Climatic and environmental variations during 130 ka : investigations from sedimentary record on the Rhône deltaic margin (Gulf of Lions, NW Mediterranean)

Type Proceedings paper
Date 2006-09
Language English
Author(s) Jouet Gwenael, Gaudin Mathieu, Bassetti Maria-Angela, Berne Serge, Rabineau MarinaORCID, Dennielou BernardORCID, Sierro F, Flores J, Taviani M
Meeting International Sedimentological Congress 2006, 27 august-1 september, Fukuoka, Japan.
Source International Sedimentological Congress 2006, 27 august-1 september, Fukuoka, Japan.
Abstract The Rhône deltaic margin (NW Mediterranean) was under the influence of a very high sedimentation flux during the last climatic cycle, because of the vicinity of major fluvial systems that fed the outer shelf during the glacial period and the inner shelf during the deglacial period. The two areas provide a complete sedimentary record of depositional events from 130 cal. kyr BP to present. This sequence represents the sedimentary expression of the glacial/interglacial cycle (100 kyr cyclicity) within the Late Quaternary succession [1]. [Extract]
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Jouet Gwenael, Gaudin Mathieu, Bassetti Maria-Angela, Berne Serge, Rabineau Marina, Dennielou Bernard, Sierro F, Flores J, Taviani M (2006). Climatic and environmental variations during 130 ka : investigations from sedimentary record on the Rhône deltaic margin (Gulf of Lions, NW Mediterranean). International Sedimentological Congress 2006, 27 august-1 september, Fukuoka, Japan. https://archimer.ifremer.fr/doc/00000/6152/