[Palaeontology, 2017, pp. 1–15] ANATOMY AND AFFINITIES OF A NEW 535-MILLION-YEAR-OLD MEDUSOZOAN FROM THE KUANCHUANPU FORMATION, SOUTH CHINA by XING WANG1,2 ,JIANHAN1,*, JEAN VANNIER2,QIANGOU3,4, XIAOGUANG YANG1,KENTAROUESUGI5, OSAMU SASAKI6 and TSUYOSHI KOMIYA7 1Early Life Institute & Department of Geology, State Key Laboratory of Continental Dynamics, Northwest University, 229 Taibai Road, Xi’an, 710069, China;
[email protected] 2UMR 5276 du CNRS, Laboratoire de geologie de Lyon: Terre, Planetes, Environnement, Universite Lyon 1, B^atiment GEODE, 2, rue Rapha€el Dubois, Villeurbanne, 69622, France 3Early Life Evolution Laboratory, School of Earth Sciences & Resources, University of Geosciences, Beijing, 100083, China 4Department of Zoology, University of Kassel, Kassel, 34132, Germany 5Japan Synchrotron Radiation Research Institute (JASRI) 1-1-1 Kouto, Sayo-cho, Sayo-gun, Hyogo Japan 6Tohoku University Museum, Tohoku University, 6-3 Aoba, Aramaki, Aoba-ku, Sendai, Japan 7Department of Earth Science & Astronomy, Graduate School of Arts and Sciences, The University of Tokyo, Tokyo, 153-8902, Japan *Corresponding author Typescript received 10 April 2017; accepted in revised form 30 June 2017 Abstract: We describe here Sinaster petalon gen. et sp. pockets. Although Sinaster cannot be straightforwardly nov., a new embryonic form from the c. 535 million-year- assigned to any crown-group within Medusozoa, the pres- old Kuanchuanpu Formation of South China (Ningqiang, ence of marginal lappets and endodermal lamellae suggests Shaanxi Province). The excellent three-dimensional, phos- that it is closer to Cubozoa and Scyphozoa than to any other phatic preservation of these microfossils allowed us to use group of modern cnidarians. The tentative placement of x-ray microtomographic techniques to make accurate recon- Sinaster within the stem-group Cubozoa is justified by the structions of their internal structures and to compare their presence of a velarium supported by a frenulum.