Conodonts (
Greek
Greek may refer to:
Greece
Anything of, from, or related to Greece, a country in Southern Europe:
*Greeks, an ethnic group.
*Greek language, a branch of the Indo-European language family.
**Proto-Greek language, the assumed last common ancestor ...
''kōnos'', "
cone", + ''odont'', "
tooth
A tooth ( : teeth) is a hard, calcified structure found in the jaws (or mouths) of many vertebrates and used to break down food. Some animals, particularly carnivores and omnivores, also use teeth to help with capturing or wounding prey, t ...
") are an extinct group of
agnatha
Agnatha (, Ancient Greek 'without jaws') is an infraphylum of jawless fish in the phylum Chordata, subphylum Vertebrata, consisting of both present ( cyclostomes) and extinct (conodonts and ostracoderms) species. Among recent animals, cyclos ...
n (jawless) vertebrates resembling eels, classified in the
class Conodonta. For many years, they were known only from their tooth-like oral elements, which are usually found in isolation and are now called conodont elements. Knowledge about soft tissues remains limited. They existed in the world's oceans for over 300 million years, from the
Cambrian
The Cambrian Period ( ; sometimes symbolized Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ag ...
to the beginning of the Jurassic. Conodont elements are widely used as
index fossils, fossils used to define and identify
geological periods
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochro ...
. The animals are also called Conodontophora (conodont bearers) to avoid ambiguity.
Discovery and understanding of conodonts
The teeth-like fossils of the conodont were first discovered by
Heinz Christian Pander
Heinz Christian Pander, also Christian Heinrich Pander ( – ), was a Russian Empire ethnic Baltic German biologist and embryologist.
Biography
In 1817 he received his doctorate from the University of Würzburg, and spent several years (1827� ...
and the results published in
Saint Petersburg, Russia
Saint Petersburg ( rus, links=no, Санкт-Петербург, a=Ru-Sankt Peterburg Leningrad Petrograd Piter.ogg, r=Sankt-Peterburg, p=ˈsankt pʲɪtʲɪrˈburk), formerly known as Petrograd (1914–1924) and later Leningrad (1924–1991), i ...
, in 1856.
The name ''pander'' is commonly used in scientific names of conodonts.
It was only in the early 1980s that the first fossil evidence of the rest of the animal was found (see below). In the 1990s exquisite fossils were found in South Africa in which the soft tissue had been converted to clay, preserving even muscle fibres. The presence of muscles for rotating the eyes showed definitively that the animals were primitive vertebrates.
Description

The 11 known fossil imprints of conodont animals record an
eel-like creature with 15 or, more rarely, 19 elements that form a bilaterally symmetrical array in the head.
The organisms ranged from 1–40 cm (''
Promissum
''Promissum'' is an extinct genus of conodonts, primitive chordates, that lived during the Upper Ordovician period.
A conodont, ''Promissum'' had a primitive mouth under its eyes with mineralized teeth, which are both typical for conodonts. It h ...
'') in length.
Conodonts had large eyes, fins with fin rays,
chevron-shaped muscles and a
notochord
In anatomy, the notochord is a flexible rod which is similar in structure to the stiffer cartilage. If a species has a notochord at any stage of its life cycle (along with 4 other features), it is, by definition, a chordate. The notochord cons ...
.
Elements
Conodont elements consist of mineralised teeth-like structures of varying morphology and complexity. The evolution of
mineralized tissues
Mineralized tissues are biological tissues that incorporate minerals into soft matrices. Typically these tissues form a protective shield or structural support. Bone, mollusc shells, deep sea sponge ''Euplectella'' species, radiolarians, diat ...
has been puzzling for more than a century. It has been hypothesized that the first mechanism of chordate tissue mineralization began either in the oral skeleton of conodonts or the dermal skeleton of early
agnathans
Agnatha (, Ancient Greek 'without jaws') is an infraphylum of jawless fish in the phylum Chordata, subphylum Vertebrata, consisting of both present (Cyclostomata, cyclostomes) and extinct (conodonts and ostracoderms) species. Among recent animal ...
