Vol. 30 No. 1 (2008): Boletín De Geología
Articles

DEPÓSITOS DE CIÉNAGA LEVANTADOS CERCA DE CARTAGENA DE INDIAS, EVIDENCIAS DE INESTABILIDAD EUSTÁTICA Y CLIMÁTICA DURANTE EL HOLOCENO SUPERIOR

Jaime de Porta
Universitat de Barcelona
Bio
Rodolfo Barrera
GTR
Bio
Ramón Julià
Institut “Jaume Almera”
Bio

Published 2009-10-20

How to Cite

de Porta, J., Barrera, R., & Julià, R. (2009). DEPÓSITOS DE CIÉNAGA LEVANTADOS CERCA DE CARTAGENA DE INDIAS, EVIDENCIAS DE INESTABILIDAD EUSTÁTICA Y CLIMÁTICA DURANTE EL HOLOCENO SUPERIOR. Boletín De Geología, 30(1). Retrieved from https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/300

Abstract

 

The marsh deposits cropping out near Galerazamba are located at 15 m above sea level and at a distance of 1,250 m from the present day Ciénaga El Totumo. This location suggests frequent changes in the sea level. A radiocarbon age of 4,150±50 yr BP was obtained from mollusc remains at the Ciénaga El Totumo. The age of the marsh corresponds to a dry climate period according to paleoenvironmental data from the northern part of South America. The Ciénaga El Totumo retreated during this dry episode. The fossil biota content found in these raised marsh deposits is poorly diversifed and corresponds to the inner part of the marsh.

Keywords: Marsh deposits; Ciénaga El Totumo; Colombia; Late Holocene; Molluscs; C-14.

 

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