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华南地区中泥盆世晚期发生了一次大海侵,而块状群体的内板珊瑚(Endophyllum)则是这次大海侵开始时的标志性化石,Endophyllum往往与其它的群体造礁珊瑚(如Argutastrea,Alveolites等)和层孔虫(如Strom-atopora,Clathrostroma等)形成生物层或生物岩礁。华南地区Endophyllum的地层层位十分稳定,大致位于牙形类的Polygnathus varcus带的下部,它经常与吉维特期标准腕足类鸮头贝(Stringocephalus)共生。根据对产自新疆北部东准噶尔和西准噶尔所谓的“Endophyllum”的外部形态特征和内部构造的微细结构的深入研究,并将它与华南地区湘、桂、黔、滇、川等省(区)所产出的Endophyllum进行仔细的对比之后认为:两者存在着很大的差别,它们应分属于不同的属、甚至不同的科或科以上的分类单元,而且它们产出的地层层位也不尽相同,北疆所谓的“Endophyllum”要比华南的Endophyllum出现得早。
In southern China, a large transgression occurred in the late Middle Devonian period, while the massive coral Endophyllum was the landmark fossil at the beginning of this major transgression. Endophyllum often co-reefed with other groups such as Argutastrea, Alveolites, etc.) and foraminifera (eg Strom-atopora, Clathrostroma, etc.) form bio-layers or bio-reefs. The stratigraphic layer of Endophyllum in southern China is very stable and lies roughly in the lower part of the Teeth type Polygnathus varcus, which often coexists with the standard Gibordian brachiopod Stringocephalus. Based on the in-depth study on the microscopic structure of the so-called “Endophyllum ” originating from East Junggar and West Junggar in northern Xinjiang and comparing it with the detailed structure of internal structure in southern and eastern Hunan, Guangxi, Guizhou, Yunnan and Sichuan provinces After careful comparison of Endophyllum produced, we conclude that there is a big difference between the two, which should belong to different genera and even different families or more taxonomic units, and their production of stratigraphic position Is not the same, the so-called “Endophyllum” in northern Xinjiang appeared earlier than Endophyllum in southern China.