SciELO - Scientific Electronic Library Online

 
vol.27 número3Historia ambiental postcolombiana del Lago Petén Itzá, GuatemalaNuevas herramientas SexI para evaluar la evolución y perturbación antrópica en campos geotérmicos: El caso del campo geotérmico de Los Azufres, México índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • No hay artículos similaresSimilares en SciELO

Compartir


Revista mexicana de ciencias geológicas

versión On-line ISSN 2007-2902versión impresa ISSN 1026-8774

Resumen

FRANCO, María Jimena. Soroceaxylon entrerriensis n.gen and n.sp. (Moraceae) from the Ituzaingó Formation (Plioceno-Pleistoceno), Paraná river basin, Argentina. Rev. mex. cienc. geol [online]. 2010, vol.27, n.3, pp.508-519. ISSN 2007-2902.

Fossil woods, found in the Pliocene-Pleistocene of Ituzaingó Formation (Paraná Basin, Argentina), are described and assigned to a new morphogenus with affinities with Moraceae family. The fossil woods have predominantly solitary vessels and in radial multiples of between two and nine elements and tangential multiple less common; very small and alternate intervessel pits; axial parenchyma scanty paratracheal, complete and incomplete and apotracheal axial parenchyma scanty and diffuse-in-aggregates; uniseriate and multiseriate rays, heterocellular rays, multiseriate rays with one to three channels probably laticifers or tanniniferous tubes and prismatic crystals in radial cells. The fossil woods are anatomically similar to the extant species ofthe genus Sorocea A. St. Hil. Moraceae probably originate in Eurasia with subsequent migration facilitated by multiple land routes. This record indicates that Moraceae were well established in the Pliocene-Pleistocene of South America.

Palabras llave : Fossil woods; Moraceae; Ituzaingó Formation; Pliocene-Pleistocene; South America.

        · resumen en Español     · texto en Español     · Español ( pdf )

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons