Myllokunmingia is a genus of basal chordate from the Lower Cambrian Maotianshan shales of China 518 mya and is thought to be a vertebrate, although this is not conclusively supported. The type species M. fengjiaoa is 28 mm long and 6 mm high. It is among the oldest possible craniates, found in the lower Cambrian Chengjiang (518 million years ago). It appears to have a skull and skeletal structures made of cartilage. There is no sign of biomineralization of the skeletal elements. The holotype was found in the Yuanshan member of the Qiongzhusi Formation in the Eoredlichia Zone near Haikou at Ercaicun, Kunming City, Yunnan, China. Some researchers have considered the other primitive chordate Haikouichthys to be synonymous with this taxon, but subsequent studies led by the British paleontologist Simon Conway Morris identified both genera to be distinct, separate taxa on the basis of different gill arrangement, the absence of branchial rays in Myllokunmingia and the myomeres having a more acute shape in Haikouichthys.
The animal has a distinct head and trunk with a forward sail-like (1.5 mm) dorsal fin and a ventral finfold (probably paired) further back. The maximum height of M. fengjiaoa is at 6 mm. The maximum height point is located around 11 mm from the anterior. The head has five or six gill pouches with hemibranchs. In the trunk there are 25 segments (myomeres) with rearward-facing chevrons. There is a notochord, a pharynx and a digestive tract that may run all the way to the rear tip of the animal. The mouth cannot be clearly identified. There may be a pericardial cavity. There are no fin radials on M. fengjiaoa. There is only one specimen, which has the tip of the tail buried in sediment.
