Holocene climate variability in the western Mediterranean region from a deepwater sediment record

Author:

Frigola J.1,Moreno A.2,Cacho I.1,Canals M.1,Sierro F. J.3,Flores J. A.3,Grimalt J. O.4,Hodell D. A.5,Curtis J. H.5

Affiliation:

1. Consolidated Research Group Marine Geosciences, Department of Stratigraphy, Paleontology and Marine Geosciences; Faculty of Geology, University of Barcelona; Barcelona Spain

2. Pyrenean Institute of Ecology; Spanish Research Scientific Council; Zaragoza Spain

3. Department of Geology; University of Salamanca; Salamanca Spain

4. Department of Environmental Chemistry; Institute of Chemical and Environmental Research-Spanish Research Scientific Council; Barcelona Spain

5. Department of Geological Sciences; University of Florida; Gainesville Florida USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference100 articles.

1. Acosta , J. 2005 El Promontorio Balear: Morfología submarina y recubrimiento sedimentario Univ. de Barcelona e Inst. Español de Oceanogr. Barcelona

2. The 8k event: Cause and consequences of a major Holocene abrupt climate change;Alley;Quat. Sci. Rev.,2005

3. A deep-sea channel in the northwestern Mediterranean Sea: Morphology and seismic structure of the Valencia channel and its surroundings;Alonso;Mar. Geophys. Res.,1995

4. Nutrients in the Mediterranean Sea, mass balance and statistical analysis of concentrations with respect to environmental change;Bethoux;Mar. Chem.,1998

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