Ixalerpeton: Difference between revisions
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| fossil_range = [[Carnian]] |
| fossil_range = [[Carnian]]<br>~{{fossilrange|237|228}} |
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| image = Ixalerpeton models.jpg |
| image = Ixalerpeton models.jpg |
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| image_caption = Models |
| image_caption = Models |
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| genus = Ixalerpeton |
| genus = Ixalerpeton |
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| parent_authority = Cabreira et al. |
| parent_authority = Cabreira et al. 2016 |
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| species = polesinensis |
| species = polesinensis |
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| authority = Cabreira et al. |
| authority = Cabreira et al. 2016 |
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'''''Ixalerpeton''''' (meaning "leaping reptile") is a genus of small, bipedal [[dinosauromorpha|dinosauromorphs]] in the [[lagerpetidae|lagerpetid]] family, containing one species, '''''I. polesinensis'''''. It lived in the [[Late Triassic]] of [[Brazil]] alongside the [[sauropodomorpha|sauropodomorph]] [[dinosaur]] ''[[Buriolestes]]''.<ref name="cabreira2016">{{cite journal | first1 = S.F. | last1 = Cabreira | first2 = A.W.A. | last2 = Kellner | first3 = S. | last3 = Dias-da-Silva | first4 = L.R. | last4 = da Silva | first5 = M. | last5 = Bronzati | first6 = J.C. | last6 = de Almeida Marsola | first7 = R.T. | last7 = Müller | first8 = J. | last8 = de Souza Bittencourt | first9 = B.J. | last9 = Batista | first10 = T. | last10 = Raugust | first11 = R. | last11 = Carrilho | first12 = A. | last12 = Brodt | first13 = M.C. | last13 = Langer | title = A Unique Late Triassic Dinosauromorph Assemblage Reveals Dinosaur Ancestral Anatomy and Diet | journal = Current Biology | doi = 10.1016/j.cub.2016.09.040 | url = http://www.cell.com/current-biology/fulltext/S0960-9822(16)31124-1 | date = 2016 | volume=26 | pages=3090–3095 | pmid=27839975}}</ref> |
'''''Ixalerpeton''''' (meaning "leaping reptile") is a genus of small, bipedal [[dinosauromorpha|dinosauromorphs]] in the [[lagerpetidae|lagerpetid]] family, containing one species, '''''I. polesinensis'''''. It lived in the [[Late Triassic]] of [[Brazil]] alongside the [[sauropodomorpha|sauropodomorph]] [[dinosaur]] ''[[Buriolestes]]''.<ref name="cabreira2016">{{cite journal | first1 = S.F. | last1 = Cabreira | first2 = A.W.A. | last2 = Kellner | first3 = S. | last3 = Dias-da-Silva | first4 = L.R. | last4 = da Silva | first5 = M. | last5 = Bronzati | first6 = J.C. | last6 = de Almeida Marsola | first7 = R.T. | last7 = Müller | first8 = J. | last8 = de Souza Bittencourt | first9 = B.J. | last9 = Batista | first10 = T. | last10 = Raugust | first11 = R. | last11 = Carrilho | first12 = A. | last12 = Brodt | first13 = M.C. | last13 = Langer | title = A Unique Late Triassic Dinosauromorph Assemblage Reveals Dinosaur Ancestral Anatomy and Diet | journal = Current Biology | doi = 10.1016/j.cub.2016.09.040 | url = http://www.cell.com/current-biology/fulltext/S0960-9822(16)31124-1 | date = 2016 | volume=26 | pages=3090–3095 | pmid=27839975}}</ref> |
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==Description== |
== Description == |
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''Ixalerpeton'' was similar to other lagerpetids (namely ''[[Dromomeron]]'' and ''[[Lagerpeton]]'') in having long hindlimbs with well-developed muscle attachments on the [[femur]]; in particular, its [[fourth trochanter]] was quite large and formed a crest (which is unlike ''Dromomeron'').<ref name="cabreira2016"/> However, the last few [[vertebral column#regional vertebrae|dorsal vertebrae]] of ''Ixalerpeton'' do not have the forward-inclining [[vertebra#structure|neural spines]] of ''Lagerpeton'' (which were associated with the latter's hopping, or saltatory, lifestyle).