unicellular predatory 1398: 1387:Journey to the Microcosmos 1022:particulate organic matter 960: 954: 912: 653:Burgess Shale preservation 4165:10.1038/s41559-018-0644-x 3901:University College London 3720:Wassilieff, Maggy (2006) 3620:Wassilieff, Maggy (2006) 3456:10.1007/s11434-012-5410-x 3384:Frontiers in Microbiology 2930:Wassilieff, Maggy (2006) 2476:courses.lumenlearning.com 2398:, and not long after the 2192: 2042: 2030: 1807:Benefits of having shells 1641: 1629: 1376: 1364: 797:single-celled prokaryotes 615:Cupriavidus metallidurans 4117:Staff (20 August 2018). 3700:10.1103/PhysRevE.60.4588 3637:Kachovich, Sarah (2018) 3596:10.3389/fmars.2018.00370 3435:Chinese Science Bulletin 3397:10.3389/fmicb.2018.03235 3190:Progress in Oceanography 2911:"Engineering with algae" 2253:(shells) of single cell 1612:Computer simulations of 1026:dissolved organic matter 336:Teeth, scales, tusks etc 4217:10.1126/science.aaa7378 3958:. Iowa State University 2999:10.1126/science.1076076 2502:Microbiological Reviews 1561:Triplococcus acanthicus 874:) may reproduce either 801:more complex eukaryotes 729:are a diverse group of 397:calcareous nannofossils 193:Choanoflagellate lorica 56:Scyphosphaera apsteinii 3779:10.1126/sciadv.1501822 2705:: CS1 maint: others ( 2638:Trends in Microbiology 2598:10.1098/rspb.2005.3195 2400:formation of the Earth 2324:deposits. While every 2258: 2166:The cell body of many 2163: 2065: 1830:Costs of having shells 1509: 1253: 1245: 1024:by vertical mixing of 910: 586:Magnetotactic bacteria 411:oolitic aragonite sand 269:scaly-foot snail shell 2237: 2159: 2060:Benthic foraminifera 2059: 1671:Further information: 1557:X-ray microtomography 1534:Cladococcus abietinus 1507: 1399:Further information: 1251: 1243: 908: 735:unicellular organisms 3559:Journal of Phycology 3378:Guinardia delicatula 3258:10.1029/2002GB002018 3042:Journal of Phycology 2375:In 2017, fossilized 2172:extracellular matrix 1960:sediment particles, 1905:Foraminiferan shapes 1656:Calcium-based shells 1636:Radiolarian geometry 1201:Guinardia delicatula 901:Silicon-based shells 870:; others (including 858:. Many protists are 717:, usually made from 4007:10.1038/nature21377 3998:2017Natur.543...60D 3807:. Springer-Verlag. 3722:"A coccolithophore" 3692:1999PhRvE..60.4588V 3447:2012ChSBu..57.3836Z 3345:10.1038/nature04883 3337:2006Natur.441..964M 3249:2003GBioC..17.1103Y 3202:2015PrOce.130..205T 3155:2012NatGe...5..886B 2991:2002Sci...298.1980B 2985:(5600): 1980–1984. 