FN Archimer Export Format
PT J
TI Deltaic and coastal sediments as recorders of Mediterranean regional climate and human impact over the past three millennia
BT 
AF JALALI, Bassem
   SICRE, Marie-Alexandrine
   KLEIN, Vincent
   SCHMIDT, Sabine
   MASELLI, Vittorio
   LIRER, Fabrizio
   BASSETTI, Maria-Angela
   TOUCANNE, Samuel
   JORRY, Stephan
   INSINGA, Donatella Domenica
   PETROSINO, Paola
   CHALES, Fanny
AS 1:1,2;2:2;3:2;4:3;5:4,5;6:6;7:7;8:8;9:8;10:6;11:9;12:2;
FF 1:;2:;3:;4:;5:;6:;7:;8:PDG-REM-GM-LGS;9:PDG-REM-GM-LGS;10:;11:;12:;
C1 Univ Sfax, Fac Sci Sfax, GEOGLOB, Sfax, Tunisia.
   Sorbonne Univ, LOCEAN Lab, CNRS IRD MNHN, Univ Paris 06, Paris, France.
   Univ Bordeaux, EPOC UMR5805, Pessac, France.
   ISMAR CNR, Ist Scienze Marine, Bologna, Italy.
   Univ Aberdeen, Sch Geosci, Dept Geol & Petr Geol, Aberdeen, Scotland.
   CNR, IAMC, Naples, Italy.
   Univ Perpignan, CNRS, CEFREM UMR5110, Perpignan, France.
   IFREMER, Lab Geodynam & Enregistrement Sedimentair, Plouzane, France.
   Univ Federico II Napoli, Dipartimento Sci Terra Ambiente & Risorse, Naples, Italy.
C2 UNIV SFAX, TUNISIA
   UNIV PARIS 06, FRANCE
   UNIV BORDEAUX, FRANCE
   ISMAR, ITALY
   UNIV ABERDEEN, UK
   IAMC CNR, ITALY
   UNIV PERPIGNAN, FRANCE
   IFREMER, FRANCE
   UNIV NAPOLI, ITALY
SI BREST
SE PDG-REM-GM-LGS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 2.888
TC 17
UR https://archimer.ifremer.fr/doc/00441/55248/56729.pdf
   https://archimer.ifremer.fr/doc/00441/55248/56730.pdf
   https://archimer.ifremer.fr/doc/00441/55248/56731.xlsx
   https://archimer.ifremer.fr/doc/00441/55248/57169.pdf
LA English
DT Article
CR ESSCAR-9
BO Le Suroît
DE ;Sea surface temperatures;Higher plant biomarker;Deltaic sediments;NW and central Mediterranean;Last millennia
AB Deltaic and shallow marine sediments represent unique natural archives to study the evolution of surface coastal ocean water properties as compared to environmental changes in adjacent continents. Sea surface temperatures (SSTs) and higher plant biomarker records were generated from the Rhone and Var River deltaic sediments (NW Mediterranean Sea), and three sites in the South Adriatic Sea (Central/Eastern Mediterranean Sea), spanning all or part of the past three millennia. Because of the high sediment accumulation rates at all core sites, we were able to produce time series at decadal time scale. SSTs in the Gulf of Lion and the convection area of the South Adriatic Sea indicate similar cold mean values (around 17°C), and pronounced cold spells, reflecting strong wind‐driven surface water heat loss. However, they differ in the rate of post‐industrial warming, which is steeper in the Gulf of Lion. The three Adriatic Sea SST records are notably different reflecting different hydrological influence from near‐shore to open sea sites. The compositional features of higher plant n‐alkanes in the Rhone and Var delta sediments and inferred vegetation types show differences consistent with the latitudinal extension of the drainage basins of both river‐streams. In the Adriatic Sea, both coastal and open sea sediments indicate enhanced land‐derived material over the past 500 years, that is not seen in the NW Mediterranean cores. We suggest that increased erosion as the result of changes in land use practices is the most likely cause for this trend. 
PY 2018
PD JUL
SO Paleoceanography And Paleoclimatology
SN 2572-4517
PU Amer Geophysical Union
VL 33
IS 6
UT 000438667300003
BP 579
EP 593
DI 10.1029/2017PA003298
ID 55248
ER

EF