Formation of bone. Dermal, perichondral and endochondral modes should be distinguished from mineral deposition in cartilage.
A skull-roof bone formed by integration of frontal and parietal components, characteristic of frogs and some other vertebrates.
A skeletal element associated with the vertebral axis. Reduction of free ribs is part of the characteristic frog body organization.
bone deposited during replacement of a cartilaginous skeletal template. It should be distinguished from calcified cartilage and a superficial perichondral bone layer.
bone forming within dermal or related connective tissues rather than replacing a cartilaginous template. Large skull-roof bones and small surface odontodes are distinct anatomical organizations.
A dermal skeleton organized into relatively large plates or bones, contrasting with a covering dominated by small separate scales or odontodes.
The dorsal component of the pelvic girdle. Its anterior elongation is an important feature of the frog-lineage locomotor apparatus.
A vertebra anterior to the sacrum. Counts depend on identifying the sacral articulation, not just numbering visible centra.
A bone of the jaw suspension in many nonmammalian vertebrates; its mobility contributes to avian cranial kinesis.
Bone tissue associated with rapid deposition. Rapid growth alone does not uniquely establish sustained endothermy.
The principal proximal bone of the lower limb and the corresponding pelvic appendage in relevant comparisons.
One of the principal forearm bones, paired with the radius bone.
One of the two principal forearm bones; movement relative to the ulna contributes to forearm rotation.
The single proximal element of the upper limb and the corresponding pectoral appendage in relevant fossil comparisons.