2873:1995Sci...268..375T 1940:Like radiolarians, 1766:Have plates called 1690:seed carrying stone 313:Vertebrate skeleton 103:Mineralized tissues 4194:Further references 4039:The New York Times 3524:Scientific Reports 3489:Scientific reports 2437:Scientific Reports 2277:Diatomaceous earth 2259: 2239:Diatomaceous earth 2164: 2066: 1543:Fossil radiolarian 1510: 1408:Radiolarian shapes 1299:diatomaceous earth 1254: 1246: 963:diatomaceous earth 911: 885:and are typically 477:diatomaceous earth 443:Great Calcite Belt 360:Scale microfossils 353:otolithic membrane 264:small shelly fauna 237:echinoderm stereom 113:Biocrystallization 4243:Biomineralization 4201:Emiliania huxleyi 4159:(10): 1556–1562. 3954:Drewes, Charlie. 3884:Favulina hexagona 3814:978-3-540-96815-3 3680:Physical Review E 3441:(30): 3836–3849. 3331:(7096): 964–967. 3143:Nature Geoscience 3054:10.1111/jpy.12441 2731:978-0-444-53181-0 2592:(1576): 2073–81. 2388:Nuvvuagittuq Belt 2381:hydrothermal vent 2306:geological record 2211: 2210: 2168:choanoflagellates 2140:Egyptian pyramids 2062:Favulina hexagona 2054: 2053: 1898:foraminifera test 1799:ultraviolet light 1743:Emiliania huxleyi 1653: 1652: 1606:Shell micrographs 1569:Middle Ordovician 1497:strontium sulfate 1392: 1391: 1303:ultraviolet light 999:transport protein 933:siliceous sponges 777:calcium carbonate 723:calcium carbonate 711: 710: 641:permineralization 626:Mineral nutrients 551:Mineral evolution 220:foraminifera test 79:Biomineralization 61:Emiliania huxleyi 16:(Redirected from 4255: 4187: 4186: 4176: 4142: 4136: 4135: 4133: 4131: 4114: 4108: 4107: 4105: 4103: 4094:. Archived from 4083: 4077: 4076: 4074: 4072: 4057: 4051: 4050: 4048: 4046: 4032:(1 March 2017). 4026: 4020: 4019: 4009: 3983: 3974: 3968: 3967: 3965: 3963: 3951: 3945: 3944: 3932: 3926: 3925: 3913: 3904: 3894: 3888: 3880: 3874: 3873: 3825: 3819: 3818: 3798: 3792: 3786: 3767:Science Advances 3763: 3750: 3735: 3729: 3718: 3712: 3711: 3686:(4): 4588–4592. 3675: 3669: 3663: 3648: 3642: 3635: 3629: 3618: 3609: 3603: 3580: 3574: 3555: 3549: 3543: 3520: 3514: 3508: 3485: 3476: 3467: 3461: 3460: 3458: 3426: 3420: 3419: 3409: 3399: 3371: 3365: 3364: 3320: 3314: 3313: 3285: 3279: 3278: 3260: 3228: 3222: 3221: 3181: 3175: 3174: 3163:10.1038/ngeo1641 3134: 3128: 3127: 3117: 3093: 3084: 3083: 3073: 3033: 3027: 3026: 2970: 2964: 2963: 2961: 2959: 2945: 2939: 2928: 2922: 2907: 2901: 2900: 2856: 2850: 2845: 2839: 2838: 2828: 2819:(10): 1095–103. 