Biology:Embolomeri
| Embolomeres | |
|---|---|
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| Restoration of Archeria from the Lower Permian of Texas. | |
Scientific classification 
| |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Superclass: | Tetrapoda |
| Clade: | Reptiliomorpha (?) |
| Order: | †Embolomeri Cope, 1885 |
| Genera | |
|
See text. | |
Embolomeri is an order of tetrapods or stem-tetrapods, possibly members of Reptiliomorpha. Embolomeres first evolved in the Early Carboniferous (Mississippian) Period and were the largest and most successful predatory tetrapods of the Late Carboniferous (Pennsylvanian) Period. They were specialized semiaquatic predators with long bodies for eel-like undulatory swimming. Embolomeres are characterized by their vertebral centra, which are formed by two cylindrical segments, the pleurocentrum at the rear and intercentrum at the front. These segments are equal in size. Most other tetrapods have pleurocentra and intercentra which are drastically different in size and shape.[1]
Embolomeres were among the earliest large carnivorous tetrapods, with members such as the crocodilian-like Proterogyrinus appearing in the Visean stage of the Carboniferous. They declined in diversity during the Permian period, though at least one representative (Archeria) was common in the Early Permian.[2] Embolomeres went extinct shortly before the end of the Permian.[3]
Classification
The order Embolomeri was first named by Edward Drinker Cope in 1884 during his revision of "batrachian" (amphibian) evolution. Embolomeri was differentiated from several other newly named amphibian orders, such as "Rachitomi", by the presence of intercentra and pleurocentra of the same size and shape, that being large cylinders. At the time, embolomere fossils were uncommon, so Cope could only identify "cricotids" such as Cricotus as possessing embolomerous vertebrae.[4] The genus name "Cricotus" is dubious, as it has been used by Cope to refer to embolomere fossils spanning anywhere between mid-Pennsylvanian deposits of Illinois and the Permian red beds of Texas . Most paleontologists now refer the red bed "Cricotus" specimens to the genus Archeria.[2]
Michel Laurin (1998) formally defined Embolomeri as "the last common ancestor of Proterogyrinus and Archeria and all of its descendants."[5] This definition excludes Eoherpeton, which is almost always considered a close ally of the group. Some authors place Silvanerpeton or chroniosuchians as close relatives as well, though they are generally agreed to lie outside Embolomeri proper.[6][7][8][9]
The poorly-defined group Anthracosauria is sometimes considered synonymous with Embolomeri, and the group's namesake, Anthracosaurus, is an embolomere. However, other authors use the term "Anthracosauria" in reference to a broader group which includes embolomeres in combination with various other reptile-like amphibians (reptiliomorphs). Reptiliomorphs are all tetrapods more closely related to living reptiles and synapsids (mammals and their ancestors), rather than living amphibians. Despite this, reptiliomorphs likely had amphibian-like biological traits, such as water-based reproduction.