<ref name="cabreira2016"/><ref name="lagerpeton1994">{{cite journal | first1 = P.C. | last1 = Sereno | first2 = A.B. | last2 = Arcucci | title = Dinosaurian precursors from the Middle Triassic of Argentina: ''Lagerpeton chanarensis'' | journal = Journal of Vertebrate Paleontology | date = 1994 | volume = 13 | issue = 4 | pages = 385–399 | doi = 10.1080/02724634.1994.10011522 | url = http://www.tandfonline.com/doi/abs/10.1080/02724634.1994.10011522}}</ref> In addition to the enlarged fourth trochanter, a suite of other traits differentiate ''Ixalerpeton'' from all previously-described lagerpetids; there is an antitrochanter on the [[ilium (bone)|ilium]]; the end of the shaft of the [[ischium]] is tall; there is no ambiens process on the [[pubis (bone)|pubis]]; the [[medial condyle of femur|medial condyle]] on the femur is relatively flat at the front end but sharply angled at the back end; and the back face of the top end of the tibia has a deep groove. |
''Ixalerpeton'' was similar to other lagerpetids (namely ''[[Dromomeron]]'' and ''[[Lagerpeton]]'') in having long hindlimbs with well-developed muscle attachments on the [[femur]]; in particular, its [[fourth trochanter]] was quite large and formed a crest (which is unlike ''Dromomeron'').<ref name="cabreira2016"/> However, the last few [[vertebral column#regional vertebrae|dorsal vertebrae]] of ''Ixalerpeton'' do not have the forward-inclining [[vertebra#structure|neural spines]] of ''Lagerpeton'' (which were associated with the latter's hopping, or saltatory, lifestyle).<ref name="cabreira2016"/><ref name="lagerpeton1994">{{cite journal | first1 = P.C. | last1 = Sereno | first2 = A.B. | last2 = Arcucci | title = Dinosaurian precursors from the Middle Triassic of Argentina: ''Lagerpeton chanarensis'' | journal = Journal of Vertebrate Paleontology | date = 1994 | volume = 13 | issue = 4 | pages = 385–399 | doi = 10.1080/02724634.1994.10011522 | url = http://www.tandfonline.com/doi/abs/10.1080/02724634.1994.10011522}}</ref> In addition to the enlarged fourth trochanter, a suite of other traits differentiate ''Ixalerpeton'' from all previously-described lagerpetids; there is an antitrochanter on the [[ilium (bone)|ilium]]; the end of the shaft of the [[ischium]] is tall; there is no ambiens process on the [[pubis (bone)|pubis]]; the [[medial condyle of femur|medial condyle]] on the femur is relatively flat at the front end but sharply angled at the back end; and the back face of the top end of the tibia has a deep groove. |
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The head and forelimbs found with ''Ixalerpeton'' are the first of these elements that have been found among lagerpetids.<ref name="physorg">{{cite news|url=http://phys.org/news/2016-11-dinosaurs-gradual-fossil-evidence.html|title=Dinosaurs' rise was 'more gradual,' new fossil evidence suggests|last=Cell Press|work=Phys.org|date=10 November 2016|accessdate=11 November 2016}}</ref> Unlike [[dinosauriformes|dinosauriforms]], the posttemporal fenestra at the back of the skull is large and unreduced; there is an extra bone, the postfrontal, bordering the eye socket; there is no supratemporal fossa, which is an indentation found on the [[frontal bone]] in dinosauriforms; and the [[glenoid cavity]] on the [[scapula]], where the scapula-[[humerus]] joint is located, faces slightly sideways instead of backwards. On the other hand, there is an anterior tympanic recess on the [[neurocranium|braincase]], and the deltopectoral crest on the humerus is long, both of which are common among basal dinosauromorphs.<ref name="cabreira2016"/> |
The head and forelimbs found with ''Ixalerpeton'' are the first of these elements that have been found among lagerpetids.<ref name="physorg">{{cite news|url=http://phys.org/news/2016-11-dinosaurs-gradual-fossil-evidence.html|title=Dinosaurs' rise was 'more gradual,' new fossil evidence suggests|last=Cell Press|work=Phys.org|date=10 November 2016|accessdate=11 November 2016}}</ref> Unlike [[dinosauriformes|dinosauriforms]], the posttemporal fenestra at the back of the skull is large and unreduced; there is an extra bone, the postfrontal, bordering the eye socket; there is no supratemporal fossa, which is an indentation found on the [[frontal bone]] in dinosauriforms; and the [[glenoid cavity]] on the [[scapula]], where the scapula-[[humerus]] joint is located, faces slightly sideways instead of backwards. On the other hand, there is an anterior tympanic recess on the [[neurocranium|braincase]], and the deltopectoral crest on the humerus is long, both of which are common among basal dinosauromorphs.<ref name="cabreira2016"/> |