2804: 2798: 2797: 2769: 2763: 2762: 2742: 2736: 2735: 2717: 2711: 2710: 2704: 2696: 2668: 2662: 2661: 2635: 2626: 2620: 2619: 2609: 2577: 2571: 2570: 2542: 2536: 2535: 2525: 2493: 2487: 2486: 2484: 2482: 2468: 2462: 2456: 2433: 2360:, together with 2318:marine sediments 2273:Pelagic sediment 2247:sedimentary rock 2223:Choanoflagellate 2219: 2202: 2197: 2196: 2185: 2135: 2116: 2104: 2086: 2074: 2047: 2046: 2035: 2034: 2023: 2000: 1988: 1924: 1915: 1840: 1817: 1788:Coccolithophores 1778: 1763: 1753:Coccolithophores 1734: 1718:Coccolithophores 1714: 1705: 1678:Coccolithophores 1667:Coccolithophores 1646: 1645: 1634: 1633: 1622: 1603: 1591: 1553: 1530: 1518: 1488: 1476: 1464: 1427: 1418: 1381: 1380: 1369: 1368: 1357: 1335: 1320: 1287: 1269: 1228: 1216: 1197: 1185: 1154: 1140: 1119: 1110: 1098: 1083: 1061: 1052: 984:half a mile deep 769:Coccolithophores 703: 696: 689: 676: 671: 670: 591:Magnetoreception 571:Ballast minerals 166:Cephalopod shell 161:Brachiopod shell 108:Remineralisation 89: 70: 48: 21: 4263: 4262: 4258: 4257: 4256: 4254: 4253: 4252: 4248:Skeletal system 4228: 4227: 4196: 4191: 4190: 4144: 4143: 4139: 4129: 4127: 4116: 4115: 4111: 4101: 4099: 4098:on 2 March 2017 4085: 4084: 4080: 4070: 4068: 4059: 4058: 4054: 4044: 4042: 4028: 4027: 4023: 3992:(7643): 60–64. 3981: 3976: 3975: 3971: 3961: 3959: 3953: 3952: 3948: 3934: 3933: 3929: 3915: 3914: 3907: 3895: 3891: 3881: 3877: 3827: 3826: 3822: 3815: 3800: 3799: 3795: 3773:(7): e1501822. 3764: 3753: 3736: 3732: 3719: 3715: 3677: 3676: 3672: 3649: 3645: 3636: 3632: 3619: 3612: 3581: 3577: 3556: 3552: 3521: 3517: 3486: 3479: 3468: 3464: 3428: 3427: 3423: 3373: 3372: 3368: 3322: 3321: 3317: 3287: 3286: 3282: 3230: 3229: 3225: 3183: 3182: 3178: 3149:(12): 886–891. 3136: 3135: 3131: 3108:(S2): 141–152. 3102:Scientia Marina 3095: 3094: 3087: 3035: 3034: 3030: 2972: 2971: 2967: 2957: 2955: 2947: 2946: 2942: 2929: 2925: 2908: 2904: 2867:(5209): 375–9. 2858: 2857: 2853: 2846: 2842: 2806: 2805: 2801: 2771: 2770: 2766: 2744: 2743: 2739: 2732: 2719: 2718: 2714: 2697: 2685: 2670: 2669: 2665: 2633: 2628: 2627: 2623: 2579: 2578: 2574: 2544: 2543: 2539: 2495: 2494: 2490: 2480: 2478: 2470: 2469: 2465: 2434: 2430: 2425: 2408: 2370:vascular plants 2283: 2265: 2232: 2225: 2220: 2200: 2194: 2188:External videos 2154: 2147: 2136: 2127: 2117: 2108: 2105: 2096: 2087: 2078: 2075: 2044: 2032: 2026:External videos 2021: 2020: 2019: 2018: 2006: 2005: 2004: 2001: 1993: 1992: 1989: 1980: 1979: 1938: 1937: 1936: 1935: 1927: 1926: 1925: 1917: 1916: 1907: 1906: 1900: 1894: 1886: 1882: 1865:polysaccharides 1862: 1858: 1854: 1848: 1847: 1846: 1845: 1844: 1841: 1832: 1831: 1825: 1824: 1823: 1822: 1821: 1818: 1809: 1808: 1794: 1793: 1792: 1791: 1784: 1783: 1782: 1779: 1771: 1770: 1764: 1755: 1754: 1746: 1739:coccolithophore 1735: 1726: 1723:The Blue Planet 1715: 1706: 1675: 1669: 1664: 1658: 1643: 1631: 1625:External videos 1620: 1619: 1618: 1617: 1614:Turing patterns 1609: 1608: 1607: 1604: 1596: 1595: 1592: 1583: 1582: 1576: 1575: 1574: 1573: 1572: 