ENSAMBLES DE MICROFÓSILES (FORAMINÍFEROS Y NANOFÓSILES CALCÁREOS) CRETÁCICOS DEL SUBSUELO DE LA CUENCA DE MAGALLANES, ISLA DE TIERRA DEL FUEGO, CHILE

Autores/as

  • Jens Michael Thissen Laboratorio de Bioestratigrafía, YPF Tecnología, Berisso, Buenos Aires, Argentina
  • Juan Pablo Pérez Panera Laboratorio de Bioestratigrafía, CONICET – YPF Tecnología, Berisso, Buenos Aires, Argentina

DOI:

https://doi.org/10.5710/PEAPA.24.09.2020.342

Palabras clave:

Foraminifera, Nanofósiles, Mesozoico, Cuenca Austral, Taxonomía

Resumen

Se estudiaron los foraminíferos y nanofósiles calcáreos en muestras de recorte de perforación lavados de tres pozos del sector chileno de la Cuenca de Magallanes. El objetivo de esta contribución es identificar, caracterizar e ilustrar estos ensambles a lo largo del registro sedimentológico cretácico, integrar los datos de los foraminíferos y nanofósiles y optimar futuros estudios bioestratigráficos en la cuenca. La sucesión cretácica analizada en los tres pozos permitió reconocer cinco ensambles discretos: el ensamble del Valanginiano–Hauteriviano está caracterizado por una baja diversidad de foraminíferos bentónicos típicos de esta edad, como Lenticulina nodosa y Astacolus gibber, y los nanofósiles marcadores Lithraphidites bollii y Eiffellithus striatus; el Aptiano–Albiano comienza con una predominancia de radiolarios en transición a foraminíferos bentónicos bien preservados y altamente diversos, principalmente gavelinéllidos, junto con abundantes foraminíferos planctónicos incluyendo Muricohedbergella delrioensis y M. portsdownensis y muy diversos nanofósiles calcáreos con el marcador Sollasites falklandensis; el Cenomaniano se puede distinguir por la presencia del nanofósil Corollithion kennedyi y también abundantes foraminíferos planctónicos; el ensamble del Coniaciano–Campaniano está caracterizado por foraminíferos planctónicos como Costellagerina bulbosa, C. pilula y Planoheterohelix reussi, así como gran diversidad de bentónicos y las especies de nanofósiles Reinhardtites anthophorus, Eiffellithus eximius y Eprolithus floralis; y finalmente el ensamble del Maastrichtiano está caracterizado principalmente por foraminíferos aglutinados y nanofósiles calcáreos muy mal preservados y poco abundantes. Se presenta una detallada lista sistemática de las especies identificadas que servirá como catálogo para la identificación de estos diferentes ensambles cretácicos en futuros trabajos en esta cuenca.

Citas

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