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==Discovery and naming== |
== Discovery and naming == |
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The [[holotype]] specimen of ''Ixalerpeton'', numbered '''ULBRA-PVT059''', consists of parts from the skull, vertebral column, and all four limbs. The specimen comes from the [[Carnian]] [[Santa Maria Formation]] of [[Brazil]], and it was found alongside two individuals of ''[[Buriolestes]]'' as well as a set of femora belonging to second individual of ''Ixalerpeton''. The genus name of ''Ixalerpeton'' combines the Greek words ''ixalos'' ("leaping") and ''erpeton'' ("reptile"), and the species name ''polesinensis'' references the town of [[São João do Polêsine]], where the dig site is located.<ref name="cabreira2016"/> |
The [[holotype]] specimen of ''Ixalerpeton'', numbered '''ULBRA-PVT059''', consists of parts from the skull, vertebral column, and all four limbs. The specimen comes from the [[Carnian]] [[Santa Maria Formation]] of [[Brazil]], and it was found alongside two individuals of ''[[Buriolestes]]'' as well as a set of femora belonging to second individual of ''Ixalerpeton''. The genus name of ''Ixalerpeton'' combines the Greek words ''ixalos'' ("leaping") and ''erpeton'' ("reptile"), and the species name ''polesinensis'' references the town of [[São João do Polêsine]], where the dig site is located.<ref name="cabreira2016"/> |
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==Classification== |
== Classification == |
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A 2016 phylogenetic analysis found that ''Ixalerpeton'' was the closest relative of ''[[Dromomeron]]''. The phylogenetic tree recovered is partially reproduced below.<ref name="cabreira2016"/> |
A 2016 phylogenetic analysis found that ''Ixalerpeton'' was the closest relative of ''[[Dromomeron]]''. The phylogenetic tree recovered is partially reproduced below.<ref name="cabreira2016"/> |
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==Paleoecology== |
== Paleoecology == |
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Similar to the [[Ischigualasto Provincial Park|Ischigualasto]]<ref name="ischigualasto2013">{{cite journal | first1 = R.N. | last1 = Martínez | first2 = C. | last2 = Apaldetti | first3 = O.A. | last3 = Alcober | first4 = C.E. | last4 = Colombi | first5 = P.C. | last5 = Sereno | first6 = E. | last6 = Fernandez | first7 = P.S. | last7 = Malnis | first8 = G.A. | last8 = Correa | first9 = D. | last9 = Abelin | title = Vertebrate succession in the Ischigualasto Formation | journal = Journal of Vertebrate Paleontology | doi = 10.1080/02724634.2013.818546 | date = 2013 | volume = 32 | pages = 10–30 | issue = Supplement 1: ''Memoir 12: Basal sauropodomorphs and the vertebrate fossil record of the Ischigualasto Formation (Late Triassic: Carnian-Norian) of Argentina'' | url = http://www.tandfonline.com/doi/abs/10.1080/02724634.2013.818546?journalCode=ujvp20}}</ref> and [[Chinle Formation|Chinle]]<ref name="chinle2007">{{cite journal | first1 = R.B. | last1 = Irmis | first2 = S.J. | last2 = Nesbitt | first3 = K. | last3 = Padian | first4 = N.D. | last4 = Smith | first5 = A.H. | last5 = Turner | first6 = D. | last6 = Woody | first7 = A. | last7 = Downs | title = A Late Triassic Dinosauromorph Assemblage from New Mexico and the Rise of Dinosaurs | date = 2007 | journal = Science | volume = 317| issue = 5836 | pages = 358–361 | doi = 10.1126/science.1143325 | url = http://science.sciencemag.org/content/317/5836/358 | pmid=17641198}}</ref> Formations, the [[Santa Maria Formation]] preserves both ''Ixalerpeton'' (a non-dinosaur dinosauromorph) and ''[[Buriolestes]]'' (a dinosaur). This indicates that dinosaurs did not rapidly replace their dinosauromorph ancestors.<ref name="cabreira2016"/> |