1554: 1545: 1544: 1536: 1531: 1522: 1519: 1500: 1489: 1480: 1477: 1468: 1465: 1441: 1440: 1439: 1438: 1430: 1429: 1428: 1420: 1419: 1410: 1409: 1403: 1397: 1378: 1366: 1360:External videos 1355: 1354: 1353: 1352: 1347:belongs to the 1345:Triparma laevis 1341: 1340: 1339: 1336: 1328: 1327: 1324:Triparma laevis 1321: 1295: 1294: 1293: 1292: 1291: 1288: 1279: 1278: 1277: 1270: 1261: 1260: 1236: 1229: 1220: 1217: 1208: 1198: 1189: 1186: 1177: 1176: 1175: 1174: 1165:Diatoms have a 1162: 1161: 1160: 1155: 1147: 1146: 1141: 1132: 1131: 1123: 1120: 1111: 1102: 1099: 1090: 1084: 1075: 1074: 1073: 1072: 1064: 1063: 1062: 1054: 1053: 1044: 1043: 1033:phytoplanktonic 996: 991:biogenic silica 965: 959: 957:diatom frustule 953: 937:biogenic silica 917: 915:Biogenic silica 903: 891:marine protists 793: 746:ocean sediments 707: 666: 659: 658: 657: 545: 537: 536: 535: 491: 483: 482: 481: 467:biogenic silica 461: 451: 450: 449: 434: 422: 401: 381: 371: 370: 369: 337: 329: 328: 327: 307: 292: 291: 290: 257:gastropod shell 225:testate amoebae 215:diatom frustule 140: 129: 128: 127: 97: 68: 67: 66: 65: 64: 53:coccolithophore 49: 40: 39: 36:Coccolithophore 28: 23: 22: 15: 12: 11: 5: 4261: 4259: 4251: 4250: 4245: 4240: 4230: 4229: 4226: 4225: 4220: 4195: 4192: 4189: 4188: 4137: 4109: 4078: 4052: 4021: 3969: 3946: 3927: 3905: 3889: 3875: 3840:(6): 612–617. 3820: 3813: 3793: 3751: 3730: 3713: 3670: 3643: 3630: 3610: 3575: 3550: 3515: 3477: 3475:, 28 May 2020. 3462: 3421: 3366: 3315: 3296:(1): 477–501. 3280: 3223: 3176: 3129: 3085: 3048:(5): 716–731. 3028: 2965: 2940: 2923: 2902: 2851: 2840: 2813:Phytopathology 2799: 2764: 2753:(3): 139–144. 2737: 2730: 2712: 2683: 2663: 2621: 2572: 2537: 2488: 2463: 2427: 2426: 2424: 2421: 2420: 2419: 2414: 2407: 2404: 2377:microorganisms 2281:Siliceous ooze 2261:Main article: 2231: 2228: 2227: 2226: 2221: 2214: 2209: 2208: 2190: 2189: 2161:Testate amoeba 2153: 2150: 2149: 2148: 2137: 2130: 2128: 2118: 2111: 2109: 2106: 2099: 2097: 2092:Ammonia tepida 2088: 2081: 2079: 2076: 2069: 2052: 2051: 2040: 2039: 2037:foraminiferans 2028: 2027: 2008: 2007: 2002: 1995: 1994: 1990: 1983: 1982: 1981: 1978:Foraminiferans 1977: 1976: 1975: 1974: 1942:foraminiferans 1929: 1928: 1919: 1918: 1910: 1909: 1908: 1904: 1903: 1902: 1901: 1896:Main article: 1893: 1892:Foraminiferans 1890: 1884: 1880: 1860: 1856: 1852: 1842: 1835: 1834: 1833: 1829: 1828: 1827: 1826: 1819: 1812: 1811: 1810: 1806: 1805: 1804: 1803: 1786: 1785: 1781:Extinct fossil 1780: 1773: 1772: 1765: 1758: 1757: 1756: 1752: 1751: 1750: 1749: 1748: 1747: 1736: 1729: 1727: 1716: 1709: 1707: 1700: 1668: 1665: 1657: 1654: 1651: 1650: 1639: 1638: 1627: 1626: 