Graptolite
Graptolites Temporal range: Rhabdopleura.[2]
Survive to the present via the living genus | |
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Cryptograptus from the Silurian of South America. Specimen at the Royal Ontario Museum | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Hemichordata |
Class: | Pterobranchia |
Subclass: | Graptolithina Bronn, 1849 |
Subgroups | |
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Graptolites are a group of
Fossil graptolites and Rhabdopleura share a colony structure of interconnected zooids housed in organic tubes (theca) which have a basic structure of stacked half-rings (fuselli). Most extinct graptolites belong to two major orders: the bush-like
The name graptolite comes from the
History
The name "graptolite" originates from the genus Graptolithus ("writing on the rocks"), which was used by
Graptolite fossils were later referred to a variety of groups, including other branching colonial animals such as bryozoans ("moss animals") and hydrozoans. The term Graptolithina was established by Bronn in 1849, who considered them to represent orthoconic cephalopods. By the mid-20th century, graptolites were recognized as a unique group closely related to living pterobranchs in the genera Rhabdopleura and Cephalodiscus, which had been described in the late 19th century. Graptolithus, as a genus, was officially abandoned in 1954 by the ICZN.[5]
Morphology
Colony structure
Each graptolite colony originates from an initial individual, called the sicular zooid, from which the subsequent
Early in the development of a colony, the tubarium splits into a variable number of branches (known as stipes) and different arrangements of the theca, features which are important in the identification of graptolite fossils. Colonies can be classified by their total number of theca rows (biserial colonies have two rows, uniserial have one) and the number of initial stipes per colony (multiramous colonies have many stipes, pauciramous colonies have two or one). Each thecal tube is mostly made up by two series of stacked semicircular half-rings, known as fuselli (sing: fusellum). The fuselli resemble growth lines when preserved in fossils, and the two stacks meet along a suture with a zig-zag pattern. Fuselli are the major reinforcing component of a tubarium, though they are assisted by one or more additional layers of looser tissue, the cortex.
The earliest graptolites appeared in the fossil record during the Cambrian, and were generally
Zooids
A mature zooid has three important regions, the preoral disc or cephalic shield, the collar and the trunk. In the collar, the mouth and anus (U-shaped digestive system) and arms are found; Graptholitina has a single pair of arms with several paired tentacles. As a nervous system, graptolites have a simple layer of fibers between the epidermis and the basal lamina, also have a collar ganglion that gives rise to several nerve branches, similar to the neural tube of chordates.[6] Proper fossils of the soft parts of graptolites have yet to be found, and it is not known if they had pharyngeal gill slits or not,[7] but based on extant Rhabdopleura, it is likely that the grapotlite zooids had the same morphology.[4]
Taxonomy
Since the 1970s, as a result of advances in
On the other hand,
Phylogeny of Pterobranchia[3] | |||||||||||||||
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Graptolithina includes several minor families as well as two main extinct orders, Dendroidea (
Taxonomy of Graptolithina by Maletz (2014):[3][4]
Subclass Graptolithina Bronn, 1849
- Incertae sedis
- Family RhabdopleuridaeHarmer, 1905
- Family †Cysticamaridae Bulman, 1955
- Family †Wimanicrustidae Bulman, 1970
- Family †Dithecodendridae Obut, 1964
- Family †Cyclograptidae Bulman, 1938
- Family
- Order †Dendroidea Nicholson, 1872
- Family †Dendrograptidae Roemer, 1897 in Frech, 1897
- Family †Acanthograptidae Bulman, 1938
- Family †Mastigograptidae Bates & Urbanek, 2002
- Order †Graptoloidea Lapworth, 1875 in Hopkinson & Lapworth, 1875 (planktic graptolites)
- Suborder †GraptodendroidinaMu & Lin, 1981 in Lin (1981)
- Family †Anisograptidae Bulman, 1950
- Suborder †Sinograpta Maletz et al., 2009
- Family †Sigmagraptidae Cooper & Fortey, 1982
- Family †Sinograptidae Mu, 1957
- Family †Abrograptidae Mu, 1958
- Suborder †Dichograptina Lapworth, 1873
- Family †Dichograptidae Lapworth, 1873
- Family †Didymograptidae Mu, 1950
- Family †Pterograptidae Mu, 1950
