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Sinoconodon
''Sinoconodon rigneyi'' is an ancient mammaliamorph or early mammal (depending on systematic approach) that appears in the fossil record of China in the Sinemurian stage of the Early Jurassic period, about 193 million years ago. While in many traits very similar to reptiles, it possessed a special, secondarily evolved jaw joint between the dentary and the squamosal bones, which had replaced the primitive reptilian one between the articular and quadrate bones, a trait commonly used to define mammals.
Although the animal is closely related to ''Morganucodon'', it is regarded as the most basal of the mammaliaforms. It differed substantially from the more mammalian ''Morganucodon'' in its dental and growth habits. Like the reptiles, it was polyphyodont, replacing many of its teeth throughout its lifetime, and it seems to have grown slowly but continuously until its death. ''Sinoconodon'' is thus less mammalian than early mammaliaforms like docodonts and morganucodonts.〔 Even the smallest known individuals had already begun the teething cycle of the front teeth, and combined with a poorly ossified jaw, it very probably did not suckle.〔(Mammals of the Mesozoic: The least mammal-like mammals )〕 The combination of reptilian and mammalian features makes it straddle the divide between the two classes anatomically and likely ecologically. There are simply no animals like it alive today.〔
==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
■ウィキペディアで「Sinoconodon」の詳細全文を読む
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