Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, China; Function Laboratory of Marine Mineral Resources, Qingdao National Laboratory for Marine Science & Technology, Qingdao, China
Université de Lyon, Université Claude Bernard Lyon 1, CNRS UMR 5276, Laboratoire de géologie de Lyon: Terre, Planètes, Environnement, Bâtiment GEODE, Villeurbanne, France
Xiaoguang Yang
State Key Laboratory of Continental Dynamics, Shaanxi Key laboratory of Early Life & Environments, Department of Geology, Northwest University, Xi’an, China
State Key Laboratory of Continental Dynamics, Shaanxi Key laboratory of Early Life & Environments, Department of Geology, Northwest University, Xi’an, China
Although fossil evidence suggests that various animal groups were able to move actively through their environment in the early stages of their evolution, virtually no direct information is available on the nature of their muscle systems. The origin of jellyfish swimming, for example, is of great interest to biologists. Exceptionally preserved muscles are described here in benthic peridermal olivooid medusozoans from the basal Cambrian of China (Kuanchuanpu Formation, ca. 535 Ma) that have direct equivalent in modern medusozoans. They consist of circular fibers distributed over the bell surface (subumbrella) and most probably have a myoepithelial origin. This is the oldest record of a muscle system in cnidarians and more generally in animals. This basic system was probably co-opted by early Cambrian jellyfish to develop capacities for jet-propelled swimming within the water column. Additional lines of fossil evidence obtained from ecdysozoans (worms and panarthropods) show that the muscle systems of early animals underwent a rapid diversification through the early Cambrian and increased their capacity to colonize a wide range of habitats both within the water column and sediment at a critical time of their evolutionary radiation.
