A phosphatized Middle Cambrian (similar to 510 million years ago) faun
a from Duyun, southern China, has yielded fossil embryos that may be o
f arthropod affinity and could belong to the co-occurring eodiscid tri
lobite Pagetia sp. The shell was most likely flexible and possessed at
least two thin layers. Four embryos reveal blastomeres, and two embry
onic stages are represented. These embryos demonstrate that the basic
paradigm for the growth of the invertebrate embryo has not changed in
more than half a billion years.