Tabla cronoestratigráfica del Cuaternario de la península ibérica (v 3.0): Nuevos datos estratigráficos, paleontológicos y arqueológicos

  • Pablo Gabriel Silva Barroso Universidad de Salamanca
  • Teresa Bardají U.D. Geología. Universidad de Alcalá. Alcalá de Henares (Madrid), España.
  • Javier Baena-Preysler Depto. Prehistoria y Arqueología. Universidad Autónoma de Madrid, Cantoblanco, Madrid, Epspaña.
  • Jorge Luis Giner-Robles Dpto. Geología y Geoquímica, Universidad Autónoma de Madrid, Cantoblanco, Madrid, España
  • Jan Van der Made Dpto. Paleobiología, Museo Nacional de Ciencias Naturales, CSIC, Madrid, Espaqña
  • Cari Zazo Dpto. Geología, Museo Nacional de Ciencias Naturales, CSIC. Madrid, España
  • Antonio Rosas Dpto. Paleobiología, Museo Nacional de Ciencias Naturales, CSIC, Madrid, España
  • Javier Lario Dpto. Ciencia Analíticas, Facultad de Ciencias, UNED. Madrid, España
Palabras clave: Cuaternario; Cronoestratigrafía; Fauna; Prehistoria; Yacimientos; península ibérica

Resumen

La tercera edición de la Tabla Cronoestratigráfica del Cuaderno de la península ibérica (v 3.0) sustituye a las versiones más antiguas editadas en 2007 (v 1.0) y 2009 (v 2.0). Desde esta fecha la Comisión Internacional de Estratigrafía (ICS), y más concretamente la Subcomisión de Estratigrafía del Cuaternario (SQS), ha estado trabajando tanto en la definición del Periodo Cuaternario como en sus subdivisiones, aportando nuevos GSSP (Global Stratotype Section and Points) para los mismos. La nueva tabla incluye los GSSPs recientemente aprobados para la subdivisión de la Serie Holocena (Groenlandiense, Norgripiense y Meghalayense), así como el nuevo piso Chibaniense (774,1 - 128,0 ka) ratificado por la IUGS a principios del 2020, que sustituye al Pleistoceno medio. Esta versión 3.0 también incluye todas las modificaciones y correcciones que han surgido desde entonces, incluyendo la actualización de datos, fechas y dataciones para los yacimientos paleontológicos y/o arqueológicos más representativos de la península. Asimismo, se ha revisado la extensión de los diferentes periodos climáticos considerados para Europa central y Alpes ajustándose a las biozonas de mamíferos y las faunas asociadas. La extensión de estas últimas ha de entenderse referida a Europa central y meridional no solo a la península ibérica. En la distribución temporal de periodos de la prehistoria y complejos tecno-culturales asociados se diferencia entre el continente africano y europeo. De la misma forma la sucesión de especies de homininos se centra también en estos dos continentes. Esta revisión ofrece una lista de referencias actualizada, así como una versión digital interactiva que se implementará próximamente.

Biografía del autor/a

Pablo Gabriel Silva Barroso, Universidad de Salamanca
Profesor Titular de Universidad nGeodinámica Externa nGeomorfología y Geofísica

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Publicado
2021-12-16
Sección
Artículos de Investigación