Cyamodus (pron.: SIE-ah-MO-dus) is a genus of known from several species described from Middle-Late Triassic of Europe and China. The genus was described by Christian Erich Hermann von Meyer in 1863, based on specimens found in Germany. Like some other placodonts, Cyamodus has an armoured carapace composed of irregular hexagonal plates, with the mouth containing a small number of large, rounded teeth that were likely involved in crushing hard shelled organisms (durophagy).
Initially considered to be an ancestral turtle due to its testudine-like head and large, bifurcated carapace. However further investigation resulted in its reclassification as a placodont, and it is closely related to other turtle-like reptiles of the Triassic period such as Henodus and Psephoderma. Similar to these other placodonts, Cyamodus lived hovering close to the sea floor, vacuuming up various shellfish, and crushing them between its blunt teeth.
Historically, the first Cyamodus remains were found in Upper Muschelkalk shallow marine limestones at near Bayreuth in Bavaria (Germany). They included the incomplete holotype skulls of Cyamodus muensteri and Cyamodus rostatus, which along with all other placodont remains recovered from the six quarries on the Lainecker Range in northern Bavaria were originally considered to have been derived from fish. The earliest Cyamodus skull was later restored by Muenster, with the addition of four teeth that had not been present in the original skull, and was named Placodus muensteri.
Further placodont remains were found by Muenster, who collected many placodont cranial remains in the Bindlach and Lainecker Range quarries. All placodont remains from those sites were then revised as being of reptilian origin by Owen (1858). A complete Cyamodus skeleton, including its skull, is known for C. hildegardis, which was found outside the Germanic Basin in the northern Tethys in Switzerland. Middle Triassic sauropterygian placodonts have become increasingly important for developing new ideas to the evolutionary history of their relatives, the turtles, whereas modern analyses place placodonts not as their ancestors using morphological cladistic analyses based on the bone osteology. The study of these placodonts contributes to our understanding of the Germanic Basin and the reptile distributions.
An intriguing placodont that appears to be intermediate between Cyamodus and the placochelyids, Protenodontosaurus italicus, was described by Giovanni Pinna in 1990.
Distinct from Paraplacodus, the skull of Cyamodus had a shorter rostrum, a smaller orbit and a larger upper temporal fenestra that was rimmed by ossifications. The teeth were flat discs, only one tooth appeared on each premaxilla and only two teeth appeared on each maxilla, with the largest teeth on the pterygoid bone. The quadratojugal joined the squamosal and sealed up the lateral temporal fenestra from the ancestral species ( Paraplacodus).
The carapace of C. hildegardis has a series of similar-sized, enlarged lateral armor plates is rounder and less laterally expanded than was hypothesized. The separate pelvic shield, also carrying a smaller set of lateral armor plates that decrease in size with an anterior/posterior gradient covering mainly the pelvic girdle and the base of the tail. The short tail is armored by four series of armor plates that also show an anterior/posterior gradient of size reduction equivalent to the size reduction of the caudal vertebrae. Until further fossils are recovered, the internal organisation of dermal plates within the two armor shields of C. hildegardis remains little known.
Cyamodus did not have any dorsal spines, although it did have a wing-like elongated flattened lateral spine that served to brace the overlying subdermal carapace. Presumably, the dorsal spines disappeared to provide a closer and better braced association between the vertebrae and the carapace.
It has also been noted that juvenile specimens of Cyamodus have an extra tooth on the roof of their mouth, compared to adult specimens. This suggests that Cyamodus reduced the number of teeth as they grew to maturity. However, this could be due to a difference between species of Cyamodus.
C. hildegardis from the Besano Formation (Middle Triassic) of the Alpine area of Switzerland and northern Italy has been reconstructed with a broad, laterally expanded main armor (carapace) and a separate smaller pelvic shield, giving it a sprawling appearance. A reexamination of the postcranial dermal armor and endoskeletal elements of the three best preserved articulated specimens of the species has led to new interpretations of the dermal armor and underlying postcranial bones, as well as a new life reconstruction.
Placodonts are typically considered to be durophagous (adapted to crushing hard-shelled organisms). C.G. Diedrich has suggested that Cyamodus and other placodonts were algae-grazers. However, this interpretation has been criticized by Torsten M. Scheyer and other researchers, and many subsequent studies about placodonts have rejected Deidrich's interpretation, and the consensus that placodonts with the exception of Henodus were Durophagy still continues to be strongly supported.
Description
Paleobiology
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