1611: 1610: 1605: 1598: 1597: 1593: 1586: 1585: 1584: 1580: 1579: 1578: 1577: 1555: 1548: 1547: 1546: 1542: 1541: 1540: 1539: 1538: 1537: 1532: 1525: 1523: 1520: 1513: 1502: 1501: 1490: 1483: 1481: 1478: 1471: 1469: 1466: 1459: 1432: 1431: 1422: 1421: 1413: 1412: 1411: 1407: 1406: 1405: 1404: 1396: 1393: 1390: 1389: 1374: 1373: 1362: 1361: 1343: 1342: 1337: 1330: 1329: 1322: 1315: 1314: 1313: 1312: 1311: 1289: 1282: 1281: 1280: 1271: 1264: 1263: 1262: 1258: 1257: 1256: 1255: 1238: 1237: 1230: 1223: 1221: 1218: 1211: 1209: 1199: 1192: 1190: 1187: 1180: 1164: 1163: 1156: 1149: 1148: 1142: 1135: 1134: 1133: 1129: 1128: 1127: 1126: 1125: 1124: 1121: 1114: 1112: 1105: 1103: 1100: 1093: 1091: 1085: 1078: 1066: 1065: 1056: 1055: 1047: 1046: 1045: 1041: 1040: 1039: 1038: 994: 955:Main article: 952: 949: 902: 899: 878:or asexually. 817:chemosynthesis 813:photosynthesis 792: 789: 750:global cycling 709: 708: 706: 705: 698: 691: 683: 680: 679: 678: 677: 661: 660: 656: 655: 650: 649: 648: 643: 633: 628: 623: 618: 611: 606: 598: 593: 588: 583: 578: 573: 568: 567: 566: 564:immobilization 561: 559:mineralization 553: 547: 546: 543: 542: 539: 538: 534: 533: 528: 527: 526: 516: 515: 514: 509: 499: 493: 492: 489: 488: 485: 484: 480: 479: 474: 472:siliceous ooze 469: 463: 462: 459:Silicification 457: 456: 453: 452: 448: 447: 446: 445: 440: 435: 423: 421: 420: 419: 418: 413: 402: 400: 399: 394: 389: 383: 382: 377: 376: 373: 372: 368: 367: 362: 357: 356: 355: 345: 339: 338: 335: 334: 331: 330: 326: 325: 320: 315: 309: 308: 298: 297: 294: 293: 289: 288: 283: 281:Sponge spicule 278: 277: 276: 274:estuary shells 271: 266: 261: 260: 259: 254: 249: 239: 229: 228: 227: 222: 217: 212: 207: 197: 196: 195: 185: 184: 183: 178: 173: 163: 158: 157: 156: 151: 142: 141: 135: 134: 131: 130: 126: 125: 120: 115: 110: 105: 99: 98: 95: 94: 91: 90: 82: 81: 75: 74: 50: 43: 42: 41: 34: 33: 32: 31: 26: 24: 18:Protist shells 14: 13: 10: 9: 6: 4: 3: 2: 4260: 4249: 4246: 4244: 4241: 4239: 4236: 4235: 4233: 4224: 4221: 4218: 4214: 4210: 4206: 4202: 4198: 4197: 4193: 4184: 4180: 4175: 4170: 4166: 4162: 4158: 4154: 4153: 4148: 4141: 4138: 4126: 4125: 4120: 4113: 4110: 4097: 4093: 4089: 4082: 4079: 4067: 4063: 4056: 4053: 4041: 4040: 4035: 4031: 4025: 4022: 4017: 4013: 4008: 4003: 3999: 3995: 3991: 3987: 3980: 3973: 3970: 3957: 3950: 3947: 3942: 3938: 3931: 3928: 3923: 3919: 3912: 3910: 3906: 3902: 3898: 3893: 3890: 3886: 3885: 3879: 3876: 3871: 3867: 3863: 3859: 3855: 3851: 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Index

Protist shells
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

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