Many studies conducted since the 1990s have also placed the group Lepospondyli as closer to amniotes than embolomeres were. Lepospondyls are a particularly unusual group of tetrapods, with some members (i.e. brachystelechids) very similar to lissamphibians and others (i.e. tuditanids) very similar to amniotes. If lepospondyls are both close relatives of amniotes and the ancestors of modern amphibians, then that means that crown-Tetrapoda (descendants of the common ancestor to all living tetrapods) is a much more restricted group than previously assumed. In this situation, various traditional orders of Tetrapoda such as Embolomeri and Temnospondyli actually would qualify as stem-tetrapods due to having evolved prior to the split between modern amphibians and amniotes.[10]
However, most authors consider temnospondyls to be the ancestors of modern amphibians. This would suggest that embolomeres are likely reptiliomorphs (closer to reptiles) and within the clade Tetrapoda.[11] However, even this classification is not stable, as some analyses have found embolomeres to be more basal than temnospondyls.[12]
Below is a cladogram from Ruta et al. (2003):[11]
| Tetrapoda |
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Genera
| List of genera | |||||
| Name | Year | Age | Location | Notes | Images |
|---|---|---|---|---|---|
| Anthracosaurus | 1863 | Pennsylvanian (Westphalian A-B) |  United Kingdom ( Scotland)
|
The namesake of Anthracosauria, possessed a small number of large fangs compared to other embolomeres | 
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| Archeria | 1918 | Early Permian |  United States ( Texas)
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A common, late-surviving member of the group, sometimes considered a species of Cricotus | 
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| Aversor | 1985 | Early Permian (Ufimian) |  Russia
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Supposedly the latest surviving eogyrinid, but very poorly known | |
| Calligenethlon | 1934 | Pennsylvanian (Bashkirian) |  Canada ( Nova Scotia)
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The largest named tetrapod preserved inside lycopod tree stumps in the Joggins Fossil Cliffs | |
| Cricotus | 1875 | Pennsylvanian | United States ( Illinois)
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Responsible for the identification of Embolomeri as a unique order of tetrapods, although its history is convoluted and its taxonomic validity is questionable | |
| Carbonoherpeton | 1985 | Pennsylvanian (Westphalian D) | Canada ( Nova Scotia)
|
A lightly built member of the group with characteristics of both archeriids and eogyrinids | |
| Diplovertebron | 1879 | Pennsylvanian (Moscovian) |  Czech Republic
|
A small member of the group sometimes confused with Gephyrostegus | 
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| Eobaphetes | 1916 | Pennsylvanian | United States ( Kansas)
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A possible relative of Anthracosaurus, originally named "Erpetosuchus" until it was determined that the name was preoccupied by a Triassic reptile. | |
| Eogyrinus | 1926 | Pennsylvanian (Westphalian B) | United Kingdom ( England)
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One of the largest and most well-known of the eogyrinids, although sometimes synonymized with Pholiderpeton | 
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| Eoherpeton | 1975 | Mississippian-Pennsylvanian (Visean-Bashkirian) | United Kingdom ( Scotland)
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One of the oldest and most basal members of the group (if it even counts as part of it), without vertebrae that were not fully embolomerous | 
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| Leptophractus | 1873 | Pennsylvanian (Westphalian D) | United States ( Ohio)
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Known from a skull found at the Linton Diamond Mine | |
| Neopteroplax | 1963 | Pennsylvanian | United States ( Ohio)
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One of the largest Carboniferous limbed vertebrates known from North America | _(Birmingham_Shale,_Upper_Pennsylvanian;_Bloomingdale,_Ohio,_USA)_1_(49761151626).jpg)
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| Palaeoherpeton | 1970 | Pennsylvanian (Westphalian A-B) | United Kingdom ( Scotland)
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An eogyrinid known as Palaeogyrinus from 1926 to 1970, until it was determined that this name was occupied by a genus of beetles | |
| 1914 | Mississippian-Pennsylvanian (Namurian) | United Kingdom ( Scotland)
|
Known from a femur, may have been a relative of Proterogyrinus | ||
| Pholiderpeton | 1869 | Pennsylvanian (Westphalian A-B) | United Kingdom ( England, Scotland)
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An eogyrinid similar to Eogyrinus which would take priority if the two were synonymized | 
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| Proterogyrinus | 1970 | Mississippian (Serpukhovian) | United States ( West Virginia), United Kingdom ( Scotland)
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An early member of the group possessing robust limbs but lacking certain adaptations of later members of the group | 
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| Pteroplax | 1868 | Pennsylvanian (Westphalian B) | United Kingdom ( England)
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Poorly known despite being among the first embolomeres to be described | 
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| Seroherpeton | 2020 | Late Permian (Wuchiapingian) |  China
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The youngest known embolomere | |
| Spondylerpeton | 1912 | Pennsylvanian | United States ( Illinois)
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A close relative of Cricotus known from vertebrae found at the Mazon Creek fossil beds |
References
- ↑ Panchen, A. L. (10 February 1972). "The skull and skeleton of Eogyrinus attheyi Watson (Amphibia: Labyrinthodontia)" (in en). Phil. Trans. R. Soc. Lond. B 263 (851): 279–326. doi:10.1098/rstb.1972.0002. ISSN 0080-4622. Bibcode: 1972RSPTB.263..279P.