.
The element array constituted a feeding apparatus that is radically different from the jaws of modern animals. They are now termed "conodont elements" to avoid confusion. The three forms of teeth, i.e., coniform cones, ramiform bars, and pectiniform platforms, probably performed different functions.
For many years, conodonts were known only from enigmatic tooth-like microfossils (200 micrometers to 5 millimeters in length), which occur commonly, but not always, in isolation and were not associated with any other fossil. Until the early 1980s, conodont teeth had not been found in association with fossils of the host organism, in a
konservat lagerstätte.
This is because the conodont animal was soft-bodied, thus everything but the teeth was unsuited for preservation under normal circumstances.
These microfossils are made of
hydroxylapatite
Hydroxyapatite, also called hydroxylapatite (HA), is a naturally occurring mineral form of calcium apatite with the formula Ca5(PO4)3(OH), but it is usually written Ca10(PO4)6(OH)2 to denote that the crystal unit cell comprises two entities. ...
(a phosphatic mineral). The conodont elements can be extracted from rock using adequate solvents.
They are widely
used in biostratigraphy. Conodont elements are also used as
paleothermometer
A paleothermometer is a methodology that provides an estimate of the ambient temperature at the time of formation of a natural material. Most paleothermometers are based on empirically-calibrated proxy relationships, such as the tree ring or TEX ...
s, a proxy for thermal alteration in the host rock, because under higher temperatures, the phosphate undergoes predictable and permanent color changes, measured with the
conodont alteration index. This has made them useful for
petroleum exploration where they are known, in rocks dating from the
Cambrian
The Cambrian Period ( ; sometimes symbolized Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ag ...
to the Late
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...
.
Multielement conodonts

The conodont apparatus may comprise a number of discrete elements, including the spathognathiform, ozarkodiniform, trichonodelliform, neoprioniodiform, and other forms.
In the 1930s, the concept of conodont assemblages was described by Hermann Schmidt and by Harold W. Scott in 1934.
Elements of ozarkodinids
The feeding apparatus of
ozarkodinids is composed of an axial Sa element at the front, flanked by two groups of four close-set elongate Sb and Sc elements which were inclined obliquely inwards and forwards. Above these elements lay a pair of arched and inward pointing (makellate) M elements. Behind the S-M array lay transversely oriented and bilaterally opposed (pectiniform, i.e. comb-shaped) Pb and Pa elements.
Ecology

The "teeth" of some conodonts have been interpreted as filter-feeding apparatuses, filtering plankton from the water and passing it down the throat. Others have been interpreted as a "grasping and crushing array".
[ Wear on some condont elements suggests that they functioned like teeth, with both wear marks likely created by food as well as by occlusion with other elements.] Studies have concluded that conodonts taxa occupied both pelagic
The pelagic zone consists of the water column of the open ocean, and can be further divided into regions by depth (as illustrated on the right). The word ''pelagic'' is derived . The pelagic zone can be thought of as an imaginary cylinder or w ...
(open ocean) and nektobenthic (swimming above the sediment surface) niches. The preserved musculature suggests that some conodonts (''Promissum'' at least) were efficient cruisers, but incapable of bursts of speed.[ Based on isotopic evidence, some Devonian conodonts have been proposed to have been low-level consumers that fed on ]zooplankton
Zooplankton are the animal component of the planktonic community ("zoo" comes from the Greek word for ''animal''). Plankton are aquatic organisms that are unable to swim effectively against currents, and consequently drift or are carried along by ...
.
A study on the population dynamics of ''Alternognathus
''Alternognathus'' is an extinct conodont
Conodonts (Greek ''kōnos'', "cone", + ''odont'', "tooth") are an extinct group of agnathan (jawless) vertebrates resembling eels, classified in the class Conodonta. For many years, they were known on ...
