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{{Short description|Extinct genus of reptiles}}
{{Automatic taxobox
{{Automatic taxobox
| taxon = Culebrasuchus
| fossil_range = [[Miocene]]
| fossil_range = [[Miocene|Early-Mid Miocene]] ([[Hemingfordian North American Stage|Hemingfordian]])<br />~{{fossil range|20.6|16.3}}
| authority = [[Alexander K. Hastings|Hastings]] ''et al.'', [[2013 in paleontology|2013]]
| authority = [[Alexander K. Hastings|Hastings]] ''et al.'', [[2013 in paleontology|2013]]
| type_species = {{extinct}}'''''Culebrasuchus mesoamericanus'''''
| type_species = {{extinct}}'''''Culebrasuchus mesoamericanus'''''
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}}
}}


'''''Culebrasuchus''''' is an [[extinct]] [[genus]] of [[caimanine|caiman]] (a type of [[crocodilian]]) known from the early–middle [[Miocene]] of the [[Panama Canal Zone]] of [[Panama]]. It contains a single [[species]], '''''Culebrasuchus mesoamericanus''''', which is based on a single [[holotype]] skull and three neck [[vertebrae]]. ''Culebrasuchus'' is thought to be the most basal member of Caimaninae, meaning that it represents the earliest radiation of caimans in the Americas. The ancestor of ''Culebrasuchus'' likely lived farther north, perhaps in what is now southern Mexico, because before the Miocene most of Panama was underwater. The movement of ''Culebrasuchus'' into the Panama Canal Zone was an early part of the [[Great American Interchange]] in which animals dispersed between North and South America across the newly formed Isthmus of Panama (although during the early-middle Miocene it had not yet formed, with 20 km of ocean still separating the continents).<ref name=PanamaCrocs>{{Cite doi|10.1080/02724634.2012.713814}}</ref>
'''''Culebrasuchus''''' is an [[extinct]], [[monotypic taxon|monotypic]] [[genus]] of [[caimanine|caiman]] [[alligatoridae|alligatorid]] known from the [[Miocene|Early to Middle Miocene]] ([[Hemingfordian North American Stage|Hemingfordian]]) of the [[Panama Canal Zone]] of [[Panama]]. It contains a single [[species]], '''''Culebrasuchus mesoamericanus'''''.<ref name=PanamaCrocs>{{Cite journal | last1 = Hastings | first1 = A. K. | last2 = Bloch | first2 = J. I. | last3 = Jaramillo | first3 = C. A. | last4 = Rincon | first4 = A. F. | last5 = MacFadden | first5 = B. J. | title = Systematics and biogeography of crocodylians from the Miocene of Panama | doi = 10.1080/02724634.2012.713814 | journal = Journal of Vertebrate Paleontology | volume = 33 | issue = 2 | pages = 239 | year = 2013 | bibcode = 2013JVPal..33..239H | s2cid = 83972694 | doi-access = free }}</ref>


== Discovery ==
Features that ''Culebrasuchus'' shares in common with other caimanines include nostrils that open upward (rather than slightly forward, as in alligatorines), and bones that do not overlap the edges of two openings in the [[skull table]] called [[Temporal fenestra|supratemporal fenestrae]]. Like living caimanines, ''Culebrasuchus ''has blunter teeth at the back of the jaw, and the teeth in the upper jaw completely overly the teeth in the lower jaw when the mouth is closed. Features in ''Culebrasuchus ''that are not found in other caimanines include the lack of ridges above the eye sockets and the large size of a hole in the lower jaw called the external mandibular fenestra. These features may be [[plesiomorphic]] ("primitive") for alligatorids. ''Culebrasuchus ''also has a straighter lower jaw than most other alligatorids, it lacks the ridges on the [[frontal bone]] between the eye sockets that are common among crocodylians, and the fourth tooth of the maxilla (rather than third, as in almost all other alligatorids) is the largest in the upper jaw.<ref name="PanamaCrocs" />
''Culebrasuchus'' was first described and named by Alexander K. Hastings, Jonathan I. Bloch, Carlos A. Jaramillo, Aldo F. Rincona and Bruce J. Macfadden in [[2013 in paleontology|2013]] based on a single [[holotype]] skull and three neck [[vertebrae]] from the [[Culebra Formation]]. ''Culebrasuchus'' is thought to be the most [[Basal (phylogenetics)|basal]] member of [[Caimaninae]], meaning that it represents the earliest radiation of caimans in the Americas. The ancestor of ''Culebrasuchus'' likely lived farther north, perhaps in what is now southern Mexico, because before the [[Miocene]] most of Panama was underwater. The movement of ''Culebrasuchus'' into the Panama Canal Zone was an early part of the [[Great American Interchange]] in which animals dispersed between North and South America across the newly formed [[Isthmus]] of Panama (although during the Early Miocene it had not yet formed, with 20&nbsp;km of ocean still separating the continents). However, ''Culebrasuchus'' was not the earliest caimanine; ''[[Orthogenysuchus]]'' and ''[[Tsoabichi]]'' are known from the [[Eocene]] of North America and ''[[Eocaiman]]'' is known from the Eocene of South America, indicating that caimanines were dispersing between the continents across large expanses of ocean long before the isthmus formed.<ref name=PanamaCrocs/>


