Labechiid stromatoporoids from the Middle Ordovician Machiakou Formation of North China and their implications for the early development of stromatoporoids

J. Jeon, Qijian Li, Zhongyang Chen, Kun Liang, S. Kershaw, Yuandong Zhang
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引用次数: 4

Abstract

Abstract The Darriwilian stromatoporoid assemblages of North China represent a critical stage in early stromatoporoid development across the peri-Gondwanan regions, reaching their highest generic diversity than elsewhere as part of the Great Ordovician Biodiversification Event. We describe four labechiid stromatoporoid species, Labechia variabilis Yabe & Sugiyama, 1930, Labechiella mingshankouensis (Ozaki, 1938), Thamnobeatricea suxianensis (Dong, 1982), and Sinodictyon columnare Yabe & Sugiyama, 1930 from the Middle Ordovician Machiakou Formation in the Xiaonanhai section near Anyang City in northern Henan Province of China. The conodont Plectodina onychodonta occurs in association with these labechiids, implying a middle to late Darriwilian age. This assemblage extends the stratigraphic range of early stromatoporoids in North China to as early as the middle Darriwilian, thus slightly older than the previously known late Darriwilian earliest records. Mutual encrustations of Labechia variabilis and Labechiella mingshankouensis in the present assemblage constructed a microbioherm, together with unidentified tubular organisms, Ortonella-like calcimicrobes, a tubeworm-like organism, and borings. The assemblages of the Darriwilian labechiid stromatoporoids vary from place to place palaeogeographically in the shallow epicontinental marine environment of North China, i.e., in a patchy manner. The significant diversification of Darriwilian labechiid stromatoporoids in North China was likely promoted by a combination of environmental and ecological factors, which include: (1) the occurrence of a very shallow epicontinental marine environment, (2) a possible increase in the carbonate saturation state in seawater, (3) favourable seawater temperature for stromatoporoids during the Middle Ordovician and (4) the scarcity of bryozoans and corals as ecological competitors in North China.
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华北中奥陶统马基雅口组Labechiid叠孔虫及其对叠孔虫早期发育的意义
华北地区Darriwilian叠合孔虫组合代表了冈瓦南周边地区早期叠合孔虫发育的关键阶段,其属多样性是奥陶系生物多样性大事件的一部分。本文描述了河南省北部安阳小南海地区中奥陶世马基雅口组的labechiia variabilis Yabe & Sugiyama, 1930, Labechiella mingshankouensis (Ozaki, 1938), Thamnobeatricea suxianensis (Dong, 1982)和Sinodictyon columnare Yabe & Sugiyama, 1930。牙形刺Plectodina onychodonta与这些唇形类一起出现,表明其存在于达里威廉时代的中晚期。该组合将华北地区早期叠层孔虫的地层范围延长至达里廉中期,比先前已知的达里廉晚期最早记录略早。变异Labechia variabilis和明山口Labechiella mingshankouensis在该组合中相互结壳,与未识别的管状生物、ortonella样钙化微生物、管状蠕虫样生物和蛀虫一起构建了一个微生物群落。在华北陆表浅海环境中,darriwillian唇孔类叠孔类的组合在古地理上因地而异,即呈斑块状。华北地区Darriwilian labechiid叠孔虫的显著多样化可能是环境和生态因素共同作用的结果,其中包括:(1)极浅陆表海洋环境的出现;(2)海水中碳酸盐饱和度可能升高;(3)中奥陶世时期海水温度有利于叠孔虫生长;(4)华北地区苔藓虫和珊瑚作为生态竞争对手的缺乏。
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