RT Journal Article
T1 Evolución eustàtica postflandriense en las marismas del Sur de la Bahía de Cádiz
T1 Postflandrian eustatic evolution in the southern salt-marshes of the Bay of Cádiz
A1 Gracia Prieto, Francisco Javier
A1 Alonso, C.
A1 Gallardo, M.
A1 Giles Pacheco, Francisco
A1 Benavente, Javier
A1 López Aguayo, F.
AB The identification and dating of Holocene marine tenaces in the southern Bay of Cádiz has allowed the reconstruction of its recent coastal evolution. Since the Flandrian maximum was reached in the Bay, about 5000 years ago, a sea level fall is deduced for the Upper Holocene. The consequences of this process consisted in a rapid sedimentary progradation in estuarine/marshland environments and a progressive continentalization of former coastal areas. Meanwhile, the exposed sandy coastline has suffered a severe retreat in some points during recent times, due to several causes, both natural (very energetic marine processes, like historical tsunami or storm waves) and anthropic (construction of dams in the fluvial basins affluent to the bay)
PB Sociedad Geológica de España
YR 1999
FD 1999
LK http://hdl.handle.net/10272/9952
UL http://hdl.handle.net/10272/9952
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026