FN Archimer Export Format PT J TI Holocene climate variability in the North-Western Mediterranean Sea (Gulf of Lions) BT AF JALALI, B. SICRE, M. -A. BASSETTI, M. -A. KALLEL, N. AS 1:1,2;2:2;3:3;4:1; FF 1:;2:;3:;4:; C1 Univ Sfax, GEOGLOB, Fac Sci Sfax, Route Soukra Km 4-BP802, Sfax 3038, Tunisia. Univ Paris 06, Univ Paris 04, CNRS IRD MNHN, LOCEAN Lab, 4 Pl Jussieu, F-75005 Paris, France. Univ Perpignan, CEFREM, Ave J-P Alduy, F-66860 Perpignan, France. C2 UNIV SFAX, TUNISIA UNIV PARIS 06, FRANCE UNIV PERPIGNAN, FRANCE IN DOAJ IF 3.543 TC 52 UR https://archimer.ifremer.fr/doc/00333/44461/44139.pdf LA English DT Article CR GMO2 - CARNAC IMAGES V LEG 1-MD114 IMAGES V LEG 4-MD114 BO Le Suroît Marion Dufresne AB Sea surface temperatures (SSTs) and land-derived input time series were generated from the Gulf of Lions inner-shelf sediments (NW Mediterranean Sea) using alkenones and high-molecular-weight odd-carbon numbered n-alkanes (TERR-alkanes), respectively. The SST record depicts three main phases: a warm Early Holocene ( ∼  18 ± 0.4  °C) followed by a cooling of  ∼  3  °C between 7000 and 1000 BP, and rapid warming from  ∼  1850 AD onwards. Several superimposed multi-decadal to centennial-scale cold events of  ∼  1  °C amplitude were also identified. TERR-alkanes were quantified in the same sedimentary horizons to identify periods of high Rhone River discharge and compare them with regional flood reconstructions. Concentrations show a broad increase from the Early Holocene towards the present with a pronounced minimum around 2500 BP and large fluctuations during the Late Holocene. Comparison with Holocene flood activity reconstructions across the Alps region suggests that sediments of the inner shelf originate mainly from the Upper Rhone River catchment basin and that they are primarily delivered during positive North Atlantic Oscillation (NAO). PY 2016 SO Climate Of The Past SN 1814-9324 PU Copernicus Gesellschaft Mbh VL 12 IS 1 UT 000371624500006 BP 91 EP 101 DI 10.5194/cp-12-91-2016 ID 44461 ER EF