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首页> 外文期刊>Alcheringa: An Australasian Journal of Palaeontology >Middle Ordovician (early Dapingian) conodonts in the Central Andean Basin of NW Argentina
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Middle Ordovician (early Dapingian) conodonts in the Central Andean Basin of NW Argentina

机译:西北西北部安第斯盆地中部的奥陶纪(大坪阶早期)牙形体

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Carlorosi, J., Heredia, S. & Ace?olaza, G, 2013. Middle Ordovician (early Dapingian) conodonts in the Central Andean Basin of NW Argentina. Alcheringa 37, 1-13. ISSN 0311-5518. This paper describes and analyzes the significance of a conodont fauna from the Alto del Cóndor Formation, exposed in the Los Colorados region of the Argentine Eastern Cordillera. Identified taxa are Baltoniodus triangularis, Baltoniodus sp. cf. B. triangularis, Drepanodus sp., Drepanoistodus basiovalis, Drepanoistodus sp. B., Erraticodon patu, Gothodus costulatus, Oistodus sp., Trapezognathus diprion, T. quadrangulum, Triangulodus sp. and Triangulodus? sp. The presence of Baltoniodus triangularis indicates the base of the Dapingian stage (Middle Ordovician). In addition, we report the coexistence of T. diprion and T. quadrangulum. The conodont association suggests a faunal affinity with Baltica and South China, both belonging to the Shallow-Sea Realm of the Temperate-Cold Domain. Josefina Carlorosi [josefinacarlorosi77@gmail]com], INSUGEO-Universidad Nacional de Tucumán-CONICET, Miguel Lillo 205, (4000) Tucumán, Argentina; Guillermo F. Ace?olaza [acecha@webmail.unt.edu.ar], Universidad Nacional de Tucumán-CONICET, Miguel Lillo 205, (4000) Tucumán, Argentina; Susana Heredia [sheredia@unsj.edu.ar], CONICET-CIGEOBIO and Instituto de Investigaciones Mineras, Facultad de Ingeniería, Universidad Nacional de San Juan, Urquiza y Libertador, (5400) San Juan, Argentina. Received 22.8.2012; revised 18.10.2012; accepted 24.10.12.
机译:卡罗罗西,J。,埃雷迪亚,S。&Ace?olaza,G,2013年。中西北奥陶纪(大坪纪早期)牙形体,位于西北阿根廷的安第斯盆地。 Alcheringa 37,1-13。 ISSN 0311-5518。本文描述并分析了阿根廷东部科迪勒拉山脉洛斯科罗拉多地区暴露的Alto delCóndor组牙形动物群的重要性。鉴定出的分类群是Baltoniodus triangleis,Baltoniodus sp.。 cf.三角芽孢杆菌,Drepanodus sp。,Drepanoistodus basiovalis,Drepanoistodus sp。 B.,Erraticodon patu,Gothodus costulatus,Oistodus sp。,Trapezognathus diprion,T.quadrangulum,Triangulodus sp。和Triangulodus? sp。 Baltoniodus triangleis的存在表明大坪期(中奥陶纪)的基础。另外,我们报告了T. diprion和T. quadrangulum并存。牙形石的联系暗示了它们与波罗的海和华南地区的动物区系亲和力,它们都属于温带冷域的浅海区。 Josefina Carlorosi [josefinacarlorosi77 @ gmail] com,INSUGEO-国立Tucumán-CONICET大学,Miguel Lillo 205,(4000),阿根廷Tucumán; Guillermo F. Ace?olaza [acecha@webmail.unt.edu.ar],国立Tucumán-CONICET大学,Miguel Lillo 205,(4000),阿根廷Tucumán; Susana Heredia [sheredia@unsj.edu.ar],CONICET-CIGEOBIO和矿业研究所,Instituto deIngeniería,国立圣胡安大学,Urquiza y Libertador(5400),阿根廷圣胡安。收到22.8.2012;修订的2012年10月18日;接受24.10.12。

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