A new record of fossil plants in Argentina: implications on the Upper Devonian-lowermost Carboniferous stratigraphic records.

PRESTIANNI, C.R.; RUSTÁN, J.J.; VACCARI, NORBERTO EMILIO; STERREN, ANDREA; RUBINSTEIN, CLAUDIA; STEEMANS PHILIP

Liege

Congreso; Palynologists and Plant Micropaleontologists of Belgium Anual Meeting, 2011; 2011

Up to now, fossiliferous, Upper Devonian sedimentary rocks have not been reliably recognized cropping out in Argentina. The single units considered as most probably recording the Devonian-Carboniferous transition are comprised within the La Punilla Formation, which integrates the main body of the Sierra de La Punilla, in the southwestern area of the La Rioja Province, in central-west Argentina (Caminos et al., 1993). In this formation, two stratigraphic units were identified: a sandy lower member considered as Middle Devonian in age on basis of the presence of Malanzania antigua, and an upper hetherolitic member of probable Mississipian age based on records of Frenguelli eximia. The presence of Upper Devonian levels, was inferred there considering the continuity of the section, but without direct paleontological evidences (Morel et al., 1994). Recently a siliciclastic sucession, was surveyed in the southernmost area of the Sierra de Las Minitas, a set of low ranges exhibiting stratigraphic and structurally complex settings, considered to be the northernmost continuation of the Sierra de la Punilla. One section of the Sierra de las Minitas (corresponding to the poorly known Jagüel Formation) is particularly interesting because it includes glacigenic diamictites deposits of discussed Devonian/Carboniferous age. Although radiometric ages of igneous bodies seemed indicate Upper Devonian-Lower Mississippian ages (Ezpeleta and Astini 2009) in nearby sections, palynological contents from this locality indicated a Middle Devonian age for the glacigenic deposits (Rubinstein et al. 2010). The section is composed of pebbled dark mudstones at the base, a thick bed of (ca.70 m) diamictites above overlied by an hetherolitic interval (alternating sandstones, mudstones and shales) with brachiopod and bivalves coquinas and scarce plants, a thick sandy interval. Towards the top, another transgressive-regressive cycle with faunal records was recognised.