'' has been published. Among other things, it demonstrates that at least this taxon had short lifespans lasting around a month. A study Sr/ Ca and Ba/Ca ratios of a population of conodonts from a carbonate platform from the Silurian of Sweden found that the different conodont species and genera likely occupied different trophic niches.
The some species of the genus '' Panderodus'' have been speculated to be venomous, based on grooves found on some elements..
Classification and phylogeny
, scientists classify the conodonts in the phylum
In biology, a phylum (; plural: phyla) is a level of classification or taxonomic rank below kingdom and above class. Traditionally, in botany the term division has been used instead of phylum, although the International Code of Nomenclatu ...
Chordata
A chordate () is an animal of the phylum Chordata (). All chordates possess, at some point during their larval or adult stages, five synapomorphies, or primary physical characteristics, that distinguish them from all the other taxa. These five ...
on the basis of their fins with fin rays, chevron-shaped muscles and notochord
In anatomy, the notochord is a flexible rod which is similar in structure to the stiffer cartilage. If a species has a notochord at any stage of its life cycle (along with 4 other features), it is, by definition, a chordate. The notochord cons ...
.
Milsom and Rigby envision them as vertebrates similar in appearance to modern hagfish and lampreys,
and phylogenetic
In biology, phylogenetics (; from Greek φυλή/ φῦλον [] "tribe, clan, race", and wikt:γενετικός, γενετικός [] "origin, source, birth") is the study of the evolutionary history and relationships among or within groups o ...
analysis suggests they are more derived than either of these groups.
However, this analysis comes with one caveat: early forms of conodonts, the protoconodonts, appear to form a distinct clade from the later paraconodonts and euconodonts. Protoconodonts likely represent a stem group to the phylum that includes chaetognath worms; this conclusion suggests that chaetognaths are not close relatives of true conodonts.
Moreover, some analyses do not regard conodonts as either vertebrate
Vertebrates () comprise all animal taxon, taxa within the subphylum Vertebrata () (chordates with vertebral column, backbones), including all mammals, birds, reptiles, amphibians, and fish. Vertebrates represent the overwhelming majority of the ...
s or craniates, because they lack the main characteristics of these groups. More recently it has been proposed that conodonts may be stem- cyclostomes, more closely related to hagfish and lampreys than other living vertebrates.
Evolutionary history
The earliest fossils of conodonts are known from the Cambrian period. Conodonts extensively diversified during the early Ordovician, reaching their apex of diversity during the middle part of the period, and experienced a sharp decline during the late Ordovician and Silurian, before reaching another peak of diversity during the mid-late Devonian. Conodont diversity declined during the Carboniferous, with an extinction event at the end of the middle Tournaisian
The Tournaisian is in the ICS geologic timescale the lowest stage or oldest age of the Mississippian, the oldest subsystem of the Carboniferous. The Tournaisian age lasted from Ma to Ma. It is preceded by the Famennian (the uppermost stag ...
and a prolonged period of significant loss of diversity during the Pennsylvanian Pennsylvanian may refer to:
* A person or thing from Pennsylvania
* Pennsylvanian (geology)
The Pennsylvanian ( , also known as Upper Carboniferous or Late Carboniferous) is, in the International Commission on Stratigraphy, ICS geologic timesca ...
. Only a handful of conodont genera were present during the Permian, though diversity increased after the P-T extinction during the Early Triassic. Diversity continued to decline during the Middle and Late Triassic, culminating in their extinction at the Triassic-Jurassic boundary. Much of their diversity during the Paleozoic was likely controlled by sea levels and temperature, with the major declines during the Late Ordovician and Late Carboniferous due to cooler temperatures, especially glacial events and associated marine regressions which reduced continental shelf area. However, their final demise is more likely related to biotic interactions, perhaps competition with new Mesozoic taxa.