==References==
== Description ==
Like many living caimans, ''Culebrasuchus'' was small in size. Other caimans that lived during the same time in South America (including those in the genera ''[[Mourasuchus]]'' and ''[[Purussaurus]]'') were much larger than ''Culebrasuchus''. Features that ''Culebrasuchus'' shares in common with other caimanines include nostrils that open upward (rather than slightly forward, as in alligatorines), and bones that do not overlap the edges of two openings in the [[skull table]] called [[Temporal fenestra|supratemporal fenestrae]]. Like living caimanines, ''Culebrasuchus ''has blunter teeth at the back of the jaw, and the teeth in the upper jaw completely overly the teeth in the lower jaw when the mouth is closed. Features in ''Culebrasuchus ''that are not found in other caimanines include the lack of ridges above the eye sockets and the large size of a hole in the lower jaw called the external mandibular fenestra. These features may be [[plesiomorphic]] ("primitive") for alligatorids. ''Culebrasuchus'' also has a straighter lower jaw than most other alligatorids, it lacks the ridges on the [[frontal bone]] between the eye sockets that are common among crocodylians, and the fourth tooth of the maxilla (rather than third, as in almost all other alligatorids) is the largest in the upper jaw.<ref name=PanamaCrocs/>
{{reflist}}


== Classification ==
{{portal|Paleontology}}
The 2013 study describing and naming ''Culebrasuchus'' placed it as the most [[Basal (phylogenetics)|basal]] member of the [[Alligatoridae]] [[subfamily]] [[Caimanine]],<ref name=PanamaCrocs/> and was confirmed by later studies.<ref name="Massonne2019">{{cite journal |author1=Tobias Massonne |author2=Davit Vasilyan |author3=Márton Rabi |author4=Madelaine Böhme |year=2019 |title=A new alligatoroid from the Eocene of Vietnam highlights an extinct Asian clade independent from extant ''Alligator sinensis'' |journal=[[PeerJ]] |volume=7 |pages=e7562 |doi=10.7717/peerj.7562 |pmid=31720094 |pmc=6839522 |doi-access=free}}</ref><ref name="Cossette2020">{{Cite journal|author1=Adam P. Cossette |author2=Christopher A. Brochu |year=2020 |title=A systematic review of the giant alligatoroid ''Deinosuchus'' from the Campanian of North America and its implications for the relationships at the root of Crocodylia |journal=[[Journal of Vertebrate Paleontology]] |volume=40 |pages=e1767638 |doi=10.1080/02724634.2020.1767638 |bibcode=2020JVPal..40E7638C |doi-access=free}}</ref>