Similar to the [[Ischigualasto Provincial Park|Ischigualasto]]<ref name="ischigualasto2013">{{cite journal | first1 = R.N. | last1 = Martínez | first2 = C. | last2 = Apaldetti | first3 = O.A. | last3 = Alcober | first4 = C.E. | last4 = Colombi | first5 = P.C. | last5 = Sereno | first6 = E. | last6 = Fernandez | first7 = P.S. | last7 = Malnis | first8 = G.A. | last8 = Correa | first9 = D. | last9 = Abelin | title = Vertebrate succession in the Ischigualasto Formation | journal = Journal of Vertebrate Paleontology | doi = 10.1080/02724634.2013.818546 | date = 2013 | volume = 32 | pages = 10–30 | issue = Supplement 1: ''Memoir 12: Basal sauropodomorphs and the vertebrate fossil record of the Ischigualasto Formation (Late Triassic: Carnian-Norian) of Argentina'' | url = http://www.tandfonline.com/doi/abs/10.1080/02724634.2013.818546?journalCode=ujvp20}}</ref> and [[Chinle Formation|Chinle]]<ref name="chinle2007">{{cite journal | first1 = R.B. | last1 = Irmis | first2 = S.J. | last2 = Nesbitt | first3 = K. | last3 = Padian | first4 = N.D. | last4 = Smith | first5 = A.H. | last5 = Turner | first6 = D. | last6 = Woody | first7 = A. | last7 = Downs | title = A Late Triassic Dinosauromorph Assemblage from New Mexico and the Rise of Dinosaurs | date = 2007 | journal = Science | volume = 317| issue = 5836 | pages = 358–361 | doi = 10.1126/science.1143325 | url = http://science.sciencemag.org/content/317/5836/358 | pmid=17641198}}</ref> Formations, the [[Santa Maria Formation]] preserves both ''Ixalerpeton'' (a non-dinosaur dinosauromorph) and ''[[Buriolestes]]'' (a dinosaur). This indicates that dinosaurs did not rapidly replace their dinosauromorph ancestors.<ref name="cabreira2016"/> |
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==References== |
== References == |
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{{reflist}} |
{{reflist}} |
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[[Category:Dinosauromorphs]] |
[[Category:Dinosauromorphs]] |
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[[Category:Late Triassic dinosauromorphs]] |
[[Category:Late Triassic dinosauromorphs]] |
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[[Category:Late Triassic reptiles of South America]] |
[[Category:Late Triassic reptiles of South America]] |
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[[Category:Santa Maria Formation]] |
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[[Category:Taxa named by Alexander Kellner]] |
[[Category:Taxa named by Alexander Kellner]] |
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Revision as of 04:23, 17 October 2017
Ixalerpeton Temporal range: Carnian ~ | |
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![]() | |
Models | |
Scientific classification ![]() | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Family: | †Lagerpetidae |
Genus: | †Ixalerpeton Cabreira et al. 2016 |
Species: | †I. polesinensis |
Binomial name | |
†Ixalerpeton polesinensis Cabreira et al. 2016 |
Ixalerpeton (meaning "leaping reptile") is a genus of small, bipedal dinosauromorphs in the lagerpetid family, containing one species, I. polesinensis. It lived in the Late Triassic of Brazil alongside the sauropodomorph dinosaur Buriolestes.[1]
Description
Ixalerpeton was similar to other lagerpetids (namely Dromomeron and Lagerpeton) in having long hindlimbs with well-developed muscle attachments on the femur; in particular, its fourth trochanter was quite large and formed a crest (which is unlike Dromomeron).[1] However, the last few dorsal vertebrae of Ixalerpeton do not have the forward-inclining neural spines of Lagerpeton (which were associated with the latter's hopping, or saltatory, lifestyle).[1][2] In addition to the enlarged fourth trochanter, a suite of other traits differentiate Ixalerpeton from all previously-described lagerpetids; there is an antitrochanter on the ilium; the end of the shaft of the ischium is tall; there is no ambiens process on the pubis; the medial condyle on the femur is relatively flat at the front end but sharply angled at the back end; and the back face of the top end of the tibia has a deep groove.