Taxonomy
Conodonta taxonomy based on Sweet & Donoghue, Mikko's Phylogeny Archive[Mikko's Phylogeny Archiv]
and Fish classification 2017.
Conodonta Pander, 1856 non Eichenberg, 1930 sensu Sweet & Donoghue, 2001 Eichenberg, 1930; Conodontochordata">onodontia; Conodontophorida Eichenberg, 1930; Conodontochordata* Paraconodonta Müller, 1962 araconodontida** Amphigeisiniformes
*** Amphigeisinidae Miller, 1981
** Westergaardodiniformes Lindström, 1970
*** Westergaardodinidae Müller, 1959 hosonodinidae/small>
*** Furnishinidae Müller & Nogami, 1971
* Conodontophora Eichenberg, 1930
** Cavidonti Sweet, 1988
*** Proconodontiformes Sweet, 1988
**** Pseudooneotodidae Wang & Aldridge, 2010
**** Proconodontidae Lindström, 1981
**** Cordylodontidae Lindström, 1970 Hass, 1959">yrtoniodontinae Hass, 1959****Fryxellodontina
*****Fryxellodontidae
Fryxellodontidae is an extinct family of conodonts in the order Proconodontida
Proconodontida is an order of conodonts.
References
* A suprageneric taxonomy of the conodonts. Maurits Lindström, Lethaia, Volume 3, Issue 4, pages 427–445 ...
Miller, 1981
***** Pygodontidae Bergstrom, 1981
****Belodellina Sweet, 1988
***** Ansellidae Faohraeus & Hunter, 1985
***** Dapsilodontidae Sweet, 1988
***** Belodellidae Khodalevich & Tschernich, 1973 ambropustulidae** Conodonti Pander, 1856 non Branson, 1938
*** Oneotodontidae Miller, 1981 Miller, 1981">eridontidae Miller, 1981
*** Protopanderodontida Sweet, 1988 anderodontida**** ? Pronodontidae Lindström, 1970
**** ? Cornuodontidae Faohraeus, 1966
**** ? Protopanderodontidae Lindström, 1970 Bergström, 1981">uanognathidae Bergström, 1981****? Strachanognathidae Bergström, 1981
****? Pseudooneotodidae
**** Clavohamulidae Lindström, 1970
**** Drepanoistodontidae Faohraeus, 1978
**** Acanthodontidae Lindström, 1970
**** Scolopodontidae Bergström, 1981
**** Panderodontidae Lindström, 1970
*** Prioniodontida
Prioniodontida, also known as the "complex conodonts", is a large clade of conodonts that includes two major evolutionary grades; the Prioniodinina and the Ozarkodinina. It includes many of the more famous conodonts, such as the giant ordovician ...
Dzik, 1976 istacodontida(paraphyletic)
**** ? Acodontidae Dzik, 1993 Sweet, 1988">ripodontinae Sweet, 1988****? Cahabagnathidae Stouge & Bagnoli 1999
****? Distacodontidae Bassler, 1925 emend. Ulrich & Bassler, 1926 repanodontinae Fahraeus & Nowlan, 1978; Lonchodininae Hass, 1959****? Gamachignathidae Wang & Aldridge, 2010
****? Jablonnodontidae Dzik, 2006
****? Nurrellidae Pomešano-Cherchi, 1967
**** ? Paracordylodontidae Bergström, 1981
****? Playfordiidae Dzik, 2002
****? Ulrichodinidae Bergström, 1981
****''Rossodus
''Rossodus'' is an extinct genus of conodonts in the clade Prioniodontida, the "complex conodonts", of the Early Ordovician
The Ordovician ( ) is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spa ...
'' Repetski & Ethington, 1983
**** Multioistodontidae Harris, 1964 ischidognathidae**** Oistodontidae Lindström, 1970
**** Periodontidae Lindström, 1970
**** Rhipidognathidae Lindström, 1970 sensu Sweet, 1988
**** Prioniodontidae Bassler, 1925
**** Phragmodontidae Bergström, 1981
**** Plectodinidae Sweet, 1988
****Icriodontacea
***** Balognathidae
Balognathidae is an extinct conodont family.
