Tomistominae
Tomistominae | |
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False gharial, Tomistoma schlegelii | |
Scientific classification (disputed) | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Reptilia |
Clade: | Archosauromorpha |
Clade: | Archosauriformes |
Order: | Crocodilia |
Clade: | Longirostres |
Superfamily: | Gavialoidea |
Family: | Gavialidae |
Subfamily: | Tomistominae Kälin, 1955 |
Genera | |
Tomistominae is a
The classification of tomistomines among Crocodylia has been in flux; while traditionally thought to be within Crocodyloidea, molecular evidence indicates that they are more closely related to true gharials as members of Gavialoidea.
Description
Tomistomines have narrow or longirostrine snouts like gharials. The living false gharial lives in fresh water and uses its long snout and sharp teeth to catch fish, although true gharials are more adapted toward
Evolutionary history
Tomistomines first appeared in the Eocene in Europe and North Africa. The oldest known tomistomine is Kentisuchus spenceri from England, although a possible tomistomine fossil from the Paleocene of Spain is even older.[1] Other early tomistomines include Maroccosuchus zennaroi from Morocco and Dollosuchus dixoni from Belgium. These early tomistomines inhabited the Tethys Ocean, which covered much of Europe and North Africa during the Paleogene. Several early tomistomines are found in coastal marine deposits, suggesting that they lived along the shoreline or in estuaries. Extinct gavialoids are also thought to have been coastal animals. The marine lifestyles of these early forms likely allowed tomistomines to spread around the Tethys, forming a northern population in Europe and a southern in North Africa.[1]
Later in the Eocene and
Tomistomines crossed the Atlantic Ocean and spread into the Americas in the Oligocene, Miocene, and
Tomistomines disappeared from Europe during the Oligocene but returned by the end of the epoch. They diversified and became common in the middle Miocene. One tomistomine, Tomistoma coppensi, is known from the late Miocene of Uganda. The appearance of tomistomines in central Africa is unusual because there is little evidence of late Miocene species in North Africa, an area where they must have traveled through from Europe.[1]
Tomistomines may have traveled from Africa into Asia when
Phylogeny
Tomistominae is
Hypotheses of tomistomine
phylogeny | |||||||||||||||||||||||
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Below is a
Crocodylidae
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Based on morphological studies of
Below is a
Longirostres |
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Traditional Tomistominae | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
(crown group) |
References
- ^ a b c d e f Piras, P.; Delfino, M.; Del Favero, L.; Kotsakis, T. (2007). "Phylogenetic position of the crocodylian Megadontosuchus arduini and tomistomine palaeobiogeography" (PDF). Acta Palaeontologica Polonica. 52 (2): 315–328.
- doi:10.1139/E09-036.
- doi:10.1146/annurev.earth.31.100901.141308. Archived from the original(PDF) on 2015-04-02. Retrieved 2011-06-25.
- ^ PMID 12775528.
- ISSN 0031-0182.
- ^ Brochu, C.A.; Gingerich, P.D. (2000). "New tomistomine crocodylian from the Middle Eocene (Bartonian) of Wadi Hitan, Fayum Province, Egypt". University of Michigan Contributions from the Museum of Paleontology. 30 (10): 251–268.
- PMID 12775527. Archived from the original(PDF) on 2022-10-09. Retrieved 2021-06-30.
- PMID 17433721.
- PMID 18372192.
- PMID 22431965.
- ^ PMID 30051855.
- PMID 33907305.