Early Ordovician (Late Floian) conodonts from the Zenta range, Cordillera Oriental, NW Argentina
LOWER Ordovician strata from the Central Andean Basin are superbly exposed in the Zenta Range of the Cordillera Oriental, NW Argentina. At the Laguna Verde section (23°18'S, 65° 1W, 4500 MASL) the sedimentary succession is mostly siliciclastic with subordinate coquinas and calcarenites (Fig. 1)...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2013 |
| País: | Argentina |
| Institución: | Consejo Nacional de Investigaciones Científicas y Técnicas |
| Repositorio: | CONICET Digital (CONICET) |
| Idioma: | inglés |
| OAI Identifier: | oai:ri.conicet.gov.ar:11336/3129 |
| Acceso en línea: | http://hdl.handle.net/11336/3129 |
| Access Level: | acceso abierto |
| Palabra clave: | Conodont Biostratigraphy Lower Ordovician Cordillera Oriental Argentina https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| Sumario: | LOWER Ordovician strata from the Central Andean Basin are superbly exposed in the Zenta Range of the Cordillera Oriental, NW Argentina. At the Laguna Verde section (23°18'S, 65° 1W, 4500 MASL) the sedimentary succession is mostly siliciclastic with subordinate coquinas and calcarenites (Fig. 1). It is unconformably overlain by glacial diamictites and quartzites from the Zapla Formation (Hirnantian). Previous conodont work by Albanesi et al. (2011) recognized the Acodus deltatus – Paroistodus proteus Zone in the nearby Abra de Santa Ana. Aráoz et al. (2008) suggested a Darriwilian to Sandbian age for the strata exposed in the Laguna Verde section, based on the presence of Erismodus and Trapezognathus. In a recent revision of the section, Carlorossi and Heredia (2013) documented from one sample Trapezognathus diprion Lindström(1954) and mentioned the occurrence of Baltoniodus triangularis Lindström (1954) and B. cf. triangularis Lindström (1954) in the same sample (p. 311 and table 2), suggesting a Dapingian age for the upper exposed levels of the Acoite Formation. In order to define the age of aforementioned strata, we took 18 rock samples from the Laguna Verde section plus 2 isolated samples (ZEN17 and ZEN17.2) located 2.5 km to the SW (23°19'S, 65° 0'W), stratigraphically below, which produced a significant conodont fauna, although the diversity is low. The rock samples (24 kg in total), which were digested in 10% acetic acid following the conventional procedures, produced 608 conodont elements. The studied specimens are relatively well preserved (CAI 2, Epstein et al., 1977), with no chemical alteration but abundant fractures that truncate cusps and denticles. The faunal association includes Acodus n. sp. (see Zeballo et al., this volume), Baltoniodus cf. triangularis, Trapezognathus? argentinensis Rao et al.(1994), Trapezognathus diprion, Trapezognathus? primitivus n. sp., Scolopodus houlianzhaiensis An and Xu in An et al. (1983), Drepanodus arcuatus Pander (1856), Drepanoistodus chucaleznensis Albanesi and Aceñolaza (2005), D. costatus (Abaimova, 1971), D. basiovalis (Sergeeva, 1963) and Erraticodon patu Cooper (1981). The record of the taxon Baltoniodus cf. triangularis confirms the presence of the homonymous biozone in the host strata, which indicates the uppermost zone of the Early Ordovician (Floian). According to its age, these strata correlate with the upper part of the Acoite Formation and equivalent units such as the Capillas/Zanjón Formation from the Subandean Ranges. The conodonts are stored in the Museo de Paleontología, Universidad Nacional de Córdoba, with repository code CORD-MP. |
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