- Family †Tetragraptidae Frech, 1897
- Suborder †Glossograptina Jaanusson, 1960
- Family †Isograptidae Harris, 1933
- Family †Glossograptidae Lapworth, 1873
- Suborder †Axonophora Frech, 1897 (biserial graptolites, and also retiolitids and monograptids)
- Infraorder †Diplograptina Lapworth, 1880
- Family †Diplograptidae Lapworth, 1873
- Subfamily †Diplograptinae Lapworth, 1873
- Subfamily †Orthograptinae Mitchell, 1987
- Family †Lasiograptidae Lapworth, 1880e
- Family †Climacograptidae Frech, 1897
- Family †Dicranograptidae Lapworth, 1873
- Subfamily †Dicranograptinae Lapworth, 1873
- Subfamily †Nemagraptinae Lapworth, 1873
- Family †Diplograptidae Lapworth, 1873
- Infraorder †Neograptina Štorch et al., 2011
- Family †Normalograptidae Štorch & Serpagli, 1993
- Family †Neodiplograptidae Melchin et al., 2011
- Subfamily †Neodiplograptinae Melchin et al., 2011
- Subfamily †Petalolithinae Bulman, 1955
- Superfamily †Retiolitoidea Lapworth, 1873
- Family †Retiolitidae Lapworth, 1873
- Subfamily †Retiolitinae Lapworth, 1873
- Subfamily †Plectograptinae Bouček & Münch, 1952
- Family †Retiolitidae Lapworth, 1873
- Superfamily †Monograptoidea Lapworth, 1873
- Family †Dimorphograptidae Elles & Wood, 1908
- Family †Monograptidae Lapworth, 1873
- Infraorder †Diplograptina Lapworth, 1880
- Suborder †
Ecology
Graptolites were a major component of the early Paleozoic ecosystems, especially for the zooplankton because the most abundant and diverse species were planktonic. Graptolites were most likely suspension feeders and strained the water for food such as plankton.[9]
Inferring by analogy with modern pterobranchs, they were able to migrate vertically through the water column for feeding efficiency and to avoid predators. With ecological models and studies of the
Their locomotion was relative to the water mass in which they lived but the exact mechanisms (such as turbulence,
There are still many questions regarding graptolite locomotion but all these mechanisms are possible alternatives depending on the species and its habitat. For benthic species, that lived attached to the sediment or any other organism, this was not a problem; the zooids were able to move but restricted within the tubarium. Although this zooid movement is possible in both planktic and benthic species, it is limited by the stolon but is particularly useful for feeding. Using their arms and tentacles, which are close to the mouth, they filter the water to catch any particles of food.[10]
Life cycle
The study of the developmental biology of Graptholitina has been possible by the discovery of the species R. compacta and R. normani in shallow waters; it is assumed that graptolite fossils had a similar development as their extant representatives. The life cycle comprises two events, the ontogeny and the astogeny, where the main difference is whether the development is happening in the individual organism or in the modular growth of the colony.
The life cycle begins with a planktonic planula-like larva produced by sexual reproduction, which later becomes the sicular zooid who starts a colony. In Rhabdopleura, the colonies bear male and female zooids but fertilized eggs are incubated in the female tubarium, and stay there until they become larvae able to swim (after 4–7 days) to settle away to start a new colony. Each larva surrounds itself in a protective cocoon where the metamorphosis to the zooid takes place (7–10 days) and attaches with the posterior part of the body, where the stalk will eventually develop.[4]
The development is indirect and
Graptolites in evolutionary development
In recent years, living graptolites have been used as a hemichordate model for
Geological relevance
Preservation
Graptolites are common fossils and have a worldwide distribution. They are most commonly found in shales and mudrocks where sea-bed fossils are rare, this type of rock having formed from sediment deposited in relatively deep water that had poor bottom circulation, was deficient in oxygen, and had no scavengers. The dead planktic graptolites, having sunk to the sea floor, would eventually become entombed in the sediment and were thus well preserved.
These colonial animals are also found in limestones and cherts, but generally these rocks were deposited in conditions which were more favorable for bottom-dwelling life, including scavengers, and undoubtedly most graptolite remains deposited here were generally eaten by other animals.