- ↑ 2.0 2.1 Romer, Alfred Sherwood (11 January 1957). "The Appendicular Skeleton of the Permian Embolomerous Amphibian Archeria". Contributions from the Museum of Paleontology 13 (5): 105–159. https://deepblue.lib.umich.edu/bitstream/handle/2027.42/48305/ID145.pdf?sequence=2.
- ↑ Chen, Jianye; Liu, Jun (2020-12-01). "The youngest occurrence of embolomeres (Tetrapoda: Anthracosauria) from the Sunjiagou Formation (Lopingian, Permian) of North China" (in English). Fossil Record 23 (2): 205–213. doi:10.5194/fr-23-205-2020. ISSN 2193-0066. https://fr.copernicus.org/articles/23/205/2020/.
- ↑ Cope, E.D. (January 1884). "The Batrachia of the Permian Period of North America". The American Naturalist 18: 26–39. doi:10.1086/273563.
- ↑ Laurin, Michel (1998). "The importance of global parsimony and historical bias in understanding tetrapod evolution. Part I. Systematics, middle ear evolution and jaw suspension". Annales des Sciences Naturelles - Zoologie et Biologie Animale 19 (1): 1–42. doi:10.1016/S0003-4339(98)80132-9. https://www.academia.edu/1177174.
- ↑ Chen, Jianye; Liu, Jun (2020-12-01). "The youngest occurrence of embolomeres (Tetrapoda: Anthracosauria) from the Sunjiagou Formation (Lopingian, Permian) of North China" (in en). Fossil Record 23 (2): 205–213. doi:10.5194/fr-23-205-2020. ISSN 2193-0066. https://fr.copernicus.org/articles/23/205/2020/.
- ↑ Klembara, Jozef; Clack, Jennifer A.; Čerňanský, Andrej (2010-09-16). "The anatomy of palate of Chroniosaurus dongusensis (Chroniosuchia, Chroniosuchidae) from the Upper Permian of Russia" (in en). Palaeontology 53 (5): 1147–1153. doi:10.1111/j.1475-4983.2010.00999.x. ISSN 0031-0239.
- ↑ Carroll, Robert L. (2012-10-18). "The Importance of Recognizing Our Limited Knowledge of the Fossil Record in the Analysis of Phylogenetic Relationships among Early Tetrapods" (in en-US). Fieldiana Life and Earth Sciences 5: 5–16. doi:10.3158/2158-5520-5.1.5. ISSN 2158-5520.
- ↑ Sookias, Roland B.; Böhmer, Christine; Clack, Jennifer A. (2014-10-07). "Redescription and Phylogenetic Analysis of the Mandible of an Enigmatic Pennsylvanian (Late Carboniferous) Tetrapod from Nova Scotia, and the Lability of Meckelian Jaw Ossification" (in en). PLOS ONE 9 (10): e109717. doi:10.1371/journal.pone.0109717. ISSN 1932-6203. PMID 25290449. Bibcode: 2014PLoSO...9j9717S.
- ↑ Laurin, M.; Reisz, R.R. (1999). "A new study of Solenodonsaurus janenschi, and a reconsideration of amniote origins and stegocephalian evolution". Canadian Journal of Earth Sciences 36 (8): 1239–1255. doi:10.1139/e99-036. https://www.academia.edu/1177181.
- ↑ 11.0 11.1 Marcello Ruta, Michael I. Coates and Donald L. J. Quicke (2003). "Early tetrapod relationships revisited". Biological Reviews 78 (2): 251–345. doi:10.1017/S1464793102006103. PMID 12803423. http://pondside.uchicago.edu/oba/faculty/coates/5.RutCoaQuick2003.pdf.
- ↑ Clack, J. A. (July 2002). "An early tetrapod from 'Romer's Gap'" (in En). Nature 418 (6893): 72–76. doi:10.1038/nature00824. ISSN 0028-0836. PMID 12097908.
Wikidata ☰ Q136529 entry
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