Genera
Genera are:
* †'' Amorphognathus''
* †'' Baltoniodus''
* †'' Birksfeldia''
* †'' Icriodella''
* †'' Notiodella''
* †'' Polyplacognathus''
* †'' Prioniodus''
* †''Promissum''
* � ...
(Hass, 1959)
***** Polyplacognathidae Bergström, 1981
***** Distomodontidae Klapper, 1981
***** Icriodellidae Sweet, 1988
***** Icriodontidae Müller & Müller, 1957
****Prioniodinida
Prioniodinida is an extinct order of conodonts, a jawless vertebrate.
Families
Families are:
* † Bactrognathidae
* † Chirognathidae
* †Ellisoniidae
* † Gondolellidae
* † Prioniodinidae
References
* Sweet, W. C; P. C.J Donoghue (200 ...
Sweet, 1988
***** ? Oepikodontidae Bergström, 1981
*****? Xaniognathidae Sweet, 1981
***** Chirognathidae Branson & Mehl, 1944
***** Prioniodinidae Bassler, 1925 Mueller, 1956">ibbardellidae Mueller, 1956***** Bactrognathidae Lindström, 1970
*****Ellisoniidae
Ellisoniidae is an extinct family of conodonts, a kind of primitive chordate.
Genera
Genera are:
* †'' Ellisonia''
* †'' Foliella''
* †'' Hadrodontina''
* †'' Parapachycladina''
* †''Parafurnishius''
* †'' Stepanovites''
References ...
Clark, 1972
*****Gondolellidae
Gondolellidae is an extinct family of conodonts in the order Ozarkodinida
Ozarkodinida is an extinct conodont order. It is part of the clade Prioniodontida, also known as the "complex conodonts".
Name
Ozarkodinida is named after the Ozark M ...
Lindström, 1970
****Ozarkodinida
Ozarkodinida is an extinct conodont order. It is part of the clade Prioniodontida, also known as the "complex conodonts".
Name
Ozarkodinida is named after the Ozark Mountains of Missouri
Missouri is a U.S. state, state in the Midwester ...
Dzik, 1976 olygnathida***** ? Anchignathodontidae Clark, 1972
*****? Archeognathidae Miller, 1969
*****? Belodontidae Huddle, 1934
*****? Coleodontidae Branson & Mehl, 1944 Müller, 1956; Loxodontidae">ibbardellidae Müller, 1956; Loxodontidae*****? Eognathodontidae Bardashev, Weddige & Ziegler, 2002
*****? Francodinidae Dzik, 2006
*****? Gladigondolellidae (Hirsch, 1994) [Sephardiellinae Plasencia, Hirsch & Márquez-Aliaga, 2007; Neogondolellinae Hirsch, 1994; Cornudininae Orchard, 2005; Epigondolellinae Orchard, 2005; Marquezellinae Plasencia ''et al.'', 2018; Paragondolellinae Orchard, 2005; Pseudofurnishiidae Ramovs, 1977]
*****?Iowagnathidae Liu ''et al.'', 2017
*****?Novispathodontidae (Orchard, 2005)
*****?Trucherognathidae Branson & Mehl, 1944
*****?Vjalovognathidae Shen, Yuan & Henderson, 2015
*****? Wapitiodontidae Orchard, 2005
***** Cryptotaxidae Klapper & Philip, 1971
*****Spathognathodontidae
Spathognathodontidae is an extinct conodont family ranging from the Silurian to the Devonian.On Classification of Pridoli (Silurian)-Lochkovian (Devonian) Spathognathodontidae (Conodonts). Murphy M.A., Valenzuela-Ríos J.I. and Carls P., 2004, Un ...
