Phosphatized univalves, recovered from the Lower Cambrian (approximate
ly 530 million years old) Qiongzhusi Formation in southern China, are
recognized as early instars belonging to bradoriid ostracodes whose la
ter instars are bivalved. The univalved form is the primitive larval c
haracter for shell-secreting crustaceans, although most post-Cambrian
ostracodes bypassed this developmental phase. The univalved-bivalved t
ransition during early ontogeny represents an important evolutionary e
vent in ostracodes, with implications for crustacean classification, a
nd implies that the ostracode ancestor achieved this bivalved capacity
before the appearance of mineralized skeletons during the ''Cambrian
explosion. ''