泰国东北长笏莱王saphung以东怀琅的莫斯科有孔虫新种群

Katsumi Ueno , Koichi Nagai , Nikorn Nakornsri , Tetsuo Sugiyama
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引用次数: 7

摘要

在泰国已知的莫斯科有孔虫动物群中,Fusulinella物种的罕见性是最有趣的特征之一。早先在泰国东北部曾发生过博氏镰刀菌Möller,但既没有描述也没有说明。在泰国东北长府府王saphung以东约5 km的怀琅(Huai Luang)石灰岩中,首次发现了一种以Fusulina pulchella群为特征的两个Fusulinella种F. bocki von Möller和F. praebocki raser - chernoussova为特征的小型有孔虫区系。地质证据表明,我们的有孔虫动物群最肯定来自与pulchella Fusulina带相关的地层,尽管F. pulchella Gryzlova没有出现在我们的动物群中。本文在槐琅发现的含fusulinella有孔虫区系,反映了晚莫斯科时代(很可能是俄罗斯标准方案中的Myachkovsky层位),为厘清Fusulina pulchella带的区系组成和比较Loei-Wang Saphung地区晚莫斯科时代的有孔虫区系与类型剖面和参考剖面的区系关系提供了重要数据。本文描述了六种毛藻纲,并列举了共存的小型有孔虫。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A new Moscovian foraminiferal fauna from Huai Luang, east of Wang Saphung, Changwat Loei, Northeast Thailand

The unusual rarity of Fusulinella species is one of the most interesting characteristics among the known Moscovian foraminiferal faunas in Thailand. Earlier an occurrence of Fusulinella bocki von Möller was documented in Northeast Thailand but with neither description nor illustration. For the first time, we have recently discovered a small foraminiferal fauna characterized by two Fusulinella species (F. bocki von Möller and F. praebocki Rauser-Chernoussova) from a limestone collected at Huai Luang, about 5 km east of Wang Saphung, Changwat Loei, Northeast Thailand, where the Fusulina pulchella fauna was reported previously. Geological evidence suggests that our foraminiferal fauna most certainly came from the strata referable to the Fusulina pulchella Zone although F. pulchella Gryzlova is absent from our fauna. The present discovery of a Fusulinella-bearing foraminiferal fauna from Huai Luang, indicative of a Late Moscovian age (most probably to the Myachkovsky Horizon in the Russian standard scheme), provides important data to clarify the faunal composition of the Fusulina pulchella Zone and to compare the Late Moscovian foraminiferal faunal affinity in the Loei-Wang Saphung area with those of the type and reference sections. In this paper, six species of fusulinaceans are described, and coexisting smaller foraminifers are listed and illustrated.

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