Sphenosuchia | |
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Life restoration ofHesperosuchus agilis | |
Scientific classification![]() | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Reptilia |
Clade: | Archosauria |
Clade: | Pseudosuchia |
Clade: | Crocodylomorpha |
Informal group: | †Sphenosuchia von Huene, 1942 |
Genera | |
Synonyms | |
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Sphenosuchia is asuborder ofbasalcrocodylomorphs that first appeared in theTriassic and occurred into theMiddle Jurassic. Most were small, gracile animals with an erect limb posture. They are now thought to be ancestral tocrocodyliforms, a group which includes all livingcrocodilians.
The earliest known members of the group (i.e.Hesperosuchus) are earlyNorian in age, found in the Blue Mesa Member of theChinle Formation. Only one sphenosuchian is currently known from the Middle Jurassic,Junggarsuchus, from theJunggar Basin (Shishugou Formation) of China during either theBathonian or theCallovian (~165 Ma) age,[1] and theHallopodidae are known from the Late Jurassic of North America.[2]
Themonophyly of the group is debated, although severalsynapomorphies characterize the clade, including extremely slender limbs, a compactcarpus and an elongatecoracoid process.
In 2002, Clark and Sues found a possible sphenosuchian clade ofDibothrosuchus,Sphenosuchus, and possiblyHesperosuchus andSaltoposuchus, with several other genera in unresolved positions (Kayentasuchus,Litargosuchus,Pseudhesperosuchus, andTerrestrisuchus).[3] More recently, however, Clarket al. (2004) argued for the paraphyly of the group, contending that morphological characters were secondarily lost in more highly derived crocodylomorphs.[1] Further analysis and study is required before the group's monophyly is resolved with certainty — a perfect phylogenetic analysis is, at present, impossible due to a paucity of fossil remains demonstrating phylogenetically informative characters.
Below is acladogram modified from Nesbitt (2011).[4] Sphenosuchians are marked by the green bracket.
Sphenosuchians |
Genus | Status | Age | Location | Unit | Notes | Images |
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Valid | Early Jurassic | ![]() | Lower Lufeng Series | ![]() | ||
Valid | Late Triassic | ![]() | Newark Supergroup | |||
Valid | Late Triassic (Carnian) | ![]() | Schilfsandstein Formation | A possible sphenosuchian;[5] alternatively, it could be anerpetosuchid.[6] | ![]() | |
Valid | Late Triassic (Carnian) | ![]() | Chinle Formation | |||
Valid | Middle Jurassic | ![]() | Shishugou Formation | ![]() | ||
Valid | Early Jurassic (Sinemurian -Pliensbachian) | ![]() | Kayenta Formation | |||
Valid | Early Jurassic | ![]() | Elliot Formation | ![]() | ||
Nomen dubium | Late Triassic | ![]() | Dockum Group | An indeterminate sphenosuchian known only from undiagnostic vertebrae[7] | ||
Valid | Early Jurassic | ![]() | Lower Lufeng Series | |||
Valid | Late Triassic (Norian) | ![]() | Los Colorados Formation | |||
Valid | Late Triassic | ![]() | Redonda Formation | |||
Valid | Late Triassic (Norian) | ![]() | Löwenstein Formation | ![]() | ||
Valid | Early Jurassic | ![]() | Elliot Formation | |||
Valid. | Late Triassic | ![]() | ![]() | |||
Valid | Late Triassic | ![]() | Ischigualasto Formation |