Chunerpeton
chianyiensis
Amphibia,
Order Caudata, Family Cryptobranchidae
Geological
Time: Middle/Late Jurassic
Size (25.4
mm = 1 inch): Fossil is 70 mm long (overall). Matrix: 80 mm by 90
mm
Fossil Site:
Daohu Valley, Ningcheng County, Neimenggu (Inner Mongolia), China
Fossil Code:
CF323
Price: Sold
Description:
The Daohuguo Beds on Inner Mongolia have yielded several Mesozoic
salamanders related to those extant today. This one is a member
of the Cryptobranchidae, the family to which the modern-day Asian
giant salamander Andrias, and the Hellbender Cryptobranchus of
the southern United States belong. Chunerpeton is the first Mesozoic
salamander from this family which was previously only known as
a fossil from the Paleocene. The fossil salamanders from these
deposits go a long way to answering questions about the evolution
of these remarkable amphibians. Phyletogentic analysis of the
Urodeles shows that Asia is the origin of the clade, leading
to the hypothesis that the basal salamanders radiated from the
region. Some salamanders demonstrate neoteny, or the capability
of reproducing while in what is apparently the larval state.
Note the soft tissue outlines preserved, and three sets of gill
structures, a telltale that this is not a larval form but a neotenic
example. Neoteny is not all that uncommon among modern-day salamanders(some
40 species in 9 different families demonstrate this strategy),
with the Mexican Salamander or Axolotl being a prime example.
This means that it retains its gills and fins, and it doesn't
develop the protruding eyes, eyelids and characteristics of other
adult salamanders. It grows much larger than a normal larval
salamander, and it reaches sexual maturity in this larval stage.
The independent occurrence of neoteny in both Mesozoic and recent
groups of salamanders makes parallel evolution of numerous morphological
features an enduring feature of their history. Few such examples
are ever available.
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