FN Archimer Export Format
PT J
TI Large-scale response of the Eastern Mediterranean thermohaline circulation to African monsoon intensification during sapropel S1 formation
BT 
AF TESI, T.
   ASIOLI, A.
   MINISINI, D.
   MASELLI, V.
   VALLE, G. Dalla
   GAMBERI, F.
   LANGONE, L.
   CATTANEO, Antonio
   MONTAGNA, P.
   TRINCARDI, F.
AS 1:1;2:2;3:3;4:4;5:1;6:1;7:1;8:5;9:1;10:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:PDG-REM-GM-LAD;9:;10:;
C1 CNR, CNR ISMAR, Ist Sci Marine, Via Gobetti 101, I-40129 Bologna, Italy.
   CNR, IGG, Via G Gradenigo 6, I-35131 Padua, Italy.
   Shell Int Explorat & Prod Inc, 3333 Highway 6 South, Houston, TX 77082 USA.
   Univ Aberdeen, Dept Geol & Petr Geol, Kings Coll, St Marys Bldg, Aberdeen AB24 3UF, Scotland.
   IFREMER, Geosci Marines EDROME, Ctr Brest, BP70, F-29280 Plouzane, France.
C2 IAMC CNR, ITALY
   IAMC CNR, ITALY
   SHELL INT EXPLORAT & PROD INC, USA
   UNIV ABERDEEN, UK
   IFREMER, FRANCE
SI BREST
SE PDG-REM-GM-LAD
IN WOS Ifremer jusqu'en 2018
   copubli-europe
   copubli-int-hors-europe
IF 4.334
TC 31
UR https://archimer.ifremer.fr/doc/00371/48205/89828.pdf
LA English
DT Article
CR PROMETE 90 (2)
BO Marion Dufresne
DE ;Sapropel S1;Mediterranean sea;African monsoons;Anoxia;Thermohaline circulation
AB The formation of Eastern Mediterranean sapropels has periodically occurred during intensification of northern hemisphere monsoon precipitation over North Africa. However, the large-scale response of the Eastern Mediterranean thermohaline circulation during these monsoon-fuelled freshening episodes is poorly constrained. Here, we investigate the formation of the youngest sapropel (S1) along an across-slope transect in the Adriatic Sea. Foraminifera-based oxygen index, redox-sensitive elements and biogeochemical parameters reveal – for the first time – that the Adriatic S1 was synchronous with the deposition of south-eastern Mediterranean S1 beds. Proxies of paleo thermohaline currents indicate that the bottom-hugging North Adriatic Dense Water (NAdDW) suddenly decreased at the sapropel onset simultaneously with the maximum freshening of the Levantine Sea during the African Humid Period. We conclude that the lack of the “salty” Levantine Intermediate Water hampered the preconditioning of the northern Adriatic waters necessary for the NAdDW formation prior to the winter cooling. Consequently, a weak NAdDW limited in turn the Eastern Mediterranean Deep Water (EMDWAdriatic) formation with important consequences for the ventilation of the Ionian basin as well. Our results highlight the importance of the Adriatic for the deep water ventilation and the interdependence among the major eastern Mediterranean water masses whose destabilization exerted first-order control on S1 deposition.
PY 2017
PD MAR
SO Quaternary Science Reviews
SN 0277-3791
PU Pergamon-elsevier Science Ltd
VL 159
UT 000395609300010
BP 139
EP 154
DI 10.1016/j.quascirev.2017.01.020
ID 48205
ER

EF