The below [[cladogram]] is from the initial 2013 study:<ref name=PanamaCrocs/>
{{clade| style=font-size:85%;line-height:85%
|1={{clade
|1={{extinct}}''[[Stangerochampsa mccabei]]''
|2={{clade
|1={{extinct}}''[[Brachychampsa montana]]''
|2={{extinct}}''[[Brachychampsa sealeyi]]''}}
|label3=&nbsp;'''[[Alligatoridae]]'''&nbsp;
|3={{clade
|1='''[[Alligatorinae]]'''
|label2=&nbsp;'''[[Caimaninae]]'''&nbsp;
|2={{clade
|1={{extinct}}'''''Culebrasuchus mesoamericanus'''''
|2={{clade
|1={{extinct}}''[[Eocaiman cavernensis]]''
|2={{clade
|1={{extinct}}''[[Tsoabichi greenriverensis]]''
|label2=[[crown group]] [[caimans]]
|2={{clade
|1={{clade
|1=''Paleosuchus palpebrosus'' [[Cuvier's dwarf caiman]]
|2=''Paleosuchus trigonatus'' [[Smooth-fronted caiman]] }}
|2={{clade
|1={{clade
|1={{extinct}}''[[Centenariosuchus gilmorei]]''
|2={{clade
|1={{extinct}}''[[Purussaurus neivensis]]''
|2={{clade
|1={{extinct}}''[[Mourasuchus]]'' spp.
|2={{extinct}}''[[Orthogenysuchus olseni]]''}} }} }}
|2={{clade
|1={{clade
|1=''Caiman crocodilus'' [[Spectacled caiman]]
|2=''Caiman yacare'' [[Yacare caiman]] }}
|2={{clade
|1=''Caiman latirostris'' [[Broad-snouted caiman]]
|2={{extinct}}''[[Caiman lutescens]]''
|3={{clade
|1={{extinct}}''[[Melanosuchus fisheri]]''
|2=''Melanosuchus niger'' [[Black caiman]] }} }} }} }} }} }} }} }} }} }} }}

Alternatively, a 2018 study by Bona ''et al.'' noted that ''Culebrasuchus'' was enigmatic and difficult to interpret, and instead proposed it to be a member of [[Alligatorinae]], closely related to the living [[American Alligator]] and [[Chinese Alligator]], as shown in the cladogram below:<ref name="Bona2018">{{Cite journal |author1=Paula Bona |author2=Martín D. Ezcurra |author3=Francisco Barrios |author4=María V. Fernandez Blanco |year=2018 |title=A new Palaeocene crocodylian from southern Argentina sheds light on the early history of caimanines |journal=[[Proceedings of the Royal Society B: Biological Sciences]] |volume=285 |issue=1885 |pages=20180843 |doi=10.1098/rspb.2018.0843 |pmid=30135152 |pmc=6125902 |doi-access=free}}</ref>
{{clade| style=font-size:85%;line-height:85%
|label1='''[[Alligatoridae]]'''
|1={{clade
|1='''[[Caimaninae]]'''
|label2='''[[Alligatorinae]]'''
|2={{clade
|1=''[[Ceratosuchus burdoshi]]''{{extinct}}
|2=''[[Allognathosuchus polyodon]]''{{extinct}}
|3=''[[Allognathosuchus wartheni]]''{{extinct}}
|4=''[[Navajosuchus mooki]]''{{extinct}}
|5=''[[Arambourgia gaudryi]]''{{extinct}}
|6={{clade
|1=''[[Procaimanoidea kayi]]''{{extinct}}
|2=''[[Procaimanoidea utahensis]]''{{extinct}} }}
|7={{clade
|1=''[[Wannaganosuchus brachymanus]]''{{extinct}}
|2={{clade
|1=''[[Alligator prenasalis]]''{{extinct}}
|2={{clade
|1=''[[Alligator mcgrewi]]''{{extinct}}
|2={{clade
|1=''[[Alligator olseni]]''{{extinct}}
|2={{clade
|1=''Alligator sinensis'' [[Chinese alligator]]
|2={{clade
|1='''''Culebrasuchus mesoamericanus'''''{{extinct}}
|2={{clade
|1=''Alligator mississippiensis'' [[American alligator]]
|2=''[[Alligator mefferdi]]''{{extinct}}
|3=''[[Alligator thomsoni]]''{{extinct}} }} }} }} }} }} }} }} }} }} }}

== See also ==
{{Portal|Paleontology}}
* ''[[Centenariosuchus]]''
* ''[[Purussaurus]]''

== References ==
{{Reflist}}


{{Extinct Crocodilia|A.}}
{{Extinct Crocodilia|A.}}
{{Taxonbar|from=Q6424491}}


[[Category:Alligatoridae]]
[[Category:Prehistoric pseudosuchian genera]]
[[Category:Burdigalian life]]
[[Category:Miocene reptiles of North America]]
[[Category:Hemingfordian]]
[[Category:Neogene Panama]]
[[Category:Fossils of Panama]]
[[Category:Fossil taxa described in 2013]]
[[Category:Fossil taxa described in 2013]]

Revision as of 08:53, 1 June 2023

Culebrasuchus
Temporal range: Early-Mid Miocene (Hemingfordian)
~20.6–16.3 Ma
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauromorpha
Clade: Archosauriformes
Order: Crocodilia
Family: Alligatoridae
Subfamily: Caimaninae
Genus: Culebrasuchus
Hastings et al., 2013
Type species
Culebrasuchus mesoamericanus
Hastings et al., 2013

