Asociación de Megafauna Paleozoica (Trilobites) provenientes del Pozo CPO 17 EST 12 Cuenca de los Llanos Orientales de Colombia

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DOI:

https://doi.org/10.32685/0120-1425/bol.geol.52.1.2025.748

Keywords:

Llano Orientales Basin, Bioestratigraphy, Paleozoic, Trilobites, Brachiopods

How to Cite

Dueñas-Jiménez, H., Monti, D. S., Lavié, F., & Patarroyo, P. (2025). Asociación de Megafauna Paleozoica (Trilobites) provenientes del Pozo CPO 17 EST 12 Cuenca de los Llanos Orientales de Colombia. Boletín Geológico, 52(1). https://doi.org/10.32685/0120-1425/bol.geol.52.1.2025.748

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Articles

Published

2025-06-30

Abstract

The results of the analysis of macrofauna from eight samples of core 14 taken in the CPO 17-EST. 12 well are presented. This well is in the Paleozoic Meta sub-basin of the Eastern Llanos Basin of Colombia (LLO). The trilobite association is not diverse and consists of olenids, assignable to the Triarthrinae subfamily, and a fragment that could belong to the Trinucleidae family. The presence of the genus Porterfieldia can be determined with certainty.  Likewise, the occurrence of a linguliform brachiopod specimen that can be associated with the family Obolidae is also recorded. The macrofaunal association allows assigning to the sediments analyzed in well CPO 17-EST. 12 an Ordovician range, Floian to Darriwilian interval. The sediments analyzed in well CPO 17-EST. 12 are basically correlatable with the section drilled in the Negritos-1 well, which was assigned an Ordovician range, Floian–Dapingian interval, with faunal differences possibly related to environmental variations. Although the wells La Heliera-1 and CPO 17-EST. 12 drilled Ordovician sediments, the sediments in the La Heliera-1 well are Tremadocian and correspond to an interval stratigraphically lower than the one drilled in the CPO 17-EST. 12 well. Most trilobite genera in Eastern Llanos Basin during the Tremadocian–Darriwilian are cosmopolitan. However, the presence of Porterfieldia and Anebolithus in the Floian–Darriwilian indicates a faunal affinity with other regions of the northwestern Gondwanan margin, particularly with the South American margin and the Avalonian terrane.

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