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The ordovician conodont trapezognathus lindstr?m, 1955 in the andean basin, Argentina

机译:奥陶纪牙形刺体trapezognathus lindstr?m,1955年,阿根廷安第斯盆地

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摘要

The Central Andean Basin is characterized by the presence of Ordovician deposits, distributed mainly in north-western Argentina. Conodonts from the Lower and Middle Ordovician were recovered from several outcrops of the Trapezognathus diprion, Baltoniodus cf. B. triangularis, and Baltoniodus triangularis biozones, and among them the genus Trapezognathus is highlighted. In this paper we describe and illustrate two species of this genus, T. diprion (lindsTr?M) and T. quadrangulum lindsTr?M. The conodont association suggests a faunal affinity with Baltica and South China.
机译:安第斯中部盆地的特征是奥陶纪沉积物的存在,主要分布在阿根廷西北部。下奥陶纪和中奥陶纪的牙形石从梯形千足虫(Baltoniodus cf.三角芽孢杆菌和三角洲巴尔通氏菌的生物区,其中突出的是梯形纲属。在本文中,我们描述并举例说明了该属的两个种,即T. diprion(lindsTr?M)和T. quadrangulum lindsTr?M。牙形刺协会暗示与波罗的海和华南地区有动物区系。

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