FN Archimer Export Format
PT J
TI High resolution evolution of terrigenous sediment yields in the Provence Basin during the last 6 Ma: relation with climate and tectonics
BT 
AF LEROUX, Estelle
   RABINEAU, Marina
   ASLANIAN, Daniel
   GORINI, Christian
   MOLLIEX, Stephane
   BACHE, Francois
   ROBIN, Cecile
   DROZ, Laurence
   MOULIN, Maryline
   POORT, Jeffrey
   RUBINO, Jean-Loup
   SUC, Jean-Pierre
AS 1:1,2,3;2:2;3:3;4:1;5:2,3;6:4;7:5;8:2;9:3;10:1;11:6;12:1,7;
FF 1:PDG-REM-GM-LGS;2:;3:PDG-REM-GM-LGS;4:;5:;6:;7:;8:;9:PDG-REM-GM-LGS;10:;11:;12:;
C1 Univ Paris 06, Sorbonne Univ, UPMC, UMR 7193,Inst Sci Terre Paris ISTeP, F-75005 Paris, France.
   CNRS, IUEM, UMR6538, Domaines Ocean, Plouzane, France.
   IFREMER, DRO GM LGG, Plouzane, France.
   Santos Ltd, Melbourne, Vic, Australia.
   Univ Rennes 1, Campus Beaulieu, Rennes, France.
   TOTAL, CSTJF, Pau, France.
   CNRS, UMR 7193, Inst Sci Terre Paris ISTeP, Paris, France.
C2 UNIV PARIS 06, FRANCE
   CNRS, FRANCE
   IFREMER, FRANCE
   SANTOS LTD, AUSTRALIA
   UNIV RENNES, FRANCE
   TOTAL, FRANCE
   CNRS, FRANCE
SI BREST
SE PDG-REM-GM-LGS
UM LGO
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
   copubli-int-hors-europe
IF 3.886
TC 18
UR https://archimer.ifremer.fr/doc/00310/42087/41520.pdf
LA English
DT Article
CR AM-MED-1
   SARDINIA
BO Le Suroît
   L'Atalante
AB Basin-wide correlation of Messinian units and Plio-Quaternary chronostratigraphic markers (5.3 Ma, 2.6 Ma, 0.9 Ma and 0.45 Ma), the mapping of total sediment thickness and the determination of overall sedimentary volumes enabled us to provide a high-resolution quantitative history of sediment volumes for the last 6 Ma along the Gulf of Lions margin. The results point to (i) a dramatic increase in terrigenous sediment input during the Messinian Salinity Crisis. This increased sedimentation reflects enhanced regional fluvial erosion related to the dramatic fall of Mediterranean base-level. Stronger weathering due to a regional wetter climate probably also increased erosional fluxes. (ii) A sediment input three times higher during the Plio-Quaternary compared to the Miocene seems in agreement with published measurements from World's ocean. However, the timing of this increase being uncertain, it implies that the trigger(s) also remain(s) uncertain. (iii) A decrease in detrital volume around 2.6 Ma is attributed to a regional change in the drainage pattern of rivers in the northwestern Alps. (iv) This study also highlights the Mid-Pleistocene Revolution around 0.9 Ma, which resulted in an almost doubling of sediment input in the Provencal Basin.
PY 2017
PD JUL
SO Basin Research
SN 0950-091X
PU Wiley
VL 29
IS 3
UT 000400617100004
BP 305
EP 339
DI 10.1111/bre.12178
ID 42087
ER

EF