FN Archimer Export Format
PT J
TI Deglacial to Holocene environmental changes in the northern Ligurian Sea: The dual influence of regional climate variability and large-scale intermediate Mediterranean circulation
BT 
AF Le Houedec, Sandrine
   Mojtahid, Meryem
   Ciobanu, Maria Cristina
   Jorry, Stephan
   Bouhdayad, Fatima Zohra
   Guyonneau, Emma
   Sourice, Stéphane
   Toucanne, Samuel
AS 1:1;2:1;3:2;4:2;5:3;6:1;7:1;8:2;
FF 1:;2:;3:PDG-REM-GM-LES;4:PDG-REM-GM-LGS;5:;6:;7:;8:PDG-REM-GM-LGS;
C1 LPG-BIAF UMR-CNRS 6112, UNIV Angers, CNRS, 2 bd Lavoisier, 49045 Angers Cedex 01, France
   IFREMER, Unité de Recherche Géosciences Marines, Laboratoire Géodynamique et enregistrement Sédimentaire, CS10070, F-29280 Plouzané, France
   Institute of Geology and Mineralogy, Faculty of Mathematics and Natural Sciences, University of Cologne, Otto-Fischer-Straße 14, 50674 Cologne, Germany
C2 UNIV ANGERS, FRANCE
   IFREMER, FRANCE
   UNIV COLOGNE, GERMANY
SI BREST
SE PDG-REM-GM-LES
   PDG-REM-GM-LGS
IN WOS Ifremer UPR
   copubli-france
   copubli-europe
   copubli-univ-france
IF 3.565
TC 3
UR https://archimer.ifremer.fr/doc/00697/80869/84541.pdf
LA English
DT Article
CR ESSCAR-9
BO Le Suroît
DE ;Foraminifera;Paleoclimatology;Western Mediterranea;Holocene
AB The sedimentary archives of the Mediterranean Sea record periodic deposits of organic-rich deposits, called sapropels in the eastern basin and organic-rich layers (ORL) in the western basin. Changes in both the Mediterranean circulation and inputs of fresh water through borderlands rivers under more humid climate, are important mechanisms to explain those events. The last ORL and sapropel S1 have different timing, respectively from ~14.5 to 9 Ka and from ~10 to 6 Ka, presumably due to different forcing factors in the western basin (i.e., melting of Alps ices). Here we present a high-resolution study of a marine sediment core located off the mouth of the Var River, one of the most dynamic river system of the northern borderland of the western Mediterranean Sea. We applied a multi-proxy approach based on benthic foraminiferal assemblages, foraminiferal δ18O and δ13C, grain size analyses, organic carbon content and XRF elemental data to decipher the regional climate signals from the basin-scale intermediate circulation signature. Our results do not show large river inputs at the timing of the last ORL deposit. On the opposite, foraminiferal and geochemical evidence indicate that the 11–6 kyr period, concomitant to Sapropel S1 event in the Eastern Mediterranean, was characterised by high river activity and low ventilated bottom waters at the studied location. Additionally, our results characterized the last 6 ka with large scale episodes of more active bottom water ventilation due perhaps to enhanced wind activity under an overall cooler climate. Time series analyses were computed from stable isotopes, Ca/Ti XRF ratio and foraminifera abundances. They show common frequencies peaks (2.2–3, 1.1–1.2, 0.9–1.0, and 0.4–0.5 kyr) most likely related to the solar activity. Also, a specific frequency band (1.5–1.6 kyr) was only recorded in benthic foraminiferal abundance and stable isotopic records. This was preferentially attributed to an oceanic-driven internal forcing. 
PY 2021
PD AUG
SO Palaeogeography Palaeoclimatology Palaeoecology
SN 0031-0182
PU Elsevier BV
VL 576
UT 000668458200011
DI 10.1016/j.palaeo.2021.110500
ID 80869
ER

EF