3.9 Article

Early Ordovician conodonts from the Santa Rosita Formation at Pantipampa, Iruya area, northwestern Argentina

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ANDEAN GEOLOGY
卷 46, 期 1, 页码 168-182

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SERVICIO NACIONAL GEOLOGIA MINERVA
DOI: 10.5027/andgeoV46n1-3141

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Conodonts; Tremadocian; Santa Rosita Formation; Iruya; Argentina

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  1. Consejo Nacional de Investigaciones Cientificas y Tecnicas
  2. Universidad Nacional de La Plata, Argentina

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A conodont assemblage recovered from the middle part of the Santa Rosita Formation at Pantipampa (Iruya area, northwestern Argentina) is described herein. It includes Cordylodus angulatus Pander, C. cayesi Druce and Jones, C. lindstromi Druce and Jones, C. hastatus Barnes, Furnishina furnishi Muller, Kallidontus gondwanicus Zeballo and Albanesi, Phakelodus elongatus An, Phakelodus tenuis (Zhang), Proconodontus muelleri Miller, Semiacontiodus sp. and Teridontus nakamurai Nogami, which are characteristic of the Cordylodus angulatus Zone (upper lower Tremadocian). In the Iruya area, the C. angulatus Zone correlates with the trilobite Kainella meridionalis Zone and the lower part of the Kainella teiichii Zone. Taxonomic diversity and relative frequency of conodont species enables the recognition of the Semiacontiodus-Teridontus community, which is characteristic of shallow marine environments.

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