SHAO Tiequan
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaLIU Yunhuan
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, China 2 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences, Nanjing 210008, ChinaWANG Qi
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaZHANG Huaqiao
3 Key Laboratory of Economic Stratigraphy and Palaeogeography, Chinese Academy of Sciences (Nanjing Institute of Geology and Palaeontology), Nanjing 210008, ChinaTANG Hanhua
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaCAO Xi
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaHE Huahua
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaZHANG Yanan
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaLI Yuan
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaZHENG Panlin
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaZHU Chengyu
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaHU Jiaxi
1 College of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaThis work was supported by the National Natural Science Foundation of China (41072012 and 41102003), the State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (113115 and 20132107), the Key Project of Central University Fund (CHD2012ZD017), College Students’ Innovative Entrepreneurial Training Program (201410710144 and 201410710105), and The Ninth “Challenge Cup” Competition of College Students’ Extracurricular Academic and Technological Achievements, Chang’an University.
SHAO Tiequan, LIU Yunhuan, WANG Qi, ZHANG Huaqiao, TANG Hanhua, CAO Xi, HE Huahua, ZHANG Yanan, LI Yuan, ZHENG Panlin, ZHU Chengyu, HU Jiaxi.2015. New Small Shelly Fossils (Acanthocassis and Xinlispina Gen. Nov.) from the Fortunian Stage (Early Cambrian) in Southern China[J]. Acta Geologica Sinica(),89(5):1470-1481
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