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handle: 10261/162683
En el testigo MW-14-CG-86B (Golfo de Cádiz) se han analizado marcadores geoquímicos y granulométricos para detectar fluctuaciones ambientales durante el Holoceno. Los datos obtenidos sugieren que la intensidad de la Mediterranean Outflow Water (MOW) ha estado relacionada con pequeñas variaciones climáticas. Durante periodos relativamente cálidos y lluviosos la MOW depositó sedimentos más finos aportados fundamentalmente por la red fluvial de las zonas emergidas adyacentes. Durante los intervalos fríos y secos una intensificación de la MOW depositó sedimentos más arenosos y aumentó la contribución eólica
Personal del ICM-CSIS forma parte del V Simposio Internacional de Ciencias del Mar, 20-22 July 2016, Alicante.-- 2 pages, 1 figure
Proyecto MOWER (CTM2012-39599-C03-01-MAR)
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