Tomistominae

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Tomistominae
Temporal range:
Ma
False gharial, Tomistoma schlegelii
Scientific classification Edit this 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

crocodylians that includes one living species, the false gharial. Many more extinct species are known, extending the range of the subfamily back to the Eocene
epoch. In contrast to the false gharial, which is a freshwater species that lives only in southeast Asia, extinct tomistomines had a global distribution and lived in estuaries and along coastlines.

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

piscivory, or fish-eating. Despite the similarity with gharials, the shapes of bones in tomistomine skulls link them with crocodiles. For example, both tomistomines and crocodiles have thin postorbital bars behind the eye sockets and a large socket for the fifth maxillary tooth. The splenial
bone of the lower jaw is long and slender, forming a distinctive "V" shape not seen in gharials.

Evolutionary history

Skull of Kentisuchus toliapicus.

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

Obik Sea, which separated Europe from Asia, also impeded travel. Tomistomines were able to cross these areas, indicating that they had tolerance to salt water.[1]

Rhamphosuchus crassidens, a giant tomistomine from India.

Tomistomines crossed the Atlantic Ocean and spread into the Americas in the Oligocene, Miocene, and

neotropical tomistomine is Charactosuchus kuleri from Jamaica. A close relationship has been proposed between C. kuleri and D. zajsanicus from Belgium, suggesting that tomistomines migrated from Europe to the Americas through the De Geer land bridge connecting Norway to Greenland and the North American mainland or the Thule land bridge connecting Scotland, Iceland, Greenland, and the North American mainland. The genus Thecachampsa was present along the eastern coast of North America during the Oligocene, Miocene, and Pliocene.[1]

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

Arabia collided with the Eurasian continent in the Early Miocene. However, Asian Miocene tomistomines may also have descended from the Eocene tomistomines that were already present in eastern Asia. Tomistomines spread throughout the Indian subcontinent during this time. One species, Rhamphosuchus crassidens, was one of the largest crocodilians that ever lived, growing to an estimated 8 to 11 metres (26 to 36 ft). New species such as Toyotamaphimeia machikanensis were present in Japan in the Pleistocene. In southeast Asia however, there is little fossil evidence of the tomistomines that preceded the false gharial. Therefore, its relation with extinct species is unclear.[1]

Phylogeny

Tomistominae is

crocodiles
.

Hypotheses of tomistomine
phylogeny
Morphological
Crocodylia
 

Gavialidae

Alligatoridae

 
Crocodylidae
 

Crocodylinae

Tomistominae

Molecular
Crocodylia
 

Alligatoridae

 Gavialoidea 

Gavialis

Tomistominae

Crocodylidae

Below is a

Crocodylidae

Crocodylinae

Tomistominae

Xaymacachampsa

Megadontosuchus

Kentisuchus

Maroccosuchus

Dollosuchoides

Tomistoma cairense

Maomingosuchus

Tomistoma schlegelii False gharial

Gavialosuchus

Tomistoma lusitanicum

Paratomistoma

Tomistoma coppensi


Based on morphological studies of

gavialoids.[6] However, recent molecular studies using DNA sequencing have consistently indicated that the false gharial (Tomistoma) (and by inference other related extinct forms in Tomistominae) actually belong to Gavialoidea (and Gavialidae).[7][4][8][9][10][11][12]

Below is a

paraphyletic with respect to the gharial:[11]

Longirostres

Crocodylidae

Gavialoidea
Gavialidae
(Gavialinae?)

Gavialis gangeticus Gharial

Gavialis bengawanicus

Gavialis browni

Gryposuchus colombianus

Ikanogavialis

Gryposuchus pachakamue

Piscogavialis

Harpacochampsa

(
stem-based group
)
(Tomistominae?)

Tomistoma lusitanicum

Tomistoma schlegelii False gharial

(
stem-based group
)
(crown group)

Tomistoma cairense

Dollosuchoides

Kentisuchus

(
stem-based group
)
Traditional Tomistominae
(crown group)

References

  1. ^ 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.
  2. .
  3. (PDF) on 2015-04-02. Retrieved 2011-06-25.
  4. ^ .
  5. .
  6. ^ 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.
  7. PMID 12775527. Archived from the original
    (PDF) on 2022-10-09. Retrieved 2021-06-30.
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  11. ^ .
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