RT Journal Article
T1 Reconstrucción paleoclimática del centro de la Península Ibérica durante los últimos 50 ka cal. BP, a partir de los datos físicos y geoquímicos del registro lacustre del mar de Fuentillejo (Campo de Calatrava, Ciudad Real)
T1 Paleoclimatic reconstruction of central Iberian Peninsula during the last 50 ka cal. BP, based on physical angeochemical data from the Fuentillejo maar lacustrine record (Campo de Calatrava, Ciudad Real)
A1 Galán, Luis
A1 Vegas, Juana
A1 García Cortés, Ángel
AB Physical (magnetic susceptibility and gamma density measurements) and geochemical (TOC, Fe andTi analysis) analysis were performed to characterize the sedimentary record in Fuentillejo maar-lake (Campode Calatrava Volcanic Field) in order to reconstruct the paleoenvironmental evolution, which controlleddeposition of different sedimentary facies. The upper 20 m of FU-1 sequence point out variations in clasticinput, water chemistry and organic fraction in the lake throughout the last 50 kyr cal. BP. Magneticsusceptibility are roughly influenced by diagenetic changes in organic rich sediments
YR 2009
FD 2009
LK http://hdl.handle.net/10272/8113
UL http://hdl.handle.net/10272/8113
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026