CAJ | 학술논문

异珊瑚化石始发现于早泥盆世，早石炭世为鼎盛时期，至早二叠世末全部绝灭。本研究将异珊瑚划分为4个化石组合，并对异珊瑚的起源、分布及迁移规律及生态环境等进行了讨论。化石组合由老至新分别为：早泥盆世Tetraphyllia组合；晚泥盆世Oligophylloides-Heterophyllia组合；早石炭世Pentaphyllia-Hexaphyllia-Radiciphyllia组合；早二叠世Dichophyllia-Heterophyllia-Hexaphylloides组合。并指出异珊瑚属于热带—亚热带至暖温带的生物类群，起源中心可能为中国华南板块。
이산호화석시발현우조니분세，조석탄세위정성시기，지조이첩세말전부절멸。본연구장이산호화분위4개화석조합，병대이산호적기원、분포급천이규률급생태배경등진행료토론。화석조합유로지신분별위：조니분세Tetraphyllia조합；만니분세Oligophylloides-Heterophyllia조합；조석탄세Pentaphyllia-Hexaphyllia-Radiciphyllia조합；조이첩세Dichophyllia-Heterophyllia-Hexaphylloides조합。병지출이산호속우열대—아열대지난온대적생물류군，기원중심가능위중국화남판괴。
The earliest Heterocorals have been found in Lower Devonian atWenshan district，Yunnan of China.The Heterocorals got their climax of evolution during Early Carboniferous，and extincted after Early Permian.There are 4 fossil assemblages divided.The authors discuss the characteristic of every fossil assemblage，the patterns of distribution and immigration，and the ecologic environments.The fossil assemblage is as follow：Tetraphyllia Assemblage of Early Devonian；Oligophylloides-Heterophyllia Assemblage of Late Devonian；Pentaphyllia-Hexaphyllia-Radiciphyllia Assemblage of Early Carboniferous；Dichophyllia-Heterophyllia-Hexaphylloides Assemblage of Early Permian.The authors point out that the South China Plate may be the deriving center of Heterocorallia and the Heterocoral is one of tropic-subtropic to warm temperate zone biotic community.