Culebrasuchus is an extinct, monotypic genus of caiman alligatorid known from the Early to Middle Miocene (Hemingfordian) of the Panama Canal Zone of Panama. It contains a single species, Culebrasuchus mesoamericanus.[1]

Discovery

Culebrasuchus was first described and named by Alexander K. Hastings, Jonathan I. Bloch, Carlos A. Jaramillo, Aldo F. Rincona and Bruce J. Macfadden in 2013 based on a single holotype skull and three neck vertebrae from the Culebra Formation. Culebrasuchus is thought to be the most basal member of Caimaninae, meaning that it represents the earliest radiation of caimans in the Americas. The ancestor of Culebrasuchus likely lived farther north, perhaps in what is now southern Mexico, because before the Miocene most of Panama was underwater. The movement of Culebrasuchus into the Panama Canal Zone was an early part of the Great American Interchange in which animals dispersed between North and South America across the newly formed Isthmus of Panama (although during the Early Miocene it had not yet formed, with 20 km of ocean still separating the continents). However, Culebrasuchus was not the earliest caimanine; Orthogenysuchus and Tsoabichi are known from the Eocene of North America and Eocaiman is known from the Eocene of South America, indicating that caimanines were dispersing between the continents across large expanses of ocean long before the isthmus formed.[1]

Description

Like many living caimans, Culebrasuchus was small in size. Other caimans that lived during the same time in South America (including those in the genera Mourasuchus and Purussaurus) were much larger than Culebrasuchus. Features that Culebrasuchus shares in common with other caimanines include nostrils that open upward (rather than slightly forward, as in alligatorines), and bones that do not overlap the edges of two openings in the skull table called supratemporal fenestrae. Like living caimanines, Culebrasuchus has blunter teeth at the back of the jaw, and the teeth in the upper jaw completely overly the teeth in the lower jaw when the mouth is closed. Features in Culebrasuchus that are not found in other caimanines include the lack of ridges above the eye sockets and the large size of a hole in the lower jaw called the external mandibular fenestra. These features may be plesiomorphic ("primitive") for alligatorids. Culebrasuchus also has a straighter lower jaw than most other alligatorids, it lacks the ridges on the frontal bone between the eye sockets that are common among crocodylians, and the fourth tooth of the maxilla (rather than third, as in almost all other alligatorids) is the largest in the upper jaw.[1]

Classification

The 2013 study describing and naming Culebrasuchus placed it as the most basal member of the Alligatoridae subfamily Caimanine,[1] and was confirmed by later studies.[2][3]

The below cladogram is from the initial 2013 study:[1]

Alternatively, a 2018 study by Bona et al. noted that Culebrasuchus was enigmatic and difficult to interpret, and instead proposed it to be a member of Alligatorinae, closely related to the living American Alligator and Chinese Alligator, as shown in the cladogram below:[4]

See also

References

  1. ^ a b c d e Hastings, A. K.; Bloch, J. I.; Jaramillo, C. A.; Rincon, A. F.; MacFadden, B. J. (2013). "Systematics and biogeography of crocodylians from the Miocene of Panama". Journal of Vertebrate Paleontology. 33 (2): 239. Bibcode:2013JVPal..33..239H. doi:10.1080/02724634.2012.713814. S2CID 83972694.
  2. ^ Tobias Massonne; Davit Vasilyan; Márton Rabi; Madelaine Böhme (2019). "A new alligatoroid from the Eocene of Vietnam highlights an extinct Asian clade independent from extant Alligator sinensis". PeerJ. 7: e7562. doi:10.7717/peerj.7562. PMC 6839522. PMID 31720094.
  3. ^ Adam P. Cossette; Christopher A. Brochu (2020). "A systematic review of the giant alligatoroid Deinosuchus from the Campanian of North America and its implications for the relationships at the root of Crocodylia". Journal of Vertebrate Paleontology. 40: e1767638. Bibcode:2020JVPal..40E7638C. doi:10.1080/02724634.2020.1767638.
  4. ^ Paula Bona; Martín D. Ezcurra; Francisco Barrios; María V. Fernandez Blanco (2018). "A new Palaeocene crocodylian from southern Argentina sheds light on the early history of caimanines". Proceedings of the Royal Society B: Biological Sciences. 285 (1885): 20180843. doi:10.1098/rspb.2018.0843. PMC 6125902. PMID 30135152.