CAJ | 학술논문

最近的研究表明，安徽霍邱地区安阳山（白大山）剖面下部碳酸盐岩段属于晚石炭世，上部碎屑岩段属于青白口纪。我们进一步对剖面进行了微体古生物分析，在晚石炭世碳酸盐岩中发现了丰富的微体古生物化石，其中以牙形石和虫颚化石数量最多。经鉴定，有牙形石Belodina和虫颚化石Marlenites marginatus，Chairidogenys borealis，Cornugenys sp.，Porrhogrnys sp.，Channahania sp.，Paradrilonersgenys cherylae等，Belodina时代为晚奥陶世，虫颚化石的时代为奥陶纪。晚石炭世地层中存在奥陶纪化石，表明可能存在奥陶系的物源区，微体化石是通过剥蚀、搬运再沉积保存到晚石炭世碳酸盐岩中。显然，新发现的微体化石可能并不具有地层意义，但是具有古地理和古构造意义。
최근적연구표명，안휘곽구지구안양산（백대산）부면하부탄산염암단속우만석탄세，상부쇄설암단속우청백구기。아문진일보대부면진행료미체고생물분석，재만석탄세탄산염암중발현료봉부적미체고생물화석，기중이아형석화충악화석수량최다。경감정，유아형석Belodina화충악화석Marlenites marginatus，Chairidogenys borealis，Cornugenys sp.，Porrhogrnys sp.，Channahania sp.，Paradrilonersgenys cherylae등，Belodina시대위만오도세，충악화석적시대위오도기。만석탄세지층중존재오도기화석，표명가능존재오도계적물원구，미체화석시통과박식、반운재침적보존도만석탄세탄산염암중。현연，신발현적미체화석가능병불구유지층의의，단시구유고지리화고구조의의。
A latest research indicated that carbonate rock member in the lower part of the Anyang Mt (Baida Mt) section, Huoqiu, Anhui belongs to late Carbonaceous epoch, clastic rock member in the upper part to Qingbaikouan period. Further micropaleonlogical analysis found abundant such fossils in the late carbonaceous carbonate rock, of which conodont and scolecodont fossils dominate in quantity. Identified conodont is Belodina, scolecodonts include Marlenites marginatus,Chairidogenys borealis,Cornugenys sp.,Porrhogrnys sp.,Channahania sp.,Paradrilonersgenys cherylae, etc. Belodina dated back to late Ordovician epoch and scolecodonts Ordovician period. Ordovician fossils occurring in later Carbonaceous epoch suggested that there may have been an Ordovician source of micro fossils, which were eroded, transported, re-deposited and preserved in late Carbonaceous carbonate rock. Obviously, this discovery may not be significant stratigraphically, but paleogeographically and paleotectonically.