The head and forelimbs found with Ixalerpeton are the first of these elements that have been found among lagerpetids.[3] Unlike dinosauriforms, the posttemporal fenestra at the back of the skull is large and unreduced; there is an extra bone, the postfrontal, bordering the eye socket; there is no supratemporal fossa, which is an indentation found on the frontal bone in dinosauriforms; and the glenoid cavity on the scapula, where the scapula-humerus joint is located, faces slightly sideways instead of backwards. On the other hand, there is an anterior tympanic recess on the braincase, and the deltopectoral crest on the humerus is long, both of which are common among basal dinosauromorphs.[1]
Discovery and naming
The holotype specimen of Ixalerpeton, numbered ULBRA-PVT059, consists of parts from the skull, vertebral column, and all four limbs. The specimen comes from the Carnian Santa Maria Formation of Brazil, and it was found alongside two individuals of Buriolestes as well as a set of femora belonging to second individual of Ixalerpeton. The genus name of Ixalerpeton combines the Greek words ixalos ("leaping") and erpeton ("reptile"), and the species name polesinensis references the town of São João do Polêsine, where the dig site is located.[1]
Classification
A 2016 phylogenetic analysis found that Ixalerpeton was the closest relative of Dromomeron. The phylogenetic tree recovered is partially reproduced below.[1]
Paleoecology
Similar to the Ischigualasto[4] and Chinle[5] Formations, the Santa Maria Formation preserves both Ixalerpeton (a non-dinosaur dinosauromorph) and Buriolestes (a dinosaur). This indicates that dinosaurs did not rapidly replace their dinosauromorph ancestors.[1]
References
- ^ a b c d e f g Cabreira, S.F.; Kellner, A.W.A.; Dias-da-Silva, S.; da Silva, L.R.; Bronzati, M.; de Almeida Marsola, J.C.; Müller, R.T.; de Souza Bittencourt, J.; Batista, B.J.; Raugust, T.; Carrilho, R.; Brodt, A.; Langer, M.C. (2016). "A Unique Late Triassic Dinosauromorph Assemblage Reveals Dinosaur Ancestral Anatomy and Diet". Current Biology. 26: 3090–3095. doi:10.1016/j.cub.2016.09.040. PMID 27839975.
- ^ Sereno, P.C.; Arcucci, A.B. (1994). "Dinosaurian precursors from the Middle Triassic of Argentina: Lagerpeton chanarensis". Journal of Vertebrate Paleontology. 13 (4): 385–399. doi:10.1080/02724634.1994.10011522.
- ^ Cell Press (10 November 2016). "Dinosaurs' rise was 'more gradual,' new fossil evidence suggests". Phys.org. Retrieved 11 November 2016.
- ^ Martínez, R.N.; Apaldetti, C.; Alcober, O.A.; Colombi, C.E.; Sereno, P.C.; Fernandez, E.; Malnis, P.S.; Correa, G.A.; Abelin, D. (2013). "Vertebrate succession in the Ischigualasto Formation". Journal of Vertebrate Paleontology. 32 (Supplement 1: Memoir 12: Basal sauropodomorphs and the vertebrate fossil record of the Ischigualasto Formation (Late Triassic: Carnian-Norian) of Argentina): 10–30. doi:10.1080/02724634.2013.818546.
- ^ Irmis, R.B.; Nesbitt, S.J.; Padian, K.; Smith, N.D.; Turner, A.H.; Woody, D.; Downs, A. (2007). "A Late Triassic Dinosauromorph Assemblage from New Mexico and the Rise of Dinosaurs". Science. 317 (5836): 358–361. doi:10.1126/science.1143325. PMID 17641198.