Hass, 1959 Ozarkodinidae Dzik, 1976">/small>Ozarkodinidae Dzik, 1976***** Pterospathodontidae Cooper, 1977 arniodontidae
***** Kockelellidae Klapper, 1981 aenodontontidae***** Polygnathidae Bassler, 1925 Bardashev, Weddige & Ziegler, 2002">Eopolygnathidae Bardashev, Weddige & Ziegler, 2002***** Palmatolepidae Sweet, 1988
***** Hindeodontidae (Hass, 1959)
*****Elictognathidae
Elictognathidae is an extinct conodont family.Supplement 2, Conodonta. SM Bergstrom, G Klapper, RL Austin, FHT Rhodes, Treatise on Invertebrate Paleontology 1981
Genera are '' Alternognathus'', '' Elictognathus'', and '' Pinacognathus''.
Refer ...
Austin & Rhodes, 1981
*****Gnathodontidae
Gnathodontidae is an extinct conodont family in the order Ozarkodinida. It consists of the extinct genus '' Icriodus''.
References
* Carboniferous gnathodontid conodont apparatuses: evidence of a dual origin for Pennsylvanian taxa. RC Grays ...
Sweet, 1988
*****Idiognathodontidae
Idiognathodontidae is an extinct conodont family.New Pennsylvanian conodonts from Oklahoma. RW Harris and RV Hollingsworth, American Journal of Science, March 1933, Series 5, Vol. 25, no. 147, pages 193-204,
Genera are ''Gnathodus'', ''Idiognat ...
Harris & Hollingsworth, 1933
***** Mestognathidae Austin & Rhodes, 1981
*****Cavusgnathidae
Cavusgnathidae is an extinct family of conodonts in the order Ozarkodinida.
Genera
Genera are,
* †'' Adetognathus''
* †''Cavusgnathus''
* †''Clydagnathus''
* †'' Ferganaegnathodus''
* †'' Neolochriea''
* †'' Patrognathus''
* †''Pse ...
Austin & Rhodes, 1981
***** Sweetognathidae Ritter, 1986
See also
* Timeline of the evolutionary history of life
The timeline of the evolutionary history of life represents the current scientific theory outlining the major events during the development of life on planet Earth. Dates in this article are consensus estimates based on scientific evidence, mai ...
* Micropaleontology
Micropaleontology (American spelling; spelled micropalaeontology in European usage) is the branch of paleontology ( palaeontology) that studies microfossils, or fossils that require the use of a microscope to see the organism, its morphology and ...
* List of conodont genera
This is a list of conodonts genera, sorted in alphabetical order.
A-C
* †'' Acanthodus''
* †''Acodus''
* †'' Acuminatella''
* †'' Alternognathus''
* †'' Amorphognathus''
* †''Ancyrodella''
* †''Ancyrognathus''
* †'' Anticostiodus ...
* Conodont biostratigraphy
Conodonts are an extinct class of animals whose feeding apparatuses called ''teeth'' or ''elements'' are common microfossils found in strata dating from the Stage 10 of the Furongian, the fourth and final series of the Cambrian, to the Rhaetian st ...
* Conodont alteration index
References
Further reading
*
*
*
* Gould, Stephen Jay (1985). "Reducing Riddles". In ''The Flamingo's Smile'', 245-260. New York, W.W. Norton and Company. .
*
*Knell, Simon J. ''The Great Fossil Enigma: The Search for the Conodont Animal'' (Indiana University Press; 2012) 440 pages
* Sweet, Walter (1988). ''The Conodonta: morphology, taxonomy, paleoecology, and evolutionary history of a long-extinct animal phylum.'' Oxford, Clarendon Press
Oxford University Press (OUP) is the university press of the University of Oxford. It is the largest university press in the world, and its printing history dates back to the 1480s. Having been officially granted the legal right to print books ...
.
*
*
External links
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{{Authority control
Furongian first appearances
Late Triassic extinctions
Cambrian chordates