CONTRIBUCIÓN AL CONOCIMIENTO DEL REGISTRO FÚNGICO FÓSIL EN BASE A ESTUDIOS PALINOMICOLÓGICOS DEL GRUPO EL FOYEL, CUENCA DE ÑIRIHUAU, PALEÓGENO, PATAGONIA ARGENTINA
DOI:
https://doi.org/10.5710/PEAPA.12.07.2024.508Palabras clave:
Esporas fúngicas fósiles, Inapertisporites, Grupo El Foyel, Formación Troncoso, OCEM, Paleógeno, ArgentinaResumen
Se describen e ilustran esporas, conidióforos e hifas de hongos fósiles recuperados de nueve muestras de fangolitas aflorantes en la sección Río Foyel, pertenecientes a las Formaciones Troncoso, Salto del Macho y Río Foyel (Grupo El Foyel). Se reconocieron representantes de 16 géneros. Entre las 26 especies descritas, se propone una nueva especie, Inapertisporites lacrimaformis. Las amerósporas son el tipo de esporas más abundantes. A partir del análisis palinoestratigráfico de los restos no polínicos (fúngicos), se sugiere una edad paleógena para el Grupo El Foyel. De las tres formaciones estudiadas, la Formación Troncoso es la que muestra la mayor abundancia y diversidad de restos fúngicos. Este rasgo podría estar evidenciando un período de condiciones climáticas óptimas (templado cálido y húmedo), probablemente relacionado con el Óptimo Climático del Eoceno Medio (OCEM). En base a las preferencias paleoecológicas de los especímenes recuperados del Grupo El Foyel, se podría inferir un ambiente boscoso próximo a un cuerpo de agua fluvial o lacustre.
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