Revista geológica de Chile
versión impresa ISSN 0716-0208
NIEMEYER, Hans et al. Triassic age of the continental Pular Formation, Sierra de Almeida, Antofagasta, northern Chile. Rev. geol. Chile [online]. 2008, vol.35, n.1, pp. 147-161. ISSN 0716-0208. http://dx.doi.org/10.4067/S0716-02082008000100007.
In this contribution, we present a reassessment of the Pular Formation age (Sierra de Almeida, Antofagasta) that in previous papers was attributed to either the Late Paleozoic or Triassic. At Quebrada del Medio, the Pular Formation includes a 379-meter-thick stratigraphic section formed from base to top by conglomerates, sandstones, black bituminous shales and limestones, tuffaceous sandstones and a poorly welded ignimbrite that accumulated in fluvial and lacustrine environments. A multidisciplinary study of the flora and fauna was undertaken. The existence of diagnostic Gondwana microflora and macroflora allows attributing a Middle Triassic to early Late Triassic age to the Pular Formation
Palabras clave : Pular Formation; Triassic; Gondwana flora; Fluvial and lacustrine environments; Chile.