Fossils are often found flattened along the bedding plane of the rocks in which they occur, though may be found in three dimensions when they are infilled by
Graptolites are normally preserved as a black
A well-known locality for graptolite fossils in Britain is
Stratigraphy
Graptolite fossils have predictable preservation, widespread distribution, and gradual change over a
The
Graptolite diversity was greatly reduced during the Sedgwickii Event in the Aeronian.[16] This event has been attested in locations such as today's Canada, Libya as well as in La Chilca Formation of Argentina (then part of Gondwana).[16]
Ranges of Graptolite taxa. |
Researchers
The following is a selection of graptolite and pterobranch researchers:[4]
- Joachim Barrande (1799–1883)
- Hanns Bruno Geinitz (1814–1900)
- James Hall (1811–1898)
- Frederick M'Coy (1817–1899)
- Henry Alleyne Nicholson (1844–1899)
- John Hopkinson (1844–1919)
- Sven Leonhard Törnquist (1840–1920)
- Sven Axel Tullberg (1852–1886)
- Gerhard Holm (1853–1926)
- Carl Wiman (1867–1944)
- Thomas Sergeant Hall (1858–1915)
- Alexander Robert Keble (1884–1963)
- Noel Benson (1885–1957)
- William John Harris (1886–1957)
- David Evan Thomas (1902–1978)
- Mu Enzhi (1917–1987)
- Li Jijin (1928–2013)
- Vladimir Nikolayevich Beklemishev(1890–1962)
- Michael Sars (1805–1869)
- George Ossian Sars (1837–1927)
- William Carmichael M'Intosh(1838–1931)
- Nancy Kirk (1916–2005)
- Roman Kozłowski (1889–1977)
- Jörg Maletz
- Denis E. B. Bates
- Alfred C. Lenz
- Chris B. Cameron
- Adam Urbanek
- David K. Loydell
- Hermann Jaeger (1929–1992)
See also
References
- ^ a b Maletz, J. (2014). Hemichordata (Pterobranchia, Enteropneusta) and the fossil record. Palaeogeography, Palaeoclimatology, Palaeoecology, 398:16-27.
- ^ a b Mitchell, C.E., Melchin, M.J., Cameron, C.B. & Maletz, J. (2013) Phylogenetic analysis reveals that Rhabdopleura is an extant graptolite. Lethaia, 46:34–56.
- ^ ISSN 1214-1119.
- ^ ISBN 9781118515617.
- ^ Bulman, M. (1970) In Teichert, C. (ed.). Treatise on Invertebrate Paleontology. Part V. Graptolithina, with sections on Enteropneusta and Pterobranchia. (2nd Edition). Geological Society of America and University of Kansas Press, Boulder, Colorado and Lawrence, Kansas, XXXII + 163 pp.
- ^ a b Sato, A., Bishop, J. & Holland, P. (2008). Developmental Biology of Pterobranch Hemichordates: History and Perspectives. Genesis, 46:587-591.
- ^ Fundamentals of Invertebrate Palaeontology: Macrofossils
- ^ a b Fortey, Richard A. (1998). Life: A Natural History of the First Four Billion Years of Life on Earth. New York: Alfred A. Knopf. p. 129.
- ^ "Graptolites". samnoblemuseum.ou.edu. Retrieved 2018-12-28.
- ^ a b c Cooper, R., Rigby, S., Loydell, D. & Bates, D. (2012) Palaeoecology of the Graptoloidea. Earth-Science Reviews, 112(1):23-41.
- ^ Röttinger, E. & Lowe, C. (2012) Evolutionary crossroads in developmental biology: hemichordates. Development, 139:2463-2475.
- ^ a b Sato, A. & Holland, P. (2008). Asymmetry in a Pterobranch Hemichordate and the Evolution of Left-Right Patterning. Developmental Dynamics, 237:3634 –3639)
- ^ Sato, A., White-Cooper, H., Doggett, K. & Holland, P. 2009. Degenerate evolution of the hedgehog gene in a hemichordate lineage. Proceedings of the National Academy of Sciences, 106(18):7491-7494.
- ^ Bapst, D., Bullock, P., Melchin, M., Sheets, D. & Mitchell, C. (2012) Graptoloid diversity and disparity became decoupled during the Ordovician mass extinction. Proceedings of the National Academy of Sciences, 109(9):3428-3433.
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- ^ .
External links
- Classification of the Graptolithoidea - Graptolites and Pterobranchs
- Podcast on Graptolites by David Bapst - Palaeocast
- Graptolites gallery by Michael P. Klimetz - Graptolites
- What are Fossil Graptolites and why are they useful in geology? - Youtube
- Writing on the rocks - Stephen Hui Geological Museum