Tintinnid

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Tintinnid
Tintinn.jpg
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Clade: Diaphoretickes
Clade: SAR
Clade: Alveolata
Phylum: Ciliophora
Class: Spirotrichea
Subclass: Choreotrichia
Order: Tintinnida
Kofoid & Campbell, 1929

Tintinnids are ciliates of the choreotrich order Tintinnida, distinguished by vase-shaped shells, the name deriving from a Latin source meaning a small tinkling bell, that are called loricae , which are mostly protein but may incorporate minute pieces of minerals. [1]

Contents

Fossil record

Fossils resembling tintinnid loricas in shape and size, Calpionellids, appear as early as the Ordovician period but are formed of calcite and as no extant ciliate taxa forms calcite shells they are unlikely to be tintinnids and probably not ciliates at all. [2] Fossils which can be reliably related to extant tintinnids (e.g. fossils of agglutinated lorica) are in the fossil record during the Jurassic but do not become abundant until the Cretaceous. [3] Tintinnids are an important part of the fossil record because of the rarity with which most other ciliates become preserved under the conditions of the marine environment. The loricae of some tintinnids are easily preserved, giving them a relatively good fossil record.

Adaptation of a cut-away drawing of Tintinnopsis campanula by Faure-Fremiet (1924) showing basic tintinnid morphology. Tintinnid taxonomy classically is based on characteristics of the lorica or shell. Species in the same genus share similar lorica architecture. For example, species in the genus Tintinnopsis all have lorica covered with small mineral particles, one end is closed, and do not have any clear (hyaline) spines or collars as part of the lorica. Faure FremietTspCamp.jpg
Adaptation of a cut-away drawing of Tintinnopsis campanula by Fauré-Fremiet (1924) showing basic tintinnid morphology. Tintinnid taxonomy classically is based on characteristics of the lorica or shell. Species in the same genus share similar lorica architecture. For example, species in the genus Tintinnopsis all have lorica covered with small mineral particles, one end is closed, and do not have any clear (hyaline) spines or collars as part of the lorica.

Description

Haeckel Ciliata Haeckel Ciliata.jpg
Haeckel Ciliata

Tintinnid loricas or shells show an amazing variety of styles. They were among the many planktonic microorganisms featured in Ernst's Haeckel's classic work popularizing the beauty of the natural world "Art forms in Nature" (Kunstformen der Natur).

Like other protists, tintinnids are complex single-celled eukaryotic organisms. Tintinnids are heterotrophic aquatic organisms. They feed primarily on photosynthetic algae and bacteria. [4] They are part of the microzooplankton (between 20 and 200 micrometres in size). Tintinnids are found in marine and freshwaters. However, they are most common in salt water and are usually present in concentrations of about 100 a liter but can reach abundances of several thousand per litre. [5] Characteristics of their lorica, or shells, are classically used to distinguish the roughly 1000 species described. However, in recent years application of histological and molecular techniques have led to many taxonomic revisions. [6]

Many species appear to have wide distributions (for example from the Chesapeake Bay to New Caledonia) while others are restricted to certain areas, such as arctic waters or coastal seas. [7] Nonetheless, in any given locale dozens of species can be found. Like other members of the microzooplankton (such as oligotrich ciliates, heterotrophic dinoflagellates, radiolarians, etc.), tintinnids are a vital link in aquatic food chains as they are the 'herbivores' of the plankton. They feed on phytoplankton (algae and cyanobacteria) and in turn act as food for larger organisms such as copepods (small crustaceans) and larval fish. [8]

The color image on the right is a specimen of Dictyocysta mitra from the Bay of Villefranche in the Mediterranean Sea. The hair-like projections pointing out of the top of the shell are the cilia of the cell. The cilia generate a water flow across the mouth of the cell, bringing food into contact and move the tintinnid. Their swimming pattern is rather 'jumpy'- or dancing- they are part of the 'choreotrichs' which means dancing hairs from their swimming behaviour and cilia. [4]

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<span class="mw-page-title-main">Zooplankton</span> Heterotrophic protistan or metazoan members of the plankton ecosystem

Zooplankton are the animal component of the planktonic community. Plankton are aquatic organisms that are unable to swim effectively against currents. Consequently, they drift or are carried along by currents in the ocean, or by currents in seas, lakes or rivers.

<span class="mw-page-title-main">Choreotrich</span> Subclass of single-celled organisms

The choreotrichs are a group of small marine ciliates. Their name reflects the impression that they appear to dance. The group includes the tintinnids, which produce species-specific loricae (shells), and are important because these may be preserved as microfossils. The cyst forms have been suggested to be affiliated to Chitinozoans, although other studies suggest Chitinozoans to have affinities to larger marine animals, and not tintinnids. Often they have been included among the oligotrichs. Tintinnids seem to be an excessively specious group as over 400 living species have been described, based on characteristics of the lorica or shell.

<span class="mw-page-title-main">Coccolith</span>

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<span class="mw-page-title-main">Calpionellid</span> Family of single-celled organisms

Calpionellids are an extinct group of eukaryotic single celled organisms of uncertain affinities. Their fossils are found in marine rocks of Upper Jurassic to Lower Cretaceous age. They were planktic organisms with urn-shaped, calcitic tests that had a widespread distribution across the Tethys Ocean from the late Tithonian to the early Valanginian and were characterised by rapid evolution, and their abundant remains in deep sea sediments from this interval are important as they allow long distance biostratigraphic correlation and precise dating. Calpionellids were not confined to the Tethys, as they have also been found in the Vaca Muerta of northern Patagonia, in what was then the southeastern Pacific. Calpionellids are divided into two main families, the Chitinoidellidae, which are the earliest members of the group, appearing in the mid Tithonian, characterised by microgranular lorica. Calpionellidae appear later, including widespread genera such as Calpionella and Calpionellites, and have combined microgranular and hyaline lorica. A third family, the Semichitinoidellidae are sometimes recognised.

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References

  1. Agatha, S; Laval-Peuto, M; Simon, P (2012). "The tintinnid lorica". In Coats, D.W.; Montagnes, D.J.S.; Stoecker, D.K.; Dolan, J.R.; Agatha, S. (eds.). The biology and ecology of tintinnid ciliates : models for marine plankton. Wiley. pp. 17–41. ISBN   978-0-470-67151-1. OCLC   793006266.
  2. Remane, J. (1987) [1985]. "Calpionellids". In Bolli, H.M.; Saunders, J. B.; Perch-Nielsen, K. (eds.). Plankton Stratigraphy. Vol. 1. Cambridge University Press. pp. 555–572. ISBN   978-0-521-36719-6.
  3. Lipps, J. H.; Stoeck, T.; Dunthorn, M. (2012). "Fossil tintinnids". The biology ... 2012 . pp. 186–197.
  4. 1 2 Montagnes, D. J. S. (2012). "Ecophysiology and behavior of tintinnids". The biology ... 2012 . pp. 85–121.
  5. McManus, G. B.; Santoferrara, L. F. (2012). "Tintinnids in microzooplankton communities". The biology ... 2012 . pp. 198–213.
  6. Agatha, S.; Strûder-Kypke, M. C. (2012). "Systematics and Evolution of tintinnid ciliates". The biology ... 2012 . pp. 42–84.
  7. Dolan, J. R.; Pierce, R. W. (2012). "Diversity and distributions of tintinnds". The biology ... 2012 . pp. 214–243.
  8. Stoecker, D. K. (2012). "Predators of tintinnids". The biology ... 2012 . pp. 122–144.